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Late Cretaceous Sponge Borings - Indicators of Salinity and Sedimentation Drumheller, Alberta

dc.contributor.advisorRisk, Michael J.
dc.contributor.authorBirchard, Mark Christopher
dc.contributor.departmentGeologyen_US
dc.date.accessioned2016-05-30T21:27:01Z
dc.date.available2016-05-30T21:27:01Z
dc.date.issued1987-04
dc.description.abstract<p> A detailed study of sponge boring morphotypes within the molluscan fauna of Upper Cretaceous estuarine sediments near Drumheller, Alberta provides information relevant to the depositional environment. Problems with regard to utilizing Entobia as a paleoenvironmental indicator and as an indicator of salinity do not appear to be insurmountable.</p> <p> Distributions and characteristics of associated marine organisms (phoronid worms, gastropods and encrusting bryozoa) suggest that sponge colonies were affected by salinity and sedimentation. Boring networks in Ostrea glabra suggest that more than one species of sponge were present. Sponge distribution patterns, changes in papilla and chamber sizes and preferential occurrence of sponge borings on certain shell thicknesses provide good evidence for responses to salinity and sedimentation.</p>en_US
dc.description.degreeBachelor of Science (BSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/19386
dc.language.isoen_USen_US
dc.subjectcretaceous, sponge, borings, indicators, salinity, sedimentation, morphotypesen_US
dc.titleLate Cretaceous Sponge Borings - Indicators of Salinity and Sedimentation Drumheller, Albertaen_US
dc.typeThesisen_US

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