The origin and early evolution of plants

Alexander M C Bowles, Christopher J Williamson, Tom Williams, T.M. Lenton, Philip C J Donoghue

Research output: Contribution to journalArticlepeer-review

51 Citations (SciVal)

Abstract

Highlights The origin of the first photosynthetic eukaryotes through to the first land plants transformed the Earth's biosphere. There is no single unified view of the processes and timing of early plant evolution despite myriad fossil and geochemical evidence. Phylogenetically targeted genomic, morphological, and Earth system data will be necessary to make significant advances in our understanding of early plant evolution given the deep timescales. Abstract Plant (archaeplastid) evolution transformed the biosphere but we are only now beginning to learn how through comparative genomics, phylogenetics and the fossil record. This has illuminated the phylogeny of Archaeplastida, Viridiplantae and Streptophyta, resolving the evolution of key characters, genes and genomes revealing many key innovations to have evolved long before the clades with which they have been casually associated. Molecular clock analyses estimate Streptophyta and Viridiplantae to have emerged in the late Mesoproterozoic-late Neoproterozoic, Archaeplastida in the late-mid Palaeoproterozoic. Together, these insights inform on the coevolution of plants and the Earth system, transforming ecology and global biogeochemical cycles, increasing weathering and precipitating snowball Earth events during which they would have been key to oxygen production and net primary productivity.
Original languageEnglish
Pages (from-to)312-329
JournalTrends in Plant Science
Volume28
Issue number3
Early online date31 Oct 2022
DOIs
Publication statusPublished - 1 Mar 2023

Acknowledgements

We thank Stefan Bengtson, Nick Butterfield, Dianne Edwards, Emmanuelle Javaux, Bruce Runnegar, Marie Catherine Sforna, and Shuhai Xiao for providing images of fossils, and the Culture Collection of Algae and Protozoa (CCAP) for images of extant algae used in this article.

Funding

We wish to acknowledge funding from the Leverhulme Trust ('iDAPT' RPG-2020-199 to C.J.W. and P.C.J.D., and RF-2022-167 to P.C.J.D.); the Natural Environment Research Council (NE/P013678/1 to P.C.J.D., and NE/P013651/1 to T.M.L.) part of the Biosphere Evolution, Transitions, and Resilience (BETR) programme cofunded by the Natural Science Foundation of China (NSFC); the John Templeton Foundation (62220 to P.C.J.D., T.A.W., and T.M.L.); and the Gordon and Betty Moore Foundation (GBMF9741 to P.C.J.D. and T.A.W.).

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