Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy
The late Barstovian Fort Polk herpetofauna represents the most diverse herpetofauna on the Gulf Coast, USA, and includes 15 genera from ten families. The herpetofaunal composition of Fort Polk and Miocene east Texas localities is similar enough to Great Plains localities that they are all considered...
Main Author: | |
---|---|
Other Authors: | |
Format: | Others |
Language: | en |
Published: |
LSU
2009
|
Subjects: | |
Online Access: | http://etd.lsu.edu/docs/available/etd-11132009-034120/ |
id |
ndltd-LSU-oai-etd.lsu.edu-etd-11132009-034120 |
---|---|
record_format |
oai_dc |
spelling |
ndltd-LSU-oai-etd.lsu.edu-etd-11132009-0341202013-01-07T22:52:36Z Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy Williams, Michael John Geology & Geophysics The late Barstovian Fort Polk herpetofauna represents the most diverse herpetofauna on the Gulf Coast, USA, and includes 15 genera from ten families. The herpetofaunal composition of Fort Polk and Miocene east Texas localities is similar enough to Great Plains localities that they are all considered to be one biogeographical province during the Barstovian. The use of ternary diagrams, ratios of herpetological elements to kg matrix screened, and natricine-colubrine indices, has allowed determining the wetness of the Fort Polk sites. Development of a composite stratigraphic section for North American fossil snakes has allowed recognition of two extinctions of fossil snakes during the Miocene. North American and European Miocene snake faunas display a replacement of boids by colubrids in the Early to Middle Miocene and Late Oligocene, respectively. European fossil snake data show a decrease in colubrid numbers from the Early to Middle Miocene. Ellwood, Brooks B. Schiebout, Judith A. Warny, Sophie A. Hanor, Jeffrey S. Tague, Robert G. LSU 2009-11-13 text application/pdf http://etd.lsu.edu/docs/available/etd-11132009-034120/ http://etd.lsu.edu/docs/available/etd-11132009-034120/ en unrestricted I hereby certify that, if appropriate, I have obtained and attached herein a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dissertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to LSU or its agents the non-exclusive license to archive and make accessible, under the conditions specified below and in appropriate University policies, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report. |
collection |
NDLTD |
language |
en |
format |
Others
|
sources |
NDLTD |
topic |
Geology & Geophysics |
spellingShingle |
Geology & Geophysics Williams, Michael John Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy |
description |
The late Barstovian Fort Polk herpetofauna represents the most diverse herpetofauna on the Gulf Coast, USA, and includes 15 genera from ten families. The herpetofaunal composition of Fort Polk and Miocene east Texas localities is similar enough to Great Plains localities that they are all considered to be one biogeographical province during the Barstovian. The use of ternary diagrams, ratios of herpetological elements to kg matrix screened, and natricine-colubrine indices, has allowed determining the wetness of the Fort Polk sites. Development of a composite stratigraphic section for North American fossil snakes has allowed recognition of two extinctions of fossil snakes during the Miocene. North American and European Miocene snake faunas display a replacement of boids by colubrids in the Early to Middle Miocene and Late Oligocene, respectively. European fossil snake data show a decrease in colubrid numbers from the Early to Middle Miocene. |
author2 |
Ellwood, Brooks B. |
author_facet |
Ellwood, Brooks B. Williams, Michael John |
author |
Williams, Michael John |
author_sort |
Williams, Michael John |
title |
Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy |
title_short |
Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy |
title_full |
Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy |
title_fullStr |
Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy |
title_full_unstemmed |
Miocene Herpetofaunas from the Central Gulf Coast, USA: Their Paleoecology, Biogeography, and Biostratigraphy |
title_sort |
miocene herpetofaunas from the central gulf coast, usa: their paleoecology, biogeography, and biostratigraphy |
publisher |
LSU |
publishDate |
2009 |
url |
http://etd.lsu.edu/docs/available/etd-11132009-034120/ |
work_keys_str_mv |
AT williamsmichaeljohn mioceneherpetofaunasfromthecentralgulfcoastusatheirpaleoecologybiogeographyandbiostratigraphy |
_version_ |
1716477919570690048 |