BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN
A summer field survey off Point Barrow, Alaska, revealed a growth of photosynthetic diatoms in Arctic sea ice. The diatoms are found in a brine solution in microfissures between ice crystals on the underside of the ice. The chlorophyl content of this layer is 100 times that of the surrounding sea wa...
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National Institute of Polar Research
1967
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Online Access: | https://doi.org/10.15094/00007439 https://doaj.org/article/625519d8cc7b44899023fa4197a47f62 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:625519d8cc7b44899023fa4197a47f62 2023-05-15T14:35:11+02:00 BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN Hiroshi MEGURO Kuniyuki ITO Hiroshi FUKUSHIMA 1967-03-01 https://doi.org/10.15094/00007439 https://doaj.org/article/625519d8cc7b44899023fa4197a47f62 en other eng National Institute of Polar Research doi:10.15094/00007439 0085-7289 2432-079X https://doaj.org/article/625519d8cc7b44899023fa4197a47f62 undefined Antarctic Record, Iss 28, Pp 2257-2271 (1967) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1967 fttriple https://doi.org/10.15094/00007439 2023-01-22T19:12:27Z A summer field survey off Point Barrow, Alaska, revealed a growth of photosynthetic diatoms in Arctic sea ice. The diatoms are found in a brine solution in microfissures between ice crystals on the underside of the ice. The chlorophyl content of this layer is 100 times that of the surrounding sea waters. Arctic sea ice is found to be neither a closed frozen system that disallows transportation of nutrient substances nor a completely inactive biochemical habitat owing to the extremely low tempereture. Glaciologically it is a kind of seasonal nutrient metabolism associated with desalinization of sea ice and photosynthesis by diatoms. A considerable fraction of the primary production of the Arctic Sea may occur in sea ice. Article in Journal/Newspaper Arctic Arctic Ocean Barrow Point Barrow Sea ice Alaska Unknown Arctic Arctic Ocean |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
geo envir |
spellingShingle |
geo envir Hiroshi MEGURO Kuniyuki ITO Hiroshi FUKUSHIMA BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN |
topic_facet |
geo envir |
description |
A summer field survey off Point Barrow, Alaska, revealed a growth of photosynthetic diatoms in Arctic sea ice. The diatoms are found in a brine solution in microfissures between ice crystals on the underside of the ice. The chlorophyl content of this layer is 100 times that of the surrounding sea waters. Arctic sea ice is found to be neither a closed frozen system that disallows transportation of nutrient substances nor a completely inactive biochemical habitat owing to the extremely low tempereture. Glaciologically it is a kind of seasonal nutrient metabolism associated with desalinization of sea ice and photosynthesis by diatoms. A considerable fraction of the primary production of the Arctic Sea may occur in sea ice. |
format |
Article in Journal/Newspaper |
author |
Hiroshi MEGURO Kuniyuki ITO Hiroshi FUKUSHIMA |
author_facet |
Hiroshi MEGURO Kuniyuki ITO Hiroshi FUKUSHIMA |
author_sort |
Hiroshi MEGURO |
title |
BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN |
title_short |
BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN |
title_full |
BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN |
title_fullStr |
BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN |
title_full_unstemmed |
BOTTOM TYPE 'PLANKTON ICE' IN THE ARCTIC OCEAN |
title_sort |
bottom type 'plankton ice' in the arctic ocean |
publisher |
National Institute of Polar Research |
publishDate |
1967 |
url |
https://doi.org/10.15094/00007439 https://doaj.org/article/625519d8cc7b44899023fa4197a47f62 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Barrow Point Barrow Sea ice Alaska |
genre_facet |
Arctic Arctic Ocean Barrow Point Barrow Sea ice Alaska |
op_source |
Antarctic Record, Iss 28, Pp 2257-2271 (1967) |
op_relation |
doi:10.15094/00007439 0085-7289 2432-079X https://doaj.org/article/625519d8cc7b44899023fa4197a47f62 |
op_rights |
undefined |
op_doi |
https://doi.org/10.15094/00007439 |
_version_ |
1766308067482271744 |