Dietary niche stability of equids across the mid-Miocene Climatic Optimum in Oregon, USA

During the middle Miocene in North America, hypsodont equids became more diverse and more abundant than brachydont equids. This pattern is evident in middle Miocene deposits of Oregon in which the brachydont taxa became extinct while the hypsodont equids flourished. This turnover, associated with morphological tooth differences, is hypothesized to be a result of dietary differences between taxa, with hypsodont species exploiting the increasing grassland landscape and demise of the brachydont species a result of less vegetation suitable for browsers. Here this hypothesis is tested and the dietary niches of four equid genera are examined using stable carbon and oxygen isotopes. Dietary niche partitioning is evident based on delta C-13 and delta O-18 values and tooth morphology: Archaeohippus, a small brachydont equid, had a narrow dietary niche most likely consuming crown leaf vegetation in the clearings of a woodland habitat; Parahipppus and Desmatippus, medium sized brachydont to incipiently hypsodont equids, ate C-3 vegetation in a relatively open environment; and aff. Acritohippus, a larger hypsodont equid, had a broad dietary niche eating C-3 grasses in a relatively open environment. The dietary niches of these four genera did not change through time or across the mid-Miocene Climatic Optimum. Local extinction of the browsing genera, especially Archaeohippus with its narrow niche breadth, was most likely due to the opening of habitats as C-3 grasses spread after the mid-Miocene Climatic Optimum. There is no evidence of C-4 vegetation in the diet of aff. Acritohippus consistent with the idea that C-4 grasses did not invade the Pacific Northwest during the middle Miocene, in contrast to other regions of North America during that time. (C) 2015 Elsevier B.V. All rights reserved.