Jurassic micropaleontology of the Grand Banks
Jurassic foraminifera in the marine deposits (up to 3km thick) of the Grand Banks of Newfoundland define eight biostratigraphic zones of Pliensbachian through Tithonian age. Jurassic marine deposition (~4cm/10k.y) kept pace with subsidence resulting in a relatively continuous, shallow marine sedimen...
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ftnewulisboa:oai:run.unl.pt:10362/1484 2024-06-09T07:47:50+00:00 Jurassic micropaleontology of the Grand Banks Gradstein, F. 2008-07-16T19:12:24Z http://hdl.handle.net/10362/1484 eng eng http://hdl.handle.net/10362/1484 openAccess Jurassic Micropaleontology Foraminifera Grand Banks article 2008 ftnewulisboa 2024-05-15T22:47:33Z Jurassic foraminifera in the marine deposits (up to 3km thick) of the Grand Banks of Newfoundland define eight biostratigraphic zones of Pliensbachian through Tithonian age. Jurassic marine deposition (~4cm/10k.y) kept pace with subsidence resulting in a relatively continuous, shallow marine sedimentation pattern. Central Grand Banks subsidence ceased in Late Jurassic time and the area became emergent with erosion taking place until Albian time. Grand Banks Jurassic foraminiferal assemblages are of a distinctly Old World affinity reflecting the contracted early Atlantic paleogeography. Compositional differences with Portuguese Middle-Late Jurassic microfauna are probably related to differences in depositional history of the Portuguese and Grand Banks Basin. Article in Journal/Newspaper Newfoundland Repositório da Universidade Nova de Lisboa (UNL) |
institution |
Open Polar |
collection |
Repositório da Universidade Nova de Lisboa (UNL) |
op_collection_id |
ftnewulisboa |
language |
English |
topic |
Jurassic Micropaleontology Foraminifera Grand Banks |
spellingShingle |
Jurassic Micropaleontology Foraminifera Grand Banks Gradstein, F. Jurassic micropaleontology of the Grand Banks |
topic_facet |
Jurassic Micropaleontology Foraminifera Grand Banks |
description |
Jurassic foraminifera in the marine deposits (up to 3km thick) of the Grand Banks of Newfoundland define eight biostratigraphic zones of Pliensbachian through Tithonian age. Jurassic marine deposition (~4cm/10k.y) kept pace with subsidence resulting in a relatively continuous, shallow marine sedimentation pattern. Central Grand Banks subsidence ceased in Late Jurassic time and the area became emergent with erosion taking place until Albian time. Grand Banks Jurassic foraminiferal assemblages are of a distinctly Old World affinity reflecting the contracted early Atlantic paleogeography. Compositional differences with Portuguese Middle-Late Jurassic microfauna are probably related to differences in depositional history of the Portuguese and Grand Banks Basin. |
format |
Article in Journal/Newspaper |
author |
Gradstein, F. |
author_facet |
Gradstein, F. |
author_sort |
Gradstein, F. |
title |
Jurassic micropaleontology of the Grand Banks |
title_short |
Jurassic micropaleontology of the Grand Banks |
title_full |
Jurassic micropaleontology of the Grand Banks |
title_fullStr |
Jurassic micropaleontology of the Grand Banks |
title_full_unstemmed |
Jurassic micropaleontology of the Grand Banks |
title_sort |
jurassic micropaleontology of the grand banks |
publishDate |
2008 |
url |
http://hdl.handle.net/10362/1484 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
http://hdl.handle.net/10362/1484 |
op_rights |
openAccess |
_version_ |
1801379293497917440 |