Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway.

Field work at Montgomery Landing took place between August, 1979 and August, 1980, and consisted of collecting 138 samples at 2 kg each, spaced at 30 cm intervals along ten selected section lines. In addition, several large bulk samples were taken and the anterior third part of a toothed whale was r...

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Main Authors: Schiebout,Judith A., van den Bold,Willem
Other Authors: LOUISIANA STATE UNIV BATON ROUGE
Format: Text
Language:English
Published: 1982
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA127111
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA127111
id ftdtic:ADA127111
record_format openpolar
spelling ftdtic:ADA127111 2023-05-15T18:33:25+02:00 Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway. Schiebout,Judith A. van den Bold,Willem LOUISIANA STATE UNIV BATON ROUGE 1982-12-23 text/html http://www.dtic.mil/docs/citations/ADA127111 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA127111 en eng http://www.dtic.mil/docs/citations/ADA127111 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geology Geochemistry and Mineralogy *WATERWAYS *PALEONTOLOGY NATURAL RESOURCES HISTORY SAMPLING LABORATORY PROCEDURES Red River Waterway Text 1982 ftdtic 2016-02-20T22:11:57Z Field work at Montgomery Landing took place between August, 1979 and August, 1980, and consisted of collecting 138 samples at 2 kg each, spaced at 30 cm intervals along ten selected section lines. In addition, several large bulk samples were taken and the anterior third part of a toothed whale was recovered. Paleontological investigation of the samples includes the study of nannofossils, foraminifera, ostracodes, corals, bryozoa, mollusks, crabs, echinoderms, otoliths and other vertebrate remains including one of the finest Eocene whale skulls known to science. Biostratigraphic study confirms assignment of these beds to the early Jacksonian (late Eocene). Biofacies studies suggest that they were deposited on a flat, shallow continental shelf during a slow transgression of the sea. Local variation and diversity of the faunas is caused mainly by changes in the influx of terrigenous and organic matter in suspension. In view of the fact that part of the locality will become inundated, and the rest of the outcrop will deteriorte soon through weathering and vegetation cover, it is recommended that research and educational use of the site be facilitated while it is accessible through dissemination of data on the site. Text toothed whale Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Geology
Geochemistry and Mineralogy
*WATERWAYS
*PALEONTOLOGY
NATURAL RESOURCES
HISTORY
SAMPLING
LABORATORY PROCEDURES
Red River Waterway
spellingShingle Geology
Geochemistry and Mineralogy
*WATERWAYS
*PALEONTOLOGY
NATURAL RESOURCES
HISTORY
SAMPLING
LABORATORY PROCEDURES
Red River Waterway
Schiebout,Judith A.
van den Bold,Willem
Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway.
topic_facet Geology
Geochemistry and Mineralogy
*WATERWAYS
*PALEONTOLOGY
NATURAL RESOURCES
HISTORY
SAMPLING
LABORATORY PROCEDURES
Red River Waterway
description Field work at Montgomery Landing took place between August, 1979 and August, 1980, and consisted of collecting 138 samples at 2 kg each, spaced at 30 cm intervals along ten selected section lines. In addition, several large bulk samples were taken and the anterior third part of a toothed whale was recovered. Paleontological investigation of the samples includes the study of nannofossils, foraminifera, ostracodes, corals, bryozoa, mollusks, crabs, echinoderms, otoliths and other vertebrate remains including one of the finest Eocene whale skulls known to science. Biostratigraphic study confirms assignment of these beds to the early Jacksonian (late Eocene). Biofacies studies suggest that they were deposited on a flat, shallow continental shelf during a slow transgression of the sea. Local variation and diversity of the faunas is caused mainly by changes in the influx of terrigenous and organic matter in suspension. In view of the fact that part of the locality will become inundated, and the rest of the outcrop will deteriorte soon through weathering and vegetation cover, it is recommended that research and educational use of the site be facilitated while it is accessible through dissemination of data on the site.
author2 LOUISIANA STATE UNIV BATON ROUGE
format Text
author Schiebout,Judith A.
van den Bold,Willem
author_facet Schiebout,Judith A.
van den Bold,Willem
author_sort Schiebout,Judith A.
title Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway.
title_short Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway.
title_full Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway.
title_fullStr Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway.
title_full_unstemmed Paleontological Investigations in the Vicinity of Montgomery Landing, Red River Waterway.
title_sort paleontological investigations in the vicinity of montgomery landing, red river waterway.
publishDate 1982
url http://www.dtic.mil/docs/citations/ADA127111
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA127111
genre toothed whale
genre_facet toothed whale
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA127111
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766218021174509568