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ALLOCHTHONOUS ORGANIC CARBON AND PHYTOPLANKTON/BACTERIOPLANKTON PRODUCTION RELATIONSHIPS IN LAKES
Author(s) -
Jansson Mats,
Bergström Ann-Kristin,
Blomqvist Peter,
Drakare Stina
Publication year - 2000
Publication title -
ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.144
H-Index - 294
eISSN - 1939-9170
pISSN - 0012-9658
DOI - 10.1890/0012-9658(2000)081[3250:aocapb]2.0.co;2
Subject(s) - bacterioplankton , phytoplankton , pelagic zone , dissolved organic carbon , environmental science , food chain , productivity , total organic carbon , carbon cycle , microbial loop , ecology , carbon fibers , heterotroph , nutrient , food web , primary producers , plankton , primary productivity , ecosystem , biology , bacteria , materials science , genetics , macroeconomics , composite number , economics , composite material
Humic lakes with high inputs of allochthonous dissolved organic carbon have a pelagic food chain that, to a large extent, is based on bacterioplankton energy mobilization from allochthonous organic carbon compounds. This is in contrast to clear lakes in which total pelagic production is based mainly on phytoplankton photosynthesis. The energy economy in humic lakes may be less efficient than in clear lakes, because it is likely that one more link is included in the food chain. Lake data from Scandinavia and North America demonstrate that shifts between food chains based on heterotrophic production and food chains based on primary production can take place at moderate increases or decreases in the concentration of dissolved organic carbon from allochthonous sources. Large variations in the loading of allochthonous organic carbon (e.g., due to climatic variations) may have considerable effects on the biostructure and productivity of lakes.