Costinuculana magharensis n. gen. n. sp. (Bivalvia, Nuculanidae) from the Middle Jurassic of Gebel Maghara, North Sinai, Egypt
The nuculanid bivalve Costinuculana magharensis new genus new species is described from the middle to upper Bathonian Kehailia Formation of Gebel Maghara, North Sinai, Egypt. Costinuculana differs from other genera of the family Nuculanidae by the presence of opisthocline ribs along the rostrum. The...
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description | The nuculanid bivalve Costinuculana magharensis new genus new species is described from the middle to upper Bathonian Kehailia Formation of Gebel Maghara, North Sinai, Egypt. Costinuculana differs from other genera of the family Nuculanidae by the presence of opisthocline ribs along the rostrum. These ribs are variable in shape and size, straight to folded posteriorly, bifurcate ventrally and occasionally postero-dorsally, and cover an area ~45% of the total valve length from the posterior end. The life position of C. magharensis n. gen. n. sp. is reconstructed on the basis of a functional interpretation of its morphology and by comparison with closely related Recent forms. The asymmetrical commarginal ribs facilitated the burrowing process. The posterior oblique ribs are asymmetrical in cross-section with a steeply concave side in the burrowing direction and slightly convex side in the opposite direction. They probably kept the bivalve in a stable position once the desired depth had been reached. The thick oblique ribs probably also increased the strength of the rostrum and offered resistance against durophagous predators, being presumably partly exposed above the sediment-water interface. Based on the associated fauna, Costinuculana n. gen. lived in a low-energy environment characterized by a fine-grained, soft substrate. |
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(Bivalvia, Nuculanidae) from the Middle Jurassic of Gebel Maghara, North Sinai, Egypt</title><source>Jstor Complete Legacy</source><source>Cambridge University Press Journals Complete</source><creator>Ayoub-Hannaa, Wagih S ; Abdelhady, Ahmad A ; Fürsich, Franz T</creator><creatorcontrib>Ayoub-Hannaa, Wagih S ; Abdelhady, Ahmad A ; Fürsich, Franz T</creatorcontrib><description>The nuculanid bivalve Costinuculana magharensis new genus new species is described from the middle to upper Bathonian Kehailia Formation of Gebel Maghara, North Sinai, Egypt. Costinuculana differs from other genera of the family Nuculanidae by the presence of opisthocline ribs along the rostrum. These ribs are variable in shape and size, straight to folded posteriorly, bifurcate ventrally and occasionally postero-dorsally, and cover an area ~45% of the total valve length from the posterior end. The life position of C. magharensis n. gen. n. sp. is reconstructed on the basis of a functional interpretation of its morphology and by comparison with closely related Recent forms. The asymmetrical commarginal ribs facilitated the burrowing process. The posterior oblique ribs are asymmetrical in cross-section with a steeply concave side in the burrowing direction and slightly convex side in the opposite direction. They probably kept the bivalve in a stable position once the desired depth had been reached. The thick oblique ribs probably also increased the strength of the rostrum and offered resistance against durophagous predators, being presumably partly exposed above the sediment-water interface. Based on the associated fauna, Costinuculana n. gen. lived in a low-energy environment characterized by a fine-grained, soft substrate.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><identifier>DOI: 10.1017/jpa.2016.161</identifier><language>eng</language><publisher>New York, USA: The Paleontological Society</publisher><subject>Abbreviations ; Africa ; Asymmetry ; Autecology ; Autobiographies ; Bathonian ; Bifurcations ; Biostratigraphy ; Bivalvia ; Burrowing organisms ; Carbonates ; Classification ; Classification (sedimentation) ; Coastal environments ; Collections ; Corals ; Costinuculana magharensis ; Cross-sections ; Diagnosis ; Dimensions ; Ecological succession ; Egypt ; Elongation ; Facies ; Fauna ; Fossil animals ; functional morphology ; Gebel Maghara ; Genera ; Geographical variations ; Geology ; Height ; Invertebrata ; invertebrate ; Jurassic ; Kehailia Formation ; Limestone ; Macrofauna ; Magnesium ; Marketing ; Mesozoic ; Middle Jurassic ; Mineral resources ; Mollusca ; Mollusks ; Morphology ; Mountains ; Mud-water interfaces ; New genera ; new taxa ; North Africa ; Nuculanidae ; Orientation ; Palaeontology ; Paleobiology ; Paleoecology ; Paleontology ; Photography ; Physical characteristics ; Predators ; Preservation ; Protobranchia ; Riblets ; Rostrum ; Science ; Sediment ; Sediment-water interface ; Sediments ; Shells ; Sinai Egypt ; Strata ; Stratigraphy ; Taxonomy ; Terminology ; Valves ; Zoobenthos ; Zoology</subject><ispartof>Journal of paleontology, 2017-05, Vol.91 (3), p.434-443</ispartof><rights>2017, The Paleontological Society</rights><rights>Copyright © 2017, The Paleontological Society</rights><rights>GeoRef, Copyright 2020, 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-a488t-1987f660044eee1576eca061a9def03f162417dbe1265168dbc3f116cee065cf3</citedby><cites>FETCH-LOGICAL-a488t-1987f660044eee1576eca061a9def03f162417dbe1265168dbc3f116cee065cf3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/48572651$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S002233601600161X/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>164,314,776,780,799,27901,27902,55603,57992,58225</link.rule.ids></links><search><creatorcontrib>Ayoub-Hannaa, Wagih S</creatorcontrib><creatorcontrib>Abdelhady, Ahmad A</creatorcontrib><creatorcontrib>Fürsich, Franz T</creatorcontrib><title>Costinuculana magharensis n. gen. n. sp. (Bivalvia, Nuculanidae) from the Middle Jurassic of Gebel Maghara, North Sinai, Egypt</title><title>Journal of paleontology</title><addtitle>J. Paleontol</addtitle><description>The nuculanid bivalve Costinuculana magharensis new genus new species is described from the middle to upper Bathonian Kehailia Formation of Gebel Maghara, North Sinai, Egypt. Costinuculana differs from other genera of the family Nuculanidae by the presence of opisthocline ribs along the rostrum. These ribs are variable in shape and size, straight to folded posteriorly, bifurcate ventrally and occasionally postero-dorsally, and cover an area ~45% of the total valve length from the posterior end. The life position of C. magharensis n. gen. n. sp. is reconstructed on the basis of a functional interpretation of its morphology and by comparison with closely related Recent forms. The asymmetrical commarginal ribs facilitated the burrowing process. The posterior oblique ribs are asymmetrical in cross-section with a steeply concave side in the burrowing direction and slightly convex side in the opposite direction. They probably kept the bivalve in a stable position once the desired depth had been reached. The thick oblique ribs probably also increased the strength of the rostrum and offered resistance against durophagous predators, being presumably partly exposed above the sediment-water interface. Based on the associated fauna, Costinuculana n. gen. lived in a low-energy environment characterized by a fine-grained, soft substrate.</description><subject>Abbreviations</subject><subject>Africa</subject><subject>Asymmetry</subject><subject>Autecology</subject><subject>Autobiographies</subject><subject>Bathonian</subject><subject>Bifurcations</subject><subject>Biostratigraphy</subject><subject>Bivalvia</subject><subject>Burrowing organisms</subject><subject>Carbonates</subject><subject>Classification</subject><subject>Classification (sedimentation)</subject><subject>Coastal environments</subject><subject>Collections</subject><subject>Corals</subject><subject>Costinuculana magharensis</subject><subject>Cross-sections</subject><subject>Diagnosis</subject><subject>Dimensions</subject><subject>Ecological succession</subject><subject>Egypt</subject><subject>Elongation</subject><subject>Facies</subject><subject>Fauna</subject><subject>Fossil animals</subject><subject>functional morphology</subject><subject>Gebel Maghara</subject><subject>Genera</subject><subject>Geographical variations</subject><subject>Geology</subject><subject>Height</subject><subject>Invertebrata</subject><subject>invertebrate</subject><subject>Jurassic</subject><subject>Kehailia Formation</subject><subject>Limestone</subject><subject>Macrofauna</subject><subject>Magnesium</subject><subject>Marketing</subject><subject>Mesozoic</subject><subject>Middle Jurassic</subject><subject>Mineral resources</subject><subject>Mollusca</subject><subject>Mollusks</subject><subject>Morphology</subject><subject>Mountains</subject><subject>Mud-water interfaces</subject><subject>New genera</subject><subject>new taxa</subject><subject>North Africa</subject><subject>Nuculanidae</subject><subject>Orientation</subject><subject>Palaeontology</subject><subject>Paleobiology</subject><subject>Paleoecology</subject><subject>Paleontology</subject><subject>Photography</subject><subject>Physical characteristics</subject><subject>Predators</subject><subject>Preservation</subject><subject>Protobranchia</subject><subject>Riblets</subject><subject>Rostrum</subject><subject>Science</subject><subject>Sediment</subject><subject>Sediment-water interface</subject><subject>Sediments</subject><subject>Shells</subject><subject>Sinai Egypt</subject><subject>Strata</subject><subject>Stratigraphy</subject><subject>Taxonomy</subject><subject>Terminology</subject><subject>Valves</subject><subject>Zoobenthos</subject><subject>Zoology</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp9kM1v1DAQxS0EEkvhxhXJEhc-NmEmThzvEValgFo4AOfIcSZZr7JxsJOiXvjbcUgFHBCSZUszv3lv_Bh7jJAiYPnqOOo0A5QpSrzDNrgTZZIJUd5lG4AsS4SQcJ89COEIgJlE3LAfexcmO8xm7vWg-Ul3B-1pCDbwIeUdxSueMKb82Rt7rftrq7f844rbRtNz3np34tOB-JVtmp74h9nrEKzhruUXVFPPr36JLnPOTwf-2Q7abvl5dzNOD9m9VveBHt2-Z-zr2_Mv-3fJ5aeL9_vXl4nOlZoS3KmylRIgz4kIi1KS0SBR7xpqQbQosxzLpqb4qwKlamoTiygNEcjCtOKMPV11R---zRSm6uhmP0TLCtVOFUoJyCK1XSnjXQie2mr09qT9TYVQLQlXMeFqSbiKCUf8yYofw-T8bzZXRbmsEfsv135HLhhLg6HvzvfNH-9s0QQFolSRTm_N9an2tunorx3_bf9iHaitcwP9f9ef3qKiVw</recordid><startdate>20170501</startdate><enddate>20170501</enddate><creator>Ayoub-Hannaa, Wagih S</creator><creator>Abdelhady, Ahmad A</creator><creator>Fürsich, Franz T</creator><general>The Paleontological Society</general><general>Cambridge University Press</general><general>Paleontological Society</general><general>SEPM Society for Sedimentary Geology</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>AEUYN</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></search><sort><creationdate>20170501</creationdate><title>Costinuculana magharensis n. gen. n. sp. (Bivalvia, Nuculanidae) from the Middle Jurassic of Gebel Maghara, North Sinai, Egypt</title><author>Ayoub-Hannaa, Wagih S ; Abdelhady, Ahmad A ; Fürsich, Franz T</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a488t-1987f660044eee1576eca061a9def03f162417dbe1265168dbc3f116cee065cf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Abbreviations</topic><topic>Africa</topic><topic>Asymmetry</topic><topic>Autecology</topic><topic>Autobiographies</topic><topic>Bathonian</topic><topic>Bifurcations</topic><topic>Biostratigraphy</topic><topic>Bivalvia</topic><topic>Burrowing organisms</topic><topic>Carbonates</topic><topic>Classification</topic><topic>Classification (sedimentation)</topic><topic>Coastal environments</topic><topic>Collections</topic><topic>Corals</topic><topic>Costinuculana magharensis</topic><topic>Cross-sections</topic><topic>Diagnosis</topic><topic>Dimensions</topic><topic>Ecological succession</topic><topic>Egypt</topic><topic>Elongation</topic><topic>Facies</topic><topic>Fauna</topic><topic>Fossil animals</topic><topic>functional morphology</topic><topic>Gebel Maghara</topic><topic>Genera</topic><topic>Geographical variations</topic><topic>Geology</topic><topic>Height</topic><topic>Invertebrata</topic><topic>invertebrate</topic><topic>Jurassic</topic><topic>Kehailia Formation</topic><topic>Limestone</topic><topic>Macrofauna</topic><topic>Magnesium</topic><topic>Marketing</topic><topic>Mesozoic</topic><topic>Middle Jurassic</topic><topic>Mineral resources</topic><topic>Mollusca</topic><topic>Mollusks</topic><topic>Morphology</topic><topic>Mountains</topic><topic>Mud-water interfaces</topic><topic>New genera</topic><topic>new taxa</topic><topic>North Africa</topic><topic>Nuculanidae</topic><topic>Orientation</topic><topic>Palaeontology</topic><topic>Paleobiology</topic><topic>Paleoecology</topic><topic>Paleontology</topic><topic>Photography</topic><topic>Physical characteristics</topic><topic>Predators</topic><topic>Preservation</topic><topic>Protobranchia</topic><topic>Riblets</topic><topic>Rostrum</topic><topic>Science</topic><topic>Sediment</topic><topic>Sediment-water interface</topic><topic>Sediments</topic><topic>Shells</topic><topic>Sinai Egypt</topic><topic>Strata</topic><topic>Stratigraphy</topic><topic>Taxonomy</topic><topic>Terminology</topic><topic>Valves</topic><topic>Zoobenthos</topic><topic>Zoology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ayoub-Hannaa, Wagih S</creatorcontrib><creatorcontrib>Abdelhady, Ahmad A</creatorcontrib><creatorcontrib>Fürsich, Franz T</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central 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(Bivalvia, Nuculanidae) from the Middle Jurassic of Gebel Maghara, North Sinai, Egypt</atitle><jtitle>Journal of paleontology</jtitle><addtitle>J. Paleontol</addtitle><date>2017-05-01</date><risdate>2017</risdate><volume>91</volume><issue>3</issue><spage>434</spage><epage>443</epage><pages>434-443</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><abstract>The nuculanid bivalve Costinuculana magharensis new genus new species is described from the middle to upper Bathonian Kehailia Formation of Gebel Maghara, North Sinai, Egypt. Costinuculana differs from other genera of the family Nuculanidae by the presence of opisthocline ribs along the rostrum. These ribs are variable in shape and size, straight to folded posteriorly, bifurcate ventrally and occasionally postero-dorsally, and cover an area ~45% of the total valve length from the posterior end. The life position of C. magharensis n. gen. n. sp. is reconstructed on the basis of a functional interpretation of its morphology and by comparison with closely related Recent forms. The asymmetrical commarginal ribs facilitated the burrowing process. The posterior oblique ribs are asymmetrical in cross-section with a steeply concave side in the burrowing direction and slightly convex side in the opposite direction. They probably kept the bivalve in a stable position once the desired depth had been reached. The thick oblique ribs probably also increased the strength of the rostrum and offered resistance against durophagous predators, being presumably partly exposed above the sediment-water interface. Based on the associated fauna, Costinuculana n. gen. lived in a low-energy environment characterized by a fine-grained, soft substrate.</abstract><cop>New York, USA</cop><pub>The Paleontological Society</pub><doi>10.1017/jpa.2016.161</doi><tpages>10</tpages></addata></record> |
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subjects | Abbreviations Africa Asymmetry Autecology Autobiographies Bathonian Bifurcations Biostratigraphy Bivalvia Burrowing organisms Carbonates Classification Classification (sedimentation) Coastal environments Collections Corals Costinuculana magharensis Cross-sections Diagnosis Dimensions Ecological succession Egypt Elongation Facies Fauna Fossil animals functional morphology Gebel Maghara Genera Geographical variations Geology Height Invertebrata invertebrate Jurassic Kehailia Formation Limestone Macrofauna Magnesium Marketing Mesozoic Middle Jurassic Mineral resources Mollusca Mollusks Morphology Mountains Mud-water interfaces New genera new taxa North Africa Nuculanidae Orientation Palaeontology Paleobiology Paleoecology Paleontology Photography Physical characteristics Predators Preservation Protobranchia Riblets Rostrum Science Sediment Sediment-water interface Sediments Shells Sinai Egypt Strata Stratigraphy Taxonomy Terminology Valves Zoobenthos Zoology |
title | Costinuculana magharensis n. gen. n. sp. (Bivalvia, Nuculanidae) from the Middle Jurassic of Gebel Maghara, North Sinai, Egypt |
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