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Late Changhsingian foraminifers of the northwestern Caucasus
Small foraminifers and fusulinaceans from Upper Permian strata in the Bolshaya and Malaya Laba, and Belaya river basins in the Peredovoy Range of the Northwestern Caucasus have been restudied. New age data show that they are clearly Late Changhsingian in age. The foraminifers occur in rocks in isola...
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Published in: | Micropaleontology 2001, Vol.47 (3), p.205-234 |
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description | Small foraminifers and fusulinaceans from Upper Permian strata in the Bolshaya and Malaya Laba, and Belaya river basins in the Peredovoy Range of the Northwestern Caucasus have been restudied. New age data show that they are clearly Late Changhsingian in age. The foraminifers occur in rocks in isolated outcrops that include bedded limestone, biohermal buildups, and terrigenous clastics. Many foraminiferal species previously described by K. Miklukho-Maklay in 1954 are here revised and redescribed based on specimens from some of the same sections. Nine new species and two new genera of small foraminifers are described. The foraminifer assemblage is correlated with similar coeval associations in South China, the South Primorye, Pamirs, and Transcaucasia. |
doi_str_mv | 10.2113/47.3.205 |
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New age data show that they are clearly Late Changhsingian in age. The foraminifers occur in rocks in isolated outcrops that include bedded limestone, biohermal buildups, and terrigenous clastics. Many foraminiferal species previously described by K. Miklukho-Maklay in 1954 are here revised and redescribed based on specimens from some of the same sections. Nine new species and two new genera of small foraminifers are described. The foraminifer assemblage is correlated with similar coeval associations in South China, the South Primorye, Pamirs, and Transcaucasia.</description><identifier>ISSN: 0026-2803</identifier><identifier>EISSN: 1937-2795</identifier><identifier>DOI: 10.2113/47.3.205</identifier><language>eng</language><publisher>American Museum of Natural History</publisher><subject>Abadehella grandis ; Agathammina psebaensis ; assemblages ; biostratigraphy ; biozones ; Caucasus ; Changhsingian ; Changhsingian age ; Commonwealth of Independent States ; correlation ; Europe ; faunal list ; Foraminifera ; Fusulinaceae ; Fusulinina ; Genera ; Geology ; Graecodiscus kotlyarae ; Hemigordius nikitinensis ; Holotypes ; Illustrative plates ; Invertebrata ; Langella malalabensis ; Lithofacies ; marine environment ; microfossils ; Midiella karinae ; morphology ; new taxa ; Northern Caucasus ; Orientalism ; Paleozoic ; Peredovoy Range ; Permian ; Protista ; Pseudocolaniella longa ; Pseudomidiella labensis ; Ravines ; River basins ; Russian Federation ; Specimens ; Stratigraphy ; taxonomy ; Upper Permian ; Urushtenella latebrosa</subject><ispartof>Micropaleontology, 2001, Vol.47 (3), p.205-234</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute.</rights><rights>Copyright 2001 Micropaleontology Press</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a402t-fc2ab3e3df8a6dcd74466e88973296efc64ebbc5fa1c949b083a35e96c1f42513</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1486002$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1486002$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,4024,27923,27924,27925,58238,58471</link.rule.ids></links><search><creatorcontrib>Pronina-Nestell, Galina P</creatorcontrib><creatorcontrib>Nestell, Merlynd K</creatorcontrib><title>Late Changhsingian foraminifers of the northwestern Caucasus</title><title>Micropaleontology</title><description>Small foraminifers and fusulinaceans from Upper Permian strata in the Bolshaya and Malaya Laba, and Belaya river basins in the Peredovoy Range of the Northwestern Caucasus have been restudied. New age data show that they are clearly Late Changhsingian in age. The foraminifers occur in rocks in isolated outcrops that include bedded limestone, biohermal buildups, and terrigenous clastics. Many foraminiferal species previously described by K. Miklukho-Maklay in 1954 are here revised and redescribed based on specimens from some of the same sections. Nine new species and two new genera of small foraminifers are described. The foraminifer assemblage is correlated with similar coeval associations in South China, the South Primorye, Pamirs, and Transcaucasia.</description><subject>Abadehella grandis</subject><subject>Agathammina psebaensis</subject><subject>assemblages</subject><subject>biostratigraphy</subject><subject>biozones</subject><subject>Caucasus</subject><subject>Changhsingian</subject><subject>Changhsingian age</subject><subject>Commonwealth of Independent States</subject><subject>correlation</subject><subject>Europe</subject><subject>faunal list</subject><subject>Foraminifera</subject><subject>Fusulinaceae</subject><subject>Fusulinina</subject><subject>Genera</subject><subject>Geology</subject><subject>Graecodiscus kotlyarae</subject><subject>Hemigordius nikitinensis</subject><subject>Holotypes</subject><subject>Illustrative plates</subject><subject>Invertebrata</subject><subject>Langella malalabensis</subject><subject>Lithofacies</subject><subject>marine environment</subject><subject>microfossils</subject><subject>Midiella karinae</subject><subject>morphology</subject><subject>new taxa</subject><subject>Northern Caucasus</subject><subject>Orientalism</subject><subject>Paleozoic</subject><subject>Peredovoy Range</subject><subject>Permian</subject><subject>Protista</subject><subject>Pseudocolaniella longa</subject><subject>Pseudomidiella labensis</subject><subject>Ravines</subject><subject>River basins</subject><subject>Russian Federation</subject><subject>Specimens</subject><subject>Stratigraphy</subject><subject>taxonomy</subject><subject>Upper Permian</subject><subject>Urushtenella latebrosa</subject><issn>0026-2803</issn><issn>1937-2795</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNpFkE1LxDAQhoMouK6CP8BDTyJI13w1ScGLFL9gwYueQ5pOtl26yZq0iP_eyAqe5vA-vDPzIHRJ8IoSwu64XLEVxdURWpCayZLKujpGC4ypKKnC7BSdpbTFGCshqwW6X5sJiqY3ftOnwW8G4wsXotkNfnAQUxFcMfVQ-BCn_gvSBNEXjZmtSXM6RyfOjAku_uYSfTw9vjcv5frt-bV5WJeGYzqVzlLTMmCdU0Z0tpOcCwFK1ZLRWoCzgkPb2soZYmtet1gxwyqohSWO04qwJbo-9O5j-JzzEXo3JAvjaDyEOWmiKOMVkRm8OYA2hpQiOL2Pw87Eb02w_tWjudRMZz0ZvTqg2zSF-M9xJbKrHN8e4g2EZAfwFr5CHDu9DXP0-dlcgpnGPO_G7Ae3W2-K</recordid><startdate>2001</startdate><enddate>2001</enddate><creator>Pronina-Nestell, Galina P</creator><creator>Nestell, Merlynd K</creator><general>American Museum of Natural History</general><general>Micropaleontology Press, American Museum of Natural History</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>2001</creationdate><title>Late Changhsingian foraminifers of the northwestern Caucasus</title><author>Pronina-Nestell, Galina P ; Nestell, Merlynd K</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a402t-fc2ab3e3df8a6dcd74466e88973296efc64ebbc5fa1c949b083a35e96c1f42513</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Abadehella grandis</topic><topic>Agathammina psebaensis</topic><topic>assemblages</topic><topic>biostratigraphy</topic><topic>biozones</topic><topic>Caucasus</topic><topic>Changhsingian</topic><topic>Changhsingian age</topic><topic>Commonwealth of Independent States</topic><topic>correlation</topic><topic>Europe</topic><topic>faunal list</topic><topic>Foraminifera</topic><topic>Fusulinaceae</topic><topic>Fusulinina</topic><topic>Genera</topic><topic>Geology</topic><topic>Graecodiscus kotlyarae</topic><topic>Hemigordius nikitinensis</topic><topic>Holotypes</topic><topic>Illustrative plates</topic><topic>Invertebrata</topic><topic>Langella malalabensis</topic><topic>Lithofacies</topic><topic>marine environment</topic><topic>microfossils</topic><topic>Midiella karinae</topic><topic>morphology</topic><topic>new taxa</topic><topic>Northern Caucasus</topic><topic>Orientalism</topic><topic>Paleozoic</topic><topic>Peredovoy Range</topic><topic>Permian</topic><topic>Protista</topic><topic>Pseudocolaniella longa</topic><topic>Pseudomidiella labensis</topic><topic>Ravines</topic><topic>River basins</topic><topic>Russian Federation</topic><topic>Specimens</topic><topic>Stratigraphy</topic><topic>taxonomy</topic><topic>Upper Permian</topic><topic>Urushtenella latebrosa</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pronina-Nestell, Galina P</creatorcontrib><creatorcontrib>Nestell, Merlynd K</creatorcontrib><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Micropaleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pronina-Nestell, Galina P</au><au>Nestell, Merlynd K</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Changhsingian foraminifers of the northwestern Caucasus</atitle><jtitle>Micropaleontology</jtitle><date>2001</date><risdate>2001</risdate><volume>47</volume><issue>3</issue><spage>205</spage><epage>234</epage><pages>205-234</pages><issn>0026-2803</issn><eissn>1937-2795</eissn><abstract>Small foraminifers and fusulinaceans from Upper Permian strata in the Bolshaya and Malaya Laba, and Belaya river basins in the Peredovoy Range of the Northwestern Caucasus have been restudied. New age data show that they are clearly Late Changhsingian in age. The foraminifers occur in rocks in isolated outcrops that include bedded limestone, biohermal buildups, and terrigenous clastics. Many foraminiferal species previously described by K. Miklukho-Maklay in 1954 are here revised and redescribed based on specimens from some of the same sections. Nine new species and two new genera of small foraminifers are described. The foraminifer assemblage is correlated with similar coeval associations in South China, the South Primorye, Pamirs, and Transcaucasia.</abstract><pub>American Museum of Natural History</pub><doi>10.2113/47.3.205</doi><tpages>30</tpages></addata></record> |
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subjects | Abadehella grandis Agathammina psebaensis assemblages biostratigraphy biozones Caucasus Changhsingian Changhsingian age Commonwealth of Independent States correlation Europe faunal list Foraminifera Fusulinaceae Fusulinina Genera Geology Graecodiscus kotlyarae Hemigordius nikitinensis Holotypes Illustrative plates Invertebrata Langella malalabensis Lithofacies marine environment microfossils Midiella karinae morphology new taxa Northern Caucasus Orientalism Paleozoic Peredovoy Range Permian Protista Pseudocolaniella longa Pseudomidiella labensis Ravines River basins Russian Federation Specimens Stratigraphy taxonomy Upper Permian Urushtenella latebrosa |
title | Late Changhsingian foraminifers of the northwestern Caucasus |
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