Radiocarbon dating and physical properties of sediment core GeoB17623-2 ...

PARASOUND (3.5 kHz) subbottom echosounder profiles acquired on the southern Spitsbergenbanken, NW Barents Sea, show iceberg-keel scouring features which are buried by sediment that accumulated during the post Last Glacial Maximum (LGM) sea-level rise. Four acoustic units (Units 1 to 4 in stratigraph...

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Main Authors: Zecchin, Massimo, Rebesco, Michele, Lucchi, Renata G, Caffau, Mauro, Lantzsch, Hendrik, Hanebuth, Till J J
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2016
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.873865
https://doi.pangaea.de/10.1594/PANGAEA.873865
id ftdatacite:10.1594/pangaea.873865
record_format openpolar
spelling ftdatacite:10.1594/pangaea.873865 2024-09-15T17:57:50+00:00 Radiocarbon dating and physical properties of sediment core GeoB17623-2 ... Zecchin, Massimo Rebesco, Michele Lucchi, Renata G Caffau, Mauro Lantzsch, Hendrik Hanebuth, Till J J 2016 application/zip https://dx.doi.org/10.1594/pangaea.873865 https://doi.pangaea.de/10.1594/PANGAEA.873865 en eng PANGAEA https://dx.doi.org/10.1016/j.margeo.2016.10.005 Creative Commons Attribution Non Commercial No Derivatives 3.0 Unported https://creativecommons.org/licenses/by-nc-nd/3.0/legalcode cc-by-nc-nd-3.0 Center for Marine Environmental Sciences MARUM article Collection Supplementary Publication Series of Datasets 2016 ftdatacite https://doi.org/10.1594/pangaea.87386510.1016/j.margeo.2016.10.005 2024-08-01T10:54:44Z PARASOUND (3.5 kHz) subbottom echosounder profiles acquired on the southern Spitsbergenbanken, NW Barents Sea, show iceberg-keel scouring features which are buried by sediment that accumulated during the post Last Glacial Maximum (LGM) sea-level rise. Four acoustic units (Units 1 to 4 in stratigraphic order) were differentiated, based on the characterization of their acoustic facies and reflection surfaces. Unit 1 shows a chaotic internal structure and is interpreted as a glacial till, whereas the laminated Units 2 to 4 accumulated by sediment settling from suspension clouds and bottom currents during the last deglaciation phase. The top of Unit 2 was frequently incised by iceberg keels, resulting in up to 12 m deep ploughmarks which were later filled and buried by Unit 3 and 4 sediments. Three main paleo-evironmental changes controlled the evolution of the facies succession: (1) The major shift from till formation (Unit 1) below grounded ice to the accumulation of laminated sediments (Unit 2) which are ... : Supplement to: Zecchin, Massimo; Rebesco, Michele; Lucchi, Renata G; Caffau, Mauro; Lantzsch, Hendrik; Hanebuth, Till J J (2016): Buried iceberg-keel scouring on the southern Spitsbergenbanken, NW Barents Sea. Marine Geology, 382, 68-79 ... Article in Journal/Newspaper Barents Sea Spitsbergenbanken DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Center for Marine Environmental Sciences MARUM
spellingShingle Center for Marine Environmental Sciences MARUM
Zecchin, Massimo
Rebesco, Michele
Lucchi, Renata G
Caffau, Mauro
Lantzsch, Hendrik
Hanebuth, Till J J
Radiocarbon dating and physical properties of sediment core GeoB17623-2 ...
topic_facet Center for Marine Environmental Sciences MARUM
description PARASOUND (3.5 kHz) subbottom echosounder profiles acquired on the southern Spitsbergenbanken, NW Barents Sea, show iceberg-keel scouring features which are buried by sediment that accumulated during the post Last Glacial Maximum (LGM) sea-level rise. Four acoustic units (Units 1 to 4 in stratigraphic order) were differentiated, based on the characterization of their acoustic facies and reflection surfaces. Unit 1 shows a chaotic internal structure and is interpreted as a glacial till, whereas the laminated Units 2 to 4 accumulated by sediment settling from suspension clouds and bottom currents during the last deglaciation phase. The top of Unit 2 was frequently incised by iceberg keels, resulting in up to 12 m deep ploughmarks which were later filled and buried by Unit 3 and 4 sediments. Three main paleo-evironmental changes controlled the evolution of the facies succession: (1) The major shift from till formation (Unit 1) below grounded ice to the accumulation of laminated sediments (Unit 2) which are ... : Supplement to: Zecchin, Massimo; Rebesco, Michele; Lucchi, Renata G; Caffau, Mauro; Lantzsch, Hendrik; Hanebuth, Till J J (2016): Buried iceberg-keel scouring on the southern Spitsbergenbanken, NW Barents Sea. Marine Geology, 382, 68-79 ...
format Article in Journal/Newspaper
author Zecchin, Massimo
Rebesco, Michele
Lucchi, Renata G
Caffau, Mauro
Lantzsch, Hendrik
Hanebuth, Till J J
author_facet Zecchin, Massimo
Rebesco, Michele
Lucchi, Renata G
Caffau, Mauro
Lantzsch, Hendrik
Hanebuth, Till J J
author_sort Zecchin, Massimo
title Radiocarbon dating and physical properties of sediment core GeoB17623-2 ...
title_short Radiocarbon dating and physical properties of sediment core GeoB17623-2 ...
title_full Radiocarbon dating and physical properties of sediment core GeoB17623-2 ...
title_fullStr Radiocarbon dating and physical properties of sediment core GeoB17623-2 ...
title_full_unstemmed Radiocarbon dating and physical properties of sediment core GeoB17623-2 ...
title_sort radiocarbon dating and physical properties of sediment core geob17623-2 ...
publisher PANGAEA
publishDate 2016
url https://dx.doi.org/10.1594/pangaea.873865
https://doi.pangaea.de/10.1594/PANGAEA.873865
genre Barents Sea
Spitsbergenbanken
genre_facet Barents Sea
Spitsbergenbanken
op_relation https://dx.doi.org/10.1016/j.margeo.2016.10.005
op_rights Creative Commons Attribution Non Commercial No Derivatives 3.0 Unported
https://creativecommons.org/licenses/by-nc-nd/3.0/legalcode
cc-by-nc-nd-3.0
op_doi https://doi.org/10.1594/pangaea.87386510.1016/j.margeo.2016.10.005
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