Dear Friends,

Two recent papers, which are coauthored by Dr. Greg J. 
Retallack and discuss the Permian mass extinction, have 
been recently published. 

They are:

Retallack, G.J. and Krull, E.S. 2006. Carbon isotopic evidence 
for terminal-Permian methane outbursts and their role in 
extinctions of animals, plants, coral reefs and peat swamps. 
In Greb, S. and DiMichele, W.A., Editors, Wetlands through 
time. Special Paper of the Geological Society of America. 
vol 399, p 249-268.

The 3 MB version of the above paper can be downloaded from:

http://www.uoregon.edu/~gregr/Papers/Ragnarok2.pdf

This paper provides a very detailed discussion of what he and
his coauthors argued caused the Permian mass extinction.

Also, there is:

Retallack, G.J., Greaver, T., Jahren, A.H., Smith, R.M.H., 
Sheldon, N.D., and Metzger, C.A., 2006, Middle-Late 
Permian mass extinction on land. Geological Society of 
America Bulletin. vol. 118, p. 1398–1411.

The 1.5 MB version of the above paper can be downloaded from:

http://www.uoregon.edu/~gregr/Papers/Mid-Late%20Permian%20extinction.pdf

The above Geological Society of America Bulletin paper is 
interesting because, they recognize two distinct and separate 
geologically abrupt mass extinctions on land. One of these 
occurs at the end of the Middle Permian (Guadalupian) at 
260.4 Ma and a later one occurring with the Permian Period 
at 251 Ma. Both of these correspond to previously recognized
marine mass extinctions. He is quite skeptical of the Permian
mass extinctions as having been related to any asteroid or
comet impact.

Other papers coauthored by Greg J. Retallack, which are
related to the Permian extinction can be found at:

http://www.uoregon.edu/~gregr/publications.html

They include:

Retallack, G.J., Jahren, A.H., Sheldon, N.D., Chakrabarti, R., 
Metzger, C.A., and Smith, R.M.H., 2005. Permian-Triassic 
boundary in Antarctica. Antarctic Science 17, 241-258.

The PDF file for this paper can be found at:

http://www.uoregon.edu/~gregr/Papers/PTAntarctica.pdf

Yours,

Paul


 
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