Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics

⋅ nutrients, ⋅ silicate:nitrate ratio, ⋅ phytoplankton.

Bibliographic Details
Main Authors: Bering Sea, Isao Koike, Hiroshi Ogawa, Toshi Nagata, Rumi Fukuda, Hideki Fukuda
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2000
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.622.9446
http://www.terrapub.co.jp/journals/JO/pdf/5703/57030253.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.622.9446 2023-05-15T14:49:03+02:00 Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics Bering Sea Isao Koike Hiroshi Ogawa Toshi Nagata Rumi Fukuda Hideki Fukuda The Pennsylvania State University CiteSeerX Archives 2000 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.622.9446 http://www.terrapub.co.jp/journals/JO/pdf/5703/57030253.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.622.9446 http://www.terrapub.co.jp/journals/JO/pdf/5703/57030253.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.terrapub.co.jp/journals/JO/pdf/5703/57030253.pdf text 2000 ftciteseerx 2016-01-08T15:05:38Z ⋅ nutrients, ⋅ silicate:nitrate ratio, ⋅ phytoplankton. Text Arctic Bering Sea Phytoplankton Unknown Arctic Bering Sea Pacific
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ⋅ nutrients, ⋅ silicate:nitrate ratio, ⋅ phytoplankton.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Bering Sea
Isao Koike
Hiroshi Ogawa
Toshi Nagata
Rumi Fukuda
Hideki Fukuda
spellingShingle Bering Sea
Isao Koike
Hiroshi Ogawa
Toshi Nagata
Rumi Fukuda
Hideki Fukuda
Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics
author_facet Bering Sea
Isao Koike
Hiroshi Ogawa
Toshi Nagata
Rumi Fukuda
Hideki Fukuda
author_sort Bering Sea
title Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics
title_short Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics
title_full Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics
title_fullStr Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics
title_full_unstemmed Copyright © The Oceanographic Society of Japan. Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics
title_sort copyright © the oceanographic society of japan. silicate to nitrate ratio of the upper sub-arctic pacific and the bering sea basin in summer: its implication for phytoplankton dynamics
publishDate 2000
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.622.9446
http://www.terrapub.co.jp/journals/JO/pdf/5703/57030253.pdf
geographic Arctic
Bering Sea
Pacific
geographic_facet Arctic
Bering Sea
Pacific
genre Arctic
Bering Sea
Phytoplankton
genre_facet Arctic
Bering Sea
Phytoplankton
op_source http://www.terrapub.co.jp/journals/JO/pdf/5703/57030253.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.622.9446
http://www.terrapub.co.jp/journals/JO/pdf/5703/57030253.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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