Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 572 _____________________________ _____________________________ Cell Cycle Analysis of Archaea BY ANDRZEJ POPLAWSKI ACTA UNIVERSITATIS UPSALIENSIS UPPSALA 2000 Dissertation for the Degree of Doctor of Philosophy in Microbiology presented at Uppsala University in 2000 Abstract Poplawski, A., 2000. Cell Cycle Analysis of Archaea. Acta Univ. Ups., Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 572. 64 pp. Uppsala. ISBN 91-554-4825-9. In my thesis, the cell cycle analysis of archaea and hyperthermophilic organisms is presented for the first time. Crenarchaea from the genus Sulfolobus were used as a model system. Flow cytometry and light microscopy were applied to investigate the timing and coordination of different cell cycle events. Furthermore, DNA content, nucleoid structure, and nucleoid distribution at different stages during the cell cycle were studied. The Sulfolobus cell cycle was characterized as having a short pre-replication and a long post-replication period. The presence of a low proportion of cells with segregated genomes in the exponentially growing population suggested a considerable time delay between termination of DNA replication and full nucleoid segregation, reminiscent of the G2 period in eukaryotic cells. The first available collection of conditional-lethal mutants of any archaeon or hyperthermophile was used to elucidate the coordination of cell cycle events. The studies showed that chromosome replication, nucleoid partition and cell division in Sulfolobus acidocaldarius, which are normally tightly coordinated during cellular growth, could be separately inhibited or uncoupled by mutation. The ftsZ gene, which is involved in cell division in bacteria and euryarchaea, was isolated from the halophilic archaeon Haloferax mediterranei. Transcriptional start sites were mapped, and putative translation initiation elements were identified. In both the upstream and downstream regions of the ftsZ gene, open reading frames were found to be conserved within the genus Haloferax. Furthermore, at the 3’ end of the ftsZ gene, the homologs of the bacterial secE and nusG genes are conserved in almost all euryarchaea analyzed so far. The studies also demonstrated the functional conservation of the FtsZ protein in different archaeal species, as well as between euryarchaea and bacteria. Andrzej Poplawski, Department of Cell and Molecular Biology, Biomedical Centre, Uppsala University, Box 596, SE-751 24, Uppsala, Sweden Andrzej Poplawski 2000 ISSN 1104-232X ISBN 91-554-4825-9 Printed in Sweden by University Printers, Uppsala 2000 1. Introduction 1.1. Archaea and the concept of three domains of life. Application of molecular tools in taxonomy has led to the division of life on Earth into three evolutionarily distinct domains (Fig. 1); Archaea, Bacteria and Eukarya (188). Fig. 1. The tree of life based on SSU rRNA analysis. Underlined archaea from genus Sulfolobus and Haloferax were analyzed in this study. Figure was adapted from the references (5, 141). 7 The phylogenetic uniqueness of archaea was initially inferred from the comparison of SSU rRNA sequences (187), upon which Archaea was subsequently subdivided into Euryarchaeota, Crenarchaeota (188) and Korarchaeota (5). Delineation of archaea from bacteria, initially a controversial idea, gradually brought about new understanding of the relationships between prokaryotes and eukaryotes, and raised the importance of Archaea in the evolution of life on Earth (35, 186). The recognition of Archaea as a separate domain of life, and their extremophilic properties attracted the scientific interest to investigate the biological characteristics of this group of organisms. Studies of different cellular and molecular properties of archaeal cells, including lipid composition (89, 178), chemical composition of the cell wall (87, 88), DNA dependent RNA polymerases, translation factors and ribosomal proteins (3, 18, 192, 193), have supported the idea of archaea being distinct from bacteria and constituting a separate branch on the tripartite tree of life. The archaeal uniqueness was further supported by analysis of the first completely sequenced genome of the archaeon Methanococcus jannaschii, which revealed that more than half of the open reading frames had no homologs within the two other domains of life (19, 99). In addition, the mosaic structure of the M. jannaschii genome was reflected by the presence of either bacterial or eukaryal homologs. The bacterial homologs were represented mostly by genes involved in metabolism, while the eukaryotic homologs were found mostly among the genes responsible for the replication, transcription and translation machineries (19, 42, 99, 139). Subsequent analyses of genomes from other archaeal species belonging to either Euryarchaeota or Crenarchaeota (50, 57, 90, 91, 96, 163) led to similar conclusions, as those based on the analysis of the M. jannaschii genome. The presence of either bacterial or eukaryal homologs within archaeal genomes, suggests that by studying archaeal properties insights into corresponding features in either Bacteria or Eukarya could be obtained. Furthermore, the discovery of the mosaic structure of the archaeal genomes resulted in a hypothesis about a chimeric origin of both archaea (99) and eukaryotes (71, 110). Comparison of cellular features including RNA processing between the three domains of life and development of new methods for studying evolutionary relationships prompted some to favor a eukaryotic-like nature of the last common universal ancestor (LUCA). According to this hypothesis, prokaryotes including archaea could appear by a reductive evolution from an eukaryotic-like ancestor (56, 142, 145). 8 The structure of the tree of life was, furthermore, influenced by the choice of proteins used for phylogenetic analyses (18, 52, 56). Conclusions based on those analyses were sometimes contradictory to that inferred from the SSU rRNA sequences (18, 52, 68, 69, 70) because of one possibility such as the lateral transfer of genes among species (83, 123, 132). The uniqueness of archaea could still be supported however, by phylogenetic analysis using whole-genome comparisons (51). Thus, a new view of the organization of the tree of life was proposed with Archaea, Bacteria and Eukarya interconnected through the network of a horizontal traffic of genes (39). 1.2 Diversity of the Archaea. Archaea constitute a group of organisms found in many environments. Initially, the crenarchaea and euryarchaea were found in extreme environments with either high temperature, low or high pH, or high salinity (168, 170). Later, the application of PCR combined with SSU rDNA analysis revealed the ubiquity of archaea all over the planet: from hydrothermal vents, ocean and coastal waters, through marine and lake sediments, hot springs and soil (141, 168, 173), to the environment at the doorstep of our department in Uppsala. 1.3 Cellular and molecular features of the Archaea. Since my thesis concerns the properties of the archaeal cell cycle, as well as the structure and sequence of regulatory elements for such processes as transcription and translation, I have included a section describing some features of these mechanisms in the different domains of life. Note that the comparison does not reflect the presence of such features in all of the organisms within each domain, and that the picture may change as soon as more data becomes available. Table 1. Major cellular features in the three domains of life Characteristic Cell wall Bacteria Variable composition (murein present) Ester linked Absent Membrane lipids Eukaryotic-type cytoskeleton Nucleus Absent Organelles (mitochondria, Absent chloroplasts, Golgi apparatus) 9 Eukarya Variable composition (never murein) Ester linked Present Archaea Variable composition (never murein) Ether linked Absent Present Present Absent Absent 1.3.1 Transcription. The basal transcription machinery in archaea has been suggested to be a simplified version of the eukaryotic RNA polymerase II machinery (11, 148, 165, 179, 193). Both archaeal and eukaryal RNA polymerase II are multisubunit complexes. For example, both Sulfolobus acidocaldarius and yeast RNA polymerase consists of 12 subunits, in contrast to E. coli where the holoenzyme consists of only 4 subunits (Table 2). Table 2. Transcription in the three domains of life Characteristic Bacteria Eukarya RNA Single Three types polymerase 4 subunits (2α, β, β´) Multisubunit (12 subunits in yeast) Mode of RNA Recognition and Recognition and polymerase binding dependent binding dependent on binding to TATA-binding protein on σ factor promoter (TBP) Promoter core -35 box; -10 box RNA polymerase II: elements TATA box, Initiator element (INR), Downstream promoter element (DPE), TFIIB recognition element Transcription Usually not Transcription factor IIB initiation required (TFIIB) and other factor factors Other Multiple Multiple transcription factors m7Gppp cap Absent Present Polyadenyla- Long polyA tail Long polyA tail present tion absent mRNA Absent Present splicing Archaea Single Multisubunit (12 subunits in Sulfolobus) Recognition and binding dependent on TBP TATA box, TFB recognition element (similar to promoter elements for RNA polymerase II) TFIIB homologue (TFB) Eukaryotic and bacterial-like factors Absent Long polyA tail absent Absent As in most eukaryotic genes, the archaeal TATA box is localized about 30 bp from the transcription initiation start (11, 148, 165). Archaea contain a homolog of eukaryotic TATA binding protein (TBP), which specifically recognizes and binds to the TATA box in the promoter region before loading the RNA polymerase (11, 165, 179). In eukaryotes, TBP is essential for initiation of transcription in all three RNA polymerase systems 10 (185). All archaeal species with the exception of halophilic ones contain a single TBP (165). The TFB recognition element (BRE) is a binding site for transcription factor B (TFB). The archaeal BRE consists of a minimum of two adenines located around position -34 to -33 with respect to the transcription initiation site (164, 165). Upon binding to the BRE, the TFB forms a complex with the TBP that is necessary for the initiation of transcription. In some euryarchaea there are multiple TFB proteins (165, 174). In addition to TBP and TFB, archaea contain many other eukaryotic and bacterial-like transcription factors (10, 11, 103) that are required for the efficient regulation of archaeal transcription. 1.3.2 Translation. The translation process in archaea appears to have traits from both bacteria and eukaryotes (Table 3). Table 3. Translation in the three domains of life Characteristic rRNA Ribosomes (subunits) Shine-Dalgarno (SD) Translation initiation codons Translation factors Initiator tRNA m7Gppp cap Bacteria 5S, 16S, 23S 70S (30S + 50S) Present Eukarya 5S, 5.8S, 18S, 28S 80S (40S + 60S), 70S in organelles Absent Archaea 5S, 16S, 23S 70S (30S + 50S) Mainly AUG, Other initiation codons (GUG, UUG etc.) also used to minor extent Multiple initiation, elongation and release factors Formyl-methionine Absent Initiation essentially Mainly AUG, restricted to AUG Other initiation codons (GUG, UUG etc.) also used to minor extent Multiple initiation, Both eukaryal and elongation and bacterial-like factors present. release factors Methionine Methionine Present Absent Present SD-like sequences are present in many archaeal genes and are localized 3 - 10 nucleotides in front of the initiation codon (2, 11, 36). Recent experimental studies with Sulfolobus solfataricus demonstrated that the Shine-Dalgarno is essential for the initiation of translation, at least in crenarchaea (27). A SD-independent initiation of translation could proceed, but only after the artificial removal of the 5´ untranslated mRNA leader region in front of the initiation codon (27). In archaeal genes that lack SD, translation was suggested to start from the first initiation codon located downstream of the transcription initiation start (36). The process of 11 translation initiation of such genes in Sulfolobus might be enhanced by yet an unidentified sequence elements, located downstream of the initiation codon, inside a coding sequence (175). As in bacteria, archaeal ribosomes are composed of 30S and 50S subunits. Archaeal rRNA further parallels bacterial rRNA since it also consists of 16S, 23S, and 5S RNAs. Furthermore, archaea possess both bacterial-like and eukaryotic-like factors (104) required for different stages of the translation process. 1.3.3 Genome organization. The size range of an archaeal chromosome is on average similar to that of bacteria: about 1.7 – 5 Mb. Mesophilic archaea often contain megaplasmids (54). A 100 kb megaplasmid was detected in Halobacterium sp. NRC-1 (133), and in species from the genus Haloferax, the sizes of megaplasmids range from 130 kb to 620 kb (127). In addition to different types of plasmids, archaea contain a spectrum of different kinds of other genetic elements such as viruses, transposons and insertion sequences (191, 194). The DNA in mesophilic archaea is negatively supercoiled, and hyperthermophilic archaea contain relaxed to positively supercoiled DNA (23, 53, 73, 74, 111). The positive supercoiling was proposed to be created by reverse gyrase, which introduces positive supercoiling into covalently closed circular DNA (34, 53, 54, 111, 176). Several proteins including histone-like proteins and histones (found only in euryarchaea) (60, 108, 143, 154, 195), were implicated to actively participate in structuring the archaeal chromosome. Smc proteins, which are required for chromosome condensation, segregation and variety of other aspects of chromosomal maintenance within bacteria and eukaryotes (26, 75, 76, 79, 84, 85, 171) together with topoisomerases, have been detected in archaea as well (12, 44, 53, 54, 111). 1.4 Cell cycle. All cells grow, duplicate their genomic DNA, and divide in order to survive. The cell cycle has been divided into distinct stages called G1, S, G2, and M in eukaryotes, and B, C, and D in bacteria (137). The periods remain distinct and separate in eukaryotic cells, whereas in bacteria the boundaries overlap when the growth rate is so fast that the generation time is shorter than the time required to duplicate and segregate the genomes (i.e. when C+D is longer than the doubling time) (137). An enormous amount of data has been acquired for both the eukaryotic and bacterial cell cycles. Yet, almost nothing was known about the cell cycle features of archaea by the time I started my research. This was mostly due to limitations in the genetic systems, lack of conditional-lethal 12 mutants and technical problems which made it difficult to apply flow cytometry and microscopy to study these organisms. Below, I present the major known features about archaeal replication, partition and division before proceeding to the Present investigation and Discussion describing the archaeal cell cycle. 1.4.1 DNA replication. In eukaryotes and bacteria, a large number of replication genes have been identified and their products isolated and characterized biochemically to provide a detailed description of this process (4, 100, 181). In archaea, proteins essential in DNA replication (Table 4) were mostly found to be homologs of eukaryotic equivalents (12, 13, 18, 22, 41, 92, 106). Table 4. Replication in the three domains of life. Function Bacteria Eukarya Archaea Origin recognition DnaA Origin recognition complex (ORC) Orc1/ Cdc6 Replicative Helicase DnaB Mcm Single strand DNA binding protein Clamp loader Ssb Minichromosome maintenance proteins (MCM) Replication protein A (RPA) Rfc (2 subunits) Sliding clamp (processivity factor) Main replicative DNA polymerase DnaN Replication factor C (5 subunits) Proliferating cell nuclear antigen (PCNA) Family B γ complex Family C Rpa Pcna Family B or D (euryarchaea) Family B (crenarchaea) DNA ligase, ATP-dependent DNA strand DNA ligase, DNA ligase, ligation on NAD-dependent ATP-dependent lagging strand Processing and DNA Pol I, FEN 1, FEN 1, removal of RNaseH RNaseH RNaseH primers The table includes proteins with either identified or predicted functions. Very little is known about the number of origins of chromosomal replication in different archaeal species. The GC skew analysis based on the asymmetrical distribution of nucleotides or short oligomers on leading 13 and lagging DNA strands, and on the abrupt changes of such distributions in regions close to the origin and terminus of replication, were applied to search for origin of replication in archaeal chromosomes (62, 109, 150, 151, 153). This analysis failed to demonstrate the presence of skew distribution in M. jannaschii and Archaeoglobus fulgidus, suggesting that these species may initiate replication of chromosome from a multiple origins (153). Skew analysis suggested a presence of a putative single origin of replication in euryarchaea such as Methanobacterium termoautotrophicum and Pyrococcus horikoshii (109, 153). Using a combination of skew analysis and the identification of an early replicating chromosomal segment in synchronous cells, a single origin of replication was identified in Pyrococcus abyssi (131). In crenarchaea, the location and number of origins of replication remains to be identified. In all organisms, the initiation of chromosomal replication requires binding of an initiation factor at the origin. Such function is performed in bacteria by DnaA and in eukaryotes by proteins assembled as an origin recognition complex (ORC) (4). Eukaryotic ORC consists of six subunits. In archaea the presence of a homolog of the largest subunit of an eukaryotic ORC, ORC1, was identified, in the chromosome of Pyrococcus furiosus (92). A homolog of an eukaryotic Cdc6 protein was detected in several archaeal species. In eukaryotes CDC6 binds to ORC complex and participate in loading helicases (MCM proteins), required to unwind the double-stranded DNA. Both DNA binding and helicase activities were experimentally demonstrated for archaeal Mcm protein (25, 94, 177). Cdc6 protein also shows similarity at amino acid level to ORC1, what may suggest similarity in functions between both proteins (92). Archaeal Cdc6 might be involved in loading of helicases as well as function as an initiator protein (13). All DNA polymerases are grouped into a distinct families, referred as A, B, C and X according to their sequence similarity and drug sensitivity (18, 22). Members of family B DNA polymerases are found both within crenarchaea and euryarchaea (22, 92). In contrast to crenarchaea, which contain multiple family B polymerases, euryarchaea possess only one equivalent from the same group (21, 22, 43, 92). Similar to their eukaryotic counterparts several members of archaeal family B polymerases are sensitive to aphidicolin (22, 92). Some members of archaeal family B 14 polymerases contain protein introns, referred to as inteins (19, 22, 78, 92, 134, 144, 190). Recently a new class of polymerases, denoted as family D, was discovered in euryarchaea (22). In P. furiosus, the DNA polymerase from this family referred to as Pol D, was found to be a heterodimeric enzyme constituted of two subunits: large DP 2 subunit with catalytic activity, and small DP 1 subunit which shows significant similarity to the eukaryotic polα, polδ, polε polymerases (22, 92, 117). Usually, different types of DNA polymerases are assigned to replicative and/or repair synthesis and recombination. The exact role of archaeal DNA polymerases is not entirely understood (13, 18, 22, 92) and needs to be investigated further. A processivity factor stimulates the replicase activity of DNA polymerase (4, 92, 138, 181). It encircles the DNA strands and through interaction with DNA polymerase ensures the connection of the replisome with DNA template during replication (4, 138). Archaeal processivity factor was found to be a homolog of an eukaryotic protein called proliferating cell nuclear antigen (PCNA) (12, 13, 22, 41, 92). In all completely sequenced euryarchaea only one homolog have been identified (19, 22, 91, 92, 96, 163), while in crenarchaea multiple Pcna were detected (22, 32, 90, 92). In both Sulfolobus solfataricus and Pyrococcus furiosus, Pcna was experimentally shown to stimulate DNA polymerase activity (20, 32). Pcna is loaded onto a DNA template by a clamp loader, which in archaea is a homolog of the eukaryotic replication factor C (RFC) (12, 13, 19, 41, 90, 91, 92, 96, 163). In contrast to eukaryotic RFC, which consists of five subunits, archaeal Rfc is composed of only of two subunits (22, 41, 92, 93). The homologies found between eukaryotic and archaeal replication proteins strongly suggest that replication machinery is more reminiscent of its eukaryotic counterpart than the bacterial one. 1.4.2 Chromosome partitioning. The sequences reminiscent of centromere-like elements and homologs of ParA and ParB proteins, involved in plasmid and chromosome partitioning in bacterial cells (59, 126, 128, 158, 159, 184), were also identified in archaea (12, 24, 59, 126). Archaeal centromere-like elements have been implicated to be essential for plasmid stability (13, 127, 160). 1.4.3 Cell division. The FtsZ protein is present in almost all bacteria, archaea, and chloroplasts studied so far (115, 152). Recently, FtsZ was also identified in mitochondria (9, 48, 124). FtsZ polymerizes into a ring 15 localized at the septum during the division process, and was suggested to provide an infrastructure for other cell division proteins (15, 16, 46, 116, 120, 152). FtsZ was also proposed to participate in the cell constriction process through conformational changes of its protofilaments (114). The FtsZ protein of the euryarchaeon M. jannaschii (19) showed a high level of similarity in tertiary structure to eukaryotic tubulin (47, 113, 136). Tubulin and FtsZ constitute a separate GTPase family with a distinct GTP binding motif: GGGTG(T/S)G (33, 135). The similarities between tubulin and FtsZ suggest that FtsZ might be an ancestor of eukaryotic tubulin (45, 46, 49, 120). In addition to the FtsZ, euryarchaea contain the homolog of bacterial MinD protein (12, 58, 152). In bacteria MinD is required for proper positioning of the septum during the process of cell division (152). Both MinD and ParA belong to a superfamily of ATPases, which consists of many proteins, including those essential for plasmid and chromosome partitioning (98). Database searches using archaeal homologs to bacterial Soj protein, which is required during the sporulation and for proper plasmid and chromosome partitioning (172), recognized MinD proteins and vice versa (12), what may suggest partially overlapping functions of MinD and Soj proteins in archaeal cells (12). 16 2. Present investigation Part I: Cell cycle characterization of Sulfolobus (papers I and II) 1.1 The use of Sulfolobus in cell cycle studies. The idea of archaea constituting a separate domain of life generated significant interest in studying the cellular and molecular properties of this group of organisms. However, the archaeal cell cycle remained uncharacterized when I focused my research interests on these organisms (see Introduction). The hypothesis of crenarchaea being relatives of eukaryotic organisms (149) had an influence on my decision to leave my studies of E. coli in order to analyze the archaeal cell cycle. I was interested in understanding to what extent the archaeal cell cycle displayed unique characteristics, and which properties were reminiscent of those found in bacterial and eukaryotic cell cycles. By testing a variety of archaeal species, I found that crenarchaea from the genus Sulfolobus were relatively easy to grow, since they did not require strict anaerobic conditions and high pressure for cultivation as many other archaea do. Moreover, and contrary to halophilic archaea, Sulfolobus cells were relatively easy to keep intact during the experiments. For these reasons, I chose the crenarchaeal species Sulfolobus acidocaldarius and Sulfolobus solfataricus as my primary subjects for the first cell cycle analyses of archaea and hyperthermophilic organisms. Before describing my experimental work, I will briefly outline the major genetic and physiological features of the genus Sulfolobus. 1.2 Properties of genus Sulfolobus. A characteristic feature of the members of the genus Sulfolobus (17) is that they are thermoacidophiles (169, 170). The optimum growth temperature and pH are about 80°C and pH 3, respectively (64, 169). The doubling time varies between 4 - 8 hours. The cells are surrounded with a glycoprotein S layer (64, 88, 147, 183). The sizes of the Sulfolobus genomes are about 3.0 Mb (8), and the genomic base composition is around 37% GC (63, 157). Sulfolobus cells possess reverse gyrase (95), which introduces positive supercoiling into covalently closed circular DNA (53, 54, 55, 95), and is suggested to be essential for stable maintenance of the chromosome at high temperatures (53). 1.3 Introduction to flow cytometry. The flow cytometry technique has been successfully applied in cell cycle studies of both eukaryotic and 17 bacterial organisms (31, 161, 162, 167). In flow cytometry, cells fixed and stained with DNA-specific fluorescent dyes pass through a measuring window at high speed. The light scatter (a measure of cell size) and the fluorescence (reflecting DNA content) for each cell is recorded, registered and analyzed by the computer software. DNA content and cell size in a population can then be represented as a two- or three-dimensional plot (Fig. 5, paper I). From DNA content distribution, the proportion of cells in different stages of the cell cycle can be measured and the length of the different cell cycle periods can be calculated. 1.4 Control experiments. We used flow cytometry to analyze the DNA content and cell size distributions of Sulfolobus species. In parallel, I studied the structure and distribution of their chromosomes within archaeal cells, using phase-fluorescence microscopy, after staining with DNAspecific dyes. Since this was the first time such analyses were performed with archaea, we designed control experiments to ensure the accuracy and reliability of our studies (Fig. 2, paper I). Treatment of cells with DNase resulted in total loss of fluorescence signal, without any affect on the light scatter distribution. Treatment with proteinase K did not significantly influence the DNA content distribution of the population, though there was a reduction in the light scatter signal. Microscopy revealed that ethanol fixed cells followed by proteinase K treatment became transparent (not shown). The fluorescence signals, however, were still maintained by the cells (not shown). Hence, proteinase treatment did not significantly alter the integrity of the S layer but most probably had an influence on the content of internal cellular proteins. There was almost no effect on DNA content and cell size distributions after treatment with RNase. Combined treatment with RNase A and proteinase K affected the light scatter distribution, but not the shape of the DNA content distribution. The fluorescence signals were slightly reduced upon such treatment. When DNA content and nucleoid structure in cells treated by Dnase, Rnase A, and proteinase K were analyzed by microscopy (Fig 1, paper II), the results were essentially the same as those obtained by flow cytometry. In conclusion, these experiments demonstrated that the fluorescence signals corresponded to DNA. Hence these techniques could be used for the visualization of DNA and determination of DNA content. 1.5 Genome sizes and numbers. Estimates of genome sizes of Sulfolobus species have been published previously. The genome size of S. solfataricus (DSM 1617) was estimated to be 3.1 Mb (157), while S. acidocaldarius 7 18 had a genome size of 2.7 Mb (97). We used flow cytometry to compare with the available data, genome sizes of Sulfolobus species analyzed in this study. In agreement with published data, the genome size of S. solfataricus (DSM 1616) was found to be significantly larger than that of S. acidocaldarius (DSM 639) both in the stationary and exponential phases. This difference was irrespective of the stains: 4-6-Diamidino-2phenylindole (DAPI), Hoechst (Fig. 3, paper I) or mixture of mithramycin and ethidium bromide (MEB) used in the analysis (paper I). To determine the DNA content of Sulfolobus with regard to the size and number of chromosomes, E. coli cells with known integral number of chromosomes were used as a reference scale (not shown). Using this scale, the DNA content from exponential phase cells, corresponding to the first and second peaks (Fig. 2 and paper I) were found to reflect one and two genome equivalents, respectively. Cells from the stationary phase were found to contain almost exclusively two genome equivalents (Fig. 2 and paper I). When non-intercalating drugs such as DAPI (28) were used, the genome sizes of both S. acidocaldarius and S. solfataricus were estimated as less than 15% from the predicted values. The flow cytometry analysis using MEB resulted in an underestimation of the Sulfolobus genome size. Furthermore, flow histograms of MEB-stained DNA showed a slightly displaced location of the 2-genome peak in stationary phase (Fig. 6, paper I), which was not apparent when non-intercalating drugs were used (Fig. 2). Since the GC content is 37% in Sulfolobus and 50% in E. coli, underestimation of the size of Sulfolobus genome using the MEB stain could be explained by the preferential binding of mithramycin to GC-rich regions (28). In addition, as DNA is negatively supercoiled in bacteria, and in a relaxed to positively supercoiled state in thermophilic archaea (53, 73, 74, 111), superhelicity could as well affect the DNA-binding properties of different drugs. In conclusion, the number of Sulfolobus genomes alternates between one and two in the exponential phase, and upon entering stationary phase Sulfolobus cells contain two genome equivalents. Furthermore, this experiment provided an easy way to estimate relative sizes of archaeal genomes. Exact determinations of genome size require comparisons between species with the same, or closely similar, GC content and chromosomal structure. 1.6 The cell cycle. The DNA content distributions obtained from the flow cytometry analyses (Fig. 2) were used to calculate the lengths of the 19 different cell cycle periods (Fig. 9, Discussion) with the help of computer simulations. The amount of cells in the B, C and D periods was estimated and converted to relative lengths of the cell cycle periods as described in paper I. The DNA content distribution in an exponentially growing culture of S. acidocaldarius was found to be slightly dependent on the optical density at the time of sampling. Therefore a range of values is given below for the length of the cell cycle periods in this species. The B period in both Sulfolobus species occupied not more that 5% of the cell cycle. The length of the C period was calculated to be 37% (157 min) for S. solfataricus, and ranged between 26 - 40% (55 to 85 min) for S. acidocaldarius. The postreplication period was estimated to be 60% in S. solfataricus and between 58 - 72% (124 - 153 min) for S. acidocaldarius. The flow cytometry analysis indicated that most of the cells contained two genome equivalents, while microscopy demonstrated that in a majority of the cells a single fluorescence focus was present (Fig. 2). Fig. 2. DNA content distributions and nucleoid visualization in S. acidocaldarius cells from exponentially growing (upper panels) and stationary phase (lower panels) cultures. The cells were fixed in ethanol and stained with DAPI before analysis. Arrows indicate cells with two separated nucleoids, as well as dividing cells. The bar is equal to 2 µm. 20 The number of cells in the population with two fully separated nucleoids was estimated by microscopy to be about 4% for S. solfataricus and 5% for S. acidocaldarius. Thus, most of the fluorescence foci should contain two unseparated genomes. This feature indicated that G2 stage (see section 1.4, Introduction) was a part of the Sulfolobus cell cycle. This period was estimated to occupy about 50% of the cell cycle. The T period (the time from the initiation of visible septum constriction to cell separation (72)) was estimated by calculating the percentage of cells in the population with visible constriction. This period was found to be 4% (19 min) and 5% (13 min) for S. solfataricus and S. acidocaldarius, respectively. In conclusion, our analysis showed, that a short B and a long postreplication period characterizes the cell cycles of both S. acidocaldarius and S. solfataricus. In addition, the G2-like period, which constitutes a part of the postreplication stage, was found to occupy a large fraction of the Sulfolobus cell cycle (paper I and II). 1.7 Nucleoids of Sulfolobus cells. Studies of chromosome distribution and structure have not been performed previously for any archaeon or hyperthermophile. Therefore, nucleoid structure from both the exponential and stationary phases of Sulfolobus cells was analyzed either in ethanolfixed or living cells (Fig. 3). A B C D Fig. 3. Nucleoid structure in the exponential and stationary phases of S. acidocaldarius cells. A and B, staining with DAPI of living cells from exponential (A) or stationary phase (B). C, DAPI staining of ethanol-fixed mixed population containing exponential and stationary phase cells. D, phase contrast illumination of C. 21 Both approaches showed that the structure of the Sulfolobus nucleoid differs between cells analyzed in the exponential and stationary phases (paper II). 1.7.1 Nucleoid structure in exponential and stationary phases. The stationary phase nucleoid was represented by a single fluorescence focus, which covered most of the cell interior and had few distinguishable features as compared to those from the exponential phase (Figs. 2 and 3). The structure of the nucleoid was not affected by the type of treatment and was similar in both ethanol-fixed and living cells (Fig. 3). Furthermore, the transparent appearance of the cells from the stationary phase (Fig. 3), after ethanol fixation, suggested differences in cellular properties as compared to exponentially growing cells. 1.7.2 Nucleoid distribution in exponential phase. In order to unravel the pattern of chromosome partitioning, a search for cells in different stages of nucleoid processing was performed for both Sulfolobus species (Fig. 4). A B C D E SA SS Fig. 4. Nucleoid structure and distribution in Sulfolobus cells. SA, S. acidocaldarius, SS, S. solfataricus. Column A, cells with a single nucleoid. B, cells with two nucleoids aligned in parallel. C, cells with separated nucleoids. D, cells with separated nucleoids and visible constriction. E, complex nucleoid structures. The majority of the cells in both S. acidocaldarius and S. solfataricus contained a single fluorescence focus, localized in the middle or at the side of the cell (column A). A small proportion of the population contained two nucleoids, displayed as clear foci or arcs within the cells. Column B shows cells in which the two nucleoids were aligned in parallel. Column C indicates cells containing fully separated nucleoids located at opposite sides of the cell. This nucleoid localization pattern was preserved during 22 cell division, as shown in column D. Examples of aberrant nucleoid structures are demonstrated in column E. 1.8 Morphological features. An unusual morphological feature which we called budding was observed in S. solfataricus and S. acidocaldarius cells under particular conditions. Budding was sporadically present in cells from the exponential phase, analyzed either directly under the microscope or after spreading on agar containing 10 mM Tris-HCl. A high number of buds was observed when cells from a liquid culture were spread onto 1% gelrite or agar in water (Fig. 5). Pronounced budding was also detected in S. acidocaldarius after prolonged incubation with DAPI (not shown). A B A S. acidocaldarius B S. solfataricus Fig. 5. Examples of budding Sulfolobus cells. Cells from exponentially growing cultures were observed by microscopy after spreading on 1% gelrite in water (column A) or 1% agar in water (column B). The upper row represents phase contrast illumination, while the middle and bottom rows show nucleoids in budding cells after the live cells were stained with DAPI for 60 min (followed by the same treatment as in row 1). 23 Part II: Conditional-lethal mutants of S. acidocaldarius (paper III) 2.1 Isolation of mutants. A major step towards further analysis of the Sulfolobus cell cycle was achieved with the first isolation and characterization of conditional-lethal mutants of S. acidocaldarius. Conditional-lethal mutants are required to study the function of essential genes (86, 119). In a conditional-lethal mutant, substitutions in the amino acid sequence of a protein result from the treatment of the cells with a mutagen. This affects proper folding of the mutant protein, and alters its activity under conditions which have no influence on the corresponding properties of the wild-type protein (86, 119). During exposure to the nonpermissive condition, the mutated protein can lose its activity completely or partially, depending upon the substitution. The isolation of conditional-lethal mutants of S. acidocaldarius was accomplished by chemically mutagenizing the cells of strain DG64 with nitrosoguanidine. Nitrosoguanidine is a mutagen known cause transitions, transversions, and -1 frameshift mutations (166). Mutants of S. acidocaldarius, which failed to grow on solid media after a shift from 70°C to 83°C, were isolated. The non-permissive temperature was close to the optimal growth temperature for wild-type Sulfolobus cells. At permissive temperature, the DNA content distributions, nucleoid structure, cell morphology and growth properties of the mutants were found to be similar to those observed for the DG64 parental strain (paper III, and Fig. 6). After the shift to the non-permissive temperature, growth and viability of the parent strain DG 64 was not affected (Fig. 3, paper III). Flow cytometry experiments showed that the percentage of cells in the B and C periods in this strain decreased slightly after the shift, but the shape of the DNA content distribution was similar to that at the permissive temperature (Fig. 2, paper III). Furthermore, nucleoid structure of DG64 after the shift was similar to that observed at 70°C (Fig. 2, paper III). Since the flow cytometry and microscopy parameters of the DG64 parent strain remained similar at both temperatures, differences in the phenotypes of the various mutants were likely to have resulted from mutations. 2.2 Phenotypic reversion. The observed phenotypes of the conditionallethal mutants of S. acidocaldarius could be due to mutations in several genes. Reversion of the mutations, which completely or partially restore the wild-type phenotype of the cell, can occur through a suppressor mutation 24 introduced either outside the gene (extragenic suppression) or in the same gene (intragenic suppression). Alternatively, mutations can revert by a true reversion which restores the wild-type sequence of the gene (86, 119). Single mutations will revert at much higher frequencies compared with multiple mutations. For example, if the reversion frequency of a point mutation in gene of E. coli was about 10-8 revertants per generation (119), than the reversion frequency of a double mutation would be at the level of 10-16. The values of reversion frequency observed in our collection of conditional-lethal mutants, were about 10-6 to 10-7 (Table 5), and were close to the frequencies of spontaneous pyrE and pyrF mutants of S. acidocaldarius (82). This is much higher than would be predicted by two or more independent reversions. Hence, we assumed that only one gene was affected in most of the mutants. 2.3 Classes of mutants. A final collection of 34 conditional-lethal mutants grown in liquid medium at 70°C were analyzed for alterations in DNA content, nucleoid structure and cell size distributions, after a shift to the non-permissive temperature of 81°C. Flow cytometry and microscopy analysis, together with measurements of growth and viability, were used to divide the mutants into five classes (Table 5). 2.3.1 Class I. Mutants from this class were characterized by arrest in the post-replication stage. Class I was further subdivided into subgroups Ia and Ib (Table 5). Class Ia was characterized by the uncoupling of cell growth from replication, as demonstrated by mutant DG132. A continuous increase of cell size without concomitant cell division, after a shift to the nonpermissive temperature, was observed in both flow cytometry and microscopy analysis (Fig. 6). There was also a decrease in the growth rate accompanied by a slight decrease in cell viability (Fig. 3, paper III). Arrest at the post-replication stage along with the absence of cells with one genome equivalent observed after the shift (Fig. 6), suggested that ongoing replication was allowed to finish but that no new initiation of replication occurred. Continuous changes in nucleoid structure were evident, especially at late time points in the experiment. The nucleoids became highly unstructured and were usually localized to the side of the cells (Fig. 6). In addition, cells with reduced fluorescence signals, probably representing DNA degradation, were detected. 25 In mutants from class Ib, represented by DG146, replication was again blocked about 3 hours after the shift, and the cells were arrested in the post-replicative period for the rest of the experiment (Fig. 6). In contrast to DG132, little or no cellular growth occurred in DG146, as indicated by the largely unaffected light scatter distribution (Fig. 6) and growth measurements (Fig. 3, paper III). Cells of DG146 were viable for more than 30 hours after the shift. A dramatic drop in cell viability (Fig. 3, paper III), and DNA degradation (Fig. 6), was observed 48 hours after the shift to nonpermissive temperature. 2.3.2 Class II. Mutants from classes II to V (Table 5) were not arrested in specific cell-cycle periods after the shift to non-permissive temperature. Mutants from class II were characterized by a progressive decrease in growth followed by loss of cell viability (Fig. 3, paper III), which coincided with DNA degradation inside the cells (Fig. 6). 2.3.3 Class III. This class (Table 5) is represented by DG134 and is characterized by an increase in both DNA content and cell size after the shift to non-permissive temperature. The growth and viability were undisturbed for at least 10 hours after the shift and were slightly reduced at later time points of the experiment (Fig. 3, paper III). Flow cytometry revealed that there was no arrest in the post-replication stage after the shift. Instead, the DNA content and cell sizes continued to increase (Fig. 6). The increase in DNA content was evident at late time points as peaks corresponding to up to 5 genome equivalents emerged in the population (Fig. 6). In addition, a large broadening of the light scatter distribution was observed (Fig. 6) what suggests that the growth of some cells in the population was inhibited at different time points of the experiment. Although some DG134 cells with unstructured nucleoids similar to those observed in DG132 were detected, the presence of many cells with clearly separated nucleoids at late time points during the experiment (Fig. 6) provided evidence for an actively operating partitioning system at nonpermissive temperature in this mutant. In addition, transparent cells, most probably resulting from the loss of cellular integrity, were present at a low frequency within the population. 2.3.4 Class IV. The shift to non-permissive temperature did not result in pronounced changes in the growth rate or morphology of the mutants from this class. This class was characterized by the presence of cells with more than 2 genome equivalents after overnight incubation at 81°C (Table 5). 26 2.3.5 Class V. Mutants from this category did not show any detectable phenotype within the time used for our analysis (usually more than 24 hours). However, the conditional-lethal phenotype was evident upon extended incubation on plates and liquid media (not shown). Fig. 6. Examples of conditional-lethal mutants with interesting cell cycle phenotypes. Bar equal to 2 µm. 27 Table 5. Phenotypic effects after the shift to non-permissive temperature*. Mutant class Ia Ib 4 5 Number of isolates 132 146 Representative strain (DG number) Flow cytometry 1. Cell cycle arrest in D period 3 3 2. Cells with >2 chromosome equivalents (o/n) 3. Cell size increase + 4. DNA degradation o/n o/n Mass increase after shift 1.Significant decrease as compared to wt + + + 2. Rapid growth arrest† 1.2 x 10-7 5.8 x 10-7 Reversion frequency (S.D.) (1.4 x 10-7; (5.9 x 10-7; n = 7) n = 5) IIa 5 149 IIb 3 155 III 4 134 IV 3 117 10 (+) 6 6 + - (o/n) - + - + (+) 1.3 x 10-7 (8 x 10-8; n = 6) + 8.2 x 10-6 (1x 10-5; n = 3) - *Designations: +, phenotype present; -, phenotype absent; 3, 6, 10, o/n, hours post-shift at which the phenotype first became evident. Parentheses indicate an intermediate phenotype. † OD increase corresponding to less than one mass doubling after the temperature shift to 81°C. Parentheses indicate a mass increase corresponding to between one and two mass doublings. Part III: The Haloferax mediterranei ftsZ gene (paper IV) 3.1 The idea behind the project. The ftsZ gene is important for cell division in prokaryotic organisms (see Introduction). The interesting morphological properties of halophilic archaeon H. mediterranei prompted us to initialize an investigation of the cell division process by analyzing the structural and functional properties of the ftsZ gene and protein in this organism. 3.2 The H. mediterranei ftsZ gene. Preliminary experiments demonstrated that primers directed against the Haloferax volcanii ftsZ gene (182) also hybridized to H. mediterranei DNA. Hence, about 20 different primers covering the entire ftsZ gene region of H. volcanii (GenBank Accession No. U37584) (182) were designed. The ftsZ gene region from H. mediterranei (1983 bp) was then amplified and sequenced (GenBank Accession No. AF196833). The ftsZ gene was localized within the sequenced region, the average GC content, transcription and translation regulatory elements, and other properties were determined (Table 6). Table 6. The main features of the ftsZ gene of H. mediterranei (GenBank accession No. AF196833) Gene Type Length Base count Average GC content TATA box (positions with reference to the No. AF196833 nucleotide sequence) Shine-Dalgarno Initiation codon Termination codon Length of the FtsZ protein Identity with the entire H. volcanii ftsZ gene ftsZ paralog 1 1092 nt 225 A, 326 C, 341 G, 200 T 61% 5´-TAATTA-3´ (410-415) Identity with the entire H. volcanii FtsZ protein GTP binding motif Z-ring (FtsZ ring) at division site ftsZ flanking gene at 5'-end ftsZ flanking genes at 3'-end 97% 5´-GAGG-3´ (475-478) 5´-ATG-3´ (487-489) 5´-TAG-3´ (1576-1578) 363 aa 90% GGGTGTG (868-888) present orf X secE, nusG 29 Phylogenetic analyses of ftsZ genes revealed that they branch into two separate clusters, denoted as paralog 1 and paralog 2 (49). The high sequence identity at both the nucleotide and amino acid levels between the H. mediterranei and H. volcanii ftsZ genes and proteins automatically grouped ftsZ of H. mediterranei as a paralog 1 (Table 6). 3.3 Transcription initiation signals. The transcription initiation start site was mapped using primer extension analysis (Fig. 2, paper IV). The putative TATA box was found to be localized about 30 nucleotides upstream of the transcriptional start site for the ftsZ gene (Table 6). 3.4 Shine-Dalgarno sequence. There are at least two potential SD sequences (SD) for the ftsZ gene in both H. mediterranei and H. volcanii. In both strains, one SD was located 3 bp and the other one 9 bp upstream of the 2nd putative translation initiation codon of the ftsZ gene (Fig. 1, paper IV). In H. volcanii, an additional potential SD sequence was localized 15 bp upstream of the 2nd initiation start codon. In H. mediterranei, the distance between one of the SD sequences and the initiation codon was the same as that for the nusG gene in the same region. This sequence was therefore suggested as the probable recognition site for translation. 3.5 Frameplot analysis. In species with high chromosomal GC content, there is an uneven distribution of the GC content within the codons. The average GC content is the highest at the third position and the lowest at the second position (14). This non-random GC distribution allows for the determination of coding regions (14, 81). In addition, translational start and stop codons are indicated by the program. These are usually located on the border between the random and non-random GC distribution. 3.5.1 Translation initiation starts. Considering the results from the examination of the nucleotide sequence, there could be three possible translation initiation start sites (ATG) for the ftsZ gene in both H. mediterranei and H. volcanii. The frameplot analysis was used, in order to differentiate between these alternatives (Fig. 7). The analysis showed that the 1st codon was located on the ascending part of the GC distribution, the 2nd on the border between random and non-random distribution and the 3rd well inside the coding sequence (Fig. 7) and hence rejected as a potential start site. The presence of the SD element in front of the 2nd ATG codon 30 was used as evidence that this codon was the preferred translation initiation codon for the ftsZ gene in both Haloferax species. Fig. 7. Frameplot analysis of the ftsZ gene region of H. mediterranei (GenBank Accession No. AF196833) and H. volcanii (GenBank Accession No. U37584). The relative GC content in different codon positions is shown in a graphical representation with open reading frames indicated above the graphs. The possible translation initiation codons and their orientation are indicated by arrowheads (<, >). Vertical bars indicate the possible stop codons. The putative translation initiation and stop codons for the ftsZ 31 gene, as well as for other genes from the analyzed region are indicated below each graph. 3.5.2 GTP binding motif of the FtsZ protein. The first and the second nucleotide in all glycine and threonine codons are GG and AC, respectively. Since the GTP binding motif of the FtsZ protein (Table 6), consists of 71.4% glycine and 28.6% threonine, it could be directly identified by frameplot analysis as a pronounced increase in the average GC content at the second position within the codons (Fig. 7). 3.5.3 Conserved gene order in the ftsZ gene region. Frameplot and database analyses revealed the existence of conserved ORFs both upstream and downstream of the ftsZ gene (Fig. 7 and Table 6). The analyses demonstrated the presence of the orfX gene upstream of the 5´-end, conserved only within the genus Haloferax. The same analyses showed a conserved cluster of secE and nusG genes located downstream of the ftsZ gene. This cluster, together with downstream ribosomal genes, is preserved in almost all archaeal and bacterial organisms (49, 180). 3.6 Functional conservation of the FtsZ protein. The extensive identity at the amino acid level among the Haloferax FtsZ proteins (Table 6) prompted us to perform immunolocalization studies of the FtsZ protein in paraformaldehyde-fixed H. mediterranei cells, using an antibody directed against the H. volcanii FtsZ (Fig. 8). In H. mediterranei, in most of the non-constricting cells and in cells with asymmetric constrictions, any formation of the FtsZ ring (Z-ring) was not detected (row F). Some cells contained a fluorescent half-band (row D) probably a Z-ring under construction, although a poor access of antibody in such cells cannot be excluded. In most cases, for H. mediterranei (row A, B and C) as well as for H. volcanii (row G), the FtsZ protein was visualized as a fluorescent band across the cells. The demonstration of a clear ring structure was possible for a few cells (row A). 32 Fig. 8. Examples of immunolocalization of the FtsZ protein in H. mediterranei and H. volcanii. Cells from exponentially growing culture of H. mediterranei and H. volcanii were chemically fixed in paraformaldehyde, and after the immunolocalization of the FtsZ protein were performed, as described in paper IV. Bar corresponds to 2 µm. 33 3. Discussion Part I: Cell cycle analysis of Sulfolobus (papers I, II and III) 1.1 Introduction. The combination of flow cytometry and microscopy has been successful in cell cycle studies of bacteria and eukaryotes (see section 1.3, Present investigation), and the work presented in this thesis demonstrates that this approach could also be used for the first cell cycle analysis of archaea. This study revealed interesting characteristics of the Sulfolobus cell cycle (Fig. 9), including features reminiscent of those observed in both bacteria and eukaryotes. Below, I will discuss properties of the cell cycle, nucleoid organization, different morphological features, and the use of conditional-lethal mutants. Fig. 9. The cell cycle of Sulfolobus. A, relative lengths of the cell cycle periods is indicated in the pie graph. Cells are indicated as circles outside the pie graph. Cells with the striped area are in the replicative period (C period), while cells with filled areas are either in prereplicative (B period) or postreplicative period. Postreplicative period consists of G2, Partition and Division (G2, Par and D) stages. B, DNA content distribution obtained by flow cytometry analysis of exponentially growing culture. 34 1.2 The B period. The small amount of time occupied by the B period during the cell cycle (about 5%) indicates that the replication machinery is competent for initiation early after cell division. As the nucleoids are localized to opposite cell halves during the division period (Fig. 4 column D), the B period could be devoted to structural changes and physical movement of the chromosome or origin of replication to a particular place in the cell. Physical movement of the origin of replication to a place containing components of the replication machinery has been shown in bacteria (107, 112), and may be required for triggering the initiation of replication in Sulfolobus cells. 1.3 The C period. The genome of Sulfolobus species is about 40% smaller as compared to E. coli, but the length of DNA replication period was found to be similar to that of E. coli growing within the same range of doubling times. The growth temperature of Sulfolobus cells is above the melting point of their DNA. At high temperature, there is a pronounced deamination of cytosine compared to mesophilic growth conditions (61). Since the mutation rate in Sulfolobus living in extreme environments corresponds to the values observed for E. coli (82), Sulfolobus cells may have developed a DNA repair system (66) able to cope with the denaturation and thermodegradation of DNA. Archaeal DNA polymerases were shown to recognize uracil generated as an effect of the deamination of cytosine and to stop in front of such lesions until they are repaired (61, 105). Frequent stops of the replisome caused by the need for removal of DNA lesions by a DNA repair system could therefore result in an increased length of the C period. The differences in the length of the C period could also be due to other features, such as differences in the replication machineries or differences in chromosome structure between archaea and bacteria. Very little is known about the regulation of Sulfolobus DNA replication. By taking into consideration the difference in genome sizes between E. coli and Sulfolobus, a reasonable assumption is that there is a single origin of replication. Multiple origins would decrease the time required for replication of the Sulfolobus chromosome and shorten the length of DNA replication period. 1.4 The G2 period. Analysis indicating a low proportion of cells with two segregated genomes in the population suggests a considerable time delay between termination of DNA replication and full chromosome separation. Thus, a period reminiscent of the G2 stage in the eukaryotic cell cycle (129, 35 137) is proposed to be present in Sulfolobus cell cycle. The G2 period constituted about 90% of the post-replication period. The low proportion of cells with fully separated nucleoids in Sulfolobus could suggest that the chromosomes may remained connected after the completion of replication, as was postulated for the eukaryotic G2 phase (129). During the long G2 stage, possible DNA damage could be repaired through recombination between the two copies of Sulfolobus chromosome. The use of multiple copies of the chromosome, and homologous recombination as a defense mechanism against lethal effects of the environment was suggested for the bacterium Deinococcus radiodurans, which has an extraordinary capacity to withstand high levels of damaging agents such as ionizing or UV radiation (6, 7, 29, 125). Similar systems protecting the chromosome from the lethal effects of high temperature might operate in Sulfolobus, although this must be experimentally proven. The reason for the presence of two genome equivalents in the G2 period might also be the maintenance of a second copy without the need for recombination. Such a strategy might assure survival of the cell in extremophilic conditions, if damage would occur in one of the copies of the genome. 1.5 DNA partition. A rearranged structure of the Sulfolobus nucleoid was observed in cells, which had entered the partition stage (Fig. 4, column B). Paired nucleoids were highly condensed, and their alignment was reminiscent of that observed for eukaryotic chromosomes during mitosis. Such similarities may indicate that certain stages of the partition process in Sulfolobus could be similar to that observed during eukaryotic mitosis. In contrast to slowly growing bacteria in which chromosome partitioning may be a gradual process occurring during replication (189), Sulfolobus cells appeared to partition their chromosomes during a limited time period of about 5% of the cell cycle, suggesting rapid movement towards the opposite halves of the cell. Recent studies showed the presence of nucleotide repeats in both Sulfolobus chromosome (24) and Sulfolobus pNOB8 plasmid (160). Such repeats are implicated in process of chromosome and plasmid partitioning in prokaryotes (126), and could possibly represent archaeal equivalent of centromere-like element (13, 24). The genes encoding putative ParA and ParB proteins were found in the Sulfolobus pNOB8 plasmid (12, 13, 24, 160). These proteins are homologs of sop/par genes involved in chromosome and plasmid partitioning in bacterial cells (59, 128). Par B protein binds to centromere-like element 36 and participates in partitioning by utilizing the energy from the ATP hydrolysis, which is provided by ParA (59, 128, 159). Nucleotide repeats identified in the Sulfolobus chromosome may constitute binding sites for protein(s) actively participating in process of chromosome partitioning, in a manner similar to that, described for a bacterial Par A and ParB proteins. Under physiological conditions, initiation of chromosomal replication in Sulfolobus is dependent upon the completion of both chromosome partitioning and cell division (paper I and (77)). Such coupling can be destroyed in the conditional-lethal mutants of S. acidocaldarius (e.g. DG134), in such a way that both chromosome replication and partitioning remain active in the absence of cell division (Fig. 6 and paper III). Results from experiments with another mutant DG132 showed that in the absence of chromosome partitioning, DNA replication is inhibited as well (Fig. 6 and paper III). Hence, these results together indicate that, in Sulfolobus cells chromosome partitioning but not division is the process essential for the initiation of chromosomal replication (paper III). 1.6 Cell Division. The similarity between the T period (the time from the initiation of visible septum constriction to separation of the cells (72)) in Sulfolobus and slowly growing bacteria (paper I) might indicate that the septation process operates through a bacterial-type mechanism. However, there is no FtsZ protein in crenarchaea and so far there is no information about the presence of any other cell division proteins in Sulfolobus. Furthermore, the only experimental evidence so far, for the mechanism of crenarchaeal cell division, was a demonstration of snapping division in vivo in Thermoproteus tenax (80). Whether the same or similar mechanism for cell division operates within Sulfolobus remains an open question. The active replication in the absence of cell division observed after the shift to the non-permissive temperature of the DG134 cell division mutant (Fig. 6) indicates that cell division is not essential for the initiation of replication (see above). Under physiological conditions, the cell division period could be necessary to assure a competent state of the replication machinery before the relatively quick initiation (of chromosome replication) event. 1.7 Nucleoid structure. There was a clear difference in nucleoid structure between exponential and stationary phase cells (Figs. 2 and 3). In exponential phase, the nucleoids were more structured and did not fill the entire cell, while upon entrance into stationary phase, they became more relaxed and occupied a larger part of the cell interior. 37 In E. coli, coupling between transcription, translation and translocation of membrane proteins has been proposed to affect the structure of nucleoids. In this model, external loops of chromosomes containing genes coding for membrane proteins are thought to be connected with the cell membrane (189). Therefore, changes in the expression of the membrane proteins upon entrance into the stationary phase would affect the anchoring and result in differences in chromosome structure. Similar mechanism could operate in Sulfolobus cells and result in the relaxation of the DNA structure in stationary phase. Alternatively, the structure of the Sulfolobus chromosome may be influenced by level of the expression of proteins involved in the regulation of DNA supercoiling and condensation, which could be dependent on changes in growth phase. The structure of the Sulfolobus chromosome was suggested to be dependent on the balance between reverse gyrase activity, creating positive supercoiling, and the relaxing activity of type II topoisomerases (111) as well as other proteins. The S. solfataricus 7 (Sso7) protein was shown to facilitate the hybridization of complementary strands of DNA (67), and was suggested to participate in maintaining the dynamic structure of DNA at high temperature (67). Changes in the amounts of proteins related to the Smc family, topoisomerases, and Sso7 levels, can be a consequence of differences in the expression of genes and turnover of proteins upon the entry into the stationary phase and could be a reason for relaxed nucleoid structure. Similar to Sulfolobus the relaxed structure of the nucleoids was also observed in stationary phase cells of E. coli (1). In contrast to Sulfolobus cells, the structure of the nucleoids in stationary phase cells of the euryarchaeon M. jannaschii was much more compact compared to nucleoids from exponential-phase cells (118). Contrary to euryarchaea, Sulfolobus and E. coli do not contain histones, proteins that tightly compact the chromosomes. Thus, the nucleoid structure in such organisms might depend on the superhelical properties of the chromosome. A decreased level of reverse gyrase expression in Sulfolobus upon entrance into stationary phase could result in decrease of the linking number of the chromosome, which could lead to the relaxation of the nucleoid structure. In contrast, decreased level of expression of topoisomerases in stationary phase of euryarchaeal cells may result in a more compact structure of the nucleoids, since the topoisomerases would no longer prevent condensation of the DNA by histones. 1.8 Budding. The appearance of bud-like extrusions in some S. acidocaldarius and S. solfataricus cells under special condition (Fig. 5), is reminiscent of the corresponding process observed in wall-less L-forms of 38 E. coli growing in the presence of calcium. In wall-less L-forms of E. coli budding was speculated to be an unusual division pattern (140). A presence of only a single bud in each of the analyzed cell, suggest that budding could be explained by taking into consideration differences in the structure of the cell envelope at one particular place of the cell. This could be due to proceeding, but still yet unfinished synthesis of the S layers, after the completion of the division process. Alternatively, changes in the structure of the cell envelope at one particular place of the cell may result from the initiation of a new cell division event. Therefore, the place for bud emergence could be used as a marker indicating either the localization of division in the mother cell or the position of the next division. The thinner cell wall could also be an advantage during the mating described for Sulfolobus cells (65, 146, 155, 156) because it would make it easier for donor and recipient cells to establish an intercellular connection between each other. 1.9 Use of conditional mutant in studies of Sulfolobus physiology. Conditional-lethal mutants offer insights into the metabolic and molecular processes involved in biosynthesis, polymerization and assembly of molecules within the cell. They are also important for understanding the function of a variety of proteins involved in DNA replication, transcription, translation, energy metabolism, biosynthesis of building blocks, catabolism, transport of macromolecules, and other processes essential for the growth and viability of cells. Below, I will briefly discuss selected examples for the use of conditional-lethal mutants of S. acidocaldarius. 1.9.1 Mutations affecting growth, protein synthesis and metabolic pathways. The group of mutants from class Ib (Table 5) did not show any effects on cell integrity. Growth and replication were rapidly halted after the shift to nonpermissive temperature, as exemplified using DG146 (Fig. 6). However, the cells remained viable for a long period, more than 30 hours after the shift (Fig. 3, paper III). Since the initiation of replication requires de novo protein synthesis, the observed arrest at the postreplication stage with two genome equivalents and the inability to initiate replication (Fig. 6) might imply damage of any component of the protein synthesis machinery. Furthermore, the observed phenotype could be a consequence of blocking particular metabolic pathways participating in the synthesis of amino acids or ATP, which is required for biosynthesis, polymerization and assembly reactions, and affect the replication of DNA and other growth properties. 39 1.9.2 Mutations affecting cellular integrity. The DNA degradation in mutants from class II (Table 5) coincides with the relatively rapid drop in viability (Fig. 3, paper III) and ghost-like appearance of the cells, after the shift to nonpermissive conditions (Fig. 6). The phenotype of the class of conditional-lethal mutants of S. acidocaldarius discussed in this section suggests that they may be useful for searching for genes that are essential for proper functioning of the cell envelope. Membrane stability of archaeal cells is essential for protection against lethal effects of extreme temperature in the living environment (40, 87, 88, 89, 178). This stability is due to the presence of ether links and isoprenoids in the membrane lipids (40, 89, 178). Mutations in the gene(s) participating in isoprenoid synthesis could allow penetration of external acid into the cells. This might be followed by acidification of the cytoplasm, leading to a quick loss in cellular viability. A proper structure of the membrane is important for electron transport, which is dependent upon proteins located in the membrane (102). As the pH of the medium is about 3, an efficient respiratory system for expelling protons out of the cytoplasm of Sulfolobus cells is essential for preserving the internal cellular pH, which is close to neutrality. Furthermore, the electron transport is required for the synthesis of ATP. Mutation in the protein components of such a system might lead to problems with ATP synthesis and the effectiveness of the proton motif force. This would affect metabolism and significantly change the internal cellular pH, leading to acidification of the cytoplasm, degradation of DNA and cell death. The S layer of Sulfolobus consists of glycoproteins (64, 88, 147, 183). Mutation(s) affecting the glycosylation pathway or proper function of the components of the S layer may alter its structure and/or integrity. This may result in damage of the integrity of the cell wall, as well as denaturation of cellular proteins, leading to a cell death. The processes described above can be studied in Sulfolobus using mutants from class I, II, and V, which constitute more than 60% of our collection. This large fraction of conditional-lethal mutants provides possibilities for discovering essential genes involved in the regulation of various cellular processes in the archaeal cell. 40 Part II: The ftsZ gene and cell division of H. mediterranei (paper IV) 2.1 Introduction. In this section, I will discuss cell division in halophilic archaeon H. mediterranei, as well as transcription and translation of its ftsZ gene. The gene organization around ftsZ in all euryarchaea was analyzed using the information provided by frameplot and database analyses. The extent of functional conservation between archaeal and bacterial FtsZ proteins was investigated. Finally, the relationship between euryarchaeal FtsZ and eukaryotic tubulin will be discussed. 2.2 Transcription initiation. Analyses of several promoter sequences of the euryarchaeal ftsZ paralog 1 suggested the presence of a putative TATAbox motif which matched the general archaeal TATA box consensus sequence, which is 5´-YTTAWA-3´ (where Y= C or T; W=A or T) (174). In contrast, the TATA box of Haloferax ftsZ (Fig. 1, paper IV) resembled neither the above consensus nor the recently proposed consensus for genes of halophilic archaea, that is 5´-TTTWWW-3´ (164). The sequence of the TATA box of Haloferax ftsZ fit with the core consensus sequence for protein coding genes 5´-TWWWWR-3´ (where W= A or T; R=A or G) (30). In halophilic archaea, there are multiple TATA binding proteins (TBPs) (133, 165, 174). Thus, the TATA box of Haloferax ftsZ that do not fit the consensus sequences might instead constitute a binding site for an alternative TBP. However, it is necessary that more genes from H. mediterranei be sequenced and analyzed in order to support such speculation. 2.3 Translation initiation signals. Two ATG translation initiation starts were proposed, the first located immediately downstream of the transcription initiation start and the second positioned downstream of the putative SD sequence (Fig. 1, paper IV and Fig. 7). The presence of SD motifs in front of the 2nd initiation codon implies a bacterial-like SD-dependent mechanism for translation initiation of the Haloferax ftsZ gene. A similar mechanism for translation initiation could also be suggested for the ftsZ paralog 1 of M. jannaschii, which also have a putative SD in front of the initiation codon. However, the second possibility that translation could be initiated by an unknown mechanism from the 1st ATG codon located close to the 5´end of the ftsZ mRNA cannot be excluded. The short (3 bp) distance between the 41 transcription initiation start of the ftsZ gene and the 1st ATG initiation codon make the possibility for the presence of SD-like sequence or any regulatory elements upstream to this codon, unlikely. In bacteria and in S. solfataricus, in genes without a SD sequence in front of the initiation codon, other regulatory sequences located instead downstream of the initiation codon might constitute a functional equivalent of the absent SD sequence (101, 175). In S. solfataricus, possibility for a presence of such regulatory sequence elements located even at the 3´-end of the mRNA, was also considered (175). Haloferax may use a similar to Sulfolobus strategy in order to initiate translation of the ftsZ gene from the 1st ATG codon. Sequence elements with partial identity to SD such as 5´-GGA-3´ which is located downstream of the 1st ATG initiation codon and partially overlaps it, or other yet undetected signal elements located downstream of the 1st ATG codon, might be necessary for initiation of translation of the ftsZ gene from this codon. 2.4 Gene organization around ftsZ. The gene cluster identified in the genus Haloferax, containing ftsZ, secE and nusG, (Fig. 5, paper IV and Fig. 7) is a part of a larger cluster coding for proteins involved in transcription translation (ribosomal proteins), and protein secretion. Even though gene order may not be preserved in general in evolution (130), this gene cluster is most likely important since it was found to be conserved in many bacteria and archaea (180), and hence proposed to be present already in the last common universal ancestor of all organisms (LUCA) (180). The clustering of the ftsZ gene with secE, nusG and other genes is present in euryarchaea (paper IV and (180)), but not in bacteria. For example, in E.coli the ftsZ is grouped with downstream genes such as the envA required in early stage of lipopolisaccharide biosynthesis and cell separation, gene with unknown function, secA required for proteins translocation across membrane (37), and the mutator gene, mutT. Therefore, linkage of the ftsZ in archaea could be explained as an accidental event, resulting from the horizontal transfer of the ftsZ gene to an archaeal ancestor, and integration of the ftsZ gene close to the cassette of genes, including secE and nusG. The one base pair spacer between secE and nusG, and the presence of an SD in front of the nusG gene strongly suggests that the genes are cotranscribed and co-translationally coupled. The clustering of secE and nusG could facilitate the physical interaction between their gene products. However, the absence of secE in the euryarchaeon Pyrococcus implies that physical interaction between the NusG and SecE proteins is not an absolute 42 requirement. Clustering might rather provide a way to coordinate gene expression, but this remains to be proven. 2.5 FtsZ and tubulin. The structural similarities between tubulin and FtsZ proteins led to the hypothesis of FtsZ being an ancestor of tubulin (see Introduction). Analysis of several archaeal genomes revealed the presence of multiple ftsZ genes, clustered separately on the phylogenetic tree and referred as paralog 1 and paralog 2 (49). Phylogenetic analysis suggested that ftsZ may diverge into multiple copies already in the archaeal ancestor (49). Thus, tubulin might have evolved from a non-essential copy of the duplicated ftsZ gene (49, 120). The FtsZ paralog 1 from Haloferax was demonstrated to be functionally conserved in both bacteria and archaea. Considering its high identity at the amino acid level to other euryarchaeal FtsZ paralog 1 proteins (paper IV), this might imply that the euryarchaeal FtsZ paralog 1 proteins are devoted to the formation of the Z-ring and all are essential for cell viability. Hence, this would exclude the paralog 1 from being an ancestor of tubulin. Instead, FtsZ paralog 2 could be a potential candidate for a tubulin precursor. 2.6 Morphological features. Some cells in the H. mediterranei population were found to be asymmetrically invaginated. This type of morphology was reminiscent of the cell division pattern observed in spherical rodA mutants of E. coli affected in peptydoglycan synthesis (38). A Z-ring could only be observed in a few of the asymmetrically invaginated H. mediterranei cells, whereas a majority of such cells did not exhibit any fluorescence (Fig. 8, row E and F). The absence of a fluorescent signal could be explained in different ways, including technical problems (e.g. poor staining and/or fixation conditions) or problems with the stability of the Z-ring. It would be interesting to target this problem using a FtsZ-GFP fusion, which eliminate the problem of harsh treatment of the cell during chemical fixation and immunolocalization studies. A GFP fusion was preferred rather than the immunolocalization for localization studies of other bacterial proteins such as Soj, and MinD (121, 122). To conclude, the lack of fluorescent signal in a majority of the cells with asymmetric invaginations suggests that the morphology of H. mediterranei cells is not enough to draw conclusions about the exact pattern of cell division. 43 2.7 Cell division. Since morphology was insufficient criterion to predict the division pattern of Haloferax cells, localization of the Z-ring was used to target this problem. The bacterial-like pattern of cell division in exponentially growing cells of H. mediterranei was reflected in the structure and presence of a Z-ring. The localization of the Z-ring to the cell septum at different stages of cell division in H. mediterranei (Fig. 8), suggests that the Haloferax cells divide by medial fission as observed in many bacteria, including E.coli. However, and in contrast to E. coli, the final stages of cell division in H. mediterranei were characterized by the presence of a morphological structure reminiscent of a cellular bridge, to which the FtsZ protein was localized (Fig 8, row B and C). These morphological structures could result from contraction of the cell by the Z ring. Such process of contraction of the cell may be driven by changes in the curvature of FtsZ filaments (114). Although the presence of the FtsZ protein and formation of the Z-ring indicate conservation of at least initial stages of cell division between bacteria and archaea, only few cell division proteins (see Introduction) were identified in completely sequenced euryarchaeal genomes (12, 152). Hence, more studies are required to reveal the complete mechanism of cell division process in the genus Haloferax. 44 4. Future projects 4.1 Correlation between growth rate and length of cell cycle periods. The correlation between the length of particular cell cycle periods and the growth rate can be studied by the flow cytometry analysis of cells growing in different media. If a decrease in growth rate is followed by an increase in the length of the post-replication period, this would support the model in which the initiation of replication is coupled to the division of the cell. However, if the pre-replication period increases in parallel within the generation time of the culture, then replication would not be coupled to the division process. 4.2 Cell division. After the development of a genetic system, the cell division mutants should be complemented using a DNA library from the parent strain DG64, in order to find a functional equivalent of the FtsZ protein in Sulfolobus. Furthermore, I want to understand how the cell division process proceeds in the cell. Since, DG134 is affected in cell division and contains up to 5 properly segregated genome equivalents, the cell division process could be followed using microscopy and flow cytometry after the cells are returned to the permissive temperature. 4.3 The ftsZ genes in halophilic archaea. In almost all completely sequenced euryarchaeal genomes multiple copies of the ftsZ gene have been detected. In contrast, only a single copy of ftsZ gene has been reported in halophilic archaea so far. Therefore, it would be interesting to investigate how many copies of the ftsZ gene may exist in halophilic archaea. A PCR fragment constituting a probe against either paralog 1 or 2 of the ftsZ gene may be used to screen a genomic library. Positive clones would be isolated, sequenced, subcloned into a shuttle vector and used for further analysis. After isolation of the ftsZ gene(s), an effort could be made towards construction of a vector with a FtsZ-GFP fusion to study the localization of different FtsZ proteins in living cells. The FtsZ-GFP fusion could be used to elucidate whether formation of the Z-ring is common to both FtsZ paralogs or primarily restricted to FtsZ paralog 1. 45 In archaea containing multiple copies of the ftsZ gene, different approaches such as mutagenesis or antisense regulation, may be used to knock out a particular copy. This will help to elucidate the function of particular paralogs and to reveal which archaeal ftsZ genes are essential for cell division and viability. 4.4 Cell cycle studies of halophilic prokaryotes. These studies should be done to get an overview, and to be able to generalize about cell cycle properties in crenarchaea and euryarchaea, as well as to compare cell cycle properties between deeply branching extremophilic archaea and bacteria. Thus, cell cycle analyses should be extended to halophilic archaea as well as halophilic and thermophilic bacteria, and I have already initiated such studies. Preliminary results revealed that in halophilic archaea, the growth conditions affect cellular morphology and nucleoid structure. In rod-shaped halophilic archaea, the nucleoid structure resembles that of E. coli, but in those with pleomorphic morphology the nucleoids have rather a complex network-like structure. Flow cytometry analysis shows that the halophilic archaea contain up to three genome equivalents in both exponential and stationary phases. In addition, anisomycin, which inhibits protein synthesis in eukaryotic cells, dramatically affected the nucleoid structure and cellular morphology of halophilic archaea. I have also initiated cell cycle studies of halophilic bacteria, such as Halomonas elongata. In the near future, the same approach will be used to study the cell cycle properties of the thermophilic bacterium Thermus thermophilus. 46 ACKNOWLEDGMENTS I would like to express my gratitude to everyone, who contributed in many different ways, to my thesis: To all of the former and present members of the Departments of Microbiology and Medical Genetics in Uppsala for providing a pleasant and stimulating atmosphere to work in. Rolf Bernander, my supervisor, for his strong support, stimulating discussions, understanding and patience. I am very grateful for the freedom I had during development of the procedures for studying the archaeal cell cycle and microbial diversity in Uppsala. Professor Kurt Nordström my first boss in Sweden, who provided me with the opportunity to come and study in Uppsala. I appreciate your determination in broadening our knowledge by pushing us to read books outside of our subject area. Santanu Dasgupta, for sharing your knowledge about different aspects of life, including science, art, religion, and Indian food. I am also grateful for your incredible input into the correcting of my Ph.D. thesis. Karin Carlson, for her understanding of my requirements for more time to finalized writing of my thesis, and discussions about microbial diversity which help me to improve the procedures for my course with the students. Klas Flärdh, for endless explanations of frameplot analysis and interesting comments about my work. Without your support with Endnote program, I would probably never have finished typing the references into my thesis. Dennis Grogan, from the University of Cincinnati (USA) for a nice and fruitful collaboration. I am very grateful for the email discussions and the tricks you suggested to help with growth, plating and preservation of the Sulfolobus strains. Diarmaid Hughes, you always impressed me with the very pedagogic and organized way you prepared presentations and answered question during Monday seminars. Leif Kirsebom who as a new Head of MIKRO brought to our department a powerful spirit. Christina Friberger, for her excellent and irreplaceable help in so many different things. Professor Alina Taylor, Krzysztof Kucharczyk and Ewa Laskowska from the Department of Biochemistry, University of Gdansk who supervised my first steps into science. Anna Podhajska, and Karol Taylor, professors of the Department of Microbiology and Molecular Biology at the University of Gdansk, for creating an enthusiastic interest in all students, including myself, in microbiology and molecular biology. Jean-Pierre Bouche and Kayemuang Cam, from the CNRS, Toulouse in France, where my interest in the ftsZ gene and various aspects of cell cycle began. I had a nice time and gained a lot of experience while being in your lab. Thomas Åkerlund, for introducing me into the world of light microscopy. The haloarchaeal group from the lab. of professor Shiladitya DasSarma: Nitin B., Fazeela M., Stacy C., Eric G., and Sean K., for their help and nice time in Amherst. The members of Dr. Harald Huber lab. from the University of Regensburg for their help at the beginning of my "Sulfolobus career". 47 To old and new archaea people Ulrika, Laurence, Karin H., Henrik K. (Blotte) and Cecilia, for help, being understanding of my (dis-) organization and most importantly for reminding me almost every day to eat. Joanna Kufel, who from my perspective kept me alive, although Leif Kirsebom, would say she has controlled my life. Emilia, one of the best friends I have ever had and my supplier of chorizo. Sophie, for being my Favorite French Star, and her two inseparable friends, our Greek Goddess Christina and their Latino Amigo Javier. Lina, with her amazing eyes, Betina and Emma S., all of whom I will remember until the end of my life. The beautiful girls Johanna B., Lotta I., Mira, Pernilla, Patricia and Solveig R., who were all absolutely required for keeping MIKRO alive in my heart. Staffan, Agnetha R., Annika, Tord, Maggan, Åsa E., Helena S., Hilde E, Magnus L., Fredrik S., Thomas Å., Per and Dan, for nice times at old MIKRO. Janne, the Ju-jutsu master; Bjorn, the (Z) Ring man; Tessi, the lucky man. Helen W., for support and non-stop discussions in the flow room and over the phone. Doro, for making very good cakes. Christina Ninalga, for the English proofreading of my thesis. Lotta T. and Helena Ö., for being nice persons. Esteban B., for nightshift discussions. Hywel, Nils, and Mathias, for the help with computers and other things that I probably forgot to mention. Fredrik P., for having fun watching pictures of your home made from a satellite. Tao, for your determination in getting things done, in whatever conditions, and for your original personality. All the ladies from Disken, for nice Swedish chats, cookies, and access to the autoclave whenever I needed it. Anna-Chey, who constantly supplies loading buffer for agarose electrophoresis and buffers for the preparation of competent cells. Lena M., for being my "swedish mother.”Solan, without you I would probably never have realized what was wrong with saying “KEBO catalog.” Eva B., for improving my Swedish. Eva F., I spent most of my 5 years time at the BMC at your place trying 10,000 different combinations in order to make the perfect "archaeal" medium. Without your high quality components and clean lab, it would have been hard to succeed. Stig, Eddie, and Hamid, for technical support whenever I needed it and for making fun of me while working in Eva F.’s lab. Anders A., for letting me live in his apartment. DOA, Veronica M., Lotta O, Hai-Tao, Johan B, Cecilia, and Ylva for years of running the course together. Jan Zabielski, for random discussions about life in Great Britain. The PCR/ABI "club", Lucia C., Ludmila, Paula, Delal, Inger, Anh-Nhi and Kiki, for their discussions and help necessary for improving my PCR and sequencing skills. Dima, Stanislav, Edward, Gala, Annika, for rakija, mushrooms, parties, russian lessons, and nice time throughout the years. Jolka, Przemek, Betito, Albert, Jan, Tomek, Maciej, Mikolaj, Patryk, Sebastian, Martin, Cici, GosiaK, and Gosia W., Helena H., Amilcar (Katracho), David (Chapin), Dick (King of Salsa), Susan, Mike, Anders, and Annika, for their presence in Sweden. All people from the "old times" at Lasse Maja and Sernanders Krog for nice time. The Bulgarian Mafia; Nina (number 1), Natalia, Elli, Petrana, Svetlio, and Timour, for perfect company and salsa lessons. I also would like to thank to Aneta and Witek. Edyta, Prezes, Tow. Trzeciak, Tomek, Jacek, Marek and Ania K., Zbyszek R., Zbiszek SZ, and Joasia Cz. for everything they did to support my work and life in Uppsala . All of the Foundations that sponsored my work in Sweden. My family, for their love and support during my studies. 48 References 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. Åkerlund, T., K. Nordström, and R. Bernander. 1995. Analysis of cell size and DNA content in exponentially growing and stationaryphase batch cultures of Escherichia coli. J Bacteriol 177:6791-7. Amils, R., P. Cammarano, and P. Londei. 1993. Translation in Archaea, p. 393-438. In M. Kates, D. Kushner and A. T. Matheson (ed.), The Biochemistry of archaea (archaebacteria) New comprehensive biochemistry; v. 26. Elsevier, Amsterdam; New York. Amils, R., L. Ramirez, J. L. Sanz, I. Marin, A. G. Pisabarro, and D. Urena. 1989. The use of functional analysis of the ribosome as a tool to determine archaebacterial phylogeny. Can J Microbiol 35:1417. Baker, T. A., and S. P. Bell. 1998. Polymerases and the replisome: machines within machines. Cell 92:295-305. Barns, S. M., C. F. Delwiche, J. D. Palmer, and N. R. Pace. 1996. Perspectives on archaeal diversity, thermophily and monophyly from environmental rRNA sequences. Proc Natl Acad Sci U S A 93:918893. Battista, J. R. 2000. Radiation resistance: the fragments that remain. Curr Biol 10:R204-5. Battista, J. R., A. M. Earl, and M. J. Park. 1999. Why is Deinococcus radiodurans so resistant to ionizing radiation? Trends Microbiol 7:362-5. Baumann, C., M. Judex, H. Huber, and R. Wirth. 1998. Estimation of genome sizes of hyperthermophiles. Extremophiles 2:101-8. Beech, P. L., T. Nheu, T. Schultz, S. Herbert, T. Lithgow, P. R. Gilson, and G. I. McFadden. 2000. Mitochondrial FtsZ in a chromophyte alga. Science 287:1276-9. Bell, S. D., S. S. Cairns, R. L. Robson, and S. P. Jackson. 1999. Transcriptional regulation of an archaeal operon in vivo and in vitro. Mol Cell 4:971-82. Bell, S. D., and S. P. Jackson. 1998. Transcription and translation in Archaea: a mosaic of eukaryal and bacterial features. Trends Microbiol 6:222-8. Bernander, R. 1998. Archaea and the cell cycle. Mol Microbiol 29:955-61. Bernander, R. 2000. Chromosome replication, nucleoid segregation and cell division in archaea. Trends Microbiol 8:278-83. Bibb, M. J., P. R. Findlay, and M. W. Johnson. 1984. The relationship between base composition and codon usage in bacterial 49 15. 16. 17. 18. 19. 20. 21. 22. 23. 24. 25. genes and its use for the simple and reliable identification of proteincoding sequences. Gene 30:157-66. Bouche, J. P., and S. Pichoff. 1998. On the birth and fate of bacterial division sites. Mol Microbiol 29:19-26. Bramhill, D. 1997. Bacterial cell division. Annu Rev Cell Dev Biol 13:395-424. Brock, T. D., K. M. Brock, R. T. Belly, and R. L. Weiss. 1972. Sulfolobus: a new genus of sulfur-oxidizing bacteria living at low pH and high temperature. Arch Microbiol 84:54-68. Brown, J. R., and W. F. Doolittle. 1997. Archaea and the prokaryote-to-eukaryote transition. Microbiol Mol Biol Rev 61:456502. Bult, C. J., O. White, G. J. Olsen, L. Zhou, R. D. Fleischmann, G. G. Sutton, J. A. Blake, L. M. FitzGerald, R. A. Clayton, J. D. Gocayne, A. R. Kerlavage, B. A. Dougherty, J. F. Tomb, M. D. Adams, C. I. Reich, R. Overbeek, E. F. Kirkness, K. G. Weinstock, J. M. Merrick, A. Glodek, J. L. Scott, N. S. M. Geoghagen, and J. C. Venter. 1996. Complete genome sequence of the methanogenic archaeon, Methanococcus jannaschii. Science 273:1058-73. Cann, I. K., S. Ishino, I. Hayashi, K. Komori, H. Toh, K. Morikawa, and Y. Ishino. 1999. Functional interactions of a homolog of proliferating cell nuclear antigen with DNA polymerases in Archaea. J Bacteriol 181:6591-9. Cann, I. K., S. Ishino, N. Nomura, Y. Sako, and Y. Ishino. 1999. Two family B DNA polymerases from Aeropyrum pernix, an aerobic hyperthermophilic crenarchaeote. J Bacteriol 181:5984-92. Cann, I. K., and Y. Ishino. 1999. Archaeal DNA replication: identifying the pieces to solve a puzzle. Genetics 152:1249-67. Charbonnier, F., and P. Forterre. 1994. Comparison of plasmid DNA topology among mesophilic and thermophilic eubacteria and archaebacteria. J Bacteriol 176:1251-9. Charlebois, R. L., Q. She, D. P. Sprott, C. W. Sensen, and R. A. Garrett. 1998. Sulfolobus genome: from genomics to biology. Curr Opin Microbiol 1:584-8. Chong, J. P., M. K. Hayashi, M. N. Simon, R. M. Xu, and B. Stillman. 2000. A double-hexamer archaeal minichromosome maintenance protein is an ATP- dependent DNA helicase. Proc Natl Acad Sci U S A 97:1530-5. 50 26. Cobbe, N., and M. M. Heck. 2000. Review: SMCs in the World of Chromosome Biology. From Prokaryotes to Higher Eukaryotes. J Struct Biol 129:123-143. 27. Condo, I., A. Ciammaruconi, D. Benelli, D. Ruggero, and P. Londei. 1999. Cis-acting signals controlling translational initiation in the thermophilic archaeon Sulfolobus solfataricus. Mol Microbiol 34:377-84. 28. Crissman, H. A., and G. T. Hirons. 1994. Staining of DNA in live and fixed cells. Methods Cell Biol 41:195-209. 29. Daly, M. J., and K. W. Minton. 1995. Interchromosomal recombination in the extremely radioresistant bacterium Deinococcus radiodurans. J Bacteriol 177:5495-505. 30. Danner, S., and J. Soppa. 1996. Characterization of the distal promoter element of halobacteria in vivo using saturation mutagenesis and selection. Mol Microbiol 19:1265-76. 31. Darzynkiewicz, Z., J. P. Robinson, and A. H. Crissman. 1994. Flow cytometry. Methods Cell Biol v. 41 and 42. Academic Press. Inc. San Diego, California. 32. De Felice, M., C. W. Sensen, R. L. Charlebois, M. Rossi, and F. M. Pisani. 1999. Two DNA polymerase sliding clamps from the thermophilic archaeon Sulfolobus solfataricus. J Mol Biol 291:47-57. 33. de Pereda, J. M., D. Leynadier, J. A. Evangelio, P. Chacon, and J. M. Andreu. 1996. Tubulin secondary structure analysis, limited proteolysis sites, and homology to FtsZ. Biochemistry 35:14203-15. 34. Delais, A. C., J. Marsault, F. Confalonieri, C. B. de La Tour, and M. Duguet. 2000. Reverse gyrase: The two domains intimately cooperate to promote positive supercoiling. J Biol Chem 275:19498504. 35. Dennis, P. P. 1986. Molecular biology of archaebacteria. J Bacteriol 168:471-8. 36. Dennis, P. P. 1997. Ancient ciphers: translation in Archaea. Cell 89:1007-10. 37. Donachie, W. D. 1993. The cell cycle of Escherichia coli. Annu Rev Microbiol 47:199-230. 38. Donachie, W. D., S. Addinall, and K. Begg. 1995. Cell shape and chromosome partition in prokaryotes or, why E. coli is rod-shaped and haploid. Bioessays 17:569-76. 39. Doolittle, W. F. 1999. Lateral genomics. Trends Cell Biol 9:M5-8. 40. Driessen, A. J. M., J. L. C. M. van de Vossenberg, and W. N. Konings. 1996. Membrane composition and ion permeability in extremophiles. FEMS Microbiol Reviews 18:139-148. 51 41. Edgell, D. R., and W. F. Doolittle. 1997. Archaea and the origin(s) of DNA replication proteins. Cell 89:995-8. 42. Edgell, D. R., and W. F. Doolittle. 1997. Archeabacterial genomics: the complete genome sequence of Methanococcus janaschii. BioEssays 19:1-4. 43. Edgell, D. R., H. P. Klenk, and W. F. Doolittle. 1997. Gene duplications in evolution of archaeal family B DNA polymerases. J Bacteriol 179:2632-40. 44. Elie, C., M. F. Baucher, C. Fondrat, and P. Forterre. 1997. A protein related to eucaryal and bacterial DNA-motor proteins in the hyperthermophilic archaeon Sulfolobus acidocaldarius. J Mol Evol 45:107-14. 45. Erickson, H. P. 1995. FtsZ, a prokaryotic homolog of tubulin? Cell 80:367-70. 46. Erickson, H. P. 1997. FtsZ, a tubulin homologue in prokaryotic cell division. Trends Cell Biol 7:362-367. 47. Erickson, H. P. 1998. Atomic structures of tubulin and FtsZ (published erratum appears in Trends Cell Biol 1998 May; 8(5):210). Trends Cell Biol 8:133-7. 48. Erickson, H. P. 2000. Dynamin and FtsZ. Missing links in mitochondrial and bacterial division. J Cell Biol 148:1103-6. 49. Faguy, D. M., and W. F. Doolittle. 1998. Cytoskeletal proteins: the evolution of cell division. Curr Biol 8:R338-41. 50. Faguy, D. M., and W. F. Doolittle. 1999. Lessons from the Aeropyrum pernix genome. Curr Biol 9:R883-6. 51. Fitz-Gibbon, S. T., and C. H. House. 1999. Whole genome-based phylogenetic analysis of free-living microorganisms. Nucleic Acids Res 27:4218-22. 52. Forterre, P. 1997. Protein versus rRNA: Problems in rooting the universal tree of life. ASM 63:89-95. 53. Forterre, P., A. Bergerat, and P. Lopez-Garcia. 1996. The unique DNA topology and DNA topoisomerases of hyperthermophilic archaea. FEMS Microbiol Rev 18:237-48. 54. Forterre, P., and C. Elie. 1993. Chromosome structure, DNA topoisomerases, and DNA polymerases in archaeabacteria, p. 325367. In M. Kates, D. Kushner and A. T. Matheson (ed.), The Biochemistry of archaea (archaebacteria) New comprehensive biochemistry; v. 26. Elsevier, Amsterdam; New York. 55. Forterre, P., C. Elie, M. Sioud, and A. Hamal. 1989. High positive supercoiling in vitro catalysed by an ATP and polyethylene glycol- 52 56. 57. 58. 59. 60. 61. 62. 63. 64. 65. 66. 67. 68. stimulated topoisomerase from Sulfolobus acidocaldarius. EMBO 4:2123-2128. Forterre, P., and H. Philippe. 1999. Where is the root of the universal tree of life? Bioessays 21:871-9. Gaasterland, T. 1999. Archaeal genomics. Curr Opin Microbiol 2:542-7. Gerard, E., B. Labedan, and P. Forterre. 1998. Isolation of a minDlike gene in the hyperthermophilic archaeon Pyrococcus AL585, and phylogenetic characterization of related proteins in the three domains of life. Gene 222:99-106. Gerdes, K., J. Moller-Jensen, and R. B. Jensen. 2000. Plasmid and chromosome partitioning: surprises from phylogeny. Mol Microbiol 37:455-466. Grayling, R. A., K. Sandman, and J. N. Reeve. 1996. Histones and chromatin structure in hyperthermophilic Archaea. FEMS Microbiol Rev 18:203-13. Greagg, M. A., M. J. Fogg, G. Panayotou, S. J. Evans, B. A. Connolly, and L. H. Pearl. 1999. A read-ahead function in archaeal DNA polymerases detects promutagenic template-strand uracil. Proc Natl Acad Sci U S A 96:9045-50. Grigoriev, A. 1998. Analyzing genomes with cumulative skew diagrams. Nucleic Acids Res 26:2286-90. Grogan, D., P. Palm, and W. Zillig. 1990. Isolate B12, which harbours a virus-like element, represents a new species of the archaebacterial genus Sulfolobus, Sulfolobus shibatae, sp. nov. Arch Microbiol 154:594-9. Grogan, D. W. 1989. Phenotypic characterization of the archaebacterial genus Sulfolobus: comparison of five wild-type strains. J Bacteriol 171:6710-9. Grogan, D. W. 1996. Exchange of genetic markers at extremely high temperatures in the archaeon Sulfolobus acidocaldarius. J Bacteriol 178:3207-11. Grogan, D. W. 2000. The question of DNA repair in hyperthermophilic archaea. Trends Microbiol 8:180-5. Guagliardi, A., A. Napoli, M. Rossi, and M. Ciaramella. 1997. Annealing of complementary DNA strands above the melting point of the duplex promoted by an archaeal protein. J Mol Biol 267:841-8. Gupta, R. S. 1998. Life's third domain (Archaea): an established fact or an endangered paradigm? Theor Popul Biol 54:91-104. 53 69. Gupta, R. S. 1998. Protein phylogenies and signature sequences: A reappraisal of evolutionary relationships among archaebacteria, eubacteria, and eukaryotes. Microbiol Mol Biol Rev 62:1435-91. 70. Gupta, R. S. 1998. What are archaebacteria: life's third domain or monoderm prokaryotes related to gram-positive bacteria? A new proposal for the classification of prokaryotic organisms. Mol Microbiol 29:695-707. 71. Gupta, R. S., and G. B. Golding. 1996. The origin of the eukaryotic cell. Trends Biochem Sci 21:166-71. 72. Helmstetter, C. E. 1996. Timing of synthetic activities in the cell cycle. p. 1627-1639. In F. C. Neidhardt, R. Curtiss III, J. L. Ingraham, E. C. C. Lin, K. B. Low, B. Magasanik, W. S. Reznikoff, M. Riley, M. Schaechter, and H. E. Umbarger (ed.) Escherichia coli and Salmonella:cellular and molecular biology, 2nd ed. ASM Press, Washington, D.C. 73. Herzel, H., O. Weiss, and E. N. Trifonov. 1998. Sequence periodicity in complete genomes of archaea suggests positive supercoiling. J Biomol Struct Dyn 16:341-5. 74. Herzel, H., O. Weiss, and E. N. Trifonov. 1999. 10-11 bp periodicities in complete genomes reflect protein structure and DNA folding. Bioinformatics 15:187-93. 75. Hirano, T. 1998. SMC protein complexes and higher-order chromosome dynamics. Curr Opin Cell Biol 10:317-22. 76. Hirano, T. 1999. SMC-mediated chromosome mechanics: a conserved scheme from bacteria to vertebrates? Genes Dev 13:11-9. 77. Hjort, K., and R. Bernander. 1999. Changes in cell size and DNA content in Sulfolobus cultures during dilution and temperature shift experiments. J Bacteriol 181:5669-75. 78. Hodges, R. A., F. B. Perler, C. J. Noren, and W. E. Jack. 1992. Protein splicing removes intervening sequences in an archaea DNA polymerase. Nucleic Acids Res 20:6153-7. 79. Holmes, V. F., and N. R. Cozzarelli. 2000. Closing the ring: links between SMC proteins and chromosome partitioning, condensation, and supercoiling. Proc Natl Acad Sci U S A 97:1322-4. 80. Horn, C., B. Paulmann, G. Kerlen, N. Junker, and H. Huber. 1999. In vivo observation of cell division of anaerobic hyperthermophiles by using a high-intensity dark-field microscope. J Bacteriol 181:5114-8. 81. Ishikawa, J., and K. Hotta. 1999. FramePlot: a new implementation of the frame analysis for predicting protein-coding regions in bacterial DNA with a high G + C content. FEMS Microbiol Lett 174:251-3. 54 82. Jacobs, K. L., and D. W. Grogan. 1997. Rates of spontaneous mutation in an archaeon from geothermal environments. J Bacteriol 179:3298-303. 83. Jain, R., M. C. Rivera, and J. A. Lake. 1999. Horizontal gene transfer among genomes: the complexity hypothesis. Proc Natl Acad Sci U S A 96:3801-6. 84. Jensen, R. B., and J. Shapiro. 1999. Chromosome segregation during the prokaryotic cell division cycle. Curr Opin Cell Biol 11:726-31. 85. Jessberger, R., C. Frei, and S. M. Gasser. 1998. Chromosome dynamics: the SMC protein family. Curr Opin Genet Dev 8:254-9. 86. Joset, F., J. Guespin-Michel, and L. O. Butler. 1993. Prokaryotic genetics: Genome organisation, transfer and plasticity. Blackwell Scientific Publications, Oxford. 87. Kandler, O., and H. Konig. 1998. Cell wall polymers in Archaea (Archaebacteria). Cell Mol Life Sci 54:305-8. 88. Kandler, O., and H. König. 1993. Cell envelopes of archaea: Structure and chemistry, p. 223-255. In M. Kates, D. Kushner and A. T. Matheson (ed.), The Biochemistry of archaea (archaebacteria) New comprehensive biochemistry; v. 26. Elsevier, Amsterdam; New York. 89. Kates, M. 1993. Membrane lipids of archaea, p. 261-292. In M. Kates, D. Kushner and A. T. Matheson (ed.), The Biochemistry of archaea (archaebacteria) New comprehensive biochemistry; v. 26. Elsevier, Amsterdam; New York. 90. Kawarabayasi, Y., Y. Hino, H. Horikawa, S. Yamazaki, Y. Haikawa, K. Jin-no, M. Takahashi, M. Sekine, S. Baba, A. Ankai, H. Kosugi, A. Hosoyama, S. Fukui, Y. Nagai, K. Nishijima, H. Nakazawa, M. Takamiya, S. Masuda, T. Funahashi, T. Tanaka, Y. Kudoh, J. Yamazaki, N. Kushida, A. Oguchi, H. Kikuchi, and et al. 1999. Complete genome sequence of an aerobic hyperthermophilic crenarchaeon, Aeropyrum pernix K1. DNA Res 6:83101, 145-52. 91. Kawarabayasi, Y., M. Sawada, H. Horikawa, Y. Haikawa, Y. Hino, S. Yamamoto, M. Sekine, S. Baba, H. Kosugi, A. Hosoyama, Y. Nagai, M. Sakai, K. Ogura, R. Otsuka, H. Nakazawa, M. Takamiya, Y. Ohfuku, T. Funahashi, T. Tanaka, Y. Kudoh, J. Yamazaki, N. Kushida, A. Oguchi, K. Aoki, and H. Kikuchi. 1998. Complete sequence and gene organization of the genome of a hyperthermophilic archaebacterium, Pyrococcus horikoshii OT3. DNA Res 5:55-76, 147-55. 55 92. Kelman, Z. 2000. DNA replication in the third domain (of life). Curr. Prot. Peptide. Sci. in press. 93. Kelman, Z., and J. Hurwitz. 2000. A unique organization of the protein subunits of the DNA polymerase clamp loader in the archaeon Methanobacterium thermoautotrophicum delta H. J Biol Chem 275:7327-36. 94. Kelman, Z., J. K. Lee, and J. Hurwitz. 1999. The single minichromosome maintenance protein of Methanobacterium thermoautotrophicum DeltaH contains DNA helicase activity. Proc Natl Acad Sci U S A 96:14783-8. 95. Kikuchi, A., and K. Asai. 1984. Reverse gyrase, a topoisomerase which introduces positive superhelical turns into DNA. Nature 309:677-81. 96. Klenk, H. P., R. A. Clayton, J. F. Tomb, O. White, K. E. Nelson, K. A. Ketchum, R. J. Dodson, M. Gwinn, E. K. Hickey, J. D. Peterson, D. L. Richardson, A. R. Kerlavage, D. E. Graham, N. C. Kyrpides, R. D. Fleischmann, J. Quackenbush, N. H. Lee, G. G. Sutton, S. Gill, E. F. Kirkness, B. A. Dougherty, K. McKenney, M. D. Adams, B. Loftus, J. C. Venter, and et al. 1997. The complete genome sequence of the hyperthermophilic, sulphate-reducing archaeon Archaeoglobus fulgidus (published erratum appears in Nature 1998 Jul 2; 394(6688):101). Nature 390:364-70. 97. Kondo, S., A. Yamagishi, and T. Oshima. 1993. A physical map of the sulfur-dependent archaebacterium Sulfolobus acidocaldarius 7 chromosome. J Bacteriol 175:1532-6. 98. Koonin, E. V. 1993. A superfamily of ATPases with diverse functions containing either classical or deviant ATP-binding motif (published erratum appears in J Mol Biol 1993 Aug 5; 232(3):1013). J Mol Biol 229:1165-74. 99. Koonin, E. V., A. R. Mushegian, M. Y. Galperin, and D. R. Walker. 1997. Comparison of archaeal and bacterial genomes: computer analysis of protein sequences predicts novel functions and suggests a chimeric origin for the archaea. Mol Microbiol 25:619-37. 100. Kornberg, A., and T. A. Baker. 1992. DNA replication. W.H. Freeman, New York. 101. Kozak, M. 1999. Initiation of translation in prokaryotes and eukaryotes. Gene 234:187-208. 102. Kröger, A. 1999. Electron-transport-coupled phosphorylation, p. 5967. In J. W. Langeler, G. Drews and H. G. Schlegel (ed.), Biology of the prokaryotes. Thieme, Stuttgart; New York; Malden, MA. 56 103. Kyrpides, N. C., and C. A. Ouzounis. 1999. Transcription in archaea. Proc Natl Acad Sci U S A 96:8545-50. 104. Kyrpides, N. C., and C. R. Woese. 1998. Universally conserved translation initiation factors. Proc Natl Acad Sci U S A 95:224-8. 105. Lasken, R. S., D. M. Schuster, and A. Rashtchian. 1996. Archaebacterial DNA polymerases tightly bind uracil-containing DNA. J Biol Chem 271:17692-6. 106. Leipe, D. D., L. Aravind, and E. V. Koonin. 1999. Did DNA replication evolve twice independently? Nucleic Acids Res 27:3389401. 107. Lemon, K. P., and A. D. Grossman. 1998. Localization of bacterial DNA polymerase: evidence for a factory model of replication. Science 282:1516-9. 108. Li, Y.-J., B. A.-S. Gahmen, and E. Kellenberger. 1999. Histones and histone-like DNA binding proteins: correlation between structural differences, properties and function. Microbiology 145:1-2. 109. Lopez, P., H. Philippe, H. Myllykallio, and P. Forterre. 1999. Identification of putative chromosomal origins of replication in Archaea. Mol Microbiol 32:883-6. 110. Lopez-Garc, P., and D. Moreira. 1999. Metabolic symbiosis at the origin of eukaryotes. Trends Biochem Sci 24:88-93. 111. Lopez-Garcia, P. 1999. DNA supercoiling and temperature adaptation: A clue to early diversification of life? J Mol Evol 49:43952. 112. Losick, R., and L. Shapiro. 1998. DNA replication. Bringing the mountain to Mohammed. Science 282:1430-1. 113. Lowe, J., and L. A. Amos. 1998. Crystal structure of the bacterial cell-division protein FtsZ. Nature 391:203-6. 114. Lu, C., M. Reedy, and H. P. Erickson. 2000. Straight and curved conformations of FtsZ are regulated by GTP hydrolysis. J Bacteriol 182:164-70. 115. Lutkenhaus, J. 1998. Organelle division: from coli to chloroplasts. Curr Biol 8:R619-21. 116. Lutkenhaus, J., and S. G. Addinall. 1997. Bacterial cell division and the Z ring. Annu Rev Biochem 66:93-116. 117. Makiniemi, M., H. Pospiech, S. Kilpelainen, M. Jokela, M. Vihinen, and J. E. Syvaoja. 1999. A novel family of DNApolymerase-associated B subunits. Trends Biochem Sci 24:14-6. 118. Malandrin, L., H. Huber, and R. Bernander. 1999. Nucleoid structure and partition in Methanococcus jannaschii: an archaeon with multiple copies of the chromosome. Genetics 152:1315-23. 57 119. Maloy, S. R., J. Cronan, J. E.,, and D. Friefelder. 1994. Microbial Genetics. Jones and Barlett Publishers, Boston MA (USA). 120. Margolin, W. 1999. The bacterial cell division maschine. ASM News 65:137-143. 121. Marston, A. L., and J. Errington. 1999. Dynamic movement of the ParA-like Soj protein of B. subtilis and its dual role in nucleoid organization and developmental regulation. Mol Cell 4:673-82. 122. Marston, A. L., H. B. Thomaides, D. H. Edwards, M. E. Sharpe, and J. Errington. 1998. Polar localization of the MinD protein of Bacillus subtilis and its role in selection of the mid-cell division site. Genes Dev 12:3419-30. 123. Martin, W. 1999. Mosaic bacterial chromosomes: a challenge en route to a tree of genomes. BioEssay 21:99-104. 124. Martin, W. 2000. Perspectives: evolutionary biology. A powerhouse divided. Science 287:1219. 125. Minton, K. W., and M. J. Daly. 1995. A model for repair of radiation-induced DNA double-strand breaks in the extreme radiophile Deinococcus radiodurans. Bioessays 17:457-64. 126. Mojica, F. J., C. Diez-Villasenor, E. Soria, and G. Juez. 2000. Biological significance of a family of regularly spaced repeats in the genomes of archaea, bacteria and mitochondria. Mol Microbiol 36:244-6. 127. Mojica, F. J., C. Ferrer, G. Juez, and F. Rodriguez-Valera. 1995. Long stretches of short tandem repeats are present in the largest replicons of the Archaea Haloferax mediterranei and Haloferax volcanii and could be involved in replicon partitioning. Mol Microbiol 17:85-93. 128. Moller-Jensen, J., R. B. Jensen, and K. Gerdes. 2000. Plasmid and chromosome segregation in procaryotes. Trends in Microbiol. 8:313320. 129. Murray, A. W., and T. Hunt. 1993. The cell cycle: an introduction. W.H. Freeman, New York. 130. Mushegian, A. R., and E. V. Koonin. 1996. Gene order is not conserved in bacterial evolution. Trends Genet 12:289-90. 131. Myllykallio, H., P. Lopez, P. Lopez-Garcia, R. Heilig, W. Saurin, Y. Zivanovic, H. Philippe, and P. Forterre. 2000. Bacterial mode of replication with eukaryotic-like machinery in a hyperthermophilic archaeon. Science 288:2212-5. 132. Nelson, K. E., R. A. Clayton, S. R. Gill, M. L. Gwinn, R. J. Dodson, D. H. Haft, E. K. Hickey, J. D. Peterson, W. C. Nelson, K. A. Ketchum, L. McDonald, T. R. Utterback, J. A. Malek, K. D. 58 Linher, M. M. Garrett, A. M. Stewart, M. D. Cotton, M. S. Pratt, C. A. Phillips, D. Richardson, J. Heidelberg, G. G. Sutton, R. D. Fleischmann, J. A. Eisen, C. M. Fraser, and et al. 1999. Evidence for lateral gene transfer between Archaea and bacteria from genome sequence of Thermotoga maritima. Nature 399:323-9. 133. Ng, W. V., S. A. Ciufo, T. M. Smith, R. E. Bumgarner, D. Baskin, J. Faust, B. Hall, C. Loretz, J. Seto, J. Slagel, L. Hood, and S. DasSarma. 1998. Snapshot of a large dynamic replicon in a halophilic archaeon: megaplasmid or minichromosome? Genome Res 8:1131-41. 134. Nishioka, M., S. Fujiwara, M. Takagi, and T. Imanaka. 1998. Characterization of two intein homing endonucleases encoded in the DNA polymerase gene of Pyrococcus kodakaraensis strain KOD1. Nucleic Acids Res 26:4409-12. 135. Nogales, E., K. H. Downing, L. A. Amos, and J. Lowe. 1998. Tubulin and FtsZ form a distinct family of GTPases. Nat Struct Biol 5:451-8. 136. Nogales, E., S. G. Wolf, and K. H. Downing. 1998. Structure of the alpha beta tubulin dimer by electron crystallography (published erratum appears in Nature 1998 May 14; 393(6681):191). Nature 391:199-203. 137. Nordstöm, K. 1999. The bacterial cell cycle, p. 541-553. In J. W. Lageler, G. Drews and H. G. Schlegel (ed.), Biology of prokaryotes. Blackwell Science, New York. 138. O'Donnell, M. 1999. Processivity factors. Curr Biol 9:R545. 139. Olsen, G. J., and C. R. Woese. 1996. Lessons from an Archaeal genome: what are we learning from Methanococcus jannaschii? Trends Genet 12:377-9. 140. Onoda, T., J. Enokizono, H. Kaya, A. Oshima, P. Freestone, and V. Norris. 2000. Effects of calcium and calcium chelators on growth and morphology of Escherichia coli L-form NC-7. J Bacteriol 182:1419-22. 141. Pace, N. R. 1997. A molecular view of microbial diversity and the biosphere. Science 276:734-40. 142. Penny, D., and A. M. Poole. 1999. The nature of last common universal ancestor. Curr. Opin. Gen. Dev. 9:672-677. 143. Pereira, S. L., R. A. Grayling, R. Lurz, and J. N. Reeve. 1997. Archaeal nucleosomes. Proc Natl Acad Sci U S A 94:12633-7. 144. Perler, F. B., D. G. Comb, W. E. Jack, L. S. Moran, B. Qiang, R. B. Kucera, J. Benner, B. E. Slatko, D. O. Nwankwo, S. K. 59 Hempstead, and et al. 1992. Intervening sequences in an Archaea DNA polymerase gene. Proc Natl Acad Sci U S A 89:557781. 145. Poole, A. M., D. C. Jeffares, and D. Penny. 1999. Early evolution: prokaryotes, the new kids on the block. BioEssays 21:880-889. 146. Prangishvili, D., S. V. Albers, I. Holz, H. P. Arnold, K. Stedman, T. Klein, H. Singh, J. Hiort, A. Schweier, J. K. Kristjansson, and W. Zillig. 1998. Conjugation in archaea: frequent occurrence of conjugative plasmids in Sulfolobus. Plasmid 40:190-202. 147. Pruschenk, R., and W. Baumeister. 1987. Three-dimensional structure of the surface protein of Sulfolobus solfataricus. Eur. J. cell biol 45:185-191. 148. Reeve, J. N., K. Sandman, and C. J. Daniels. 1997. Archaeal histones, nucleosomes, and transcription initiation. Cell 89:999-1002. 149. Rivera, M. C., and J. A. Lake. 1992. Evidence that eukaryotes and eocyte prokaryotes are immediate relatives. Science 257:74-6. 150. Rocha, E. P., A. Danchin, and A. Viari. 1999. Bacterial DNA strand compositional asymmetry. Trends Microbiol 7:308. 151. Rocha, E. P., A. Danchin, and A. Viari. 1999. Universal replication biases in bacteria. Mol Microbiol 32:11-6. 152. Rothfield, L., S. Justice, and J. Garcia-Lara. 1999. Bacterial cell division. Annu Rev Genet 33:423-48. 153. Salzberg, S. L., A. J. Salzberg, A. R. Kerlavage, and J. F. Tomb. 1998. Skewed oligomers and origins of replication. Gene 217:57-67. 154. Sandman, K., S. L. Pereira, and J. N. Reeve. 1998. Diversity of prokaryotic chromosomal proteins and the origin of the nucleosome. Cell Mol Life Sci 54:1350-64. 155. Schleper, C., I. Holz, D. Janekovic, J. Murphy, and W. Zillig. 1995. A multicopy plasmid of the extremely thermophilic archaeon Sulfolobus effects its transfer to recipients by mating. J Bacteriol 177:4417-26. 156. Schmidt, K. J., K. E. Beck, and D. W. Grogan. 1999. UV stimulation of chromosomal marker exchange in Sulfolobus acidocaldarius: implications for DNA repair, conjugation and homologous recombination at extremely high temperatures. Genetics 152:1407-15. 157. Sensen, C. W., H. P. Klenk, R. K. Singh, G. Allard, C. C. Chan, Q. Y. Liu, S. L. Penny, F. Young, M. E. Schenk, T. Gaasterland, W. F. Doolittle, M. A. Ragan, and R. L. Charlebois. 1996. Organizational characteristics and information content of an archaeal genome: 156 kb of sequence from Sulfolobus solfataricus P2. Mol Microbiol 22:175-91. 60 158. Shapiro, L., and R. Losick. 2000. Dynamic spatial regulation in the bacterial cell. Cell 100:89-98. 159. Sharpe, M. E., and J. Errington. 1999. Upheaval in the bacterial nucleoid. An active chromosome segregation mechanism. Trends Genet 15:70-4. 160. She, Q., H. Phan, R. A. Garrett, S. V. Albers, K. M. Stedman, and W. Zillig. 1998. Genetic profile of pNOB8 from Sulfolobus: the first conjugative plasmid from an archaeon. Extremophiles 2:417-25. 161. Skarstad, K., R. Bernander, and E. Boye. 1995. Analysis of DNA replication in vivo by flow cytometry. Methods Enzymol 262:604-13. 162. Skarstad, K., R. Bernander, S. Wold, H. B. Steen, and E. Boye. 1996. Cell cycle analysis of microorganisms, p. 241-255. In M. AlRubeai and A. N. Emery (ed.), Flow cytometry in cell culture. Marcel Dekker, Inc, New York. 163. Smith, D. R., L. A. Doucette-Stamm, C. Deloughery, H. Lee, J. Dubois, T. Aldredge, R. Bashirzadeh, D. Blakely, R. Cook, K. Gilbert, D. Harrison, L. Hoang, P. Keagle, W. Lumm, B. Pothier, D. Qiu, R. Spadafora, R. Vicaire, Y. Wang, J. Wierzbowski, R. Gibson, N. Jiwani, A. Caruso, D. Bush, J. N. Reeve, and et al. 1997. Complete genome sequence of Methanobacterium thermoautotrophicum deltaH: functional analysis and comparative genomics. J Bacteriol 179:7135-55. 164. Soppa, J. 1999. Normalized nucleotide frequencies allow the definition of archaeal promoter elements for different archaeal groups and reveal base-specific TFB contacts upstream of the TATA box. Mol Microbiol 31:1589-92. 165. Soppa, J. 1999. Transcription initiation in Archaea: facts, factors and future aspects. Mol Microbiol 31:1295-305. 166. Stanier, R. Y., J. L. Ingraham, M. L. Wheelis, and P. R. Painter. 1988. General Microbiology. Macmillan Education LTD, London. 167. Steen, H. B., K. Skarstad, and E. Boye. 1990. DNA measurements of bacteria. Methods Cell Biol 33:519-26. 168. Stein, J. L., and M. I. Simon. 1996. Archaeal ubiquity. Proc. Natl. Acad. Sci. USA 93:6228-6230. 169. Stetter, K. O. 1996. Hyperthermophilic procaryotes. FEMS Microbiol Rev 18:149-158. 170. Stetter, K. O. 1999. Extremophiles and their adaptation to hot environments. FEBS Lett 452:22-5. 171. Strunnikov, A. V. 1998. SMC proteins and chromosome structure. Trends Cell Biol 8:454-9. 61 172. Sullivan, S. M., and J. R. Maddock. 2000. Bacterial sporulation: pole-to-pole protein oscillation. Curr Biol 10:R159-61. 173. Takai, K., and K. Horikoshi. 1999. Genetic diversity of archaea in deep-sea hydrothermal vent environments. Genetics 152:1285-97. 174. Thompson, D. K., J. R. Palmer, and C. J. Daniels. 1999. Expression and heat-responsive regulation of a TFIIB homologue from the archaeon Haloferax volcanii. Mol Microbiol 33:1081-92. 175. Tolstrup, N., C. W. Sensen, R. A. Garrett, and I. G. Clausen. 2000. Two different and highly organized mechanisms of translation initiation in the archaeon Sulfolobus solfataricus. Extremophiles 4:175-9. 176. Tse-Dinh, Y. C. 1998. Bacterial and archeal type I topoisomerases. Biochim Biophys Acta 1400:19-27. 177. Tye, B. K. 2000. From the cover: insights into DNA replication from the third domain of life. Proc Natl Acad Sci U S A 97:2399-401. 178. van de Vossenberg, J. L., A. J. Driessen, and W. N. Konings. 1998. The essence of being extremophilic: the role of the unique archaeal membrane lipids. Extremophiles 2:163-70. 179. van der Oost, J., M. Ciaramella, M. Moracci, F. M. Pisani, M. Rossi, and W. M. de Vos. 1998. Molecular biology of hyperthermophilic Archaea. Adv Biochem Eng Biotechnol 61:87-115. 180. Wächtershäuser, G. 1998. Towards a reconstruction of ancestral genomes by gene cluster alignment. System. Appl. Microbiol. 21:473477. 181. Waga, S., and B. Stillman. 1998. The DNA replication fork in eukaryotic cells. Annu Rev Biochem 67:721-51. 182. Wang, X., and J. Lutkenhaus. 1996. FtsZ ring: the eubacterial division apparatus conserved in archaebacteria. Mol Microbiol 21:313-9. 183. Weiss, R. L. 1974. Subunit cell wall of Sulfolobus acidocaldarius. J Bacteriol 118:275-84. 184. Wheeler, R. T., and L. Shapiro. 1997. Bacterial chromosome segregation: is there a mitotic apparatus? Cell 88:577-9. 185. White, R. J., and S. P. Jackson. 1992. The TATA-binding protein: a central role in transcription by RNA polymerases I, II and III. Trends Genet 8:284-8. 186. Whitman, W. B., F. Pfeifer, P. Blum, and A. Klein. 1999. What archaea have to tell biologists. Genetics 152:1245-8. 187. Woese, C. R., and G. E. Fox. 1977. Phylogenetic structure of the prokaryotic domain: the primary kingdoms. Proc Natl Acad Sci U S A 74:5088-90. 62 188. Woese, C. R., O. Kandler, and M. L. Wheelis. 1990. Towards a natural system of organisms: proposal for the domains Archaea, Bacteria, and Eucarya. Proc Natl Acad Sci U S A 87:4576-9. 189. Woldringh, C. L., P. R. Jensen, and H. V. Westerhoff. 1995. Structure and partitioning of bacterial DNA: determined by a balance of compaction and expansion forces? FEMS Microbiol Lett 131:23542. 190. Xu, M. Q., M. W. Southworth, F. B. Mersha, L. J. Hornstra, and F. B. Perler. 1993. In vitro protein splicing of purified precursor and the identification of a branched intermediate. Cell 75:1371-7. 191. Zillig, W., H. P. Arnold, I. Holz, D. Prangishvili, A. Schweier, K. Stedman, Q. She, H. Phan, R. Garrett, and J. K. Kristjansson. 1998. Genetic elements in the extremely thermophilic archaeon Sulfolobus. Extremophiles 2:131-40. 192. Zillig, W., H. P. Klenk, P. Palm, G. Puhler, F. Gropp, R. A. Garrett, and H. Leffers. 1989. The phylogenetic relations of DNAdependent RNA polymerases of archaebacteria, eukaryotes, and eubacteria. Can J Microbiol 35:73-80. 193. Zillig, W., P. Palm, H. Klenk, D. Langer, U. Hudepohl, J. Hain, and H. Lanzendorfer M, I. 1993. Transcription in archaea, p. 367391. In M. Kates, D. Kushner and A. T. Matheson (ed.), The Biochemistry of archaea (archaebacteria) New comprehensive biochemistry; v. 26. Elsevier, Amsterdam; New York. 194. Zillig, W., D. Prangishvilli, C. Schleper, M. Elferink, I. Holz, S. Albers, D. Janekovic, and D. Gotz. 1996. Viruses, plasmids and other genetic elements of thermophilic and hyperthermophilic Archaea. FEMS Microbiol Rev 18:225-36. 195. Zlatanova, J. 1997. Archaeal chromatin: virtual or real? Proc Natl Acad Sci U S A 94:12251-4. 63
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