Hi Wayne and others:

Part of the problem is that reconstructing trends in environmental 
conditions (temperature, pH, O, etc.) are non-trivial and full of 
complicated (and often cross-cancelling) interrelationships (i.e., 
pinning one unknown variable requires assumptions about the other 
unknown one).  Also, most efforts so far have focused on critical 
time intervals (such as Cambrian radiation and mass extinctions), 
making long-term correlative trends uncommon.  Older (Archean and 
Proterozoic) records are in general even patchier and more prone to 
degradation.

General historical geology textbooks are a pretty good start for 
generalities.  The Stanley textbook you noted is wonderful, and has 
the useful feature that each chapter has a two-page visual overview 
showing major trends and relationships between atmosphere/oceans, 
geology, and biology.  These visual overviews should give you a 
pretty simple visual aid.

An increasingly active subdiscipline in geobiology these days you may 
find interesting is termed paleophysiology.  Some recent overviews 
and case studies (especially looking at roles of oxygenation) can be 
seen in the following articles:

Canfield, D.E., S.W. Poulton, and G.M. 
Narbonne.  2007.  Late-Neoproterozoic deep-ocean oxygenation and the 
rise of animal life.  Science 315: 92-95.

Ward, P., C. Labandeira, M. Laurin, and R.A. 
Berner.  2006.  Confirmation of Romer's Gap as a low oxygen interval 
constraining the timing of initial arthropod and vertebrate 
terrestrialization.  PNAS 103: 16818-16822.

Acquisti, C., J. Kleffe, and S. Collins.  2007.  Oxygen content of 
transmembrane proteins over macroevolutionary time scales.  Nature 445: 47-52.

Knoll, A.H., R.K. Bambach, J.L. Payne, S. Pruss, and W.W. 
Fischer.  2007.  Paleophysiology and end-Permian mass 
extinction.  Earth and Planetary Science Letters 256: 295-313.

Graham, J.B., R. Dudley, N.M. Aguilar, and C. 
Gans.  1995.  Implications of the late Paleozoic oxygen pulse for 
physiology and evolution.  Nature 375: 117-120.

None of these offer a simple figure spanning Earth history, but they 
illustrate the variety of ways (and the varied lines of data) we're 
using to examine these relationships.

Cheers,
Phil


At 08:57 PM 9/3/2007, Wayne Tyson wrote:

>** Stanley, Steven M. Earth System History. New York: W.H. Freeman
>and Company, 1999.

~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
   Phil Novack-Gottshall
   Assistant Professor                            [EMAIL PROTECTED]
   Department of Geosciences
   University of West Georgia
   Carrollton, GA 30118-3100

   Phone: 678-839-4061
   Fax: 678-839-4071        http://www.westga.edu/~pnovackg
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