Infrazonal biostratigraphy of the Upper Cretaceous in the East European province based on benthic foraminifers, Part 1: Cenomanian-Coniacian
A chart of infrazonal biostratigraphic subdivision of Cenomanian-Coniacian deposits in the East European paleobiogeographic province is based on distribution of benthic foraminifers. The suggested chart characterizes successive trend of changes in ecologic assemblages of benthic foraminifers and mor...
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| Veröffentlicht in: | Stratigraphy and geological correlation 2008-06, Vol.16 (3), p.257-266 |
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| description | A chart of infrazonal biostratigraphic subdivision of Cenomanian-Coniacian deposits in the East European paleobiogeographic province is based on distribution of benthic foraminifers. The suggested chart characterizes successive trend of changes in ecologic assemblages of benthic foraminifers and morphologic evolution of certain agglutinated (
Gaudryina, Bolivinopsis, Heterostomella, Arenobulimina, Ataxophragmium, Ataxoorbignyna, Marssonella
) and secretory (
Globorotalites, Valvulinera, Gyroidinoides, Stensioeina, Osangularia, Berthelina, Pseudovalvulineria, Gavelinella, Cibicides, Praebulimina, Reussella
) foraminiferal genera. The chart includes 7 zones and 13 subzones, most of which are recognizable over the vast territory from the Mangyshalk to southern Baltic areas. It is correlated with the acknowledged ammonoid and inoceramid zonations. Five stadia of taxonomic changes in foraminiferal assemblages, which are substantiated in this work, show that principal biotic events took place in the mid-late Cenomanian, during the Cenomanian-Turonian and early-middle Turonian transitions, in the late Turonian, and at the early-middle Coniacian boundary time. |
| doi_str_mv | 10.1134/S0869593808030039 |
| format | Article |
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Gaudryina, Bolivinopsis, Heterostomella, Arenobulimina, Ataxophragmium, Ataxoorbignyna, Marssonella
) and secretory (
Globorotalites, Valvulinera, Gyroidinoides, Stensioeina, Osangularia, Berthelina, Pseudovalvulineria, Gavelinella, Cibicides, Praebulimina, Reussella
) foraminiferal genera. The chart includes 7 zones and 13 subzones, most of which are recognizable over the vast territory from the Mangyshalk to southern Baltic areas. It is correlated with the acknowledged ammonoid and inoceramid zonations. Five stadia of taxonomic changes in foraminiferal assemblages, which are substantiated in this work, show that principal biotic events took place in the mid-late Cenomanian, during the Cenomanian-Turonian and early-middle Turonian transitions, in the late Turonian, and at the early-middle Coniacian boundary time.</description><identifier>ISSN: 0869-5938</identifier><identifier>EISSN: 1555-6263</identifier><identifier>DOI: 10.1134/S0869593808030039</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Ammonoidea ; Archaeology ; Cibicides ; Cretaceous ; Earth and Environmental Science ; Earth Sciences ; Evolution ; Foraminifera ; Gaudryina ; Geophysics/Geodesy ; Gyroidinoides ; Historical Geology ; Mineralogy ; Morphology ; Osangularia ; Reussella ; Sedimentology ; Stratigraphy ; Structural Geology ; Taxonomy</subject><ispartof>Stratigraphy and geological correlation, 2008-06, Vol.16 (3), p.257-266</ispartof><rights>Pleiades Publishing, Ltd. 2008</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c346t-976a45488c4afb5c8642bd50ac9c499f13139304adf1e9197f9b706c3343507c3</citedby><cites>FETCH-LOGICAL-c346t-976a45488c4afb5c8642bd50ac9c499f13139304adf1e9197f9b706c3343507c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0869593808030039$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0869593808030039$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Beniamovski, V. N.</creatorcontrib><title>Infrazonal biostratigraphy of the Upper Cretaceous in the East European province based on benthic foraminifers, Part 1: Cenomanian-Coniacian</title><title>Stratigraphy and geological correlation</title><addtitle>Stratigr. Geol. Correl</addtitle><description>A chart of infrazonal biostratigraphic subdivision of Cenomanian-Coniacian deposits in the East European paleobiogeographic province is based on distribution of benthic foraminifers. The suggested chart characterizes successive trend of changes in ecologic assemblages of benthic foraminifers and morphologic evolution of certain agglutinated (
Gaudryina, Bolivinopsis, Heterostomella, Arenobulimina, Ataxophragmium, Ataxoorbignyna, Marssonella
) and secretory (
Globorotalites, Valvulinera, Gyroidinoides, Stensioeina, Osangularia, Berthelina, Pseudovalvulineria, Gavelinella, Cibicides, Praebulimina, Reussella
) foraminiferal genera. The chart includes 7 zones and 13 subzones, most of which are recognizable over the vast territory from the Mangyshalk to southern Baltic areas. It is correlated with the acknowledged ammonoid and inoceramid zonations. Five stadia of taxonomic changes in foraminiferal assemblages, which are substantiated in this work, show that principal biotic events took place in the mid-late Cenomanian, during the Cenomanian-Turonian and early-middle Turonian transitions, in the late Turonian, and at the early-middle Coniacian boundary time.</description><subject>Ammonoidea</subject><subject>Archaeology</subject><subject>Cibicides</subject><subject>Cretaceous</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evolution</subject><subject>Foraminifera</subject><subject>Gaudryina</subject><subject>Geophysics/Geodesy</subject><subject>Gyroidinoides</subject><subject>Historical Geology</subject><subject>Mineralogy</subject><subject>Morphology</subject><subject>Osangularia</subject><subject>Reussella</subject><subject>Sedimentology</subject><subject>Stratigraphy</subject><subject>Structural Geology</subject><subject>Taxonomy</subject><issn>0869-5938</issn><issn>1555-6263</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kdtKAzEQhoMoWA8P4F3wwitXk02yu_FOlnoAQUF7vcymSRtpkzVJBX0GH9rUCoLi1Qzzf_8wB4SOKDmjlPHzR9JUUkjWkIYwQpjcQiMqhCiqsmLbaLSWi7W-i_ZifCaEc17VI_Rx60yAd-9ggXvrYwqQ7CzAMH_D3uA013gyDDrgNugESvtVxNZ91ccQEx6vgh80ODwE_2qd0riHqKfYO9xrl-ZWYeMDLK2zRod4ih8gJEwvcKudX4Kz4IrW56BydoB2DCyiPvyO-2hyNX5qb4q7--vb9vKuUIxXqZB1BVzwplEcTC9UU_GynwoCSioupaGMMskIh6mhWlJZG9nXpFKMcSZIrdg-Otn0zUO_rHRM3dJGpRcLcOsFO5rvlEGSweNf4LNfhXyr2JWU8LKktcgQ3UAq-BiDNt0Q7BLCW0dJt35O9-c52VNuPDGzbqbDT-P_TZ_DkpGR</recordid><startdate>20080601</startdate><enddate>20080601</enddate><creator>Beniamovski, V. 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N.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Stratigraphy and geological correlation</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Beniamovski, V. N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Infrazonal biostratigraphy of the Upper Cretaceous in the East European province based on benthic foraminifers, Part 1: Cenomanian-Coniacian</atitle><jtitle>Stratigraphy and geological correlation</jtitle><stitle>Stratigr. Geol. Correl</stitle><date>2008-06-01</date><risdate>2008</risdate><volume>16</volume><issue>3</issue><spage>257</spage><epage>266</epage><pages>257-266</pages><issn>0869-5938</issn><eissn>1555-6263</eissn><abstract>A chart of infrazonal biostratigraphic subdivision of Cenomanian-Coniacian deposits in the East European paleobiogeographic province is based on distribution of benthic foraminifers. The suggested chart characterizes successive trend of changes in ecologic assemblages of benthic foraminifers and morphologic evolution of certain agglutinated (
Gaudryina, Bolivinopsis, Heterostomella, Arenobulimina, Ataxophragmium, Ataxoorbignyna, Marssonella
) and secretory (
Globorotalites, Valvulinera, Gyroidinoides, Stensioeina, Osangularia, Berthelina, Pseudovalvulineria, Gavelinella, Cibicides, Praebulimina, Reussella
) foraminiferal genera. The chart includes 7 zones and 13 subzones, most of which are recognizable over the vast territory from the Mangyshalk to southern Baltic areas. It is correlated with the acknowledged ammonoid and inoceramid zonations. Five stadia of taxonomic changes in foraminiferal assemblages, which are substantiated in this work, show that principal biotic events took place in the mid-late Cenomanian, during the Cenomanian-Turonian and early-middle Turonian transitions, in the late Turonian, and at the early-middle Coniacian boundary time.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0869593808030039</doi><tpages>10</tpages></addata></record> |
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| subjects | Ammonoidea Archaeology Cibicides Cretaceous Earth and Environmental Science Earth Sciences Evolution Foraminifera Gaudryina Geophysics/Geodesy Gyroidinoides Historical Geology Mineralogy Morphology Osangularia Reussella Sedimentology Stratigraphy Structural Geology Taxonomy |
| title | Infrazonal biostratigraphy of the Upper Cretaceous in the East European province based on benthic foraminifers, Part 1: Cenomanian-Coniacian |
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