(Table T1) Geochemical composition of ODP Site 177-1089 sediments ...
A primary objective of Ocean Drilling Program Leg 177 was to document changes in circulation and biogeochemical cycling on glacial/interglacial time scales across a wide latitudinal range of the south Atlantic Ocean. One of the more northerly sites drilled, Site 1089 (41°S, 10°E), is located within...
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ftdatacite:10.1594/pangaea.787340 2024-06-09T07:49:34+00:00 (Table T1) Geochemical composition of ODP Site 177-1089 sediments ... Latimer, Jennifer C Filipelli, Gabriel M 2001 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.787340 https://doi.pangaea.de/10.1594/PANGAEA.787340 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.177.102.2001 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label DEPTH, sediment/rock Phosphorus Titanium Barium Cadmium Zinc Manganese Strontium Magnesium Iron Aluminium Calcium Composite Core DSDP/ODP/IODP sample designation Inductively coupled plasma atomic emission spectroscope ICP-AES Leg177 Joides Resolution Ocean Drilling Program ODP Supplementary Dataset dataset Dataset 2001 ftdatacite https://doi.org/10.1594/pangaea.78734010.2973/odp.proc.sr.177.102.2001 2024-05-13T12:06:36Z A primary objective of Ocean Drilling Program Leg 177 was to document changes in circulation and biogeochemical cycling on glacial/interglacial time scales across a wide latitudinal range of the south Atlantic Ocean. One of the more northerly sites drilled, Site 1089 (41°S, 10°E), is located within the present-day Subantarctic Zone, south of the Subtropical Front. The drilling site itself is located in the southern Cape Basin at a water depth of 4620 m. Pleistocene sediments at this site are dominated by interbedded carbonate and opal oozes. Initial shipboard stratigraphy identified the opal-rich sediments as deposited during glacial intervals and the carbonate-rich sediments as deposited during interglacial intervals (Gersonde, Hodell, Blum, et al., 1999, doi:10.2973/odp.proc.ir.177.1999). Postcruise isotopic stratigraphy, however, verified that this site displayed a Pacific Pleistocene sedimentation pattern with glacial intervals marked by high carbonate content (Hodell and Charles, 1999).To assess changes ... : Sediment depth is given in mcd. ... Dataset South Atlantic Ocean DataCite Metadata Store (German National Library of Science and Technology) Pacific |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
English |
topic |
Sample code/label DEPTH, sediment/rock Phosphorus Titanium Barium Cadmium Zinc Manganese Strontium Magnesium Iron Aluminium Calcium Composite Core DSDP/ODP/IODP sample designation Inductively coupled plasma atomic emission spectroscope ICP-AES Leg177 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Sample code/label DEPTH, sediment/rock Phosphorus Titanium Barium Cadmium Zinc Manganese Strontium Magnesium Iron Aluminium Calcium Composite Core DSDP/ODP/IODP sample designation Inductively coupled plasma atomic emission spectroscope ICP-AES Leg177 Joides Resolution Ocean Drilling Program ODP Latimer, Jennifer C Filipelli, Gabriel M (Table T1) Geochemical composition of ODP Site 177-1089 sediments ... |
topic_facet |
Sample code/label DEPTH, sediment/rock Phosphorus Titanium Barium Cadmium Zinc Manganese Strontium Magnesium Iron Aluminium Calcium Composite Core DSDP/ODP/IODP sample designation Inductively coupled plasma atomic emission spectroscope ICP-AES Leg177 Joides Resolution Ocean Drilling Program ODP |
description |
A primary objective of Ocean Drilling Program Leg 177 was to document changes in circulation and biogeochemical cycling on glacial/interglacial time scales across a wide latitudinal range of the south Atlantic Ocean. One of the more northerly sites drilled, Site 1089 (41°S, 10°E), is located within the present-day Subantarctic Zone, south of the Subtropical Front. The drilling site itself is located in the southern Cape Basin at a water depth of 4620 m. Pleistocene sediments at this site are dominated by interbedded carbonate and opal oozes. Initial shipboard stratigraphy identified the opal-rich sediments as deposited during glacial intervals and the carbonate-rich sediments as deposited during interglacial intervals (Gersonde, Hodell, Blum, et al., 1999, doi:10.2973/odp.proc.ir.177.1999). Postcruise isotopic stratigraphy, however, verified that this site displayed a Pacific Pleistocene sedimentation pattern with glacial intervals marked by high carbonate content (Hodell and Charles, 1999).To assess changes ... : Sediment depth is given in mcd. ... |
format |
Dataset |
author |
Latimer, Jennifer C Filipelli, Gabriel M |
author_facet |
Latimer, Jennifer C Filipelli, Gabriel M |
author_sort |
Latimer, Jennifer C |
title |
(Table T1) Geochemical composition of ODP Site 177-1089 sediments ... |
title_short |
(Table T1) Geochemical composition of ODP Site 177-1089 sediments ... |
title_full |
(Table T1) Geochemical composition of ODP Site 177-1089 sediments ... |
title_fullStr |
(Table T1) Geochemical composition of ODP Site 177-1089 sediments ... |
title_full_unstemmed |
(Table T1) Geochemical composition of ODP Site 177-1089 sediments ... |
title_sort |
(table t1) geochemical composition of odp site 177-1089 sediments ... |
publisher |
PANGAEA |
publishDate |
2001 |
url |
https://dx.doi.org/10.1594/pangaea.787340 https://doi.pangaea.de/10.1594/PANGAEA.787340 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.177.102.2001 |
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.78734010.2973/odp.proc.sr.177.102.2001 |
_version_ |
1801382244398399488 |