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Light as a Controlling Factor of Winter Phytoplankton in a Monomictic Reservoir

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F22%3A00559100" target="_blank" >RIV/60077344:_____/22:00559100 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985807:_____/22:00559100 RIV/60076658:12310/22:43904795 RIV/00216208:11310/22:10453756 RIV/67985912:_____/22:00559100 RIV/62156489:43210/22:43921554

  • Result on the web

    <a href="https://dx.doi.org/10.1016/j.limno.2022.125995" target="_blank" >https://dx.doi.org/10.1016/j.limno.2022.125995</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.limno.2022.125995" target="_blank" >10.1016/j.limno.2022.125995</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Light as a Controlling Factor of Winter Phytoplankton in a Monomictic Reservoir

  • Original language description

    Factors affecting the seasonal succession of plankton communities in freshwater temperate lakes have been thoroughly studied for decades. However, there are still relatively few data describing the winter season patterns in detail, as the focus has been mostly on spring to autumn conditions. Ice cover is often the crucial factor limiting light availability for winter phytoplankton, but in warm monomictic lakes is usually lacking and the gradually increasing solar radiation should, theoretically, drive phytoplankton growth. In this study conducted in 2002–2010, we documented regular sharp increases in phytoplankton chlorophyll a, starting just after the winter solstice and lasting throughout the total circulation and/or unstable inverse stratification period in the monomictic Slapy reservoir (Czechia). Chlorophyll a concentrations analysed in one-week intervals reached their yearly minimum of 0.2–0.8 µg L−1 in the solstice period, and the spring peak occurred before the onset of stable thermal stratification. The regular pattern was slightly disrupted in some years, associated with short periods of ice cover. Winter phytoplankton were species poor and dominated by diatoms, cryptophytes, green algae, and cyanobacteria. Using semiparametric regression approach, we aimed to test if selected environmental parameters had a significant effect on the observed winter trend. The resulting model revealed that solar radiation and water temperature positively influenced log chlorophyll a concentrations, whereas water age had a significant negative effect. On the other hand, zooplankton density and ice cover effects were not significant. The shapes of the marginal effects of water temperature and solar radiation were nonlinear, and the interaction of these two major factors was significant. The model-based estimated chlorophyll a concentrations showed a shift from radiation dominance to temperature-positive effects along the temperature gradient. This might represent as yet neglected pattern of phytoplankton seasonal development in warm monomictic lakes worldwide.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10617 - Marine biology, freshwater biology, limnology

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2022

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Limnologica

  • ISSN

    0075-9511

  • e-ISSN

    1873-5851

  • Volume of the periodical

    95

  • Issue of the periodical within the volume

    July 2022

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    11

  • Pages from-to

    125995

  • UT code for WoS article

    000823266600002

  • EID of the result in the Scopus database

    2-s2.0-85133782613