Sedimentological investigation on 4 cores from the Antarctic continental margin ...

Sedimentary sequences spanning early Oligocene and Neogene time intervals were recovered with piston and gravity cores along erosional structures at northern Gunnerus Ridge and Kainan Maru Seamount in the southernmost Indian Ocean. Results of sedimentological investigations help to reconstruct the C...

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Main Authors: Hillenbrand, Claus-Dieter, Ehrmann, Werner
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.734001
https://doi.pangaea.de/10.1594/PANGAEA.734001
id ftdatacite:10.1594/pangaea.734001
record_format openpolar
spelling ftdatacite:10.1594/pangaea.734001 2024-04-28T08:02:52+00:00 Sedimentological investigation on 4 cores from the Antarctic continental margin ... Hillenbrand, Claus-Dieter Ehrmann, Werner 2003 application/zip https://dx.doi.org/10.1594/pangaea.734001 https://doi.pangaea.de/10.1594/PANGAEA.734001 en eng PANGAEA https://dx.doi.org/10.1017/s0954102003001640 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type Piston corer BGR type ANT-VIII/6 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Supplementary Publication Series of Datasets Collection 2003 ftdatacite https://doi.org/10.1594/pangaea.73400110.1017/s0954102003001640 2024-04-02T09:30:57Z Sedimentary sequences spanning early Oligocene and Neogene time intervals were recovered with piston and gravity cores along erosional structures at northern Gunnerus Ridge and Kainan Maru Seamount in the southernmost Indian Ocean. Results of sedimentological investigations help to reconstruct the Cenozoic palaeoenvironment. Main emphasis was placed on grain size and clay mineral data. The clay mineral assemblages are dominated by illite and smectite. Chlorite and kaolinite occur in trace amounts. Whereas illite has a distinct source on the East Antarctic craton, smectite is of somewhat speculative origin, but probably is derived from erosion of Cenozoic or older shelf sediments. The presence of terrigenous sand indicates that ice-rafting was active throughout the time represented by the investigated cores, although with varying intensity. During the early Oligocene interval (30.1–29.0 Ma), siliceous phytoplankton production dominated sedimentation. Environmental conditions were quite different from those on ... : Supplement to: Hillenbrand, Claus-Dieter; Ehrmann, Werner (2003): Palaeoenvironmental Implications from Tertiary Sediments of Kainan Maru Seamount and Northern Gunnerus Ridge. Antarctic Science, 15, 522-536 ... Article in Journal/Newspaper Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
Piston corer BGR type
ANT-VIII/6
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Gravity corer Kiel type
Piston corer BGR type
ANT-VIII/6
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Hillenbrand, Claus-Dieter
Ehrmann, Werner
Sedimentological investigation on 4 cores from the Antarctic continental margin ...
topic_facet Gravity corer Kiel type
Piston corer BGR type
ANT-VIII/6
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Sedimentary sequences spanning early Oligocene and Neogene time intervals were recovered with piston and gravity cores along erosional structures at northern Gunnerus Ridge and Kainan Maru Seamount in the southernmost Indian Ocean. Results of sedimentological investigations help to reconstruct the Cenozoic palaeoenvironment. Main emphasis was placed on grain size and clay mineral data. The clay mineral assemblages are dominated by illite and smectite. Chlorite and kaolinite occur in trace amounts. Whereas illite has a distinct source on the East Antarctic craton, smectite is of somewhat speculative origin, but probably is derived from erosion of Cenozoic or older shelf sediments. The presence of terrigenous sand indicates that ice-rafting was active throughout the time represented by the investigated cores, although with varying intensity. During the early Oligocene interval (30.1–29.0 Ma), siliceous phytoplankton production dominated sedimentation. Environmental conditions were quite different from those on ... : Supplement to: Hillenbrand, Claus-Dieter; Ehrmann, Werner (2003): Palaeoenvironmental Implications from Tertiary Sediments of Kainan Maru Seamount and Northern Gunnerus Ridge. Antarctic Science, 15, 522-536 ...
format Article in Journal/Newspaper
author Hillenbrand, Claus-Dieter
Ehrmann, Werner
author_facet Hillenbrand, Claus-Dieter
Ehrmann, Werner
author_sort Hillenbrand, Claus-Dieter
title Sedimentological investigation on 4 cores from the Antarctic continental margin ...
title_short Sedimentological investigation on 4 cores from the Antarctic continental margin ...
title_full Sedimentological investigation on 4 cores from the Antarctic continental margin ...
title_fullStr Sedimentological investigation on 4 cores from the Antarctic continental margin ...
title_full_unstemmed Sedimentological investigation on 4 cores from the Antarctic continental margin ...
title_sort sedimentological investigation on 4 cores from the antarctic continental margin ...
publisher PANGAEA
publishDate 2003
url https://dx.doi.org/10.1594/pangaea.734001
https://doi.pangaea.de/10.1594/PANGAEA.734001
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation https://dx.doi.org/10.1017/s0954102003001640
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.73400110.1017/s0954102003001640
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