Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ...
Rapid climate changes at the onset of the last deglaciation and during Heinrich Event H4 were studied in detail at IMAGES cores MD95-2039 and MD95-2040 from the Western Iberian margin. A major reorganisation of surface water hydrography, benthic foraminiferal community structure, and deepwater isoto...
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ftdatacite:10.1594/pangaea.733303 2024-03-31T07:54:06+00:00 Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ... Schönfeld, Joachim Zahn, Rainer de Abreu, Lucia 2003 application/zip https://dx.doi.org/10.1594/pangaea.733303 https://doi.pangaea.de/10.1594/PANGAEA.733303 en eng PANGAEA https://dx.doi.org/10.1016/s0921-8181(02)00197-2 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Western Iberian Margin Calypso Corer MD101 Marion Dufresne 1995 International Marine Global Change Study IMAGES Supplementary Publication Series of Datasets article Collection 2003 ftdatacite https://doi.org/10.1594/pangaea.73330310.1016/s0921-8181(02)00197-2 2024-03-04T13:35:39Z Rapid climate changes at the onset of the last deglaciation and during Heinrich Event H4 were studied in detail at IMAGES cores MD95-2039 and MD95-2040 from the Western Iberian margin. A major reorganisation of surface water hydrography, benthic foraminiferal community structure, and deepwater isotopic composition commenced already 540 years before the Last Isotopic Maximum (LIM) at 17.43 cal. ka and within 670 years affected all environments. Changes were initiated by meltwater spill in the Nordic Seas and northern North Atlantic that commenced 100 years before concomitant changes were felt off western Iberia. Benthic foraminiferal associations record the drawdown of deepwater oxygenation during meltwater and subsequent Heinrich Events H1 and H4 with a bloom of dysoxic species. At a water depth of 3380 m, benthic oxygen isotopes depict the influence of brines from sea ice formation during ice-rafting pulses and meltwater spill. The brines conceivably were a source of ventilation and provided oxygen to the ... : Supplement to: Schönfeld, Joachim; Zahn, Rainer; de Abreu, Lucia (2003): Surface to deep water response to rapid climate changes at the western Iberian Margin. Global and Planetary Change, 36(4), 237-264 ... Article in Journal/Newspaper Nordic Seas North Atlantic Sea ice DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Western Iberian Margin Calypso Corer MD101 Marion Dufresne 1995 International Marine Global Change Study IMAGES |
spellingShingle |
Western Iberian Margin Calypso Corer MD101 Marion Dufresne 1995 International Marine Global Change Study IMAGES Schönfeld, Joachim Zahn, Rainer de Abreu, Lucia Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ... |
topic_facet |
Western Iberian Margin Calypso Corer MD101 Marion Dufresne 1995 International Marine Global Change Study IMAGES |
description |
Rapid climate changes at the onset of the last deglaciation and during Heinrich Event H4 were studied in detail at IMAGES cores MD95-2039 and MD95-2040 from the Western Iberian margin. A major reorganisation of surface water hydrography, benthic foraminiferal community structure, and deepwater isotopic composition commenced already 540 years before the Last Isotopic Maximum (LIM) at 17.43 cal. ka and within 670 years affected all environments. Changes were initiated by meltwater spill in the Nordic Seas and northern North Atlantic that commenced 100 years before concomitant changes were felt off western Iberia. Benthic foraminiferal associations record the drawdown of deepwater oxygenation during meltwater and subsequent Heinrich Events H1 and H4 with a bloom of dysoxic species. At a water depth of 3380 m, benthic oxygen isotopes depict the influence of brines from sea ice formation during ice-rafting pulses and meltwater spill. The brines conceivably were a source of ventilation and provided oxygen to the ... : Supplement to: Schönfeld, Joachim; Zahn, Rainer; de Abreu, Lucia (2003): Surface to deep water response to rapid climate changes at the western Iberian Margin. Global and Planetary Change, 36(4), 237-264 ... |
format |
Article in Journal/Newspaper |
author |
Schönfeld, Joachim Zahn, Rainer de Abreu, Lucia |
author_facet |
Schönfeld, Joachim Zahn, Rainer de Abreu, Lucia |
author_sort |
Schönfeld, Joachim |
title |
Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ... |
title_short |
Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ... |
title_full |
Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ... |
title_fullStr |
Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ... |
title_full_unstemmed |
Stable isotope ratios and foraminiferal abundance of sediment cores from the Western Iberian Margin ... |
title_sort |
stable isotope ratios and foraminiferal abundance of sediment cores from the western iberian margin ... |
publisher |
PANGAEA |
publishDate |
2003 |
url |
https://dx.doi.org/10.1594/pangaea.733303 https://doi.pangaea.de/10.1594/PANGAEA.733303 |
genre |
Nordic Seas North Atlantic Sea ice |
genre_facet |
Nordic Seas North Atlantic Sea ice |
op_relation |
https://dx.doi.org/10.1016/s0921-8181(02)00197-2 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.73330310.1016/s0921-8181(02)00197-2 |
_version_ |
1795034709709815808 |