Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau
Characterization of sediment from Ocean Drilling Program Site 745, representing the East Kerguelen Ridge sediment drift, addresses important issues surrounding the timing of Miocene to present East Antarctic ice sheet stability and oceanic environmental change. Our results show three periods of grea...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.713614 2024-09-15T17:45:52+00:00 Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau Joseph, Leah H Rea, David K van der Pluijm, Ben A Gleason, James D LATITUDE: -59.595000 * LONGITUDE: 85.854200 * DATE/TIME START: 1988-02-08T00:00:00 * DATE/TIME END: 1988-02-10T17:15:00 2002 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.713614 https://doi.org/10.1594/PANGAEA.713614 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.713614 https://doi.org/10.1594/PANGAEA.713614 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Joseph, Leah H; Rea, David K; van der Pluijm, Ben A; Gleason, James D (2002): Antarctic environmental variability since the late Miocene: ODP Site 745, the East Kerguelen sediment drift. Earth and Planetary Science Letters, 201(1), 127-142, https://doi.org/10.1016/S0012-821X(02)00661-1 119-745 119-745B COMPCORE Composite Core DRILL Drilling/drill rig Indian Ocean Joides Resolution Leg119 Ocean Drilling Program ODP dataset publication series 2002 ftpangaea https://doi.org/10.1594/PANGAEA.71361410.1016/S0012-821X(02)00661-1 2024-07-24T02:31:42Z Characterization of sediment from Ocean Drilling Program Site 745, representing the East Kerguelen Ridge sediment drift, addresses important issues surrounding the timing of Miocene to present East Antarctic ice sheet stability and oceanic environmental change. Our results show three periods of greatly enhanced accumulation of Antarctic-derived sediment, at 6.4-5.9 Ma, 4.9-4.4 Ma and 1.1-0.8 Ma, potentially indicative of warmer, less stable ice sheets at these times. Conversely, the accumulation of Antarctic-derived material is comparatively less during the middle of the Pliocene warm epoch (4.8-3.2 Ma). The deep flow forming the Kerguelen drift was stronger during the latest Miocene and earliest Pliocene and has decreased in intensity continuously since then. Other/Unknown Material Antarc* Antarctic Ice Sheet PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(85.854200,85.854200,-59.595000,-59.595000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
119-745 119-745B COMPCORE Composite Core DRILL Drilling/drill rig Indian Ocean Joides Resolution Leg119 Ocean Drilling Program ODP |
spellingShingle |
119-745 119-745B COMPCORE Composite Core DRILL Drilling/drill rig Indian Ocean Joides Resolution Leg119 Ocean Drilling Program ODP Joseph, Leah H Rea, David K van der Pluijm, Ben A Gleason, James D Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau |
topic_facet |
119-745 119-745B COMPCORE Composite Core DRILL Drilling/drill rig Indian Ocean Joides Resolution Leg119 Ocean Drilling Program ODP |
description |
Characterization of sediment from Ocean Drilling Program Site 745, representing the East Kerguelen Ridge sediment drift, addresses important issues surrounding the timing of Miocene to present East Antarctic ice sheet stability and oceanic environmental change. Our results show three periods of greatly enhanced accumulation of Antarctic-derived sediment, at 6.4-5.9 Ma, 4.9-4.4 Ma and 1.1-0.8 Ma, potentially indicative of warmer, less stable ice sheets at these times. Conversely, the accumulation of Antarctic-derived material is comparatively less during the middle of the Pliocene warm epoch (4.8-3.2 Ma). The deep flow forming the Kerguelen drift was stronger during the latest Miocene and earliest Pliocene and has decreased in intensity continuously since then. |
format |
Other/Unknown Material |
author |
Joseph, Leah H Rea, David K van der Pluijm, Ben A Gleason, James D |
author_facet |
Joseph, Leah H Rea, David K van der Pluijm, Ben A Gleason, James D |
author_sort |
Joseph, Leah H |
title |
Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau |
title_short |
Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau |
title_full |
Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau |
title_fullStr |
Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau |
title_full_unstemmed |
Sedimentology and Lead and Strontium isotope ratios of Miocene sediments from the Kerguelen Plateau |
title_sort |
sedimentology and lead and strontium isotope ratios of miocene sediments from the kerguelen plateau |
publisher |
PANGAEA |
publishDate |
2002 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.713614 https://doi.org/10.1594/PANGAEA.713614 |
op_coverage |
LATITUDE: -59.595000 * LONGITUDE: 85.854200 * DATE/TIME START: 1988-02-08T00:00:00 * DATE/TIME END: 1988-02-10T17:15:00 |
long_lat |
ENVELOPE(85.854200,85.854200,-59.595000,-59.595000) |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_source |
Supplement to: Joseph, Leah H; Rea, David K; van der Pluijm, Ben A; Gleason, James D (2002): Antarctic environmental variability since the late Miocene: ODP Site 745, the East Kerguelen sediment drift. Earth and Planetary Science Letters, 201(1), 127-142, https://doi.org/10.1016/S0012-821X(02)00661-1 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.713614 https://doi.org/10.1594/PANGAEA.713614 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.71361410.1016/S0012-821X(02)00661-1 |
_version_ |
1810493780767277056 |