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dc.contributor.authorPacker, Stephen Ronald
dc.contributor.otherSchool of Geography, Earth and Environmental Sciencesen_US
dc.date.accessioned2013-10-10T12:01:25Z
dc.date.available2013-10-10T12:01:25Z
dc.date.issued1991
dc.identifierNOT AVAILABLEen_US
dc.identifier.urihttp://hdl.handle.net/10026.1/2153
dc.descriptionThis is a digitised version of a thesis that was deposited in the University Library. If you are the author and you have a query about this item please contact PEARL Admin (pearladmin@plymouth.ac.uk)
dc.descriptionMerged with duplicate record 10026.1/720 on 10.04.2017 by CS (TIS)
dc.description.abstract

The foraminiferal fauna recorded from the Amager Greensand, Amager Limestone and Bavnodde Greensand formations of Bornholm, Denmark are described herein. These formations range in age from Early Albian to Middle Santonian. The succession contains major breaks in deposition. A new foraminiferal biozonal scheme is presented, comprising six local assemblage biozones. These are compared to foraminiferal zonal schemes proposed for other areas of Northwest Europe. This data is then integrated with published data from macrofossil groups. Palaeoecological data is presented utilising foraminiferal group composition through the succession. An event synthesis is proposed for the study interval combining palaeoecology, biostratigraphy, lithostratigraphy and basin events. Transgressive phases are recognised in the Early Albian, Early Cenomanian and Late Cenomanian-Early Turonian. The Coniacian interval overall shows stable outer shelf water depths, whilst the Late Coniacian-Santonian is probably characterised by an initial phase of increasing water depth followed by a probably tectonically influenced water depth reduction.

en_US
dc.language.isoenen_US
dc.publisherUniversity of Plymouthen_US
dc.titleForaminiferal biostratigraphy and palaeoecology of the Albian to Santonian (Cretaceous) of Bornholm, Denmarken_US
dc.typeThesis
plymouth.versionFull versionen_US
dc.identifier.doihttp://dx.doi.org/10.24382/3528
dc.identifier.doihttp://dx.doi.org/10.24382/3528


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