Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ...
Water exchange between the Black Sea and the Mediterranean Sea has been a major focus of the paleohydrography of the eastern Mediterranean. Glacial melt water released from the Black Sea is a potential factor in the formation of sapropel S1, an organic-rich sediment layer that accumulated during the...
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ftdatacite:10.1594/pangaea.736518 2024-09-15T18:31:04+00:00 Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ... Sperling, Michael R Schmiedl, Gerhard Hemleben, Christoph Emeis, Kay-Christian Erlenkeuser, Helmut Grootes, Pieter Meiert 2003 application/zip https://dx.doi.org/10.1594/pangaea.736518 https://doi.pangaea.de/10.1594/PANGAEA.736518 en eng PANGAEA https://dx.doi.org/10.1016/s0031-0182(02)00596-5 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Piston corer Meischner large M44/1 M44/3 Meteor 1986 Geosciences, University of Bremen GeoB Paleoceanography at Tübingen University GeoTü Southern European Seas Assessing and Modelling Ecosystem Changes SESAME article Collection Supplementary Publication Series of Datasets 2003 ftdatacite https://doi.org/10.1594/pangaea.73651810.1016/s0031-0182(02)00596-5 2024-07-03T13:10:33Z Water exchange between the Black Sea and the Mediterranean Sea has been a major focus of the paleohydrography of the eastern Mediterranean. Glacial melt water released from the Black Sea is a potential factor in the formation of sapropel S1, an organic-rich sediment layer that accumulated during the Early Holocene. A high-resolution study done on sediments from the Marmara Sea, the gateway between the Mediterranean and the Black Sea, sheds light on the Holocene exchange processes. Past sea surface temperature and sea surface salinity (SSS) were derived from stable oxygen isotope ratios (delta18O) of foraminiferal calcite and alkenone unsaturation ratios (Uk'37). Heavy delta18O values and high SSS in the Marmara Sea suggest absence of low salinity water from the Black Sea during S1. The comparison with data from the Levantine Basin and southern Aegean Sea outlines gradients of freshening in the eastern Mediterranean Sea, whereby the major sources of freshwater were closer to the Levantine Basin. It is thus ... : Supplement to: Sperling, Michael R; Schmiedl, Gerhard; Hemleben, Christoph; Emeis, Kay-Christian; Erlenkeuser, Helmut; Grootes, Pieter Meiert (2003): Black Sea impact on the formation of eastern Mediterranean sapropel S1? Evidence from the Marmara Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 190, 9-21 ... Article in Journal/Newspaper Planktonic foraminifera DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Piston corer Meischner large M44/1 M44/3 Meteor 1986 Geosciences, University of Bremen GeoB Paleoceanography at Tübingen University GeoTü Southern European Seas Assessing and Modelling Ecosystem Changes SESAME |
spellingShingle |
Piston corer Meischner large M44/1 M44/3 Meteor 1986 Geosciences, University of Bremen GeoB Paleoceanography at Tübingen University GeoTü Southern European Seas Assessing and Modelling Ecosystem Changes SESAME Sperling, Michael R Schmiedl, Gerhard Hemleben, Christoph Emeis, Kay-Christian Erlenkeuser, Helmut Grootes, Pieter Meiert Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ... |
topic_facet |
Piston corer Meischner large M44/1 M44/3 Meteor 1986 Geosciences, University of Bremen GeoB Paleoceanography at Tübingen University GeoTü Southern European Seas Assessing and Modelling Ecosystem Changes SESAME |
description |
Water exchange between the Black Sea and the Mediterranean Sea has been a major focus of the paleohydrography of the eastern Mediterranean. Glacial melt water released from the Black Sea is a potential factor in the formation of sapropel S1, an organic-rich sediment layer that accumulated during the Early Holocene. A high-resolution study done on sediments from the Marmara Sea, the gateway between the Mediterranean and the Black Sea, sheds light on the Holocene exchange processes. Past sea surface temperature and sea surface salinity (SSS) were derived from stable oxygen isotope ratios (delta18O) of foraminiferal calcite and alkenone unsaturation ratios (Uk'37). Heavy delta18O values and high SSS in the Marmara Sea suggest absence of low salinity water from the Black Sea during S1. The comparison with data from the Levantine Basin and southern Aegean Sea outlines gradients of freshening in the eastern Mediterranean Sea, whereby the major sources of freshwater were closer to the Levantine Basin. It is thus ... : Supplement to: Sperling, Michael R; Schmiedl, Gerhard; Hemleben, Christoph; Emeis, Kay-Christian; Erlenkeuser, Helmut; Grootes, Pieter Meiert (2003): Black Sea impact on the formation of eastern Mediterranean sapropel S1? Evidence from the Marmara Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 190, 9-21 ... |
format |
Article in Journal/Newspaper |
author |
Sperling, Michael R Schmiedl, Gerhard Hemleben, Christoph Emeis, Kay-Christian Erlenkeuser, Helmut Grootes, Pieter Meiert |
author_facet |
Sperling, Michael R Schmiedl, Gerhard Hemleben, Christoph Emeis, Kay-Christian Erlenkeuser, Helmut Grootes, Pieter Meiert |
author_sort |
Sperling, Michael R |
title |
Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ... |
title_short |
Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ... |
title_full |
Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ... |
title_fullStr |
Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ... |
title_full_unstemmed |
Planktonic foraminifera and sea surface temperature reconstruction of sediments from the Mediterranean Sea ... |
title_sort |
planktonic foraminifera and sea surface temperature reconstruction of sediments from the mediterranean sea ... |
publisher |
PANGAEA |
publishDate |
2003 |
url |
https://dx.doi.org/10.1594/pangaea.736518 https://doi.pangaea.de/10.1594/PANGAEA.736518 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1016/s0031-0182(02)00596-5 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.73651810.1016/s0031-0182(02)00596-5 |
_version_ |
1810472661056225280 |