Devonian Plants from the Type Section of the Ghost River Formation of Western Alberta
Plant fossils, including branched axes, foliar structures, fructifications, and dispersed spores have recently been discovered from the type section of the Ghost River formation. The megafossils, although commonly fragmentary, suggest a late Middle or early Upper Devonian age for the beds. This disc...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1962-03, Vol.135 (3507), p.930-931 |
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creator | Greggs, R. G. McGregor, D. C. Rouse, Glenn E. |
description | Plant fossils, including branched axes, foliar structures, fructifications, and dispersed spores have recently been discovered from the type section of the Ghost River formation. The megafossils, although commonly fragmentary, suggest a late Middle or early Upper Devonian age for the beds. This discovery suggests that equivalent strata in other regions may also contain plant remains, the discovery of which would add significantly to our knowledge of Devonian floras in western North America. |
doi_str_mv | 10.1126/science.135.3507.930 |
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G.</creatorcontrib><creatorcontrib>McGregor, D. C.</creatorcontrib><creatorcontrib>Rouse, Glenn E.</creatorcontrib><title>Devonian Plants from the Type Section of the Ghost River Formation of Western Alberta</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>Plant fossils, including branched axes, foliar structures, fructifications, and dispersed spores have recently been discovered from the type section of the Ghost River formation. The megafossils, although commonly fragmentary, suggest a late Middle or early Upper Devonian age for the beds. This discovery suggests that equivalent strata in other regions may also contain plant remains, the discovery of which would add significantly to our knowledge of Devonian floras in western North America.</description><subject>Cambrian series 3</subject><subject>Canyons</subject><subject>Dolomite</subject><subject>Flora</subject><subject>Fossils</subject><subject>Plant collections</subject><subject>Plants</subject><subject>Spores</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1962</creationdate><recordtype>article</recordtype><recordid>eNpNkNFKwzAUhoMobk7fYEjuvGpNmqZtLsd0UxAU3fAypOkJ61ibmXSDvb2Zq-jVgfzfn5N8CI0piSlNsnuva2g1xJTxmHGSx4KRMzSkRPBIJISdoyEhLIsKkvMBuvJ-TUjIBLtEA5oXNAvkEC0fYG_bWrX4baPazmPjbIO7FeDFYQv4A3RX2xZb83M2X1nf4fd6Dw7PrGvUb_gJvgPX4smmBNepa3Rh1MbDTT9HaDl7XEyfopfX-fN08hIplhddVJUFGEMToyAjCeWJLsGIVGuhk1ILllTKqApSQTJDSZVVgvOEBb4oIeVFxkbo7nTv1tmvXXiDbGqvYRO-AnbnZc4YLfJgK5DpidTOeu_AyK2rG-UOkhJ59Cl7nzL4lEefMvgMtdt-wa5soPor9QIDMD4Ba99Z9y8nRc5T9g0Pe3z5</recordid><startdate>19620316</startdate><enddate>19620316</enddate><creator>Greggs, R. G.</creator><creator>McGregor, D. C.</creator><creator>Rouse, Glenn E.</creator><general>American Association for the Advancement of Science</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope></search><sort><creationdate>19620316</creationdate><title>Devonian Plants from the Type Section of the Ghost River Formation of Western Alberta</title><author>Greggs, R. G. ; McGregor, D. C. ; Rouse, Glenn E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a378t-db8eff12fae602152cbef94cc9c2bc932dafade4906f10d6d9552312f8be45863</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1962</creationdate><topic>Cambrian series 3</topic><topic>Canyons</topic><topic>Dolomite</topic><topic>Flora</topic><topic>Fossils</topic><topic>Plant collections</topic><topic>Plants</topic><topic>Spores</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Greggs, R. G.</creatorcontrib><creatorcontrib>McGregor, D. 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C.</au><au>Rouse, Glenn E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Devonian Plants from the Type Section of the Ghost River Formation of Western Alberta</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>1962-03-16</date><risdate>1962</risdate><volume>135</volume><issue>3507</issue><spage>930</spage><epage>931</epage><pages>930-931</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><abstract>Plant fossils, including branched axes, foliar structures, fructifications, and dispersed spores have recently been discovered from the type section of the Ghost River formation. The megafossils, although commonly fragmentary, suggest a late Middle or early Upper Devonian age for the beds. This discovery suggests that equivalent strata in other regions may also contain plant remains, the discovery of which would add significantly to our knowledge of Devonian floras in western North America.</abstract><cop>United States</cop><pub>American Association for the Advancement of Science</pub><pmid>17816109</pmid><doi>10.1126/science.135.3507.930</doi><tpages>2</tpages></addata></record> |
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ispartof | Science (American Association for the Advancement of Science), 1962-03, Vol.135 (3507), p.930-931 |
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source | JSTOR Archive Collection A-Z Listing; American Association for the Advancement of Science |
subjects | Cambrian series 3 Canyons Dolomite Flora Fossils Plant collections Plants Spores |
title | Devonian Plants from the Type Section of the Ghost River Formation of Western Alberta |
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