Please use this identifier to cite or link to this item:
http://doi.org/10.25358/openscience-7072
Full metadata record
DC Field | Value | Language |
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dc.contributor.author | Budsky, Alexander | - |
dc.contributor.author | Wassenburg, Jasper A. | - |
dc.contributor.author | Mertz-Kraus, Regina | - |
dc.contributor.author | Spötl, Christoph | - |
dc.contributor.author | Jochum, Klaus Peter | - |
dc.contributor.author | Gibert, Luis | - |
dc.contributor.author | Scholz, Denis | - |
dc.date.accessioned | 2022-06-02T08:11:59Z | - |
dc.date.available | 2022-06-02T08:11:59Z | - |
dc.date.issued | 2019 | - |
dc.identifier.uri | https://openscience.ub.uni-mainz.de/handle/20.500.12030/7086 | - |
dc.description.abstract | The climate of the western Mediterranean was characterized by a strong precipitation gradient during the Holocene driven by atmospheric circulation patterns. The scarcity of terrestrial paleoclimate archives has precluded exploring this hydroclimate pattern during Marine Isotope Stages 5 to 3. Here we present stable carbon and oxygen isotope records from three flowstones from southeast Iberia, which show that Dansgaard/Oeschger events were associated with more humid conditions. This is in agreement with other records from the Iberian Peninsula, the Mediterranean, and western Europe, which all responded in a similar way to millennial-scale climate variability in Greenland. This general increase in precipitation during Dansgaard/Oeschger events cannot be explained by any present-day or Holocene winter atmospheric circulation pattern. Instead, we suggest that changes in sea surface temperature played a dominant role in determining precipitation amounts in the western Mediterranean. | en_GB |
dc.language.iso | eng | de |
dc.rights | CC BY | * |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | * |
dc.subject.ddc | 550 Geowissenschaften | de_DE |
dc.subject.ddc | 550 Earth sciences | en_GB |
dc.title | Western Mediterranean climate response to Dansgaard/Oeschger events : new insights from speleothem records | en_GB |
dc.type | Zeitschriftenaufsatz | de |
dc.identifier.doi | http://doi.org/10.25358/openscience-7072 | - |
jgu.type.dinitype | article | en_GB |
jgu.type.version | Published version | de |
jgu.type.resource | Text | de |
jgu.organisation.department | FB 09 Chemie, Pharmazie u. Geowissensch. | de |
jgu.organisation.number | 7950 | - |
jgu.organisation.name | Johannes Gutenberg-Universität Mainz | - |
jgu.rights.accessrights | openAccess | - |
jgu.journal.title | Geophysical research letters | de |
jgu.journal.volume | 46 | de |
jgu.journal.issue | 15 | de |
jgu.pages.start | 9042 | de |
jgu.pages.end | 9053 | de |
jgu.publisher.year | 2019 | - |
jgu.publisher.name | Wiley | de |
jgu.publisher.place | Hoboken, NJ | de |
jgu.publisher.issn | 1944-8007 | de |
jgu.organisation.place | Mainz | - |
jgu.subject.ddccode | 550 | de |
jgu.publisher.doi | 10.1029/2019GL084009 | de |
jgu.organisation.ror | https://ror.org/023b0x485 | |
Appears in collections: | JGU-Publikationen |
Files in This Item:
File | Description | Size | Format | ||
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western_mediterranean_climate-20220602100329003.pdf | 2.03 MB | Adobe PDF | View/Open |