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. 2012 Nov 28;7(11):e49802. doi: 10.1371/journal.pone.0049802

Table 4. Carbon and nitrogen isotope values from bone collagen of the prehistoric humans and fauna from Grotta d’Oriente.

Lab. N. (S-EVA) Context Species Bone δ13C (‰) δ15N (‰) %C %N C/N % coll.
8378* Oriente X Homo sapiens Ulna −17.8 10.6 38.9 14.2 3.2 0.9
2799 Oriente B Homo sapiens Rib −18.9 11.1 43.5 15.7 3.2 3.1
2800 Oriente B Homo sapiens Rib −18.8 11.2 43.3 15.4 3.3 3.8
2801 Oriente B Homo sapiens Rib −19.0 11.6 43.8 15.8 3.2 5.3
13802 C110/180 Cervus elaphus Metacarpal −20.7 8.5 43.1 15.0 3.4 6.2
13803 B114/160 Cervus elaphus Phalanx I −20.5 5.8 43.0 15.0 3.3 6.9
13807 B80/100 Cervus elaphus Phalanx II −21.0 5.9 41.8 14.6 3.3 3.2
13812 B60/80 Bos primigenius Phalanx II −21.0 6.7 42.4 14.7 3.4 5.1
13814* B60/80 Bos primigenius Ischium −21.2 6.8 45.4 16.3 3.3 12.1
13810 C75/110 Sus scrofa Radius −20.1 8.4 43.7 15.4 3.3 5.9
13811 C75/110 Sus scrofa Metapodial −21.8 4.2 43.4 15.3 3.3 12.4
13804 B80/100 Vulpes vulpes Humerus −20.0 7.3 43.0 15.1 3.3 5.1
13805 B100/114 Vulpes vulpes Ulna −19.5 7.8 42.3 14.7 3.4 2.3
13813 B60/80 Vulpes vulpes Humerus −19.5 7.0 43.5 15.3 3.3 8.7
13798 B40/60 E. marginatus Quadratum −8.9 9.3 30.1 10.6 3.3 3.5
13799 B40/60 E. marginatus Dentary −9.6 9.3 42.9 14.9 3.3 4.6
13800 C14/40 E. marginatus Frontal −9.7 9.9 42.0 14.8 3.3 5.1
13808 A80/114 Ovis vel Capra Femur −21.7 6.6 43.9 15.0 3.4 8.6
13809 A80/114 Ovis vel Capra Radius −16.2 6.3 44.3 15.9 3.3 13.8
13815 C14/40 Ovis vel Capra Mandible −20.4 7.5 43.5 15.1 3.4 9.9

The fauna includes: red deer (C. elaphus), aurochs (B. primigenius), wild boar (S. scrofa), red fox (V. vulpes), ovicaprids (Ovis vel Capra) and dusky grouper (E. marginatus). The C. elaphus specimen S-EVA 13802 originates from stratigraphic unit 110–180 cm in Trench C and is in a different state of preservation compared to all other bones analyzed, thereby pre-dating the Mesolithic humans (Oriente B and X) and most certainly also the late Upper Palaeolithic individual (Oriente C). The wild boar (S. scrofa) specimen S-EVA 13810 is a juvenile and its high δ15N value compared to S-EVA 13811 (an adult) probably reflects in part the isotopic composition of protein acquired before weaning. The samples of ovicaprids (Ovis vel Capra) are early Neolithic and post-date all the humans from Grotta d’Oriente. This might also be the case of the dusky grouper (Epinephelus marginatus) specimen from stratigraphic unit 14–40 cm of Trench C (S-EVA 13800).