On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?

Autores
Schloss, Irene Ruth; Wasilowska, A; Dumont, D; Almandoz, Gaston Osvaldo; Hernando, Marcelo Pablo; Michaud Tremblay, C. A; Saravia, L.; Rzepecki, M.; Monien, P.; Monien, D.; Kopczynska, E. E.; Bers, A.V.; Ferreyra, G. A.
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Since the early 1990s, phytoplankton has been studied and monitored in Potter Cove (PC) and Admiralty Bay (AB), King George/25 de Mayo Island (KGI), South Shetlands. Phytoplankton biomass is typically low compared to other Antarctic shelf environments, with average spring—summer values below 1 mg chlorophyll a (Chl a) m−3. The physical conditions in the area (reduced irradiance induced by particles originated from the land, intense winds) limit the coastal productivity at KGI, as a result of shallow Sverdrup's critical depths (Zc) and large turbulent mixing depths (Zt). In January 2010 a large phytoplankton bloom with a maximum of around 20 mg Chl a m−3, and monthly averages of 4 (PC) and 6 (AB) mg Chl a m−3, was observed in the area, making it by far the largest recorded bloom over the last 20 yr. Dominant phytoplankton species were the typical bloom-forming diatoms that are usually found in the western Antarctic Peninsula area. Anomalously cold air temperature and dominant winds from the eastern sector seem to explain adequate light : mixing environment. Local physical conditions were analyzed by means of the relationship between Zc and Zt, and conditions were found adequate for allowing phytoplankton development. However, a multiyear analysis indicates that these conditions may be necessary but not sufficient to guarantee phytoplankton accumulation. The relation between maximum Chl a values and air temperature suggests that bottom-up control would render such large blooms even less frequent in KGI under the warmer climate expected in the area during the second half of the present century.
Fil: Schloss, Irene Ruth. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université du Québec à Rimousk; Canadá
Fil: Wasilowska, A. Warsaw University; Polonia
Fil: Dumont, D. Université du Québec à Rimousk; Canadá
Fil: Almandoz, Gaston Osvaldo. Universidad Nacional de la Plata. Facultad de Ciencias Naturales y Museo. Division Ficología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Hernando, Marcelo Pablo. Comisión Nacional de Energía Atómica; Argentina
Fil: Michaud Tremblay, C. A. Université du Québec à Rimouski; Canadá
Fil: Saravia, L.. Universidad Nacional de General Sarmiento; Argentina
Fil: Rzepecki, M.. Polish Academy of Sciences; Argentina
Fil: Monien, P.. University Oldenburg; Alemania
Fil: Monien, D.. University Oldenburg; Alemania
Fil: Kopczynska, E. E.. Polish Academy of Sciences; Argentina
Fil: Bers, A.V.. Alfred-Wegener-Institute for Polar and Marine Research; Alemania
Fil: Ferreyra, G. A.. Université du Québec à Rimouski; Canadá
Materia
Climate Change
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/24800

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network_name_str CONICET Digital (CONICET)
spelling On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?Schloss, Irene RuthWasilowska, ADumont, DAlmandoz, Gaston OsvaldoHernando, Marcelo PabloMichaud Tremblay, C. ASaravia, L.Rzepecki, M.Monien, P.Monien, D.Kopczynska, E. E.Bers, A.V.Ferreyra, G. A.Climate Changehttps://purl.org/becyt/ford/1.6https://purl.org/becyt/ford/1Since the early 1990s, phytoplankton has been studied and monitored in Potter Cove (PC) and Admiralty Bay (AB), King George/25 de Mayo Island (KGI), South Shetlands. Phytoplankton biomass is typically low compared to other Antarctic shelf environments, with average spring—summer values below 1 mg chlorophyll a (Chl a) m−3. The physical conditions in the area (reduced irradiance induced by particles originated from the land, intense winds) limit the coastal productivity at KGI, as a result of shallow Sverdrup's critical depths (Zc) and large turbulent mixing depths (Zt). In January 2010 a large phytoplankton bloom with a maximum of around 20 mg Chl a m−3, and monthly averages of 4 (PC) and 6 (AB) mg Chl a m−3, was observed in the area, making it by far the largest recorded bloom over the last 20 yr. Dominant phytoplankton species were the typical bloom-forming diatoms that are usually found in the western Antarctic Peninsula area. Anomalously cold air temperature and dominant winds from the eastern sector seem to explain adequate light : mixing environment. Local physical conditions were analyzed by means of the relationship between Zc and Zt, and conditions were found adequate for allowing phytoplankton development. However, a multiyear analysis indicates that these conditions may be necessary but not sufficient to guarantee phytoplankton accumulation. The relation between maximum Chl a values and air temperature suggests that bottom-up control would render such large blooms even less frequent in KGI under the warmer climate expected in the area during the second half of the present century.Fil: Schloss, Irene Ruth. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université du Québec à Rimousk; CanadáFil: Wasilowska, A. Warsaw University; PoloniaFil: Dumont, D. Université du Québec à Rimousk; CanadáFil: Almandoz, Gaston Osvaldo. Universidad Nacional de la Plata. Facultad de Ciencias Naturales y Museo. Division Ficología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Hernando, Marcelo Pablo. Comisión Nacional de Energía Atómica; ArgentinaFil: Michaud Tremblay, C. A. Université du Québec à Rimouski; CanadáFil: Saravia, L.. Universidad Nacional de General Sarmiento; ArgentinaFil: Rzepecki, M.. Polish Academy of Sciences; ArgentinaFil: Monien, P.. University Oldenburg; AlemaniaFil: Monien, D.. University Oldenburg; AlemaniaFil: Kopczynska, E. E.. Polish Academy of Sciences; ArgentinaFil: Bers, A.V.. Alfred-Wegener-Institute for Polar and Marine Research; AlemaniaFil: Ferreyra, G. A.. Université du Québec à Rimouski; CanadáAmer Soc Limnology Oceanography2014-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/24800Schloss, Irene Ruth; Wasilowska, A; Dumont, D; Almandoz, Gaston Osvaldo; Hernando, Marcelo Pablo; et al.; On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?; Amer Soc Limnology Oceanography; Limnology and Oceanography; 59; 1; 1-2014; 195-2100024-3590CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.4319/lo.2014.59.1.0195info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.4319/lo.2014.59.1.0195/abstractinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:22:46Zoai:ri.conicet.gov.ar:11336/24800instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-22 11:22:46.492CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
title On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
spellingShingle On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
Schloss, Irene Ruth
Climate Change
title_short On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
title_full On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
title_fullStr On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
title_full_unstemmed On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
title_sort On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?
dc.creator.none.fl_str_mv Schloss, Irene Ruth
Wasilowska, A
Dumont, D
Almandoz, Gaston Osvaldo
Hernando, Marcelo Pablo
Michaud Tremblay, C. A
Saravia, L.
Rzepecki, M.
Monien, P.
Monien, D.
Kopczynska, E. E.
Bers, A.V.
Ferreyra, G. A.
author Schloss, Irene Ruth
author_facet Schloss, Irene Ruth
Wasilowska, A
Dumont, D
Almandoz, Gaston Osvaldo
Hernando, Marcelo Pablo
Michaud Tremblay, C. A
Saravia, L.
Rzepecki, M.
Monien, P.
Monien, D.
Kopczynska, E. E.
Bers, A.V.
Ferreyra, G. A.
author_role author
author2 Wasilowska, A
Dumont, D
Almandoz, Gaston Osvaldo
Hernando, Marcelo Pablo
Michaud Tremblay, C. A
Saravia, L.
Rzepecki, M.
Monien, P.
Monien, D.
Kopczynska, E. E.
Bers, A.V.
Ferreyra, G. A.
author2_role author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Climate Change
topic Climate Change
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.6
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Since the early 1990s, phytoplankton has been studied and monitored in Potter Cove (PC) and Admiralty Bay (AB), King George/25 de Mayo Island (KGI), South Shetlands. Phytoplankton biomass is typically low compared to other Antarctic shelf environments, with average spring—summer values below 1 mg chlorophyll a (Chl a) m−3. The physical conditions in the area (reduced irradiance induced by particles originated from the land, intense winds) limit the coastal productivity at KGI, as a result of shallow Sverdrup's critical depths (Zc) and large turbulent mixing depths (Zt). In January 2010 a large phytoplankton bloom with a maximum of around 20 mg Chl a m−3, and monthly averages of 4 (PC) and 6 (AB) mg Chl a m−3, was observed in the area, making it by far the largest recorded bloom over the last 20 yr. Dominant phytoplankton species were the typical bloom-forming diatoms that are usually found in the western Antarctic Peninsula area. Anomalously cold air temperature and dominant winds from the eastern sector seem to explain adequate light : mixing environment. Local physical conditions were analyzed by means of the relationship between Zc and Zt, and conditions were found adequate for allowing phytoplankton development. However, a multiyear analysis indicates that these conditions may be necessary but not sufficient to guarantee phytoplankton accumulation. The relation between maximum Chl a values and air temperature suggests that bottom-up control would render such large blooms even less frequent in KGI under the warmer climate expected in the area during the second half of the present century.
Fil: Schloss, Irene Ruth. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université du Québec à Rimousk; Canadá
Fil: Wasilowska, A. Warsaw University; Polonia
Fil: Dumont, D. Université du Québec à Rimousk; Canadá
Fil: Almandoz, Gaston Osvaldo. Universidad Nacional de la Plata. Facultad de Ciencias Naturales y Museo. Division Ficología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Hernando, Marcelo Pablo. Comisión Nacional de Energía Atómica; Argentina
Fil: Michaud Tremblay, C. A. Université du Québec à Rimouski; Canadá
Fil: Saravia, L.. Universidad Nacional de General Sarmiento; Argentina
Fil: Rzepecki, M.. Polish Academy of Sciences; Argentina
Fil: Monien, P.. University Oldenburg; Alemania
Fil: Monien, D.. University Oldenburg; Alemania
Fil: Kopczynska, E. E.. Polish Academy of Sciences; Argentina
Fil: Bers, A.V.. Alfred-Wegener-Institute for Polar and Marine Research; Alemania
Fil: Ferreyra, G. A.. Université du Québec à Rimouski; Canadá
description Since the early 1990s, phytoplankton has been studied and monitored in Potter Cove (PC) and Admiralty Bay (AB), King George/25 de Mayo Island (KGI), South Shetlands. Phytoplankton biomass is typically low compared to other Antarctic shelf environments, with average spring—summer values below 1 mg chlorophyll a (Chl a) m−3. The physical conditions in the area (reduced irradiance induced by particles originated from the land, intense winds) limit the coastal productivity at KGI, as a result of shallow Sverdrup's critical depths (Zc) and large turbulent mixing depths (Zt). In January 2010 a large phytoplankton bloom with a maximum of around 20 mg Chl a m−3, and monthly averages of 4 (PC) and 6 (AB) mg Chl a m−3, was observed in the area, making it by far the largest recorded bloom over the last 20 yr. Dominant phytoplankton species were the typical bloom-forming diatoms that are usually found in the western Antarctic Peninsula area. Anomalously cold air temperature and dominant winds from the eastern sector seem to explain adequate light : mixing environment. Local physical conditions were analyzed by means of the relationship between Zc and Zt, and conditions were found adequate for allowing phytoplankton development. However, a multiyear analysis indicates that these conditions may be necessary but not sufficient to guarantee phytoplankton accumulation. The relation between maximum Chl a values and air temperature suggests that bottom-up control would render such large blooms even less frequent in KGI under the warmer climate expected in the area during the second half of the present century.
publishDate 2014
dc.date.none.fl_str_mv 2014-01
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/24800
Schloss, Irene Ruth; Wasilowska, A; Dumont, D; Almandoz, Gaston Osvaldo; Hernando, Marcelo Pablo; et al.; On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?; Amer Soc Limnology Oceanography; Limnology and Oceanography; 59; 1; 1-2014; 195-210
0024-3590
CONICET Digital
CONICET
url http://hdl.handle.net/11336/24800
identifier_str_mv Schloss, Irene Ruth; Wasilowska, A; Dumont, D; Almandoz, Gaston Osvaldo; Hernando, Marcelo Pablo; et al.; On the phytoplankton bloom in coastal waters of southern King George Island (Antarctica) in January 2010: An exceptional feature?; Amer Soc Limnology Oceanography; Limnology and Oceanography; 59; 1; 1-2014; 195-210
0024-3590
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.4319/lo.2014.59.1.0195
info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.4319/lo.2014.59.1.0195/abstract
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Amer Soc Limnology Oceanography
publisher.none.fl_str_mv Amer Soc Limnology Oceanography
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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