Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ...
The Saalian was one of the largest glaciations during the Quaternary with an ice sheet extending considerably wider into the Eurasian continent than during other glacials. Orbital variations caused the ice sheet to switch between growing and shrinking. The partial retreat of the ice sheet and meltwa...
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ftdatacite:10.1594/pangaea.906161 2024-09-15T18:12:13+00:00 Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ... Wegwerth, Antje 2019 application/zip https://dx.doi.org/10.1594/pangaea.906161 https://doi.pangaea.de/10.1594/PANGAEA.906161 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2019.07.008 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 87Sr/86Srostracods Black Sea "Lake" d18Oostracods Eurasia Meltwater MIS 6 palaeohydrology Pleistocene Radiogenic isotopes Saalian glaciation Tephra article Collection Supplementary Publication Series of Datasets 2019 ftdatacite https://doi.org/10.1594/pangaea.90616110.1016/j.quascirev.2019.07.008 2024-08-01T10:55:41Z The Saalian was one of the largest glaciations during the Quaternary with an ice sheet extending considerably wider into the Eurasian continent than during other glacials. Orbital variations caused the ice sheet to switch between growing and shrinking. The partial retreat of the ice sheet and meltwater discharge resulted in global sea-level rise and increased lake levels of inland seas with broader environmental implications. During Marine Isotope Stage 6 (MIS 6), meltwater entered the formerly enclosed Black Sea at least twice as documented in a d18O record from Anatolian speleothems. Here we present a sedimentary record from the Black Sea "Lake" covering MIS 6 and provide evidence for three meltwater periods coinciding with insolation maxima (BSWP-6-1: 180-167 ka BP, BSWP-6-2: 160-145 ka BP, BSWPII: 133-130 ka BP). While d18Oostracods and Sr/Caostracods point to pronounced meltwater supply and decreasing salinity, 87Sr/86Srostracods shed light on meltwater sources and pathways. During all three periods, ... : Supplement to: Wegwerth, Antje; Dellwig, Olaf; Wulf, Sabine; Plessen, Birgit; Kleinhanns, Ilka C; Nowaczyk, Norbert R; Jiabo, Liu; Arz, Helge Wolfgang (2019): Major hydrological shifts in the Black Sea “Lake” in response to ice sheet collapses during MIS 6 (130–184 ka BP). Quaternary Science Reviews, 219, 126-144 ... Article in Journal/Newspaper Ice Sheet DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
87Sr/86Srostracods Black Sea "Lake" d18Oostracods Eurasia Meltwater MIS 6 palaeohydrology Pleistocene Radiogenic isotopes Saalian glaciation Tephra |
spellingShingle |
87Sr/86Srostracods Black Sea "Lake" d18Oostracods Eurasia Meltwater MIS 6 palaeohydrology Pleistocene Radiogenic isotopes Saalian glaciation Tephra Wegwerth, Antje Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ... |
topic_facet |
87Sr/86Srostracods Black Sea "Lake" d18Oostracods Eurasia Meltwater MIS 6 palaeohydrology Pleistocene Radiogenic isotopes Saalian glaciation Tephra |
description |
The Saalian was one of the largest glaciations during the Quaternary with an ice sheet extending considerably wider into the Eurasian continent than during other glacials. Orbital variations caused the ice sheet to switch between growing and shrinking. The partial retreat of the ice sheet and meltwater discharge resulted in global sea-level rise and increased lake levels of inland seas with broader environmental implications. During Marine Isotope Stage 6 (MIS 6), meltwater entered the formerly enclosed Black Sea at least twice as documented in a d18O record from Anatolian speleothems. Here we present a sedimentary record from the Black Sea "Lake" covering MIS 6 and provide evidence for three meltwater periods coinciding with insolation maxima (BSWP-6-1: 180-167 ka BP, BSWP-6-2: 160-145 ka BP, BSWPII: 133-130 ka BP). While d18Oostracods and Sr/Caostracods point to pronounced meltwater supply and decreasing salinity, 87Sr/86Srostracods shed light on meltwater sources and pathways. During all three periods, ... : Supplement to: Wegwerth, Antje; Dellwig, Olaf; Wulf, Sabine; Plessen, Birgit; Kleinhanns, Ilka C; Nowaczyk, Norbert R; Jiabo, Liu; Arz, Helge Wolfgang (2019): Major hydrological shifts in the Black Sea “Lake” in response to ice sheet collapses during MIS 6 (130–184 ka BP). Quaternary Science Reviews, 219, 126-144 ... |
format |
Article in Journal/Newspaper |
author |
Wegwerth, Antje |
author_facet |
Wegwerth, Antje |
author_sort |
Wegwerth, Antje |
title |
Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ... |
title_short |
Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ... |
title_full |
Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ... |
title_fullStr |
Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ... |
title_full_unstemmed |
Proxy data of Black Sea cores covering MIS 6 (184-130 ka BP) ... |
title_sort |
proxy data of black sea cores covering mis 6 (184-130 ka bp) ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.906161 https://doi.pangaea.de/10.1594/PANGAEA.906161 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2019.07.008 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.90616110.1016/j.quascirev.2019.07.008 |
_version_ |
1810449797510856704 |