Abstract
The timing of the origin of crown-angiosperms exemplifies the impact of competing approaches to establishing evolutionary timescales. Fossils of unequivocal crown-angiosperms are not known from before the Cretaceous, and yet molecular estimates range from the Late Jurassic to the Permian. We show that the disagreement between molecular and palaeobotanical estimates is an artefact of interpretations of the fossil record. We employ relaxed molecular clock methods that reflect competing interpretations of the fossil record to show that such methods are entirely capable of recovering an explosive diversification of angiosperms if the fossil record can be interpreted confidently to support this. We argue that older putative angiosperm records have insufficient claim on crown-angiosperm affinity to justify their use in divergence time estimation and, in their absence, estimate crown-angiosperms to have diverged in a Late Jurassic-Early Cretaceous interval. This diminishes the Jurassic gap between molecular clock estimates and literal interpretations of the fossil record but expands the Jurassic gap in the fossil record of stem-angiosperms that is not readily rationalized. Attention should be refocused on the history of stem-angiosperms in which the body plan of this most successful lineage of land plants was assembled.
Original language | English |
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Article number | 242158 |
Journal | Royal Society Open Science |
Volume | 12 |
Issue number | 5 |
Early online date | 28 May 2025 |
DOIs | |
Publication status | Published - 28 May 2025 |
Data Availability Statement
Electronic supplementary material is available online [67]. All data and input files are available at [68].Acknowledgements
We thank Sandra Alvarez-Careterro (UCL), Mario dos Reis (QMUL) and Ziheng Yang (UCL) for discussion.Funding
We thank Sandra Alvarez-Careterro (UCL), Mario dos Reis (QMUL) and Ziheng Yang (UCL) for discussion. J.C. was supported by a Prize Fellowship from the University of Bath. P.C.J.D. was funded by Natural Environment Research Council (NERC) grant (NEP013678/1), part of the Biosphere, Evolution, Transitions and Resilience (BETR) programme, which is co-funded by the Natural Science Foundation for China (NSFC), Biotechnology and Biological Sciences Research Council (BBSRC) grants (BB/T012773/1; BB/Y00339X/1) and a Leverhulme Trust Research Fellowship (RF-2022-167). J.C. was supported by a Prize Fellowship from the University of Bath. P.C.J.D. was funded by Natural Environment Research Council (NERC) grant (NEP013678/1), part of the Biosphere, Evolution, Transitions and Resilience (BETR) programme, which is co-funded by the Natural Science Foundation for China (NSFC), Biotechnology and Biological Sciences Research Council (BBSRC) grants (BB/T012773/1; BB/Y00339X/1) and a Leverhulme Trust Research Fellowship (RF-2022-167). Acknowledgements
Funders | Funder number |
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Université Catholique de Louvain | |
Queen Mary University of London | |
Mario dos Reis | |
University of Bath | |
National Natural Science Foundation of China | |
Natural Environment Research Council | NEP013678/1 |
Biotechnology and Biological Sciences Research Council | BB/T012773/1, BB/Y00339X/1 |
Leverhulme Trust | RF-2022-167 |
Keywords
- angiosperm
- flower
- fossil record
- macroevolution
- molecular clock
- timescale
ASJC Scopus subject areas
- General