Preservation and Erosion of Theropod Tracks in Eolian Deposits: Examples from the Middle Jurassic Entrada Sandstone, Utah, U.S.A
The Middle Jurassic Entrada Sandstone, exposed near the town of Escalante, southern Utah, consists of large‐scale cross‐bedded eolian deposits that are interbedded with horizontally laminated sand sheets and thin sets of eolian cross‐strata, representing periods with a moister climate. The flat‐bedd...
Gespeichert in:
Veröffentlicht in: | The Journal of geology 2007-05, Vol.115 (3), p.375-386 |
---|---|
Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 386 |
---|---|
container_issue | 3 |
container_start_page | 375 |
container_title | The Journal of geology |
container_volume | 115 |
creator | Milàn, Jesper Loope, David B. |
description | The Middle Jurassic Entrada Sandstone, exposed near the town of Escalante, southern Utah, consists of large‐scale cross‐bedded eolian deposits that are interbedded with horizontally laminated sand sheets and thin sets of eolian cross‐strata, representing periods with a moister climate. The flat‐bedded units contain numerous tracks and trackways from small to large‐sized theropod dinosaurs. These tracks are today exposed in several distinct erosional states, allowing detailed studies of track and undertrack formation in eolian deposits. Tracks that originally were emplaced on sloping surfaces show, in their present‐day erosional state, a morphology distinct from those originally emplaced on horizontal surfaces. Further, the range of eroded track morphologies can help identify badly eroded tracks from nonbiogenic structures in similar deposits. |
doi_str_mv | 10.1086/512758 |
format | Article |
fullrecord | <record><control><sourceid>jstor_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1086_512758</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>10.1086/512758</jstor_id><sourcerecordid>10.1086/512758</sourcerecordid><originalsourceid>FETCH-LOGICAL-a390t-a730a12d5a40a8077d3272a19e2e1070c4559c61ac2e066253f87dfa8a4812b93</originalsourceid><addsrcrecordid>eNpFkE1LxDAQQIMouK76D4Qg4smuk6RpUm_LWr9QFFzPZWxTt-tuU5NW9OZPN1LRSyaHxxvmEbLPYMJAJ6eScSX1BhkxKVQkeZJukhEA5xETKtkmO94vAZjgEkbk68EZb9w7drVtKDYlzZz1P39b0fnCONvaks4dFq-e1g3N7KrGhp6bNlCdP6PZB67blfG0cnZNu4Whd3VZrgy96R16Xxc0azqHJdLHYPedbcwJfepwEd7J42S6S7YqXHmz9zvH5Okim8-uotv7y-vZ9DZCkUIXoRKAjJcSY0ANSpWCK44sNdwwUFDEUqZFwrDgBpKES1FpVVaoMdaMP6diTA4Hb-vsW298ly9t75qwMmdpHAuhEwjQ8QAVIYJ3pspbV6_RfeYM8p-4-RA3gEcD2BeLusAX24aM_l_5hx0M2DIc7v5kAiDRWjPxDU5fgJI</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>194433860</pqid></control><display><type>article</type><title>Preservation and Erosion of Theropod Tracks in Eolian Deposits: Examples from the Middle Jurassic Entrada Sandstone, Utah, U.S.A</title><source>Jstor Complete Legacy</source><creator>Milàn, Jesper ; Loope, David B.</creator><creatorcontrib>Milàn, Jesper ; Loope, David B.</creatorcontrib><description>The Middle Jurassic Entrada Sandstone, exposed near the town of Escalante, southern Utah, consists of large‐scale cross‐bedded eolian deposits that are interbedded with horizontally laminated sand sheets and thin sets of eolian cross‐strata, representing periods with a moister climate. The flat‐bedded units contain numerous tracks and trackways from small to large‐sized theropod dinosaurs. These tracks are today exposed in several distinct erosional states, allowing detailed studies of track and undertrack formation in eolian deposits. Tracks that originally were emplaced on sloping surfaces show, in their present‐day erosional state, a morphology distinct from those originally emplaced on horizontal surfaces. Further, the range of eroded track morphologies can help identify badly eroded tracks from nonbiogenic structures in similar deposits.</description><identifier>ISSN: 0022-1376</identifier><identifier>EISSN: 1537-5269</identifier><identifier>DOI: 10.1086/512758</identifier><identifier>CODEN: JGEOAZ</identifier><language>eng</language><publisher>Chicago: The University of Chicago Press</publisher><subject>Claws ; Deformation ; Dinosaurs ; Eolian deposits ; Geology ; Metatarsus ; Outcrops ; Petrology ; Preservation ; Rocks ; Sand ; Sand sheets ; Sandstones ; Sediments</subject><ispartof>The Journal of geology, 2007-05, Vol.115 (3), p.375-386</ispartof><rights>2007 by The University of Chicago. All rights reserved.</rights><rights>Copyright University of Chicago, acting through its Press May 2007</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a390t-a730a12d5a40a8077d3272a19e2e1070c4559c61ac2e066253f87dfa8a4812b93</citedby><cites>FETCH-LOGICAL-a390t-a730a12d5a40a8077d3272a19e2e1070c4559c61ac2e066253f87dfa8a4812b93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,799,27901,27902</link.rule.ids></links><search><creatorcontrib>Milàn, Jesper</creatorcontrib><creatorcontrib>Loope, David B.</creatorcontrib><title>Preservation and Erosion of Theropod Tracks in Eolian Deposits: Examples from the Middle Jurassic Entrada Sandstone, Utah, U.S.A</title><title>The Journal of geology</title><description>The Middle Jurassic Entrada Sandstone, exposed near the town of Escalante, southern Utah, consists of large‐scale cross‐bedded eolian deposits that are interbedded with horizontally laminated sand sheets and thin sets of eolian cross‐strata, representing periods with a moister climate. The flat‐bedded units contain numerous tracks and trackways from small to large‐sized theropod dinosaurs. These tracks are today exposed in several distinct erosional states, allowing detailed studies of track and undertrack formation in eolian deposits. Tracks that originally were emplaced on sloping surfaces show, in their present‐day erosional state, a morphology distinct from those originally emplaced on horizontal surfaces. Further, the range of eroded track morphologies can help identify badly eroded tracks from nonbiogenic structures in similar deposits.</description><subject>Claws</subject><subject>Deformation</subject><subject>Dinosaurs</subject><subject>Eolian deposits</subject><subject>Geology</subject><subject>Metatarsus</subject><subject>Outcrops</subject><subject>Petrology</subject><subject>Preservation</subject><subject>Rocks</subject><subject>Sand</subject><subject>Sand sheets</subject><subject>Sandstones</subject><subject>Sediments</subject><issn>0022-1376</issn><issn>1537-5269</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNpFkE1LxDAQQIMouK76D4Qg4smuk6RpUm_LWr9QFFzPZWxTt-tuU5NW9OZPN1LRSyaHxxvmEbLPYMJAJ6eScSX1BhkxKVQkeZJukhEA5xETKtkmO94vAZjgEkbk68EZb9w7drVtKDYlzZz1P39b0fnCONvaks4dFq-e1g3N7KrGhp6bNlCdP6PZB67blfG0cnZNu4Whd3VZrgy96R16Xxc0azqHJdLHYPedbcwJfepwEd7J42S6S7YqXHmz9zvH5Okim8-uotv7y-vZ9DZCkUIXoRKAjJcSY0ANSpWCK44sNdwwUFDEUqZFwrDgBpKES1FpVVaoMdaMP6diTA4Hb-vsW298ly9t75qwMmdpHAuhEwjQ8QAVIYJ3pspbV6_RfeYM8p-4-RA3gEcD2BeLusAX24aM_l_5hx0M2DIc7v5kAiDRWjPxDU5fgJI</recordid><startdate>200705</startdate><enddate>200705</enddate><creator>Milàn, Jesper</creator><creator>Loope, David B.</creator><general>The University of Chicago Press</general><general>University of Chicago, acting through its Press</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope></search><sort><creationdate>200705</creationdate><title>Preservation and Erosion of Theropod Tracks in Eolian Deposits: Examples from the Middle Jurassic Entrada Sandstone, Utah, U.S.A</title><author>Milàn, Jesper ; Loope, David B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a390t-a730a12d5a40a8077d3272a19e2e1070c4559c61ac2e066253f87dfa8a4812b93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>Claws</topic><topic>Deformation</topic><topic>Dinosaurs</topic><topic>Eolian deposits</topic><topic>Geology</topic><topic>Metatarsus</topic><topic>Outcrops</topic><topic>Petrology</topic><topic>Preservation</topic><topic>Rocks</topic><topic>Sand</topic><topic>Sand sheets</topic><topic>Sandstones</topic><topic>Sediments</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Milàn, Jesper</creatorcontrib><creatorcontrib>Loope, David B.</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>The Journal of geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Milàn, Jesper</au><au>Loope, David B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Preservation and Erosion of Theropod Tracks in Eolian Deposits: Examples from the Middle Jurassic Entrada Sandstone, Utah, U.S.A</atitle><jtitle>The Journal of geology</jtitle><date>2007-05</date><risdate>2007</risdate><volume>115</volume><issue>3</issue><spage>375</spage><epage>386</epage><pages>375-386</pages><issn>0022-1376</issn><eissn>1537-5269</eissn><coden>JGEOAZ</coden><abstract>The Middle Jurassic Entrada Sandstone, exposed near the town of Escalante, southern Utah, consists of large‐scale cross‐bedded eolian deposits that are interbedded with horizontally laminated sand sheets and thin sets of eolian cross‐strata, representing periods with a moister climate. The flat‐bedded units contain numerous tracks and trackways from small to large‐sized theropod dinosaurs. These tracks are today exposed in several distinct erosional states, allowing detailed studies of track and undertrack formation in eolian deposits. Tracks that originally were emplaced on sloping surfaces show, in their present‐day erosional state, a morphology distinct from those originally emplaced on horizontal surfaces. Further, the range of eroded track morphologies can help identify badly eroded tracks from nonbiogenic structures in similar deposits.</abstract><cop>Chicago</cop><pub>The University of Chicago Press</pub><doi>10.1086/512758</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0022-1376 |
ispartof | The Journal of geology, 2007-05, Vol.115 (3), p.375-386 |
issn | 0022-1376 1537-5269 |
language | eng |
recordid | cdi_crossref_primary_10_1086_512758 |
source | Jstor Complete Legacy |
subjects | Claws Deformation Dinosaurs Eolian deposits Geology Metatarsus Outcrops Petrology Preservation Rocks Sand Sand sheets Sandstones Sediments |
title | Preservation and Erosion of Theropod Tracks in Eolian Deposits: Examples from the Middle Jurassic Entrada Sandstone, Utah, U.S.A |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-03T01%3A59%3A33IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Preservation%20and%20Erosion%20of%20Theropod%20Tracks%20in%20Eolian%20Deposits:%20Examples%20from%20the%20Middle%20Jurassic%20Entrada%20Sandstone,%20Utah,%20U.S.A&rft.jtitle=The%20Journal%20of%20geology&rft.au=Mil%C3%A0n,%20Jesper&rft.date=2007-05&rft.volume=115&rft.issue=3&rft.spage=375&rft.epage=386&rft.pages=375-386&rft.issn=0022-1376&rft.eissn=1537-5269&rft.coden=JGEOAZ&rft_id=info:doi/10.1086/512758&rft_dat=%3Cjstor_cross%3E10.1086/512758%3C/jstor_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=194433860&rft_id=info:pmid/&rft_jstor_id=10.1086/512758&rfr_iscdi=true |