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Winter Anomalies of Seston, Phytoplankton and Cations in a Colorado (U.S.A.) Alpine Flowage Lake
Author(s) -
Heermann Scott J.
Publication year - 1978
Publication title -
internationale revue der gesamten hydrobiologie und hydrographie
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.524
H-Index - 52
eISSN - 1522-2632
pISSN - 0020-9309
DOI - 10.1002/iroh.19780630609
Subject(s) - seston , phytoplankton , environmental science , environmental chemistry , chemistry , zoology , nutrient , ecology , biology
Year‐round changes of phytoplankton, organic and inorganic seston, and dissolved and suspended concentrations of Ca, Mg, Na, K, Fe, Mn, Zn, and Cu were studied and correlated in Long Lake, an ultra‐oligotrophic alpine flowage lake of northcentral Colorado, U.S.A. Dissolved cation levels for Ca, Mg, Na, K, Mn, and Fe, both sestonic fractions and phytoplankton densities reached and sustained a maximum during April and May under heavy cover of ice and snow, and a minimum during open‐season from mid‐June to mid‐October. Rates of monthly water renewal varied greatly with a low of 0.28 turnovers in April and a high of 15.37 turnovers in June. Massive flushing in June and July reduced dissolved Fe levels to <0.060 mg/l from a typical maxima >8.0 mg/l in April and May. Tests for linear correlation between the various cations, sestonic fractions and phytoplankton showed in most cases positive and significant ( p <.05) relationships. For most dissolved Fe and Mn pairings with phytoplankton and seston exceptionally significant ( p < 0.001) relationships were observed.