Researchers Study Cave’s ‘Breathing’ for Better Climate  Clues
 
Newswise — A University of Arkansas researcher studying the way caves  “
breathe” is providing new insights into the process by which scientists study  
paleoclimates.
 
Katherine Knierim, a graduate student at the University of Arkansas, together 
 with Phil Hays of the geosciences department and the U.S. Geological Survey 
and  Erik Pollock of the University of Arkansas Stable Isotope Laboratory, are 
 conducting close examinations of carbon cycling in an Ozark cave. Caves  “
breathe” in the sense that air flows in and out as air pressure changes. 
The researchers have found that carbon dioxide pressures vary with external  
temperatures and ground cover, indicating a possible link between the carbon  
found in rock formations in the caves and seasonal changes. They presented 
their  findings at a recent meeting of the American Geophysical Union. 
The movement of carbon in cave systems is controlled by the concentration of  
carbon dioxide. When conditions are right, this carbon can be deposited as  
layers in stalagmites, stalactites and soda straws. These layers resemble the  
rings found in trees, except that they can date back millions of years, hold  
information about cave conditions. 
“People have been using these formations as paleoclimate records,” Hays 
said.  However, researchers make an assumption when they do so. 
“The problem is that you have to assume you are getting even carbon and  
oxygen isotope exchange,” Knierim said. Isotopes, or atoms of the same type but 
 
with slightly different weights, are found in plants, animals, organic matter  
and rocks. Different types of material have unique “signatures,” or 
proportions  of a particular atom at a particular atomic weight.  
By looking at carbon isotope ratios in cave topsoils, the cave atmosphere and 
 the stream within the cave, Knierim and her colleagues will be able to 
determine  the different contributions of carbon sources to the formations. 
This 
will help  scientists develop more accurate paleoclimate conditions from cave  
formations. 
A greater knowledge of how carbon cycles through cave systems also will help  
scientists develop better methods for watershed management. 
The researchers are in the geosciences department of the J. William Fulbright 
 College of Arts and Sciences. 
_http://www.newswise.com/articles/view/549811/_ (http://www.newswise.c
om/articles/view/549811/) 
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