The future as the key to the past for palaeobotany?

Continued increase in the concentration of atmospheric CO(2) and its possible effects on global climate has generated intense research interest on the likely responses of terrestrial plants and vegetation. Results from this new research provide quantitative information on plant function and growth in an environment with a high CO(2) concentration, but are also relevant to understanding plant growth in the distant past and to the techniques employed by palaeobotanists for reconstructing past climates from fossil plant remains. Experimental CO(2) enrichment of plants has demonstrated direct effects on leaf physiognomy, the tolerance of plants to low temperature and the relationship between tree rings, CO(2) and climate; it therefore signals the need for caution in interpreting palaeoclimates from fossils.