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Assessing the potential for the stomatal characters of extant and fossil Ginkgo leaves to signal atmospheric CO₂ change¹

²Laboratory of Systematic and Evolutionary Botany, and Department of Palaeobotany, Institute of Botany, Chinese Academy of Sciences, Xiangshan, Beijing 100093, P. R. China ³Department of Geology, Royal Holloway, University of London, Egham, Surrey TW20 0EX, UK ⁴Department of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, UK

The stomatal density and index of fossil Ginkgo leaves (Early Jurassic to Early Cretaceous) have been investigated to test whether these plant fossils provide evidence for CO₂-rich atmosphere in the Mesozoic. We first assessed five sources of natural variation in the stomatal density and index of extant Gingko biloba leaves: (1) timing of leaf maturation, (2) young vs. fully developed leaves, (3) short shoots vs. long shoots, (4) position in the canopy, and (5) male vs. female trees. Our analysis indicated that some significant differences in leaf stomatal density and index were evident arising from these considerations. However, this variability was considerably less than the difference in leaf stomatal density and index between modern and fossil samples, with the stomatal index of four species of Mesozoic Ginkgo (G. coriacea, G. huttoni, G. yimaensis, and G. obrutschewii) 60–40% lower than the modern values recorded in this study for extant G. biloba. Calculated as stomatal ratios (the stomatal index of the fossil leaves relative to the modern value), the values generally tracked the CO₂ variations predicted by a long-term carbon cycle model confirming the utility of this plant group to provide a reasonable measure of ancient atmospheric CO₂ change.

Key Words: atmospheric CO₂ • cuticles • Ginkgo • plant fossils • stomatal density • stomatal index • stomatal ratio

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