New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India

In western Rajasthan, India, the Jodhpur Sandstone of the Marwar Supergroup has yielded a new Ediacaran fossil assemblage comprising macroscopic well-preserved specimens of Aspidella, Hiemalora, large Ediacaran discs, Tirasiana disciformis, Medusinites asteroides, Anfesta-like Ediacaran body fossils...

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Published in:Estudios Geológicos
Main Author: Parihar, V. S.
Format: Article in Journal/Newspaper
Language:English
Published: Consejo Superior de Investigaciones Científicas 2019
Subjects:
Online Access:http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001
https://doi.org/10.3989/egeol.43590.563
id ftjegeologicos:oai:estudiosgeologicos.revistas.csic.es:article/1001
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institution Open Polar
collection Estudios Geológicos (E-Journal)
op_collection_id ftjegeologicos
language English
topic Jodhpur Sandstone
Soft-bodied metazoans
Mat structures
Ediacaran
Arenisca de Jodhpur
Metazoos de cuerpo blando
Estructuras microbianas
Ediacárico
spellingShingle Jodhpur Sandstone
Soft-bodied metazoans
Mat structures
Ediacaran
Arenisca de Jodhpur
Metazoos de cuerpo blando
Estructuras microbianas
Ediacárico
Parihar, V. S.
New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India
topic_facet Jodhpur Sandstone
Soft-bodied metazoans
Mat structures
Ediacaran
Arenisca de Jodhpur
Metazoos de cuerpo blando
Estructuras microbianas
Ediacárico
description In western Rajasthan, India, the Jodhpur Sandstone of the Marwar Supergroup has yielded a new Ediacaran fossil assemblage comprising macroscopic well-preserved specimens of Aspidella, Hiemalora, large Ediacaran discs, Tirasiana disciformis, Medusinites asteroides, Anfesta-like Ediacaran body fossils and microbial mat structures (Arumberia banksi, Kinneyia mat structures, wrinkle mat structures and other mat structures). The fossil record allows suggesting a broad correlation with the Fermuse Formation, Newfoundland, South Australia, White Sea of Russia and Norway, and regionally correlated with the Bhander Group of Vindhyan Supergroup and Krol Group of Lesser Himalaya. En el oeste de Rajasthan, India, la Arenisca de Jodhpur (Supergrupo de Marwar) ha librado un nuevo conjunto fósil ediacárico que comprende especímenes macroscópicos bien conservados de Aspidella, Hiemalora, grandes discos ediacáricos, Tirasiana disciformis, asteroides de Medusinites, fósiles de cuerpo blando ediacáricos similares a Anfesta y estructuras de tapices microbianas (Arumberia banksi, estructuras microbianas de tipo Kinneyia, estructuras microbianas arrugadas y otras estructuras microbianas). El registro fósil permite sugerir una amplia correlación con la Formación de Fermuse, Terranova, Australia meridional, el Mar Blanco de Rusia y Noruega, y la correlación regional con el Grupo de Bhander (Supergroup de Vindhyan) y el Grupo de Krol del Himalaya Interior.
format Article in Journal/Newspaper
author Parihar, V. S.
author_facet Parihar, V. S.
author_sort Parihar, V. S.
title New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India
title_short New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India
title_full New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India
title_fullStr New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India
title_full_unstemmed New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India
title_sort new record of ediacaran biota from the jodhpur sandstone of marwar supergroup, western rajasthan, india
publisher Consejo Superior de Investigaciones Científicas
publishDate 2019
url http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001
https://doi.org/10.3989/egeol.43590.563
long_lat ENVELOPE(-55.233,-55.233,-61.250,-61.250)
ENVELOPE(-56.866,-56.866,-64.300,-64.300)
ENVELOPE(-12.333,-12.333,-71.333,-71.333)
geographic White Sea
Norway
Blanco
Fósiles
Noruega
geographic_facet White Sea
Norway
Blanco
Fósiles
Noruega
genre Mar Blanco
Newfoundland
Terranova
White Sea
genre_facet Mar Blanco
Newfoundland
Terranova
White Sea
op_source Estudios Geológicos; Vol. 75 No. 2 (2019); e108
Estudios Geológicos; Vol. 75 Núm. 2 (2019); e108
1988-3250
0367-0449
10.3989/egeol.16728
op_relation http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001/1258
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http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001/1260
Billings, E. (1872). On some fossils from the Primordial rocks of Newfoundland. Canadian Naturalist, 6: 465-479. https://doi.org/10.5962/bhl.title.38279
Chauhan, D.S.; Mathur, K.M. & Narayan Ram (2001). Geological nature of the Pokaran boulder Bed: Palaeoenvironment, Palaoclimatic and Stratigraphic Implication. Journal of the Geological Society of India, 58: 425-433.
Chauhan, D.S.; Bhanwara Ram & Narayan Ram (2004). Jodhpur Sandstone: A gift of Ancient Beaches of Western Rajasthan. Geological Society of India, 64: 265-276.
Fedonkin, M.A. (1980). New Precambrian Coelenterata in the north of the Russian platform. Paleontological Journal, 14: 1-10.
Fedonkin, M.A. (1987). The non-skeletal fauna of the Vendian and its place in the evolution of the Metazoa. Trudy Paleontologiceskogo Instituta Akademia Nauk SSSR, 226: 1-174.
Fedonkin, M.A. (1992). Vendian faunas and the early evolution of the Metazoa. In: Origin and Early Evolution of the Metazoa (Lipps, J.H. & Signor, P.W., Eds.). Plenum, New York, 87-129. https://doi.org/10.1007/978-1-4899-2427-8_4
Gehling, J.G. (1999). Microbial mats in Terminal Proterozoic siliciclastic Ediacaran death masks. Palaios, 14: 40-57. https://doi.org/10.2307/3515360
Gehling, J.G.; Narbonne, G.M. & Anderson, M.M. (2000). The first named Ediacaran body fossil, Aspidella terranovica. Palaeontology, 43: 427-456. https://doi.org/10.1111/j.0031-0239.2000.00134.x
Glaessner & Walter, M.R. (1975). New Precambrian fossils from the Arumbera Sandstone, Northern Territory, Australia. Alcheringa, 1: 56-69. https://doi.org/10.1080/03115517508619480
Gregory, L.C.; Meert, J.G.; Bingen, B.H. Pandit, M.K. & Torsvik, T.H. (2009). Paleomagnetic and geochronologic study of Malani Igneous suite, NW India: implications for the configuration of Rodinia and the assembly of Gondwana. Precambrian Research, 170: 13-26. https://doi.org/10.1016/j.precamres.2008.11.004
Hagadorn, J.W.; Fedo, C.M. & Waggoner, B.M. (2000). Early Cambrian Ediacaran-type fossils from California. Journal of Paleontology, 74: 731-740. 2.0.CO;2" target="_blank">https://doi.org/10.1666/0022-3360(2000)074<0731:ECETFF>2.0.CO;2
Kumar, V. & Chandra, R. (2005). Geology and evolution of Nagaur - Ganganagar Basin with special reference to salt and potash mineralization. Geological Survey of India Special Publication, 62: 1-151.
Kumar, S. & Pandey, S.K. (2009). Note on the occurrence of Arumberia and associated fossils from the Jodhpur Sandstone, Marwar Supergroup, Western Rajasthan. Journal Palaeontological Society of India, 54: 171-178.
McCall, G.J.H. (2006). The Vendian (Ediacaran) in the geological record: Enigmas in geology's prelude to the Cambrian explosion. Earth-Science Reviews, 77: 1-229. https://doi.org/10.1016/j.earscirev.2005.08.004
Narayan Ram & Chauhan, D.S. (2007). The Jodhpur sandstone of Bhopalgarh area: Its geological nature and environment of deposition. Emerging trends of research in Geology, NW India (Avadich, P.C. & Bhu, H., Eds.). MLSU, Udaipur (Rajastan), 89-103.
Noffke, N. (2010). Geobiology: Microbial Mats in Sandy Deposit from the Archean Era to Today. Springer Heidelberg.
Noffke, N.; Gerdes, G.; Klenke T. & Krumbein, W.E. (2001). Microbially induced sedimentary structures - a new category within the classification of primary sedimentary structures. Journal of Sedimentary Research, 71: 649-656. https://doi.org/10.1306/2DC4095D-0E47-11D7-8643000102C1865D
Palij, V.M. (1976). Palaeontologiya i Stratigrafiya Verkhnego Kembriya i Nizhnego Paleozoya Yugo-Zapada Vostochno-Evröpeiskoi Platformy. Kiev, Naukova dumka, 63-77.
Pandey, D.K. & Bahadur, T. (2009). A Review of the Stratigraphy of Marwar Supergroup of west- central Rajasthan. Journal Geological Society of India, 73: 747-758. https://doi.org/10.1007/s12594-009-0060-6
Pareek, H.S. (1981). Configuration and sedimentary stratigraphy of western Rajasthan. Journal of the Geological Society of India, 22: 517-523.
Pareek, H.S. (1984). Pre-Quarternary geology and mineral resources of north- western Rajasthan. Memoirs of the Geological Survey of India, 115: 1-99.
Parihar, V.S.; Gaur, V. & Nama, S.L. (2012). Trace fossils and microbial-mat Induced sedimentary structures from the Girbhaker sandstone of Marwar Super group, Bhopalgarh, Jodhpur, Rajasthan, India. Journal of Earth Science and Climate Change, S12: 002. https://doi.org/10.4172/2157-7617.S12-002
Raghav, K.S.; De, C. & Jain, R.L. (2005). The first record of Vendian medusoids and trace fossil bearing algal mat ground from the basal part of the Marwar Supergroup of Rajasthan, India. Indian Minerals, 59: 23-30.
Sarkar, S.; Bose, P.K.; Samantha, P.; Sengupta, P. & Eriksson, P. (2008). Microbial mat mediated structures in the Ediacaran Sonia Sandstone, Rajasthan, India and their implications for Proterozoic sedimentation. Precambrian Research, 162: 248-263. https://doi.org/10.1016/j.precamres.2007.07.019
Sprigg, R.C. (1949). Early Cambrian "jellyfishes" at Ediacara, South Australia and Mount John, Kimberley District, Western Australia. Transactions of the Royal Society of South Australia, 73: 72-99.
Srivastava, P. (2012). Ediacaran discs from the Jodhpur Sandstone, Marwar Supergroup, India: a biological diversification or taphonomic interplay? International Journal of Geosciences, 3: 1120-1126. https://doi.org/10.4236/ijg.2012.35113
Wade, M. (1972). Hydrozoa and Scyphozoa and other medusoides from the Precambrian, Ediacara Fauna, South Australia. Palaeontology, 15: 197-225.
Walcott, C.D. (1916). Cambrian geology and paleontology III, No. 2 - Precambrian Algonkian algal flora. Smithsonian Miscellaneous Collections, 64: 77-156.
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001
doi:10.3989/egeol.43590.563
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spelling ftjegeologicos:oai:estudiosgeologicos.revistas.csic.es:article/1001 2023-05-15T17:10:13+02:00 New Record of Ediacaran Biota from the Jodhpur Sandstone of Marwar Supergroup, western Rajasthan, India Nuevo registro de la biota ediacárica en la Arenisca de Jodhpur (Supergrupo de Marwar), Rajasthan occidental, India Parihar, V. S. 2019-12-30 text/html application/pdf application/xml http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001 https://doi.org/10.3989/egeol.43590.563 eng eng Consejo Superior de Investigaciones Científicas http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001/1258 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001/1259 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001/1260 Billings, E. (1872). On some fossils from the Primordial rocks of Newfoundland. Canadian Naturalist, 6: 465-479. https://doi.org/10.5962/bhl.title.38279 Chauhan, D.S.; Mathur, K.M. & Narayan Ram (2001). Geological nature of the Pokaran boulder Bed: Palaeoenvironment, Palaoclimatic and Stratigraphic Implication. Journal of the Geological Society of India, 58: 425-433. Chauhan, D.S.; Bhanwara Ram & Narayan Ram (2004). Jodhpur Sandstone: A gift of Ancient Beaches of Western Rajasthan. Geological Society of India, 64: 265-276. Fedonkin, M.A. (1980). New Precambrian Coelenterata in the north of the Russian platform. Paleontological Journal, 14: 1-10. Fedonkin, M.A. (1987). The non-skeletal fauna of the Vendian and its place in the evolution of the Metazoa. Trudy Paleontologiceskogo Instituta Akademia Nauk SSSR, 226: 1-174. Fedonkin, M.A. (1992). Vendian faunas and the early evolution of the Metazoa. In: Origin and Early Evolution of the Metazoa (Lipps, J.H. & Signor, P.W., Eds.). Plenum, New York, 87-129. https://doi.org/10.1007/978-1-4899-2427-8_4 Gehling, J.G. (1999). Microbial mats in Terminal Proterozoic siliciclastic Ediacaran death masks. Palaios, 14: 40-57. https://doi.org/10.2307/3515360 Gehling, J.G.; Narbonne, G.M. & Anderson, M.M. (2000). The first named Ediacaran body fossil, Aspidella terranovica. Palaeontology, 43: 427-456. https://doi.org/10.1111/j.0031-0239.2000.00134.x Glaessner & Walter, M.R. (1975). New Precambrian fossils from the Arumbera Sandstone, Northern Territory, Australia. Alcheringa, 1: 56-69. https://doi.org/10.1080/03115517508619480 Gregory, L.C.; Meert, J.G.; Bingen, B.H. Pandit, M.K. & Torsvik, T.H. (2009). Paleomagnetic and geochronologic study of Malani Igneous suite, NW India: implications for the configuration of Rodinia and the assembly of Gondwana. Precambrian Research, 170: 13-26. https://doi.org/10.1016/j.precamres.2008.11.004 Hagadorn, J.W.; Fedo, C.M. & Waggoner, B.M. (2000). Early Cambrian Ediacaran-type fossils from California. Journal of Paleontology, 74: 731-740. 2.0.CO;2" target="_blank">https://doi.org/10.1666/0022-3360(2000)074<0731:ECETFF>2.0.CO;2 Kumar, V. & Chandra, R. (2005). Geology and evolution of Nagaur - Ganganagar Basin with special reference to salt and potash mineralization. Geological Survey of India Special Publication, 62: 1-151. Kumar, S. & Pandey, S.K. (2009). Note on the occurrence of Arumberia and associated fossils from the Jodhpur Sandstone, Marwar Supergroup, Western Rajasthan. Journal Palaeontological Society of India, 54: 171-178. McCall, G.J.H. (2006). The Vendian (Ediacaran) in the geological record: Enigmas in geology's prelude to the Cambrian explosion. Earth-Science Reviews, 77: 1-229. https://doi.org/10.1016/j.earscirev.2005.08.004 Narayan Ram & Chauhan, D.S. (2007). The Jodhpur sandstone of Bhopalgarh area: Its geological nature and environment of deposition. Emerging trends of research in Geology, NW India (Avadich, P.C. & Bhu, H., Eds.). MLSU, Udaipur (Rajastan), 89-103. Noffke, N. (2010). Geobiology: Microbial Mats in Sandy Deposit from the Archean Era to Today. Springer Heidelberg. Noffke, N.; Gerdes, G.; Klenke T. & Krumbein, W.E. (2001). Microbially induced sedimentary structures - a new category within the classification of primary sedimentary structures. Journal of Sedimentary Research, 71: 649-656. https://doi.org/10.1306/2DC4095D-0E47-11D7-8643000102C1865D Palij, V.M. (1976). Palaeontologiya i Stratigrafiya Verkhnego Kembriya i Nizhnego Paleozoya Yugo-Zapada Vostochno-Evröpeiskoi Platformy. Kiev, Naukova dumka, 63-77. Pandey, D.K. & Bahadur, T. (2009). A Review of the Stratigraphy of Marwar Supergroup of west- central Rajasthan. Journal Geological Society of India, 73: 747-758. https://doi.org/10.1007/s12594-009-0060-6 Pareek, H.S. (1981). Configuration and sedimentary stratigraphy of western Rajasthan. Journal of the Geological Society of India, 22: 517-523. Pareek, H.S. (1984). Pre-Quarternary geology and mineral resources of north- western Rajasthan. Memoirs of the Geological Survey of India, 115: 1-99. Parihar, V.S.; Gaur, V. & Nama, S.L. (2012). Trace fossils and microbial-mat Induced sedimentary structures from the Girbhaker sandstone of Marwar Super group, Bhopalgarh, Jodhpur, Rajasthan, India. Journal of Earth Science and Climate Change, S12: 002. https://doi.org/10.4172/2157-7617.S12-002 Raghav, K.S.; De, C. & Jain, R.L. (2005). The first record of Vendian medusoids and trace fossil bearing algal mat ground from the basal part of the Marwar Supergroup of Rajasthan, India. Indian Minerals, 59: 23-30. Sarkar, S.; Bose, P.K.; Samantha, P.; Sengupta, P. & Eriksson, P. (2008). Microbial mat mediated structures in the Ediacaran Sonia Sandstone, Rajasthan, India and their implications for Proterozoic sedimentation. Precambrian Research, 162: 248-263. https://doi.org/10.1016/j.precamres.2007.07.019 Sprigg, R.C. (1949). Early Cambrian "jellyfishes" at Ediacara, South Australia and Mount John, Kimberley District, Western Australia. Transactions of the Royal Society of South Australia, 73: 72-99. Srivastava, P. (2012). Ediacaran discs from the Jodhpur Sandstone, Marwar Supergroup, India: a biological diversification or taphonomic interplay? International Journal of Geosciences, 3: 1120-1126. https://doi.org/10.4236/ijg.2012.35113 Wade, M. (1972). Hydrozoa and Scyphozoa and other medusoides from the Precambrian, Ediacara Fauna, South Australia. Palaeontology, 15: 197-225. Walcott, C.D. (1916). Cambrian geology and paleontology III, No. 2 - Precambrian Algonkian algal flora. Smithsonian Miscellaneous Collections, 64: 77-156. http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/1001 doi:10.3989/egeol.43590.563 Derechos de autor 2019 Consejo Superior de Investigaciones Científicas (CSIC) https://creativecommons.org/licenses/by/4.0 CC-BY Estudios Geológicos; Vol. 75 No. 2 (2019); e108 Estudios Geológicos; Vol. 75 Núm. 2 (2019); e108 1988-3250 0367-0449 10.3989/egeol.16728 Jodhpur Sandstone Soft-bodied metazoans Mat structures Ediacaran Arenisca de Jodhpur Metazoos de cuerpo blando Estructuras microbianas Ediacárico info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed article Artículo revisado por pares 2019 ftjegeologicos https://doi.org/10.3989/egeol.43590.563 https://doi.org/10.3989/egeol.16728 https://doi.org/10.5962/bhl.title.38279 https://doi.org/10.2307/3515360 https://doi.org/10.1016/j.earscirev.2005.08.004 2020-12-13T10:08:29Z In western Rajasthan, India, the Jodhpur Sandstone of the Marwar Supergroup has yielded a new Ediacaran fossil assemblage comprising macroscopic well-preserved specimens of Aspidella, Hiemalora, large Ediacaran discs, Tirasiana disciformis, Medusinites asteroides, Anfesta-like Ediacaran body fossils and microbial mat structures (Arumberia banksi, Kinneyia mat structures, wrinkle mat structures and other mat structures). The fossil record allows suggesting a broad correlation with the Fermuse Formation, Newfoundland, South Australia, White Sea of Russia and Norway, and regionally correlated with the Bhander Group of Vindhyan Supergroup and Krol Group of Lesser Himalaya. En el oeste de Rajasthan, India, la Arenisca de Jodhpur (Supergrupo de Marwar) ha librado un nuevo conjunto fósil ediacárico que comprende especímenes macroscópicos bien conservados de Aspidella, Hiemalora, grandes discos ediacáricos, Tirasiana disciformis, asteroides de Medusinites, fósiles de cuerpo blando ediacáricos similares a Anfesta y estructuras de tapices microbianas (Arumberia banksi, estructuras microbianas de tipo Kinneyia, estructuras microbianas arrugadas y otras estructuras microbianas). El registro fósil permite sugerir una amplia correlación con la Formación de Fermuse, Terranova, Australia meridional, el Mar Blanco de Rusia y Noruega, y la correlación regional con el Grupo de Bhander (Supergroup de Vindhyan) y el Grupo de Krol del Himalaya Interior. Article in Journal/Newspaper Mar Blanco Newfoundland Terranova White Sea Estudios Geológicos (E-Journal) White Sea Norway Blanco ENVELOPE(-55.233,-55.233,-61.250,-61.250) Fósiles ENVELOPE(-56.866,-56.866,-64.300,-64.300) Noruega ENVELOPE(-12.333,-12.333,-71.333,-71.333) Estudios Geológicos 75 2 108