Susceptibility of sediment cores of the Laptev Sea ...
Marine geological investigations were performed across the Laptev Sea continental shelf and slope. Thirty sampling sites were selected covering a depth range of ca 3500 m. Maximum core recovery was 9 m. PARASOUND sub-bottom profiling was used for site surveying and provided important information on...
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ftdatacite:10.1594/pangaea.733565 2024-09-15T18:17:31+00:00 Susceptibility of sediment cores of the Laptev Sea ... Nürnberg, Dirk Fütterer, Dieter K Niessen, Frank Et Al. 1995 application/zip https://dx.doi.org/10.1594/pangaea.733565 https://doi.pangaea.de/10.1594/PANGAEA.733565 en eng PANGAEA https://dx.doi.org/10.1111/j.1751-8369.1995.tb00709.x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type Kasten corer ARK-IX/4 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 1995 ftdatacite https://doi.org/10.1594/pangaea.73356510.1111/j.1751-8369.1995.tb00709.x 2024-07-03T13:10:33Z Marine geological investigations were performed across the Laptev Sea continental shelf and slope. Thirty sampling sites were selected covering a depth range of ca 3500 m. Maximum core recovery was 9 m. PARASOUND sub-bottom profiling was used for site surveying and provided important information on the depositional environment of the continental margin together with sedimentological and stratigraphical investigations.Undisturbed horizontal layering of the sea-floor sediments is a common feature for the Laptev Sea shelf. There is no indication for glaciation of the broad shelf region during the Last Glacial, since moraine deposits are missing. However, a high number of plough marks in places points to recent to sub-recent ice-erosion which has led to an intensive sediment reworking on the shelf. Several broadly incised river channels recorded near the shelf edge are related to Pleistocene drainage systems of large Siberian rivers which cut into the dry shelves during the Last Glacial Maximum and were ... : Supplement to: Nürnberg, Dirk; Fütterer, Dieter K; Niessen, Frank; et al. (1995): The depositional environment of the Laptev Sea continental margin: preliminiary results from the R/V Polarstern ARK IX-4 cruise. Polar Research, 14(1), 43-53 ... Article in Journal/Newspaper laptev Laptev Sea DataCite |
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language |
English |
topic |
Gravity corer Kiel type Kasten corer ARK-IX/4 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
Gravity corer Kiel type Kasten corer ARK-IX/4 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN Nürnberg, Dirk Fütterer, Dieter K Niessen, Frank Et Al. Susceptibility of sediment cores of the Laptev Sea ... |
topic_facet |
Gravity corer Kiel type Kasten corer ARK-IX/4 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
description |
Marine geological investigations were performed across the Laptev Sea continental shelf and slope. Thirty sampling sites were selected covering a depth range of ca 3500 m. Maximum core recovery was 9 m. PARASOUND sub-bottom profiling was used for site surveying and provided important information on the depositional environment of the continental margin together with sedimentological and stratigraphical investigations.Undisturbed horizontal layering of the sea-floor sediments is a common feature for the Laptev Sea shelf. There is no indication for glaciation of the broad shelf region during the Last Glacial, since moraine deposits are missing. However, a high number of plough marks in places points to recent to sub-recent ice-erosion which has led to an intensive sediment reworking on the shelf. Several broadly incised river channels recorded near the shelf edge are related to Pleistocene drainage systems of large Siberian rivers which cut into the dry shelves during the Last Glacial Maximum and were ... : Supplement to: Nürnberg, Dirk; Fütterer, Dieter K; Niessen, Frank; et al. (1995): The depositional environment of the Laptev Sea continental margin: preliminiary results from the R/V Polarstern ARK IX-4 cruise. Polar Research, 14(1), 43-53 ... |
format |
Article in Journal/Newspaper |
author |
Nürnberg, Dirk Fütterer, Dieter K Niessen, Frank Et Al. |
author_facet |
Nürnberg, Dirk Fütterer, Dieter K Niessen, Frank Et Al. |
author_sort |
Nürnberg, Dirk |
title |
Susceptibility of sediment cores of the Laptev Sea ... |
title_short |
Susceptibility of sediment cores of the Laptev Sea ... |
title_full |
Susceptibility of sediment cores of the Laptev Sea ... |
title_fullStr |
Susceptibility of sediment cores of the Laptev Sea ... |
title_full_unstemmed |
Susceptibility of sediment cores of the Laptev Sea ... |
title_sort |
susceptibility of sediment cores of the laptev sea ... |
publisher |
PANGAEA |
publishDate |
1995 |
url |
https://dx.doi.org/10.1594/pangaea.733565 https://doi.pangaea.de/10.1594/PANGAEA.733565 |
genre |
laptev Laptev Sea |
genre_facet |
laptev Laptev Sea |
op_relation |
https://dx.doi.org/10.1111/j.1751-8369.1995.tb00709.x |
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.73356510.1111/j.1751-8369.1995.tb00709.x |
_version_ |
1810455532940558336 |