dc.creatorMurthy, Srikanta
dc.creatorKavali, Pauline Sabina
dc.creatorDi Pasquo Lartigue, Maria
dc.creatorChakraborti, Bhaskar
dc.date.accessioned2019-12-03T23:16:27Z
dc.date.accessioned2022-10-15T09:38:59Z
dc.date.available2019-12-03T23:16:27Z
dc.date.available2022-10-15T09:38:59Z
dc.date.created2019-12-03T23:16:27Z
dc.date.issued2018-10-15
dc.identifierMurthy, Srikanta; Kavali, Pauline Sabina; Di Pasquo Lartigue, Maria; Chakraborti, Bhaskar; Late Pennsylvanian and Early Cisuralian palynofloras from the Rajmahal Basin, eastern India, and their chronological significance; Taylor & Francis Ltd; Historical Biology; 15-10-2018; 1-17
dc.identifier0891-2963
dc.identifierhttp://hdl.handle.net/11336/91300
dc.identifier1029-2381
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4371336
dc.description.abstractThis work documents for the first time a palynological assemblage in the Rajmahal Basin, tentatively considered probable youngest Late Pennsylvanian assemblage, which was hitherto considered early Permian. The palynocomposition consists of 39 species (5 spores, 25 monosaccate, 5 bisaccate- 3 non striate and 2 striate grains, scarce Navifusa sp., scolecodont, algae and fungal hyphae). Two assemblages are described based on the first appearance of taxa, Assemblage I (608.90–599.00 m) dominated by monosaccates and absence of bisaccates and spores. Assemblage II (592.0–590.80 m) also dominated by monosaccates but with the inception of spores, bisaccates and marine palynomorphs. The Assemblage I is correlated to the oldest Potonieisporites neglectus Assemblage Zone of Tiwari and Tripathi based on their similarities and the absence of species recorded in the Assemblage II which is correlated to their overlying Plicatipollenites gondwanensis Assemblage Zone. Palynoassemblages similar to the Assemblage I, radiometrically constrained to the Late Pennsylvanian across Gondwana, along with the lack of diagnostic Permian pollen grains as well as marine Eurydesma fauna and terrestrial glossopterids, tentatively support an older age at least for the lower interval of the Talchir Formation. The latter fossils associated to Assemblage II confirm an early Permian age.
dc.languageeng
dc.publisherTaylor & Francis Ltd
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.tandfonline.com/doi/full/10.1080/08912963.2018.1529763
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1080/08912963.2018.1529763
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectBRAHMANI-BIRBHUM COALFIELD
dc.subjectCARBONIFEROUS-PERMIAN BOUNDARY
dc.subjectGLOBAL CORRELATION
dc.subjectPALYNOSTRATIGRAPHY
dc.subjectRAJMAHAL BASIN
dc.subjectSALBADHRA-GOMARPAHARI REGION
dc.subjectTALCHIR FORMATION
dc.titleLate Pennsylvanian and Early Cisuralian palynofloras from the Rajmahal Basin, eastern India, and their chronological significance
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion


Este ítem pertenece a la siguiente institución