Extended Data Fig. 10: Cartograms of the predicted slope coefficient between the velocity of species range shifts and the velocity of isotherm shifts along elevational gradients for terrestrial endotherms, phanerogams and cryptogams.
From: Species better track climate warming in the oceans than on land
Slope estimate per 2° × 2° grid cell along elevational gradients for a, endotherms, b, phanerogams and c, cryptogams. The number of range shift estimates (that is sample size) in each grid cell was used to distort the map: the bigger the grid cell, the larger the sample size. Note that negative slopes do not necessarily mean that species are shifting in the opposite direction to isotherm shifts (see Extended Data Fig. 9).
