Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz
Core MVSEIS08-TG-2 was acquired during the Euromargin-MVSEIS08 cruise on the Moroccan margin, south of the Gulf of Cadiz. This site was targeted to discuss the possibility of the saline upper branch of the Mediterranean Outflow Water (MOW) diverging southwards along the Moroccan margin, in addition...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.966606 2024-09-15T18:31:02+00:00 Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel LATITUDE: 34.971330 * LONGITUDE: -6.841170 2024 application/zip, 9 datasets https://doi.pangaea.de/10.1594/PANGAEA.966606 https://doi.org/10.1594/PANGAEA.966606 en eng PANGAEA Lebreiro, Susana Martin; Antón López, Laura; Reguera, Maria Isabel; Marzocchi, Alice (2018): Paleoceanographic and climatic implications of a new Mediterranean Outflow branch in the southern Gulf of Cadiz. Quaternary Science Reviews, 197, 92-111, https://doi.org/10.1016/j.quascirev.2018.07.036 https://doi.pangaea.de/10.1594/PANGAEA.966606 https://doi.org/10.1594/PANGAEA.966606 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess contourites Gulf of Cadiz Heinrich Event 1 Mediterranean outflow MOW sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas dataset bundled publication 2024 ftpangaea https://doi.org/10.1594/PANGAEA.96660610.1016/j.quascirev.2018.07.036 2024-07-24T02:31:21Z Core MVSEIS08-TG-2 was acquired during the Euromargin-MVSEIS08 cruise on the Moroccan margin, south of the Gulf of Cadiz. This site was targeted to discuss the possibility of the saline upper branch of the Mediterranean Outflow Water (MOW) diverging southwards along the Moroccan margin, in addition to the well-established northern MOW current. The southern TG-2 is a 2.12 m gravity core. Contourite records cover the time interval from the last deglaciation starting at HS1 (18.6 ka) to the Holocene. New datasets of current velocity (sortable silt) and water mass origin (O and C isotopes of benthic foraminifera) define the intensity of the MOW as contourite deposits, together with element ratios (XRF-scan) and physical properties of the sediment. O and C isotopes of planktonic foraminifera, foraminiferal species and sea surface temperature (simmax.28 transfer function) were used to determine millennial climate changes during the last deglaciation. Other/Unknown Material Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-6.841170,-6.841170,34.971330,34.971330) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
contourites Gulf of Cadiz Heinrich Event 1 Mediterranean outflow MOW sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas |
spellingShingle |
contourites Gulf of Cadiz Heinrich Event 1 Mediterranean outflow MOW sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz |
topic_facet |
contourites Gulf of Cadiz Heinrich Event 1 Mediterranean outflow MOW sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas |
description |
Core MVSEIS08-TG-2 was acquired during the Euromargin-MVSEIS08 cruise on the Moroccan margin, south of the Gulf of Cadiz. This site was targeted to discuss the possibility of the saline upper branch of the Mediterranean Outflow Water (MOW) diverging southwards along the Moroccan margin, in addition to the well-established northern MOW current. The southern TG-2 is a 2.12 m gravity core. Contourite records cover the time interval from the last deglaciation starting at HS1 (18.6 ka) to the Holocene. New datasets of current velocity (sortable silt) and water mass origin (O and C isotopes of benthic foraminifera) define the intensity of the MOW as contourite deposits, together with element ratios (XRF-scan) and physical properties of the sediment. O and C isotopes of planktonic foraminifera, foraminiferal species and sea surface temperature (simmax.28 transfer function) were used to determine millennial climate changes during the last deglaciation. |
format |
Other/Unknown Material |
author |
Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel |
author_facet |
Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel |
author_sort |
Lebreiro, Susana Martin |
title |
Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz |
title_short |
Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz |
title_full |
Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz |
title_fullStr |
Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz |
title_full_unstemmed |
Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz |
title_sort |
analysis of a sediment core mvseis08_tg-2 taken during the mvseis2008 expedition in gulf of cadiz |
publisher |
PANGAEA |
publishDate |
2024 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.966606 https://doi.org/10.1594/PANGAEA.966606 |
op_coverage |
LATITUDE: 34.971330 * LONGITUDE: -6.841170 |
long_lat |
ENVELOPE(-6.841170,-6.841170,34.971330,34.971330) |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
Lebreiro, Susana Martin; Antón López, Laura; Reguera, Maria Isabel; Marzocchi, Alice (2018): Paleoceanographic and climatic implications of a new Mediterranean Outflow branch in the southern Gulf of Cadiz. Quaternary Science Reviews, 197, 92-111, https://doi.org/10.1016/j.quascirev.2018.07.036 https://doi.pangaea.de/10.1594/PANGAEA.966606 https://doi.org/10.1594/PANGAEA.966606 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.96660610.1016/j.quascirev.2018.07.036 |
_version_ |
1810472618587848704 |