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...
Main Authors: | , , , , , |
---|---|
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 |
_version_ |
1810434034633801728 |