Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ...

Ocean Drilling Program (ODP) Leg 207, on the Demerara Rise in the western tropical North Atlantic, recovered multiple Cretaceous-Paleogene boundary sections containing an ejecta layer. Sedimentological, geochemical, and paleontological changes across the boundary closely match patterns expected for...

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Main Authors: MacLeod, Kenneth G, Whitney, Donna L, Huber, Brian T, Koeberl, Christian
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.719608
https://doi.pangaea.de/10.1594/PANGAEA.719608
id ftdatacite:10.1594/pangaea.719608
record_format openpolar
spelling ftdatacite:10.1594/pangaea.719608 2024-09-30T14:39:23+00:00 Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ... MacLeod, Kenneth G Whitney, Donna L Huber, Brian T Koeberl, Christian 2007 application/zip https://dx.doi.org/10.1594/pangaea.719608 https://doi.pangaea.de/10.1594/PANGAEA.719608 en eng PANGAEA https://dx.doi.org/10.1130/b25955.1 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Drilling/drill rig Leg207 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2007 ftdatacite https://doi.org/10.1594/pangaea.71960810.1130/b25955.1 2024-09-02T08:37:33Z Ocean Drilling Program (ODP) Leg 207, on the Demerara Rise in the western tropical North Atlantic, recovered multiple Cretaceous-Paleogene boundary sections containing an ejecta layer. Sedimentological, geochemical, and paleontological changes across the boundary closely match patterns expected for a mass extinction caused by a single impact. A normally graded, ~2-cm-thick bed of spherules that is interpreted as a primary air-fall deposit of impact ejecta occurs between sediments of the highest Cretaceous Plummerita hantkeninoides foraminiferal zone and the lowest Paleogene P0 foraminiferal zone. There are no other spherule layers in the section. In addition to extinction of Cretaceous taxa, foraminiferal abundance drops from abundant to rare across the boundary. Ir concentrations reach a maximum of ~1.5 ppb at the top of the spherule bed, and the Ir anomaly is associated with enrichment in other siderophile elements. We attribute the unusually well-preserved and relatively simple stratigraphy to the fact ... : Supplement to: MacLeod, Kenneth G; Whitney, Donna L; Huber, Brian T; Koeberl, Christian (2007): Impact and extinction in remarkably complete Cretaceous-Tertiary boundary sections from Demerara Rise, tropical western North Atlantic. Geological Society of America Bulletin, 119(1-2), 101-115 ... Article in Journal/Newspaper North Atlantic DataCite Macleod ENVELOPE(-61.966,-61.966,-64.091,-64.091)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Drilling/drill rig
Leg207
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Composite Core
Drilling/drill rig
Leg207
Joides Resolution
Ocean Drilling Program ODP
MacLeod, Kenneth G
Whitney, Donna L
Huber, Brian T
Koeberl, Christian
Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ...
topic_facet Composite Core
Drilling/drill rig
Leg207
Joides Resolution
Ocean Drilling Program ODP
description Ocean Drilling Program (ODP) Leg 207, on the Demerara Rise in the western tropical North Atlantic, recovered multiple Cretaceous-Paleogene boundary sections containing an ejecta layer. Sedimentological, geochemical, and paleontological changes across the boundary closely match patterns expected for a mass extinction caused by a single impact. A normally graded, ~2-cm-thick bed of spherules that is interpreted as a primary air-fall deposit of impact ejecta occurs between sediments of the highest Cretaceous Plummerita hantkeninoides foraminiferal zone and the lowest Paleogene P0 foraminiferal zone. There are no other spherule layers in the section. In addition to extinction of Cretaceous taxa, foraminiferal abundance drops from abundant to rare across the boundary. Ir concentrations reach a maximum of ~1.5 ppb at the top of the spherule bed, and the Ir anomaly is associated with enrichment in other siderophile elements. We attribute the unusually well-preserved and relatively simple stratigraphy to the fact ... : Supplement to: MacLeod, Kenneth G; Whitney, Donna L; Huber, Brian T; Koeberl, Christian (2007): Impact and extinction in remarkably complete Cretaceous-Tertiary boundary sections from Demerara Rise, tropical western North Atlantic. Geological Society of America Bulletin, 119(1-2), 101-115 ...
format Article in Journal/Newspaper
author MacLeod, Kenneth G
Whitney, Donna L
Huber, Brian T
Koeberl, Christian
author_facet MacLeod, Kenneth G
Whitney, Donna L
Huber, Brian T
Koeberl, Christian
author_sort MacLeod, Kenneth G
title Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ...
title_short Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ...
title_full Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ...
title_fullStr Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ...
title_full_unstemmed Composition of sediments samples spanning the Cretaceous-Tertiary boundary at ODP Site 207-1259 ...
title_sort composition of sediments samples spanning the cretaceous-tertiary boundary at odp site 207-1259 ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.719608
https://doi.pangaea.de/10.1594/PANGAEA.719608
long_lat ENVELOPE(-61.966,-61.966,-64.091,-64.091)
geographic Macleod
geographic_facet Macleod
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1130/b25955.1
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.71960810.1130/b25955.1
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