The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ...
Glacier highstands since the Last Glacial Maximum are well documented for many regions, but little is known about glacier fluctuations and lowstands during the Holocene. This is because the traces of minimum extents are difficult to identify and at many places are still ice covered, limiting the acc...
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ftdatacite:10.7892/boris.46229 2024-09-30T14:36:28+00:00 The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ... Herren, Pierre-Alain Eichler, Anja Machguth, Horst Papina, Tatyana Tobler, Leonhard Zapf, Alexander Schwikowski, Margit 2013 application/pdf https://dx.doi.org/10.7892/boris.46229 https://boris.unibe.ch/46229/ en eng Pergamon info:eu-repo/semantics/restrictedAccess info:eu-repo/semantics/openAccess 570 Life sciences; biology 540 Chemistry Text ScholarlyArticle article-journal 2013 ftdatacite https://doi.org/10.7892/boris.46229 2024-09-02T10:00:02Z Glacier highstands since the Last Glacial Maximum are well documented for many regions, but little is known about glacier fluctuations and lowstands during the Holocene. This is because the traces of minimum extents are difficult to identify and at many places are still ice covered, limiting the access to sample material. Here we report a new approach to assess minimal glacier extent, using a 72-m long surface-to-bedrock ice core drilled on Khukh Nuru Uul, a glacier in the Tsambagarav mountain range of the Mongolian Altai (4130 m asl, 48°39.338′N, 90°50.826′E). The small ice cap has low ice temperatures and flat bedrock topography at the drill site. This indicates minimal lateral glacier flow and thereby preserved climate signals. The upper two-thirds of the ice core contain 200 years of climate information with annual resolution, whereas the lower third is subject to strong thinning of the annual layers with a basal ice age of approximately 6000 years before present (BP). We interpret the basal ice age as ... Text Ice cap ice core DataCite |
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570 Life sciences; biology 540 Chemistry |
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570 Life sciences; biology 540 Chemistry Herren, Pierre-Alain Eichler, Anja Machguth, Horst Papina, Tatyana Tobler, Leonhard Zapf, Alexander Schwikowski, Margit The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ... |
topic_facet |
570 Life sciences; biology 540 Chemistry |
description |
Glacier highstands since the Last Glacial Maximum are well documented for many regions, but little is known about glacier fluctuations and lowstands during the Holocene. This is because the traces of minimum extents are difficult to identify and at many places are still ice covered, limiting the access to sample material. Here we report a new approach to assess minimal glacier extent, using a 72-m long surface-to-bedrock ice core drilled on Khukh Nuru Uul, a glacier in the Tsambagarav mountain range of the Mongolian Altai (4130 m asl, 48°39.338′N, 90°50.826′E). The small ice cap has low ice temperatures and flat bedrock topography at the drill site. This indicates minimal lateral glacier flow and thereby preserved climate signals. The upper two-thirds of the ice core contain 200 years of climate information with annual resolution, whereas the lower third is subject to strong thinning of the annual layers with a basal ice age of approximately 6000 years before present (BP). We interpret the basal ice age as ... |
format |
Text |
author |
Herren, Pierre-Alain Eichler, Anja Machguth, Horst Papina, Tatyana Tobler, Leonhard Zapf, Alexander Schwikowski, Margit |
author_facet |
Herren, Pierre-Alain Eichler, Anja Machguth, Horst Papina, Tatyana Tobler, Leonhard Zapf, Alexander Schwikowski, Margit |
author_sort |
Herren, Pierre-Alain |
title |
The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ... |
title_short |
The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ... |
title_full |
The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ... |
title_fullStr |
The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ... |
title_full_unstemmed |
The onset of Neoglaciation 6000 years ago in western Mongolia revealed by an ice core from the Tsambagarav mountain range ... |
title_sort |
onset of neoglaciation 6000 years ago in western mongolia revealed by an ice core from the tsambagarav mountain range ... |
publisher |
Pergamon |
publishDate |
2013 |
url |
https://dx.doi.org/10.7892/boris.46229 https://boris.unibe.ch/46229/ |
genre |
Ice cap ice core |
genre_facet |
Ice cap ice core |
op_rights |
info:eu-repo/semantics/restrictedAccess info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.7892/boris.46229 |
_version_ |
1811639505235476480 |