From: Predicting the potential distribution of the parasitic Cuscuta chinensis under global warming
Habitat suitability | Historical periods | ||||||||
---|---|---|---|---|---|---|---|---|---|
Last glacial maximum | Mid-holocene | 1960–1990 | |||||||
Area (million km2) | TAPCT (%) | PCT (%) | Area (million km2) | TAPCT (%) | PCT (%) | Area (million km2) | TAPCT (%) | PCT (%) | |
0–0.25 | 140.0203 | – | 94.04 | 140.6176 | + 0.43 | 94.44 | 140.7554 | + 0.01 | 94.53 |
0.25–0.5 | 4.0135 | – | 2.70 | 3.3286 | − 17.06 | 2.24 | 3.2669 | − 1.86 | 2.19 |
0.5–0.75 | 2.5989 | – | 1.75 | 2.1175 | − 18.52 | 1.42 | 2.1213 | + 0.18 | 1.42 |
0.75–1 | 2.2673 | – | 1.52 | 2.8362 | + 25.09 | 1.90 | 2.7565 | − 2.81 | 1.85 |