Benthic foraminifera from the Albian shallow-marine limestones in the Geyik Dağı area (Central Taurides), southern Turkey
Cretaceous carbonates in the Geyik Dağı area (Central Taurides, southern Turkey) are represented by two successions with different paleoenvironmental settings: open shelf to slope succession of Cenomanian to Danian age and inner platform succession of Albian to Maastrichtian age, which is interrupte...
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| Veröffentlicht in: | Journal of paleontology 2021-07, Vol.95 (4), p.673-693 |
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| creator | Solak, Cemile Taslı, Kemal Koç, Hayati |
| description | Cretaceous carbonates in the Geyik Dağı area (Central Taurides, southern Turkey) are represented by two successions with different paleoenvironmental settings: open shelf to slope succession of Cenomanian to Danian age and inner platform succession of Albian to Maastrichtian age, which is interrupted by a post-Cenomanian disconformity. Outcropped lowermost part of the platform-type one is composed of rudistid limestones corresponding to the Urgonian-type carbonates and belongs to the Geyik Dağı Unit (=Anamas-Akseki Carbonate Platform). It contains a rich assemblage of larger benthic foraminifera including orbitolinid, chrysalidinid, cuneolinid, nezzazatid, and miliolid taxa, which has been illustrated and documented here for the first time from the upper Albian of the Tauride Carbonate Platform. The occurrence of such a diversified foraminiferal fauna indicates a prominent high diversity that took place in the Tauride Carbonate Platform during the late Albian time, which corresponds to a major emersion period in some parts of the platform. |
| doi_str_mv | 10.1017/jpa.2021.17 |
| format | Article |
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Outcropped lowermost part of the platform-type one is composed of rudistid limestones corresponding to the Urgonian-type carbonates and belongs to the Geyik Dağı Unit (=Anamas-Akseki Carbonate Platform). It contains a rich assemblage of larger benthic foraminifera including orbitolinid, chrysalidinid, cuneolinid, nezzazatid, and miliolid taxa, which has been illustrated and documented here for the first time from the upper Albian of the Tauride Carbonate Platform. The occurrence of such a diversified foraminiferal fauna indicates a prominent high diversity that took place in the Tauride Carbonate Platform during the late Albian time, which corresponds to a major emersion period in some parts of the platform.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><identifier>DOI: 10.1017/jpa.2021.17</identifier><language>eng</language><publisher>New York, USA: The Paleontological Society</publisher><subject>Age ; Albian ; Anatolia ; Asia ; assemblages ; benthic taxa ; Benthos ; biostratigraphy ; Carbonates ; Cretaceous ; Fault lines ; Foraminifera ; Geyik Mountains ; invertebrate ; lithostratigraphy ; Lower Cretaceous ; Mesozoic ; microfossils ; Middle East ; morphology ; Paleontology ; Platforms (geology) ; REGULAR ARTICLES ; Sediments ; Stratigraphy ; Taurus Mountains ; Taxonomy ; tests ; Turkey</subject><ispartof>Journal of paleontology, 2021-07, Vol.95 (4), p.673-693</ispartof><rights>Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of The Paleontological Society</rights><rights>GeoRef, Copyright 2021, American Geosciences Institute. Reference includes data from GeoScienceWorld @Alexandria, VA @USA @United States. Abstract, Copyright, The Paleontological Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a322t-1ed88c415a62f3a6136935ecb74146a790a8ddc497ad0a816cee48c04b1ec6d23</citedby><cites>FETCH-LOGICAL-a322t-1ed88c415a62f3a6136935ecb74146a790a8ddc497ad0a816cee48c04b1ec6d23</cites><orcidid>0000-0003-1393-5625</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0022336021000172/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>164,314,780,784,27924,27925,55628</link.rule.ids></links><search><creatorcontrib>Solak, Cemile</creatorcontrib><creatorcontrib>Taslı, Kemal</creatorcontrib><creatorcontrib>Koç, Hayati</creatorcontrib><title>Benthic foraminifera from the Albian shallow-marine limestones in the Geyik Dağı area (Central Taurides), southern Turkey</title><title>Journal of paleontology</title><addtitle>J. Paleontol</addtitle><description>Cretaceous carbonates in the Geyik Dağı area (Central Taurides, southern Turkey) are represented by two successions with different paleoenvironmental settings: open shelf to slope succession of Cenomanian to Danian age and inner platform succession of Albian to Maastrichtian age, which is interrupted by a post-Cenomanian disconformity. Outcropped lowermost part of the platform-type one is composed of rudistid limestones corresponding to the Urgonian-type carbonates and belongs to the Geyik Dağı Unit (=Anamas-Akseki Carbonate Platform). It contains a rich assemblage of larger benthic foraminifera including orbitolinid, chrysalidinid, cuneolinid, nezzazatid, and miliolid taxa, which has been illustrated and documented here for the first time from the upper Albian of the Tauride Carbonate Platform. The occurrence of such a diversified foraminiferal fauna indicates a prominent high diversity that took place in the Tauride Carbonate Platform during the late Albian time, which corresponds to a major emersion period in some parts of the platform.</description><subject>Age</subject><subject>Albian</subject><subject>Anatolia</subject><subject>Asia</subject><subject>assemblages</subject><subject>benthic taxa</subject><subject>Benthos</subject><subject>biostratigraphy</subject><subject>Carbonates</subject><subject>Cretaceous</subject><subject>Fault lines</subject><subject>Foraminifera</subject><subject>Geyik Mountains</subject><subject>invertebrate</subject><subject>lithostratigraphy</subject><subject>Lower Cretaceous</subject><subject>Mesozoic</subject><subject>microfossils</subject><subject>Middle East</subject><subject>morphology</subject><subject>Paleontology</subject><subject>Platforms (geology)</subject><subject>REGULAR ARTICLES</subject><subject>Sediments</subject><subject>Stratigraphy</subject><subject>Taurus Mountains</subject><subject>Taxonomy</subject><subject>tests</subject><subject>Turkey</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp9kMFuEzEQQC0EEqFw4gcscaGCDR7bsbPHEqAgVeISzqtZ72zjdNcOdlZVxMfwDfxDPwyHVKIHxGl8eHqeeYy9BDEHAfbddodzKSTMwT5iM6iVraRS9jGbCSFlpZQRT9mznLdCgDQAM_bjPYX9xjvex4SjD76nhLxPceT7DfGLofUYeN7gMMTbasTkA_HBj5T3MVDmPvzhLungb_gHvPt594tjIuSvV0WccOBrnJLvKJ-_5TlOBU6Br6d0Q4fn7EmPQ6YX9_OMffv0cb36XF19vfyyuriqUEm5r4C65dJpWKCRvUIDytRqQa61GrRBWwtcdp3TtcWuPME4Ir10QrdAznRSnbFXJ-8uxe9T2bzZximF8mUjF6rWtVbWFurNiXIp5pyob3bJl4MPDYjmWLcpdZtj3QYe0NcUs_MUHN3GNHQP1EdS6FoaUejq3o1jW2pc01_u3_bzE9_6WDL_d5PfNVSaTg</recordid><startdate>20210701</startdate><enddate>20210701</enddate><creator>Solak, Cemile</creator><creator>Taslı, Kemal</creator><creator>Koç, Hayati</creator><general>The Paleontological Society</general><general>Cambridge University Press</general><general>Paleontological Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>4T-</scope><scope>4U-</scope><scope>7SN</scope><scope>7TN</scope><scope>7XB</scope><scope>88A</scope><scope>88I</scope><scope>8AF</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H95</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>LK8</scope><scope>M2O</scope><scope>M2P</scope><scope>M7P</scope><scope>MBDVC</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>R05</scope><scope>S0X</scope><orcidid>https://orcid.org/0000-0003-1393-5625</orcidid></search><sort><creationdate>20210701</creationdate><title>Benthic foraminifera from the Albian shallow-marine limestones in the Geyik Dağı area (Central Taurides), southern Turkey</title><author>Solak, Cemile ; Taslı, Kemal ; Koç, Hayati</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a322t-1ed88c415a62f3a6136935ecb74146a790a8ddc497ad0a816cee48c04b1ec6d23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Age</topic><topic>Albian</topic><topic>Anatolia</topic><topic>Asia</topic><topic>assemblages</topic><topic>benthic taxa</topic><topic>Benthos</topic><topic>biostratigraphy</topic><topic>Carbonates</topic><topic>Cretaceous</topic><topic>Fault lines</topic><topic>Foraminifera</topic><topic>Geyik Mountains</topic><topic>invertebrate</topic><topic>lithostratigraphy</topic><topic>Lower Cretaceous</topic><topic>Mesozoic</topic><topic>microfossils</topic><topic>Middle East</topic><topic>morphology</topic><topic>Paleontology</topic><topic>Platforms (geology)</topic><topic>REGULAR ARTICLES</topic><topic>Sediments</topic><topic>Stratigraphy</topic><topic>Taurus Mountains</topic><topic>Taxonomy</topic><topic>tests</topic><topic>Turkey</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Solak, Cemile</creatorcontrib><creatorcontrib>Taslı, Kemal</creatorcontrib><creatorcontrib>Koç, Hayati</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Docstoc</collection><collection>University Readers</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Biology Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>eLibrary</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</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>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Biological Science Collection</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Biological Science Database</collection><collection>Research Library (Corporate)</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>ProQuest Central Basic</collection><collection>University of Michigan</collection><collection>SIRS Editorial</collection><jtitle>Journal of paleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Solak, Cemile</au><au>Taslı, Kemal</au><au>Koç, Hayati</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Benthic foraminifera from the Albian shallow-marine limestones in the Geyik Dağı area (Central Taurides), southern Turkey</atitle><jtitle>Journal of paleontology</jtitle><addtitle>J. Paleontol</addtitle><date>2021-07-01</date><risdate>2021</risdate><volume>95</volume><issue>4</issue><spage>673</spage><epage>693</epage><pages>673-693</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><abstract>Cretaceous carbonates in the Geyik Dağı area (Central Taurides, southern Turkey) are represented by two successions with different paleoenvironmental settings: open shelf to slope succession of Cenomanian to Danian age and inner platform succession of Albian to Maastrichtian age, which is interrupted by a post-Cenomanian disconformity. Outcropped lowermost part of the platform-type one is composed of rudistid limestones corresponding to the Urgonian-type carbonates and belongs to the Geyik Dağı Unit (=Anamas-Akseki Carbonate Platform). It contains a rich assemblage of larger benthic foraminifera including orbitolinid, chrysalidinid, cuneolinid, nezzazatid, and miliolid taxa, which has been illustrated and documented here for the first time from the upper Albian of the Tauride Carbonate Platform. The occurrence of such a diversified foraminiferal fauna indicates a prominent high diversity that took place in the Tauride Carbonate Platform during the late Albian time, which corresponds to a major emersion period in some parts of the platform.</abstract><cop>New York, USA</cop><pub>The Paleontological Society</pub><doi>10.1017/jpa.2021.17</doi><tpages>21</tpages><orcidid>https://orcid.org/0000-0003-1393-5625</orcidid></addata></record> |
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| ispartof | Journal of paleontology, 2021-07, Vol.95 (4), p.673-693 |
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| subjects | Age Albian Anatolia Asia assemblages benthic taxa Benthos biostratigraphy Carbonates Cretaceous Fault lines Foraminifera Geyik Mountains invertebrate lithostratigraphy Lower Cretaceous Mesozoic microfossils Middle East morphology Paleontology Platforms (geology) REGULAR ARTICLES Sediments Stratigraphy Taurus Mountains Taxonomy tests Turkey |
| title | Benthic foraminifera from the Albian shallow-marine limestones in the Geyik Dağı area (Central Taurides), southern Turkey |
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