From: Palaeoecological differences underlie rare co-occurrence of Miocene European primates
Morphotypes | # M | pS | pR | pH | MS | #C | δ13C | SD δ13C | δ18OCO3 | SD δ18OCO3 | #P | δ18OPO4 | SD δ18OPO4 | Δ δ18OCO3-δ18OPO4 |  |  | ||
 Morphotype 1 | 8 | 69.2 | 30.8 | 100 | 0.31 | 8 | − 10.5 | 0.7 | 27.9 | 1.0 | 6 | 19.6 | 1.4 | 8.4 |  |  | ||
 Morphotype 2 | 24 | 80.6 | 19.4 | 100 | 0.19 | 21 | − 11.8 | 0.8 | 27.7 | 1.5 | 19 | 19.1 | 1.9 | 8.7 |  |  | ||
 Morphotype 3 | 11 | 86.7 | 13.3 | 95 | 0.21 | 6 | − 11.0 | 1.2 | 27.0 | 0.6 | 5 | 18.5 | 1.1 | 8.3 |  |  | ||
Environmental phases | #M | pS | pR | pH | MS | #C | δ13C | SD δ13C | δ18OCO3 | SD δ18OCO3 | #P | δ18OPO4 | SD δ18OPO4 | Δ δ18OCO3-δ18OPO4 | δ13Cdiet, mequ | MAPa (mm/year) | MAPb (mm/year) | MAT (°C) |
 Phase III (11.70–11.60 Ma) | 23 | 71.9 | 28.1 | 97.3 | 0.32 | 19 | − 11.1 | 1.2 | 27.2 | 1.2 | 19 | 18.5 | 1.6 | 8.7 | − 27.2 | 801 | 608 | 17.1 |
 Phase II (11.90–11.79 Ma) | 15 | 83.3 | 16.7 | 100 | 0.16 | 13 | − 11.4 | 1.2 | 27.7 | 1.2 | 6 | 19.8 | 1.7 | 8.2 | − 27.5 | 992 | 765 | 20.3 |
 Phase I (12.33–11.95 Ma) | 7 | 90.9 | 9.1 | 100 | 0.09 | 5 | − 12.0 | 0.3 | 28.9 | 0.8 | 5 | 20.4 | 0.9 | 8.5 | − 28.1 | 1190 | 928 | 21.8 |