Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)

The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whet...
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Autor*in:	Verma, Sanjay K. [verfasserIn] Bajpai, Sunil [verfasserIn] Yadav, Ravi [verfasserIn] Roy, Arindam [verfasserIn] Maurya, Abhayanand S. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs

Übergeordnetes Werk:	Enthalten in: Cretaceous research - London : Academic Press, 1980, 156
Übergeordnetes Werk:	volume:156

DOI / URN:	10.1016/j.cretres.2023.105789

Katalog-ID:	ELV066607264

Internformat


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245	1	0	\|a Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)
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520			\|a The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a).
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700	1		\|a Maurya, Abhayanand S. \|e verfasserin \|4 aut
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allfields	10.1016/j.cretres.2023.105789 doi (DE-627)ELV066607264 (ELSEVIER)S0195-6671(23)00317-8 DE-627 ger DE-627 rda eng 550 VZ 38.16 bkl Verma, Sanjay K. verfasserin aut Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian) 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a). Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs Bajpai, Sunil verfasserin (orcid)0000-0002-2279-445X aut Yadav, Ravi verfasserin aut Roy, Arindam verfasserin aut Maurya, Abhayanand S. verfasserin aut Enthalten in Cretaceous research London : Academic Press, 1980 156 Online-Ressource (DE-627)254909787 (DE-600)1463187-8 (DE-576)259270644 0195-6671 nnns volume:156 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.16 Stratigraphie VZ AR 156
spelling	10.1016/j.cretres.2023.105789 doi (DE-627)ELV066607264 (ELSEVIER)S0195-6671(23)00317-8 DE-627 ger DE-627 rda eng 550 VZ 38.16 bkl Verma, Sanjay K. verfasserin aut Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian) 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a). Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs Bajpai, Sunil verfasserin (orcid)0000-0002-2279-445X aut Yadav, Ravi verfasserin aut Roy, Arindam verfasserin aut Maurya, Abhayanand S. verfasserin aut Enthalten in Cretaceous research London : Academic Press, 1980 156 Online-Ressource (DE-627)254909787 (DE-600)1463187-8 (DE-576)259270644 0195-6671 nnns volume:156 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.16 Stratigraphie VZ AR 156
allfields_unstemmed	10.1016/j.cretres.2023.105789 doi (DE-627)ELV066607264 (ELSEVIER)S0195-6671(23)00317-8 DE-627 ger DE-627 rda eng 550 VZ 38.16 bkl Verma, Sanjay K. verfasserin aut Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian) 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a). Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs Bajpai, Sunil verfasserin (orcid)0000-0002-2279-445X aut Yadav, Ravi verfasserin aut Roy, Arindam verfasserin aut Maurya, Abhayanand S. verfasserin aut Enthalten in Cretaceous research London : Academic Press, 1980 156 Online-Ressource (DE-627)254909787 (DE-600)1463187-8 (DE-576)259270644 0195-6671 nnns volume:156 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.16 Stratigraphie VZ AR 156
allfieldsGer	10.1016/j.cretres.2023.105789 doi (DE-627)ELV066607264 (ELSEVIER)S0195-6671(23)00317-8 DE-627 ger DE-627 rda eng 550 VZ 38.16 bkl Verma, Sanjay K. verfasserin aut Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian) 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a). Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs Bajpai, Sunil verfasserin (orcid)0000-0002-2279-445X aut Yadav, Ravi verfasserin aut Roy, Arindam verfasserin aut Maurya, Abhayanand S. verfasserin aut Enthalten in Cretaceous research London : Academic Press, 1980 156 Online-Ressource (DE-627)254909787 (DE-600)1463187-8 (DE-576)259270644 0195-6671 nnns volume:156 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.16 Stratigraphie VZ AR 156
allfieldsSound	10.1016/j.cretres.2023.105789 doi (DE-627)ELV066607264 (ELSEVIER)S0195-6671(23)00317-8 DE-627 ger DE-627 rda eng 550 VZ 38.16 bkl Verma, Sanjay K. verfasserin aut Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian) 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a). Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs Bajpai, Sunil verfasserin (orcid)0000-0002-2279-445X aut Yadav, Ravi verfasserin aut Roy, Arindam verfasserin aut Maurya, Abhayanand S. verfasserin aut Enthalten in Cretaceous research London : Academic Press, 1980 156 Online-Ressource (DE-627)254909787 (DE-600)1463187-8 (DE-576)259270644 0195-6671 nnns volume:156 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.16 Stratigraphie VZ AR 156
language	English
source	Enthalten in Cretaceous research 156 volume:156
sourceStr	Enthalten in Cretaceous research 156 volume:156
format_phy_str_mv	Article
bklname	Stratigraphie
institution	findex.gbv.de
topic_facet	Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs
dewey-raw	550
isfreeaccess_bool	false
container_title	Cretaceous research
authorswithroles_txt_mv	Verma, Sanjay K. @@aut@@ Bajpai, Sunil @@aut@@ Yadav, Ravi @@aut@@ Roy, Arindam @@aut@@ Maurya, Abhayanand S. @@aut@@
publishDateDaySort_date	2023-01-01T00:00:00Z
hierarchy_top_id	254909787
dewey-sort	3550
id	ELV066607264
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author	Verma, Sanjay K.
spellingShingle	Verma, Sanjay K. ddc 550 bkl 38.16 misc Cretaceous-Paleogene boundary misc Deccan traps misc India misc Marine transgression misc Elasmobranchs Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)
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topic_title	550 VZ 38.16 bkl Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian) Cretaceous-Paleogene boundary Deccan traps India Marine transgression Elasmobranchs
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title	Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)
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title_full	Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)
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title_sort	potential faunal evidence for western epicontinental seaway along the narmada rift in peninsular india during the latest cretaceous (maastrichtian)
title_auth	Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)
abstract	The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a).
abstractGer	The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a).
abstract_unstemmed	The pathways of marine incursions into central India around the Cretaceous-Paleogene (K-Pg) transition are a matter of ongoing debate. While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. The Narmada Seaway extended hundreds of kilometres inland from India's western margin, beginning in the late Cenomanian with the deposition of long known Bagh Beds and continuing intermittently until the early Paleocene (Danian, Zone P1a).
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title_short	Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)
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author2	Bajpai, Sunil Yadav, Ravi Roy, Arindam Maurya, Abhayanand S.
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up_date	2024-07-06T18:21:29.116Z
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While there is a general consensus regarding marine incursions from the southeast coast of India along the Godavari rift, it is still highly controversial as to whether such incursions also took place from the western margin, along the Narmada-Tapti rift. Here we report the first fossil evidence (batoid and pycnodontid fishes) suggesting potential marine influences during the deposition of freshwater Deccan intertrappean sediments (late Cretaceous, Maastrichtian) in the lower Narmada valley of west-central peninsular India. The discovery of several isolated teeth of the stingray genus Igdabatis (I. indicus) along with a pycnodontid tooth in a predominantly freshwater intertrappean section at Mohanpura, district Dhar (Madhya Pradesh state) is significant, especially since living myliobatids are essential inhabitants of coastal marine ecosystems. Similar previously recorded occurrences of Igdabatis and pycnodontids from several other Maastrichtian infra- and intertrappean localities on the eastern and southeastern fringes of the Deccan Volcanic Province have been interpreted as evidence of marine incursions from India's eastern margin along the Godavari rift. The present records from district Dhar tentatively suggest the existence of a nearby epicontinental seaway (the Narmada Seaway) during the Maastrichtian. 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Potential faunal evidence for western epicontinental seaway along the Narmada rift in peninsular India during the latest Cretaceous (Maastrichtian)

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