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Titlebook: Understanding Leadership Perspectives; Theoretical and Prac Gilbert W. Fairholm,Matthew R. Fairholm Book 2009 Springer-Verlag New York 2009

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f many species do not always correspond to their total ranges. Apparent extinctions in the North Sea area appear to coincide with the onset of unfavourable environmental conditions, usually in the form of shallowing.
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will highlight the unique and critical insights that can be gained by the inclusion of palaeontological data into modern ecological or conservation studies.978-3-642-44098-4978-3-642-25038-5Series ISSN 2197-9596 Series E-ISSN 2197-960X
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Matthew R Fairholm,Gilbert W Fairholmasserines secondarily regained anisodactyl feet in their evolutionary history. Based on these new insights in the evolution of parrots and passerines, some fossil taxa, which were initially identified as stem group representatives of the Psittaciformes, are now considered to be zygodactyl stem group passerines.
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Matthew R Fairholm,Gilbert W Fairholm top of Younger Dryas (M3c/M4) is dated to 10.610 v.y. BP when first distinct layers of planktonic diatoms occur. Therefore the Pleistocene/Holocene boundary is fixed lithologically by varve counting, beginning at the isochrone of LST (11.323+/-224 v.y. BP), to 10.610 v.y. BP.
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Matthew R Fairholm,Gilbert W Fairholmo recognized, other mechanisms, e.g. motions of micro-plates or exotic terranes, may also cause rock masses to rotate about verical axes. Therefore paleomagnetic data on rotation must be combined with structural data in order to identify the contribution of faulting to block rotation.
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978-1-4419-2745-3Springer-Verlag New York 2009
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