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Belize Stalagmite Carbon Isotope Data
Entry ID:
NOAA_NCDC_PALEO_2002-081
Summary
Abstract:
The El Nino/Southern Oscillation (ENSO) system is a prominent component of
interannual climate variability, and the Southern Oscillation Index (SOI) is a primary measure of the state of the ENSO system. Here, we present evidence that ENSO-related changes in the terrestrial carbon cycle can be recorded by stalagmites, thus providing a proxy for past El Nino events. Our analysis of a stalagmite from Belize reveals a strong correlation between the SOI and carbon isotope ratios (d13C values), even though the site experiences no discernible local weather effects that are correlated with the SOI. d13C values of this stalagmite must reflect changes in the overlying rainforest ecosystem's carbon budget that are sensitive to subtle modifications of local weather related to ENSO.
Related URL
Geographic Coverage
(Click for Interactive Map)
Spatial coordinates
Temporal Coverage
Start Date:
2010-11-08
Stop Date:
2010-12-05
Start Date:
2011-11-08
Stop Date:
2011-11-19
Location Keywords
Science Keywords
ISO Topic Category
Quality
Geography department at the University of Otago, New Zealand. Please contact the investigator for more information.
Data Set Progress
COMPLETE
Data Center
Personnel
Role:
INVESTIGATOR
Phone:
+64 3 479 8786
Fax:
+64 3 479 9037
Email:
sjf at geography.otago.ac.nz
Contact Address:
Department of Geography
University of Otago
PO BOX 59
City:
Dunedin
Country:
New Zealand
Publications/References
Fitzsimons, S.J. and Lorrain, R. Subglacial Processes.In Singh, V. P.; Singh, P.; Haritashya, U.K. (Eds.) Encyclopedia of Snow, Ice and Glaciers, Springer ISBN: 978-90-481-2643-9 (2011)
Lorrain, R. and Fitzsimons, S.J. Cold-based glaciers. In Singh, V. P.; Singh, P.; Haritashya, U.K. (Eds.) Encyclopedia of Snow, Ice and Glaciers, Springer ISBN: 978-90-481-2643-9 (2011) Pautler, B.G., Simpson, A. J., Simpson, M. J., Tseng, Li-H., Spraul, M., Dubnick, A. Sharp, M.J. and Fitzsimons, S.J. (2011) Detection and Structural Identification of Dissolved Organic Matter in Antarctic Glacial Ice at Natural Abundance by SPR-W5-WATERGATE 1H NMR Spectroscopy’, Environmental Science and Technology DOI: 10.1021/es200697c Creation and Review Dates
DIF Creation Date:
2012-05-31
Last DIF Revision Date:
2012-06-08
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