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Interannual variability of algal populations and their influence on lake metabolism
Author(s) -
HEANEY S.I.,
PARKER J.E.,
BUTTERWICK C.,
CLARKE K.J.
Publication year - 1996
Publication title -
freshwater biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.297
H-Index - 156
eISSN - 1365-2427
pISSN - 0046-5070
DOI - 10.1111/j.1365-2427.1996.tb01769.x
Subject(s) - hypolimnion , epilimnion , structural basin , phytoplankton , hydrobiology , environmental science , drainage basin , hydrology (agriculture) , range (aeronautics) , ecology , plankton , eutrophication , oceanography , geology , nutrient , biology , geography , geomorphology , materials science , cartography , geotechnical engineering , aquatic environment , composite material
SUMMARY1 An input‐output phosphorus budget is given for Windermere and its two basins based on data available for the late 1980s. The annual areal total phosphorus loading for the whole lake was 1.04 g P m ‐2 yr ‐1 and for the North and South Basins were 1.08 and 1.70 g P m ‐2 yr ‐1 , respectively. For the whole lake and its South Basin the values were similar to the upper range of critical loads calculated according to the equation of Vollenweider (1976) for the transition between oligotrophy and eutrophy while that for the North Basin (1.08 g P m ‐2 yr ‐1 ) was within this range of critical loadings but towards its lower end. 2 Changes in the quality of summer phytoplankton are described for Windermere, particularly its South Basin, between 1978 and 1989 in relation to the utilization of nitrate‐nitrogen (NO 3 ‐N) in the epilimnion, deoxygenarion of the hypolimnion and the ratio of epilimnetic volume to hypolimnetic volume, E v / H v The two basins of Windermere with values of E v / H v of 0.79 (South Basin) and 0.50 (North Basin) have contrasting conditions of summer deoxygenarion. The shallower South Basin shows marked interannual variability in the development of hypolimnetic anoxia. Years with large hypolimnetic anoxia during autumn are correlated with the production during summer of large populations of the poorly grazed blue‐green alga Oscillatoria bourrellyi and exhaustion of NO 3 ‐N in the upper layers. During years when anoxia does not develop the summer phytoplankton consists of small easily grazed algae or larger ones subject to parasitic epidemics. The deeper North Basin never becomes anoxic even though it can contain similar sized populations of O. bourrellyi to the South Basin. 3 A possible explanation of the between basin and, for the South Basin, between year variation of utilization of NO 3 ‐N and level of hypolimnetic deoxygenarion is that algal quality can determine lake metabolism dependent upon lake or basin morphology. Poorly grazed large forms such as O. bourrellyi act as sinks for NO 3 ‐N. On sedimentation such populations act as a ‘short circuit’ mechanism descending into deeper layers in sufficient quantities to cause anoxia. Other species subject to crustacean or microbial grazing are mineralized in the epilimnion with little sedimentation to the deeper waters. Subsequent recycling of nitrogen as NH 4 ‐N takes place in the upper layers or thermocline which is more readily taken up by subsequent production. The influence of such ‘short circuit’ mechanisms is reduced in deep lakes and exacerbated in shallow ones. 4 The success of species such as O. bourrellyi is dependent upon a sufficient inoculum, an adequate supply of nutrients and the depth of intermittent mixing. The importance of these factors in regulating presence and timing of summer populations is illustrated and discussed.