The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater
International audience This paper provides new data on the evolution of the Caspian Sea and Black Sea from the Last Glacial Maximum until ca. 12 cal kyr BP. We present new analyses (clay mineralogy, grain-size, Nd isotopes and pollen) applied to sediments from the river terraces in the lower Volga,...
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Online Access: | https://insu.hal.science/insu-03745248 https://insu.hal.science/insu-03745248/document https://insu.hal.science/insu-03745248/file/1-s2.0-S027737911630227X-main.pdf https://doi.org/10.1016/j.quascirev.2016.06.019 |
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ftinsu:oai:HAL:insu-03745248v1 2024-04-21T08:05:02+00:00 The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater Tudryn, Alina Leroy, Suzanne A. G. Toucanne, Samuel Gibert-Brunet, Elisabeth Tucholka, Piotr Lavrushin, Yuri A. Dufaure, Olivier Miska, Serge Bayon, Germain Géosciences Paris Sud (GEOPS) Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS) Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) 2016 https://insu.hal.science/insu-03745248 https://insu.hal.science/insu-03745248/document https://insu.hal.science/insu-03745248/file/1-s2.0-S027737911630227X-main.pdf https://doi.org/10.1016/j.quascirev.2016.06.019 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2016.06.019 insu-03745248 https://insu.hal.science/insu-03745248 https://insu.hal.science/insu-03745248/document https://insu.hal.science/insu-03745248/file/1-s2.0-S027737911630227X-main.pdf BIBCODE: 2016QSRv.148.29T doi:10.1016/j.quascirev.2016.06.019 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://insu.hal.science/insu-03745248 Quaternary Science Reviews, 2016, 148, pp.29-43. ⟨10.1016/j.quascirev.2016.06.019⟩ Caspian sea Black sea SIS deglaciation Early Khvalynian transgression Chocolate clays Red layers Clay minerals Neodymium isotopes Pollen Late Pleistocene [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2016 ftinsu https://doi.org/10.1016/j.quascirev.2016.06.019 2024-04-05T00:31:43Z International audience This paper provides new data on the evolution of the Caspian Sea and Black Sea from the Last Glacial Maximum until ca. 12 cal kyr BP. We present new analyses (clay mineralogy, grain-size, Nd isotopes and pollen) applied to sediments from the river terraces in the lower Volga, from the middle Caspian Sea and from the western part of the Black Sea. The results show that during the last deglaciation, the Ponto-Caspian basin collected meltwater and fine-grained sediment from the southern margin of the Scandinavian Ice Sheet (SIS) via the Dniepr and Volga Rivers. It induced the deposition of characteristic red-brownish/chocolate-coloured illite-rich sediments (Red Layers in the Black Sea and Chocolate Clays in the Caspian Sea) that originated from the Baltic Shield area according to Nd data. This general evolution, common to both seas was nevertheless differentiated over time due to the specificities of their catchment areas and due to the movement of the southern margin of the SIS. Our results indicate that in the eastern part of the East European Plain, the meltwater from the SIS margin supplied the Caspian Sea during the deglaciation until ∼13.8 cal kyr BP, and possibly from the LGM. That led to the Early Khvalynian transgressive stage(s) and Chocolate Clays deposition in the now-emerged northern flat part of the Caspian Sea (river terraces in the modern lower Volga) and in its middle basin. In the western part of the East European Plain, our results confirm the release of meltwater from the SIS margin into the Black Sea that occurred between 17.2 and 15.7 cal kyr BP, as previously proposed. Indeed, recent findings concerning the evolution of the southern margin of the SIS and the Black Sea, show that during the last deglaciation, occurred a westward release of meltwater into the North Atlantic (between ca. 20 and 16.7 cal kyr BP), and a southward one into the Black Sea (between 17.2 and 15.7 cal kyr BP). After the Red Layers/Chocolate Clays deposition in both seas and until 12 cal kyr BP, ... Article in Journal/Newspaper Ice Sheet North Atlantic Institut national des sciences de l'Univers: HAL-INSU Quaternary Science Reviews 148 29 43 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
Caspian sea Black sea SIS deglaciation Early Khvalynian transgression Chocolate clays Red layers Clay minerals Neodymium isotopes Pollen Late Pleistocene [SDU]Sciences of the Universe [physics] |
spellingShingle |
Caspian sea Black sea SIS deglaciation Early Khvalynian transgression Chocolate clays Red layers Clay minerals Neodymium isotopes Pollen Late Pleistocene [SDU]Sciences of the Universe [physics] Tudryn, Alina Leroy, Suzanne A. G. Toucanne, Samuel Gibert-Brunet, Elisabeth Tucholka, Piotr Lavrushin, Yuri A. Dufaure, Olivier Miska, Serge Bayon, Germain The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater |
topic_facet |
Caspian sea Black sea SIS deglaciation Early Khvalynian transgression Chocolate clays Red layers Clay minerals Neodymium isotopes Pollen Late Pleistocene [SDU]Sciences of the Universe [physics] |
description |
International audience This paper provides new data on the evolution of the Caspian Sea and Black Sea from the Last Glacial Maximum until ca. 12 cal kyr BP. We present new analyses (clay mineralogy, grain-size, Nd isotopes and pollen) applied to sediments from the river terraces in the lower Volga, from the middle Caspian Sea and from the western part of the Black Sea. The results show that during the last deglaciation, the Ponto-Caspian basin collected meltwater and fine-grained sediment from the southern margin of the Scandinavian Ice Sheet (SIS) via the Dniepr and Volga Rivers. It induced the deposition of characteristic red-brownish/chocolate-coloured illite-rich sediments (Red Layers in the Black Sea and Chocolate Clays in the Caspian Sea) that originated from the Baltic Shield area according to Nd data. This general evolution, common to both seas was nevertheless differentiated over time due to the specificities of their catchment areas and due to the movement of the southern margin of the SIS. Our results indicate that in the eastern part of the East European Plain, the meltwater from the SIS margin supplied the Caspian Sea during the deglaciation until ∼13.8 cal kyr BP, and possibly from the LGM. That led to the Early Khvalynian transgressive stage(s) and Chocolate Clays deposition in the now-emerged northern flat part of the Caspian Sea (river terraces in the modern lower Volga) and in its middle basin. In the western part of the East European Plain, our results confirm the release of meltwater from the SIS margin into the Black Sea that occurred between 17.2 and 15.7 cal kyr BP, as previously proposed. Indeed, recent findings concerning the evolution of the southern margin of the SIS and the Black Sea, show that during the last deglaciation, occurred a westward release of meltwater into the North Atlantic (between ca. 20 and 16.7 cal kyr BP), and a southward one into the Black Sea (between 17.2 and 15.7 cal kyr BP). After the Red Layers/Chocolate Clays deposition in both seas and until 12 cal kyr BP, ... |
author2 |
Géosciences Paris Sud (GEOPS) Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS) Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) |
format |
Article in Journal/Newspaper |
author |
Tudryn, Alina Leroy, Suzanne A. G. Toucanne, Samuel Gibert-Brunet, Elisabeth Tucholka, Piotr Lavrushin, Yuri A. Dufaure, Olivier Miska, Serge Bayon, Germain |
author_facet |
Tudryn, Alina Leroy, Suzanne A. G. Toucanne, Samuel Gibert-Brunet, Elisabeth Tucholka, Piotr Lavrushin, Yuri A. Dufaure, Olivier Miska, Serge Bayon, Germain |
author_sort |
Tudryn, Alina |
title |
The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater |
title_short |
The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater |
title_full |
The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater |
title_fullStr |
The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater |
title_full_unstemmed |
The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater |
title_sort |
ponto-caspian basin as a final trap for southeastern scandinavian ice-sheet meltwater |
publisher |
HAL CCSD |
publishDate |
2016 |
url |
https://insu.hal.science/insu-03745248 https://insu.hal.science/insu-03745248/document https://insu.hal.science/insu-03745248/file/1-s2.0-S027737911630227X-main.pdf https://doi.org/10.1016/j.quascirev.2016.06.019 |
genre |
Ice Sheet North Atlantic |
genre_facet |
Ice Sheet North Atlantic |
op_source |
ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://insu.hal.science/insu-03745248 Quaternary Science Reviews, 2016, 148, pp.29-43. ⟨10.1016/j.quascirev.2016.06.019⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2016.06.019 insu-03745248 https://insu.hal.science/insu-03745248 https://insu.hal.science/insu-03745248/document https://insu.hal.science/insu-03745248/file/1-s2.0-S027737911630227X-main.pdf BIBCODE: 2016QSRv.148.29T doi:10.1016/j.quascirev.2016.06.019 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2016.06.019 |
container_title |
Quaternary Science Reviews |
container_volume |
148 |
container_start_page |
29 |
op_container_end_page |
43 |
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1796944581452890112 |