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| Main Authors: | , , |
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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2023
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| Online Access: | https://doi.org/10.1594/PANGAEA.960587 |
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| _version_ | 1867170120043855872 |
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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 |