Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia)
- Autores
- Flores Melo, Elizabeth Ximena; Giesecke, R.; Schloss, Irene Ruth; Latorre, Maite Pilmayquen; Durrieu de Madron, X.; Bourrin, F.; Spinelli, Mariela Lorena; Menniti, C.; González, H. E.; Menschel, E.; Martín de Nascimento, Jacobo
- Año de publicación
- 2024
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Beagle Channel is a 300-km long passage connecting the Pacific and Atlantic Oceans at ~55° S, where glaciers and river streams meet subantarctic waters. Here we present the first evaluation of downward fluxes and composition of particulate matter in the channel. Settling particle fluxes were collected by sequential sediment traps deployed in two contrasting areas: one in the western part of the channel, corresponding to an early post-glacial environment (site A) and a second, fully deglaciated, river-dominated environment (site B) in the eastern part. In early summer, fluxes at both sites are driven by organic matter produced in spring, with peak organic carbon fluxes of 289 and 413 mg C m−2 d−1 at sites A and B, respectively (C:N ratios of 7.3 and 6.3, respectively). During winter, the fluxes of fecal pellets, particulate organic carbon (POC) and particulate nitrogen (PON) were at their minimum. At site A (integrated annual POC flux of 74 g C m−2 yr−1), seasonality was weak and the flux was driven by ballast material (>95% of total particle flux) of glacial origin year-around, which also promotes the POC export. According to isotopic and taxonomic analyses performed at site A, the low seasonality in the organic component of the flux appears to be mainly related to autochthonous production of nano- and picophytoplankton during autumn and winter, later replaced by microphytoplankton fluxes during spring and summer. At site B, ballast material accounted for <60% of total mass flux and the POC flux showed a marked seasonality with a well-defined maximum after the spring phytoplankton bloom. Regarding the contribution of zooplankton, fecal pellets of appendicularians dominated at the western sector of the channel (site A) while Munida gregaria pellets dominated the flux at the eastern site (site B). This work is a contribution to ongoing efforts to unveil the physical and biogeochemical variables driving the biological carbon pump and the land-sea connections in this high-latitude ecosystem threatened by climate change.
Fil: Flores Melo, Elizabeth Ximena. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Giesecke, R.. Universidad Austral de Chile; Chile
Fil: Schloss, Irene Ruth. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Latorre, Maite Pilmayquen. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Durrieu de Madron, X.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; Francia
Fil: Bourrin, F.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; Francia
Fil: Spinelli, Mariela Lorena. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Biodiversidad y Biología Experimental y Aplicada. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Biodiversidad y Biología Experimental y Aplicada; Argentina
Fil: Menniti, C.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; Francia
Fil: González, H. E.. Universidad Austral de Chile; Chile
Fil: Menschel, E.. Centro de Investigacion En Ecosistemas de la Patagonia;
Fil: Martín de Nascimento, Jacobo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina - Materia
-
BALLAST MATTER
BEAGLE CHANNEL
HIGH LATITUDE ECOSYSTEMS
PELAGIC-BENTHIC COUPLING
SOUTHERN PATAGONIA
VERTICAL CARBON FLUX - 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:11336/240721
Ver los metadatos del registro completo
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oai:ri.conicet.gov.ar:11336/240721 |
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repository_id_str |
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CONICET Digital (CONICET) |
spelling |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia)Flores Melo, Elizabeth XimenaGiesecke, R.Schloss, Irene RuthLatorre, Maite PilmayquenDurrieu de Madron, X.Bourrin, F.Spinelli, Mariela LorenaMenniti, C.González, H. E.Menschel, E.Martín de Nascimento, JacoboBALLAST MATTERBEAGLE CHANNELHIGH LATITUDE ECOSYSTEMSPELAGIC-BENTHIC COUPLINGSOUTHERN PATAGONIAVERTICAL CARBON FLUXhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Beagle Channel is a 300-km long passage connecting the Pacific and Atlantic Oceans at ~55° S, where glaciers and river streams meet subantarctic waters. Here we present the first evaluation of downward fluxes and composition of particulate matter in the channel. Settling particle fluxes were collected by sequential sediment traps deployed in two contrasting areas: one in the western part of the channel, corresponding to an early post-glacial environment (site A) and a second, fully deglaciated, river-dominated environment (site B) in the eastern part. In early summer, fluxes at both sites are driven by organic matter produced in spring, with peak organic carbon fluxes of 289 and 413 mg C m−2 d−1 at sites A and B, respectively (C:N ratios of 7.3 and 6.3, respectively). During winter, the fluxes of fecal pellets, particulate organic carbon (POC) and particulate nitrogen (PON) were at their minimum. At site A (integrated annual POC flux of 74 g C m−2 yr−1), seasonality was weak and the flux was driven by ballast material (>95% of total particle flux) of glacial origin year-around, which also promotes the POC export. According to isotopic and taxonomic analyses performed at site A, the low seasonality in the organic component of the flux appears to be mainly related to autochthonous production of nano- and picophytoplankton during autumn and winter, later replaced by microphytoplankton fluxes during spring and summer. At site B, ballast material accounted for <60% of total mass flux and the POC flux showed a marked seasonality with a well-defined maximum after the spring phytoplankton bloom. Regarding the contribution of zooplankton, fecal pellets of appendicularians dominated at the western sector of the channel (site A) while Munida gregaria pellets dominated the flux at the eastern site (site B). This work is a contribution to ongoing efforts to unveil the physical and biogeochemical variables driving the biological carbon pump and the land-sea connections in this high-latitude ecosystem threatened by climate change.Fil: Flores Melo, Elizabeth Ximena. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Giesecke, R.. Universidad Austral de Chile; ChileFil: Schloss, Irene Ruth. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; ArgentinaFil: Latorre, Maite Pilmayquen. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Durrieu de Madron, X.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; FranciaFil: Bourrin, F.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; FranciaFil: Spinelli, Mariela Lorena. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Biodiversidad y Biología Experimental y Aplicada. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Biodiversidad y Biología Experimental y Aplicada; ArgentinaFil: Menniti, C.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; FranciaFil: González, H. E.. Universidad Austral de Chile; ChileFil: Menschel, E.. Centro de Investigacion En Ecosistemas de la Patagonia;Fil: Martín de Nascimento, Jacobo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaElsevier Science2024-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/240721Flores Melo, Elizabeth Ximena; Giesecke, R.; Schloss, Irene Ruth; Latorre, Maite Pilmayquen; Durrieu de Madron, X.; et al.; Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia); Elsevier Science; Journal of Marine Systems; 241; 1-2024; 1-360924-7963CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://linkinghub.elsevier.com/retrieve/pii/S092479632300057Xinfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.jmarsys.2023.103913info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:34:17Zoai:ri.conicet.gov.ar:11336/240721instacron: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:34982025-09-29 09:34:17.695CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) |
title |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) |
spellingShingle |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) Flores Melo, Elizabeth Ximena BALLAST MATTER BEAGLE CHANNEL HIGH LATITUDE ECOSYSTEMS PELAGIC-BENTHIC COUPLING SOUTHERN PATAGONIA VERTICAL CARBON FLUX |
title_short |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) |
title_full |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) |
title_fullStr |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) |
title_full_unstemmed |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) |
title_sort |
Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia) |
dc.creator.none.fl_str_mv |
Flores Melo, Elizabeth Ximena Giesecke, R. Schloss, Irene Ruth Latorre, Maite Pilmayquen Durrieu de Madron, X. Bourrin, F. Spinelli, Mariela Lorena Menniti, C. González, H. E. Menschel, E. Martín de Nascimento, Jacobo |
author |
Flores Melo, Elizabeth Ximena |
author_facet |
Flores Melo, Elizabeth Ximena Giesecke, R. Schloss, Irene Ruth Latorre, Maite Pilmayquen Durrieu de Madron, X. Bourrin, F. Spinelli, Mariela Lorena Menniti, C. González, H. E. Menschel, E. Martín de Nascimento, Jacobo |
author_role |
author |
author2 |
Giesecke, R. Schloss, Irene Ruth Latorre, Maite Pilmayquen Durrieu de Madron, X. Bourrin, F. Spinelli, Mariela Lorena Menniti, C. González, H. E. Menschel, E. Martín de Nascimento, Jacobo |
author2_role |
author author author author author author author author author author |
dc.subject.none.fl_str_mv |
BALLAST MATTER BEAGLE CHANNEL HIGH LATITUDE ECOSYSTEMS PELAGIC-BENTHIC COUPLING SOUTHERN PATAGONIA VERTICAL CARBON FLUX |
topic |
BALLAST MATTER BEAGLE CHANNEL HIGH LATITUDE ECOSYSTEMS PELAGIC-BENTHIC COUPLING SOUTHERN PATAGONIA VERTICAL CARBON FLUX |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Beagle Channel is a 300-km long passage connecting the Pacific and Atlantic Oceans at ~55° S, where glaciers and river streams meet subantarctic waters. Here we present the first evaluation of downward fluxes and composition of particulate matter in the channel. Settling particle fluxes were collected by sequential sediment traps deployed in two contrasting areas: one in the western part of the channel, corresponding to an early post-glacial environment (site A) and a second, fully deglaciated, river-dominated environment (site B) in the eastern part. In early summer, fluxes at both sites are driven by organic matter produced in spring, with peak organic carbon fluxes of 289 and 413 mg C m−2 d−1 at sites A and B, respectively (C:N ratios of 7.3 and 6.3, respectively). During winter, the fluxes of fecal pellets, particulate organic carbon (POC) and particulate nitrogen (PON) were at their minimum. At site A (integrated annual POC flux of 74 g C m−2 yr−1), seasonality was weak and the flux was driven by ballast material (>95% of total particle flux) of glacial origin year-around, which also promotes the POC export. According to isotopic and taxonomic analyses performed at site A, the low seasonality in the organic component of the flux appears to be mainly related to autochthonous production of nano- and picophytoplankton during autumn and winter, later replaced by microphytoplankton fluxes during spring and summer. At site B, ballast material accounted for <60% of total mass flux and the POC flux showed a marked seasonality with a well-defined maximum after the spring phytoplankton bloom. Regarding the contribution of zooplankton, fecal pellets of appendicularians dominated at the western sector of the channel (site A) while Munida gregaria pellets dominated the flux at the eastern site (site B). This work is a contribution to ongoing efforts to unveil the physical and biogeochemical variables driving the biological carbon pump and the land-sea connections in this high-latitude ecosystem threatened by climate change. Fil: Flores Melo, Elizabeth Ximena. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Giesecke, R.. Universidad Austral de Chile; Chile Fil: Schloss, Irene Ruth. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina Fil: Latorre, Maite Pilmayquen. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Durrieu de Madron, X.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; Francia Fil: Bourrin, F.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; Francia Fil: Spinelli, Mariela Lorena. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Biodiversidad y Biología Experimental y Aplicada. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Biodiversidad y Biología Experimental y Aplicada; Argentina Fil: Menniti, C.. Centre de Formation et de Recherche sur les Environnements Méditerranéens; Francia Fil: González, H. E.. Universidad Austral de Chile; Chile Fil: Menschel, E.. Centro de Investigacion En Ecosistemas de la Patagonia; Fil: Martín de Nascimento, Jacobo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina |
description |
The Beagle Channel is a 300-km long passage connecting the Pacific and Atlantic Oceans at ~55° S, where glaciers and river streams meet subantarctic waters. Here we present the first evaluation of downward fluxes and composition of particulate matter in the channel. Settling particle fluxes were collected by sequential sediment traps deployed in two contrasting areas: one in the western part of the channel, corresponding to an early post-glacial environment (site A) and a second, fully deglaciated, river-dominated environment (site B) in the eastern part. In early summer, fluxes at both sites are driven by organic matter produced in spring, with peak organic carbon fluxes of 289 and 413 mg C m−2 d−1 at sites A and B, respectively (C:N ratios of 7.3 and 6.3, respectively). During winter, the fluxes of fecal pellets, particulate organic carbon (POC) and particulate nitrogen (PON) were at their minimum. At site A (integrated annual POC flux of 74 g C m−2 yr−1), seasonality was weak and the flux was driven by ballast material (>95% of total particle flux) of glacial origin year-around, which also promotes the POC export. According to isotopic and taxonomic analyses performed at site A, the low seasonality in the organic component of the flux appears to be mainly related to autochthonous production of nano- and picophytoplankton during autumn and winter, later replaced by microphytoplankton fluxes during spring and summer. At site B, ballast material accounted for <60% of total mass flux and the POC flux showed a marked seasonality with a well-defined maximum after the spring phytoplankton bloom. Regarding the contribution of zooplankton, fecal pellets of appendicularians dominated at the western sector of the channel (site A) while Munida gregaria pellets dominated the flux at the eastern site (site B). This work is a contribution to ongoing efforts to unveil the physical and biogeochemical variables driving the biological carbon pump and the land-sea connections in this high-latitude ecosystem threatened by climate change. |
publishDate |
2024 |
dc.date.none.fl_str_mv |
2024-01 |
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/11336/240721 Flores Melo, Elizabeth Ximena; Giesecke, R.; Schloss, Irene Ruth; Latorre, Maite Pilmayquen; Durrieu de Madron, X.; et al.; Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia); Elsevier Science; Journal of Marine Systems; 241; 1-2024; 1-36 0924-7963 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/240721 |
identifier_str_mv |
Flores Melo, Elizabeth Ximena; Giesecke, R.; Schloss, Irene Ruth; Latorre, Maite Pilmayquen; Durrieu de Madron, X.; et al.; Seasonal and spatial variability of vertical particle flux along the Beagle Channel (Southern Patagonia); Elsevier Science; Journal of Marine Systems; 241; 1-2024; 1-36 0924-7963 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://linkinghub.elsevier.com/retrieve/pii/S092479632300057X info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jmarsys.2023.103913 |
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 application/pdf application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Elsevier Science |
publisher.none.fl_str_mv |
Elsevier Science |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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1844613060426203136 |
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13.070432 |