Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ...
Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y. At Ocean Drilling Program (ODP) Site 1101 (Leg 178), which recovered sediments back to 3.1 Ma, glacial-inter...
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ftdatacite:10.1594/pangaea.706581 2024-09-15T17:47:23+00:00 Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ... Cowan, Ellen A Hillenbrand, Claus-Dieter Hassler, Lauren E Ake, Matthew T 2008 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.706581 https://doi.pangaea.de/10.1594/PANGAEA.706581 en eng PANGAEA https://dx.doi.org/10.1016/j.palaeo.2008.03.010 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock AGE Sample code/label Roundness Quartz, surface texture Quartz Comment Drilling/drill rig DSDP/ODP/IODP sample designation Scanning electron microscope SEM Counting 250-2000 µm fraction Leg178 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 2008 ftdatacite https://doi.org/10.1594/pangaea.70658110.1016/j.palaeo.2008.03.010 2024-08-01T10:51:01Z Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y. At Ocean Drilling Program (ODP) Site 1101 (Leg 178), which recovered sediments back to 3.1 Ma, glacial-interglacial cyclicity was identified based on the biogenic component and sedimentary structures observed in X-radiographs, magnetic susceptibility and lithofacies descriptions. Glacial intervals are dominated by fine-grained laminated mud and interglacial units consist of bioturbated muds enriched in biogenic components. From 2.2 to 0.76 Ma, planktonic foraminifera and calcareous nannofossils dominate in the interglacials suggesting a shift of the Antarctic Polar Front (APF) to the south near the drifts. Prior to 2.2 Ma, cyclicity cannot be identified and diatoms dominate the biogenic component and high percent opal suggests warmer conditions south of the APF and reduced sea ice over the drifts. Analyses of the ... : The composite depth scales and age models of Barker (2002, doi:10.2973/odp.proc.sr.178.219.2001) were used to develop a chronology. The age of each sample collected from Sites 1101 was computed by linear interpolation between magnetostratigraphic datums from Acton et al. (2002, doi:10.2973/odp.proc.sr.178.235.2002). ... Dataset Antarc* Antarctic Antarctic Peninsula Planktonic foraminifera Sea ice DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock AGE Sample code/label Roundness Quartz, surface texture Quartz Comment Drilling/drill rig DSDP/ODP/IODP sample designation Scanning electron microscope SEM Counting 250-2000 µm fraction Leg178 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
DEPTH, sediment/rock AGE Sample code/label Roundness Quartz, surface texture Quartz Comment Drilling/drill rig DSDP/ODP/IODP sample designation Scanning electron microscope SEM Counting 250-2000 µm fraction Leg178 Joides Resolution Ocean Drilling Program ODP Cowan, Ellen A Hillenbrand, Claus-Dieter Hassler, Lauren E Ake, Matthew T Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ... |
topic_facet |
DEPTH, sediment/rock AGE Sample code/label Roundness Quartz, surface texture Quartz Comment Drilling/drill rig DSDP/ODP/IODP sample designation Scanning electron microscope SEM Counting 250-2000 µm fraction Leg178 Joides Resolution Ocean Drilling Program ODP |
description |
Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y. At Ocean Drilling Program (ODP) Site 1101 (Leg 178), which recovered sediments back to 3.1 Ma, glacial-interglacial cyclicity was identified based on the biogenic component and sedimentary structures observed in X-radiographs, magnetic susceptibility and lithofacies descriptions. Glacial intervals are dominated by fine-grained laminated mud and interglacial units consist of bioturbated muds enriched in biogenic components. From 2.2 to 0.76 Ma, planktonic foraminifera and calcareous nannofossils dominate in the interglacials suggesting a shift of the Antarctic Polar Front (APF) to the south near the drifts. Prior to 2.2 Ma, cyclicity cannot be identified and diatoms dominate the biogenic component and high percent opal suggests warmer conditions south of the APF and reduced sea ice over the drifts. Analyses of the ... : The composite depth scales and age models of Barker (2002, doi:10.2973/odp.proc.sr.178.219.2001) were used to develop a chronology. The age of each sample collected from Sites 1101 was computed by linear interpolation between magnetostratigraphic datums from Acton et al. (2002, doi:10.2973/odp.proc.sr.178.235.2002). ... |
format |
Dataset |
author |
Cowan, Ellen A Hillenbrand, Claus-Dieter Hassler, Lauren E Ake, Matthew T |
author_facet |
Cowan, Ellen A Hillenbrand, Claus-Dieter Hassler, Lauren E Ake, Matthew T |
author_sort |
Cowan, Ellen A |
title |
Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ... |
title_short |
Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ... |
title_full |
Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ... |
title_fullStr |
Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ... |
title_full_unstemmed |
Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1) ... |
title_sort |
occurrence of microtextures recorded from quartz sand grains of odp hole 178-1101a (table 1) ... |
publisher |
PANGAEA |
publishDate |
2008 |
url |
https://dx.doi.org/10.1594/pangaea.706581 https://doi.pangaea.de/10.1594/PANGAEA.706581 |
genre |
Antarc* Antarctic Antarctic Peninsula Planktonic foraminifera Sea ice |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Planktonic foraminifera Sea ice |
op_relation |
https://dx.doi.org/10.1016/j.palaeo.2008.03.010 |
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.70658110.1016/j.palaeo.2008.03.010 |
_version_ |
1810496648553431040 |