Neogene and Quaternary planktonic foraminifera of the Baffin Bay ...

During Ocean Drilling Program Leg 105, 11 holes were drilled in the Labrador Sea and Baffin Bay. Site 645 in Baffin Bay was drilled to a depth of 1147 meters below seafloor (mbsf); planktonic foraminifers were recovered in the upper 110.3 m and in a short interval between 283.8 and 293.5 mbsf. Low s...

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Bibliographic Details
Main Authors: Aksu, Ali E, Kaminski, Michael Anthony
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.744966
https://doi.pangaea.de/10.1594/PANGAEA.744966
id ftdatacite:10.1594/pangaea.744966
record_format openpolar
spelling ftdatacite:10.1594/pangaea.744966 2023-05-15T15:34:57+02:00 Neogene and Quaternary planktonic foraminifera of the Baffin Bay ... Aksu, Ali E Kaminski, Michael Anthony 1989 application/zip https://dx.doi.org/10.1594/pangaea.744966 https://doi.pangaea.de/10.1594/PANGAEA.744966 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.105.122.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg105 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1989 ftdatacite https://doi.org/10.1594/pangaea.74496610.2973/odp.proc.sr.105.122.1989 2023-04-03T13:12:12Z During Ocean Drilling Program Leg 105, 11 holes were drilled in the Labrador Sea and Baffin Bay. Site 645 in Baffin Bay was drilled to a depth of 1147 meters below seafloor (mbsf); planktonic foraminifers were recovered in the upper 110.3 m and in a short interval between 283.8 and 293.5 mbsf. Low species diversity and the lack of species with short stratigraphic ranges inhibited establishment of a planktonic foraminifer biostratigraphic framework at Site 645. Holes 646B and 647A in the Labrador Sea were drilled to depths of 766.7 and 716.6 mbsf, respectively. Although the observed assemblages in the Labrador Sea holes were of low diversity, the first and last occurrences of several age-diagnostic species, when integrated with paleomagnetic stratigraphy, allowed the establishment of a high-latitude Miocene to Holocene planktonic foraminifer biochronology. To determine the relative timing of planktonic foraminifer datum events in the eastern North Atlantic and the Labrador Sea, this biochronology is compared ... : Supplement to: Aksu, Ali E; Kaminski, Michael Anthony (1989): Neogene and Quaternary planktonic foraminifer biostratigraphy and biochronology in Baffin Bay and the Lareador Sea. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 287-304 ... Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Labrador Sea North Atlantic Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Baffin Bay
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
Aksu, Ali E
Kaminski, Michael Anthony
Neogene and Quaternary planktonic foraminifera of the Baffin Bay ...
topic_facet Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
description During Ocean Drilling Program Leg 105, 11 holes were drilled in the Labrador Sea and Baffin Bay. Site 645 in Baffin Bay was drilled to a depth of 1147 meters below seafloor (mbsf); planktonic foraminifers were recovered in the upper 110.3 m and in a short interval between 283.8 and 293.5 mbsf. Low species diversity and the lack of species with short stratigraphic ranges inhibited establishment of a planktonic foraminifer biostratigraphic framework at Site 645. Holes 646B and 647A in the Labrador Sea were drilled to depths of 766.7 and 716.6 mbsf, respectively. Although the observed assemblages in the Labrador Sea holes were of low diversity, the first and last occurrences of several age-diagnostic species, when integrated with paleomagnetic stratigraphy, allowed the establishment of a high-latitude Miocene to Holocene planktonic foraminifer biochronology. To determine the relative timing of planktonic foraminifer datum events in the eastern North Atlantic and the Labrador Sea, this biochronology is compared ... : Supplement to: Aksu, Ali E; Kaminski, Michael Anthony (1989): Neogene and Quaternary planktonic foraminifer biostratigraphy and biochronology in Baffin Bay and the Lareador Sea. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 287-304 ...
format Article in Journal/Newspaper
author Aksu, Ali E
Kaminski, Michael Anthony
author_facet Aksu, Ali E
Kaminski, Michael Anthony
author_sort Aksu, Ali E
title Neogene and Quaternary planktonic foraminifera of the Baffin Bay ...
title_short Neogene and Quaternary planktonic foraminifera of the Baffin Bay ...
title_full Neogene and Quaternary planktonic foraminifera of the Baffin Bay ...
title_fullStr Neogene and Quaternary planktonic foraminifera of the Baffin Bay ...
title_full_unstemmed Neogene and Quaternary planktonic foraminifera of the Baffin Bay ...
title_sort neogene and quaternary planktonic foraminifera of the baffin bay ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.744966
https://doi.pangaea.de/10.1594/PANGAEA.744966
geographic Baffin Bay
geographic_facet Baffin Bay
genre Baffin Bay
Baffin Bay
Baffin
Labrador Sea
North Atlantic
Planktonic foraminifera
genre_facet Baffin Bay
Baffin Bay
Baffin
Labrador Sea
North Atlantic
Planktonic foraminifera
op_relation https://dx.doi.org/10.2973/odp.proc.sr.105.122.1989
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.74496610.2973/odp.proc.sr.105.122.1989
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