Composition of organic matter in waters of the Barents Sea
Concentration of dissolved and suspended organic carbon in the Barents Sea decreases with increasing depth and in meridional direction from south to north. This fact is attributed to uneven supply of organic matter (OM) from different sources. Large amounts of OM are present in the water column of t...
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1982
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.755600 2023-05-15T15:38:02+02:00 Composition of organic matter in waters of the Barents Sea Belyaeva, Alexandra N Romankevich, Evgeny A MEDIAN LATITUDE: 73.298486 * MEDIAN LONGITUDE: 39.725722 * SOUTH-BOUND LATITUDE: 69.940000 * WEST-BOUND LONGITUDE: 32.520000 * NORTH-BOUND LATITUDE: 80.100000 * EAST-BOUND LONGITUDE: 55.000000 1982-01-12 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.755600 https://doi.org/10.1594/PANGAEA.755600 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.755600 https://doi.org/10.1594/PANGAEA.755600 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Belyaeva, Alexandra N; Romankevich, Evgeny A (1982): Organic matter in a water column of the Barents Sea. Oceanology, 22(2), 188-195 AK23-2010 AK23-2014 AK23-2028 AK23-2041 AK23-2042 AK23-2063 Akademik Kurchatov AKU23 Archive of Ocean Data ARCOD Barents Sea MULT Multiple investigations Dataset 1982 ftpangaea https://doi.org/10.1594/PANGAEA.755600 2023-01-20T07:32:01Z Concentration of dissolved and suspended organic carbon in the Barents Sea decreases with increasing depth and in meridional direction from south to north. This fact is attributed to uneven supply of organic matter (OM) from different sources. Large amounts of OM are present in the water column of the Barents Sea, which is a result of high productivity of this water mass and slow decomposition of OM at low temperatures and lowered activity of microflora. Larger amount of OM reaches bottom sediments of the Barents Sea more than in seas, which have similar depth and productivity, but are located at low latitudes. Characteristic features of distribution of lipids and suspended matter in sea water are examined. Dataset Barents Sea PANGAEA - Data Publisher for Earth & Environmental Science Barents Sea ENVELOPE(32.520000,55.000000,80.100000,69.940000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AK23-2010 AK23-2014 AK23-2028 AK23-2041 AK23-2042 AK23-2063 Akademik Kurchatov AKU23 Archive of Ocean Data ARCOD Barents Sea MULT Multiple investigations |
spellingShingle |
AK23-2010 AK23-2014 AK23-2028 AK23-2041 AK23-2042 AK23-2063 Akademik Kurchatov AKU23 Archive of Ocean Data ARCOD Barents Sea MULT Multiple investigations Belyaeva, Alexandra N Romankevich, Evgeny A Composition of organic matter in waters of the Barents Sea |
topic_facet |
AK23-2010 AK23-2014 AK23-2028 AK23-2041 AK23-2042 AK23-2063 Akademik Kurchatov AKU23 Archive of Ocean Data ARCOD Barents Sea MULT Multiple investigations |
description |
Concentration of dissolved and suspended organic carbon in the Barents Sea decreases with increasing depth and in meridional direction from south to north. This fact is attributed to uneven supply of organic matter (OM) from different sources. Large amounts of OM are present in the water column of the Barents Sea, which is a result of high productivity of this water mass and slow decomposition of OM at low temperatures and lowered activity of microflora. Larger amount of OM reaches bottom sediments of the Barents Sea more than in seas, which have similar depth and productivity, but are located at low latitudes. Characteristic features of distribution of lipids and suspended matter in sea water are examined. |
format |
Dataset |
author |
Belyaeva, Alexandra N Romankevich, Evgeny A |
author_facet |
Belyaeva, Alexandra N Romankevich, Evgeny A |
author_sort |
Belyaeva, Alexandra N |
title |
Composition of organic matter in waters of the Barents Sea |
title_short |
Composition of organic matter in waters of the Barents Sea |
title_full |
Composition of organic matter in waters of the Barents Sea |
title_fullStr |
Composition of organic matter in waters of the Barents Sea |
title_full_unstemmed |
Composition of organic matter in waters of the Barents Sea |
title_sort |
composition of organic matter in waters of the barents sea |
publisher |
PANGAEA |
publishDate |
1982 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.755600 https://doi.org/10.1594/PANGAEA.755600 |
op_coverage |
MEDIAN LATITUDE: 73.298486 * MEDIAN LONGITUDE: 39.725722 * SOUTH-BOUND LATITUDE: 69.940000 * WEST-BOUND LONGITUDE: 32.520000 * NORTH-BOUND LATITUDE: 80.100000 * EAST-BOUND LONGITUDE: 55.000000 |
long_lat |
ENVELOPE(32.520000,55.000000,80.100000,69.940000) |
geographic |
Barents Sea |
geographic_facet |
Barents Sea |
genre |
Barents Sea |
genre_facet |
Barents Sea |
op_source |
Supplement to: Belyaeva, Alexandra N; Romankevich, Evgeny A (1982): Organic matter in a water column of the Barents Sea. Oceanology, 22(2), 188-195 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.755600 https://doi.org/10.1594/PANGAEA.755600 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.755600 |
_version_ |
1766368726371794944 |