Тип публикации: статья из журнала
Год издания: 2018
Идентификатор DOI: 10.1134/S1028334X18040207
Аннотация: The process of gas exchange of CO2 in the atmosphere-water system and its relation to the daily course of variable fluorescence of phytoplankton is studied on the basis of long-term (2004-2014) measurements during the open water period for Lake Baikal. It is found that the decrease in photosynthetic activity of plankton is almost synchronous to the increase in the CO2 flux from atmosphere to water. It follows from comparison of the spring and summer data with December measurements that the daily decrease in variable fluorescence of phytoplankton is caused by the internal daily rhythm of the photosynthetic activity of plankton.
Издание
Журнал: DOKLADY EARTH SCIENCES
Выпуск журнала: Vol. 479, Is. 2
Номера страниц: 507-510
ISSN журнала: 1028334X
Место издания: NEW YORK
Издатель: MAIK NAUKA/INTERPERIODICA/SPRINGER
Персоны
- Zavoruev V.V. (Siberian Fed Univ, Krasnoyarsk 660041, Russia; Russian Acad Sci, Siberian Branch, Inst Computat Modeling, Krasnoyarsk 660036, Russia)
- Domysheva V.M. (Russian Acad Sci, Siberian Branch, Limnol Inst, Irkutsk 664033, Russia)
- Pestunov D.A. (Russian Acad Sci, Siberian Branch, Zuev Inst Atmospher Opt, Tomsk 634055, Russia)
- Sakirko M.V. (Russian Acad Sci, Siberian Branch, Limnol Inst, Irkutsk 664033, Russia)
- Panchenko M.V. (Russian Acad Sci, Siberian Branch, Zuev Inst Atmospher Opt, Tomsk 634055, Russia)
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