Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records
In this paper, I would like to provide refined relative chronological data to loess-paleosol section situated on the IV. and V. terraces of Red Hill (Moravia), based on a comparison with Heirich events, North and South hemispheric ice core records. The last glacial–interglacial loess section is almo...
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ftmtakojs:oai:ojs3.mtak.hu:article/3019 2023-05-15T16:38:55+02:00 Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records Kis, Éva 2012-12-13 application/pdf https://ojs.mtak.hu/index.php/hungeobull/article/view/3019 eng eng Research Centre for Astronomy and Earth Sciences https://ojs.mtak.hu/index.php/hungeobull/article/view/3019/2279 https://ojs.mtak.hu/index.php/hungeobull/article/view/3019 Copyright (c) 2012 Éva Kis http://creativecommons.org/licenses/by-nc-nd/4.0 CC-BY-NC-ND Hungarian Geographical Bulletin; Vol. 61 No. 4 (2012); 327-341 Hungarian Geographical Bulletin; Évf. 61 szám 4 (2012); 327-341 2064-5147 2064-5031 Heinrich events ice cores loess-paleosol series chronology δ18O values info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 2012 ftmtakojs 2022-08-31T11:30:28Z In this paper, I would like to provide refined relative chronological data to loess-paleosol section situated on the IV. and V. terraces of Red Hill (Moravia), based on a comparison with Heirich events, North and South hemispheric ice core records. The last glacial–interglacial loess section is almost complete, all of the interstadial soils can be identified in the series instead of the eroded upper part of the PK I complex.The onset of the formation of recent soil can be parallelized to H0 event (~12 000), the double structural soils to H1 and H2 events, the eroded soils of PK I to H3 and H4, while the lower part of the complex has been correlated with H5 and H6 events (~63 ka BP). The loess series above PK I has been classifi ed into Würm-3, the strata between PK I and PK II belong to the Würm-2. The lower part, under PK II is mostly clayey, cannot be regarded as a cold climate deposit. After the Riss/Würm interglacial the climate has changed slowly, and the typical glacial climate has started only after 75 ka BP. Article in Journal/Newspaper ice core MTAK Folyorat-Szerkesztö Rendszer (Magyar Tudományos Akadémia Könyvtára) Red Hill ENVELOPE(-58.500,-58.500,-62.233,-62.233) |
institution |
Open Polar |
collection |
MTAK Folyorat-Szerkesztö Rendszer (Magyar Tudományos Akadémia Könyvtára) |
op_collection_id |
ftmtakojs |
language |
English |
topic |
Heinrich events ice cores loess-paleosol series chronology δ18O values |
spellingShingle |
Heinrich events ice cores loess-paleosol series chronology δ18O values Kis, Éva Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records |
topic_facet |
Heinrich events ice cores loess-paleosol series chronology δ18O values |
description |
In this paper, I would like to provide refined relative chronological data to loess-paleosol section situated on the IV. and V. terraces of Red Hill (Moravia), based on a comparison with Heirich events, North and South hemispheric ice core records. The last glacial–interglacial loess section is almost complete, all of the interstadial soils can be identified in the series instead of the eroded upper part of the PK I complex.The onset of the formation of recent soil can be parallelized to H0 event (~12 000), the double structural soils to H1 and H2 events, the eroded soils of PK I to H3 and H4, while the lower part of the complex has been correlated with H5 and H6 events (~63 ka BP). The loess series above PK I has been classifi ed into Würm-3, the strata between PK I and PK II belong to the Würm-2. The lower part, under PK II is mostly clayey, cannot be regarded as a cold climate deposit. After the Riss/Würm interglacial the climate has changed slowly, and the typical glacial climate has started only after 75 ka BP. |
format |
Article in Journal/Newspaper |
author |
Kis, Éva |
author_facet |
Kis, Éva |
author_sort |
Kis, Éva |
title |
Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records |
title_short |
Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records |
title_full |
Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records |
title_fullStr |
Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records |
title_full_unstemmed |
Parallelization of Last Glacial loess-paleosol section of Red Hill with Heinrich events and ice core records |
title_sort |
parallelization of last glacial loess-paleosol section of red hill with heinrich events and ice core records |
publisher |
Research Centre for Astronomy and Earth Sciences |
publishDate |
2012 |
url |
https://ojs.mtak.hu/index.php/hungeobull/article/view/3019 |
long_lat |
ENVELOPE(-58.500,-58.500,-62.233,-62.233) |
geographic |
Red Hill |
geographic_facet |
Red Hill |
genre |
ice core |
genre_facet |
ice core |
op_source |
Hungarian Geographical Bulletin; Vol. 61 No. 4 (2012); 327-341 Hungarian Geographical Bulletin; Évf. 61 szám 4 (2012); 327-341 2064-5147 2064-5031 |
op_relation |
https://ojs.mtak.hu/index.php/hungeobull/article/view/3019/2279 https://ojs.mtak.hu/index.php/hungeobull/article/view/3019 |
op_rights |
Copyright (c) 2012 Éva Kis http://creativecommons.org/licenses/by-nc-nd/4.0 |
op_rightsnorm |
CC-BY-NC-ND |
_version_ |
1766029278763286528 |