Marine osmium isotope record across the Cretaceous-Tertiary boundary ...

A composite late Maastrichtian (65.5 to 68.5 Ma) marine osmium (Os) isotope record, based on samples from the Southern Ocean (ODP Site 690), the Tropical Pacific Ocean (DSDP Site 577), the South Atlantic (DSDP Site 525) and the paleo-Tethys Ocean demonstrates that subaerially exposed pelagic carbona...

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Main Authors: Robinson, Nicole, Ravizza, Gregory E, Coccioni, Rodolfo, Peucker-Ehrenbrink, Bernhard, Norris, Richard D
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.785723
https://doi.pangaea.de/10.1594/PANGAEA.785723
id ftdatacite:10.1594/pangaea.785723
record_format openpolar
spelling ftdatacite:10.1594/pangaea.785723 2024-09-30T14:43:36+00:00 Marine osmium isotope record across the Cretaceous-Tertiary boundary ... Robinson, Nicole Ravizza, Gregory E Coccioni, Rodolfo Peucker-Ehrenbrink, Bernhard Norris, Richard D 2009 application/zip https://dx.doi.org/10.1594/pangaea.785723 https://doi.pangaea.de/10.1594/PANGAEA.785723 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2009.02.019 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2009 ftdatacite https://doi.org/10.1594/pangaea.78572310.1016/j.epsl.2009.02.019 2024-09-02T08:36:09Z A composite late Maastrichtian (65.5 to 68.5 Ma) marine osmium (Os) isotope record, based on samples from the Southern Ocean (ODP Site 690), the Tropical Pacific Ocean (DSDP Site 577), the South Atlantic (DSDP Site 525) and the paleo-Tethys Ocean demonstrates that subaerially exposed pelagic carbonates can record seawater Os isotope variations with a fidelity comparable to sediments recovered from the seafloor. New results provide robust evidence of a 20% decline in seawater 187Os/188Os over a period of about 200 kyr early in magnetochron C29r well below the Cretaceous-Paleogene Boundary (KPB), confirming previously reported low-resolution data from the South Atlantic Ocean. New results also confirm a second more rapid decline in 187Os/188Os associated with the KPB that is accompanied by a significant increase in Os concentrations. Complementary platinum (Pt) and iridium (Ir) concentration data indicate that the length scale of diagenetic remobilization of platinum group elements from the KPB is less than 1 ... : Supplement to: Robinson, Nicole; Ravizza, Gregory E; Coccioni, Rodolfo; Peucker-Ehrenbrink, Bernhard; Norris, Richard D (2009): A high-resolution marine 187Os/188Os record for the late Maastrichtian: Distinguishing the chemical fingerprints of Deccan volcanism and the KP impact event. Earth and Planetary Science Letters, 281(3-4), 159-168 ... Article in Journal/Newspaper South Atlantic Ocean Southern Ocean DataCite Pacific Southern Ocean
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
spellingShingle Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
Robinson, Nicole
Ravizza, Gregory E
Coccioni, Rodolfo
Peucker-Ehrenbrink, Bernhard
Norris, Richard D
Marine osmium isotope record across the Cretaceous-Tertiary boundary ...
topic_facet Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
description A composite late Maastrichtian (65.5 to 68.5 Ma) marine osmium (Os) isotope record, based on samples from the Southern Ocean (ODP Site 690), the Tropical Pacific Ocean (DSDP Site 577), the South Atlantic (DSDP Site 525) and the paleo-Tethys Ocean demonstrates that subaerially exposed pelagic carbonates can record seawater Os isotope variations with a fidelity comparable to sediments recovered from the seafloor. New results provide robust evidence of a 20% decline in seawater 187Os/188Os over a period of about 200 kyr early in magnetochron C29r well below the Cretaceous-Paleogene Boundary (KPB), confirming previously reported low-resolution data from the South Atlantic Ocean. New results also confirm a second more rapid decline in 187Os/188Os associated with the KPB that is accompanied by a significant increase in Os concentrations. Complementary platinum (Pt) and iridium (Ir) concentration data indicate that the length scale of diagenetic remobilization of platinum group elements from the KPB is less than 1 ... : Supplement to: Robinson, Nicole; Ravizza, Gregory E; Coccioni, Rodolfo; Peucker-Ehrenbrink, Bernhard; Norris, Richard D (2009): A high-resolution marine 187Os/188Os record for the late Maastrichtian: Distinguishing the chemical fingerprints of Deccan volcanism and the KP impact event. Earth and Planetary Science Letters, 281(3-4), 159-168 ...
format Article in Journal/Newspaper
author Robinson, Nicole
Ravizza, Gregory E
Coccioni, Rodolfo
Peucker-Ehrenbrink, Bernhard
Norris, Richard D
author_facet Robinson, Nicole
Ravizza, Gregory E
Coccioni, Rodolfo
Peucker-Ehrenbrink, Bernhard
Norris, Richard D
author_sort Robinson, Nicole
title Marine osmium isotope record across the Cretaceous-Tertiary boundary ...
title_short Marine osmium isotope record across the Cretaceous-Tertiary boundary ...
title_full Marine osmium isotope record across the Cretaceous-Tertiary boundary ...
title_fullStr Marine osmium isotope record across the Cretaceous-Tertiary boundary ...
title_full_unstemmed Marine osmium isotope record across the Cretaceous-Tertiary boundary ...
title_sort marine osmium isotope record across the cretaceous-tertiary boundary ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.785723
https://doi.pangaea.de/10.1594/PANGAEA.785723
geographic Pacific
Southern Ocean
geographic_facet Pacific
Southern Ocean
genre South Atlantic Ocean
Southern Ocean
genre_facet South Atlantic Ocean
Southern Ocean
op_relation https://dx.doi.org/10.1016/j.epsl.2009.02.019
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.78572310.1016/j.epsl.2009.02.019
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