Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ...
High-resolution bio- and chemostratigraphy of an earliest Pliocene section from ODP Site 652 indicates that postflood paleoceanographic conditions in the Tyrrhenian Sea can be sub-divided into two discrete intervals. The first is manifested by an acme of Sphaeroidinellopsis spp., increasing carbonat...
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ftdatacite:10.1594/pangaea.746047 2024-09-15T18:31:03+00:00 Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ... McKenzie, Judith A Sprovieri, Rodolfo 1990 application/zip https://dx.doi.org/10.1594/pangaea.746047 https://doi.pangaea.de/10.1594/PANGAEA.746047 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.107.162.1990 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg107 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1990 ftdatacite https://doi.org/10.1594/pangaea.74604710.2973/odp.proc.sr.107.162.1990 2024-08-01T10:54:23Z High-resolution bio- and chemostratigraphy of an earliest Pliocene section from ODP Site 652 indicates that postflood paleoceanographic conditions in the Tyrrhenian Sea can be sub-divided into two discrete intervals. The first is manifested by an acme of Sphaeroidinellopsis spp., increasing carbonate contents, and a progressive decrease upsection in both the d13C and dl8O values of the planktonic foraminifera. The lower part of the acme interval contains unusual surface-to-bottom water isotope gradients suggesting a stratification of two water masses. Normal gradients in the upper part of the acme interval suggest a well-mixed water body. Between the end of the acme interval and the MP11/MP12 boundary, denoted by the first occurrence (F.O.) of Globorotalia margaritae, a migrational first appearance, there was a catastrophic collapse of the gradient marking an onset of the second post-flood interval. The disintegration of habitable conditions is suggested by a sharp decrease in carbonate content and the ... : Supplement to: McKenzie, Judith A; Sprovieri, Rodolfo (1990): Paleoceanographic conditions following the earliest Pliocene flooding of the Tyrrhenian Sea. In: Kastens, KA; Mascle, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 107, 405-414 ... Article in Journal/Newspaper Planktonic foraminifera DataCite |
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Open Polar |
collection |
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ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg107 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg107 Joides Resolution Ocean Drilling Program ODP McKenzie, Judith A Sprovieri, Rodolfo Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ... |
topic_facet |
Drilling/drill rig Leg107 Joides Resolution Ocean Drilling Program ODP |
description |
High-resolution bio- and chemostratigraphy of an earliest Pliocene section from ODP Site 652 indicates that postflood paleoceanographic conditions in the Tyrrhenian Sea can be sub-divided into two discrete intervals. The first is manifested by an acme of Sphaeroidinellopsis spp., increasing carbonate contents, and a progressive decrease upsection in both the d13C and dl8O values of the planktonic foraminifera. The lower part of the acme interval contains unusual surface-to-bottom water isotope gradients suggesting a stratification of two water masses. Normal gradients in the upper part of the acme interval suggest a well-mixed water body. Between the end of the acme interval and the MP11/MP12 boundary, denoted by the first occurrence (F.O.) of Globorotalia margaritae, a migrational first appearance, there was a catastrophic collapse of the gradient marking an onset of the second post-flood interval. The disintegration of habitable conditions is suggested by a sharp decrease in carbonate content and the ... : Supplement to: McKenzie, Judith A; Sprovieri, Rodolfo (1990): Paleoceanographic conditions following the earliest Pliocene flooding of the Tyrrhenian Sea. In: Kastens, KA; Mascle, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 107, 405-414 ... |
format |
Article in Journal/Newspaper |
author |
McKenzie, Judith A Sprovieri, Rodolfo |
author_facet |
McKenzie, Judith A Sprovieri, Rodolfo |
author_sort |
McKenzie, Judith A |
title |
Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ... |
title_short |
Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ... |
title_full |
Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ... |
title_fullStr |
Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ... |
title_full_unstemmed |
Stable carbon and oxygen isotopes of foraminifera fand carbon content of ODP Leg 107 holes ... |
title_sort |
stable carbon and oxygen isotopes of foraminifera fand carbon content of odp leg 107 holes ... |
publisher |
PANGAEA |
publishDate |
1990 |
url |
https://dx.doi.org/10.1594/pangaea.746047 https://doi.pangaea.de/10.1594/PANGAEA.746047 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.107.162.1990 |
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.74604710.2973/odp.proc.sr.107.162.1990 |
_version_ |
1810472642279374848 |