The Timescale of Early Land Plant Evolution PNAS PLUS
The timescale of early land plant evolution PNAS PLUS Jennifer L. Morrisa,1, Mark N. Putticka,b,1, James W. Clarka, Dianne Edwardsc, Paul Kenrickb, Silvia Presseld, Charles H. Wellmane, Ziheng Yangf,g, Harald Schneidera,d,h,2, and Philip C. J. Donoghuea,2 aSchool of Earth Sciences, University of Bristol, Bristol BS8 1TQ, United Kingdom; bDepartment of Earth Sciences, Natural History Museum, London SW7 5BD, United Kingdom; cSchool of Earth and Ocean Sciences, Cardiff University, Cardiff CF10, United Kingdom; dDepartment of Life Sciences, Natural History Museum, London SW7 5BD, United Kingdom; eDepartment of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, United Kingdom; fDepartment of Genetics, Evolution and Environment, University College London, London WC1E 6BT, United Kingdom; gRadclie Institute for Advanced Studies, Harvard University, Cambridge, MA 02138; and hCenter of Integrative Conservation, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Yunnan 666303, China Edited by Peter R. Crane, Oak Spring Garden Foundation, Upperville, VA, and approved January 17, 2018 (received for review November 10, 2017) Establishing the timescale of early land plant evolution is essential recourse but to molecular clock methodology, employing the for testing hypotheses on the coevolution of land plants and known fossil record to calibrate and constrain molecular evolu- Earth’s System. The sparseness of early land plant megafossils and tion to time. Unfortunately, the relationships among the four stratigraphic controls on their distribution make the fossil record principal lineages of land plants, namely, hornworts, liverworts, an unreliable guide, leaving only the molecular clock. However, mosses, and tracheophytes, are unresolved, with almost every the application of molecular clock methodology is challenged by possible solution currently considered viable (14).
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