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

Geology; February 2007; v. 35; no. 2; p. 111-114; DOI: 10.1130/G23145A.1
© 2007 Geological Society of America
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
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI 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 ISI Web of Science (3)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Frappier, A. B.
Right arrow Articles by Frappier, B. R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Stalagmite stable isotope record of recent tropical cyclone events

Amy Benoit Frappier*,1, Dork Sahagian2, Scott J. Carpenter3, Luis A. González4 and Brian R. Frappier5

1 Department of Geology & Geophysics, Boston College, Chestnut Hill, Massachusetts 02467, USA
2 Environmental Initiative and Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015, USA
3 Center for Global and Regional Environmental Research and Department of Geoscience, University of Iowa, Iowa City, Iowa 52242, USA
4 Department of Geology, University of Kansas, Lawrence, Kansas 66045, USA
5 Department of Natural Resources, University of New Hampshire, Durham, New Hampshire 03857, USA

We present a 23 yr stalagmite record (1977–2000) of oxygen isotope variation, associated with 11 tropical cyclones (TCs), from Actun Tunichil Muknal cave in central Belize. High-resolution microsampling yielded a record of monthly to weekly temporal resolution that contains abrupt decreases (negative excursions) in calcite {delta}18O values that correspond with recent TC rain events nearby. A logistic discriminant model reliably identified TC proxy signals using the measurable parameters {delta}18O and {delta}13C values, and single point changes in {delta}18O value. The logistic model correctly identified 80% of excursions as TC events and incorrectly classified only 1 of nearly 1200 nonstorm sampling points. In addition to enabling high-resolution TC frequency reconstruction, this geologic proxy also provides information about the intensity of individual TCs. A multiple regression predicted TC intensity (R2 = 0.465, p = 0.034) using sampling frequency and excursion amplitude. Consistent with previous low-resolution studies, we found that the decadal average {delta}18O value was lower during the 1990s when several TCs produced rainfall in the area, but higher during the 1980s when only one TC struck. Longer, accurately dated, high-resolution speleothem stable isotope records may be a useful new tool for paleotempestology, to clarify associations between highly variable TC activity and the dynamic range of Quaternary climate.

Key Words: speleothems • stable isotopes • paleotempestology • hurricanes • paleoclimatology • Central America







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Geological Society of America