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. 2001 Feb 20;98(5):2485–2490. doi: 10.1073/pnas.041616098

Table 2.

Past climatic variables for archaeological sites estimated from δ13C values in bison bone, associated dietary fractions of C4 plants, and correlations of C4 fractions with weather variables

*NWS Station/ Archaeological Site yr BP MNI Annual precipitation
June precipitation
August minimum temperature
mm P mm P °C P
*Gillette (2 east) Present 391.2  (95.5) 71.4 (45.7) 12.1  (1.5)
 CKM 12,590 4 371.2  (12.0) 0.09 62.2 (20.4) 0.07 11.4  (0.1) <0.001
*Morrisey Present 306.1  (65.5) 52.6 (25.9) 14.2  (1.5)
 ABF 12,590 9 378.9  (20.3) <0.001 63.5 (3.5) 0.02 11.5  (0.2) <0.001
 ABAB 12,390 14 363.6  (10.7) <0.001 60.9 (1.8) 0.05 11.3  (0.1) <0.001
 ABHG 11,910 11 397.6  (26.0) <0.001 66.7 (4.4) <0.01 11.7  (0.3) <0.001
*Upton Present 367.3  (77.7) 65.3 (37.9) 11.5  (1.6)
 HK 7,280 12 415.5  (34.0) <0.01 69.8 (5.8) 0.26 11.9  (0.4) 0.09

Values for present weather are from NWS reporting stations of closest geographic proximity (*) (numbers of reporting years ranged from 64 to 69 at Gillette, 20 to 33 at Morrisey, and 39 to 42 at Upton). For archaeological sites, we calculated the standard deviation of dietary C4 from standard deviations in δ13C values of each population of bison sampled. The standard error about the regression (sy.x) is ±37.35 mm for normal annual precipitation, ±8.25 mm for normal June average precipitation, and ±0.86°C for normal August minimum temperature. Past values in bold are significantly different from current weather at the nearest NWS station (two-tailed t test). Standard deviations are in parentheses. MNI, minimum number of individual bison sampled.