Academic literature on the topic 'Paleopedology – Eocene'

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Journal articles on the topic "Paleopedology – Eocene"

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Hasiotis, Stephen T., Andres Asian, and Thomas M. Bown. "Origin, architecture, and paleoecology of the early Eocene continental ichnofossilScaphichnium hamatum— integration of ichnology and paleopedology." Ichnos 3, no. 1 (October 1993): 1–9. http://dx.doi.org/10.1080/10420949309386369.

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Smith, J. J., S. T. Hasiotis, M. J. Kraus, and D. T. Woody. "Relationship of Floodplain Ichnocoenoses to Paleopedology, Paleohydrology, and Paleoclimate in the Willwood Formation, Wyoming, During the Paleocene-eocene Thermal Maximum." PALAIOS 23, no. 10 (October 1, 2008): 683–99. http://dx.doi.org/10.2110/palo.2007.p07-080r.

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Terry, Jr, Dennis O. "Paleopedology of the Chadron Formation of Northwestern Nebraska: implications for paleoclimatic change in the North American midcontinent across the Eocene–Oligocene boundary." Palaeogeography, Palaeoclimatology, Palaeoecology 168, no. 1-2 (April 2001): 1–38. http://dx.doi.org/10.1016/s0031-0182(00)00248-0.

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Bown, Thomas M., and Mary J. Kraus. "Time-Stratigraphic Reconstruction and Integration of Paleopedologic, Sedimentologic, and Biotic Events (Willwood Formation, Lower Eocene, Northwest Wyoming, U.S.A.)." PALAIOS 8, no. 1 (February 1993): 68. http://dx.doi.org/10.2307/3515222.

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Dissertations / Theses on the topic "Paleopedology – Eocene"

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Dyer, Kuwanna Monique. "Facies architecture and paleopedology of ancient river systems, Eocene Wilkins Peak Member of the lacustrine Green River Formation, Wyoming." 2005. http://catalog.hathitrust.org/api/volumes/oclc/63165776.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 2005.
Includes one colored folded map in pocket. Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 84-91).
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Mullin, Michelle R. D. "Stable isotope record of soil carbonates from the Eocene-Oligocene transition, Badlands National Park, South Dakota, USA." 2010. http://liblink.bsu.edu/uhtbin/catkey/1632468.

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Sections in and around Badlands National Park, Custer County, South Dakota contain a wealth of faunal and floral data within the White River Group. The Chadronian and Orellan North American Land Mammal Ages define the Eocene-Oligocene boundary here. Faunal and floral changes associated with the Chadronian-Orellan interval have long been attributed to the global Greenhouse-Icehouse climatic transition. Stable isotopes were obtained from paleosol carbonates across the Chadronian-Orellan boundary at three locations in Badlands National Park. Results show wide fluctuations of oxygen isotopes in the uppermost Chadronian and lower Orellan, while carbon isotopes remain relatively stable. The records provide an opportunity to compare the continental response to global change with a near-shore marine system response (Gulf Coastal Plain, USA); and to the world at large. Results indicate a decoupling of the terrestrial response to the Oi-1 glacial event from the marine response. Local conditions appear to play an important role in controlling the record of stable isotopes in paleosol carbonates in the region.
Geologic history of the Eocene-Oligocene -- Climate records -- Causes of climate change -- Climate change across the Eocene-Oligocene -- Current findings -- Discussion.
Department of Geology
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Books on the topic "Paleopedology – Eocene"

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1957-, Bestland Erick A., and Fremd Theodore J. 1952-, eds. Eocene and Oligocene paleosols of central Oregon. Boulder, Colo: Geological Society of America, 1999.

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(Editor), Gregory J. Retallack, Erick A. Bestland (Editor), and Theodore J. Fremd (Editor), eds. Eocene and Oligocene Paleosols of Central Oregon (Special Papers (Geological Society of America), 344.). Geological Society of America, 1999.

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Conference papers on the topic "Paleopedology – Eocene"

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Hasiotis, Stephen, Debra Hanneman, Charles Wideman, Donald Lofgren, and William C. McIntosh. "INTEGRATING SEDIMENTOLOGY, ICHNOLOGY, AND PALEOPEDOLOGY TO RECONSTRUCT LANDSCAPES AND ECOSYSTEMS OF THE UPPER EOCENE PIPESTONE SPRINGS STRATA, WESTERN MONTANA." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-370629.

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