RECORD OF TITHOPELTOCERAS ARKELL (AMMONOIDEA) FROM THE LATE TITHONIAN OF KUTCH, INDIA: ITS STRATIGRAPHIC AND PALEOBIOGEOGRAPHIC SIGNIFICANCE
Jurassic-Cretaceous sedimentation in Kutch took place on an epicontinental platform which experienced many transgressive-regressive phases and became progressively shallow (Biswas, 1991). As a result, marine fossils, like ammonites and other stenohaline groups, are not ubiquitous and uniformly distr...
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| description | Jurassic-Cretaceous sedimentation in Kutch took place on an epicontinental platform which experienced many transgressive-regressive phases and became progressively shallow (Biswas, 1991). As a result, marine fossils, like ammonites and other stenohaline groups, are not ubiquitous and uniformly distributed throughout the succession. From the Late Jurassic the Kutch basin witnessed major sea-level fluctuations and during the Tithonian the effects of transgressive-regressive couplets were more frequently registered. The record of ammonites in many areas, especially in the Indo–Madagascar Faunal Province, including Kutch (personal observation), are mainly associated with the transgressive events (Riccardi, 1991 and references therein). In Kutch, the spatiotemporal distribution of the ammonite-bearing beds is discrete in nature and these are not always regionally persistent. Many previous works based on the study of museum collections (e.g., Spath, 1927–1933) were plagued with stratigraphic imprecision and inadequate knowledge of the ammonite-rich localities, and generally lacked accurate lithologic description of any section. This led to poor resolution of the regional biostratigraphy based on Tithonian ammonites. |
| doi_str_mv | 10.1666/0022-3360(2005)079<0619:ROTAAF>2.0.CO;2 |
| format | Article |
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As a result, marine fossils, like ammonites and other stenohaline groups, are not ubiquitous and uniformly distributed throughout the succession. From the Late Jurassic the Kutch basin witnessed major sea-level fluctuations and during the Tithonian the effects of transgressive-regressive couplets were more frequently registered. The record of ammonites in many areas, especially in the Indo–Madagascar Faunal Province, including Kutch (personal observation), are mainly associated with the transgressive events (Riccardi, 1991 and references therein). In Kutch, the spatiotemporal distribution of the ammonite-bearing beds is discrete in nature and these are not always regionally persistent. Many previous works based on the study of museum collections (e.g., Spath, 1927–1933) were plagued with stratigraphic imprecision and inadequate knowledge of the ammonite-rich localities, and generally lacked accurate lithologic description of any section. This led to poor resolution of the regional biostratigraphy based on Tithonian ammonites.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><identifier>DOI: 10.1666/0022-3360(2005)079<0619:ROTAAF>2.0.CO;2</identifier><identifier>CODEN: JPALAZ</identifier><language>eng</language><publisher>New York, USA: Cambridge University Press</publisher><subject>Ammonoidea ; Asia ; Berriasellidae ; Bhuj Formation ; biogeography ; biostratigraphy ; Cephalopoda ; Endemic species ; Fauna ; Fossils ; Genera ; Geology ; Gujarat India ; India ; Indian Peninsula ; Invertebrata ; invertebrate ; Jurassic ; Kutch India ; Lakhapar India ; Late Jurassic epoch ; Mesozoic ; Mollusca ; Mollusks ; morphology ; new taxa ; Paleoecology ; paleogeography ; PALEONTOLOGICAL NOTES ; Paleontology ; Portlandian ; Stratigraphy ; taxonomy ; Tetrabranchiata ; Tithonian ; Tithonian age ; Tithopeltoceras ; Tithopeltoceras lakhaparensis ; Umia Member ; Upper Jurassic</subject><ispartof>Journal of paleontology, 2005-05, Vol.79 (3), p.619-624</ispartof><rights>The Paleontological Society</rights><rights>Copyright © The Paleontological Society</rights><rights>GeoRef, Copyright 2020, American Geosciences Institute.</rights><rights>Copyright 2005 The Paleontological Society</rights><rights>Copyright Paleontological Society May 2005</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a485t-e4bf7ff8f51d9dea93df803fb5e8de4637d20bee936136fcfce8a5bc49e20f4e3</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(2005)079<0619:ROTAAF>2.0.CO;2$$EPDF$$P50$$Gbioone$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/4095031$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,26977,27923,27924,52362,58016,58249</link.rule.ids></links><search><creatorcontrib>SHOME, SABYASACHI</creatorcontrib><creatorcontrib>BARDHAN, SUBHENDU</creatorcontrib><creatorcontrib>DE, SOMA</creatorcontrib><title>RECORD OF TITHOPELTOCERAS ARKELL (AMMONOIDEA) FROM THE LATE TITHONIAN OF KUTCH, INDIA: ITS STRATIGRAPHIC AND PALEOBIOGEOGRAPHIC SIGNIFICANCE</title><title>Journal of paleontology</title><addtitle>J. Paleontol</addtitle><description>Jurassic-Cretaceous sedimentation in Kutch took place on an epicontinental platform which experienced many transgressive-regressive phases and became progressively shallow (Biswas, 1991). As a result, marine fossils, like ammonites and other stenohaline groups, are not ubiquitous and uniformly distributed throughout the succession. From the Late Jurassic the Kutch basin witnessed major sea-level fluctuations and during the Tithonian the effects of transgressive-regressive couplets were more frequently registered. The record of ammonites in many areas, especially in the Indo–Madagascar Faunal Province, including Kutch (personal observation), are mainly associated with the transgressive events (Riccardi, 1991 and references therein). In Kutch, the spatiotemporal distribution of the ammonite-bearing beds is discrete in nature and these are not always regionally persistent. Many previous works based on the study of museum collections (e.g., Spath, 1927–1933) were plagued with stratigraphic imprecision and inadequate knowledge of the ammonite-rich localities, and generally lacked accurate lithologic description of any section. This led to poor resolution of the regional biostratigraphy based on Tithonian ammonites.</description><subject>Ammonoidea</subject><subject>Asia</subject><subject>Berriasellidae</subject><subject>Bhuj Formation</subject><subject>biogeography</subject><subject>biostratigraphy</subject><subject>Cephalopoda</subject><subject>Endemic species</subject><subject>Fauna</subject><subject>Fossils</subject><subject>Genera</subject><subject>Geology</subject><subject>Gujarat India</subject><subject>India</subject><subject>Indian Peninsula</subject><subject>Invertebrata</subject><subject>invertebrate</subject><subject>Jurassic</subject><subject>Kutch India</subject><subject>Lakhapar India</subject><subject>Late Jurassic epoch</subject><subject>Mesozoic</subject><subject>Mollusca</subject><subject>Mollusks</subject><subject>morphology</subject><subject>new taxa</subject><subject>Paleoecology</subject><subject>paleogeography</subject><subject>PALEONTOLOGICAL NOTES</subject><subject>Paleontology</subject><subject>Portlandian</subject><subject>Stratigraphy</subject><subject>taxonomy</subject><subject>Tetrabranchiata</subject><subject>Tithonian</subject><subject>Tithonian age</subject><subject>Tithopeltoceras</subject><subject>Tithopeltoceras lakhaparensis</subject><subject>Umia Member</subject><subject>Upper Jurassic</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</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>eNqdkc2O0zAUhSMEEqXwBiwsFmhGkI5_EicZEJJJndSaNK7SzNrKjz1K1TZD0grxDjw0CRkGxA5Wlny_c3x8j2VdIbhAlNIrCDG2CaHwAkPoXkIv-AgpCq4zmTMWfcILuAjlB_zEmqGAeDYmxHtqzR5Vz60Xfb-DEGGK0Mz6nvFQZksgI5CLfCU3PMllyDO2BSy74UkCLth6LVMplpxdgiiTa5CvOEhYzidFKlg6ym9u83D1Hoh0Kdg1EPkWbPOM5SLO2GYlQsDSJdiwhMvPQsZc_rreijgVkQhZGvKX1jNT7Hv96uGcW7cRH1ztRMYDkdiF47snWzul8YzxjYvqoNZFQGrjQ2JKV_u1dijxagxLrQNCEaGmMpX2C7esnEBjaBxN5tbbyfe-a7-cdX9Sh6av9H5fHHV77hXyHOL6bjCAb_4Cd-25Ow7ZFCYIUuy7cIDiCaq6tu87bdR91xyK7ptCUI2VqXH5aly-GitTQ2VqrExNlSmsoArl4Di3Xk9Ou_7Udo82DgyGZ9AwfjeN73TbV40-Vvpr2-3rP0L9tCcUB-5Ai4dYxaHsmvpO_-b-PRifvMqmbY_6vz_4A3PGxFI</recordid><startdate>20050501</startdate><enddate>20050501</enddate><creator>SHOME, SABYASACHI</creator><creator>BARDHAN, SUBHENDU</creator><creator>DE, SOMA</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>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><scope>H96</scope></search><sort><creationdate>20050501</creationdate><title>RECORD OF TITHOPELTOCERAS ARKELL (AMMONOIDEA) FROM THE LATE TITHONIAN OF KUTCH, INDIA: ITS STRATIGRAPHIC AND PALEOBIOGEOGRAPHIC SIGNIFICANCE</title><author>SHOME, SABYASACHI ; 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Paleontol</addtitle><date>2005-05-01</date><risdate>2005</risdate><volume>79</volume><issue>3</issue><spage>619</spage><epage>624</epage><pages>619-624</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><coden>JPALAZ</coden><abstract>Jurassic-Cretaceous sedimentation in Kutch took place on an epicontinental platform which experienced many transgressive-regressive phases and became progressively shallow (Biswas, 1991). As a result, marine fossils, like ammonites and other stenohaline groups, are not ubiquitous and uniformly distributed throughout the succession. From the Late Jurassic the Kutch basin witnessed major sea-level fluctuations and during the Tithonian the effects of transgressive-regressive couplets were more frequently registered. The record of ammonites in many areas, especially in the Indo–Madagascar Faunal Province, including Kutch (personal observation), are mainly associated with the transgressive events (Riccardi, 1991 and references therein). In Kutch, the spatiotemporal distribution of the ammonite-bearing beds is discrete in nature and these are not always regionally persistent. Many previous works based on the study of museum collections (e.g., Spath, 1927–1933) were plagued with stratigraphic imprecision and inadequate knowledge of the ammonite-rich localities, and generally lacked accurate lithologic description of any section. This led to poor resolution of the regional biostratigraphy based on Tithonian ammonites.</abstract><cop>New York, USA</cop><pub>Cambridge University Press</pub><doi>10.1666/0022-3360(2005)079<0619:ROTAAF>2.0.CO;2</doi><tpages>6</tpages></addata></record> |
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| ispartof | Journal of paleontology, 2005-05, Vol.79 (3), p.619-624 |
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| subjects | Ammonoidea Asia Berriasellidae Bhuj Formation biogeography biostratigraphy Cephalopoda Endemic species Fauna Fossils Genera Geology Gujarat India India Indian Peninsula Invertebrata invertebrate Jurassic Kutch India Lakhapar India Late Jurassic epoch Mesozoic Mollusca Mollusks morphology new taxa Paleoecology paleogeography PALEONTOLOGICAL NOTES Paleontology Portlandian Stratigraphy taxonomy Tetrabranchiata Tithonian Tithonian age Tithopeltoceras Tithopeltoceras lakhaparensis Umia Member Upper Jurassic |
| title | RECORD OF TITHOPELTOCERAS ARKELL (AMMONOIDEA) FROM THE LATE TITHONIAN OF KUTCH, INDIA: ITS STRATIGRAPHIC AND PALEOBIOGEOGRAPHIC SIGNIFICANCE |
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