A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW
Twenty-two species of dinoflagellates and acritarchs, and thirty species of spores and pollen are reported from twenty Lower Cretaceous core samples of shale and siltstone from the South Barrow Test Well No.1 in Point Barrow, Alaska. The stratigraphic distribution of the fifty-two species is summari...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.582.7328 2023-05-15T15:39:30+02:00 A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.7328 http://palynology.geoscienceworld.org/content/24/1/201.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.7328 http://palynology.geoscienceworld.org/content/24/1/201.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://palynology.geoscienceworld.org/content/24/1/201.full.pdf text ftciteseerx 2016-08-28T00:03:26Z Twenty-two species of dinoflagellates and acritarchs, and thirty species of spores and pollen are reported from twenty Lower Cretaceous core samples of shale and siltstone from the South Barrow Test Well No.1 in Point Barrow, Alaska. The stratigraphic distribution of the fifty-two species is summarized, and four stratigraphic intervals are established. Based on diagnostic di-noflagellate cysts, the geologic age for the Torok Formation is suggested to be Aptian–Albian, and the age of the “Pebble Shale” unit is suggested to be Barremian–Aptian. The depositional environment is considered to be marine. Text Barrow Point Barrow Alaska Unknown |
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ftciteseerx |
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English |
description |
Twenty-two species of dinoflagellates and acritarchs, and thirty species of spores and pollen are reported from twenty Lower Cretaceous core samples of shale and siltstone from the South Barrow Test Well No.1 in Point Barrow, Alaska. The stratigraphic distribution of the fifty-two species is summarized, and four stratigraphic intervals are established. Based on diagnostic di-noflagellate cysts, the geologic age for the Torok Formation is suggested to be Aptian–Albian, and the age of the “Pebble Shale” unit is suggested to be Barremian–Aptian. The depositional environment is considered to be marine. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
title |
A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW |
spellingShingle |
A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW |
title_short |
A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW |
title_full |
A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW |
title_fullStr |
A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW |
title_full_unstemmed |
A. Kimyai: Lower Cretaceous Palynology, Point Barrow, Alaska 201PALYNOLOGY AND BIOSTRATIGRAPHY OF THE LOWER CRETACEOUS SEDIMENTS IN THE SOUTH BARROW |
title_sort |
a. kimyai: lower cretaceous palynology, point barrow, alaska 201palynology and biostratigraphy of the lower cretaceous sediments in the south barrow |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.7328 http://palynology.geoscienceworld.org/content/24/1/201.full.pdf |
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Barrow Point Barrow Alaska |
genre_facet |
Barrow Point Barrow Alaska |
op_source |
http://palynology.geoscienceworld.org/content/24/1/201.full.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.7328 http://palynology.geoscienceworld.org/content/24/1/201.full.pdf |
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1766371221830631424 |