Palynology and micropaleontology of the Clam Bank Formation (Lower Devonian) of western Newfoundland, Canada
Sandstone and siltstone samples collected from the lowest part of the Clam Bank Formation in western Newfoundland contain a distinctive monospecific conodont assemblage of Ozarkodina remscheidensis eosteinhornensis and O. remscheidensis ssp., confidently dated as Late Ludlow through Lochkovian. Paly...
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| Veröffentlicht in: | Palynology 2002, Vol.26 (1), p.185-215 |
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| creator | Burden, Elliott T Quinn, Louise Nowlan, Godfrey S Bailey-Nill, Linda A |
| description | Sandstone and siltstone samples collected from the lowest part of the Clam Bank Formation in western Newfoundland contain a distinctive monospecific conodont assemblage of Ozarkodina remscheidensis eosteinhornensis and O. remscheidensis ssp., confidently dated as Late Ludlow through Lochkovian. Palynomorph assemblages of terrestrial spores, acritarchs, chitinozoans, scolecodonts and plant fragments are relatively abundant and diverse in the lower 250 m of this formation. Taxa include the cryptospore genera Cymbohilates, Acontotetras, Hispanaediscus, Laevolancis, and Tetrahedraletes, spore genera Ambitisporites, Aneurospora, Apiculiretusispora, Emphanisporites, Retusotriletes, Synorisporites, Vermiverruspora, and a new species Stellatispora fahraeusi. Acritarchs include the taxon Triangulina sanpetrensis and chitinozoa include Angochitina chlupaci. Palynomorphs indicate a Lochkovian age, corresponding with the Apiculiretusispora sp. E zone from Europe. In well preserved samples from this section, the fossil terrestrial palynomorph assemblages from these shallow marine deposits correspond closely in species diversity and concentration with values reported for modern shelf deposits located adjacent to low Arctic moss and sedge tundra. By inference, earliest Devonian terrestrial vegetation must have been relatively well developed on this ancient coastline. |
| doi_str_mv | 10.2113/0260185 |
| format | Article |
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Palynomorph assemblages of terrestrial spores, acritarchs, chitinozoans, scolecodonts and plant fragments are relatively abundant and diverse in the lower 250 m of this formation. Taxa include the cryptospore genera Cymbohilates, Acontotetras, Hispanaediscus, Laevolancis, and Tetrahedraletes, spore genera Ambitisporites, Aneurospora, Apiculiretusispora, Emphanisporites, Retusotriletes, Synorisporites, Vermiverruspora, and a new species Stellatispora fahraeusi. Acritarchs include the taxon Triangulina sanpetrensis and chitinozoa include Angochitina chlupaci. Palynomorphs indicate a Lochkovian age, corresponding with the Apiculiretusispora sp. E zone from Europe. In well preserved samples from this section, the fossil terrestrial palynomorph assemblages from these shallow marine deposits correspond closely in species diversity and concentration with values reported for modern shelf deposits located adjacent to low Arctic moss and sedge tundra. By inference, earliest Devonian terrestrial vegetation must have been relatively well developed on this ancient coastline.</description><identifier>ISSN: 0191-6122</identifier><identifier>EISSN: 1558-9188</identifier><identifier>DOI: 10.2113/0260185</identifier><language>eng</language><publisher>American Association of Stratigraphic Palynologists</publisher><subject>acritarchs ; assemblages ; Canada ; Chitinozoa ; Clam Bank Formation ; Clams ; clastic rocks ; coastal environment ; Conodonta ; correlation ; Devonian ; Eastern Canada ; Fossils ; Geological surveys ; Geology ; Invertebrata ; Lochkovian ; Lower Devonian ; microfossils ; new taxa ; Newfoundland ; Newfoundland and Labrador ; Newfoundland Island ; paleoecology ; Paleontology ; Paleozoic ; Palynology ; Palynomorphs ; Port au Port Peninsula ; sandstone ; scolecodonts ; sedimentary rocks ; siltstone ; Siltstones ; species diversity ; Spores ; Stellatispora ; Stellatispora fahraeusi ; Stratigraphy ; Taxa ; taxonomy ; terrestrial environment ; vegetation ; Vermes</subject><ispartof>Palynology, 2002, Vol.26 (1), p.185-215</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute.</rights><rights>Copyright 2002 The American Association of Stratigraphic Palynologists Foundation</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a1501-e7cf1f9ff67ea5ba06c8f57725d6143ab1a4d69c510a2ddd291abbbf24af229d3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/3687691$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/3687691$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>315,782,786,805,4026,27930,27931,27932,58024,58257</link.rule.ids></links><search><creatorcontrib>Burden, Elliott T</creatorcontrib><creatorcontrib>Quinn, Louise</creatorcontrib><creatorcontrib>Nowlan, Godfrey S</creatorcontrib><creatorcontrib>Bailey-Nill, Linda A</creatorcontrib><title>Palynology and micropaleontology of the Clam Bank Formation (Lower Devonian) of western Newfoundland, Canada</title><title>Palynology</title><description>Sandstone and siltstone samples collected from the lowest part of the Clam Bank Formation in western Newfoundland contain a distinctive monospecific conodont assemblage of Ozarkodina remscheidensis eosteinhornensis and O. remscheidensis ssp., confidently dated as Late Ludlow through Lochkovian. Palynomorph assemblages of terrestrial spores, acritarchs, chitinozoans, scolecodonts and plant fragments are relatively abundant and diverse in the lower 250 m of this formation. Taxa include the cryptospore genera Cymbohilates, Acontotetras, Hispanaediscus, Laevolancis, and Tetrahedraletes, spore genera Ambitisporites, Aneurospora, Apiculiretusispora, Emphanisporites, Retusotriletes, Synorisporites, Vermiverruspora, and a new species Stellatispora fahraeusi. Acritarchs include the taxon Triangulina sanpetrensis and chitinozoa include Angochitina chlupaci. Palynomorphs indicate a Lochkovian age, corresponding with the Apiculiretusispora sp. E zone from Europe. In well preserved samples from this section, the fossil terrestrial palynomorph assemblages from these shallow marine deposits correspond closely in species diversity and concentration with values reported for modern shelf deposits located adjacent to low Arctic moss and sedge tundra. By inference, earliest Devonian terrestrial vegetation must have been relatively well developed on this ancient coastline.</description><subject>acritarchs</subject><subject>assemblages</subject><subject>Canada</subject><subject>Chitinozoa</subject><subject>Clam Bank Formation</subject><subject>Clams</subject><subject>clastic rocks</subject><subject>coastal environment</subject><subject>Conodonta</subject><subject>correlation</subject><subject>Devonian</subject><subject>Eastern Canada</subject><subject>Fossils</subject><subject>Geological surveys</subject><subject>Geology</subject><subject>Invertebrata</subject><subject>Lochkovian</subject><subject>Lower Devonian</subject><subject>microfossils</subject><subject>new taxa</subject><subject>Newfoundland</subject><subject>Newfoundland and Labrador</subject><subject>Newfoundland Island</subject><subject>paleoecology</subject><subject>Paleontology</subject><subject>Paleozoic</subject><subject>Palynology</subject><subject>Palynomorphs</subject><subject>Port au Port Peninsula</subject><subject>sandstone</subject><subject>scolecodonts</subject><subject>sedimentary rocks</subject><subject>siltstone</subject><subject>Siltstones</subject><subject>species diversity</subject><subject>Spores</subject><subject>Stellatispora</subject><subject>Stellatispora fahraeusi</subject><subject>Stratigraphy</subject><subject>Taxa</subject><subject>taxonomy</subject><subject>terrestrial environment</subject><subject>vegetation</subject><subject>Vermes</subject><issn>0191-6122</issn><issn>1558-9188</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNo9kFFLwzAUhYMoOKf4B3zIm4pWc5MlbR-1OhWG-qDP5bZJZmebjLSz7N9b6fDpwj0fB85HyCmwGw4gbhlXDBK5RyYgZRKlkCT7ZMIghUgB54fkqG1XjAklZDIh9TvWW-drv9xSdJo2VRn8GmvjXTd-vaXdl6FZjQ29R_dN5z402FXe0YuF702gD-bHuwrd5R_bm7YzwdFX01u_cboeWq9phg41HpMDi3VrTnZ3Sj7njx_Zc7R4e3rJ7hYRgmQQmbi0YFNrVWxQFshUmVgZx1xqBTOBBeBMq7SUwJBrrXkKWBSF5TO0nKdaTMn52DtsadtgbL4OVYNhmwPL_yTlO0kDeTaSq7bz4R8TKolVCkN8NcZL49uyMq40vQ-1zld-E9wwIeeDyZyJGICLX1_2cp0</recordid><startdate>2002</startdate><enddate>2002</enddate><creator>Burden, Elliott T</creator><creator>Quinn, Louise</creator><creator>Nowlan, Godfrey S</creator><creator>Bailey-Nill, Linda A</creator><general>American Association of Stratigraphic Palynologists</general><general>American Association of Stratigraphic Palynologists Foundation</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>2002</creationdate><title>Palynology and micropaleontology of the Clam Bank Formation (Lower Devonian) of western Newfoundland, Canada</title><author>Burden, Elliott T ; Quinn, Louise ; Nowlan, Godfrey S ; Bailey-Nill, Linda A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a1501-e7cf1f9ff67ea5ba06c8f57725d6143ab1a4d69c510a2ddd291abbbf24af229d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>acritarchs</topic><topic>assemblages</topic><topic>Canada</topic><topic>Chitinozoa</topic><topic>Clam Bank Formation</topic><topic>Clams</topic><topic>clastic rocks</topic><topic>coastal environment</topic><topic>Conodonta</topic><topic>correlation</topic><topic>Devonian</topic><topic>Eastern Canada</topic><topic>Fossils</topic><topic>Geological surveys</topic><topic>Geology</topic><topic>Invertebrata</topic><topic>Lochkovian</topic><topic>Lower Devonian</topic><topic>microfossils</topic><topic>new taxa</topic><topic>Newfoundland</topic><topic>Newfoundland and Labrador</topic><topic>Newfoundland Island</topic><topic>paleoecology</topic><topic>Paleontology</topic><topic>Paleozoic</topic><topic>Palynology</topic><topic>Palynomorphs</topic><topic>Port au Port Peninsula</topic><topic>sandstone</topic><topic>scolecodonts</topic><topic>sedimentary rocks</topic><topic>siltstone</topic><topic>Siltstones</topic><topic>species diversity</topic><topic>Spores</topic><topic>Stellatispora</topic><topic>Stellatispora fahraeusi</topic><topic>Stratigraphy</topic><topic>Taxa</topic><topic>taxonomy</topic><topic>terrestrial environment</topic><topic>vegetation</topic><topic>Vermes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Burden, Elliott T</creatorcontrib><creatorcontrib>Quinn, Louise</creatorcontrib><creatorcontrib>Nowlan, Godfrey S</creatorcontrib><creatorcontrib>Bailey-Nill, Linda A</creatorcontrib><collection>CrossRef</collection><jtitle>Palynology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Burden, Elliott T</au><au>Quinn, Louise</au><au>Nowlan, Godfrey S</au><au>Bailey-Nill, Linda A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Palynology and micropaleontology of the Clam Bank Formation (Lower Devonian) of western Newfoundland, Canada</atitle><jtitle>Palynology</jtitle><date>2002</date><risdate>2002</risdate><volume>26</volume><issue>1</issue><spage>185</spage><epage>215</epage><pages>185-215</pages><issn>0191-6122</issn><eissn>1558-9188</eissn><abstract>Sandstone and siltstone samples collected from the lowest part of the Clam Bank Formation in western Newfoundland contain a distinctive monospecific conodont assemblage of Ozarkodina remscheidensis eosteinhornensis and O. remscheidensis ssp., confidently dated as Late Ludlow through Lochkovian. Palynomorph assemblages of terrestrial spores, acritarchs, chitinozoans, scolecodonts and plant fragments are relatively abundant and diverse in the lower 250 m of this formation. Taxa include the cryptospore genera Cymbohilates, Acontotetras, Hispanaediscus, Laevolancis, and Tetrahedraletes, spore genera Ambitisporites, Aneurospora, Apiculiretusispora, Emphanisporites, Retusotriletes, Synorisporites, Vermiverruspora, and a new species Stellatispora fahraeusi. Acritarchs include the taxon Triangulina sanpetrensis and chitinozoa include Angochitina chlupaci. Palynomorphs indicate a Lochkovian age, corresponding with the Apiculiretusispora sp. E zone from Europe. In well preserved samples from this section, the fossil terrestrial palynomorph assemblages from these shallow marine deposits correspond closely in species diversity and concentration with values reported for modern shelf deposits located adjacent to low Arctic moss and sedge tundra. By inference, earliest Devonian terrestrial vegetation must have been relatively well developed on this ancient coastline.</abstract><pub>American Association of Stratigraphic Palynologists</pub><doi>10.2113/0260185</doi><tpages>31</tpages></addata></record> |
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| subjects | acritarchs assemblages Canada Chitinozoa Clam Bank Formation Clams clastic rocks coastal environment Conodonta correlation Devonian Eastern Canada Fossils Geological surveys Geology Invertebrata Lochkovian Lower Devonian microfossils new taxa Newfoundland Newfoundland and Labrador Newfoundland Island paleoecology Paleontology Paleozoic Palynology Palynomorphs Port au Port Peninsula sandstone scolecodonts sedimentary rocks siltstone Siltstones species diversity Spores Stellatispora Stellatispora fahraeusi Stratigraphy Taxa taxonomy terrestrial environment vegetation Vermes |
| title | Palynology and micropaleontology of the Clam Bank Formation (Lower Devonian) of western Newfoundland, Canada |
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