Journal
JOURNAL OF THE NORTH AMERICAN BENTHOLOGICAL SOCIETY
Volume 20, Issue 2, Pages 241-254Publisher
NORTH AMER BENTHOLOGICAL SOC
DOI: 10.2307/1468319
Keywords
food webs; tropical floodplains; primary and secondary production; trophic dynamics; fish production; energy flow
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Stable isotope data and indirect methods for estimating consumer production were used in a foodweb analysis for the Orinoco River floodplain, Venezuela. The ratio of annual production to mean annual biomass (P-a/(B) over bar) was estimated from mass at maturity for all major categories of consumers. Field data on (B) over bar then were used to estimate P-a, for each major category. Carbon sources for all categories of consumers were identified through delta C-13 analysis, and trophic shifts in delta N-15 were used in assigning trophic levels to consumers. The ultimate Carbon source for both invertebrates and fish was algae (phytoplankton and periphyton), even though macrophytes and Litterfall from the floodplain forest composed 98% of potentially available C. Production of invertebrate consumers (benthos, rhizofauna, and zooplankton), which occurred almost entirely through l(st)-level consumption, was estimated as 14 g C m(-)2 y(-1). Fish, which produced 11 g C m-2 y-(1), showed a mean delta N-15 trophic shift of 1.8 units above the algal C source, suggesting that similar to 20% of fish production was directly accountable to consumption of algal C (l(st)-level consumption), and that most of the remainder was attributable to l(st)-level carnivory. Data on production and trophic shifts implied trophic efficiency of 5% for invertebrates and 20% for fish. Although the food web is focused on a very small fraction of potentially available primary C (algae), this C source can account quantitatively for the observed production of both invertebrates and fish. The food web showed marked trophic compression (large consumers supported by trophic levels 1 and 2), which is the only means by which high production of large consumers can be sustained on a small fraction of the potentially available C.
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