Benthic foraminifera of ODP Leg 104 holes
Benthic foraminifers have been studied in about 900 samples from Sites 642, 643, and 644 (ODP Leg 104, Voring Plateau), ranging in age from Eocene to Holocene. This sequence has been subdivided into seven assemblage zones. The Eocene to middle Miocene deposits are characterized by an agglutinated fa...
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PANGAEA
1989
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.738546 https://doi.org/10.1594/PANGAEA.738546 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.738546 2023-05-15T17:47:05+02:00 Benthic foraminifera of ODP Leg 104 holes Osterman, Lisa Ellen Qvale, G MEDIAN LATITUDE: 67.211660 * MEDIAN LONGITUDE: 2.879660 * SOUTH-BOUND LATITUDE: 66.678300 * WEST-BOUND LONGITUDE: 1.033300 * NORTH-BOUND LATITUDE: 67.715000 * EAST-BOUND LONGITUDE: 4.576700 * DATE/TIME START: 1985-06-28T14:40:00 * DATE/TIME END: 1985-08-09T10:15:00 1989-06-02 application/zip, 5 datasets https://doi.pangaea.de/10.1594/PANGAEA.738546 https://doi.org/10.1594/PANGAEA.738546 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.738546 https://doi.org/10.1594/PANGAEA.738546 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Osterman, Lisa Ellen; Qvale, G (1989): Benthic foraminifers from the Vøring Plateau (ODP Leg 104). In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 745-768, https://doi.org/10.2973/odp.proc.sr.104.159.1989 104-642B 104-642C 104-642D 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP Dataset 1989 ftpangaea https://doi.org/10.1594/PANGAEA.738546 https://doi.org/10.2973/odp.proc.sr.104.159.1989 2023-01-20T07:31:48Z Benthic foraminifers have been studied in about 900 samples from Sites 642, 643, and 644 (ODP Leg 104, Voring Plateau), ranging in age from Eocene to Holocene. This sequence has been subdivided into seven assemblage zones. The Eocene to middle Miocene deposits are characterized by an agglutinated fauna. This reflects an environment causing dissolution of calcareous tests rather than the original living fauna. The upper Miocene to middle Pliocene deposits contain a diverse benthic foraminiferal fauna dominated by calcareous forms. The uppermost part of the sediment record, deposited during late Pliocene to Holocene, is characterized by many barren intervals and samples containing shallow-water species as well as ice-rafted material indicating glacial periods. Interglacials are reflected in samples containing a true oceanic foraminifer assemblage and no coarse clastic material. Dataset Norwegian Sea PANGAEA - Data Publisher for Earth & Environmental Science Norwegian Sea ENVELOPE(1.033300,4.576700,67.715000,66.678300) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
104-642B 104-642C 104-642D 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP |
spellingShingle |
104-642B 104-642C 104-642D 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP Osterman, Lisa Ellen Qvale, G Benthic foraminifera of ODP Leg 104 holes |
topic_facet |
104-642B 104-642C 104-642D 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP |
description |
Benthic foraminifers have been studied in about 900 samples from Sites 642, 643, and 644 (ODP Leg 104, Voring Plateau), ranging in age from Eocene to Holocene. This sequence has been subdivided into seven assemblage zones. The Eocene to middle Miocene deposits are characterized by an agglutinated fauna. This reflects an environment causing dissolution of calcareous tests rather than the original living fauna. The upper Miocene to middle Pliocene deposits contain a diverse benthic foraminiferal fauna dominated by calcareous forms. The uppermost part of the sediment record, deposited during late Pliocene to Holocene, is characterized by many barren intervals and samples containing shallow-water species as well as ice-rafted material indicating glacial periods. Interglacials are reflected in samples containing a true oceanic foraminifer assemblage and no coarse clastic material. |
format |
Dataset |
author |
Osterman, Lisa Ellen Qvale, G |
author_facet |
Osterman, Lisa Ellen Qvale, G |
author_sort |
Osterman, Lisa Ellen |
title |
Benthic foraminifera of ODP Leg 104 holes |
title_short |
Benthic foraminifera of ODP Leg 104 holes |
title_full |
Benthic foraminifera of ODP Leg 104 holes |
title_fullStr |
Benthic foraminifera of ODP Leg 104 holes |
title_full_unstemmed |
Benthic foraminifera of ODP Leg 104 holes |
title_sort |
benthic foraminifera of odp leg 104 holes |
publisher |
PANGAEA |
publishDate |
1989 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.738546 https://doi.org/10.1594/PANGAEA.738546 |
op_coverage |
MEDIAN LATITUDE: 67.211660 * MEDIAN LONGITUDE: 2.879660 * SOUTH-BOUND LATITUDE: 66.678300 * WEST-BOUND LONGITUDE: 1.033300 * NORTH-BOUND LATITUDE: 67.715000 * EAST-BOUND LONGITUDE: 4.576700 * DATE/TIME START: 1985-06-28T14:40:00 * DATE/TIME END: 1985-08-09T10:15:00 |
long_lat |
ENVELOPE(1.033300,4.576700,67.715000,66.678300) |
geographic |
Norwegian Sea |
geographic_facet |
Norwegian Sea |
genre |
Norwegian Sea |
genre_facet |
Norwegian Sea |
op_source |
Supplement to: Osterman, Lisa Ellen; Qvale, G (1989): Benthic foraminifers from the Vøring Plateau (ODP Leg 104). In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 745-768, https://doi.org/10.2973/odp.proc.sr.104.159.1989 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.738546 https://doi.org/10.1594/PANGAEA.738546 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.738546 https://doi.org/10.2973/odp.proc.sr.104.159.1989 |
_version_ |
1766151386894958592 |