Physical properties and fine fraction from loess at Rasova/Lower Danube
In this study we provide a correlative age model for last glacial loess at the Rasova-Valea cu Pietre site in the Lower Danube region, based on the correlation of palaeoenvironmental proxies to independently dated palaeoclimate archives, luminescence dating and independent age control provided by th...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.870532 2023-05-15T16:29:27+02:00 Physical properties and fine fraction from loess at Rasova/Lower Danube Zeeden, Christian Hambach, Ulrich Veres, Daniel Fitzsimmons, Kathryn E Obreht, Igor Bösken, Janina Lehmkuhl, Frank LATITUDE: 44.254250 * LONGITUDE: 27.951470 2016-01-09 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.870532 https://doi.org/10.1594/PANGAEA.870532 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.870532 https://doi.org/10.1594/PANGAEA.870532 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Zeeden, Christian; Hambach, Ulrich; Veres, Daniel; Fitzsimmons, Kathryn E; Obreht, Igor; Bösken, Janina; Lehmkuhl, Frank (2016): Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period. Palaeogeography, Palaeoclimatology, Palaeoecology, https://doi.org/10.1016/j.palaeo.2016.12.029 Danube Romania Europe OUTCROP Outcrop sample Rasova_section Dataset 2016 ftpangaea https://doi.org/10.1594/PANGAEA.870532 https://doi.org/10.1016/j.palaeo.2016.12.029 2023-01-20T07:33:50Z In this study we provide a correlative age model for last glacial loess at the Rasova-Valea cu Pietre site in the Lower Danube region, based on the correlation of palaeoenvironmental proxies to independently dated palaeoclimate archives, luminescence dating and independent age control provided by the geochemically confirmed presence of the Campanian Ignimbrite (CI) tephra. The CI tephra, originating in the Phlegrean fields of southern Italy, has been dated elsewhere by 40Ar/39Ar to 39?40 ka BP, and is frequently found in the Lower Danube loess. As such, the CI tephra represents a valuable temporal and stratigraphic maker across loess deposits in the region. Our age model facilitates high-resolution correlation of palaeoenvironmental features observed at Rasova to palaeoclimate archives in Greenland and the Black Sea ? Mediterranean area. We observe semi-cyclic behaviour of the frequency dependent magnetic susceptibility throughout the profile, which we ascribe to millennial-scale climate variability also observed elsewhere in the Black Sea region. This is the first study to clearly identify millennial-scale climate variability over the Holocene and last glacial in the Lower Danube loess. Proxy variability in the Holocene indicates continuous aeolian sedimentation through this epoch. Dataset Greenland PANGAEA - Data Publisher for Earth & Environmental Science Greenland ENVELOPE(27.951470,27.951470,44.254250,44.254250) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Danube Romania Europe OUTCROP Outcrop sample Rasova_section |
spellingShingle |
Danube Romania Europe OUTCROP Outcrop sample Rasova_section Zeeden, Christian Hambach, Ulrich Veres, Daniel Fitzsimmons, Kathryn E Obreht, Igor Bösken, Janina Lehmkuhl, Frank Physical properties and fine fraction from loess at Rasova/Lower Danube |
topic_facet |
Danube Romania Europe OUTCROP Outcrop sample Rasova_section |
description |
In this study we provide a correlative age model for last glacial loess at the Rasova-Valea cu Pietre site in the Lower Danube region, based on the correlation of palaeoenvironmental proxies to independently dated palaeoclimate archives, luminescence dating and independent age control provided by the geochemically confirmed presence of the Campanian Ignimbrite (CI) tephra. The CI tephra, originating in the Phlegrean fields of southern Italy, has been dated elsewhere by 40Ar/39Ar to 39?40 ka BP, and is frequently found in the Lower Danube loess. As such, the CI tephra represents a valuable temporal and stratigraphic maker across loess deposits in the region. Our age model facilitates high-resolution correlation of palaeoenvironmental features observed at Rasova to palaeoclimate archives in Greenland and the Black Sea ? Mediterranean area. We observe semi-cyclic behaviour of the frequency dependent magnetic susceptibility throughout the profile, which we ascribe to millennial-scale climate variability also observed elsewhere in the Black Sea region. This is the first study to clearly identify millennial-scale climate variability over the Holocene and last glacial in the Lower Danube loess. Proxy variability in the Holocene indicates continuous aeolian sedimentation through this epoch. |
format |
Dataset |
author |
Zeeden, Christian Hambach, Ulrich Veres, Daniel Fitzsimmons, Kathryn E Obreht, Igor Bösken, Janina Lehmkuhl, Frank |
author_facet |
Zeeden, Christian Hambach, Ulrich Veres, Daniel Fitzsimmons, Kathryn E Obreht, Igor Bösken, Janina Lehmkuhl, Frank |
author_sort |
Zeeden, Christian |
title |
Physical properties and fine fraction from loess at Rasova/Lower Danube |
title_short |
Physical properties and fine fraction from loess at Rasova/Lower Danube |
title_full |
Physical properties and fine fraction from loess at Rasova/Lower Danube |
title_fullStr |
Physical properties and fine fraction from loess at Rasova/Lower Danube |
title_full_unstemmed |
Physical properties and fine fraction from loess at Rasova/Lower Danube |
title_sort |
physical properties and fine fraction from loess at rasova/lower danube |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.870532 https://doi.org/10.1594/PANGAEA.870532 |
op_coverage |
LATITUDE: 44.254250 * LONGITUDE: 27.951470 |
long_lat |
ENVELOPE(27.951470,27.951470,44.254250,44.254250) |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_source |
Supplement to: Zeeden, Christian; Hambach, Ulrich; Veres, Daniel; Fitzsimmons, Kathryn E; Obreht, Igor; Bösken, Janina; Lehmkuhl, Frank (2016): Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period. Palaeogeography, Palaeoclimatology, Palaeoecology, https://doi.org/10.1016/j.palaeo.2016.12.029 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.870532 https://doi.org/10.1594/PANGAEA.870532 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.870532 https://doi.org/10.1016/j.palaeo.2016.12.029 |
_version_ |
1766019150263615488 |