Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ...

The sediments recovered at ODP Sites 745 and 746 in the Australian-Antarctic Basin are characterized by cyclic facies changes between clayey diatom oozes and diatomaceous clays ranging in age from late Miocene (about 10 Ma) to Quaternary. The gravel and terrigenous sand content of the sediments is u...

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Main Authors: Ehrmann, Werner, Grobe, Hannes, Fütterer, Dieter K
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1991
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.587843
https://doi.pangaea.de/10.1594/PANGAEA.587843
id ftdatacite:10.1594/pangaea.587843
record_format openpolar
spelling ftdatacite:10.1594/pangaea.587843 2024-09-15T17:44:51+00:00 Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ... Ehrmann, Werner Grobe, Hannes Fütterer, Dieter K 1991 application/zip https://dx.doi.org/10.1594/pangaea.587843 https://doi.pangaea.de/10.1594/PANGAEA.587843 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.119.208.1991 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1991 ftdatacite https://doi.org/10.1594/pangaea.58784310.2973/odp.proc.sr.119.208.1991 2024-08-01T11:00:37Z The sediments recovered at ODP Sites 745 and 746 in the Australian-Antarctic Basin are characterized by cyclic facies changes between clayey diatom oozes and diatomaceous clays ranging in age from late Miocene (about 10 Ma) to Quaternary. The gravel and terrigenous sand content of the sediments is used as an indicator of the intensity of ice rafting through time. Maxima are recorded at 8.7-7.9, 6.6-6.0, 5.0-4.4, and 4.0-3.2 Ma. The maxima in more recent times are much less pronounced and occur at 2.4-1.6 and 1.4-1.0 Ma. All sand- and gravel-sized terrigenous sediment particles are of gneissic or granitic origin and originated from the East Antarctic continent. The maxima of ice rafting recorded at Sites 745 and 746 do not appear to represent local phenomena. Rather they document major advances and decays of the Antarctic ice shelves and glaciers and therefore represent events of great importance for the reconstruction of the paleoceanography of the Southern Ocean and the glacial history of Antarctica. In ... : Supplement to: Ehrmann, Werner; Grobe, Hannes; Fütterer, Dieter K (1991): Late Miocene to Holocene glacial history of east Antarctica revealed by sediments from sites 745 and 746. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 239-260 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Shelves Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg119
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg119
Joides Resolution
Ocean Drilling Program ODP
Ehrmann, Werner
Grobe, Hannes
Fütterer, Dieter K
Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ...
topic_facet Drilling/drill rig
Leg119
Joides Resolution
Ocean Drilling Program ODP
description The sediments recovered at ODP Sites 745 and 746 in the Australian-Antarctic Basin are characterized by cyclic facies changes between clayey diatom oozes and diatomaceous clays ranging in age from late Miocene (about 10 Ma) to Quaternary. The gravel and terrigenous sand content of the sediments is used as an indicator of the intensity of ice rafting through time. Maxima are recorded at 8.7-7.9, 6.6-6.0, 5.0-4.4, and 4.0-3.2 Ma. The maxima in more recent times are much less pronounced and occur at 2.4-1.6 and 1.4-1.0 Ma. All sand- and gravel-sized terrigenous sediment particles are of gneissic or granitic origin and originated from the East Antarctic continent. The maxima of ice rafting recorded at Sites 745 and 746 do not appear to represent local phenomena. Rather they document major advances and decays of the Antarctic ice shelves and glaciers and therefore represent events of great importance for the reconstruction of the paleoceanography of the Southern Ocean and the glacial history of Antarctica. In ... : Supplement to: Ehrmann, Werner; Grobe, Hannes; Fütterer, Dieter K (1991): Late Miocene to Holocene glacial history of east Antarctica revealed by sediments from sites 745 and 746. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 239-260 ...
format Article in Journal/Newspaper
author Ehrmann, Werner
Grobe, Hannes
Fütterer, Dieter K
author_facet Ehrmann, Werner
Grobe, Hannes
Fütterer, Dieter K
author_sort Ehrmann, Werner
title Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ...
title_short Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ...
title_full Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ...
title_fullStr Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ...
title_full_unstemmed Clay and bulk mineralogy of ODP sites 119-745 and 119-746 from the Southern Ocean ...
title_sort clay and bulk mineralogy of odp sites 119-745 and 119-746 from the southern ocean ...
publisher PANGAEA
publishDate 1991
url https://dx.doi.org/10.1594/pangaea.587843
https://doi.pangaea.de/10.1594/PANGAEA.587843
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Shelves
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Shelves
Southern Ocean
op_relation https://dx.doi.org/10.2973/odp.proc.sr.119.208.1991
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.58784310.2973/odp.proc.sr.119.208.1991
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