Nutrient concentrations and primary production in the Bering Sea in June 1992
Calculations of new production (NP) are made based on hydrochemical characteristics, recycling production (RP) is assessed on the basis of recycling of phosphorus and nitrogen. Photosynthesis, coupling with uptake of nutrients and development of minimum of silicate and maximum of oxygen, at the lowe...
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1995
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.755746 2023-05-15T15:43:03+02:00 Nutrient concentrations and primary production in the Bering Sea in June 1992 Sapozhnikov, Victor V Naletova, I A MEDIAN LATITUDE: 58.860000 * MEDIAN LONGITUDE: 170.813333 * SOUTH-BOUND LATITUDE: 56.150000 * WEST-BOUND LONGITUDE: 164.140000 * NORTH-BOUND LATITUDE: 61.960000 * EAST-BOUND LONGITUDE: 178.270000 1995-01-13 application/zip, 15 datasets https://doi.pangaea.de/10.1594/PANGAEA.755746 https://doi.org/10.1594/PANGAEA.755746 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.755746 https://doi.org/10.1594/PANGAEA.755746 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Sapozhnikov, Victor V; Naletova, I A (1995): Studies of the biohydrochemical structure of the euphotic layer and primary production in the Bering Sea. Oceanology, 35(2), 189-196 Akademik Kurchatov AKU26A Archive of Ocean Data ARCOD Bering Sea MULT Multiple investigations Sap-92-2105 Sap-92-2106 Sap-92-2110 Sap-92-2111 Sap-92-2112 Sap-92-2117 Sap-92-2123 Sap-92-2126 Sap-92-2127 Sap-92-2129 Sap-92-2130 Sap-92-2133 Sap-92-2134 Sap-92-2138 Sap-92-2139 Dataset 1995 ftpangaea https://doi.org/10.1594/PANGAEA.755746 2023-01-20T07:32:01Z Calculations of new production (NP) are made based on hydrochemical characteristics, recycling production (RP) is assessed on the basis of recycling of phosphorus and nitrogen. Photosynthesis, coupling with uptake of nutrients and development of minimum of silicate and maximum of oxygen, at the lower chlorophyll maximum in the pycnocline is discussed. In situ determination of production by C-14 and oxygen and vertical scanning of chlorophyll A have permitted to calculate assimilation numbers for all the biohydrochemical areas and to map primary production (PP) distribution in the Bering Sea. The total PP in the Bering Sea has been assessed as 6.4x10**8 t C/yr. Dataset Bering Sea PANGAEA - Data Publisher for Earth & Environmental Science Bering Sea ENVELOPE(164.140000,178.270000,61.960000,56.150000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Akademik Kurchatov AKU26A Archive of Ocean Data ARCOD Bering Sea MULT Multiple investigations Sap-92-2105 Sap-92-2106 Sap-92-2110 Sap-92-2111 Sap-92-2112 Sap-92-2117 Sap-92-2123 Sap-92-2126 Sap-92-2127 Sap-92-2129 Sap-92-2130 Sap-92-2133 Sap-92-2134 Sap-92-2138 Sap-92-2139 |
spellingShingle |
Akademik Kurchatov AKU26A Archive of Ocean Data ARCOD Bering Sea MULT Multiple investigations Sap-92-2105 Sap-92-2106 Sap-92-2110 Sap-92-2111 Sap-92-2112 Sap-92-2117 Sap-92-2123 Sap-92-2126 Sap-92-2127 Sap-92-2129 Sap-92-2130 Sap-92-2133 Sap-92-2134 Sap-92-2138 Sap-92-2139 Sapozhnikov, Victor V Naletova, I A Nutrient concentrations and primary production in the Bering Sea in June 1992 |
topic_facet |
Akademik Kurchatov AKU26A Archive of Ocean Data ARCOD Bering Sea MULT Multiple investigations Sap-92-2105 Sap-92-2106 Sap-92-2110 Sap-92-2111 Sap-92-2112 Sap-92-2117 Sap-92-2123 Sap-92-2126 Sap-92-2127 Sap-92-2129 Sap-92-2130 Sap-92-2133 Sap-92-2134 Sap-92-2138 Sap-92-2139 |
description |
Calculations of new production (NP) are made based on hydrochemical characteristics, recycling production (RP) is assessed on the basis of recycling of phosphorus and nitrogen. Photosynthesis, coupling with uptake of nutrients and development of minimum of silicate and maximum of oxygen, at the lower chlorophyll maximum in the pycnocline is discussed. In situ determination of production by C-14 and oxygen and vertical scanning of chlorophyll A have permitted to calculate assimilation numbers for all the biohydrochemical areas and to map primary production (PP) distribution in the Bering Sea. The total PP in the Bering Sea has been assessed as 6.4x10**8 t C/yr. |
format |
Dataset |
author |
Sapozhnikov, Victor V Naletova, I A |
author_facet |
Sapozhnikov, Victor V Naletova, I A |
author_sort |
Sapozhnikov, Victor V |
title |
Nutrient concentrations and primary production in the Bering Sea in June 1992 |
title_short |
Nutrient concentrations and primary production in the Bering Sea in June 1992 |
title_full |
Nutrient concentrations and primary production in the Bering Sea in June 1992 |
title_fullStr |
Nutrient concentrations and primary production in the Bering Sea in June 1992 |
title_full_unstemmed |
Nutrient concentrations and primary production in the Bering Sea in June 1992 |
title_sort |
nutrient concentrations and primary production in the bering sea in june 1992 |
publisher |
PANGAEA |
publishDate |
1995 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.755746 https://doi.org/10.1594/PANGAEA.755746 |
op_coverage |
MEDIAN LATITUDE: 58.860000 * MEDIAN LONGITUDE: 170.813333 * SOUTH-BOUND LATITUDE: 56.150000 * WEST-BOUND LONGITUDE: 164.140000 * NORTH-BOUND LATITUDE: 61.960000 * EAST-BOUND LONGITUDE: 178.270000 |
long_lat |
ENVELOPE(164.140000,178.270000,61.960000,56.150000) |
geographic |
Bering Sea |
geographic_facet |
Bering Sea |
genre |
Bering Sea |
genre_facet |
Bering Sea |
op_source |
Supplement to: Sapozhnikov, Victor V; Naletova, I A (1995): Studies of the biohydrochemical structure of the euphotic layer and primary production in the Bering Sea. Oceanology, 35(2), 189-196 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.755746 https://doi.org/10.1594/PANGAEA.755746 |
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.755746 |
_version_ |
1766377066999054336 |