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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Bibliographic Details
Main Authors: Nürnberg, Dirk, Fütterer, Dieter K, Niessen, Frank, Et Al.
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1995
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.733565
https://doi.pangaea.de/10.1594/PANGAEA.733565
id ftdatacite:10.1594/pangaea.733565
record_format openpolar
spelling 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
institution Open Polar
collection DataCite
op_collection_id ftdatacite
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
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