A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian

M.S. University of Hawaii at Manoa 2016. Includes bibliographical references. The marine osmium (Os) isotope record can potentially act as an independent proxy indicator of major volcanic activity, marked by decreases in seawater 187Os/188Os to more mantle-like values. A composite late Maastrichtian...

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Main Author: Robinson, Nicole
Format: Thesis
Language:English
Published: [Honolulu] : [University of Hawaii at Manoa], [August 2016] 2016
Subjects:
Online Access:http://hdl.handle.net/10125/51464
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spelling ftunivhawaiimano:oai:scholarspace.manoa.hawaii.edu:10125/51464 2023-05-15T18:25:47+02:00 A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian Robinson, Nicole 2016-08 application/pdf http://hdl.handle.net/10125/51464 eng eng [Honolulu] : [University of Hawaii at Manoa], [August 2016] Theses for the degree of Master of Science (University of Hawaii at Manoa). Geology & Geophysics http://hdl.handle.net/10125/51464 Osmium isotopes Maastrichtian K-Pg Deccan Large igneous provinces Thesis Text 2016 ftunivhawaiimano 2022-07-17T13:07:55Z M.S. University of Hawaii at Manoa 2016. Includes bibliographical references. The marine osmium (Os) isotope record can potentially act as an independent proxy indicator of major volcanic activity, marked by decreases in seawater 187Os/188Os to more mantle-like values. A composite late Maastrichtian (66 to 68.5 Ma) marine Os record, based on bulk sediment samples from the Southern Ocean (Ocean Drilling Program (ODP) Site 690), the Tropical Pacific Ocean (Deep Sea Drilling Project (DSDP) Site 577), the South Atlantic (DSDP Site 525) and the paleo-Tethys Ocean, provides robust evidence of a 20% decline in seawater 187Os/188Os over a period of about 200 ka early in magnetochron C29r, ending approximately 200 ka before the Cretaceous-Paleogene (K-Pg) boundary (Robinson et al., 2009). This shift in 187Os/188Os is interpreted as a chemostratigraphic marker of Deccan volcanism, and is temporally separate from the Os isotope excursion associated with the Chicxulub impact at the K-Pg boundary. Improved geochronologic data constraining the eruptive history of the Deccan (Renne et al., 2015; Schoene et al., 2015), as well as Os isotope records coinciding with other episodes of large igneous province (LIP) eruption (Duvivier et al., 2015; Bottini et al., 2012; Kuroda et al., 2010), provide a new and larger context for understanding the response of the marine Os record to LIP emplacement. Comparison of Os isotope records coinciding with other LIP events to the Deccan/K-Pg record reveal important differences in the structure and duration of shifts in the Os isotope record, and precludes a single interpretation of all LIP-associated Os isotope excursions. Thesis Southern Ocean renne ScholarSpace at University of Hawaii at Manoa Pacific Renne ENVELOPE(9.698,9.698,63.505,63.505) Southern Ocean
institution Open Polar
collection ScholarSpace at University of Hawaii at Manoa
op_collection_id ftunivhawaiimano
language English
topic Osmium isotopes
Maastrichtian
K-Pg
Deccan
Large igneous provinces
spellingShingle Osmium isotopes
Maastrichtian
K-Pg
Deccan
Large igneous provinces
Robinson, Nicole
A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian
topic_facet Osmium isotopes
Maastrichtian
K-Pg
Deccan
Large igneous provinces
description M.S. University of Hawaii at Manoa 2016. Includes bibliographical references. The marine osmium (Os) isotope record can potentially act as an independent proxy indicator of major volcanic activity, marked by decreases in seawater 187Os/188Os to more mantle-like values. A composite late Maastrichtian (66 to 68.5 Ma) marine Os record, based on bulk sediment samples from the Southern Ocean (Ocean Drilling Program (ODP) Site 690), the Tropical Pacific Ocean (Deep Sea Drilling Project (DSDP) Site 577), the South Atlantic (DSDP Site 525) and the paleo-Tethys Ocean, provides robust evidence of a 20% decline in seawater 187Os/188Os over a period of about 200 ka early in magnetochron C29r, ending approximately 200 ka before the Cretaceous-Paleogene (K-Pg) boundary (Robinson et al., 2009). This shift in 187Os/188Os is interpreted as a chemostratigraphic marker of Deccan volcanism, and is temporally separate from the Os isotope excursion associated with the Chicxulub impact at the K-Pg boundary. Improved geochronologic data constraining the eruptive history of the Deccan (Renne et al., 2015; Schoene et al., 2015), as well as Os isotope records coinciding with other episodes of large igneous province (LIP) eruption (Duvivier et al., 2015; Bottini et al., 2012; Kuroda et al., 2010), provide a new and larger context for understanding the response of the marine Os record to LIP emplacement. Comparison of Os isotope records coinciding with other LIP events to the Deccan/K-Pg record reveal important differences in the structure and duration of shifts in the Os isotope record, and precludes a single interpretation of all LIP-associated Os isotope excursions.
format Thesis
author Robinson, Nicole
author_facet Robinson, Nicole
author_sort Robinson, Nicole
title A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian
title_short A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian
title_full A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian
title_fullStr A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian
title_full_unstemmed A High-Resolution Marine 187 OS / 188 OS Record for the Late Maastrichtian
title_sort high-resolution marine 187 os / 188 os record for the late maastrichtian
publisher [Honolulu] : [University of Hawaii at Manoa], [August 2016]
publishDate 2016
url http://hdl.handle.net/10125/51464
long_lat ENVELOPE(9.698,9.698,63.505,63.505)
geographic Pacific
Renne
Southern Ocean
geographic_facet Pacific
Renne
Southern Ocean
genre Southern Ocean
renne
genre_facet Southern Ocean
renne
op_relation Theses for the degree of Master of Science (University of Hawaii at Manoa). Geology & Geophysics
http://hdl.handle.net/10125/51464
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