Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ...
Oxygen isotopic compositions of the tests of planktonic foraminifera from several Deep Sea Drilling Project sites provide a general picture of low-latitude marine temperatures from Maastrichtian time to the present. Bottom temperatures determined from the isotopic compositions of benthonic foraminif...
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Online Access: | https://dx.doi.org/10.1594/pangaea.720968 https://doi.pangaea.de/10.1594/PANGAEA.720968 |
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ftdatacite:10.1594/pangaea.720968 2024-09-15T18:31:03+00:00 Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ... Savin, Samuel M Douglas, Robert G Stehli, Francis G 1975 application/zip https://dx.doi.org/10.1594/pangaea.720968 https://doi.pangaea.de/10.1594/PANGAEA.720968 en eng PANGAEA ftp://rock.geosociety.org/pub/reposit/1975/7526.pdf https://dx.doi.org/10.1130/0016-7606(1975)86<1499:tmp>2.0.co;2 ftp://rock.geosociety.org/pub/reposit/1975/7526.pdf Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Piston corer Leg3 Leg6 Leg7 Leg8 Leg9 Leg17 ELT21 ELT24 Glomar Challenger Eltanin Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1975 ftdatacite https://doi.org/10.1594/pangaea.72096810.1130/0016-7606(1975)86<1499:tmp>2.0.co;2 2024-08-01T10:54:44Z Oxygen isotopic compositions of the tests of planktonic foraminifera from several Deep Sea Drilling Project sites provide a general picture of low-latitude marine temperatures from Maastrichtian time to the present. Bottom temperatures determined from the isotopic compositions of benthonic foraminifera are interpreted as being indicative of high-latitude surface temperatures. Prior to the beginning of middle Miocene time, high- and low-latitude temperatures changed in parallel fashion. Following an apparently small and short-lived drop in temperature near the Tertiary-Cretaceous boundary, temperatures remained warm and relatively constant through Paleocene and early and middle Eocene time; bottom temperatures then were on the order of 12°C. A sharp temperature drop in late Eocene time was followed by a more gradual lowering of temperature, culminating in a late Oligocene high-latitude temperature minimum of about 4°C. A temperature rise through early Miocene time was followed in middle Miocene time by a ... : Supplement to: Savin, Samuel M; Douglas, Robert G; Stehli, Francis G (1975): Tertiary marine paleotemperatures. Geological Society of America Bulletin, 86(11), 1499-1510 ... Article in Journal/Newspaper Planktonic foraminifera DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Piston corer Leg3 Leg6 Leg7 Leg8 Leg9 Leg17 ELT21 ELT24 Glomar Challenger Eltanin Deep Sea Drilling Project DSDP |
spellingShingle |
Drilling/drill rig Piston corer Leg3 Leg6 Leg7 Leg8 Leg9 Leg17 ELT21 ELT24 Glomar Challenger Eltanin Deep Sea Drilling Project DSDP Savin, Samuel M Douglas, Robert G Stehli, Francis G Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ... |
topic_facet |
Drilling/drill rig Piston corer Leg3 Leg6 Leg7 Leg8 Leg9 Leg17 ELT21 ELT24 Glomar Challenger Eltanin Deep Sea Drilling Project DSDP |
description |
Oxygen isotopic compositions of the tests of planktonic foraminifera from several Deep Sea Drilling Project sites provide a general picture of low-latitude marine temperatures from Maastrichtian time to the present. Bottom temperatures determined from the isotopic compositions of benthonic foraminifera are interpreted as being indicative of high-latitude surface temperatures. Prior to the beginning of middle Miocene time, high- and low-latitude temperatures changed in parallel fashion. Following an apparently small and short-lived drop in temperature near the Tertiary-Cretaceous boundary, temperatures remained warm and relatively constant through Paleocene and early and middle Eocene time; bottom temperatures then were on the order of 12°C. A sharp temperature drop in late Eocene time was followed by a more gradual lowering of temperature, culminating in a late Oligocene high-latitude temperature minimum of about 4°C. A temperature rise through early Miocene time was followed in middle Miocene time by a ... : Supplement to: Savin, Samuel M; Douglas, Robert G; Stehli, Francis G (1975): Tertiary marine paleotemperatures. Geological Society of America Bulletin, 86(11), 1499-1510 ... |
format |
Article in Journal/Newspaper |
author |
Savin, Samuel M Douglas, Robert G Stehli, Francis G |
author_facet |
Savin, Samuel M Douglas, Robert G Stehli, Francis G |
author_sort |
Savin, Samuel M |
title |
Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ... |
title_short |
Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ... |
title_full |
Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ... |
title_fullStr |
Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ... |
title_full_unstemmed |
Isotopic composition of foraminifera from sediments of DSDP Legs 3, 6-9, 17 ... |
title_sort |
isotopic composition of foraminifera from sediments of dsdp legs 3, 6-9, 17 ... |
publisher |
PANGAEA |
publishDate |
1975 |
url |
https://dx.doi.org/10.1594/pangaea.720968 https://doi.pangaea.de/10.1594/PANGAEA.720968 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
ftp://rock.geosociety.org/pub/reposit/1975/7526.pdf https://dx.doi.org/10.1130/0016-7606(1975)86<1499:tmp>2.0.co;2 ftp://rock.geosociety.org/pub/reposit/1975/7526.pdf |
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.72096810.1130/0016-7606(1975)86<1499:tmp>2.0.co;2 |
_version_ |
1810472635814903808 |