Components of the carbon cycle in the Russian Arctic seas: Primary production and flux of Corg from the photic layer.

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dc.contributor.author Vinogradov, Mikhail E
dc.contributor.author Vedernikov, Vladimir I
dc.contributor.author Romankevich, Evgeny A
dc.contributor.author Vetrov, Alexander A
dc.coverage.spatial MEDIAN LATITUDE: 76.702902 * MEDIAN LONGITUDE: 42.656078 * SOUTH-BOUND LATITUDE: 70.568333 * WEST-BOUND LONGITUDE: 5.666667 * NORTH-BOUND LATITUDE: 81.666667 * EAST-BOUND LONGITUDE: 83.448333 * DATE/TIME START: 1987-05-21T00:00:00 * DATE/TIME END: 1994-09-30T00:00:00 * MINIMUM DEPTH, water: 9 m * MAXIMUM DEPTH, water: 1950 m
dc.date.accessioned 2019-11-24T08:50:25Z
dc.date.available 2019-11-24T08:50:25Z
dc.date.issued 2000-08-10
dc.identifier https://doi.pangaea.de/10.1594/PANGAEA.763799
dc.identifier https://doi.org/10.1594/PANGAEA.763799
dc.identifier.citation Vinogradov, Mikhail E; Vedernikov, Vladimir I; Romankevich, Evgeny A; Vetrov, Alexander A (2000): Components of the carbon cycle in the Russian Arctic seas: Primary production and flux of Corg from the photic layer. Translated from Okeanologiya, 2000, 40(2), 221-233, Oceanology, 40(2), 204-215
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/7765
dc.description.abstract On the basis of analysis of satellite and field data collected in Russian Arctic Seas maps of distribution of primary production for different months of the vegetation period were compiled. These maps were used to estimate annual primary production of organic carbon: 55 million tons in the Barents Sea; about 20 million tons in the Kara Sea; 10-15 million tons in the Laptev Sea and in the East Siberian Sea, 42 million tons in the Chukchi Sea. In the central and eastern parts of the Barents Sea during the vegetation period values of primary production decreased by factor >5 (from >500 to <100 mg C/m**2/day). By reviewing results of studies with sediment traps vertical fluxes of organic carbon in different regions of the Arctic Basin were estimated. Significant temporal variability of Corg fluxes with maxima during phytoplankton blooms (by 830 mg C/m**2/day) was noted. Typical summer fluxes of Corg are 10-40 mg C/m**2/day in the southern Barents Sea, 1-10 mg C/m**2/day in the northern Barents Sea and in the Kara Sea, and up to 370 mg C/m**2/day in the zone of marginal filters of the Ob and Yenisey rivers.
dc.format text/tab-separated-values, 237 data points
dc.language.iso en
dc.publisher PANGAEA
dc.rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rights Access constraints: unrestricted
dc.source Supplement to: Vinogradov, Mikhail E; Vedernikov, Vladimir I; Romankevich, Evgeny A; Vetrov, Alexander A (2000): Components of the carbon cycle in the Russian Arctic seas: Primary production and flux of Corg from the photic layer. Translated from Okeanologiya, 2000, 40(2), 221-233, Oceanology, 40(2), 204-215
dc.subject Archive of Ocean Data
dc.subject ARCOD
dc.subject Arctic Ocean, Central Basin
dc.subject Barents Sea
dc.subject Carbon, organic flux
dc.subject Date
dc.subject Date/time end
dc.subject Date/Time of event
dc.subject Date/Time of event 2
dc.subject Date/time start
dc.subject DEPTH, water
dc.subject Greenland Sea
dc.subject Total mass flux per day
dc.subject trap sample
dc.subject VVRV-00-01
dc.subject VVRV-00-02
dc.subject VVRV-00-03
dc.subject VVRV-00-04
dc.subject VVRV-00-05
dc.subject VVRV-00-06
dc.subject VVRV-00-07
dc.subject VVRV-00-08
dc.subject VVRV-00-09
dc.subject VVRV-00-10
dc.subject VVRV-00-11
dc.subject VVRV-00-12
dc.subject VVRV-00-13
dc.subject VVRV-00-14
dc.subject VVRV-00-15
dc.subject VVRV-00-16
dc.subject VVRV-00-17
dc.subject VVRV-00-18
dc.subject VVRV-00-19
dc.subject VVRV-00-20
dc.subject VVRV-00-21
dc.subject VVRV-00-22
dc.subject VVRV-00-23
dc.subject VVRV-00-24
dc.subject VVRV-00-25
dc.subject VVRV-00-26
dc.subject VVRV-00-27
dc.subject VVRV-00-28
dc.subject Weighing dry trap material
dc.title Components of the carbon cycle in the Russian Arctic seas: Primary production and flux of Corg from the photic layer.
dc.title.alternative (Table 2) Vertical fluxes of organic carbon and sediment matter from the photic zone in the Arctic Basin
dc.type Dataset


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