Additional Occurrences and Extension of Stratigraphic Range of the Problematical Micro-Organism Nuia
Representatives of the problematical micro-organism Nuia siberica Maslov, 1954, have been found in three widely spaced areas of North America. These occurrences extend the stratigraphic range of Nuia from Late Cambrian? into Middle Ordovician (rocks of Porterfieldian age). Nuia siberica is found in...
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| Veröffentlicht in: | Journal of paleontology 1967-11, Vol.41 (6), p.1457-1460 |
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| container_title | Journal of paleontology |
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| creator | Toomey, Donald Francis |
| description | Representatives of the problematical micro-organism Nuia siberica Maslov, 1954, have been found in three widely spaced areas of North America. These occurrences extend the stratigraphic range of Nuia from Late Cambrian? into Middle Ordovician (rocks of Porterfieldian age). Nuia siberica is found in the Day Point, Crown Point, and Valcour Limestones (Chazyan) of the Champlain Valley of northern New York and western Vermont, the Bromide Formation (Middle Ordovician) of southern Oklahoma, and the Black Rock Formation (Early Ordovician) of northeastern Arkansas. Significantly, Nuia is found in both biostromal layers and mound horizons and apparently is intimately associated with various algal forms, lithistid sponges, and spongelike organisms. |
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These occurrences extend the stratigraphic range of Nuia from Late Cambrian? into Middle Ordovician (rocks of Porterfieldian age). Nuia siberica is found in the Day Point, Crown Point, and Valcour Limestones (Chazyan) of the Champlain Valley of northern New York and western Vermont, the Bromide Formation (Middle Ordovician) of southern Oklahoma, and the Black Rock Formation (Early Ordovician) of northeastern Arkansas. Significantly, Nuia is found in both biostromal layers and mound horizons and apparently is intimately associated with various algal forms, lithistid sponges, and spongelike organisms.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><language>eng</language><publisher>Society of Economic Paleontologists and Mineralogists and the Paleontological Society</publisher><subject>Algae ; Bromides ; Carbonates ; Islands ; Lakes ; Limestones ; Middle Ordovician epoch ; Rocks ; Sediments ; Sponges</subject><ispartof>Journal of paleontology, 1967-11, Vol.41 (6), p.1457-1460</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1302191$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1302191$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,57992,58225</link.rule.ids></links><search><creatorcontrib>Toomey, Donald Francis</creatorcontrib><title>Additional Occurrences and Extension of Stratigraphic Range of the Problematical Micro-Organism Nuia</title><title>Journal of paleontology</title><description>Representatives of the problematical micro-organism Nuia siberica Maslov, 1954, have been found in three widely spaced areas of North America. These occurrences extend the stratigraphic range of Nuia from Late Cambrian? into Middle Ordovician (rocks of Porterfieldian age). Nuia siberica is found in the Day Point, Crown Point, and Valcour Limestones (Chazyan) of the Champlain Valley of northern New York and western Vermont, the Bromide Formation (Middle Ordovician) of southern Oklahoma, and the Black Rock Formation (Early Ordovician) of northeastern Arkansas. Significantly, Nuia is found in both biostromal layers and mound horizons and apparently is intimately associated with various algal forms, lithistid sponges, and spongelike organisms.</description><subject>Algae</subject><subject>Bromides</subject><subject>Carbonates</subject><subject>Islands</subject><subject>Lakes</subject><subject>Limestones</subject><subject>Middle Ordovician epoch</subject><subject>Rocks</subject><subject>Sediments</subject><subject>Sponges</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1967</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotjF1LwzAYhYMoOKf_wIv8gUDeJE3ayzHmB2xWdPcjzUeX0aYjyUD_vRW9OofzHJ4rtICGK8I4V9doQSljhHNJb9FdzidKgUmABbIra0MJU9QDbo25pOSicRnraPHmq7iYZ4Ynjz9L0iX0SZ-PweAPHXv3O5ejw-9p6gY3ztjMll0waSJt6nUMecRvl6Dv0Y3XQ3YP_7lE-6fNfv1Ctu3z63q1JVoIIN6ySjS1pFDNtVEA1ndMCe66RlRW1NQDM7SmBmrJZD0_nTZWVZJ5qSrFl-jxT3vKZUqHcwqjTt8H4JRBA_wHkOJPZQ</recordid><startdate>19671101</startdate><enddate>19671101</enddate><creator>Toomey, Donald Francis</creator><general>Society of Economic Paleontologists and Mineralogists and the Paleontological Society</general><scope/></search><sort><creationdate>19671101</creationdate><title>Additional Occurrences and Extension of Stratigraphic Range of the Problematical Micro-Organism Nuia</title><author>Toomey, Donald Francis</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a441-fd254986015fd29711dfb2743eb945d480f12c080c186268860eacd7562f67573</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1967</creationdate><topic>Algae</topic><topic>Bromides</topic><topic>Carbonates</topic><topic>Islands</topic><topic>Lakes</topic><topic>Limestones</topic><topic>Middle Ordovician epoch</topic><topic>Rocks</topic><topic>Sediments</topic><topic>Sponges</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Toomey, Donald Francis</creatorcontrib><jtitle>Journal of paleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Toomey, Donald Francis</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Additional Occurrences and Extension of Stratigraphic Range of the Problematical Micro-Organism Nuia</atitle><jtitle>Journal of paleontology</jtitle><date>1967-11-01</date><risdate>1967</risdate><volume>41</volume><issue>6</issue><spage>1457</spage><epage>1460</epage><pages>1457-1460</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><abstract>Representatives of the problematical micro-organism Nuia siberica Maslov, 1954, have been found in three widely spaced areas of North America. These occurrences extend the stratigraphic range of Nuia from Late Cambrian? into Middle Ordovician (rocks of Porterfieldian age). Nuia siberica is found in the Day Point, Crown Point, and Valcour Limestones (Chazyan) of the Champlain Valley of northern New York and western Vermont, the Bromide Formation (Middle Ordovician) of southern Oklahoma, and the Black Rock Formation (Early Ordovician) of northeastern Arkansas. Significantly, Nuia is found in both biostromal layers and mound horizons and apparently is intimately associated with various algal forms, lithistid sponges, and spongelike organisms.</abstract><pub>Society of Economic Paleontologists and Mineralogists and the Paleontological Society</pub><tpages>4</tpages></addata></record> |
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| ispartof | Journal of paleontology, 1967-11, Vol.41 (6), p.1457-1460 |
| issn | 0022-3360 1937-2337 |
| language | eng |
| recordid | cdi_jstor_primary_1302191 |
| source | Jstor Complete Legacy |
| subjects | Algae Bromides Carbonates Islands Lakes Limestones Middle Ordovician epoch Rocks Sediments Sponges |
| title | Additional Occurrences and Extension of Stratigraphic Range of the Problematical Micro-Organism Nuia |
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