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Diatoms from the Shelton Mastodon Site
dc.contributor.authorStoermer, Eugene F.en_US
dc.contributor.authorKociolek, John P.en_US
dc.contributor.authorShoshani, Jeheskelen_US
dc.contributor.authorFrisch, C.en_US
dc.date.accessioned2006-09-08T21:01:59Z
dc.date.available2006-09-08T21:01:59Z
dc.date.issued1988-12en_US
dc.identifier.citationStoermer, E. F.; Kociolek, J. P.; Shoshani, J.; Frisch, C.; (1988). "Diatoms from the Shelton Mastodon Site." Journal of Paleolimnology 1(3): 193-199. <http://hdl.handle.net/2027.42/43068>en_US
dc.identifier.issn0921-2728en_US
dc.identifier.issn1573-0417en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/43068
dc.description.abstractA fairly diverse and abundant diatom flora is associated with remains of Mammut americanum at the Shelton Mastodon Site in northern Oakland County, Michigan. The most abundant elements of this flora are species commonly recorded from late-glacial deposits in North America and Europe. The nearest modern analogues of this flora are assemblages deposited in small lakes in the high arctic and present day periglacial environments. Based on the diatoms present, the most probable depositional habitat was the margin of a moderately alkaline (pH>7.0) and moderately productive pond which existed under arctic conditions.en_US
dc.format.extent1133407 bytes
dc.format.extent3115 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherKluwer Academic Publishers; Springer Science+Business Mediaen_US
dc.subject.otherLife Sciencesen_US
dc.subject.otherGeochemistryen_US
dc.subject.otherHydrogeologyen_US
dc.subject.otherMeteorology/Climatologyen_US
dc.subject.otherSedimentologyen_US
dc.subject.otherHydrobiologyen_US
dc.subject.otherDiatomsen_US
dc.subject.otherMammuten_US
dc.subject.otherMichiganen_US
dc.subject.otherLate Glacialen_US
dc.titleDiatoms from the Shelton Mastodon Siteen_US
dc.typeArticleen_US
dc.subject.hlbsecondlevelGeology and Earth Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumGreat Lakes Research Division, University of Michigan, 48109, Ann Arbor, MI, USAen_US
dc.contributor.affiliationumGreat Lakes Research Division, University of Michigan, 48109, Ann Arbor, MI, USAen_US
dc.contributor.affiliationotherDepartment of Biological Sciences, Wayne State University, 48202, Detroit, MI, USAen_US
dc.contributor.affiliationotherDepartment of Biological Sciences, Wayne State University, 48202, Detroit, MI, USAen_US
dc.contributor.affiliationumcampusAnn Arboren_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/43068/1/10933_2004_Article_BF00177765.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1007/BF00177765en_US
dc.identifier.sourceJournal of Paleolimnologyen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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