Stable carbon, oxygen, and nitrogen, isotope analysis of plants from a South Asian tropical forest: Implications for primatology. Issue 6 (27th March 2017)

• Record Type: Journal Article
• Authors: Roberts, Patrick; Blumenthal, Scott A.; Dittus, Wolfgang; Wedage, Oshan; Lee‐Thorp, Julia A.
• Is Part Of: American journal of primatology. Volume 79:Issue 6(2017:Jun.)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2017-03-27
• Subjects: diet -- plant ecology -- primates -- South Asia -- stable isotope ecology; Primates -- Periodicals; Primates -- Périodiques; 599.8
• DOI: 10.1002/ajp.22656
• Languages: English
• ISSNs: 0275-2565

Abstract

Abstract: Stable isotope analysis of primate tissues in tropical forest contexts is an increasingly popular means of obtaining information about niche distinctions among sympatric species, including preferences in feeding height, forest canopy density, plant parts, and trophism. However, issues of equifinality mean that feeding height, canopy density, as well as the plant parts and plant species consumed, may produce similar or confounding effects. With a few exceptions, researchers have so far relied largely on general principles and/or limited plant data from the study area as references for deducing the predominant drivers of primate isotope variation. Here, we explore variation in the stable carbon (δ 13 C), nitrogen (δ 15 N), and oxygen (δ 18 O) isotope ratios of 288 plant samples identified as important to the three primate species from the Polonnaruwa Nature Sanctuary, Sri Lanka, relative to plant part, season, and canopy height. Our results show that plant part and height have the greatest effect on the δ 13 C and δ 18 O measurements of plants of immediate relevance to the primates, Macaca sinica, Semnopithecus priam thersites, and Trachypithecus vetulus, living in this monsoonal tropical forest. We find no influence of plant part, height or season on the δ 15 N of measured plants. While the plant part effect is particularly pronounced in δ 13 C between fruits and leaves, differential feeding height, and plant taxonomy influence plant δ 13 C and δ 18 O differences in addition to plant organ. Given that species composition in different regions and forest types will differ, the results urge caution in extrapolating general isotopic trends without substantial local baselines studies.