Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ...
The clay mineral assemblages of upper Eocene to lower Miocene sediments recovered at the CIROS-1 and MSSTS-1 drill sites on the McMurdo Sound shelf, Antarctica, were analyzed in order to reconstruct the Cenozoic Antarctic paleoclimate and ice dynamics. The assemblages are dominated by smectite and i...
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ftdatacite:10.1594/pangaea.730374 2024-09-15T17:47:25+00:00 Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ... Ehrmann, Werner 1998 application/zip https://dx.doi.org/10.1594/pangaea.730374 https://doi.pangaea.de/10.1594/PANGAEA.730374 en eng PANGAEA https://dx.doi.org/10.1016/s0031-0182(97)00138-7 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig CIROS MSSTS Sampling/drilling ice article Collection Supplementary Publication Series of Datasets 1998 ftdatacite https://doi.org/10.1594/pangaea.73037410.1016/s0031-0182(97)00138-7 2024-08-01T10:58:30Z The clay mineral assemblages of upper Eocene to lower Miocene sediments recovered at the CIROS-1 and MSSTS-1 drill sites on the McMurdo Sound shelf, Antarctica, were analyzed in order to reconstruct the Cenozoic Antarctic paleoclimate and ice dynamics. The assemblages are dominated by smectite and illite, with minor amounts of chlorite and kaolinite. The highest smectite amounts and best smectite crystallinities occur in the upper Eocene part of CIROS-1, below 425-445 mbsf. They indicate that during their deposition, chemical weathering conditions prevailed on the nearby continent. Large parts of East Antarctica were probably ice-free at that time, but some glaciers reached the sea and contributed to the glaciomarine sedimentation. In contrast, only minor total amounts of smectite are present in Oligocene and younger sediments due to the shift to mainly physical weathering on an ice-covered Antarctic continent. However, relative smectite percentages rise to more than 60% during two late Oligocene intervals ... : Supplement to: Ehrmann, Werner (1998): Implications of late Eocene to early Miocene clay mineral assemblages in McMurdo Sound (Ross Sea, Antarctica) on paleoclimate and ice dynamics. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3-4), 213-231 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica McMurdo Sound Ross Sea DataCite |
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English |
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Drilling/drill rig CIROS MSSTS Sampling/drilling ice |
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Drilling/drill rig CIROS MSSTS Sampling/drilling ice Ehrmann, Werner Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ... |
topic_facet |
Drilling/drill rig CIROS MSSTS Sampling/drilling ice |
description |
The clay mineral assemblages of upper Eocene to lower Miocene sediments recovered at the CIROS-1 and MSSTS-1 drill sites on the McMurdo Sound shelf, Antarctica, were analyzed in order to reconstruct the Cenozoic Antarctic paleoclimate and ice dynamics. The assemblages are dominated by smectite and illite, with minor amounts of chlorite and kaolinite. The highest smectite amounts and best smectite crystallinities occur in the upper Eocene part of CIROS-1, below 425-445 mbsf. They indicate that during their deposition, chemical weathering conditions prevailed on the nearby continent. Large parts of East Antarctica were probably ice-free at that time, but some glaciers reached the sea and contributed to the glaciomarine sedimentation. In contrast, only minor total amounts of smectite are present in Oligocene and younger sediments due to the shift to mainly physical weathering on an ice-covered Antarctic continent. However, relative smectite percentages rise to more than 60% during two late Oligocene intervals ... : Supplement to: Ehrmann, Werner (1998): Implications of late Eocene to early Miocene clay mineral assemblages in McMurdo Sound (Ross Sea, Antarctica) on paleoclimate and ice dynamics. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3-4), 213-231 ... |
format |
Article in Journal/Newspaper |
author |
Ehrmann, Werner |
author_facet |
Ehrmann, Werner |
author_sort |
Ehrmann, Werner |
title |
Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ... |
title_short |
Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ... |
title_full |
Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ... |
title_fullStr |
Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ... |
title_full_unstemmed |
Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica ... |
title_sort |
clay mineralogy of late eocene to early miocene sediments of mcmurdo sound, antarctica ... |
publisher |
PANGAEA |
publishDate |
1998 |
url |
https://dx.doi.org/10.1594/pangaea.730374 https://doi.pangaea.de/10.1594/PANGAEA.730374 |
genre |
Antarc* Antarctic Antarctica East Antarctica McMurdo Sound Ross Sea |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica McMurdo Sound Ross Sea |
op_relation |
https://dx.doi.org/10.1016/s0031-0182(97)00138-7 |
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.73037410.1016/s0031-0182(97)00138-7 |
_version_ |
1810496693435629568 |