BIOTROPICA 37(3): 397–402 2005 10.1111/j.1744-7429.2005.00052.x Microbial Biomass, Respiration, and Decomposition of Hura crepitans L. (Euphorbiaceae) Leaves in a Tropical Stream1 Manuela Abelho2,4 , Claudia Cressa3 , and Manuel A. S. Graça4 2 Departamento de Ciências Exactas e do Ambiente, Escola Superior Agrária de Coimbra, Bencanta, 3040-316 Coimbra, Portugal 3 Centro de Biologı́a Celular, Laboratório de Biologı́a Experimental, Universidad Central de Venezuela, Apartado Postal 47114, Caracas 1041-A, Venezuela 4 IMAR – Institute of Marine Research, C/O Departamento de Zoologia, Universidade de Coimbra, 3004-517 Coimbra, Portugal ABSTRACT The processing of leaves in temperate streams has been the subject of numerous studies but equivalent tropical ecosystems have received little attention. We investigated leaf breakdown of a tropical tree species (Hura crepitans, Euphorbiaceae), in a tropical stream using leaf bags (0.5 mm mesh) over a period of 24 days. We followed the loss of mass and the changes in adenosine triphosphate (ATP) concentrations and respiration rates associated with the decomposing leaves. The breakdown rate was fast (k = −0.0672/d, k d = −0.0031/degree-day), with 81 percent loss of the initial mass within 24 days. This high rate was probably related to the stable and high water temperature (22◦ C) favoring strong biological activity. Respiration rates increased until day 16 (1.1 mg O 2 /h/g AFDM), but maximum ATP concentrations were attained at day 9 (725 nmol ATP/g AFDM) when leaf mass remaining was 52 percent. To determine the relative importance of fungi and bacteria during leaf decomposition, ATP concentrations, and respiration rates were determined in samples treated with antibiotics, after incubation in the stream. The results of the samples treated with the antifungal or the bacterial antibiotic suggest a higher contribution of the fungal community for total microbial biomass and a higher contribution of the bacterial community for microbial respiration rates, especially during the later stages of leaf decomposition. However, these results should be analyzed with caution since both antibacterial and antifungal agents did not totally eliminate microbial activity and biomass. RESUMEN La descomposición de hojas en riachuelos de zonas templadas ha sido bien estudiada pero en zonas tropicales se le ha dado poca atención. La descomposición de hojas de la especie tropical Hura crepitans fue estudiada en un rı́o tropical colocando hojas en bolsas de tela con malla de 0.5 mm por un periodo de 24 dı́as. Se documento la cantidad de masa pérdida y las fluctuaciónes en las concentraciónes trifosfato de adenina (ATP) y en las tasas respiratorias asociadas con las hojas en descomposición. La tasa de descomposición fue rápida (k = −0.0672/dı́a, k d = −0.0031/grados-dı́a), con 81por ciento de masa inicial perdida al final de 24 dı́as. La tasa observada esta probablemente relacionada con la temperatura estable y elevada del agua (22◦ C), favoreciendo una fuerte actividad biológica. Las tasas de respiración aumentaron hasta el dı́a 16 (1.1 mg O 2 /h/g AFDM), pero la concentración máxima de ATP fue obtenida en el dı́a 9 (725 nmol ATP/g AFDM), cuando la masa restante estaba al 52 por ciento. Para cuantificar la importancia relativa de hongos y bacterias durante la descomposición, las concentraciones de ATP y las tasas de respiración fueron determinadas en muestras tratadas con antibióticos, después de ser incubadas en lo rı́o. Los resultados individuales de los tratamientos contra las bacterias y contra los hongos sugieren una mayor contribución de la comunidad de hongos para la biomasa microbiana total y una mayor contribución de la comunidad de bacterias para las tasas de respiración, principalmente durante las fases más tardı́as de la descomposición. Sin embargo, estos resultados deben ser analizados con cautela ya que los antibióticos no fueron completamente eficientes para eliminar la actividad y biomasa de los microorganismos. Key words: ATP; bacteria; fungi; Hura crepitans; leaf decomposition; respiration; tropical stream; Venezuela. ALLOCHTHONOUS ORGANIC MATTER, such as leaf litter from riparian vegetation, is the most important source of energy in forested headwater streams (e.g., Fisher & Likens 1973, Abelho 2001). Leaf litter breakdown is thus a key element of ecosystem function in such streams (Rowe et al. 1996). Four major mechanisms are responsible for the decomposition of leaf litter in streams: leaching, microbial degradation, macroinvertebrate feeding activities, and flow-related fragmentation (e.g., Boling et al. 1975, Webster & Benfield 1986, Gessner et al. 1999). Irons et al. (1994) suggested that the relative importance of shredding versus microbial processing increases at cooler, higher latitudes along the latitudinal thermal gradient. However, some authors argue that the contribution of macroconsumers, such as decapod crustaceans, has been overlooked in tropical streams and that these animals may be more important in processing 1 Received organic matter than are small consumers (Rosemond et al. 1998, Covich et al. 1999). The reason for an increased importance of microbes toward the tropics in litter decomposition is the positive effect of elevated temperature on biological activity (Benstead 1996, Rosemond et al. 1998, Mathuriau & Chauvet 2002). Fungi, especially aquatic hyphomycetes, are considered the main microbial decomposers of leaf litter in streams (Bärlocher 1992, Suberkropp 1992, Gessner 1997, Gessner et al. 1997, Hieber & Gessner 2002). However, some authors argue that bacteria can also play an important role due to their rapid turnover, especially during later stages of decomposition (Weyers & Suberkropp 1996, Baldy & Gessner 1997). Leaf litter decomposition has been the subject of numerous studies in temperate streams (see review by Abelho 2001), but little is known about the process in the tropics, especially regarding microbial colonization and activity. The objective of this study was 10 April 2003; revision accepted 15 December 2004. 397 398 Abelho, Cressa, and Graça to document microbial mediated decomposition of Hura crepitans leaves in a tropical stream. METHODS STUDY SITE.—Fieldwork was conducted in Camurı́ stream, a hardwater stream located 20 km north of Caracas, at the north slope of the Avila Mountain, North Venezuela (approximately 10◦ 30 N, 66◦ 30 W). At the study site the stream flows through evergreen and deciduous tree communities that provided year-round shading and inputs of leaf litter. A riffle area was chosen as the specific site of the study. The streambed at the study site was 2.0–2.5 m wide and was composed of bedrock and cobbles with sand. During the study period, discharge was 0.14 m3 /sec (range = 0.09–0.20 m3 /sec), current velocity at the bags was 31 cm/sec (range = 22–40 cm/sec), depth at the bags was 26 cm (range = 24– 28 cm), pH was 7.9 (range = 7.7–8.5), conductivity was 109 µS/cm (range 100–115 µS/cm), dissolved oxygen was 9.5 mg/L (range = 9.3–9.7 mg/L), and mean water temperature was 22◦ C (range = 20–23◦ C). PREPARATION, COLLECTION AND PROCESSING OF LITTERBAGS.— Senescent leaves of the deciduous tree Hura crepitans L. (Family Euphorbiaceae) were collected prior to abscission from trees in Venezuela. Initial nitrogen and phosphorus content of the leaves (Graça et al. 2001) was 1.4 percent N and 0.23 percent P. Leaves were air-dried, and a known amount (3.1 ± 0.1 g) was placed in 0.5 mm mesh-size bags. On 7 March 1997 (during late litterfall period) 35 litterbags were tied to iron rods anchored in the streambed. The contents of an additional seven bags were oven-dried (60◦ C, 72 h) to calculate a mean humidity factor (oven-dry mass/air-dry mass). The initial oven-dry mass in the experimental bags was estimated by multiplying initial air-dry mass by the mean humidity factor (0.91, range 0.89–0.93). Seven bags were randomly collected after 1, 5, 9, 16, and 24 days, and returned to the laboratory individually in a container of stream water. The bags were opened and the leaves were gently washed to remove loosely attached debris. From each bag, five sets of eight leaf discs (total = 40 discs) were cut with a cork borer (diameter 14.5 mm). The rest of the leaf material in each bag was oven-dried (60◦ C, 72 h) to determine dry mass. One set of eight leaf discs (reference) was oven-dried and ashed (500◦ C, 5 h) to determine ash-free dry mass (AFDM). The other sets were used to determine respiration rates and ATP concentrations associated with the decomposing leaf litter (see below). The dry mass remaining on each sampling date was calculated as the dry mass of the bulk material remaining plus five times the dry mass of the eight reference leaf discs. RESPIRATION RATES.—Respiration rates were assessed at stream temperature (22◦ C) using a flow-through system described by Wrona and Davies (1984) and Abelho and Graça (2001). Each set of eight leaf discs was placed in glass chambers (volume 8 mL) and supplied with a continuous and unidirectional flow (Manostat Sarah peristaltic pump, position 40) of 100 percent oxygenated and filtered (Sartorius cellulose nitrate 0.45 µm filters) stream water. Seven additional chambers without leaf discs (blanks) were used as controls. The mean flow in the chambers was 7.0 mL/h (range = 4.8–9.6 mL/h). After total replacement of the chambers’ volume (1–2 h), dissolved oxygen was measured by collecting the water flowing through the chambers (1 mL syringe) and injecting it into a 100-µL chamber adapted to an oxygen electrode (Strathkelvin Instruments, Glasgow, UK, model 781). Two to three replicate measurements were made on each chamber with a time interval of approximately 1 h. To assess respiration rates, the difference in oxygen concentration (mg O 2 /L) between the water column (blanks) and the samples was calculated and multiplied by the flow (L/h) within each chamber. Final values were calculated on the basis of AFDM of the eight reference leaf discs (mg O 2 /h/g AFDM). ATP CONCENTRATIONS.—After measuring the respiration rates, the same sets of eight leaf discs were homogenized (Omni Mixer Homogenizer, position 6, 60 sec) with 5 mL 1.2 N H 2 SO 4 containing 8 g/L oxalic acid, and 5 mL 0.05 M HEPES buffer (N-[2-Hydroxyethyl] piperazine-N -[2-ethanesulfonic acid]: C 8 H 17 N 2 O 4 SNa), centrifuged (refrigerated centrifuge, 10,000 rpm, 20 min), neutralized (NH 4 OH), and frozen at −20◦ C (Suberkropp et al. 1983). ATP was quantified with a luminometer, using the firefly bioluminescence method (Karl 1980). Absolute quantitative determinations of the amount of extracted ATP were made by measuring relative changes in peak height before and after the addition of internal standards (Holm-Hansen & Karl 1978). At least two readings were made on each sample. Final values were calculated on the basis of AFDM of the eight reference leaf discs (nmol ATP/g AFDM). The values presented have been corrected for extraction efficiency in each session. Extraction efficiency in each session was determined by adding a known amount of ATP (500 nmol) to an extra sample of eight noncolonized, air-dried leaf discs. Mean extraction efficiency was 65 percent (range = 22–73%). RELATIVE IMPORTANCE OF FUNGI AND BACTERIA.—After cutting the discs, each of the four sets of eight leaf discs was placed in a 100-mL flask containing filtered stream water (Sartorius cellulose nitrate 0.45 µm filters) and one of the following treatments: (1) antibacterial (50 mL/L penicillin-streptomycin solution; Sigma N0906), (2) antifungal (50 mL/L nystatin suspension; Sigma N1638), (3) antibacterial + antifungal (50 mL/L penicillin-streptomycin solution + 50 mL/L nystatin suspension), and (4) control (no antibiotics added). The flasks were incubated for 36 h in an orbital shaker (70 rpm) at stream temperature (22◦ C) and then the leaf discs were used to determine microbial respiration and ATP concentration associated with the leaves (see above). DATA ANALYSIS.—Leaf mass loss was expressed as a percentage of initial dry mass remaining. A negative exponential model was fitted by linear regression on logarithmically (ln) transformed data with the initial leaf mass (intercept) fixed at 100 percent, to determine breakdown rate k. Temperature-specific breakdown rate (k d ) was Decomposition of Hura crepitans Leaves in a Tropical Stream 399 calculated by using cumulative degree-days as the independent variable. The degree-days elapsed were determined by multiplying the temperature measured on a sampling date by the days elapsed since the previous reading. Respiration rates and ATP concentrations in the four treatments over the experimental period were tested for normality (those not normally distributed were log transformed) and compared using two-way ANOVA and Tukey’s HSD test (Zar 1996). Statistical analyses were conducted using the software STATISTICA 6.0. RESULTS BREAKDOWN RATE, MICROBIAL BIOMASS, AND ACTIVITY.—Leaves lost 19 percent of initial dry mass during the first 24 h in the stream (Fig. 1). Mass loss data fitted well to the breakdown model (F > 1141, df = 41, P < 0.0001). Breakdown rate of Hura crepitans leaves was rapid (k = −0.0672/d ± 0.0020 SE, k d = −0.0031/degreed ± 0.0001 SE); the bags lost 81 percent of their initial dry mass within 24 days. Because the litterbags were vandalized, no material was available for collection on day 31. The leaf material remaining on day 24 was composed of very small fragments, insufficient to determine ATP concentrations and respiration rates. At the beginning of the study, the leaves contained low amounts of ATP (5.8 ± 1.7 nmol ATP/g AFDM), but ATP content increased rapidly thereafter, with peak values of 725.1±117.5 nmol ATP/g AFDM at 9 days, when the remaining dry mass was 52 percent (Fig. 2). Respiration rates increased rapidly and continuously throughout the experiment (Fig. 2), attaining maximum values on day 16 (1.07 ± 0.09 mg O 2 /h/g AFDM). FIGURE 2. Changes in respiration rates and ATP concentrations associated with decomposing leaves of Hura crepitans in the tropical stream Camurı́ (mean ± 1 SE, N = 7). the treatment containing both antibacterial and antifungal agents (Fig. 3), although the values were generally significantly lower than in the other treatments (Table 1). ATP concentrations were higher in the antibacterial treatment than in antifungal treatment (Fig. 3), suggesting that the fungal community dominated microbial biomass associated with leaf litter. Respiration rates were higher in the antibacterial than in the antifungal treatment during the first 9 days of decomposition; after a maximum at day 5, respiration rates steadily decreased in the antibacterial treatment, whereas these rates increased in the antifungal treatment until the end of the experiment (Fig. 3). RELATIVE IMPORTANCE OF FUNGI AND BACTERIA.—Both microbial respiration plus measurable concentrations of ATP were found in DISCUSSION LEAF DECOMPOSITION, ATP CONCENTRATIONS, AND RESPIRATION leaves of Hura crepitans decomposed very rapidly in stream Camurı́ (k = −0.0672/d) showing one of the highest rates reported in the literature (e.g., Abelho 2001), although most of the studies allowed invertebrates to feed on the leaves (Padgett 1976, Verghese & Furtado 1987, Benstead 1996, Mathuriau & Chauvet 2002, Pamrong et al. 2002). Our results were consistent with other observations of fast breakdown in tropical streams (Irons et al. 1994, Rosemond et al. 1998). The high and stable water temperature (22◦ C), together with the hardwater characteristics of our stream, probably played a major role in controlling microbial activity associated with the leaves. When calculated as a temperature-specific processing rate, the breakdown rate (k d = −0.0031/degree-day) was still high (Cummins et al. 1989) and similar or higher than that reported for other leaf species in mid-latitude or even tropical streams (Irons et al. 1994, Mathuriau & Chauvet 2002). Microbial biomass and activity have rarely been assessed in leaves decomposing in tropical streams. In our study, the leaf litter was rapidly colonized by microorganisms, and attained higher ATP RATES.—The FIGURE 1. Dry mass remaining of Hura crepitans leaves decomposing in the tropical stream Camurı́ (mean ± 1 SE, N = 7). 400 Abelho, Cressa, and Graça TABLE 1. Results of multiple comparisons (Tukey test HSD) after two-way ANOVA (time vs. treatment). Time had a significant effect ( F > 20.405, df = 4, P < 0.0001), and there was a significant interaction between time and treatment in all tests ( F > 3.481, df = 12, P < 0.001). Treatments with the same letter are significantly different (P < 0.05). B = antibacterial treatment, F = antifungal treatment, BF = antibacterial and antifungal treatment, C = control. FIGURE 3. Changes in (a) respiration rates and (b) ATP concentrations associated with decomposing leaves of Hura crepitans treated with both (BF) and one of the antifungal or the antibacterial antibiotics (mean ± 1 SE, N = 7). concentrations (725 nmol/g AFDM) than in temperate streams, where ATP concentrations reached a maximum of 330–496 nmol/g AFDM in 15–115 days (Meyer & Johnson 1983, Suberkropp & Chauvet 1995). This result suggests that microbial processing is an important component of litter decomposition in this tropical stream. Fungal biomass has been reported to account for 88–100 percent of total microbial biomass associated with several leaf species decomposing in temperate streams (e.g., Baldy et al. 1995, Weyers & Suberkropp 1996, Baldy & Gessner 1997). To allow comparisons with other studies, we assumed that this was also the case in this tropical stream and converted ATP concentrations to microbial dry mass using the conversion value 1.75 mg (3.18 nmol) ATP/g fungal dry mass (Suberkropp et al. 1993). Fungal biomass estimated in this way accounted for a maximum of 23 percent 2-way ANOVA Tukey test Respiration rates (mg O 2 /L/g/AFDM) F = 17.858, df = 3, P < 0.0001 Ca > Fb > Bac > BFabc ATP concentrations (nmol ATP/g/AFDM) F = 10.857, df = 3, P < 0.0001 Ba > Cab > Fa > BFab of total detrital dry mass on day 9. The values were higher than those reported in the literature for temperate (5–18%; Gessner & Chauvet 1994, Suberkropp 1995, Paul & Meyer 1996) or even tropical streams (9.6%; Mathuriau & Chauvet 2002). Therefore, either fungal biomass was extremely high in the studied stream, or other microorganisms besides aquatic hyphomycetes were also important during decomposition. The maximum respiration rates associated with the decomposing leaves (1.07 mg O 2 /h/g AFDM) were in the range of those reported by Suberkropp (1991) for softwater (0.4 mg O 2 /h/g) and hardwater (1.3 mg O 2 /h/g) streams of North America. Since respiration is an indicator of carbon use by decomposers, we suggest that a difference between temperate and tropical streams is the velocity at which microbes colonize and decompose leaf material. The chemical characteristics of the leaves could have played a major role in controlling microbial colonization and the observed high breakdown rates. Leaching seems to be enhanced in tropical streams (Covich 1988). In our study the initial mass loss, generally attributed to leaching of soluble compounds, was high (19% in the first day) and in the range of values obtained in other studies (Mathuriau & Chauvet 2002). Leaching, together with the fast colonization by microorganisms, probably a result of a relatively high initial nutrient content and a low content of condensed tannins, could have interacted, resulting in the high mass loss observed in the experiment. According to Stout (1989), most of the tropical leaves with low condensed tannins have rapid (k = −0.0178/d ± 0.0045 SD) or very fast (k = −0.1182/d ± 0.0050 SD) breakdown rates. Our values are intermediate between these two, suggesting that Hura crepitans has a low condensed tannin content. Mathuriau and Chauvet (2002) obtained breakdown rates similar to ours using tropical leaf species with low tannin contents (1.13%). RELATIVE IMPORTANC OF FUNGI AND BACTERIA.—The temporal dynamics of ATP concentrations and respiration rates were similar until day 9. From that point on, ATP concentrations decreased while respiration rates continued to increase suggesting that a change had occurred in the microbial colonization of leaf litter. This change could be due to a replacement of the pioneer fungi, which are Decomposition of Hura crepitans Leaves in a Tropical Stream generally the first leaf-colonizers, by bacteria, which would account for lower biomass but higher activity (Baldy et al. 2002), as suggested by the continued increase in respiration rates. This pattern is also consistent with the results obtained with the antibiotics. The residual activity and biomass associated with leaves treated with both antifungal and antibacterial agents showed that antibiotics were not efficient enough to eliminate biotic activity. However, despite the residual activity, samples treated with the antifungal or antibacterial antibiotics differed, either in the amounts or in the temporal dynamics: antifungal agents were more effective in reducing microbial biomass and respiration until day 9, whereas antibacterial agents were more efficient from day 9 onward. These results suggest that fungi were the main microorganisms colonizing leaf litter in the early stages, and, as in temperate streams, they tend to be replaced by bacteria in later stages (Baldy & Gessner 1997). However, bacterial biomass associated with decomposing leaves may be relatively more abundant in tropical than in temperate streams. In conclusion, our results suggest that microbial-mediated leaf breakdown in our tropical stream was high in comparison with results from temperate streams. Microorganisms, as shown by the high ATP concentrations associated with the leaves, developed abundantly and rapidly, supporting previous findings regarding the dominance of microorganisms on leaf decomposition in tropical streams (Mathuriau & Chauvet 2002). The relative importance of bacteria and fungi during leaf decomposition seems to follow the patterns observed in temperate streams, with fungi dominating the early stages of decomposition and bacteria dominating when leaf litter is already fragmented and softened. ACKNOWLEDGMENTS This work was financed by the European Union (ISC-937084VE) and by Fundação para a Ciência e a Tecnologia (FCT) through a program grant (PBIC/C/BIA/2056/95) and through a scholarship to Manuela Abelho (PRAXIS XXI/BD/2952/94). We thank Centro de Neurociências (CNC) of Universidade de Coimbra (Portugal), through Dr. Martinho do Rosário, and Laboratório de Biologı́a Experimental of Universidad Central de Venezuela through Dr. Alexis Mendonza and Dr. Blas Dorta, for laboratory facilities. We especially acknowledge the precious help of Ângela Ribeiro in the work with the luminometer and Dr. Keller Suberkropp for valuable comments on an earlier version of the manuscript. LITERATURE CITED ABELHO, M. 2001. From litterfall to breakdown in streams: A review. The Scientific World 1: 656–580. ———, AND M. A. S. GRAÇA. 2001. Use of a flow-through system for assessing microbial respiration rates associated with decomposing leaves. Limnetica 19: 169–176. BALDY, V., AND M. O. GESSNER. 1997. Towards a budget of leaf litter decomposition in a first-order woodland stream. C.R. Académie des sciences Paris, Sciences de la vie/Life Sciences 320: 747–758. 401 ———, M. O. GESSNER, AND E. CHAUVET. 1995. Bacteria, fungi and the breakdown of leaf litter in a large river. Oikos 74: 93–102. ———, E. CHAUVET, J. Y. CHARCOSSET, AND M. O. GESSNER. 2002. Microbial dynamics associated with leaves decomposing in the mainstream and floodplain pond of a large river. Aquat. Microbial Ecol. 28: 25– 36. BÄRLOCHER, F. 1992. Community organization. In F. Bärlocher (Ed.). The ecology of aquatic hyphomycetes, pp. 38–76. Ecological Studies 94. Springer-Verlag, Berlin. BENSTEAD, J. P. 1996. Macroinvertebrates and the processing of leaf litter in a tropical stream. Biotropica 28: 367–375. BOLING, R. H. JR., E. D. GOODMAN, J. A. VAN SICKLE, J. O. ZIMMER, K. W. CUMMINS, R. C. PETERSEN, AND S. R. REICE. 1975. Toward a model of detritus processing in a woodland stream. Ecology 56: 141–151. COVICH, A. P. 1988. Geographical and historical comparisons of neotropical streams: Biotic diversity and detrital processing in highly variable habitats. J. N. Am. Benthol. Soc. 7: 361–386. ———, M. A. PALMER, AND T. A. CROWL. 1999. The role of benthic invertebrate species in freshwater ecosystems. BioScience 49: 119–127. CUMMNINS, K. W., M. A. WILZBACH, D. M. GATES, J. B. PERRY, AND W. B. TALIAFERRO. 1989. Shredders and riparian vegetation. BioScience 39: 24–30. FISHER, S. G., AND G. E. LIKENS. 1973. Energy flow in Bear Brook, New Hampshire: An alternative approach to stream metabolism. Ecol. Monog. 43: 421–439. GESSNER, M. O. 1997. Fungal biomass, production and sporulation associated with particulate organic matter in streams. In J. Pozo and A. Elosegi (Eds.). In Proceedings of the European Meeting on Litter Breakdown in Rivers and Streams, September 24–26, 1997, Bilbao, Spain, pp. 33–44. Limnetica 13: 1–102. ———, AND E. CHAUVET. 1994. Importance of stream microfungi in controlling breakdown rates of leaf litter. Ecology 75: 1807–1817. ———, ———, AND M. DOBSON. 1999. A perspective on leaf litter breakdown in streams. Oikos 85: 377–384. ———, K. SUBERKROPP, AND E. CHAUVET. 1997. Decomposition of plant litter by fungi in marine and freshwater ecosystems. In D. T. Wicklow and B. Söderström (Eds.). The Mycota, pp. 303–322, Volume 4. SpringerVerlag, Berlin. GRAÇA, M. A. S., C. CRESSA, M. O. GESSNER, M. J. FEIO, K. A. CALLIES, AND C. BARRIOS. 2001. Food quality, feeding preferences, survival and growth of shredders from temperate and tropical streams. Freshwater Biol. 46: 1–11. HIEBER, M., AND M. O. GESSNER. 2002. Contribution of stream detritivores, fungi, and bacteria to leaf breakdown based on biomass estimates. Ecology 83: 1026–1038. HOLM-HANSEN, O., AND D. M. KARL. 1978. Biomass and adenylate energy charge determination in microbial cell extracts and environmental samples. Meth. Enzymol. 57: 73–85. IRONS, J. C., M. W. OSWOOD, R. J. STOUT, AND C. M. PRINGLE.1994. Latitudinal patterns in leaf litter breakdown: Is temperature really important? Freshwater Biol. 32: 401–411. KARL, D. M. 1980. Cellular nucleotide measurements and applications in microbial ecology. Microbiol. Rev. 44: 739–796. MATHURIAU, C., AND E. CHAUVET. 2002. Breakdown of leaf litter in a neotropical stream. J. N. Am. Benthol. Soc. 21: 384–396. 402 Abelho, Cressa, and Graça MEYER, J. L., AND C. JOHNSON. 1983. The influence of elevated nitrate concentration on rate of leaf decomposition in a stream. Freshwater Biol. 13: ———. 1995. The influence of nutrients on fungal growth, productivity, and sporulation during leaf breakdown in streams. Can. J. Bot. 73: S1361– 177–183. PADGETT, D. E. 1976. Leaf decomposition by fungi in a tropical rainforest stream. Biotropica 8: 166–178. S1369. ———, AND E. CHAUVET. 1995. Regulation of leaf breakdown by fungi in streams: Influences of water chemistry. Ecology 76: 1433–1445. PAMRONG, S., K. BUAPETCH, AND M. BUATHONG. 2002. Leaf decomposition rates in three tropical streams of southern Thailand: The influence of land-use. Verh. Int. Verein. Limnol. 28: 475–479. ———, T. L. ARSUFFI, AND J. P. ANDERSON. 1983. Comparison of degradative ability, enzymatic activity, and palability of aquatic hyphomycetes grown on leaf litter. Appl. Environ. Microbiol. 46: 237–244. PAUL, M. J., AND J. L. MEYER. 1996. Fungal biomass of 3 leaf litter species during decay in an Appalachian stream. J. N. Am. Benthol. Soc. 15: 421–432. ROSEMOND, A. D., C. M. PRINGLE, AND A. RAMIREZ. 1998. Macroconsumer ———, M. O. GESSNER, AND E. CHAUVET. 1993. Comparison of ATP and ergosterol as indicators of fungal biomass associated with decomposing leaves in streams. Appl. Environ. Microbiol. 59: 3367–3372. effects on insect detritı́voros and detritus processing in a tropical stream. Freshwater Biol. 39: 515–523. ROWE, J. M., S. K. MEEGAN, E. S. ENGSTROM, S. A. PERRY, AND W. B. PERRY. VERGHESE, S., AND J. I. FURTADO. 1987. Decomposition of leaf litter in a tropical freshwater swamp, the Tasek Bera, Malaysia. Arch. Hydrobiol. Beih. Ergebn. Limnol. 28: 425–434. 1996. Comparison of leaf processing rates under different temperature regimes in three headwater streams. Freshwater Biol. 36: 277–288. WEBSTER, J. R., AND E. F. BENFIELD. 1986. Vascular plant breakdown in freshwater ecosystems. Ann. Rev. Ecol. Syst. 17: 567–594. STOUT, J. R. 1989. Effects on condensed tannins on leaf processing in midlatitude and tropical streams: A theoretical approach. Can. J. Fish. Aquat. Sci. 46: 1097–1106. WEYERS, H., AND K. SUBERKROPPP. 1996. Fungal and bacterial production during the breakdown of yellow poplar leaves in 2 streams. J. N. Am. Benthol. Soc. 15: 408–420. SUBERKROPP, K. 1991. Relationships between growth and sporulation of aquatic hyphomycetes on decomposing leaf litter. Mycol. Res. 9: 843–850. ———.1992. Aquatic hyphomycete communities. In G. C. Carroll and D. T. WRONA, F. J., AND R. W. DAVIES. 1984. An improved flow-through respirometer for aquatic macroinvertebrates bioenergetic research. Can. J. Fish. Aquat. Sci. 41: 380–385. Wicklow (Eds.). The fungal community: Its organization and role in the ecosystem, pp. 729–748, 2nd edition. Marcel Dekker, New York. ZAR, J. H. 1996. Biostatistical analysis, 3rd edition. Prentice-Hall, Upper Saddle River, New Jersey.
© Copyright 2026 Paperzz