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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/24800
Ver los metadatos del registro completo
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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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1846781749016657920 |
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12.982451 |