Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ...
The development of the seasonal phytoplankton bloom in the Ross Sea was studied during two cruises. The first, conducted in November-December 1994, investigated the initiation and rapid growth of the bloom, whereas the second (December 1995-January 1996) concentrated on the bloom's maximum biom...
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ftdatacite:10.1594/pangaea.758059 2024-09-15T17:45:51+00:00 Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ... Smith, Walker O Jr Nelson, David M Mathot, Sylvie 1999 application/zip https://dx.doi.org/10.1594/pangaea.758059 https://doi.pangaea.de/10.1594/PANGAEA.758059 en eng PANGAEA https://dx.doi.org/10.1093/plankt/21.8.1519 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Bottle, Niskin Bio-Rosette RossSeaBloomProject1994 RossSeaBloomProject1995/1996 Nathaniel B. Palmer article Collection Supplementary Publication Series of Datasets 1999 ftdatacite https://doi.org/10.1594/pangaea.75805910.1093/plankt/21.8.1519 2024-08-01T10:50:55Z The development of the seasonal phytoplankton bloom in the Ross Sea was studied during two cruises. The first, conducted in November-December 1994, investigated the initiation and rapid growth of the bloom, whereas the second (December 1995-January 1996) concentrated on the bloom's maximum biomass period and the subsequent decline in biomass. Central to the understanding of the controls of growth and the summer decline of the bloom is a quantitative assessment of the growth rate of phytoplankton. Growth rates were estimated over two time scales with different methods. The first estimated daily growth rates from isotropic incorporation under simulated in situ conditions, including 14C, 15N and 32Si uptake measurements combined with estimates of standing stocks of particulate organic carbon, nitrogen and biogenic silica. The second method used daily to weekly changes in biomass at selected locations, with net growth rates being estimated from changes in standing stocks of phytoplankton. In addition, growth ... : Supplement to: Smith, Walker O Jr; Nelson, David M; Mathot, Sylvie (1999): Phytoplankton growth rates in the Ross Sea, Antarctica, determined by independent methods: temporal variations. Journal of Plankton Research, 21(8), 1519-1536 ... Article in Journal/Newspaper Antarc* Antarctica Ross Sea DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Bottle, Niskin Bio-Rosette RossSeaBloomProject1994 RossSeaBloomProject1995/1996 Nathaniel B. Palmer |
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Bottle, Niskin Bio-Rosette RossSeaBloomProject1994 RossSeaBloomProject1995/1996 Nathaniel B. Palmer Smith, Walker O Jr Nelson, David M Mathot, Sylvie Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ... |
topic_facet |
Bottle, Niskin Bio-Rosette RossSeaBloomProject1994 RossSeaBloomProject1995/1996 Nathaniel B. Palmer |
description |
The development of the seasonal phytoplankton bloom in the Ross Sea was studied during two cruises. The first, conducted in November-December 1994, investigated the initiation and rapid growth of the bloom, whereas the second (December 1995-January 1996) concentrated on the bloom's maximum biomass period and the subsequent decline in biomass. Central to the understanding of the controls of growth and the summer decline of the bloom is a quantitative assessment of the growth rate of phytoplankton. Growth rates were estimated over two time scales with different methods. The first estimated daily growth rates from isotropic incorporation under simulated in situ conditions, including 14C, 15N and 32Si uptake measurements combined with estimates of standing stocks of particulate organic carbon, nitrogen and biogenic silica. The second method used daily to weekly changes in biomass at selected locations, with net growth rates being estimated from changes in standing stocks of phytoplankton. In addition, growth ... : Supplement to: Smith, Walker O Jr; Nelson, David M; Mathot, Sylvie (1999): Phytoplankton growth rates in the Ross Sea, Antarctica, determined by independent methods: temporal variations. Journal of Plankton Research, 21(8), 1519-1536 ... |
format |
Article in Journal/Newspaper |
author |
Smith, Walker O Jr Nelson, David M Mathot, Sylvie |
author_facet |
Smith, Walker O Jr Nelson, David M Mathot, Sylvie |
author_sort |
Smith, Walker O Jr |
title |
Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ... |
title_short |
Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ... |
title_full |
Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ... |
title_fullStr |
Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ... |
title_full_unstemmed |
Biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the Ross Sea Bloom Project 1994-1996 ... |
title_sort |
biogenic and lithogenic silica, silicic acid, production of biogenic silica, and irradiance measurements during the ross sea bloom project 1994-1996 ... |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://dx.doi.org/10.1594/pangaea.758059 https://doi.pangaea.de/10.1594/PANGAEA.758059 |
genre |
Antarc* Antarctica Ross Sea |
genre_facet |
Antarc* Antarctica Ross Sea |
op_relation |
https://dx.doi.org/10.1093/plankt/21.8.1519 |
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.75805910.1093/plankt/21.8.1519 |
_version_ |
1810493768095236096 |