Abstract
Geophagy among orangutans is the most poorly documented in contrast to the knowledge of soil-eating practices of other great ape species. Observations of soil consumption by orangutans in the Sungai Wain Forest Preserve (Wanariset) of Borneo are presented, along with physico-mineral–chemical analyses of the ingested soil in an effort to understand what might stimulate the activity. The consumed soils are: light colored, not excessively weathered by normal standards, higher in the clay size fraction relative to controls, and are comprised of a mix of clay minerals without any specificity of 1:1, 2:1 and/or 2:1:1 (Si:Al) species. The geophagic soils contain chlorides below detection limits, effectively eliminating salt as a stimulus. Soil chemical and geochemical analyses confirm that orangutans prefer soils with pH levels near or above 4.0, while controls are consistently lower (pH = 3.5–4.0), a considerable difference in acidity for at least four out of six soils consumed. Geochemical analysis shows Al, Fe and K are high in the consumed vs control samples; higher Al follows from higher clay percentages in the consumed earth. Iron and K may play physiological roles, but Fe is mostly in the ferrous form (Fe+2) and may not be readily taken up by the animals. The preferential choice of consumed samples, with pH above 4.0 and higher clay contents, may promote a more beneficial intestinal environment.
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Acknowledgments
This research was carried out with funding from Quaternary Surveys, Toronto and a minor research grant from York University to WCM. We thank Anne Russon (York University) for collecting the samples and making them available to us for analysis.
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Mahaney, W.C., Hancock, R.G.V., Aufreiter, S. et al. Bornean orangutan geophagy: analysis of ingested and control soils. Environ Geochem Health 38, 51–64 (2016). https://doi.org/10.1007/s10653-015-9678-z
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DOI: https://doi.org/10.1007/s10653-015-9678-z