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. 2008 Apr 14;105(15):5786–5791. doi: 10.1073/pnas.0800884105

Table 1.

Mean values of carbon and oxygen isotope ratios for each taxon

Taxon n Mean δ13C, ‰ PDB
Mean (±1σ) δ18O,‰ PDB Mean (±1σ) δ18O,‰ SMOW
Enamel (±1σ) Ecosystem
Fossils
    Moeritherium sp. 5 −8.882 ± 0.36 −22.882 −3.887 ± 0.42 26.901 ± 0.44
    Barytherium sp. 5 −7.847 ± 0.56 −21.847 −4.255 ± 0.44 26.523 ± 0.45
    Anthracotheriid 6 −8.499 ± 1.16 −22.499 0.747 ± 1.23 31.680 ± 1.27
    Thyrohyrax meyeri 6 −7.961 ± 0.70 −21.961 1.336 ± 0.73 32.287 ± 0.75
    Saghatherium bowni 9 −8.276 ± 0.45 −22.276 2.019 ± 1.04 32.991 ± 1.07
    Hyracoid (BQ-2) 6 −6.216 ± 0.44 −20.216 −0.079 ± 0.73 30.828 ± 0.75
Rocks
    Rock from L-41 4 −0.842 ± 0.69 −1.734 ± 2.22 29.122 ± 2.29
    Sample L-41a 1 −9.475 1.770 32.735
    Rock from BQ-2 9 −0.538 ± 0.31 6.975 ± 1.10 38.100 ± 1.13

″Rock from L-41″ does not include sample L-41a, which is displayed separately to show the distinct difference between it and other L-41 results. n = number of specimens successfully sampled for each mammal group. Ecosystem δ13C values were obtained by subtracting an enamel-diet fractionation value of 14‰ from the enamel values.