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Fish taphonomy and environmental inference in paleolimnology

dc.contributor.authorElder, R. L.en_US
dc.contributor.authorSmith, Gerald R.en_US
dc.date.accessioned2006-04-07T20:32:59Z
dc.date.available2006-04-07T20:32:59Z
dc.date.issued1988-01en_US
dc.identifier.citationElder, R. L., Smith, G. R. (1988/01)."Fish taphonomy and environmental inference in paleolimnology." Palaeogeography, Palaeoclimatology, Palaeoecology 62(1-4): 577-592. <http://hdl.handle.net/2027.42/27579>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6V6R-48C7DKR-2P/2/eb44dc19362e13b8180548285ef9eca3en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/27579
dc.description.abstractThe contribution of fish studies to palaeoecology generally takes the form of (1) inference from analogies in modern fish faunas and (2) fish taphonomy--the pattern of death and dispersal of bones. (1) Modern fish faunas and associated organisms provide taxonomic, ecological, or functional analogues for interpretation of ancient limiting factors and behaviors. These inferences presume taxonomic conservatism. They also presume functional relationships between morphological form and feeding mode or habitat. They become weak with increased geologic age or phyletic distance between ancient subject and modern anaogue. (2) Fish taphonomy may contribute information about limnology, community composition, life history, mortality, depositional environment, and preservation. Taphonomic reconstruction of ecology and preservation depends on the applicability of analogous processes in modern ecology and l limnology.In aquatic taphonomy, temperature is the most important factor in determining the fate of a carcass. Above about 16[deg]C (depending on depth and pressure), most carcasses are made buoyant by bacterial decay gases and are transported to the surface where they may decay further and fall piecemeal into deepwater environments, or drift to beach environments where wave energy disarticulates, abrades, and scatters the bones. Below about 16[deg]C, most carcasses remain on the bottom until buried; they may be disturbed by scavengers, depending on oxygen concentration in the hypolimnion.en_US
dc.format.extent2313797 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleFish taphonomy and environmental inference in paleolimnologyen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelGeology and Earth Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumMuseum of Paleontology, University of Michigan, Ann Arbor, MI 48109, U.S.A.; Department of Geology, Oberlin College, Oberlin, OH 44074, U.S.A.en_US
dc.contributor.affiliationumMuseum of Paleontology, University of Michigan, Ann Arbor, MI 48109, U.S.A.; Department of Geology, Oberlin College, Oberlin, OH 44074, U.S.A.en_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/27579/1/0000623.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0031-0182(88)90072-7en_US
dc.identifier.sourcePalaeogeography, Palaeoclimatology, Palaeoecologyen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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