GNATHOSTOME MICROREMAINS FROM THE LOWER DEVONIAN JAWF FORMATION, SAUDI ARABIA
Calcareous horizons in the Qasr and Hammamiyat members (Lower Devonian, ?Pragian and lower Emsian) of the Jawf Formation, northwestern Saudi Arabia, yielded a rich assemblage of microremains from acanthodian, placoderm, chondrichthyan, and sarcopterygian vertebrates. The most abundant elements are s...
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| Veröffentlicht in: | Journal of paleontology 2006-05, Vol.80 (3), p.537-560 |
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| creator | BURROW, CAROLE J LELIÈVRE, HERVÉ JANJOU, DOMINIQUE |
| description | Calcareous horizons in the Qasr and Hammamiyat members (Lower Devonian, ?Pragian and lower Emsian) of the Jawf Formation, northwestern Saudi Arabia, yielded a rich assemblage of microremains from acanthodian, placoderm, chondrichthyan, and sarcopterygian vertebrates. The most abundant elements are scales from acanthodians Nostolepis spp., Milesacanthus ancestralis n. sp., Canadalepis? sp., and Gomphonchus? fromensis, scales and dermal bone fragments from acanthothoracid and ?rhenanid placoderms, and teeth from onychodontids. Rarer occurrences include ?chondrichthyan scales of several different morphotypes, and petalichthid and ?ptyctodontid placoderm elements. The Qasr Member assemblage shows a close resemblance to slightly older faunas from the Lochkovian of Brittany and Spain. The Hammamiyat Member microvertebrate fauna shows closest affinity with that of the stratigraphically lower Qasr Member, with similarities also to coeval faunas from southeastern Australia, late Emsian/Eifelian faunas from west-central Europe, and the Givetian Aztec Siltstone fauna from Antarctica. |
| doi_str_mv | 10.1666/0022-3360(2006)80[537:GMFTLD]2.0.CO;2 |
| format | Article |
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The most abundant elements are scales from acanthodians Nostolepis spp., Milesacanthus ancestralis n. sp., Canadalepis? sp., and Gomphonchus? fromensis, scales and dermal bone fragments from acanthothoracid and ?rhenanid placoderms, and teeth from onychodontids. Rarer occurrences include ?chondrichthyan scales of several different morphotypes, and petalichthid and ?ptyctodontid placoderm elements. The Qasr Member assemblage shows a close resemblance to slightly older faunas from the Lochkovian of Brittany and Spain. The Hammamiyat Member microvertebrate fauna shows closest affinity with that of the stratigraphically lower Qasr Member, with similarities also to coeval faunas from southeastern Australia, late Emsian/Eifelian faunas from west-central Europe, and the Givetian Aztec Siltstone fauna from Antarctica.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><identifier>DOI: 10.1666/0022-3360(2006)80[537:GMFTLD]2.0.CO;2</identifier><identifier>CODEN: JPALAZ</identifier><language>eng</language><publisher>New York, USA: Cambridge University Press</publisher><subject>Acanthodii ; Al Qalibah Quadrangle ; Arabian Peninsula ; Asia ; Bones ; Canals ; Chondrichthyes ; Chordata ; Crown rump length ; Devonian ; Diplacanthidae ; Earth Sciences ; Emsian age ; Fauna ; faunal list ; faunal studies ; Fish scales ; Fossils ; Geology ; Gomphonchus ; Hammamiyat Member ; Histology ; Jawf Formation ; lithostratigraphy ; Lower Devonian ; Milesacanthus ancestralis ; morphology ; new taxa ; Osteichthyes ; Paleontology ; Paleozoic ; Pisces ; Placodermi ; Qasr Member ; Sarcopterygii ; Saudi Arabia ; Sciences of the Universe ; Taxonomy ; Teeth ; Vertebrata ; vertebrate ; Vertebrates</subject><ispartof>Journal of paleontology, 2006-05, Vol.80 (3), p.537-560</ispartof><rights>The Paleontological Society</rights><rights>Copyright © 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><rights>Copyright 2006 The Paleontological Society</rights><rights>Copyright Paleontological Society May 2006</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a581t-67f7a27349329076462c2d3d44c0277da0fbaa67222993c4321ceab910ad64e83</citedby><cites>FETCH-LOGICAL-a581t-67f7a27349329076462c2d3d44c0277da0fbaa67222993c4321ceab910ad64e83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://bioone.org/doi/pdf/10.1666/0022-3360(2006)80[537:GMFTLD]2.0.CO;2$$EPDF$$P50$$Gbioone$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/4095150$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,780,784,803,885,26978,27924,27925,52363,58017,58250</link.rule.ids><backlink>$$Uhttps://hal.science/hal-00162872$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>BURROW, CAROLE J</creatorcontrib><creatorcontrib>LELIÈVRE, HERVÉ</creatorcontrib><creatorcontrib>JANJOU, DOMINIQUE</creatorcontrib><title>GNATHOSTOME MICROREMAINS FROM THE LOWER DEVONIAN JAWF FORMATION, SAUDI ARABIA</title><title>Journal of paleontology</title><addtitle>J. Paleontol</addtitle><description>Calcareous horizons in the Qasr and Hammamiyat members (Lower Devonian, ?Pragian and lower Emsian) of the Jawf Formation, northwestern Saudi Arabia, yielded a rich assemblage of microremains from acanthodian, placoderm, chondrichthyan, and sarcopterygian vertebrates. The most abundant elements are scales from acanthodians Nostolepis spp., Milesacanthus ancestralis n. sp., Canadalepis? sp., and Gomphonchus? fromensis, scales and dermal bone fragments from acanthothoracid and ?rhenanid placoderms, and teeth from onychodontids. Rarer occurrences include ?chondrichthyan scales of several different morphotypes, and petalichthid and ?ptyctodontid placoderm elements. The Qasr Member assemblage shows a close resemblance to slightly older faunas from the Lochkovian of Brittany and Spain. The Hammamiyat Member microvertebrate fauna shows closest affinity with that of the stratigraphically lower Qasr Member, with similarities also to coeval faunas from southeastern Australia, late Emsian/Eifelian faunas from west-central Europe, and the Givetian Aztec Siltstone fauna from Antarctica.</description><subject>Acanthodii</subject><subject>Al Qalibah Quadrangle</subject><subject>Arabian Peninsula</subject><subject>Asia</subject><subject>Bones</subject><subject>Canals</subject><subject>Chondrichthyes</subject><subject>Chordata</subject><subject>Crown rump length</subject><subject>Devonian</subject><subject>Diplacanthidae</subject><subject>Earth Sciences</subject><subject>Emsian age</subject><subject>Fauna</subject><subject>faunal list</subject><subject>faunal studies</subject><subject>Fish scales</subject><subject>Fossils</subject><subject>Geology</subject><subject>Gomphonchus</subject><subject>Hammamiyat Member</subject><subject>Histology</subject><subject>Jawf Formation</subject><subject>lithostratigraphy</subject><subject>Lower Devonian</subject><subject>Milesacanthus ancestralis</subject><subject>morphology</subject><subject>new taxa</subject><subject>Osteichthyes</subject><subject>Paleontology</subject><subject>Paleozoic</subject><subject>Pisces</subject><subject>Placodermi</subject><subject>Qasr Member</subject><subject>Sarcopterygii</subject><subject>Saudi Arabia</subject><subject>Sciences of the Universe</subject><subject>Taxonomy</subject><subject>Teeth</subject><subject>Vertebrata</subject><subject>vertebrate</subject><subject>Vertebrates</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</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>eNqdkVGvk0AQhYnRxFr9Bz4QH4w3Sp2dpbugTyuFFlPYhHK9D8ZstrC90tByhVbjvxfCTTW-6dMmO9-cOTPHshwCM8IYewuA6FDK4BUCsCsPPs8pf7dMony9-IIzmAXyPT6wJsSn3EFK-UNrcul5bD3puj0AQUbIxEqWqchXcpPLJLSTOMhkFiYiTjd2lMnEzlehvZY3YWYvwk8yjUVqfxQ3kR3JLBF5LNM39kZcL2JbZOJDLJ5aj3a67syz-3dqXUdhHqyctVzGgVg7eu6Rk8P4jmvk1PUp-sCZy7DAkpauWwByXmrYbbVmHBF9nxYuRVIYvfUJ6JK5xqNT62rU_aprdddWB93-VI2u1Eqs1fDX78fQ4_id9OzLkb1rm29n053UoeoKU9f6aJpzpwhH7nowgC_-AvfNuT32eyikBJiH7jA5HKGibbquNbvLeAJqSEcNl1bDpdWQjvJA9emoMR2FClQge72p9XzU2Xenpr2IuODPyRz68uuxfGuarqjMsTA_mrYu_7A0iAMjc8Z6enlvSh-2bVXemt_cv9oKRqVt1TRH85_L_QIFn704</recordid><startdate>20060501</startdate><enddate>20060501</enddate><creator>BURROW, CAROLE J</creator><creator>LELIÈVRE, HERVÉ</creator><creator>JANJOU, DOMINIQUE</creator><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><scope>H96</scope><scope>1XC</scope></search><sort><creationdate>20060501</creationdate><title>GNATHOSTOME MICROREMAINS FROM THE LOWER DEVONIAN JAWF FORMATION, SAUDI ARABIA</title><author>BURROW, CAROLE J ; 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Paleontol</addtitle><date>2006-05-01</date><risdate>2006</risdate><volume>80</volume><issue>3</issue><spage>537</spage><epage>560</epage><pages>537-560</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><coden>JPALAZ</coden><abstract>Calcareous horizons in the Qasr and Hammamiyat members (Lower Devonian, ?Pragian and lower Emsian) of the Jawf Formation, northwestern Saudi Arabia, yielded a rich assemblage of microremains from acanthodian, placoderm, chondrichthyan, and sarcopterygian vertebrates. The most abundant elements are scales from acanthodians Nostolepis spp., Milesacanthus ancestralis n. sp., Canadalepis? sp., and Gomphonchus? fromensis, scales and dermal bone fragments from acanthothoracid and ?rhenanid placoderms, and teeth from onychodontids. Rarer occurrences include ?chondrichthyan scales of several different morphotypes, and petalichthid and ?ptyctodontid placoderm elements. The Qasr Member assemblage shows a close resemblance to slightly older faunas from the Lochkovian of Brittany and Spain. The Hammamiyat Member microvertebrate fauna shows closest affinity with that of the stratigraphically lower Qasr Member, with similarities also to coeval faunas from southeastern Australia, late Emsian/Eifelian faunas from west-central Europe, and the Givetian Aztec Siltstone fauna from Antarctica.</abstract><cop>New York, USA</cop><pub>Cambridge University Press</pub><doi>10.1666/0022-3360(2006)80[537:GMFTLD]2.0.CO;2</doi><tpages>24</tpages></addata></record> |
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| ispartof | Journal of paleontology, 2006-05, Vol.80 (3), p.537-560 |
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| subjects | Acanthodii Al Qalibah Quadrangle Arabian Peninsula Asia Bones Canals Chondrichthyes Chordata Crown rump length Devonian Diplacanthidae Earth Sciences Emsian age Fauna faunal list faunal studies Fish scales Fossils Geology Gomphonchus Hammamiyat Member Histology Jawf Formation lithostratigraphy Lower Devonian Milesacanthus ancestralis morphology new taxa Osteichthyes Paleontology Paleozoic Pisces Placodermi Qasr Member Sarcopterygii Saudi Arabia Sciences of the Universe Taxonomy Teeth Vertebrata vertebrate Vertebrates |
| title | GNATHOSTOME MICROREMAINS FROM THE LOWER DEVONIAN JAWF FORMATION, SAUDI ARABIA |
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