Loudon James E, Sandberg Paul A, Wrangham Richard W, Fahey Babette, Sponheimer Matt
Department of Anthropology, East Carolina University, Greenville, North Carolina.
Sam Noble Oklahoma Museum of Natural History, University of Oklahoma, Norman, Oklahoma.
Am J Primatol. 2016 Oct;78(10):1070-85. doi: 10.1002/ajp.22552. Epub 2016 May 17.
Stable isotope analysis has long been used to study the dietary ecology of living and fossil primates, and there has been increasing interest in using stable isotopes to study primate habitat use and anthropogenic impacts on non-human primates. Here, we examine the stable carbon and nitrogen isotope compositions of chimpanzees (Pan troglodytes) from seven communities in Uganda across a continuum of habitat structure (closed to more open) and access to anthropogenic resources (no reliance to heavy reliance). In general, the hair δ(13) C, but not δ(15) N, values of these communities vary depending on forest structure and degree of anthropogenic influence. When integrated with previously published hair δ(13) C and δ(15) N values for Pan, it is apparent that modern "savanna" and "forest" Pan form discrete clusters in carbon and nitrogen isotope space, although there are exceptions probably relating to microhabitat specialization. The combined dataset also reveals that Pan δ(13) C values (but not δ(15) N values) are inversely related to rainfall (r(2) = 0.62). We converted Pan hair δ(13) C values to enamel equivalents and made comparisons to the fossil hominoids Sivapithecus sp., Gigantopithecus blacki, Ardipithecus ramidus, and Australopithecus anamensis. The δ(13) C values of the fossil hominins Ar. ramidus and Au. anamensis do not cluster with the δ(13) C values of modern Pan in "forest" habitats, or with fossil hominoids that are believed to have inhabited forests. Am. J. Primatol. 78:1070-1085, 2016. © 2016 Wiley Periodicals, Inc.
长期以来,稳定同位素分析一直被用于研究现存和化石灵长类动物的饮食生态学,并且人们越来越有兴趣利用稳定同位素来研究灵长类动物的栖息地利用情况以及人类活动对非人类灵长类动物的影响。在此,我们研究了乌干达七个群落的黑猩猩(Pan troglodytes)的稳定碳和氮同位素组成,这些群落分布在一个连续的栖息地结构范围内(从封闭到更开阔),以及获取人为资源的程度范围内(从无依赖到高度依赖)。总体而言,这些群落的毛发δ(13)C值(而非δ(15)N值)会因森林结构和人为影响程度的不同而有所变化。当将这些数据与先前发表的Pan的毛发δ(13)C和δ(15)N值相结合时,很明显现代的“稀树草原”和“森林”Pan在碳和氮同位素空间中形成了离散的聚类,尽管也有一些例外情况可能与微生境特化有关。综合数据集还显示,Pan的δ(13)C值(而非δ(15)N值)与降雨量呈负相关(r(2) = 0.62)。我们将Pan的毛发δ(13)C值转换为牙釉质等效值,并与化石类人猿西瓦古猿属(Sivapithecus sp.)、巨型猩猩(Gigantopithecus blacki)、拉密达地猿(Ardipithecus ramidus)和南方古猿阿法种(Australopithecus anamensis)进行了比较。化石人族拉密达地猿和南方古猿阿法种的δ(13)C值,既没有与现代“森林”栖息地的Pan的δ(13)C值聚类在一起,也没有与被认为栖息在森林中的化石类人猿的δ(13)C值聚类在一起。《美国灵长类学杂志》78:1070 - 1085,2016年。© 2016威利期刊公司。