Fig. 3: Comparison of environmental indicators from Angrenjin Co with other archeological and paleoclimatic records.
From: 3,600 years of human adaptation to drought intensification on the southern Tibetan Plateau

(a) Concentrations of coprophilous fungal spores (grazing indicator) from Angrenjin Co (this study); (b) Age distribution of zooarchaeological sites in the high-altitude areas of the STP (the brown pie charts represent the proportion of domesticated animal remains among total animal remains) (Supplementary Table 2), BG (E–P) is the Bangga site (early phase), and the sites correspond to those in Fig. 1A; (c) Stellera concentrations from Angrenjin Co42; (d) Age distribution of archeological sites with cereals in the high-altitude areas of the STP (Supplementary Table 2) (site locations are shown in Fig. 1A; (e) The ratio of cereal-type Poaceae to total Poaceae, and (f) Poaceae >40 μm concentration (cereal indicators) from Angrenjin Co (this study); (g) Glomus-type concentrations (erosion indicator) from Angrenjin Co (this study); (h) Gelasinospora sp. distribution and charcoal >100 μm concentration (fire indicators) from Angrenjin Co (this study); (i) Pollen PCA1 sample scores from Angrenjin Co42; (j) Geochemical PCA1 sample scores from Angrenjin Co43; (k) Reconstructed summer precipitation anomaly (mm/day) from Angrenjin Co44; (l) Grain size PCA1 sample scores from Paru Co45; (m) Median grain size (μm) from Nam Co46; (n) Reconstructed mean annual air temperature (°C)47. All climate proxies are fitted with Generalized additive models (GAMs). The shaded bands are 95% confidence intervals.