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Article: Biostratigraphic summary, Leg 125

TitleBiostratigraphic summary, Leg 125
Authors
Stabell, BAli, JCiampo, GMilner, GWang, YJXu, Y
Issue Date1992
Citation
Proc., Scientific Results, Ocp, Leg 125, Bonin/Mariana Region, 1992, p. 615-622 How to Cite?
AbstractSamples from 15 holes at nine sites in the Izu-Bonin-Mariana region were examined for calcareous nannofossils, foraminifers, diatoms, and radiolarians. The age of the containing sediments range from middle Eocene to Holocene. Nannofossils provided the most useful biostratigraphic framework, but were supplemented with satisfactory agreement by data from foraminifers, radiolarians, and diatoms. Evidence from the biostratigraphic framework shows the likely presence of a sedimentary hiatus in the early Miocene. The presence of a single short hiatus in the early Oligocene and two in the late Miocene and early Pliocene is suggested, but supporting evidence other than nannofossil data is sparse. Evidence from approximate age-depth plots shows that sediment accumulation varies from hole to hole. -from Authors
Persistent Identifierhttp://hdl.handle.net/10722/150958

 

DC FieldValueLanguage
dc.contributor.authorStabell, Ben_US
dc.contributor.authorAli, Jen_US
dc.contributor.authorCiampo, Gen_US
dc.contributor.authorMilner, Gen_US
dc.contributor.authorWang, YJen_US
dc.contributor.authorXu, Yen_US
dc.date.accessioned2012-06-26T06:15:16Z-
dc.date.available2012-06-26T06:15:16Z-
dc.date.issued1992en_US
dc.identifier.citationProc., Scientific Results, Ocp, Leg 125, Bonin/Mariana Region, 1992, p. 615-622en_US
dc.identifier.urihttp://hdl.handle.net/10722/150958-
dc.description.abstractSamples from 15 holes at nine sites in the Izu-Bonin-Mariana region were examined for calcareous nannofossils, foraminifers, diatoms, and radiolarians. The age of the containing sediments range from middle Eocene to Holocene. Nannofossils provided the most useful biostratigraphic framework, but were supplemented with satisfactory agreement by data from foraminifers, radiolarians, and diatoms. Evidence from the biostratigraphic framework shows the likely presence of a sedimentary hiatus in the early Miocene. The presence of a single short hiatus in the early Oligocene and two in the late Miocene and early Pliocene is suggested, but supporting evidence other than nannofossil data is sparse. Evidence from approximate age-depth plots shows that sediment accumulation varies from hole to hole. -from Authorsen_US
dc.languageengen_US
dc.relation.ispartofProc., scientific results, OCP, Leg 125, Bonin/Mariana regionen_US
dc.titleBiostratigraphic summary, Leg 125en_US
dc.typeArticleen_US
dc.identifier.emailAli, J:jrali@hku.hken_US
dc.identifier.authorityAli, J=rp00659en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0027100708en_US
dc.identifier.spage615en_US
dc.identifier.epage622en_US
dc.identifier.scopusauthoridStabell, B=7006471445en_US
dc.identifier.scopusauthoridAli, J=7102266465en_US
dc.identifier.scopusauthoridCiampo, G=6506865829en_US
dc.identifier.scopusauthoridMilner, G=7006680385en_US
dc.identifier.scopusauthoridWang, YJ=7601507632en_US
dc.identifier.scopusauthoridXu, Y=7407815098en_US

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