Evolution, 58(11), 2004, pp. 2486–2497 RATES OF MOLECULAR EVOLUTION IN NUCLEAR GENES OF EAST MEDITERRANEAN SCORPIONS BENJAMIN GANTENBEIN1,2 1 School AND PETER D. KEIGHTLEY1 of Biological Sciences, University of Edinburgh, West Mains Road, Edinburgh EH9 3JT, United Kingdom Abstract. Scorpions of the genus Mesobuthus represent a useful terrestrial model system for studying molecular evolution. They are distributed on several Aegean islands and the adjacent mainland, they are believed to have low rates of dispersal, and evolutionary divergence dates of taxa are available based on biogeographic events that separated islands from each other and the mainland. Here, we present data on polymorphism and synonymous (Ks) and nonsynonymous (Ka) substitution rates for nine nuclear protein-coding genes of two east Mediterranean scorpion species, Mesobuthus gibbosus and M. cyprius (Buthidae). Levels of polymorphism tend to be lower in populations from islands (mean nucleotide diversity ⫽ 0.0071 ⫾ 0.0028) than in mainland populations (mean ⫽ 0.0201 ⫾ 0.0085). By using linear regression of genetic divergence versus isolation time, we estimate Ks to be 3.17 ⫾ 1.54 per (site ⫻ 109 years), and Ka to be 0.39 ⫾ 0.94 per (site ⫻ 109 years). These estimates for both Ks and Ka are considerably lower than for many other invertebrates, such as Drosophila, and may be attributed to scorpions’ mammal-like generation times (⬃2 years) and low metabolic rates. Phylogenetic analysis using maximum likelihood revealed a phylogeny that is congruent with that expected based on biogeographic events and in which divergences at synonymous sites are proportional to the dates that the taxa are believed to have split. Tests of equality of branch lengths for the Cyprus and Crete lineages revealed that Ks-estimates are about the same in both lineages, as expected from the biogeographic events that separated the islands, but Ka was increased in the Cyprus lineage compared to the Cretan lineage. Key words. East Mediterranean, local molecular clock, Mesobuthus, nuclear protein-coding DNA, scorpions. Received July 26, 2004. The molecular clock hypothesis postulates rate constancy of molecular evolution (Margoliash 1963; Zuckerkandl and Pauling 1965; Ohta and Kimura 1971; Gillespie 1989; Li 1997) and has stimulated much interest. If macromolecules (proteins or DNA sequences) evolve at constant rates, they can be used to date divergence times between taxa (Hasegawa et al. 1985, 1987; Kishino et al. 2001). Although the existence of a universal molecular clock has always been controversial, several studies have attempted to calibrate local molecular clocks by focusing on particular groups of organisms, such as vertebrates (Yoder and Yang 2000). Such local clocks appear to tick surprisingly linearly through time (Knowlton et al. 1993; Beerli et al. 1996; Knowlton and Weight 1998). Calibrating a molecular clock requires information from reliable external sources, preferably well-dated fossils or biogeographic events (Hillis et al. 1996). Such evidence has been used to date divergence events in vertebrates (Kumar and Hedges 1998; Hedges and Kumar 2003), but has been much less used in invertebrates. Together with the lack of fossil invertebrates, this has resulted in a lack of information on rates of molecular evolution for invertebrates, taxa that make up 98% of worldwide biodiversity (Brusca 2000). Recently, deep evolutionary splits among arthropods have been dated using a molecular clock based on nuclear gene sequence data (Peterson et al. 2004; Pisani et al. 2004). However, the date of the deuterostome-arthropod split and relative evolutionary rates of evolution among the different arthopod groups remain controversial. Here, we present new genetic data on nine nuclear protein-coding genes of two East Mediterranean scorpion species of the genus Mesobuthus Vachon 1950 for which well-dated divergence times are available. Due to the 2 Present address: AO Research Institute, Clavadelerstrasse, CH7270 Davos Platz, Switzerland; E-mail: [email protected]. Accepted August 3, 2004. joining of the Stait of Gibraltar, it is believed that the Mediterranean Basin dried out 5.6 million years ago (known as the Mediterranean Salinity Crisis, MSC). As a result, many Mediterranean islands were connected to the mainland via land bridges over a period of 100,000 years. About 5.33 million years ago, the reopening of the Strait of Gibraltar led to the refilling of Mediterranean over a period of only about 100 years (Krijgsman et al. 1999; Duggen et al. 2003). Scorpions of the Mediterranean basin therefore offer an excellent opportunity to study evolutionary rates in invertebrates. First, it can be assumed that scorpion populations inhabited the Mediterranean islands during the MSC and exchanged genes during the establishment of land bridges. Second, it is likely that the populations subsequently remained isolated, as scorpions show extremely low dispersal rates (annually 1–30 m; Polis et al. 1985), and genetic data on allozymes and nuclear and mitochondrial DNA (mtDNA) sequences suggest a strong population structure with high FST-estimates between subpopulations and low dispersal rates (Yamashita and Polis 1995; Gantenbein et al. 2001; Gantenbein 2004). The scorpion genus Mesobuthus has its main species diversity in central Asia (Fet et al. 2000) and contains many species of considerable toxicity to humans (Keegan 1998). The genus has recently been the subject of molecular studies on between-species phylogeny and within-species phylogeography (Gantenbein et al. 2003). Molecular and morphological phylogenetic analysis has revealed that populations of the island of Cyprus represent a divergent lineage; therefore, these have been assigned a species rank (i.e., Mesobuthus cyprius Gantenbein and Kropf 2000; Gantenbein et al. 2000). A recent phylogeographic study using DNA sequence data from a fragment of the mitochondrial large ribosomal subunit (16S; Gantenbein and Largiadèr 2002) on the Aegean sister species Mesobuthus gibbosus (Brullé 1832), 2486 䉷 2004 The Society for the Study of Evolution. All rights reserved. MOLECULAR CLOCK OF MEDITERRANEAN SCORPIONS a species with a vicariant distribution across the Greek Balkans, Anatolia, and numerous Aegean islands, revealed an excellent linear correlation between time and geological separation time. An independent estimate for the evolutionary rate of the orthologous mtDNA fragment was also obtained from a clock calibration of Buthus occitanus populations from both sides of the Strait of Gibraltar (Gantenbein and Largiadèr 2003). However, little is known about evolutionary rate of nuclear genes in scorpions and in arthropods in general. With few exceptions, studies of arthropods outside Drosophila have dealt with mitochondrial genes or nuclear ribosomal sequences (Giribet et al. 2001; Gaunt and Miles 2002). In scorpions, genetic research of nuclear DNA has focused on toxin genes, and comparative phylogenetic studies are very scarce (Loret and Hammock 2001; Froy and Gurevitz 2003). In this paper we estimate rates of molecular evolution for East Mediterranean scorpions in nuclear protein-coding genes, using nine loci that have recently been isolated from a cDNA library of this species (our data, in progress). We calibrate the clock using a linear regression approach and phylogenetic methods. MATERIALS AND METHODS Sampling Strategy Scorpions of the two buthid species M. cyprius Gantenbein and Kropf 2000 and M. gibbosus (Brullé 1832) were collected between 1996–2002 (exact collection dates are available on request). The distribution of the two species, the sampling localities, and the sample sizes are shown in Figure 1 and Table 1 (Kinzelbach 1975). Generally specimens were collected from a circular area of about 300 m2. For the purpose of rooting the phylogeny, we included data from two congeneric species M. eupeus (C. L. Koch 1839) and M. caucasicus (Nordmann 1840) (Table 1), which are sister clades to the ingroup (Fet et al. 2003; Gantenbein et al. 2003). DNA Analysis DNA was extracted from muscle tissue (pedipalp or legs) using either chloroform/phenol ethanol precipitation (Sambrook et al. 1989) or by using the Gentra (Ashby de la Zouch, Leicestershire, U.K.) Puregene DNA isolation kit. Genomic DNA was eluted in 50 l of 10 mM Tris-HCl/1 mM EDTA (pH 8.0). Polymerase chain reaction (PCR) primers were designed from two tissue-specific (body and tail) expressed sequence tag (EST) libraries of an adult M. gibbosus specimen (B. Gantenbein, M. Thomson, A. Rosie, J. Parkinson, I. Gantenbein, and M. Blaxter, unpubl. data). From a PCR screen of 52 randomly chosen genes, only nine could be amplified. The amplification failures might be due to the presence of long introns. Table 2 indicates likely gene identities derived from BLAST E-values and sequence similarity of BLASTX matches against the nucleotide database, the primer sequences, and cross-links to Flybase reference numbers. To amplify these genes, a general PCR cycling profile was used; initial denaturation 95⬚C for 5 min followed by 35 cycles of 25 sec at 95⬚C, 20 sec at 50⬚C, and 90 sec at 72⬚C. PCR reactions 2487 were carried out in 20-l volumes using Qiagen (Crawley, West Sussex, U.K.) Taq polymerase with 2 l of genomic DNA (about 50–100 ng) in a MJ-Research (Rayne/Brayntrace, Essex, U.K.) PTC-100 thermocycler. Products were inspected on 1.5% agarose gels for multiple bands and were then purified using a PEG8000 precipitation protocol (Andolfatto et al. 2003). Gel purification (1-to-1 Biology, Qbiogene, Cambridge, U.K.) and subsequent subcloning of the PCR product was applied in the case of loci 1 and 3, where sequencing failed due to difficult templates containing repeats, and for the amplification of the outgroups. For cloning of PCR products, amplicons were cloned into the plasmid vector pCR2.1 using the TOPO Cloning Kit (Invitrogen Corp., Paisley, U.K.). At least four and up to 10 positive clones were chosen per transformation. M13 universal primers were used to screen colonies by PCR. PCR primers were again removed by polyethylene glycol (PEG 8000) precipitation, and purified templates were sequenced on both strands using M13for and M13rev primers and DYEnamic ET Dye Terminator Kit (Amersham Biosciences, Little Chalfont, Buckinghamshire, U.K.). PCR products were sequenced using the forward PCR primer (Table 2). Sequencing reactions were precipitated with ethanol and sodium acetate and run on an ABI377XL sequencer or on an ABI3730 capillary sequencer (Applied Biosystems, Foster City, CA). All sequences were checked manually for sequencing errors. Consensus sequences of subcloning (loci 1 and 3) were assembled using the Seqman (Dnastar, Inc., Madison, WI) package. All sequences were deposited in the EMBL nucleotide sequence database (http://www.ebi.ac.uk) under the following accession numbers; loci 01–03: AJ605341–AJ605513; loci 04–06: AJ605780–AJ605953; loci 07–09: AJ606701–AJ606874. Analyses of Multilocus DNA Sequences A total of 58 sequences were aligned using the multiple alignment algorithm of ClustalX (Thompson et al. 1997). Alignment of protein-coding sequences was unambiguous due to the presence of open reading frames. We calculated the number of polymorphic sites, GC-content, and nucleotide diversity () within exons and intronic regions (Nei and Li 1979) from the polymorphism data within each major phylogenetic clade. Calibration of a Molecular Clock We calculated estimates of pairwise Ks and Ka, DNA substitution rates using the method of Nei and Gojobori (1986), which corrects for multiple hits assuming the model of Jukes and Cantor (1969). Ks and Ka were calculated using DNASP 4.0 (Rozas and Rozas 1999). We then calculated the mean of Ks and Ka (and their standard errors) between major clades as identified from phylogenetic analysis (see below) and plotted these estimates against geological separation time. We corrected the mean of Ks and Ka between clades for ancestral polymorphism using the following formula: ¯ net ⫽ K ¯ AB ⫺ (K ¯A ⫹ K ¯ B)/2, K (1) where K̄net is the net evolutionary rate, K̄AB is the mean evolutionary rate between clades A and B, and K̄A and K̄B are 2488 B. GANTENBEIN AND P. D. KEIGHTLEY FIG. 1. (A) Sampling sites of the two buthid scorpion species Mesobuthus cyprius Gantenbein and Kropf 2000 and M. gibbosus (Brullé 1932) in the east Mediterranean area. Abbreviations of sampling sites are given in Table 1, numbers refer to the number of localities per major biogeographic region. (B) Enlargement of Aegean region. Arrows indicate isolation times based on geological evidence (see Material and Methods section). the mean evolutionary rates within clade A and B, respectively (Nei and Li 1979). The mean nucleotide substitutions per (site ⫻ 10⫺9 year) was estimated by linear regression including an intercept in the model for each gene and for a concatenated supergene. A test for equality of slopes was performed as described in Sokal and Rohlf (1995), based on deviations from the mean slope and an analysis of variance. Intronic data of each gene were treated as noncoding DNA in DNASP 4.0, and estimates of Ks were regressed against divergence time for each gene separately and for a concatenated superintron. Evolutionary rates for intronic data (obtained as slopes of regressions) were then tested pairwise for significant deviations from the slope (i.e., rate) of the codon data using the F-test statistics from Sokal and Rohlf (1995). Separation times for Mesobuthus populations are based on the dating of the MSC and on tectonic movements of the Hellenic arc and are as follows: Cyprus (CY) versus mainland (B, P, CA, WA, SA) and, CY versus Crete (CR): 5.33 million years; Karpathos (KA) versus West Anatolia (WA): 3 million years; KA versus Rhodes (RH): 3 million years; and RH versus WA: 1.8 million years) (Hsü et al. 1977; Beerli et al. 1996; Krijgsman et al. 1999; Gantenbein and Largiadèr 2002; Duggen et al. 2003). The divergence date of 5.33 million years is based on the assumption of isolation of populations since the refilling of the Mediterranean Basin. The other two estimates come from tectonic movements of the Hellenic arc, which includes the islands of Crete, Karpathos, and Rhodes. The island of Karpathos’ connection to the mainland was broken at some time during the middle or late Pliocene (3 million year ago; Kuss 1975). Rhodes itself was connected to the Anatolian mainland until the late Pliocene or early Pleistocene (1.8 million years ago; Meulenkamp et al. 1972). Greek islands such as Samos, Kos, and Lesvos, which are surrounded by shallow waters (less than 120 m deep) were most likely connected to the Anatolian mainland during the last Pleistocene ice age (25,000 years ago). The sea level during that time was 120 m lower than the present sea level (Fairbanks 1989). Tree reconstruction of DNA sequences was carried out to resolve the relationships between island and adjacent mainland populations and to estimate evolutionary rates from branch lengths. For phylogenetic analyses all ambiguities (132 bp) and gaps (369 bp) were stripped out, as recom- 2489 MOLECULAR CLOCK OF MEDITERRANEAN SCORPIONS TABLE 1. Biogeographic region Sampling sites and sample sizes. Locality, country1 Abbreviation N Mesobuthus cyprius Gantenbein and Kropf 2000 Cyprus Tepebasi (TR) Kantara (TR) McyCY1a-d McyCY2a-b 4 2 A. Scholl A. Scholl Mesobuthus gibbosus (Brullé, 1832) Greek Balkan Parga (GR) Visitsa (GR) Mt. Olympus (GR) Central Anatolia Avanos (TR) Hacibectas (TR) Crete Vai (GR) Zakros (GR) Agios Ioanis (GR) Kares (GR) Vraskes (GR) Camares (GR) Omalos Plateau (GR) Nida Plateau (GR) locality NA (GR) Fourni Island Fourni island (GR) Gavdos Gavdos (GR) Ikaria Ikaria (GR) Karpathos Pigadia (GR) Amoopi (GR) Kos locality NA (GR) Lesvos locality NA (GR) Megisti Megisti (GR) Peloponnesus Mathia (GR) Rhodes Lindos (GR) Kolympia (GR) Monolithos (GR) South Anatolia Selale (TR) Aspendos (TR) Samos Chora (GR) Kusneika (GR) West Anatolia Yerkesik (TR) Mugla (TR) Ula (TR) MgiB1a MgiB2a MgiB3a MgiCA1a-b MgiCA2a-b MgiCR1a MgiCR2a-e MgiCR3a MgiCR4a MgiCR5a MgiCR6a MgiCR7a MgiCR8a MgiCR9a MgiFO1a MgiGA1a MgiIK1a MgiKA1a-b MgiKA2a-b MgiKO1a MgiLE1a-b MgiME1a MgiP1a-d MgiRH1a-b MgiRH2a-b MgiRH3a-b MgiSA1a-b MgiSA2a MgiSAM1a MgiSAM2a MgiWA1a-b MgiWA2a-b MgiWA3a-b 1 1 1 2 2 1 5 1 1 1 1 1 1 1 1 1 1 2 2 1 2 1 4 2 2 2 2 1 1 1 1 1 2 V. Fet V. Fet V. Fet A. Scholl A. Scholl I. Stathi I. Stathi C. Kropf M. Braunwalder M. Braunwalder B. Lüscher I. Stathi I. Stathi E. Aistleitner I. Stathi I. Stathi I. Stathi A. Scholl A. Scholl I. Stathi I. Stathi I. Stathi B. and I. Gantenbein A. Scholl A. Scholl A. Scholl A. Scholl A. Scholl A. Scholl A. Scholl A. Scholl A. Scholl A. Scholl Outgroup Mesobuthus eupeus Central Anatolia Cemilköy (TR) Meu 1 A. Scholl Mesobuthus caucasicus Central Asia Jarkurgan (UZ) Mca 1 A. Gromov, V. Fet 1 Collector Country codes: GR, Greece; TR, Turkey; UZ, Uzbekistan. mended by Swofford et al. (1996), leaving 3355 bp of concatenated DNA data for all taxa. We followed the total-evidence approach by concatenating DNA sequences into a supergene, including introns (Huelsenbeck et al. 1996). For phylogenetic tree search using maximum likelihood (ML) we used the general time reversible model with gamma correction (GTR ⫹ ⌫) as a DNA substitution model for the supergene. This model was suggested by comparing hierarchical likelihood-ratio tests (log likelihood ratios between models are available on request). Rate heterogeneity among sites was assumed to follow distribution (the shape parameter ␣ was estimated using ML) with four categories, each parameterized by its mean (Yang 1996). The tree space was explored by 10 heuristic tree searches without enforcing a molecular clock and by randomizing the order of the sequence input in PAUP* 4.0b10 (Swofford 1998). For the calibration of a local molecular clock within the previously revealed phylogenetic tree, we constrained particular branch lengths to have equal evolutionary rates (Yoder and Yang 2000). For this purpose we analyzed the concatenated intron-exon data (3856 bp) using the HYPHY package (Kosakovsky-Pond and Muse 2002) and defined 15 partitions in total, one partition per coding gene (nine in total) and one partition for each intronic data per gene (six in total, Table 3). For coding partitions we applied the MG94 ⫻ HKY85 DNA substitution model (Hasegawa et al. 1985; Muse and Gaut 1994) and for noncoding sequences we chose the HKY85 model. To reduce the parameter space, we decided to use majority-rule consensus sequences (one sequence per major phylogeographic clade). This resulted in 14 ingroup sequences and two outgroup sequences in the data matrix. We then maximized the ML function and tested whether constrained topologies, that is, local molecular clocks (null hypothesis), differ significantly from the more parameter-rich Lysozyme precursor C (Lys-C) 9 TAACAGTTGTTATCATTGATAAATTGG CG1385 BU092283/BU092304/ CB334110 BU092099/BU092259/ BU092303/CB333841/ CB333849/CB334134/ CB334149 Defensin 4kD 8 CG9111 CG8137 BU092239 Serinproteinase inhibitor Spn2 7 CG3315 BU092065 Thioredoxin1 (Trxr-1) 6 ATGGCTGGATTAGGAAGACGTCTTGTC TAACTTGACCATTTACCTAGAATGTCAC CATGTACTGACGCTGGCATTGCC ATTGGCGGGATATTACTTGTG TGAACAGTTAGCTAAGGC TTAACCCATTGATTAACTTCAT GCCATGAAAGCCGTTGCTATTCT ACGACACAAATACAGGTGA ATGGCTTTCAAGTTTTCATTTTTCG Chaperonin10-Heat shock protein 5 CG11267 Serin-type endopepdidase 4 TTATTGTATCCCTATTAGAATCGCAGTTTAAGG CG10527 BU092199/ BU092224/CB334031 BU092102/BU092213/ BU092333/CB333837/ CB333846/CB334064/ CB334077/BU091908 BU091831 Methyl transferase 3 Locus Number CG7532 CG11221 BU091820 Protein kinase 2 GAGTGTCATGCCAATAGATTACAG ATCCACACATCTTCTAAAACGGTTAATTC TCTGATGTATGGCAGATGGCAATG CGAACTCAAGATCCACTCCTGTACTCG TGGGTTCCAGCTCGCAGCGGTAACG AACTTCGTAGTCGGAATACGAATGTTCTC AGTTCTTATTGGTGTTCTTCTTTTGG CG9896 BU092066/BU092133 Unknown protein 1 Drosophila EST Accession numbers Primer sequences (5⬘ -3⬘ ) B. GANTENBEIN AND P. D. KEIGHTLEY TABLE 2. Gene identification and primers for amplification of nine nuclear protein-encoding genes. 2490 model, that is, assuming no clock in any of the branches (Huelsenbeck and Hillis 1996). In particular, we were interested to know whether the branch length of the Cyprus lineage equals the branch of the Crete lineage, since both of these islands were expected to have diverged from each other 5.33 million years ago. As a second constraint, we tested whether the branch of the island of Karpathos lineage equals 3/5.33 times the branch length of the Cyprus or the Crete lineage. The third constraint concerned the branch length of the Rhodes lineage to the ancestral node connecting the island with the Anatolian mainland, which was set to 1.8/5.33 times the Cyprus lineage. We then tested these constraint models against the alternative parameter-rich model using the 2approximated likelihood ratio statistics. Hybridization on the Island of Rhodes Molecular clock calibrations may be affected by recurrent gene flow (hybridization) (Fleischer et al. 1998; Schierup and Hein 2000; Posada and Crandall 2002). A previous allozyme study of M. gibbosus found evidence for recent artificial transplantation from the Greek mainland to the island of Rhodes, where they apparently hybridize with the autochthonous population (Gantenbein and Largiadèr 2002). In this study genotype classes were assigned based on a three-locus hybrid index ranging from 0 to 6. A hybrid index of 0 was assigned to a genotype homozygous for Greek mainland alleles, and an index of 6 was assigned to a genotype homozygous for Anatolian mainland samples. Here, we exclusively sequenced specimens (n ⫽ 6) that were assigned a hybrid index of 6. Thus, disturbance of the clock calibration and phylogenetic tree reconstruction should be minimized. RESULTS Genetic Variation within Major Clades All nine genes analyzed showed some level of polymorphism (Table 3). Locus 8 (defensin), was the most variable of the nine genes ( ⫽ 0.0704 ⫾ 0.007) due to a high number of polymorphic sites (S) for a relatively short gene fragment (78 bp of 147 bp ⫽ 0.53%). The least polymorphic gene (26 polymorphic sites of 248 bp ⫽ 0.10%) is locus 6 (Trxr-1). Estimates of and S were generally lower within the population samples of major islands than within mainland samples. For Cyprus samples, estimates of range from 0 to 0.1149 (gene 8, defensin), and similar low estimates are observed for the island of Crete, ranging from 0.0042 to 0.0533. The genetic variability within the two populations sampled from the relatively small island of Karpathos, was negligible in all nine genes compared to Cyprus, Crete, and Rhodes. Sequence variability on populations of Rhodes, however, was in the same range as Cyprus and Crete. Intron-Exon Structure of Scorpion Genes We identified 11 introns in total, based on the comparison of the genomic sequences with the respective EST-clone (Table 3). The lengths of the introns are given in Table 3 for each major phylogenetic clade. Splicing sites were generally of the exon/GT-type in the 5⬘-region and of the AG/exontype in the 3⬘-region. This pattern was also recently found 2491 MOLECULAR CLOCK OF MEDITERRANEAN SCORPIONS TABLE 3. Population1 Locus 1 2 3 4 5 6 7 8 9 1-9 B, P, CY CR KA RH all B, P, CY CR KA RH all B, P, CY CR KA RH all B, P, CY CR KA RH all B, P, CY CR KA RH all B, P, CY CR KA RH all B, P, CY CR KA RH all B, P, CY CR KA RH all B, P, CY CR KA RH all CA, WA, SA CA, WA, SA CA, WA, SA CA, WA, SA CA, WA, SA CA, WA, SA CA, WA, SA CA, WA, SA CA, WA, SA Genetic polymorphism within and among populations. Coding2 Noncoding2 Exons Polymorphic2 Parsimony informative2 Nucleotide diversity SE 357 607 612 606 609 357 328 332 335 336 336 327 339 360 360 351 360 402 258 261 258 261 261 261 183 186 186 192 186 156 375 378 372 378 375 363 342 342 342 342 339 318 72 72 78 78 90 66 309 312 315 315 312 288 254 250 255 249 252 257 0 0 0 0 0 0 73 66 62 74 64 42 76 74 76 51 51 51 65 66 62 67 68 74 0 0 0 0 0 0 0 0 0 0 0 0 108 112 100 122 116 81 495 520 518 523 517 476 4 4 4 4 4 4 1 1 1 1 1 1 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 4 4 4 4 4 4 29 7 5 5 4 67 3 1 1 0 0 11 23 1 6 2 1 28 4 1 2 0 0 57 26 12 10 0 2 32 0 1 7 0 7 13 26 0 4 0 18 44 57 49 37 2 27 78 123 64 8 34 44 223 11 1 3 1 1 33 2 0 1 0 0 7 13 0 5 0 0 16 3 0 0 0 0 21 15 0 6 0 0 18 1 0 2 0 2 11 15 0 4 0 7 31 42 13 15 0 15 49 99 28 0 2 5 165 0.0012 0.0042 0.0023 0.0044 0.0025 0.0003 0.0018 0.0010 0.0008 0.0000 0.0000 0.0046 0.0090 0.0008 0.0042 0.0024 0.0013 0.0000 0.0040 0.0010 0.0009 0.0000 0.0000 0.0179 0.0236 0.0159 0.0000 0.0000 0.0026 0.0151 0.0010 0.0014 0.0042 0.0000 0.0055 0.0046 0.0180 0.0000 0.0036 0.0000 0.0217 0.0237 0.0812 0.1149 0.0553 0.0050 0.0605 0.0704 0.0415 0.0215 0.0032 0.0214 0.0195 0.0346 ⫾0.0018 ⫾0.0016 ⫾0.0006 ⫾0.0018 ⫾0.0008 ⫾0.0016 ⫾0.0005 ⫾0.0007 ⫾0.0004 ⫾0.0000 ⫾0.0000 ⫾0.0005 ⫾0.0000 ⫾0.0005 ⫾0.0005 ⫾0.0013 ⫾0.0004 ⫾0.0011 ⫾0.0000 ⫾0.0006 ⫾0.0008 ⫾0.0000 ⫾0.0000 ⫾0.0008 ⫾0.0062 ⫾0.0103 ⫾0.0037 ⫾0.0000 ⫾0.0011 ⫾0.0024 ⫾0.0003 ⫾0.0005 ⫾0.0018 ⫾0.0000 ⫾0.0016 ⫾0.0007 ⫾0.0024 ⫾0.0000 ⫾0.0008 ⫾0.0000 ⫾0.0000 ⫾0.0030 ⫾0.0158 ⫾0.0199 ⫾0.0095 ⫾0.0017 ⫾0.0124 ⫾0.0075 ⫾0.0046 ⫾0.0028 ⫾0.0010 ⫾0.0044 ⫾0.0039 ⫾0.0029 1 Populations are B, Balkan; CR, Crete; CY, Cyprus; KA, Karpathos; P, Peloponnesus; CA, Central Anatolia; RH, Rhodes; SA, South Anatolia; WA, Western Anatolia. 2 All base-pair counts exclude ambiguities and gaps in the alignment. in the intron-exon structure of sodium and potassium channel toxins in scorpions (Froy et al. 1999) and is generally observed in eukaryotes (Levin 1994). The splicing site at the 5⬘-end is GTAAG in six of 11 cases. The splicing site at the 3⬘-end was found to be AG in all introns. The TACTAACbox, a conserved gene sequence reported for introns, involved in the splicing process, is usually located about 30 bp upstream in the 3⬘ region of other eukaryotes. We observed the following deviations from this box in scorpions: TTATAAC in intron 1, TGACAAC in intron 2, GATTAAT in intron3, all in gene 1, TTATAAT in gene 3, and GTATAAT (most likely) in gene 4. There was no obvious box in the intron of gene 5. Mean GC-content of the noncoding region was 18.6% and GC-content of the coding region was 42.0% (mean of GC2 and GC3 was 40.6% and 31.3%, respectively). 2492 B. GANTENBEIN AND P. D. KEIGHTLEY TABLE 4. Estimates of net nonsynonymous (Ka) and net synonymous (Ks) substitution rates (substitutions per site) between clades with known divergence times (million years). Net Ka and Ks are also given for between-mainland comparisons. Clade1 comparison (N) Ka SE Ks SE Ka/Ks Between island-mainland populations CY(6)-B(3) 5.33 CY(6)-P(4) 5.33 CY(6)-CA(4) 5.33 CY(6)-CR(12) 5.33 CY(6)-SA(3) 5.33 CY(6)-WA(4) 5.33 CR(12)-B(3) 5.33 CR(12)-CA(4) 5.33 CR(12)-P(4) 5.33 CR(12)-SA(3) 5.33 CR(12)-WA(4) 5.33 K(33-36)-WA(4) 3 K(33-36)-RH(6) 3 RH(6)-WA(4) 1.8 0.0156 0.0160 0.0177 0.0168 0.0178 0.0146 0.0053 0.0060 0.0042 0.0068 0.0069 0.0057 0.0056 0.0038 0.0011 0.0015 0.0018 0.0011 0.0011 0.0011 0.0004 0.0007 0.0009 0.0009 0.0012 0.0004 0.0003 0.0011 0.0284 0.0268 0.0261 0.0198 0.0267 0.0266 0.0290 0.0227 0.0265 0.0156 0.0261 0.0170 0.0117 0.0088 0.0011 0.0008 0.0007 0.0007 0.0005 0.0002 0.0009 0.0021 0.0003 0.0003 0.0002 0.0005 0.0005 0.0011 0.551 0.595 0.676 0.848 0.669 0.550 0.184 0.266 0.158 0.434 0.263 0.335 0.477 0.434 Between mainland-mainland populations B(3)-P(4) NA B(3)-CA(4) NA B(3)-SA(3) NA B(3)-WA(4) NA CA(4)-SA(3) NA CA(4)-P(4) NA CA(4)-WA(4) NA P(4)-WA(3) NA P(4)-SA(3) NA 0.0000 0.0031 0.0038 0.0039 0.0088 0.0029 0.0054 0.0042 0.0050 0.0002 0.0019 0.0019 0.0020 0.0033 0.0023 0.0020 0.0015 0.0014 0.0022 0.0123 0.0157 0.0141 0.0186 0.0096 0.0094 0.0151 0.0210 0.0009 0.0011 0.0003 0.0019 0.0005 0.0029 0.0038 0.0035 0.0031 0.000 0.256 0.243 0.279 0.473 0.304 0.568 0.277 0.238 1 Time Clades are defined in Table 1. Linear Regression Analysis of Clock Calibration (Supergene Approach) Linear Regression-Based Clock Calibration (Single-Gene Approach) Means of Ks and Ka estimated for mainland and island clades and divergence time are given in Table 4. The ratio of Ka/Ks, a general indicator of adaptive changes, ranges from 0.158 (CR-P comparison) to 0.848 (CY-CR comparison). Thus, the CY-CR comparison shows more amino acid replacements than all other comparisons. The genetic differentiation among mainland clades (i.e., B, CA, P, SA, WA) is in some cases also considerable (Table 4) and range up to 0.021 for Ks between P and SA. The differentiation between CA and SA with 0.0186 for Ks is also remarkable. These two population groups are separated by a high mountain chain, which represents a natural geographic dispersal barrier. Translating these rates into evolutionary time estimates points to the existence of very old population groups and that these mainland populations in some cases diverged from each other for about the same time frame as island populations diverged from mainland populations (5.33 million years ago). The linear regression of the concatenated supergene is shown in Figure 2. The regression shows a linear increase in the synonymous substitution rate (Ks) with expected divergence time (slope ␣ ⫽ 2.28 ⫾ 0.44 substitutions per [site ⫻ 109 years], P ⬍ 0.0001, intercept  ⫽ 2.26 ⫾ 4.80, P ⫽ 0.89; Table 5, Fig. 2A). The slope for the introns is slightly steeper (Fig. 2B), due to the two extreme values at the 5.33 Million years ago calibration point (i.e., the comparisons CYSA and CR-P). The value of the nonsynonymous substitution rate (Ka) is less clear, since the slope is not significantly different from zero (␣ ⫽ 1.18 ⫾ 0.60, P ⫽ 0.07,  ⫽ ⫺0.50, P ⫽ 0.87). The mean of estimates of Ks and Ka between major clades of known divergence times were calculated for each gene separately in the same way as for the concatenated supergene and plotted against divergence time. Fitting linear regressions through these plots reveals variation in the regression slope estimates across the nine genes. The slopes and their F-statistics for the individual genes and R2 for each regression are summarized in Table 5, computed including an intercept. The intercepts are not significantly different from zero except for genes 7 and 9 for Ks and for genes 4, 6, and 8 for Ka. Leastsquare estimates of slopes are not significantly different from zero in five of the nine genes for Ks and are only significant for Ka in one case. Analysis of variance among the slopes gave significant F-ratio statistics (Table 5), supporting the hypothesis that these genes vary in their selective constraints or in their mutation rates. The standard errors of the slopes (Ks and Ka) for the supergene approach are downwardly biased, and thus, are generally smaller than the standard errors calculated from the mean of slopes (Sokal and Rohlf 1995; Hillis et al. 1996). The evolutionary rates for the introns (expressed as Ks) of the six genes vary between ⫺4.96 and 6.20 (mean 3.45 ⫾ 1.18) nucleotide substitutions per (site ⫻ 109 years). This is similar to the mean Ks at synonymous sites of the proteincoding data. Phylogenetic Inference The heuristic ML tree search, calculated without enforcing a molecular clock, revealed a single tree (Fig. 3) containing MOLECULAR CLOCK OF MEDITERRANEAN SCORPIONS 2493 solved, but sequences from the same sampling locality tend to cluster together with high bootstrap support. The four sequences from the island of Karpathos, a geographically wellseparated island from the Anatolian mainland, are also well separated from neighboring islands. Sequences from the island of Rhodes cluster at a relatively low divergence level compared to the Cyprus lineage. At first sight, branch lengths of the tree seem to agree very well with the presumed separation time from geology (Figs. 1, 3). To further investigate this qualitative finding, we tested whether the branch lengths of the Cyprus and Cretan lineage could be constrained to equal length and whether the branch length of the Karpathos lineage (blKA) corresponds to 3/5.33th the branch length of the Cyprus (blCY) and Createan lineage (blCR). In addition, the Rhodes lineage (blRH) was constrained to have diverged 1.8/5.33th of the branch length of the Cyprus or Crete lineage. The phylogeny of the 16 majority-rule consensus sequences reveals a slightly different tree topology from the 58 taxa phylogeny, but the major conclusion that the Cyprus, Cretan, and Karpathos island sequences are well-separated remains (tree not shown). The constraint model (null hypothesis; blCY ⫽ blCR and blKA ⫽ 3/5.33blCY and blRH ⫽ 1.8/5.33blCY) is not significantly different from the unconstrained model (alternative hypothesis) if only synonymous rates are considered; 2␦ ⫽ 2(l0 ⫺ l1) ⫽ 2(13,553.80 ⫺ 13,542.60) ⫽ 22.40, df ⫽ 56, P ⫽ 0.66. Thus, Ks of each exon partition fits the proposed molecular clock model fairly well. However, if Ks and Ka are constrained according to the above branch length ratios, the difference in log likelihood between the trees is significantly lower (2␦ ⫽ 2(l0 ⫺ l1) ⫽ 2(10,584.95 ⫺ 10,542.60) ⫽ 84.70, df ⫽ 52, P ⫽ 0.0028). This is mainly caused from the Cyprus lineage, which has an increased Ka, as calculated from the branch length (mean of nine branch lengths ⫽ 7.40 ⫾ 3.88 substitutions per [site ⫻ 109 years]) as compared to the Cretan lineage (mean 2.70 ⫾ 1.84 substitutions per [site ⫻ 109 years]). DISCUSSION Estimates of Evolutionary Rates in Protein-Coding Genes FIG. 2. (A) Mean estimates of synonymous (Ks) and (C) nonsynonymous (Ka) DNA substitutions per site based on a supergene (⫽ nine concatenated single genes) plotted against evolutionary time. For comparison, Ks for concatenated introns (B) plotted against time is also given. The 95% confidence limits of the mean are shown. 11 lineages, each supported by rather high bootstrap values. The outgroup species, Mesobuthus eupeus and M. caucasicus are well separated by long branches from the ingroup sequences. The most conspicuous ingroup lineage is the Cyprus lineage, and its branch length is even longer than that of the Cretan lineage. This finding supports the recent elevation of the Cyprus lineage to the species level, M. cyprius, based on morphological and allozyme data (Gantenbein et al. 2000). The phylogenetic relationships among the mainland samples (B, P, CA, SA, WA) and the several small Greek island samples (KO, SAM, IK, FO, LE, ME) are less clearly re- The range of variation in evolutionary rates among our sample of nine loci is considerable and could originate from sampling, different mutation rates, and/or different evolutionary constraints acting on each gene. Li (1997) provides estimates for evolutionary rates for Drosophila (33 proteins) and mammals (47 proteins). For Drosophila proteins, the average Ks was 15.6 ⫾ 5.5 (per site ⫻ 109 years) and for mammals 3.51 ⫾ 1.01. Estimates for Ka were 1.91 ⫾ 1.42 in Drosophila genes and 0.74 ⫾ 0.67 in mammals. Our estimates for Ks (3.17 ⫾ 1.54 per [site ⫻ 109 years]) and Ka (0.39 ⫾ 0.94 per [site ⫻ 109 years]) are therefore comparable to rates estimated in mammalian genes. However, these datasets differ from each other in the choice of protein sequences, and our estimates are potentially biased by the fact that primers were designed from a cDNA library, which tends to overrepresent highly expressed genes. To our knowledge there is no other study with a similar DNA dataset from any other invertebrate with a comparably well-calibrated molecular clock (Zhang and Hewitt 2003). Since buthid scorpions have a generation time of about 24 months, which is more like mammals than invertebrates, the 2494 B. GANTENBEIN AND P. D. KEIGHTLEY TABLE 5. Estimates of evolutionary rates for nine single protein-coding genes from linear regression analysis and from a concatenated supergene. Asterisks mark significant P-values at the 0.05 level. Locus Protein-coding Ks 1 2 3 4 5 6 7 8 9 Mean F8,108 Ks supergene Slope ⫾SE P-value Intercept ⫾SE P-value R2 4.07 1.76 1.35 3.30 2.67 1.73 ⫺1.58 14.71 0.49 3.17 1.50 0.77 1.13 1.16 1.66 1.15 1.72 3.89 1.78 1.54 0.02* 0.04* 0.25 0.01* 0.13 0.16 0.37 0.00* 0.79 5.29 0.15 0.34 ⫺5.18 ⫺6.63 ⫺2.69 26.17 ⫺13.62 27.05 2.26 7.30 3.76 5.50 5.65 8.09 5.60 8.39 18.98 8.70 4.80 0.48 0.97 0.95 0.38 0.43 0.64 0.01* 0.49 0.01* 0.38 0.30 0.11 0.40 0.18 0.16 0.07 0.54 0.01 2.28 0.44 0.32 2.17 0.89 0.69 2.28 0.51 0.29 ⫺0.10 0.44 ⫺0.27 5.42 ⫺5.40 0.32 0.39 0.55 0.22 0.27 0.36 0.88 0.27 3.35 5.50 1.17 0.94 ⫺4.64 ⫺1.26 ⫺0.72 4.24 1.18 3.47 ⫺6.85 77.76 7.38 8.95 2.69 1.09 1.31 1.75 4.28 1.33 16.34 26.84 5.71 8.72 0.11 0.27 0.59 0.03* 0.79 0.02* 0.68 0.01* 0.22 0.59 0.30 0.09 0.01 0.02 0.07 0.18 0.07 0.01 1.18 0.60 ⫺0.50 2.92 0.87 0.24 4.17 5.73 4.74 6.20 ⫺4.96 3.44 3.22 4.42 0.61 1.30 2.21 2.95 6.51 2.24 1.69 1.30 ⫺4.33 ⫺14.22 ⫺6.05 ⫺8.39 74.12 6.18 7.88 ⫺7.00 2.97 6.34 10.79 14.42 31.79 10.96 13.52 6.36 0.17 0.04* 0.59 0.57 0.04* 0.58 0.80 0.62 0.28 0.27 0.05 0.16 0.29 0.49 ⬍0.0001* 0.00* Ka 1 2 3 4 5 6 7 8 9 Mean F8,108 Ka supergene Noncoding/intronic Introns gene 1 3 4 5 8 9 Mean All Introns F5,72 low estimates could be a consequence of a long generation time. However, it is also possible that this is a consequence of differences in metabolic rates, scorpions surely being at the lower end of the range (Martin and Palumbi 1993; Lighton et al. 2001); a recent comparative study on metabolic rates in arachnids and insects revealed that scorpion metabolic rates are about one-quarter of those of insects, spiders, mites, and solpugids of the same size (Lighton et al. 2001), and scorpions are among the animals having the lowest metabolism rates in the animal kingdom. It is plausible that generation time and metabolic rate influence evolutionary rate synergistically (Martin and Palumbi 1993). Finally, it has also been shown that body size is positively correlated with evolutionary rate, at least in mammals (Martin and Palumbi 1993). It is unknown whether such correlations exist in poikilothermic animals or invertebrates in general. Further data are available on evolutionary rates in mitochondrial genes in scorpions. These genes generally evolve faster than nuclear genes (Lynch and Jarrell 1993; Martin and Palumbi 1993; Simon et al. 1994), and several mechanisms have been formulated to account for this effect: the lack of recombination in animal mtDNA (Rokas et al. 2003) and less efficient DNA repair mechanisms (Martin and Pal- 0.00* 0.04* 0.30 0.80 0.62 0.35 0.13 0.34 0.79 ⬍0.0001* 0.07 0.00* 0.00* 0.05* 0.06 0.46 0.15 0.01* ⬍0.0001* umbi 1993; Avise 1994). For vertebrate mtDNA, the rate of molecular evolution has been estimated at 2% per Million years ago (or 1 ⫻ 10⫺8 substitutions per [year ⫻ site] per lineage; Brown et al. 1979). This often cited mitochondrial molecular clock for vertebrates has recently been evaluated using mtDNA clock calibrations of invertebrate species such as Hawaiian Drosophila (DeSalle et al. 1987; Fleischer et al. 1998), Hawaiian crickets of the genus Laupala (Fleischer et al. 1998), South American butterflies of the genus Heliconius (Brower 1994), and in North African-Iberian carabids of the genus Carabus (Prüser and Mossakowski 1998) and Timarcha (Gómez-Zurita et al. 2000). These rates range between 4.9 and 7.0 ⫻ 10⫺9 substitutions per (years ⫻ site) per lineage, and are surprisingly close to rates observed in vertebrates (Brown et al. 1979). In scorpions, the evolutionary rate of two mitochondrial genes, the subunit I of cytochrome oxidase, and the large ribosomal subunit (16S rRNA), have been estimated at ⬃1% divergence per million years for the Aegean species M. gibbosus, which translates to 5.0 substitutions per (site ⫻ 109 year) per lineage (Gantenbein and Largiadèr 2002, 2003; Gantenbein et al. 2003). In scorpions, synonymous sites in mtDNA genes evolve about two times faster than in nuclear DNA proteins. However, it has been MOLECULAR CLOCK OF MEDITERRANEAN SCORPIONS 2495 FIG. 3. Maximum likelihood (ML) tree of east Mediterranean scorpion populations of the genus Mesobuthus based on a concatenated supergene of exon-intron data of nine nuclear protein genes. The ML-model was a GTR ⫹ G with the following parameters: A ⫽ 0.342, C ⫽ 0.174, G ⫽ 0.207, T ⫽ 0.277; gamma shape parameter ␣ ⫽ 0.785; proportion of invariable sites I ⫽ 0.460; rate parameters, AC ⫽ 0.798, A-G ⫽ 0.887, A-T ⫽ 0.635, G-C ⫽ 0.743, C-T ⫽ 1.743, G-T ⫽ 1.0, respectively. Nodes at branches refer to bootstrap values ⬎65% inferred from neighbor-joining using 1000 ML-estimated pairwise distance-pseudo replicates as the input matrix. Designations for sequences are given in Table 1. Arrows indicate well-dated branching points of lineages. shown that the ratios between mean nuclear DNA and mtDNA differ significantly among animal groups (Caccone et al. 1988). Biogeographic Conclusions and the Reliability of Calibration Dates The inferred phylogeny (Fig. 3) supports the hypothesis that all of the analyzed specimens are autochthonous, and there is no obvious case of recent artificial transplantation having affected the clock calibration. The Cyprus lineage is well separated from M. gibbosus, and the tree confirms M. eupeus and M. caucasicus as outgroup species. This tree shape observed for nuclear genes is also in agreement with a recent DNA study using combined DNA data of two mtDNA fragments and the PK gene (locus 2 of this study; Fet et al. 2003; Gantenbein et al. 2003). The clustering among island and mainland populations of M. gibbosus is in general agreement with the allozyme tree of Gantenbein and Largiadèr (2002). The fact that the mainland populations of M. gibbosus are genetically very distinct (genetic divergence CA-SA, SAWA) supports the hypothesis that the genus Mesobuthus is 2496 B. GANTENBEIN AND P. D. KEIGHTLEY of central Asian origin, where it is most diverse and where several species and subspecies have been described. The Aegean island system is particularly well understood geologically (Meulenkamp et al. 1972; Kuss 1975; Le Pichon and Angelier 1979; Meulenkamp 1985), and the geological isolation dates are believed to be reliable. Although our initial hypothesis of colonization and subsequent isolation of scorpion populations is a very strong assumption (see Materials and Methods) the estimated Ks-values appear to follow a linear molecular clock model (Fig. 2). Thus, other factors, such as different ancestral population sizes between mainland and island samples, might not be important influences on evolutionary rates in scorpions. ACKNOWLEDGMENTS We thank I. Gantenbein-Ritter for laboratory assistance. F. Balloux, A. Eyre-Walker, and D. Gaffney critically commented on an earlier version of the manuscript. BG was supported by a Swiss National Science Foundation IHP grant (83-EU-065528), the Royal Society (R-36579), and the Basler Stiftung für experimentelle Zoologie (c/o Eidgenössisches Tropeninstitut). Field trips were supported by the commission for travelgrants of the Swiss Academy of Natural Science. LITERATURE CITED Andolfatto, P., M. Scriber, and B. Charlesworth. 2003. No association between mitochondrial DNA haplotypes and a femalelimited mimikry phenotype in Papilio glaucus. Evolution 57: 305–316. Avise, J. 1994. Molecular markers, natural history and evolution. Chapman and Hill, New York. Beerli, P., H. Hotz, and H. Uzzell. 1996. Geologically dated sea barriers calibrate a protein clock for Aegean water frogs. Evolution 50:1676–1687. Brower, A. V. Z. 1994. Rapid morphological radiation and convergence among races of the butterfly Heliconius erato inferred from patterns of mitochondrial DNA evolution. Proc. Natl. Acad. Sci. USA 91:6491–6495. Brown, W. M., M. George Jr., and A. C. Wilson. 1979. Rapid evolution of animal mitochondrial DNA. Proc. Natl. Acad. Sci. USA 44:1967–1971. Brusca, R. C. 2000. Unraveling the history of arthropod biodiversification. Ann. Mo. Bot. Gard. 87:13–25. Caccone, A., G. D. Amato, and J. R. Powell. 1988. Rates and patterns of scnDNA and mtDNA divergence within the Drosophila melanogaster subgroup. Genetics 118:671–683. DeSalle, R., T. Freedman, E. M. Prager, and A. C. Wilson. 1987. Tempo and mode of sequence evolution in mitochondrial DNA. J. Mol. Evol. 26:157–164. Duggen, S., K. Hoernle, P. van den Bogaard, L. Rupke, and J. P. Morgan. 2003. Deep roots of the Messinian salinity crisis. Nature 422:602–606. Fairbanks, R. G. 1989. A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the younger Dryas event and deep-ocean circulation. Nature 342:637–642. Fet, V., W. D. Sissom, G. Lowe, and M. E. Braunwalder. 2000. Catalog of the scorpions of the world (1758–1998). The New York Entomological Society, New York. Fet, V., B. Gantenbein, A. V. Gromov, G. Lowe, and W. R. Lourenço. 2003. The first molecular phylogeny of Buthidae (Scorpiones). Euscorpius 4:1–12. Fleischer, R. C., C. E. McIntosh, and C. L. Tarr. 1998. Evolution on a volcanic conveyor belt: using phylogeographic reconstructions and K-Ar-based ages of the Hawaiian Islands to estimate molecular evolutionary rates. Mol. Ecol. 7:533–545. Froy, O., and M. Gurevitz. 2003. New insight on scorpion diver- gence inferred from comparative analysis of toxin structure, pharmacology and distribution. Toxicon 42:549–555. Froy, O., T. Sagiv, M. Poreh, D. Urbach, N. Zilberberg, and M. Gurevitz. 1999. Dynamic diversification from a putative common ancestor of scorpion toxins affecting sodium, potassium, and chloride channels. J. Mol. Evol. 48:187–196. Gantenbein, B. 2004. The genetic population structure of Buthus occitanus (Scorpiones: Buthidae) across the Strait of Gibraltar: calibrating a molecular clock using nuclear allozyme variation. Biol. J. Linn. Soc. 81:519–534. Gantenbein, B., and C. R. Largiadèr. 2002. Mesobuthus gibbosus (Scorpiones: Buthidae) on the island of Rhodes: hybridisation between Ulysses’ stowaways and native scorpions? Mol. Ecol. 11:925–938. ———. 2003. The phylogeographic importance of the Strait of Gibraltar as a gene flow barrier in terrestrial arthropods: a case study with the scorpion Buthus occitanus as model organism. Mol. Phylogenet. Evol. 28:119–130. Gantenbein, B., C. Kropf, C. R. Largiadèr, and A. Scholl. 2000. Molecular and morphological evidence for the presence of a new buthid taxon (Scorpiones: Buthidae) on the island of Cyprus. Rev. Suisse Zool. 107:213–232. Gantenbein, B., M. E. Soleglad, and V. Fet. 2001. Euscorpius balearicus Caporiacco, 1950, stat. nov. (Scorpiones: Euscorpiidae): molecular (allozymes and mtDNA) and morphological evidence for an endemic Balearic Islands species. Org. Divers. Evol. 1: 301–320. Gantenbein, B., V. Fet, and A. V. Gromov. 2003. The first DNA phylogeny of four species of Mesobuthus Vachon, 1950 (Scorpiones, Buthidae) from Eurasia. J. Arachnol. 31:412–420. Gaunt, M. W., and M. A. Miles. 2002. An insect molecular clock dates the origin of the insects and accords with palaeontological and biogeographic landmarks. Mol. Biol. Evol. 19:748–761. Gillespie, J. H. 1989. Lineage effects and the index of dispersion of molecular evolution. Mol. Biol. Evol. 6:636–648. Giribet, G., G. D. Edgecombe, and W. C. Wheeler. 2001. Arthropod phylogeny based on eight molecular loci and morphology. Nature 13:157–161. Gómez-Zurita, J., C. Juan, and E. Petitpierre. 2000. The evolutionary history of the genus Timarcha (Coleoptera, Chrysomelidae) inferred from mitochondrial COII gene and partial 16S rDNA sequences. Mol. Phylogenet. Evol. 14:304–317. Hasegawa, M., H. Kishino, and T. Yano. 1985. Dating of the humanape splitting by a molecular clock of mitochondrial DNA. J. Mol. Evol. 22:160–174. ———. 1987. Man’s place in Hominoidea as inferred from molecular clocks of DNA. J. Mol. Evol. 26:132–147. Hedges, S. B., and S. Kumar. 2003. Genomic clocks and evolutionary time scales. Trends Genet. 19:200–206. Hillis, D. M., B. K. Mable, and C. Moritz. 1996. Applications of molecular systematics. Pp. 515–545 in D. M. Hillis, C. Moritz, and B. K. Mable, eds. Molecular systematics. Sinauer Associates, Sunderland, MA. Hsü, K. J., L. Montadert, D. Bernoulli, M. B. Cita, A. Erickson, R. E. Garrison, R. B. Kidd, F. Mèlierés, C. Müller, and R. Wright. 1977. History of the Mediterranean salinity crisis. Nature 267: 399–403. Huelsenbeck, J. P., and D. M. Hillis. 1996. Parametric bootstrapping in molecular phylogenetics: applications and performance. Pp. 19–47 in J. D. Ferraris and S. R. Palumbi, eds. Molecular zoology: advances, strategies, and protocols. John Wiley and Sons, New York. Huelsenbeck, J. P., J. J. Bull, and C. W. Cunningham. 1996. Combining data in phylogenetic analysis. Trends Ecol. Evol. 11: 152–158. Jukes, T. H., and C. R. Cantor. 1969. Evolution of protein molecules. Pp. 21–132 in H. N. Munro, ed. Mammalian protein metabolism. Academic Press, New York. Keegan, H. L. 1998. Scorpions of medical importance. Fitzgerald Publishing, London. Kinzelbach, R. 1975. Die Skorpione des Agais. Beiträge zur Systematik, Phylogenie und Biogeographie. Zool. Jb. Syst. 102: 12–50. MOLECULAR CLOCK OF MEDITERRANEAN SCORPIONS Kishino, H., J. L. Thorne, and W. J. Bruno. 2001. Performance of a divergence time estimation method under a probabilistic model of rate evolution. Mol. Biol. Evol. 18:352–361. Knowlton, N., and L. A. Weight. 1998. New dates and new rates for divergence across the Isthmus of Panama. Proc. R. Soc. Lond. B 265:2257–2263. Knowlton, N., L. A. Weigt, L. A. Solorzano, D. K. Mills, and E. Bermingham. 1993. Divergence in proteins, mitochondrial DNA, and reproductive compatibility across the Isthmus of Panama. Science 260:1629–1631. Kosakovsky-Pond, S., and S. V. Muse. 2002. HYPHY: hypothesis testing using phylogeny. Available via www.hyphy.org. Krijgsman, W., F. J. Hilgen, I. Raffi, F. J. Sierro, and D. S. Wilson. 1999. Chronology, causes and progression of the Messinian salinity crisis. Nature 400:652–655. Kumar, S., and B. Hedges. 1998. A molecular timescale for vertebrate evolution. Nature 392:917–920. Kuss, S. E. 1975. Die pleistozänen Hirsche der ost-mediterranen Inseln Kreta, Kasos, Karpathos und Rhodos (Griechenland). Ber. Naturforsch. Gem. Freib. Breisgau 65:25–79. Le Pichon, X., and J. Angelier. 1979. The hellenic Arc and trench system: a key to the neotectonic evolution of the eastern Mediterranean area. Tectonophysics 60:1–42. Levin, B. 1994. Genes V. Oxford Univ. Press, Oxford, U.K. Li, W.-H. 1997. Molecular evolution. Sinauer Associates, Sunderland, MA. Lighton, J., P. Brownell, B. Joos, and R. Turner. 2001. Low metabolic rate in scorpions: implications for population biomass and cannibalism. J. Exp. Biol. 204:607–613. Loret, E., and B. Hammock. 2001. Structure and neurotoxicity of venoms. Pp. 204–233 in P. Brownell and G. A. Polis, eds. Scorpion biology and research. Oxford Univ. Press, New York. Lynch, M., and P. E. Jarrell. 1993. A method for calibrating molecular clocks and its application to animal mitochondrial DNA. Genetics 135:1197–1208. Margoliash, E. 1963. Primary structure and evolution of cytochrome c. Proc. Natl. Acad. Sci. USA 50:672–679. Martin, A. P., and S. R. Palumbi. 1993. Body size, metabolic rate, generation time and the molecular clock. Proc. Natl. Acad. Sci. USA 90:4087–4091. Meulenkamp, J. E. 1985. Aspects of the late Cenozoic evolution of the Aegean region. Pp. 307–321 in D. J. Stanley and F. C. Wezel, eds. Geological evolution of the Mediterranean Basin. Springer, New York. Meulenkamp, J. E., E. F. J. De Mulder, and A. Van de Werd. 1972. Sedimentary history and paleogeography of the late Cenozoic of the island of Rhodos. Z. Deutsch. Geol. Ges. 123:541–553. Muse, S., and B. Gaut. 1994. A likelihood approach for comparing synonymous and nonsynonymous nucleotide substitution rates, with application to the chloroplast genome. Mol. Biol. Evol. 11: 715–724. Nei, M., and T. Gojobori. 1986. Simple methods for estimating the number of synonymous and nonsynonymous nucleotide substitutions. Mol. Biol. Evol. 3:418–426. Nei, M., and W. H. Li. 1979. Mathematical model for studying genetic variation in terms of restriction endonucleases. Proc. Natl. Acad. Sci. USA 76:5269–5273. Ohta, T., and M. Kimura. 1971. On the constancy of the evolutionary rate of cistrons. J. Mol. Evol. 1:18–25. 2497 Peterson, K. J., J. B. Lyons, K. S. Novak, C. M. Takacs, M. J. Wargo, and M. A. McPeek. 2004. Estimating metazoan divergence times with a molecular clock. Proc. Natl. Acad. Sci. USA 101:6536–6541. Pisani, D., L. L. Poling, M. Lyons-Weiler, and S. B. Hedges. 2004. The colonization of land by animals: molecular phylogeny and divergence times among arthropods. BMC Biology 2:1–10. Polis, G. A., C. N. McReynolds, and G. R. Ford. 1985. Home range geometry of the desert scorpion Paruroctonus mesaensis. Oecologia (Berlin) 67:273–277. Posada, D., and K. A. Crandall. 2002. The effect of recombination on the accuracy of phylogeny estimation. J. Mol. Biol. 54: 396–402. Prüser, F., and D. Mossakowski. 1998. Low substitution rates in mitochondrial DNA in Mediterranean carabid species. Insect Mol. Biol. 7:121–128. Rokas, A., E. D. Ladoukakis, and E. Zouros. 2003. Animal mitochondrial DNA recombination revisited. Trends Ecol. Evol. 18: 411–417. Rozas, J., and R. Rozas. 1999. DnaSP version 3: an integrated program for molecular population genetics and molecular evolution analysis. Bioinformatics 15:174–175. Sambrook, J., E. F. Fritsch, and T. Maniatis. 1989. Molecular cloning: a laboratory manual. Cold Spring Harbor Laboratory Press, Cold Spring Harbor, NY. Schierup, M. H., and J. Hein. 2000. Consequences of recombination on traditional phylogenetic analysis. Genetics 156:879–891. Simon, C., F. Frati, A. Beckenbach, B. Crespi, H. Liu, and P. Flook. 1994. Evolution, weighting, and phylogenetic utility of mitochondrial gene sequences and a compilation of conserved polymerase chain reaction primers. Entomol. Soc. Am. 87:651–701. Sokal, R. R., and F. J. Rohlf. 1995. Biometry. 3rd ed. W. H. Freeman, New York. Swofford, D. L. 1998. PAUP*: phylogenetic analysis using parsimony (* and other methods). Ver. 4. Sinauer Associates, Sunderland, MA. Swofford, D. L., G. J. Olsen, P. J. Waddell, and D. M. Hillis. 1996. Phylogenetic inference. Pp. 407–510 in D. M. Hillis, C. Moritz, and B. K. Mable, eds. Molecular systematics. Sinauer Associates, Sunderland, MA. Thompson, J. D., T. J. Gibson, F. Plewniak, F. Jeanmougin, and D. G. Higgins. 1997. The ClustalX windows interface: flexible strategies for multiple sequence alignment aided by quality analysis tools. Nucleic Acids Res. 25:4876–4882. Yamashita, T., and G. A. Polis. 1995. Geographical analysis of scorpion populations on habitat islands. Heredity 75:495–505. Yang, Z. 1996. Among-site rate variation and its impact on phylogenetic analyses. Trends Ecol. Evol. 11:367–372. Yoder, A. D., and Z. Yang. 2000. Estimation of primate speciation dates using local molecular clocks. Mol. Biol. Evol. 17: 1081–1090. Zhang, D.-X., and G. M. Hewitt. 2003. Nuclear DNA analyses in genetic studies of populations: practice, problems and prospects. Mol. Ecol. 12:563–584. Zuckerkandl, E., and L. Pauling. 1965. Evolutionary divergence and convergence in proteins. Pp. 97–166 in V. Bryson and H. J. Vogel, eds. Evolving genes and proteins. Academic Press, New York. Corresponding Editor: M. Nachman
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