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Persistence of net heterotrophy in lakes during nutrient addition and food web manipulations
Author(s) -
Cole Jonathan J.,
Pace Michael L.,
Carpenter Stephen R.,
Kitchell James F.
Publication year - 2000
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.2000.45.8.1718
Subject(s) - food web , primary production , nutrient , zooplankton , heterotroph , environmental science , planktivore , ecosystem , organic matter , diel vertical migration , ecosystem respiration , zoology , ecology , biology , phytoplankton , genetics , bacteria
Net ecosystem production (NEP) is the difference between gross primary production (GPP) and community respiration (R). We estimated in situ NEP using three independent approaches (net CO 2 gas flux, net O 2 gas flux, and continuous diel O 2 measurements) over a 4–7 yr period in a series of small lakes in which food webs were manipulated and nutrient loadings were experimentally varied. In the absence of manipulation, these lakes were net heterotrophic according to all three approaches. NEP (NEP = GPP‐R) was consistently negative and averaged −35.5 ± 3.7 (standard error) mmol C m −2 d −1 . Nutrient enrichment, in the absence of strong planktivory, tended to cause increases in estimates of both GPP and R (estimated from the continuous O 2 data) but resulted in little change in the GPP/R ratio, which remained <1, or NEP, which remained negative. When planktivorous fish dominated the food web, large zooplankton were rare and nutrient enrichment produced positive values of NEP by all three methods. Among lakes and years, daily values of NEP ranged from −241 to +175 mmol m −2 d −1 ; mean seasonal NEP was positive only under a combination of high nutrient loading and a planktivore‐dominated food web. Community R is significantly subsidized by allochthonous sources of organic matter in these lakes. Combining all lakes and years, we estimate that ~26 mmol C m −2 d −1 of allochthonous origin is respired on average. This respiration of allochthonous organic matter represents 13 to 43% of total R, and this fraction declines with increasing GPP.