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Bown, Thomas M., Kraus, Mary J. (1993) Time-Stratigraphic Reconstruction and Integration of Paleopedologic, Sedimentologic, and Biotic Events (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.) PALAIOS, 8 (1) 68 doi:10.2307/3515222

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Reference TypeJournal (article/letter/editorial)
TitleTime-Stratigraphic Reconstruction and Integration of Paleopedologic, Sedimentologic, and Biotic Events (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.)
JournalPALAIOS
AuthorsBown, Thomas M.Author
Kraus, Mary J.Author
Year1993 (February)Volume8
Issue1
PublisherSociety for Sedimentary Geology
DOIdoi:10.2307/3515222Search in ResearchGate
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Mindat Ref. ID411688Long-form Identifiermindat:1:5:411688:6
GUID0
Full ReferenceBown, Thomas M., Kraus, Mary J. (1993) Time-Stratigraphic Reconstruction and Integration of Paleopedologic, Sedimentologic, and Biotic Events (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.) PALAIOS, 8 (1) 68 doi:10.2307/3515222
Plain TextBown, Thomas M., Kraus, Mary J. (1993) Time-Stratigraphic Reconstruction and Integration of Paleopedologic, Sedimentologic, and Biotic Events (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.) PALAIOS, 8 (1) 68 doi:10.2307/3515222
In(1993, February) PALAIOS Vol. 8 (1) Society for Sedimentary Geology

See Also

These are possibly similar items as determined by title/reference text matching only.

Bown, Thomas M., Kraus, Mary J. (1983) Ichnofossils of the alluvial Willwood Formation (lower Eocene), Bighorn Basin, northwest Wyoming, U.S.A. Palaeogeography, Palaeoclimatology, Palaeoecology, 43 (1) 95-128 doi:10.1016/0031-0182(83)90050-0
Bown, Thomas M., Kraus, Mary J. (1981) Lower Eocene alluvial paleosols (Willwood Formation, Northwest Wyoming, U.S.A.) and their significance for paleoecology, paleoclimatology, and basin analysis. Palaeogeography, Palaeoclimatology, Palaeoecology, 34. 1-30 doi:10.1016/0031-0182(81)90056-0
Bown, Thomas M., J. Kraus, Mary (1981) Vertebrate fossil-bearing paleosol units (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.): Implications for taphonomy, biostratigraphy, and assemblage analysis. Palaeogeography, Palaeoclimatology, Palaeoecology, 34. 31-56 doi:10.1016/0031-0182(81)90057-2
WOODY, D. T., SMITH, J. J., KRAUS, M. J., HASIOTIS, S. T. (2014) MANGANESE-BEARING RHIZOCRETIONS IN THE WILLWOOD FORMATION, WYOMING, U.S.A.: IMPLICATIONS FOR PALEOCLIMATE DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM. PALAIOS, 29 (6) 266-276 doi:10.2110/palo.2013.105
Kraus, Mary J., Bown, Thomas M. (1993) Short-term sediment accumulation rates determined from Eocene alluvial paleosols. Geology, 21 (8) 743 doi:10.1130/0091-7613(1993)021<0743:stsard>2.3.co;2
Davies-Vollum, K. Sian, Wing, Scott L. (1998) Sedimentological, Taphonomic, and Climatic Aspects of Eocene Swamp Deposits (Willwood Formation, Bighorn Basin, Wyoming) PALAIOS, 13 (1) 28 doi:10.2307/3515279
Bown, Thomas M., Rose, Kenneth D. (1991) Evolutionary relationships of a new genus and three new species of Omomyid primates (Willwood Formation, Lower Eocene, Bighorn Basin, Wyoming). Journal of Human Evolution, 20 (6). 465-480 doi:10.1016/0047-2484(91)90020-v
Wood, A. R., Kraus, M. J., Gingerich, P. D. (2008) Downslope Fossil Contamination: Mammal-Bearing Fluvial Conglomerates and the Paleocene-Eocene Faunal Transition (Willwood Formation, Bighorn Basin, Wyoming) PALAIOS, 23 (6) 380-390 doi:10.2110/palo.2007.p07-045r
Aziz, Hayfaa Abdul, Hilgen, Frits J., van Luijk, Gerson M., Sluijs, Appy, Kraus, Mary J., Pares, Josep M., Gingerich, Philip D. (2008) Astronomical climate control on paleosol stacking patterns in the upper Paleocene–lower Eocene Willwood Formation, Bighorn Basin, Wyoming. Geology, 36 (7) 531 doi:10.1130/g24734a.1
Bown, Thomas M., Kraus, Mary J., Aslan, Andres (1992) Floodplains and paleosols in the Wyoming Eocene sequence: implications for the taphonomy and paleoecology of faunas. The Paleontological Society Special Publications, 6. 31 doi:10.1017/s2475262200005918
Smith, J. J., Hasiotis, S. T., Kraus, M. J., Woody, D. T. (2008) Relationship of Floodplain Ichnocoenoses to Paleopedology, Paleohydrology, and Paleoclimate in the Willwood Formation, Wyoming, During the Paleocene-eocene Thermal Maximum. PALAIOS, 23 (10) 683-699 doi:10.2110/palo.2007.p07-080r
 
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