Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP
The so-called 8.2 ka event represents one of the most prominent cold climate anomalies during the Holocene warm period. Accordingly, several studies have addressed its trigger mechanisms, absolute dating and regional characteristics so far. However, knowledge about subsequent climate recovery is sti...
Main Authors: | , , , , , , , , , , , , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2017
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.880316 https://doi.org/10.1594/PANGAEA.880316 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.880316 |
---|---|
record_format |
openpolar |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.880316 2024-09-15T18:23:50+00:00 Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP Andersen, Nils Lauterbach, Stefan Erlenkeuser, Helmut Danielopol, Dan L Namiotko, Tadeusz Hüls, Matthias Belmecheri, Soumaya Dulski, Peter Nantke, Carla Meyer, Hanno Chapligin, Bernhard von Grafenstein, Ulrich Brauer, Achim LATITUDE: 47.811400 * LONGITUDE: 13.402500 * MINIMUM DEPTH, sediment/rock: 8.960 m * MAXIMUM DEPTH, sediment/rock: 9.690 m 2017 text/tab-separated-values, 441 data points https://doi.pangaea.de/10.1594/PANGAEA.880316 https://doi.org/10.1594/PANGAEA.880316 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.880316 https://doi.org/10.1594/PANGAEA.880316 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Andersen, Nils; Lauterbach, Stefan; Erlenkeuser, Helmut; Danielopol, Dan L; Namiotko, Tadeusz; Hüls, Matthias; Belmecheri, Soumaya; Dulski, Peter; Nantke, Carla; Meyer, Hanno; Chapligin, Bernhard; von Grafenstein, Ulrich; Brauer, Achim (2017): Evidence for higher-than-average air temperatures after the 8.2 ka event provided by a Central European d18O record. Quaternary Science Reviews, 172, 96-108, https://doi.org/10.1016/j.quascirev.2017.08.001 AGE AWI_Envi DEPTH sediment/rock Lake Mondsee European Alps Mo05 Ostracoda δ18O PCUWI Piston corer UWITEC Polar Terrestrial Environmental Systems @ AWI Reconstructed Varve age water dataset 2017 ftpangaea https://doi.org/10.1594/PANGAEA.88031610.1016/j.quascirev.2017.08.001 2024-07-24T02:31:33Z The so-called 8.2 ka event represents one of the most prominent cold climate anomalies during the Holocene warm period. Accordingly, several studies have addressed its trigger mechanisms, absolute dating and regional characteristics so far. However, knowledge about subsequent climate recovery is still limited although this might be essential for the understanding of rapid climatic changes. Here we present a new sub-decadally resolved and precisely dated oxygen isotope (d18O) record for the interval between 7.7 and 8.7 ka BP, derived from the calcareous valves of benthic ostracods preserved in the varved lake sediments of pre-Alpine Mondsee (Austria). Besides a clear reflection of the 8.2 ka event, showing a good agreement in timing, duration and magnitude with other regional stable isotope records, the high-resolution Mondsee lake sediment record provides evidence for a 75-year-long interval of higher-than-average d18O values directly after the 8.2 ka event, possibly reflecting increased air temperatures in Central Europe. This observation is consistent with evidence from other proxy records in the North Atlantic realm, thus most probably reflecting a hemispheric-scale climate signal rather than a local phenomenon. As a possible trigger we suggest an enhanced resumption of the Atlantic meridional overturning circulation (AMOC), supporting assumptions from climate model simulations. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(13.402500,13.402500,47.811400,47.811400) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AGE AWI_Envi DEPTH sediment/rock Lake Mondsee European Alps Mo05 Ostracoda δ18O PCUWI Piston corer UWITEC Polar Terrestrial Environmental Systems @ AWI Reconstructed Varve age water |
spellingShingle |
AGE AWI_Envi DEPTH sediment/rock Lake Mondsee European Alps Mo05 Ostracoda δ18O PCUWI Piston corer UWITEC Polar Terrestrial Environmental Systems @ AWI Reconstructed Varve age water Andersen, Nils Lauterbach, Stefan Erlenkeuser, Helmut Danielopol, Dan L Namiotko, Tadeusz Hüls, Matthias Belmecheri, Soumaya Dulski, Peter Nantke, Carla Meyer, Hanno Chapligin, Bernhard von Grafenstein, Ulrich Brauer, Achim Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP |
topic_facet |
AGE AWI_Envi DEPTH sediment/rock Lake Mondsee European Alps Mo05 Ostracoda δ18O PCUWI Piston corer UWITEC Polar Terrestrial Environmental Systems @ AWI Reconstructed Varve age water |
description |
The so-called 8.2 ka event represents one of the most prominent cold climate anomalies during the Holocene warm period. Accordingly, several studies have addressed its trigger mechanisms, absolute dating and regional characteristics so far. However, knowledge about subsequent climate recovery is still limited although this might be essential for the understanding of rapid climatic changes. Here we present a new sub-decadally resolved and precisely dated oxygen isotope (d18O) record for the interval between 7.7 and 8.7 ka BP, derived from the calcareous valves of benthic ostracods preserved in the varved lake sediments of pre-Alpine Mondsee (Austria). Besides a clear reflection of the 8.2 ka event, showing a good agreement in timing, duration and magnitude with other regional stable isotope records, the high-resolution Mondsee lake sediment record provides evidence for a 75-year-long interval of higher-than-average d18O values directly after the 8.2 ka event, possibly reflecting increased air temperatures in Central Europe. This observation is consistent with evidence from other proxy records in the North Atlantic realm, thus most probably reflecting a hemispheric-scale climate signal rather than a local phenomenon. As a possible trigger we suggest an enhanced resumption of the Atlantic meridional overturning circulation (AMOC), supporting assumptions from climate model simulations. |
format |
Dataset |
author |
Andersen, Nils Lauterbach, Stefan Erlenkeuser, Helmut Danielopol, Dan L Namiotko, Tadeusz Hüls, Matthias Belmecheri, Soumaya Dulski, Peter Nantke, Carla Meyer, Hanno Chapligin, Bernhard von Grafenstein, Ulrich Brauer, Achim |
author_facet |
Andersen, Nils Lauterbach, Stefan Erlenkeuser, Helmut Danielopol, Dan L Namiotko, Tadeusz Hüls, Matthias Belmecheri, Soumaya Dulski, Peter Nantke, Carla Meyer, Hanno Chapligin, Bernhard von Grafenstein, Ulrich Brauer, Achim |
author_sort |
Andersen, Nils |
title |
Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP |
title_short |
Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP |
title_full |
Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP |
title_fullStr |
Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP |
title_full_unstemmed |
Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP |
title_sort |
oxygen isotope (δ¹⁸o) values of benthic ostracods from varved sediments from mondsee (austria) for the interval 7.7-8.7 ka bp |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.880316 https://doi.org/10.1594/PANGAEA.880316 |
op_coverage |
LATITUDE: 47.811400 * LONGITUDE: 13.402500 * MINIMUM DEPTH, sediment/rock: 8.960 m * MAXIMUM DEPTH, sediment/rock: 9.690 m |
long_lat |
ENVELOPE(13.402500,13.402500,47.811400,47.811400) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Andersen, Nils; Lauterbach, Stefan; Erlenkeuser, Helmut; Danielopol, Dan L; Namiotko, Tadeusz; Hüls, Matthias; Belmecheri, Soumaya; Dulski, Peter; Nantke, Carla; Meyer, Hanno; Chapligin, Bernhard; von Grafenstein, Ulrich; Brauer, Achim (2017): Evidence for higher-than-average air temperatures after the 8.2 ka event provided by a Central European d18O record. Quaternary Science Reviews, 172, 96-108, https://doi.org/10.1016/j.quascirev.2017.08.001 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.880316 https://doi.org/10.1594/PANGAEA.880316 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.88031610.1016/j.quascirev.2017.08.001 |
_version_ |
1810464107650875392 |