Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ...

A study was performed from August 11 to September 3, 1998 in the Pechora Sea, which covered the shallow-water southeastern Barents Sea. Chlorophyll a concentration in the surface layer (C_chls) ranged from 0.08 to 1.15 mg/m**3, while primary production in the water column (C_phs) Varied from 17 to 1...

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Main Authors: Vedernikov, Vladimir I, Gagarin, Vladimir I, Burenkov, Vladimir I
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.761440
https://doi.pangaea.de/10.1594/PANGAEA.761440
id ftdatacite:10.1594/pangaea.761440
record_format openpolar
spelling ftdatacite:10.1594/pangaea.761440 2024-09-15T17:57:52+00:00 Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ... Vedernikov, Vladimir I Gagarin, Vladimir I Burenkov, Vladimir I 2001 application/zip https://dx.doi.org/10.1594/pangaea.761440 https://doi.pangaea.de/10.1594/PANGAEA.761440 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Water sample ASV13 Akademik Sergey Vavilov Archive of Ocean Data ARCOD article Collection Supplementary Publication Series of Datasets 2001 ftdatacite https://doi.org/10.1594/pangaea.761440 2024-08-01T10:54:23Z A study was performed from August 11 to September 3, 1998 in the Pechora Sea, which covered the shallow-water southeastern Barents Sea. Chlorophyll a concentration in the surface layer (C_chls) ranged from 0.08 to 1.15 mg/m**3, while primary production in the water column (C_phs) Varied from 17 to 170 mg C/m**2/day, aver. 75 mg C/m**2/day. Transition from central deep-water (60-190 m) parts of the sea to coastal shallow-water (15-30 m) parts was accompanied by increase of average C_chls values 2.4 times (from 0.21 to 0.51 mg/m**3) and decrease in average C_phs 1.6 times (from 95 to 58 mg C/m**2/day); the latter, in turn, resulted from decrease in thickness of the photosynthetic layer (H_ph) from 55 to 12 m and its relative transparency (H) from 17 to 4 m. This sharp change in H value and absence of a positive feedback between C_chls and C_phs were most probably related to rapid increase in the role of yellow substance and suspended matter in absorption of solar radiation in coastal waters. In sea areas with ... : Supplement to: Vedernikov, Vladimir I; Gagarin, Vladimir I; Burenkov, Vladimir I (2001): Features of distribution of primary production and chlorophyll in the Pechora Sea in August-September 1998. Translated from Okeanologiya, 2001, 41(1), 69-79, Oceanology, 41(1), 64-74 ... Article in Journal/Newspaper Barents Sea Pechora Pechora Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Water sample
ASV13
Akademik Sergey Vavilov
Archive of Ocean Data ARCOD
spellingShingle Water sample
ASV13
Akademik Sergey Vavilov
Archive of Ocean Data ARCOD
Vedernikov, Vladimir I
Gagarin, Vladimir I
Burenkov, Vladimir I
Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ...
topic_facet Water sample
ASV13
Akademik Sergey Vavilov
Archive of Ocean Data ARCOD
description A study was performed from August 11 to September 3, 1998 in the Pechora Sea, which covered the shallow-water southeastern Barents Sea. Chlorophyll a concentration in the surface layer (C_chls) ranged from 0.08 to 1.15 mg/m**3, while primary production in the water column (C_phs) Varied from 17 to 170 mg C/m**2/day, aver. 75 mg C/m**2/day. Transition from central deep-water (60-190 m) parts of the sea to coastal shallow-water (15-30 m) parts was accompanied by increase of average C_chls values 2.4 times (from 0.21 to 0.51 mg/m**3) and decrease in average C_phs 1.6 times (from 95 to 58 mg C/m**2/day); the latter, in turn, resulted from decrease in thickness of the photosynthetic layer (H_ph) from 55 to 12 m and its relative transparency (H) from 17 to 4 m. This sharp change in H value and absence of a positive feedback between C_chls and C_phs were most probably related to rapid increase in the role of yellow substance and suspended matter in absorption of solar radiation in coastal waters. In sea areas with ... : Supplement to: Vedernikov, Vladimir I; Gagarin, Vladimir I; Burenkov, Vladimir I (2001): Features of distribution of primary production and chlorophyll in the Pechora Sea in August-September 1998. Translated from Okeanologiya, 2001, 41(1), 69-79, Oceanology, 41(1), 64-74 ...
format Article in Journal/Newspaper
author Vedernikov, Vladimir I
Gagarin, Vladimir I
Burenkov, Vladimir I
author_facet Vedernikov, Vladimir I
Gagarin, Vladimir I
Burenkov, Vladimir I
author_sort Vedernikov, Vladimir I
title Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ...
title_short Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ...
title_full Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ...
title_fullStr Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ...
title_full_unstemmed Primary production of phytoplankton and chlorophyll a in the southeast Barents Sea in August-September 1998 ...
title_sort primary production of phytoplankton and chlorophyll a in the southeast barents sea in august-september 1998 ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.761440
https://doi.pangaea.de/10.1594/PANGAEA.761440
genre Barents Sea
Pechora
Pechora Sea
genre_facet Barents Sea
Pechora
Pechora Sea
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.761440
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