Mediterranean faunal evolution and biochronological events during the last 24 kyr
We generated high-resolution biochronological records in the Mediterranean Sea covering the period extending to the Late-glacial. The present study is based on micropaleontological, sea-surface temperature (SST) and oxygen isotopic analyses performed along three well-dated deep-sea cores: REC13–53,...
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ftarchimer:oai:archimer.ifremer.fr:80342 2023-05-15T16:29:20+02:00 Mediterranean faunal evolution and biochronological events during the last 24 kyr Zouari, Sonda Boussetta, Soumaya Siani, Giuseppe Tisnerat-laborde, Nadine Thil, François Kallel, Abdelaziz Michel, Elisabeth Kallel, Nejib 2021-05 application/pdf https://archimer.ifremer.fr/doc/00691/80342/83427.pdf https://doi.org/10.1016/j.marmicro.2021.101997 https://archimer.ifremer.fr/doc/00691/80342/ eng eng Elsevier BV https://archimer.ifremer.fr/doc/00691/80342/83427.pdf doi:10.1016/j.marmicro.2021.101997 https://archimer.ifremer.fr/doc/00691/80342/ info:eu-repo/semantics/openAccess restricted use Marine Micropaleontology (0377-8398) (Elsevier BV), 2021-05 , Vol. 165 , P. 101997 (16p.) Mediterranean Sea Planktonic foraminifera SST LGM Bio-event AMS(14)C text Publication info:eu-repo/semantics/article 2021 ftarchimer https://doi.org/10.1016/j.marmicro.2021.101997 2022-05-03T22:50:02Z We generated high-resolution biochronological records in the Mediterranean Sea covering the period extending to the Late-glacial. The present study is based on micropaleontological, sea-surface temperature (SST) and oxygen isotopic analyses performed along three well-dated deep-sea cores: REC13–53, KET80–19 and MD84–641 recovered in the Siculo-Tunisian Strait, Tyrrhenian Sea and Levantine Basin, respectively. The quantitative distributional patterns of planktic foraminifera permitted to identify seven biozones based on the apparition and/or disappearance of the main specific taxa or by their noticeable abundance peaks. Abundance records display that major changes in planktic foraminiferal assemblages have a similar pattern mainly in central and western basins. In particular, four recognized bio-events can be used to establish or to improve the chronology of Mediterranean deep-sea cores. The comparison of the SST estimates and foraminiferal records with those of NGRIP ice-core shows a similarity between the Greenland climate and the Mediterranean hydrology. This indicates that the main climate changes recorded in the North Atlantic are globally in phase with those observed in the Mediterranean region. Article in Journal/Newspaper Greenland ice core NGRIP North Atlantic Planktonic foraminifera Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Greenland Marine Micropaleontology 165 101997 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
Mediterranean Sea Planktonic foraminifera SST LGM Bio-event AMS(14)C |
spellingShingle |
Mediterranean Sea Planktonic foraminifera SST LGM Bio-event AMS(14)C Zouari, Sonda Boussetta, Soumaya Siani, Giuseppe Tisnerat-laborde, Nadine Thil, François Kallel, Abdelaziz Michel, Elisabeth Kallel, Nejib Mediterranean faunal evolution and biochronological events during the last 24 kyr |
topic_facet |
Mediterranean Sea Planktonic foraminifera SST LGM Bio-event AMS(14)C |
description |
We generated high-resolution biochronological records in the Mediterranean Sea covering the period extending to the Late-glacial. The present study is based on micropaleontological, sea-surface temperature (SST) and oxygen isotopic analyses performed along three well-dated deep-sea cores: REC13–53, KET80–19 and MD84–641 recovered in the Siculo-Tunisian Strait, Tyrrhenian Sea and Levantine Basin, respectively. The quantitative distributional patterns of planktic foraminifera permitted to identify seven biozones based on the apparition and/or disappearance of the main specific taxa or by their noticeable abundance peaks. Abundance records display that major changes in planktic foraminiferal assemblages have a similar pattern mainly in central and western basins. In particular, four recognized bio-events can be used to establish or to improve the chronology of Mediterranean deep-sea cores. The comparison of the SST estimates and foraminiferal records with those of NGRIP ice-core shows a similarity between the Greenland climate and the Mediterranean hydrology. This indicates that the main climate changes recorded in the North Atlantic are globally in phase with those observed in the Mediterranean region. |
format |
Article in Journal/Newspaper |
author |
Zouari, Sonda Boussetta, Soumaya Siani, Giuseppe Tisnerat-laborde, Nadine Thil, François Kallel, Abdelaziz Michel, Elisabeth Kallel, Nejib |
author_facet |
Zouari, Sonda Boussetta, Soumaya Siani, Giuseppe Tisnerat-laborde, Nadine Thil, François Kallel, Abdelaziz Michel, Elisabeth Kallel, Nejib |
author_sort |
Zouari, Sonda |
title |
Mediterranean faunal evolution and biochronological events during the last 24 kyr |
title_short |
Mediterranean faunal evolution and biochronological events during the last 24 kyr |
title_full |
Mediterranean faunal evolution and biochronological events during the last 24 kyr |
title_fullStr |
Mediterranean faunal evolution and biochronological events during the last 24 kyr |
title_full_unstemmed |
Mediterranean faunal evolution and biochronological events during the last 24 kyr |
title_sort |
mediterranean faunal evolution and biochronological events during the last 24 kyr |
publisher |
Elsevier BV |
publishDate |
2021 |
url |
https://archimer.ifremer.fr/doc/00691/80342/83427.pdf https://doi.org/10.1016/j.marmicro.2021.101997 https://archimer.ifremer.fr/doc/00691/80342/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland ice core NGRIP North Atlantic Planktonic foraminifera |
genre_facet |
Greenland ice core NGRIP North Atlantic Planktonic foraminifera |
op_source |
Marine Micropaleontology (0377-8398) (Elsevier BV), 2021-05 , Vol. 165 , P. 101997 (16p.) |
op_relation |
https://archimer.ifremer.fr/doc/00691/80342/83427.pdf doi:10.1016/j.marmicro.2021.101997 https://archimer.ifremer.fr/doc/00691/80342/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1016/j.marmicro.2021.101997 |
container_title |
Marine Micropaleontology |
container_volume |
165 |
container_start_page |
101997 |
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1766019024794157056 |