Notes 2303 Isotopic analyses of bone collagen of European cave bears (Ursus speleaus) have provided additional insight into their nutritional ecology, but these analyses are a tool that must be used in conjunction with other methods of investigation. While Bocherens’ comments focused purely on the methodology of isotope analyses to argue that cave bears were vegetarians, we base our conclusion of omnivory in this comment on ursid morphology, isotopic analyses, digestive physiology, and foraging dynamics. However, we do wish to (i) correct an error identified by Bocherens and (ii) propose an alternative view of cave bear diets that bridges the relatively narrow conclusions reached by other recent investigators. All Pleistocene samples analyzed by Hilderbrand et al. (1996) were bone collagen extracted from adult specimens. Thus, the influence of a cub’s milk diet and the resulting increased δ15N signatures of dentine collagen are irrelevant to the conclusions of Hilderbrand et al. (1996). However, the error that we made was in assuming that the collagen values in Bocherens et al. (1994, Table 5) were for bone. Because they are actually tooth collagen values, they are not comparable to the bone collagen values measured by Hilderbrand et al. (1996). While geographic variation in isotopic signatures can occur, the degree of variation seen is not enough to refute the conclusions reached by Hilderbrand et al. (1996). The north to south δ15N gradient suggested by Bocherens is not a simple, straightforward process (Cormie and Schwarcz 1994). While grazing bovids would generally increase their consumption of C4 grasses in more southerly latitudes and thereby have an increased δ15N signature, cave bears are characteristic of “a food chain based on C3 plants” (Nelson 1998). North American cervids, ranging from latitude 36 to 60N, preferentially feed on C3 plants and display similar δ15N signatures (3.9 ± 0.6‰ in Alaska, 4.0 ± 1.0‰ in Yellowstone National Park, and 4.3 ± 1.0‰ in Colorado and New Mexico (Jacoby et al. 1999)). Cave bear remains have been found across a similar latitudinal range (38–52N) in Europe (Kurten 1976). Hilderbrand et al. (1996) recognized that cave bears ranged across Europe and likely consumed varied diets, therefore adult cave bear specimens were selected from widely diverse geographic locations. Thus, rather than infer characteristics of the entire species from samples collected at a few sites in France (Bocherens et al. 1994), Hilderbrand et al. (1996) assesed the dietary ecology of the species from samples collected across the cave bear’s range. Yield, %C, and %N of extracted collagen were assessed for all samples by Hilderbrand et al. (1996). However, these values were not reported because (i) no isotope values would have been reported if it was not certain that bone collagen was indeed being used, as yield of extraction and purity are basic to all such studies (Chisholm et al. 1983, cited by Hilderbrand et al. 1996), and (ii) assessment of the European cave bear diet was a small part of a much larger study in which more than 1000 samples were analyzed for their isotope content, and the reporting of all such data seemed superfluous. The δ15N values reported for bone collagen of modern and historic mammals by Bocherens et al. (1994) and Hilderbrand et al. (1996), with the exception of the cave bear, are very similar and within expected ranges. However, the cave bear bone collagen values are very different, 2.9 ± 1.3‰ (n = 9) (Table 1 in Bocherens et al. 1994) versus 8.4 ± 0.5‰ (n = 10) (Hilderbrand et al. 1996). Either a mistake was made by one group, as suggested by Bocherens, or both values are correct and require a biological explanation. The traditional view of European cave bears as herbivores originated from studies of morphology, specifically jaw structure, dentition, and tooth wear (Kurten 1972), prior to detailed studies of bear nutritional ecology. Kurten (1972) argued that “vegetarianism [had] gone to a veritable culmination in the cave bear” in which the “lengthened and expanded molars” were necessary to degrade the “tough cellulose which encased the plant cell wall.” Recent studies of cave bear diets using morphology and (or) isotopic analyses have led to varying conclusions, including that they were (i) a strictly vegetarian (Bocherens et al. 1994), (ii) highly omnivorous, specializing on plant parts (e.g., “particularly tough nuts and fibrous tubers”) and invertebrates (e.g., grubs) (Stiner et al. 1998), (iii) highly specialized “root grubbers” that could not have been vegetarian in the sense of consuming only leaves and stems but may have supplemented their diet with rodents encountered during root digging (Mattson 1997), and (iv) omnivores that consumed vertebrate flesh in addition to the wide range of other plant and animal foods consumed by north-temperate-zone bears (Hilderbrand et al. 1996). While tooth wear and dentition indicate that plant matter, tubers, and associated abrasive material were components of