TY  - JOUR
A1  - Bechteler, Julia
A1  - Schmidt, Alexander R.
A1  - Renner, Matthew A. M.
A1  - Wang, Bo
A1  - Pérez-Escobar, Oscar Alejandro
A1  - Schäfer-Verwimp, Alfons
A1  - Feldberg, Kathrin
A1  - Heinrichs, Jochen
T1  - A Burmese amber fossil of Radula (Porellales, Jungermanniopsida) provides insights into the Cretaceous evolution of epiphytic lineages of leafy liverworts
Y1  - 2017
VL  - 20
IS  - 2
SP  - 201
EP  - 213
JF  - Fossil Record
DO  - 10.5194/fr-20-201-2017
DO  - 10.5194/fr-20-201-2017-supplement
DO  - 10.23689/fidgeo-2270
N2  - DNA-based divergence time estimates suggested major changes in the composition of epiphyte lineages of liverworts during the Cretaceous; however, evidence from the fossil record is scarce. We present the first Cretaceous fossil of the predominantly epiphytic leafy liverwort genus Radula in ca. 100 Myr old Burmese amber. The fossil's exquisite preservation allows first insights into the morphology of early crown group representatives of Radula occurring in gymnosperm-dominated forests. Ancestral character state reconstruction aligns the fossil with the crown group of Radula subg. Odontoradula; however, corresponding divergence time estimates using the software BEAST lead to unrealistically old age estimates. Alternatively, assignment of the fossil to the stem of subg. Odontoradula results in a stem age estimate of Radula of 227.8 Ma (95 % highest posterior density (HPD): 165.7–306.7) and a crown group estimate of 176.3 Ma (135.1–227.4), in agreement with analyses employing standard substitution rates (stem age 235.6 Ma (142.9–368.5), crown group age 183.8 Ma (109.9–289.1)). The fossil likely belongs to the stem lineage of Radula subg. Odontoradula. The fossil's modern morphology suggests that switches from gymnosperm to angiosperm phorophytes occurred without changes in plant body plans in epiphytic liverworts. The fossil provides evidence for striking morphological homoplasy in time. Even conservative node assignments of the fossil support older rather than younger age estimates of the Radula crown group, involving origins for most extant subgenera by the end of the Cretaceous and diversification of their crown groups in the Cenozoic.
UR  - http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/6583
ER  -