International audience[No abstract available

The number of available liverwort fossils substantially increased within the past decade, which is mainly due to new findings from Cretaceous and Cenozoic amber deposits. Many of them, however, are fragmentary and not predestined for consideration in evolutionary analyses. Here, we list those liverwort fossils that we suggest as suitable for calibrating phylogenetic reconstructions, along with brief descriptions, justification of their use, and age information. Our recommendations are based on thorough microscopic investigation of available fossils from worldwide amber collections including recent findings. We recommend that the following 42 fossil taxa can be used as confident minimum age constraints in phylogenetic reconstructions: Acrolejeunea ucrainica (35 Ma), Anastrophyllum rovnoi (35 Ma), Bazzania polyodus (34 Ma), Blepharolejeunea obovata (15 Ma), the genus Bryopteris with B. bispinosa and B. succinea (15 Ma), Calypogeia stenzeliana (34 Ma), Cephaloziella nadezhdae (35 Ma), the genus Ceratolejeunea with C. antiqua, C. palaeomexicana, and C. sublaetefusca (15 Ma), Cheilolejeunea latiloba (34 Ma), Cheirorhiza brittae (158 Ma), Cololejeunea sp. (15 Ma), Cyclolejeunea archaica (15 Ma), Dibrachiella grollei (15 Ma), Diettertia montanensis (112 Ma), Drepanolejeunea eogena (15 Ma), the genus Frullania with F. baerlocheri, F. cretacea, and F. partita (99 Ma), Frullania subgen. Frullania with F. casparyi (34 Ma) and F. riclefgrollei (35 Ma), F. subgen. Trachycolea with F. rovnoi (35 Ma) and F. schumannii (34 Ma), Gackstroemia cretacea (99 Ma), Geocalyx heinrichsii (34 Ma), the genus Lejeunea with L. hamatiloba, L. miocenica, L. resinata, and L. urbanioides (15 Ma), Lopholejeunea subnigricans (15 Ma), Marchantites cyathodoides (228 Ma), Marchesinia brachiata (15 Ma), Metzgeriothallus sharonae (383 Ma), Microlejeunea nyiahae (52 Ma), Neurolejeunea macrostipula (15 Ma), Nipponolejeunea europaea (34 Ma), Notoscyphus balticus (34 Ma), Odontoschisma (sect. Iwatsukia) dimorpha (34 Ma), Plagiochila groehnii (34 Ma), Porella subgrandiloba (34 Ma), Protolophozia kutscheri (34 Ma), Radula (subgen. Odontoradula) cretacea (99 Ma), R. (subgen. Amentuloradula) heinrichsii (99 Ma), Scapania hoffeinsiana (34 Ma), Solenostoma berendtii (34 Ma), Spruceanthus polonicus (34 Ma), Stictolejeunea squamata (15 Ma), Tetralophozia groehnii (34 Ma), Thysananthus auriculatus (15 Ma), Thysananthus contortus (34 Ma). Furthermore, we transfer Lophozia kutscheri to Protolophozia, Archilejeunea grollei to Dibrachiella, Frullania ucrainica to Acrolejeunea, and Mastigolejeunea extincta to Spruceanthus, based on new fossil evidence and morphological revisions.

No abstract

Three new fossil bryophytes are described from Jurassic and Lower Cretaceous deposits of the Transbaikalia region of Russia. The complex thalloid hepatic Khasurtythallus monosolenioides gen. et sp. nov. belongs to the Marchantiidae, but its combination of characters precludes unequivocal placement in any of the five orders of this subclass, representing most likely an extinct lineage. Paleaethallus squarrosus gen. et sp. nov. is a thalloid plant with scales similar to those of complex thalloid hepatics, although their arrangement and the overall plant structure has little in common with any extant hepatics. Dispersed moss capsules, three of which have attached calyptrae, are described as a form genus Kulindobryum gen. nov. Despite incomplete preservation, some rare characters indicate possible relationship to the genus Tayloria of the Splachnaceae, an extant family of mosses adapted to grow on animal dung, dead bodies and bones. Notably, Kulindobryum co‐occurs with bones of the small feathered dinosaurs Kulindadromeus, which also supports an affiliation of Kulindobryum with the Splachnaceae. The most common and best known Mesozoic moss for the region, the genus Bryokhutuliinia, is appraised for its systematic position and probable affinities with the Dicranales. A scoring approach is introduced for the comparative method of taxonomic placement of fossils with partial suites of morphological characters at the family or order level.

No abstract

No abstract

No abstract

No abstract