Extended Data Fig. 8: The climate warming tracking capacity of marine organisms.
From: Species better track climate warming in the oceans than on land
Combined effect of mean annual sea surface temperature prior to the baseline survey (baseline temperatures) and human pressures on the environment (the standardized HFI) on the slope of the relationship between the velocity of marine species range shifts and the VIS along the latitudinal gradient in the oceans (climate warming tracking capacity). The white lines and hatching represent the range of conditions for which marine taxa closely track the shifting isotherms in latitude (that is slope parameter not significantly different from 1 based on 5,000 bootstrap iterations). White transparent dots show the distribution of the raw data (N = 1,403 range shift estimates) used to fit the model. This plot includes both marine ectotherms and cryptogams.
