Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ...
In wide areas of Northern Siberia, glaciers have been absent since the Late Pleistocene. Therefore, ground ice and especially ice wedges are used as archives for paleoclimatic studies. In the present study, carried out on the Bykovsky Peninsula, eastern Lena Delta, we were able to distinguish ice we...
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ftdatacite:10.1594/pangaea.758211 2024-09-15T18:17:35+00:00 Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ... Kunitsky, Victor V Schirrmeister, Lutz Grosse, Guido Kienast, Frank 2002 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.758211 https://doi.pangaea.de/10.1594/PANGAEA.758211 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Date/Time of event Location of event Elevation of event Width Length Thickness Clastic material Sample code/label Area/locality pH Oxidation reduction RedOx potential Calcium Magnesium Sodium Bicarbonate ion Sulfate Chloride dataset Supplementary Dataset Dataset 2002 ftdatacite https://doi.org/10.1594/pangaea.758211 2024-08-01T10:58:30Z In wide areas of Northern Siberia, glaciers have been absent since the Late Pleistocene. Therefore, ground ice and especially ice wedges are used as archives for paleoclimatic studies. In the present study, carried out on the Bykovsky Peninsula, eastern Lena Delta, we were able to distinguish ice wedges of different genetic units by means of oxygen and hydrogen isotopes. The results obtained by this study on the Ice Complex, a peculiar periglacial phenomenon, allowed the reconstruction of the climate history with a subdivision of a period of very cold winters (60-55 ka), followed by a long stable period of cold winter temperatures (50-24 ka), Between 20 ka and 11 ka, climate warming is indicated in stable isotope compositions, most probably after the Late Glacial Maximum. At that time, a change of the marine source of the precipitation from a more humid source to the present North AtIantic source region was assumed. For the Ice Complex, a continuous age-height relationship was established, indicating ... : Supplement to: Kunitsky, Victor V; Schirrmeister, Lutz; Grosse, Guido; Kienast, Frank (2002): Snow patches in nival landscapes and their role for the Ice Complex formation in the Laptev Sea coastal lowlands. Polarforschung, 70, 53-67 ... Dataset laptev Laptev Sea lena delta Siberia DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event Date/Time of event Location of event Elevation of event Width Length Thickness Clastic material Sample code/label Area/locality pH Oxidation reduction RedOx potential Calcium Magnesium Sodium Bicarbonate ion Sulfate Chloride |
spellingShingle |
Event label Latitude of event Longitude of event Date/Time of event Location of event Elevation of event Width Length Thickness Clastic material Sample code/label Area/locality pH Oxidation reduction RedOx potential Calcium Magnesium Sodium Bicarbonate ion Sulfate Chloride Kunitsky, Victor V Schirrmeister, Lutz Grosse, Guido Kienast, Frank Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ... |
topic_facet |
Event label Latitude of event Longitude of event Date/Time of event Location of event Elevation of event Width Length Thickness Clastic material Sample code/label Area/locality pH Oxidation reduction RedOx potential Calcium Magnesium Sodium Bicarbonate ion Sulfate Chloride |
description |
In wide areas of Northern Siberia, glaciers have been absent since the Late Pleistocene. Therefore, ground ice and especially ice wedges are used as archives for paleoclimatic studies. In the present study, carried out on the Bykovsky Peninsula, eastern Lena Delta, we were able to distinguish ice wedges of different genetic units by means of oxygen and hydrogen isotopes. The results obtained by this study on the Ice Complex, a peculiar periglacial phenomenon, allowed the reconstruction of the climate history with a subdivision of a period of very cold winters (60-55 ka), followed by a long stable period of cold winter temperatures (50-24 ka), Between 20 ka and 11 ka, climate warming is indicated in stable isotope compositions, most probably after the Late Glacial Maximum. At that time, a change of the marine source of the precipitation from a more humid source to the present North AtIantic source region was assumed. For the Ice Complex, a continuous age-height relationship was established, indicating ... : Supplement to: Kunitsky, Victor V; Schirrmeister, Lutz; Grosse, Guido; Kienast, Frank (2002): Snow patches in nival landscapes and their role for the Ice Complex formation in the Laptev Sea coastal lowlands. Polarforschung, 70, 53-67 ... |
format |
Dataset |
author |
Kunitsky, Victor V Schirrmeister, Lutz Grosse, Guido Kienast, Frank |
author_facet |
Kunitsky, Victor V Schirrmeister, Lutz Grosse, Guido Kienast, Frank |
author_sort |
Kunitsky, Victor V |
title |
Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ... |
title_short |
Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ... |
title_full |
Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ... |
title_fullStr |
Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ... |
title_full_unstemmed |
Tab. 1+7: Hydrochemical analyses of firn and meltwater from different "cold" snow patches ... |
title_sort |
tab. 1+7: hydrochemical analyses of firn and meltwater from different "cold" snow patches ... |
publisher |
PANGAEA |
publishDate |
2002 |
url |
https://dx.doi.org/10.1594/pangaea.758211 https://doi.pangaea.de/10.1594/PANGAEA.758211 |
genre |
laptev Laptev Sea lena delta Siberia |
genre_facet |
laptev Laptev Sea lena delta Siberia |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.758211 |
_version_ |
1810455640470978560 |