Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Mineralogical Magazine Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Mineralogical Magazine; February 2008; v. 72; no. 1; p. 317-320; DOI: 10.1180/minmag.2008.072.1.317
© 2008 Mineralogical Society of Great Britain and Ireland
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Gislason, S. R.
Right arrow Articles by Oskarsson, N.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Session 4: Global geochemical cycles and climate change

The feedback between climate and weathering

S. R. Gislason1,*, E. H. Oelkers2, E. S. Eiriksdottir1, M. I. Kardjilov1, G. Gisladottir1, B. Sigfusson1, A. Snorrason3, S. Elefsen3, J. Hardardottir3, P. Torssander4 and N. Oskarsson1

1 Institute of Earth Sciences, University of Iceland, Sturlugata 7, 101 Reykjavík, Iceland
2 Géochimie et Biogéochimie Experimentale –LMTG/Université Paul Sabatier, 14 rue Edouard Belin, 31400 Toulouse, France
3 National Energy Authority, Grensásvegi 9, 108 Reykjavík, Iceland
4 Department of Geology and Geochemistry, Stockholm University, SE-10691 Stockholm, Sweden

* E-mail: sigrg{at}raunvis.hi.is

ABSTRACT

Long-term climate moderation is commonly attributed to chemical weathering; the greater the temperature and precipitation the faster the weathering rate. To test this widely-held hypothesis, we performed a field study and determined the weathering rates of eight nearly pristine north-east Iceland river catchments with varying glacial cover over 44 y. Statistically significant linear positive correlations were found between mean annual temperature and chemical weathering in all eight catchments and between mean annual temperature and mechanical weathering and runoff in seven of the eight catchments. The runoff, mechanical weathering flux, and chemical weathering fluxes in these catchments are found to increase from 6 to 16%, 8 to 30%, and 4 to 14%, respectively, depending on the catchment for each degree of temperature increase. Positive correlations were found between time and mechanical and chemical weathering for all catchments. In summary, these results demonstrate a significant feedback between climate and Earth surface weathering, and suggest that this weathering rate is currently increasing with time due to global warming.

KEYWORDS: climate moderation, chemical weathering, CO2 fixation, global carbon cycle







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of Great Britain and Ireland