Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic

A large part of the Pacific Arctic basin experiences ice-free conditions in summer as a result of sea ice cover steadily decreasing over the last decades. To evaluate the impact of sea ice retreat on the marine ecosystem, phytoplankton in situ observations were acquired over the Chukchi shelf and th...

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Published in:Biogeosciences
Main Authors: P. Coupel, H. Y. Jin, M. Joo, R. Horner, H. A. Bouvet, M.-A. Sicre, J.-C. Gascard, J. F. Chen, V. Garçon, D. Ruiz-Pino
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2012
Subjects:
Online Access:https://doi.org/10.5194/bg-9-4835-2012
https://doaj.org/article/c78ec91730f14145a9687b2a138623e5
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spelling ftdoajarticles:oai:doaj.org/article:c78ec91730f14145a9687b2a138623e5 2023-05-15T14:29:12+02:00 Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic P. Coupel H. Y. Jin M. Joo R. Horner H. A. Bouvet M.-A. Sicre J.-C. Gascard J. F. Chen V. Garçon D. Ruiz-Pino 2012-11-01T00:00:00Z https://doi.org/10.5194/bg-9-4835-2012 https://doaj.org/article/c78ec91730f14145a9687b2a138623e5 EN eng Copernicus Publications http://www.biogeosciences.net/9/4835/2012/bg-9-4835-2012.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-9-4835-2012 1726-4170 1726-4189 https://doaj.org/article/c78ec91730f14145a9687b2a138623e5 Biogeosciences, Vol 9, Iss 11, Pp 4835-4850 (2012) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2012 ftdoajarticles https://doi.org/10.5194/bg-9-4835-2012 2022-12-30T21:27:33Z A large part of the Pacific Arctic basin experiences ice-free conditions in summer as a result of sea ice cover steadily decreasing over the last decades. To evaluate the impact of sea ice retreat on the marine ecosystem, phytoplankton in situ observations were acquired over the Chukchi shelf and the Canadian basin in 2008, a year of high melting. Pigment analyses and taxonomy enumerations were used to characterise the distribution of main phytoplanktonic groups. Marked spatial variability of the phytoplankton distribution was observed in summer 2008. Comparison of eight phytoplankton functional groups and 3 size-classes (pico-, nano- and micro-phytoplankton) also showed significant differences in abundance, biomass and distribution between summer of low ice cover (2008) and heavy ice summer (1994). Environmental parameters such as freshening, stratification, light and nutrient availability are discussed as possible causes to explain the observed differences in phytoplankton community structure between 1994 and 2008. Article in Journal/Newspaper Arctic Basin Arctic Chukchi Pacific Arctic Phytoplankton Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Pacific Chukchi Shelf ENVELOPE(-169.167,-169.167,70.550,70.550) Biogeosciences 9 11 4835 4850
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
spellingShingle Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
P. Coupel
H. Y. Jin
M. Joo
R. Horner
H. A. Bouvet
M.-A. Sicre
J.-C. Gascard
J. F. Chen
V. Garçon
D. Ruiz-Pino
Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic
topic_facet Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
description A large part of the Pacific Arctic basin experiences ice-free conditions in summer as a result of sea ice cover steadily decreasing over the last decades. To evaluate the impact of sea ice retreat on the marine ecosystem, phytoplankton in situ observations were acquired over the Chukchi shelf and the Canadian basin in 2008, a year of high melting. Pigment analyses and taxonomy enumerations were used to characterise the distribution of main phytoplanktonic groups. Marked spatial variability of the phytoplankton distribution was observed in summer 2008. Comparison of eight phytoplankton functional groups and 3 size-classes (pico-, nano- and micro-phytoplankton) also showed significant differences in abundance, biomass and distribution between summer of low ice cover (2008) and heavy ice summer (1994). Environmental parameters such as freshening, stratification, light and nutrient availability are discussed as possible causes to explain the observed differences in phytoplankton community structure between 1994 and 2008.
format Article in Journal/Newspaper
author P. Coupel
H. Y. Jin
M. Joo
R. Horner
H. A. Bouvet
M.-A. Sicre
J.-C. Gascard
J. F. Chen
V. Garçon
D. Ruiz-Pino
author_facet P. Coupel
H. Y. Jin
M. Joo
R. Horner
H. A. Bouvet
M.-A. Sicre
J.-C. Gascard
J. F. Chen
V. Garçon
D. Ruiz-Pino
author_sort P. Coupel
title Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic
title_short Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic
title_full Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic
title_fullStr Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic
title_full_unstemmed Phytoplankton distribution in unusually low sea ice cover over the Pacific Arctic
title_sort phytoplankton distribution in unusually low sea ice cover over the pacific arctic
publisher Copernicus Publications
publishDate 2012
url https://doi.org/10.5194/bg-9-4835-2012
https://doaj.org/article/c78ec91730f14145a9687b2a138623e5
long_lat ENVELOPE(-169.167,-169.167,70.550,70.550)
geographic Arctic
Pacific
Chukchi Shelf
geographic_facet Arctic
Pacific
Chukchi Shelf
genre Arctic Basin
Arctic
Chukchi
Pacific Arctic
Phytoplankton
Sea ice
genre_facet Arctic Basin
Arctic
Chukchi
Pacific Arctic
Phytoplankton
Sea ice
op_source Biogeosciences, Vol 9, Iss 11, Pp 4835-4850 (2012)
op_relation http://www.biogeosciences.net/9/4835/2012/bg-9-4835-2012.pdf
https://doaj.org/toc/1726-4170
https://doaj.org/toc/1726-4189
doi:10.5194/bg-9-4835-2012
1726-4170
1726-4189
https://doaj.org/article/c78ec91730f14145a9687b2a138623e5
op_doi https://doi.org/10.5194/bg-9-4835-2012
container_title Biogeosciences
container_volume 9
container_issue 11
container_start_page 4835
op_container_end_page 4850
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