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Main Authors: Gingele, Franz, De Deckker, Patrick, Hillenbrand, Claus-Dieter
Format: Dataset Open Access
Language:en
Published: PANGAEA 2023
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Online Access:https://doi.org/10.1594/PANGAEA.960587
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author Gingele, Franz
De Deckker, Patrick
Hillenbrand, Claus-Dieter
author_facet Gingele, Franz
De Deckker, Patrick
Hillenbrand, Claus-Dieter
collection Datos científicos de ciencias marinas y ambientales
contents The data presents sedimentological data (relative percentages of silt, clay, together with smectite, illite, kaolinite, and chlorite relative percentages) from gravity core MD03-2611. The sedimentological data was obtained by Dr. Franz Gingele and first published in Gingele et al. (2004) but was not yet freely accessible. The 11.97 m long core MD03-2611 was collected during the AUSCAN cruise in 2003 on-board the research vessel Marion Dufresne II (Hill and De Deckker, 2004; https://doi.org/10.17600/3200090). It was retrieved from a small plateau south of Kangaroo Island at 2420 m depth (36°43.80'S, 136°32.90'E) facing the mouth of the Murray River. The datasets cover the last 94 ka and have been used to understand how deep-sea benthic environments respond to changes occurring within surface waters and on land.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_960587
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Clay mineralogy from sediment core MD03-2611 (South Australian margin, AUSCAN cruise)
Gingele, Franz
De Deckker, Patrick
Hillenbrand, Claus-Dieter
AUSCAN; Australia; Benthic foraminifera; Canyons; Chlorite; Clay; Clay/Silt ratio; Clay minerals; DEPTH, sediment/rock; GC; Grain size, sieving/settling tube; Gravity corer; Illite; Kaolinite; Marion Dufresne (1995); MD032611G; MD03-2611G; MD131; Quaternary; Sediment archives; Silt; Silt/clay ratio; Smectite; Southern Ocean
The data presents sedimentological data (relative percentages of silt, clay, together with smectite, illite, kaolinite, and chlorite relative percentages) from gravity core MD03-2611. The sedimentological data was obtained by Dr. Franz Gingele and first published in Gingele et al. (2004) but was not yet freely accessible. The 11.97 m long core MD03-2611 was collected during the AUSCAN cruise in 2003 on-board the research vessel Marion Dufresne II (Hill and De Deckker, 2004; https://doi.org/10.17600/3200090). It was retrieved from a small plateau south of Kangaroo Island at 2420 m depth (36°43.80'S, 136°32.90'E) facing the mouth of the Murray River. The datasets cover the last 94 ka and have been used to understand how deep-sea benthic environments respond to changes occurring within surface waters and on land.
title Clay mineralogy from sediment core MD03-2611 (South Australian margin, AUSCAN cruise)
topic AUSCAN; Australia; Benthic foraminifera; Canyons; Chlorite; Clay; Clay/Silt ratio; Clay minerals; DEPTH, sediment/rock; GC; Grain size, sieving/settling tube; Gravity corer; Illite; Kaolinite; Marion Dufresne (1995); MD032611G; MD03-2611G; MD131; Quaternary; Sediment archives; Silt; Silt/clay ratio; Smectite; Southern Ocean
url https://doi.org/10.1594/PANGAEA.960587