Cenozoic ostracoda of ODP Leg 104 holes
Ostracodes are less common than might be normally expected at Sites 642, 643, and 644, perhaps pointing to the fact that the marine habitat below the overlying Pleistocene ice covers was a severe environment. This explanation, however, would not apply to the Pliocene and Miocene deposits from which...
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1989
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.742576 2024-09-15T18:14:01+00:00 Cenozoic ostracoda of ODP Leg 104 holes Malz, Heinz MEDIAN LATITUDE: 67.212660 * MEDIAN LONGITUDE: 2.879320 * SOUTH-BOUND LATITUDE: 66.678300 * WEST-BOUND LONGITUDE: 1.033300 * NORTH-BOUND LATITUDE: 67.715000 * EAST-BOUND LONGITUDE: 4.576700 * DATE/TIME START: 1985-06-28T03:15:00 * DATE/TIME END: 1985-08-09T10:15:00 1989 application/zip, 5 datasets https://doi.pangaea.de/10.1594/PANGAEA.742576 https://doi.org/10.1594/PANGAEA.742576 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.742576 https://doi.org/10.1594/PANGAEA.742576 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Malz, Heinz (1989): Cenozoic ostracodes of the Vøring Plateau (ODP Leg 104, sites 642, 643, and 644). 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, 769-775, https://doi.org/10.2973/odp.proc.sr.104.198.1989 104-642A 104-642B 104-642C 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP dataset publication series 1989 ftpangaea https://doi.org/10.1594/PANGAEA.74257610.2973/odp.proc.sr.104.198.1989 2024-07-24T02:31:20Z Ostracodes are less common than might be normally expected at Sites 642, 643, and 644, perhaps pointing to the fact that the marine habitat below the overlying Pleistocene ice covers was a severe environment. This explanation, however, would not apply to the Pliocene and Miocene deposits from which ostracodes are just as poorly represented. In the latter case the Iceland-Faeroe Ridge might still have acted as a submerged barrier that did not allow an open ocean circulation of bottom waters. Thus the barrier presumably prevented an exchange of cold subarctic bottom water with that of the open Atlantic and therefore benthic deep-sea migration from the south was impeded. Some Quaternary species are, for the first time, recorded to extend to the Pliocene and/or Miocene. Other/Unknown Material Iceland Norwegian Sea Subarctic PANGAEA - Data Publisher for Earth & Environmental Science 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 |
104-642A 104-642B 104-642C 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP |
spellingShingle |
104-642A 104-642B 104-642C 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP Malz, Heinz Cenozoic ostracoda of ODP Leg 104 holes |
topic_facet |
104-642A 104-642B 104-642C 104-643A 104-644A DRILL Drilling/drill rig Joides Resolution Leg104 Norwegian Sea Ocean Drilling Program ODP |
description |
Ostracodes are less common than might be normally expected at Sites 642, 643, and 644, perhaps pointing to the fact that the marine habitat below the overlying Pleistocene ice covers was a severe environment. This explanation, however, would not apply to the Pliocene and Miocene deposits from which ostracodes are just as poorly represented. In the latter case the Iceland-Faeroe Ridge might still have acted as a submerged barrier that did not allow an open ocean circulation of bottom waters. Thus the barrier presumably prevented an exchange of cold subarctic bottom water with that of the open Atlantic and therefore benthic deep-sea migration from the south was impeded. Some Quaternary species are, for the first time, recorded to extend to the Pliocene and/or Miocene. |
format |
Other/Unknown Material |
author |
Malz, Heinz |
author_facet |
Malz, Heinz |
author_sort |
Malz, Heinz |
title |
Cenozoic ostracoda of ODP Leg 104 holes |
title_short |
Cenozoic ostracoda of ODP Leg 104 holes |
title_full |
Cenozoic ostracoda of ODP Leg 104 holes |
title_fullStr |
Cenozoic ostracoda of ODP Leg 104 holes |
title_full_unstemmed |
Cenozoic ostracoda of ODP Leg 104 holes |
title_sort |
cenozoic ostracoda of odp leg 104 holes |
publisher |
PANGAEA |
publishDate |
1989 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.742576 https://doi.org/10.1594/PANGAEA.742576 |
op_coverage |
MEDIAN LATITUDE: 67.212660 * MEDIAN LONGITUDE: 2.879320 * SOUTH-BOUND LATITUDE: 66.678300 * WEST-BOUND LONGITUDE: 1.033300 * NORTH-BOUND LATITUDE: 67.715000 * EAST-BOUND LONGITUDE: 4.576700 * DATE/TIME START: 1985-06-28T03:15:00 * DATE/TIME END: 1985-08-09T10:15:00 |
long_lat |
ENVELOPE(1.033300,4.576700,67.715000,66.678300) |
genre |
Iceland Norwegian Sea Subarctic |
genre_facet |
Iceland Norwegian Sea Subarctic |
op_source |
Supplement to: Malz, Heinz (1989): Cenozoic ostracodes of the Vøring Plateau (ODP Leg 104, sites 642, 643, and 644). 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, 769-775, https://doi.org/10.2973/odp.proc.sr.104.198.1989 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.742576 https://doi.org/10.1594/PANGAEA.742576 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.74257610.2973/odp.proc.sr.104.198.1989 |
_version_ |
1810451808628244480 |