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The interactive effects of calcium concentration and temperature on the survival and reproduction of Daphnia pulex at high and low food concentrations
Author(s) -
Ashforth Dawn,
Yan Norman D.
Publication year - 2008
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.2008.53.2.0420
Subject(s) - daphnia pulex , daphnia , zoology , reproduction , biology , calcium , cladocera , acclimatization , botany , ecology , chemistry , crustacean , organic chemistry
We reared Daphnia pulex in a fully defined medium at seven calcium (Ca) concentrations (0.1, 0.5, 1, 1.5, 2, 5, and 10 mg Ca L −1 ), two mixed algal densities (high food: 30 mg chlorophyll a L −1 and low food: 3 mg Chl a L −1 ), and four temperatures (20ºC, 24ºC, 28ºC, and 32ºC) in a fully factorial design. The minimum Ca concentration required for the survival and reproduction of D. pulex was between 0.1 and 0.5 mg Ca L −1 . Daphniids reared at 0.1 mg Ca L −1 lived no longer than 10 d and did not reproduce. Although offspring were produced at 0.5 mg Ca L −1 and above, reproduction was reduced below 1.5 mg Ca L −1 due to delays in maturity and reductions in both the brood size and number of broods produced within the 15 d of the experiment. As a result, the intrinsic rate of natural increase, r, decreased dramatically between 1.5 and 1 mg Ca L −1 , and was undefined at 0.1 mg Ca L −1 . Higher temperatures and reduced algal biomass enhanced the susceptibility of D. pulex to low Ca concentrations by raising the reproductive threshold to 1.5 mg Ca L −1 . Thermal stress at 32ºC was so great that daphniids lived no longer than 5 d and did not reproduce. Hence, r was undefined at 32ºC. In order to sustain D. pulex populations and potentially other Ca‐sensitive daphniids, fresh waters must maintain a Ca concentration of at least 0.5 mg Ca L −1 , although concentrations as high as 1.5 mg Ca L −1 may be required for daphniids to withstand the concurrent reductions in algal biomass and rising water temperatures that are now commonplace on the south‐central Canadian Shield.