Stomatal Density and Index of Fossil Plants Track Atmospheric Carbon Dioxide in the Palaeozoic

It has been demonstrated that the leaves of a range of foresttree species have responded to the rising concentration of atmosphericCO₂ over the last 200 years by a decrease in both stomatal densityand stomatal index. This response has also been demonstratedexperimentally by growing plants under elevated CO₂ concentrations.Investigation of Quaternary fossil leaves has shown a correspondingstomatal response to changing CO₂ concentrations through a glacial-interglacialcycle, as revealed by ice core data. Tertiary leaves show asimilar pattern of stomatal density change, using palynologicalevidence of palaeo-temperature as a proxy measure of CO₂ concentration.The present work extends this approach into the Palaeozoic fossilplant record. The stomatal density and index of Early Devonian,Carboniferous and Early Permian plants has been investigated,to test for any relationship that they may show with the changesin atmospheric CO₂ concentration, derived from physical evidence,over that period. Observed changes in the stomatal data givesupport to the suggestion from physical evidence, that atmosphericCO₂ concentrations fell from an Early Devonian high of 10-12times its present value, to one comparable to that of the presentday by the end of the Carboniferous. These results suggest thatstomatal density of fossil leaves has potential value for assessingchanges in atmospheric CO₂ concentration through geologicaltime.Copyright 1995, 1999 Academic Press Aglaophyton major, Sawdonia ornata, Swillingtonia denticulata, Lebachia frondosa, Juncus effusus, Psilotum nudum, Araucaria heterophylla, stomatal density, stomatal index, Palaeozoic CO₂