georefid:1998-039842SEDIS Publication Catalogue
ana.macario@awi.de
http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=1998-039842<gco:CharacterString>Isotopic evidence of a rapid cooling and continuous sedimentation across the Eocene-Oligocene boundary of Wagapadhar and Waior, Kutch</gco:CharacterString>1998-01-01publicationgeorefid:1998-039842Sarangi, S.Indian School of Mines, Department of Applied Geology, Dhanbad, IndiaauthorSarkar, A.Physical Research Laboratory, IndiaauthorBhattacharya, S. K.Presidency College, IndiaauthorRay, A. K.authorGeological Society of India, Bangalore, IndiapublisherdocumentHardcopyJournal of the Geological Society of India51 (2)245-248High resolution oxygen isotope analysis of samples from two different Eocene Oligocene Boundary (EOB) sections of Wagapadhar and Waior of Kutch area and their correlation with DSDP sites indicate continuity of sedimentation at these sites. A rapid cooling of -6 degrees C across the EOB, synchronous with extinction of Eocene larger benthic foraminifera, is also observed.completedStratigraphyIsotope geochemistryAsiabenthic taxaC-13/C-12carbonCenozoiccoolingcorrelationDeep Sea Drilling ProjectEoceneextinctionForaminiferaGujarat IndiaIndiaIndian PeninsulaInvertebrataisotope ratiosisotopesKutch IndialithofaciesmicrofossilsO-18/O-16OligoceneoxygenPaleogeneProtistasedimentationstable isotopesstratigraphic boundarystratigraphyTertiaryunconformitiesWagapadhar IndiaWaior IndiaEnglishgeoscientificInformation68.350068.450023.150023.4500