(Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ...

Benthic foraminiferal data from Ocean Drilling Program Site 1098 indicate significant changes in deep-water conditions of the Palmer Deep, western Antarctic Peninsula margin, throughout the Holocene (13 ka to present). The earliest Holocene represents a period of transition from the Last Glacial Max...

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Bibliographic Details
Main Authors: Ishman, Scott E, Sperling, Michael R
Format: Dataset
Language:English
Published: PANGAEA 2002
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.713686
https://doi.pangaea.de/10.1594/PANGAEA.713686
id ftdatacite:10.1594/pangaea.713686
record_format openpolar
spelling ftdatacite:10.1594/pangaea.713686 2024-02-27T08:33:22+00:00 (Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ... Ishman, Scott E Sperling, Michael R 2002 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.713686 https://doi.pangaea.de/10.1594/PANGAEA.713686 en eng PANGAEA ftp://rock.geosociety.org/pub/reposit/2002/2002044.pdf https://dx.doi.org/10.1130/0091-7613(2002)030<0435:bfrohd>2.0.co;2 ftp://rock.geosociety.org/pub/reposit/2002/2002044.pdf Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 AGE Depth, composite Astrononion echolsi Bolivina pseudopunctata Bulimina aculeata Cibicides lobatulus Fursenkoina earlandi Fursenkoina fusiformis Globocassidulina biora Globocassidulina crassa rossensis Miliammina arenacea Nonionella iridea Pullenia bulloides Trifarina angulosa Trochammina intermedia Neogloboquadrina pachyderma Number of species Accumulation rate, benthic foraminifera by number Factor 1 Factor 2 Factor 3 Drilling/drill rig Counting >63 µm fraction Calculated Leg178 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 2002 ftdatacite https://doi.org/10.1594/pangaea.71368610.1130/0091-7613(2002)030<0435:bfrohd>2.0.co;2 2024-02-01T16:06:24Z Benthic foraminiferal data from Ocean Drilling Program Site 1098 indicate significant changes in deep-water conditions of the Palmer Deep, western Antarctic Peninsula margin, throughout the Holocene (13 ka to present). The earliest Holocene represents a period of transition from the Last Glacial Maximum (LGM). Cold bottom waters, similar to saline shelf water (SSW), dominated the middle Holocene. The late Holocene in the Palmer Deep has been characterized by alternating dominance of circumpolar deep water (CDW) and saline shelf water. These changes have global oceanographic and climatic implications. We suggest that the middle Holocene bottom-water record, in the absence of circumpolar deep water on the western Antarctic Peninsula shelf, indicates high saline shelf water production and/or weakened circumpolar deep water production during the middle Holocene climatic optimum. The late Holocene benthic foraminiferal record indicates rapidly fluctuating sea-ice conditions and may indicate a teleconnection ... : In the original table foraminiferal data are given without units. Units # used here are provisory. ... Dataset Antarc* Antarctic Antarctic Peninsula Neogloboquadrina pachyderma Sea ice DataCite Metadata Store (German National Library of Science and Technology) Antarctic Antarctic Peninsula Palmer Deep ENVELOPE(-64.400,-64.400,-64.950,-64.950)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic AGE
Depth, composite
Astrononion echolsi
Bolivina pseudopunctata
Bulimina aculeata
Cibicides lobatulus
Fursenkoina earlandi
Fursenkoina fusiformis
Globocassidulina biora
Globocassidulina crassa rossensis
Miliammina arenacea
Nonionella iridea
Pullenia bulloides
Trifarina angulosa
Trochammina intermedia
Neogloboquadrina pachyderma
Number of species
Accumulation rate, benthic foraminifera by number
Factor 1
Factor 2
Factor 3
Drilling/drill rig
Counting >63 µm fraction
Calculated
Leg178
Joides Resolution
Ocean Drilling Program ODP
spellingShingle AGE
Depth, composite
Astrononion echolsi
Bolivina pseudopunctata
Bulimina aculeata
Cibicides lobatulus
Fursenkoina earlandi
Fursenkoina fusiformis
Globocassidulina biora
Globocassidulina crassa rossensis
Miliammina arenacea
Nonionella iridea
Pullenia bulloides
Trifarina angulosa
Trochammina intermedia
Neogloboquadrina pachyderma
Number of species
Accumulation rate, benthic foraminifera by number
Factor 1
Factor 2
Factor 3
Drilling/drill rig
Counting >63 µm fraction
Calculated
Leg178
Joides Resolution
Ocean Drilling Program ODP
Ishman, Scott E
Sperling, Michael R
(Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ...
topic_facet AGE
Depth, composite
Astrononion echolsi
Bolivina pseudopunctata
Bulimina aculeata
Cibicides lobatulus
Fursenkoina earlandi
Fursenkoina fusiformis
Globocassidulina biora
Globocassidulina crassa rossensis
Miliammina arenacea
Nonionella iridea
Pullenia bulloides
Trifarina angulosa
Trochammina intermedia
Neogloboquadrina pachyderma
Number of species
Accumulation rate, benthic foraminifera by number
Factor 1
Factor 2
Factor 3
Drilling/drill rig
Counting >63 µm fraction
Calculated
Leg178
Joides Resolution
Ocean Drilling Program ODP
description Benthic foraminiferal data from Ocean Drilling Program Site 1098 indicate significant changes in deep-water conditions of the Palmer Deep, western Antarctic Peninsula margin, throughout the Holocene (13 ka to present). The earliest Holocene represents a period of transition from the Last Glacial Maximum (LGM). Cold bottom waters, similar to saline shelf water (SSW), dominated the middle Holocene. The late Holocene in the Palmer Deep has been characterized by alternating dominance of circumpolar deep water (CDW) and saline shelf water. These changes have global oceanographic and climatic implications. We suggest that the middle Holocene bottom-water record, in the absence of circumpolar deep water on the western Antarctic Peninsula shelf, indicates high saline shelf water production and/or weakened circumpolar deep water production during the middle Holocene climatic optimum. The late Holocene benthic foraminiferal record indicates rapidly fluctuating sea-ice conditions and may indicate a teleconnection ... : In the original table foraminiferal data are given without units. Units # used here are provisory. ...
format Dataset
author Ishman, Scott E
Sperling, Michael R
author_facet Ishman, Scott E
Sperling, Michael R
author_sort Ishman, Scott E
title (Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ...
title_short (Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ...
title_full (Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ...
title_fullStr (Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ...
title_full_unstemmed (Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B ...
title_sort (appendix table dr1) foraminiferal distribution data for odp hole 178-1098b ...
publisher PANGAEA
publishDate 2002
url https://dx.doi.org/10.1594/pangaea.713686
https://doi.pangaea.de/10.1594/PANGAEA.713686
long_lat ENVELOPE(-64.400,-64.400,-64.950,-64.950)
geographic Antarctic
Antarctic Peninsula
Palmer Deep
geographic_facet Antarctic
Antarctic Peninsula
Palmer Deep
genre Antarc*
Antarctic
Antarctic Peninsula
Neogloboquadrina pachyderma
Sea ice
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Neogloboquadrina pachyderma
Sea ice
op_relation ftp://rock.geosociety.org/pub/reposit/2002/2002044.pdf
https://dx.doi.org/10.1130/0091-7613(2002)030<0435:bfrohd>2.0.co;2
ftp://rock.geosociety.org/pub/reposit/2002/2002044.pdf
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.71368610.1130/0091-7613(2002)030<0435:bfrohd>2.0.co;2
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