scholarly journals A polycomb repressive complex 2 gene regulates apogamy and gives evolutionary insights into early land plant evolution

2009 ◽  
Vol 106 (38) ◽  
pp. 16321-16326 ◽  
Author(s):  
Y. Okano ◽  
N. Aono ◽  
Y. Hiwatashi ◽  
T. Murata ◽  
T. Nishiyama ◽  
...  
Nature Plants ◽  
2020 ◽  
Vol 6 (2) ◽  
pp. 107-118 ◽  
Author(s):  
Jian Zhang ◽  
Xin-Xing Fu ◽  
Rui-Qi Li ◽  
Xiang Zhao ◽  
Yang Liu ◽  
...  

2004 ◽  
Vol 58 (2) ◽  
pp. 154-162 ◽  
Author(s):  
Stefan A. Rensing ◽  
Justine Kiessling ◽  
Ralf Reski ◽  
Eva L. Decker

2018 ◽  
Vol 115 (10) ◽  
pp. E2274-E2283 ◽  
Author(s):  
Jennifer L. Morris ◽  
Mark N. Puttick ◽  
James W. Clark ◽  
Dianne Edwards ◽  
Paul Kenrick ◽  
...  

Establishing the timescale of early land plant evolution is essential for testing hypotheses on the coevolution of land plants and Earth’s System. The sparseness of early land plant megafossils and stratigraphic controls on their distribution make the fossil record an unreliable guide, leaving only the molecular clock. However, the application of molecular clock methodology is challenged by the current impasse in attempts to resolve the evolutionary relationships among the living bryophytes and tracheophytes. Here, we establish a timescale for early land plant evolution that integrates over topological uncertainty by exploring the impact of competing hypotheses on bryophyte−tracheophyte relationships, among other variables, on divergence time estimation. We codify 37 fossil calibrations for Viridiplantae following best practice. We apply these calibrations in a Bayesian relaxed molecular clock analysis of a phylogenomic dataset encompassing the diversity of Embryophyta and their relatives within Viridiplantae. Topology and dataset sizes have little impact on age estimates, with greater differences among alternative clock models and calibration strategies. For all analyses, a Cambrian origin of Embryophyta is recovered with highest probability. The estimated ages for crown tracheophytes range from Late Ordovician to late Silurian. This timescale implies an early establishment of terrestrial ecosystems by land plants that is in close accord with recent estimates for the origin of terrestrial animal lineages. Biogeochemical models that are constrained by the fossil record of early land plants, or attempt to explain their impact, must consider the implications of a much earlier, middle Cambrian–Early Ordovician, origin.


2007 ◽  
Vol 168 (5) ◽  
pp. 709-717 ◽  
Author(s):  
Milena Groth‐Malonek ◽  
Theresia Rein ◽  
Rosemary Wilson ◽  
Henk Groth ◽  
Jochen Heinrichs ◽  
...  

2015 ◽  
Vol 37 (3) ◽  
pp. 157-170 ◽  
Author(s):  
Juan Carlos Villarreal ◽  
Karen S. Renzaglia

2017 ◽  
Vol 60 (3) ◽  
pp. 281-288 ◽  
Author(s):  
Wilson A. Taylor ◽  
Paul K. Strother ◽  
Marco Vecoli ◽  
Sa’id Al-Hajri

2018 ◽  
Vol 11 (3) ◽  
pp. 1-14 ◽  
Author(s):  
Sophie de Vries ◽  
Jan de Vries ◽  
Janina K. von Dahlen ◽  
Sven B. Gould ◽  
John M. Archibald ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document