Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6349724 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2015 | 25 Pages |
Abstract
The age of four large termite mounds has been determined by 14C-dating the acid-insoluble organic carbon fraction of samples taken along the central vertical axis of two active and two abandoned mounds. The age sequence in the active mounds is erratic, but the results for the abandoned mounds show a logical increase of 14C-age with depth. The ages measured at 50 cm above ground level were 2335-2119 cal yr BP for the large abandoned mound (630 cm high), and 796-684 cal yr BP for the small abandoned mound (320 cm high). Cold-water-extractable organic carbon (CWEOC) measurements combined with spectroscopic analysis revealed that the lower parts of the active mounds may have been contaminated with recent carbon that leached from the active nest. Nonetheless, this method appears to provide reliable age estimates of large, abandoned termite mounds, which are older than previously estimated. Furthermore, historical mound growth rates seem to correspond to past temperature changes, suggesting a relation between past environmental conditions and mound occupancy.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Hans Erens, Mathieu Boudin, Florias Mees, Basile Bazirake Mujinya, Geert Baert, Mark Van Strydonck, Pascal Boeckx, Eric Van Ranst,