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Chakraborty, Abhijit
- Fossil Polyplacophora (Mollusca) from Upper Talchir Sediments of Dudhi Nala, Hazaribagh, Bihar
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Affiliations
1 Department of Geology, Presidency College, 86/1 College Street, Calcutta-700 073, IN
2 Departtnent of Geology, Jogamaya Devi College, Calcutta-700 026, IN
1 Department of Geology, Presidency College, 86/1 College Street, Calcutta-700 073, IN
2 Departtnent of Geology, Jogamaya Devi College, Calcutta-700 026, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 54, No 5 (1999), Pagination: 523-527Abstract
External casts comparable with Polyplacophora (Mollusca), collected from the sand/silt-mud alternation facies (turbidite) of upper Talchir sediments of Dudhi Nala, West Bokaro basin, Hazaribagh district, Bihar are described and illustrated here for the first time. These sediments were reported to be unfossiliferous. Polyplacophoran morphology of the fossils indicate a marine link of the West Bokaro basin during the upper Talchir times. Dudhi Nala area is presently considered to be yet another locality proximal to the eastern limit of the Lower Permian marine incursion in the Indian peninsula along the Raniganj-Daltonganj-Manendragarh-Umaria belt.Keywords
Palaeontology, Polyplacophora, Lower Permian, Talchir Sediments, Gondwana, Bihar.- Crustacean Burrow Fills as Obstacles for Current Crescents in Permo-Carboniferous Talchir formation, Raniganj Basin, Eastern India
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Authors
Affiliations
1 Department of Geology, Presidency College, 86/1, College Street, Kolkata - 700 073, IN
2 Departmenotf Geology, Jogamaya Devi College, 92, S. P. Mukherjee Road, Kolkata -700026, IN
1 Department of Geology, Presidency College, 86/1, College Street, Kolkata - 700 073, IN
2 Departmenotf Geology, Jogamaya Devi College, 92, S. P. Mukherjee Road, Kolkata -700026, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 69, No 6 (2007), Pagination: 1267-1270Abstract
Current crescents genetically linked to exposed heads of the passively filled mud-lined tunneled crustacean burrows on the sandy substrate are being reported from the upper shelf sediments of glacio-marine Talchir Formation (Permo-Carboniferous), Raniganj Basin, Eastern India. Such burrow-linked current crescents may be used as a tool for the identification of sedimentary environment and its energy condition.Keywords
Current crescents, Crustacean burrows, Storm sediments, Talchir Formation, Raniganj Basin.- Early Permian Xiphosurid Trackways from India
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Authors
Affiliations
1 Department of Geology, Jogamaya Devi College, 96 S. P. Mukherjee Road, Kolkata - 700 026, IN
2 Department of Geology and Centre of Advance Studies in Precambrian Geology, Presidency University, 86/1 College Street, Kolkata - 700 073, IN
1 Department of Geology, Jogamaya Devi College, 96 S. P. Mukherjee Road, Kolkata - 700 026, IN
2 Department of Geology and Centre of Advance Studies in Precambrian Geology, Presidency University, 86/1 College Street, Kolkata - 700 073, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 80, No 1 (2012), Pagination: 129-135Abstract
Present work is the first report of Early Permian xiphosurid trackways from India. Surface trackways and undertracks, preserved within ice-marginal storm-affected, shoreface sediments of the Talchir Formation, Jayanti coalbasin closely resemble Kouphichnium Nopsca 1923. Trackways reveal distinct heteropody with foliate pusher impressions, paired series of semi-circular, oval, V- or Y-shaped chilate (walking) leg impressions. Varied ventral impressions also include telson drag marks and telson dents; spine drag marks, book-gills impression, genal gouges as well as symmetric, paired lateral genal furrows, partial cubichnial impressions of prosoma and spinose opisthosoma. A tentative early Permian age (Asselian/Sakmarian) and marginal marine facies association points towards a paleolimuloidae affinity for the trace makers, which is in conformity with their inferred widths of exoskeleton, sub-rounded prosoma and subtriangular spinose opisthosoma with predictable movable spines. Flexed pusher impressions and co-dominant pincer impressions as well as, other ventral impressions in abundance, confirm crawling as their dominant mode of locomotion. Inferred presence of juvenile crawlers in the community suggests a probable shoreline or marginal marine ecospace.Keywords
Trackways, Xiphosura, Kouphichnium, Permian, Marginal Marine.References
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