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LATE ORDOVICIAN SEISMITES OF KENTUCKY AND OHIO: A SEDIMENTOLOGICAL AND SEQUENCE STRATIGRAPHIC APPROACHMCLAUGHLIN, PATRICK IAN 27 September 2002 (has links)
No description available.
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Microstratigraphic Analysis of an Amalgamated Horizon in the Type Cincinnatian:Implications for Spatio-Temporal Resolution in the Fossil RecordBarbour, Susan Leigh 16 September 2002 (has links)
No description available.
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43 |
METHODOLOGICAL ADVANCES IN THE USE OF FAUNAL GRADIENT ANALYSIS FOR REGIONAL PALEOECOLOGICAL INVESTIGATIONS IN THE TYPE CINCINNATIAN SERIES (UPPER ORDOVICIAN)WEBBER, ANDREW JULIAN 17 April 2003 (has links)
No description available.
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44 |
INTER- AND INTRASPECIFIC MORPHOLOGICAL VARIATION OF CRINOID COLUMNALS IN RELATION TO WATER DEPTH IN THE TYPE CINCINNATIAN (UPPER ORDOVICIAN)DELINE, BRADLEY L. 17 July 2006 (has links)
No description available.
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The Regional and Global Diversity of Tentaculitoids: A New Look at the Spatio-Temporal and Paleogeographic History of an Enigmatic GroupWittmer, Jacalyn M. January 2009 (has links)
No description available.
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46 |
Sequence Stratigraphy and Event Correlations of Upper Black River and Lower Trenton Group Carbonates of Northern New York State and Southern Ontario, CanadaCornell, Sean Richard 11 October 2001 (has links)
No description available.
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Quantitative Paleobiogeography of Maysvillian (Late Ordovician) Brachiopod Species of the Cincinnati Arch: a Test of Niche Modeling Methods for Paleobiogeographic ReconstructionWalls, Bradley J. 14 August 2009 (has links)
No description available.
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48 |
Macroevolution and Paleobiogeography of Middle to Late Ordovician Brachiopods: A Phylogenetic Biogeographic ApproachWright, David F. 26 July 2012 (has links)
No description available.
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49 |
Dimensional Grain Orientation of Ordovician Turbidite GreywackesOnions, Diane 10 1900 (has links)
This study describes the analysis of orientation of elongate quartz grains in turbidite greywackes of the Normanskill Formation, (Ord.) New York.
No relationship is found between grain orientation and sole features of the beds. No relationship exists between grain orientations taken at different levels above the base of the beds.
Maximum grain size and maximum elongation decrease upwards in the beds. The most elongate grains are those which most clearly show preferred orientation. / Thesis / Master of Science (MSc)
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Palaeobotanical Analysis of Certain Upper Ordovician Sedimentary Rocks Emphasizing Microfossil FragmentsThorne, William 10 1900 (has links)
Several methods for the palaeobotanical analysis of inorganic rocks are developed and through the employment of these methods both microfossils and macrofossils have been recovered from certain Upper Ordovician Strata. These fragments are assigned to series, basing such designation upon their sources and individual morphological characteristics. The problematical identity and biological importance of these fragments is discussed, and their practical usage in problems of correlation is considered. / Thesis / Master of Science (MSc)
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