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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 (19772000) 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
18O values that correspond with recent TC rain events nearby. A logistic discriminant model reliably identified TC proxy signals using the measurable parameters
18O and
13C values, and single point changes in
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
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
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