“…The terrestrialization of plants (embryophytes; Janvier, 2010;Gerrienne et al, 2016;Servais et al, 2019) during Ordovician-Devonian times altered early land ecosystems, instigating the development of soils, and causing major pCO2 fluctuations and changes in geochemical cycles (Algeo and Scheckler, 1998;Beerling, 2007;Kenrick et al, 2012;Morris et al, 2015;Xue et al, 2015Xue et al, , 2016Qie et al, 2019). These changes were triggered by key diversification events among plants linked to the appearance of evolutionary innovations, such as vascular tissues, leaves, seeds and secondary growth (i.e., wood), which together culminated in the establishing of the earliest forests (Decombeix et al, 2011;Kenrick et al, 2012;Xue et al, 2015Xue et al, , 2016Xue et al, , 2018Cascales-Miñana et al, 2019a;Wang et al, 2019;Stein et al, 2020). Since the 1980s, various researchers have focused their attention on documenting the diversity pattern of this early vegetation (e.g., Banks, 1980;Knoll et al, 1984;Edwards and Davies, 1990;Raymond and Metz, 1995;Meyer-Berthaud et al, 2010;Stein et al, 2012;Cascales-Miñana, 2016;Xue et al, 2016;Wang et al, 2019).…”