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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Main Author: Wegwerth, Antje
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.906161
https://doi.pangaea.de/10.1594/PANGAEA.906161
id ftdatacite:10.1594/pangaea.906161
record_format openpolar
spelling 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
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