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Ecosystem‐specific patterns in the relationship between zooplankton and POM or microplankton del 13 C
Author(s) -
del Giorgio Paul A.,
France Robert L.
Publication year - 1996
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.1996.41.2.0359
Subject(s) - zooplankton , plankton , phytoplankton , pelagic zone , estuary , oceanography , environmental science , bacterioplankton , ecology , ecosystem , organic matter , dissolved organic carbon , biology , nutrient , geology
Measurements of plankton δ 13 C from 28 temperate lakes show that zooplankton are depleted in 13 C relative to smaller planktonic size fractions. A broad literature survey indicates that this is a general pattern in lakes but not in marine and estuarine plankton communities, where zooplankton are generally enriched in 13 C relative to particulate organic matter (POM) or microplankton. Marine plankton thus conform to the assumptions that pelagic food webs are essentially driven by phytoplankton and that POM or small planktonic size classes largely reflect algal carbon, which is transferred to zooplankton with a slight enrichment in 13 C. The plankton of lakes and possibly of estuaries, however, do not conform to this expectation. We show that there is a continuum in the δ 13 C differences between POM and zooplankton from open ocean to coastal areas and estuaries and that a similar pattern occurs from unproductive to highly productive lakes. These differences probably reflect both the degree in POM dilution by nonalgal sources of organic carbon and depthrelated changes in the isotopic signature of phytoplankton in lakes and suggest systematic differences in organic carbon flow pathways among aquatic ecosystems.