Plankton distribution associated with frontal zones
We studied the effect of four types of fronts- the coastal front, the middle front, the shelf partition front and the shelf break front on the quantitative distribution and the composition of plankton communities in the Pribilof area of the eastern Bering Sea shelf in late spring and summer of 1993...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.505.9741 2023-05-15T15:43:54+02:00 Plankton distribution associated with frontal zones Mikhail V. Flint Irina N. Sukhanova Er I. Kopylov Sergei G. Poyarkov Terry E. Whitledge The Pennsylvania State University CiteSeerX Archives 2002 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.9741 http://www.pmel.noaa.gov/foci/sebscc/special_issue/manuscripts/flint_rev.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.9741 http://www.pmel.noaa.gov/foci/sebscc/special_issue/manuscripts/flint_rev.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.pmel.noaa.gov/foci/sebscc/special_issue/manuscripts/flint_rev.pdf text 2002 ftciteseerx 2016-01-08T09:22:33Z We studied the effect of four types of fronts- the coastal front, the middle front, the shelf partition front and the shelf break front on the quantitative distribution and the composition of plankton communities in the Pribilof area of the eastern Bering Sea shelf in late spring and summer of 1993 and 1994. The coastal fronts near St. Paul and St. George Islands and the coastal domains encircled by the fronts, featured specific taxonomic composition of planktonic algae, high abundance and production of phytoplankton, as well as large numbers of heterotrophic nanoplankton. The coastal fronts were also characterized by high values of total mesozooplankton biomass, high concentrations of Calanus marshallae, as well as relatively high abundances of Parasagitta setosa and Euphausiacea compared to surrounding shelf waters. We hypothesize that wind induced erosion of a weak thermocline in the inner part of the coastal front as well as transfrontal water exchange in subthermocline layers result in nutrient enrichment of the euphotic layer in the coastal fronts and coastal domains in summer time. This leads to prolonged high primary production and high phytoplankton biomass. In this paper a new type of front – the shelf partition front located 45-55 km to the north-east off St. Paul Island is described which is assumed to be formed by the flux of oceanic domain waters onto the shelf. This front features a high abundance of phytoplankton and a high level of primary production compared to the adjacent middle shelf. Near the southwestern periphery of the front a mesozooplankton peak occurred, composed of C. marshallae, with biomass Text Bering Sea Unknown Bering Sea George Islands ENVELOPE(-121.887,-121.887,65.534,65.534) |
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Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
We studied the effect of four types of fronts- the coastal front, the middle front, the shelf partition front and the shelf break front on the quantitative distribution and the composition of plankton communities in the Pribilof area of the eastern Bering Sea shelf in late spring and summer of 1993 and 1994. The coastal fronts near St. Paul and St. George Islands and the coastal domains encircled by the fronts, featured specific taxonomic composition of planktonic algae, high abundance and production of phytoplankton, as well as large numbers of heterotrophic nanoplankton. The coastal fronts were also characterized by high values of total mesozooplankton biomass, high concentrations of Calanus marshallae, as well as relatively high abundances of Parasagitta setosa and Euphausiacea compared to surrounding shelf waters. We hypothesize that wind induced erosion of a weak thermocline in the inner part of the coastal front as well as transfrontal water exchange in subthermocline layers result in nutrient enrichment of the euphotic layer in the coastal fronts and coastal domains in summer time. This leads to prolonged high primary production and high phytoplankton biomass. In this paper a new type of front – the shelf partition front located 45-55 km to the north-east off St. Paul Island is described which is assumed to be formed by the flux of oceanic domain waters onto the shelf. This front features a high abundance of phytoplankton and a high level of primary production compared to the adjacent middle shelf. Near the southwestern periphery of the front a mesozooplankton peak occurred, composed of C. marshallae, with biomass |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Mikhail V. Flint Irina N. Sukhanova Er I. Kopylov Sergei G. Poyarkov Terry E. Whitledge |
spellingShingle |
Mikhail V. Flint Irina N. Sukhanova Er I. Kopylov Sergei G. Poyarkov Terry E. Whitledge Plankton distribution associated with frontal zones |
author_facet |
Mikhail V. Flint Irina N. Sukhanova Er I. Kopylov Sergei G. Poyarkov Terry E. Whitledge |
author_sort |
Mikhail V. Flint |
title |
Plankton distribution associated with frontal zones |
title_short |
Plankton distribution associated with frontal zones |
title_full |
Plankton distribution associated with frontal zones |
title_fullStr |
Plankton distribution associated with frontal zones |
title_full_unstemmed |
Plankton distribution associated with frontal zones |
title_sort |
plankton distribution associated with frontal zones |
publishDate |
2002 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.9741 http://www.pmel.noaa.gov/foci/sebscc/special_issue/manuscripts/flint_rev.pdf |
long_lat |
ENVELOPE(-121.887,-121.887,65.534,65.534) |
geographic |
Bering Sea George Islands |
geographic_facet |
Bering Sea George Islands |
genre |
Bering Sea |
genre_facet |
Bering Sea |
op_source |
http://www.pmel.noaa.gov/foci/sebscc/special_issue/manuscripts/flint_rev.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.9741 http://www.pmel.noaa.gov/foci/sebscc/special_issue/manuscripts/flint_rev.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766378109542596608 |