Ocean productivity across the subtropical front over the last deglaciation

5th Past Global Changes (PAGES) Ocean Sciences Meeting, 9-13 May 2017, Zaragoza The Subtropical Front (STF) separates warm and saltier subtropical waters from the cold, less saline and nutrient-rich subantarctic waters of the Southern Ocean. Determining its past north-south movements is crucial, for...

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Main Authors: Calvo, Eva María, Quirós-Collazos, Lucía, Bostock, H., Schouten, Stefan, Neil, H., Pelejero, Carles
Format: Conference Object
Language:unknown
Published: PAGES International Project Office 2017
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Online Access:http://hdl.handle.net/10261/178686
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spelling ftcsic:oai:digital.csic.es:10261/178686 2024-02-11T10:08:52+01:00 Ocean productivity across the subtropical front over the last deglaciation Calvo, Eva María Quirós-Collazos, Lucía Bostock, H. Schouten, Stefan Neil, H. Pelejero, Carles 2017-05-09 http://hdl.handle.net/10261/178686 unknown PAGES International Project Office http://pastglobalchanges.org/calendar/2017/127-pages/1552-5th-pages-open-science-meeting Sí 5th PAGES Ocean Sciences Meeting (2017) http://hdl.handle.net/10261/178686 none comunicación de congreso http://purl.org/coar/resource_type/c_5794 2017 ftcsic 2024-01-16T10:37:35Z 5th Past Global Changes (PAGES) Ocean Sciences Meeting, 9-13 May 2017, Zaragoza The Subtropical Front (STF) separates warm and saltier subtropical waters from the cold, less saline and nutrient-rich subantarctic waters of the Southern Ocean. Determining its past north-south movements is crucial, for instance, to understand the role of such frontal systems on ocean productivity of the subantarctic region, as opposed to increased Fe availability. Three marine cores were recovered south of New Zealand, along a latitudinal transect crossing the modern STF. We have analysed long chain alkenones, as markers of coccolithophore productivity and past sea surface temperatures, n-alkanes and n-alcohols, as proxies for continental input and dust-derived iron and long chain diols as tracers of diatom productivity. Reconstructed SST changes show a 3-4°C temperature gradient during the Holocene between the core locations, while during the last glacial period no temperature gradient existed, with 8-9°C recorded at all three sites. This suggests a northward displacement of the STF during the cold glacial climate and the prevalence of subantarctic waters at the core sites, between 47 and 50.5°S. An increased productivity and continental input during the glacial and early deglaciation suggest that both Fe fertilization and equatorward migration of fronts likely drove the biological productivity of the region. The SST evolution will also be complemented with a temperature reconstruction based on the relative distribution of isoprenoid GDGTs, the TEXH86 index, which in this region, we believe may record deeper temperatures than coccolithophores Peer Reviewed Conference Object Southern Ocean Digital.CSIC (Spanish National Research Council) New Zealand Southern Ocean
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
description 5th Past Global Changes (PAGES) Ocean Sciences Meeting, 9-13 May 2017, Zaragoza The Subtropical Front (STF) separates warm and saltier subtropical waters from the cold, less saline and nutrient-rich subantarctic waters of the Southern Ocean. Determining its past north-south movements is crucial, for instance, to understand the role of such frontal systems on ocean productivity of the subantarctic region, as opposed to increased Fe availability. Three marine cores were recovered south of New Zealand, along a latitudinal transect crossing the modern STF. We have analysed long chain alkenones, as markers of coccolithophore productivity and past sea surface temperatures, n-alkanes and n-alcohols, as proxies for continental input and dust-derived iron and long chain diols as tracers of diatom productivity. Reconstructed SST changes show a 3-4°C temperature gradient during the Holocene between the core locations, while during the last glacial period no temperature gradient existed, with 8-9°C recorded at all three sites. This suggests a northward displacement of the STF during the cold glacial climate and the prevalence of subantarctic waters at the core sites, between 47 and 50.5°S. An increased productivity and continental input during the glacial and early deglaciation suggest that both Fe fertilization and equatorward migration of fronts likely drove the biological productivity of the region. The SST evolution will also be complemented with a temperature reconstruction based on the relative distribution of isoprenoid GDGTs, the TEXH86 index, which in this region, we believe may record deeper temperatures than coccolithophores Peer Reviewed
format Conference Object
author Calvo, Eva María
Quirós-Collazos, Lucía
Bostock, H.
Schouten, Stefan
Neil, H.
Pelejero, Carles
spellingShingle Calvo, Eva María
Quirós-Collazos, Lucía
Bostock, H.
Schouten, Stefan
Neil, H.
Pelejero, Carles
Ocean productivity across the subtropical front over the last deglaciation
author_facet Calvo, Eva María
Quirós-Collazos, Lucía
Bostock, H.
Schouten, Stefan
Neil, H.
Pelejero, Carles
author_sort Calvo, Eva María
title Ocean productivity across the subtropical front over the last deglaciation
title_short Ocean productivity across the subtropical front over the last deglaciation
title_full Ocean productivity across the subtropical front over the last deglaciation
title_fullStr Ocean productivity across the subtropical front over the last deglaciation
title_full_unstemmed Ocean productivity across the subtropical front over the last deglaciation
title_sort ocean productivity across the subtropical front over the last deglaciation
publisher PAGES International Project Office
publishDate 2017
url http://hdl.handle.net/10261/178686
geographic New Zealand
Southern Ocean
geographic_facet New Zealand
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation http://pastglobalchanges.org/calendar/2017/127-pages/1552-5th-pages-open-science-meeting

5th PAGES Ocean Sciences Meeting (2017)
http://hdl.handle.net/10261/178686
op_rights none
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