Peculiarities of the primary production process in the Kara Sea at the end of the vegetation season
- Авторы: Mosharov S.A.1,2, Demidov A.B.1, Simakova U.V.1
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Учреждения:
- Shirshov Institute of Oceanology
- Bauman Moscow State Technical University
- Выпуск: Том 56, № 1 (2016)
- Страницы: 84-94
- Раздел: Marine Biology
- URL: https://bakhtiniada.ru/0001-4370/article/view/149090
- DOI: https://doi.org/10.1134/S0001437016010100
- ID: 149090
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Аннотация
Research was implemented from September 15 through October 4, 2011 in the Kara Sea along transects located southeastwards Novaya Zemlya, in the St. Anna Trough, the Yenisei River estuary, and the adjacent shelf. The concentration of chlorophyll a was the highest in the photic zone (0.05–2.30 mg/m3, on average, 0.80 ± 0.37 mg/m3). The maximal concentration of Chl a at most of the stations located in the water layer of 7–30 m. Integral primary production in the water column varied from 3.0 to 151.0 mg C/m2 per day, on average, 37.2 ± 36.6 mg C/m2 per day. The maximal rate of primary production at most of the stations has been observed for the surface layer of the water column. Within the upper mixed water layer, relative primary production was from 31 to 100% (on average, 77 ± 20%). The most productive zone was the waters along Yenisei transect. In the estuary and at the adjacent shelf, primary production was 50 mg C/m2 per day, exceeding the range observed for other areas by 1.5–2.0 times. The concentrations of silica and nitrogen together with light regime and water temperature were the major limiting factors affecting the primary production rate in the Kara Sea in autumn.
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Об авторах
S. Mosharov
Shirshov Institute of Oceanology; Bauman Moscow State Technical University
Автор, ответственный за переписку.
Email: mosharov@ocean.ru
Россия, Moscow; Moscow
A. Demidov
Shirshov Institute of Oceanology
Email: mosharov@ocean.ru
Россия, Moscow
U. Simakova
Shirshov Institute of Oceanology
Email: mosharov@ocean.ru
Россия, Moscow
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