The earliest records of internally stratified cyanobacterial and algal lichens from the Lower Devonian of the Welsh Borderland

• Published in: The New phytologist 2013-01, Vol.197 (1), p.264-275
• Main Authors: Honegger, Rosmarie, Edwards, Dianne, Axe, Lindsey
• Format: Article
• Language: English
• Subjects: Algae; Aquatic plants; Ascomycota; Ascomycota - classification; Ascomycota - cytology; Biological Evolution; Cambrian; Cell Wall - ultrastructure; charcoalification; Chlorolichenomycites salopensis; Chlorophyta - classification; Chlorophyta - cytology; Continental margins; Cretaceous; Cyanobacteria; Cyanobacteria - classification; Cyanobacteria - cytology; Cyanolichenomycites devonicus; Devonian; Electron microscopy; fossil lichen; fossil Nostoc; Fossils; Fruit bodies; Fungi; heteromerous lichen; Hyphae; Hyphae - ultrastructure; Lichens; Lichens - classification; Lichens - cytology; Lochkovian strata; Microscopy, Electron, Scanning; Microscopy, Electron, Transmission; Nutrition; Phylogeny; Plants; Pycnidia; pycnidial conidioma; Records; Scanning electron microscopy; Species Specificity; Spores; Spores, Fungal - ultrastructure; Stratification; Symbionts; Symbiosis; Thalli; Thallus; Triassic; Wales
• ISSN: 0028-646X; 1469-8137
• DOI: 10.1111/nph.12009

Lichenization is assumed to be a very ancient mode of fungal nutrition, but fossil records are rare. Here we describe two fragments of exceptionally preserved, probably charred, lichen thalli with internal stratification. Cyanolichenomycites devonicus has a cyanobacterial and Chlorolichenomycites salopensis a unicellular, presumably green algal photobiont. Fruiting bodies are missing. Cyanolichenomycites devonicus forms asexual spores in a pycnidium. All specimens were examined with scanning electron microscopy techniques. The fossils were extracted by maceration. Extant lichens and free-living cyanobacteria were either experimentally charcoalified for comparison or conventionally prepared. Based on their septate hyphal structure, both specimens are tentatively interpreted as representatives of the Pezizomycotina (Ascomycota). Their presence in 415 million yr (Myr) old rocks from the Welsh Borderland predates existing Late Cretaceous records of pycnidial conidiomata by some 325 Myr and Triassic records of lichens with broadly similar organization by some 195 Myr. These fossils represent the oldest known record of lichens with symbionts and anatomy as typically found in morphologically advanced taxa today. The latter does not apply to Winfrenatia reticulata, the enigmatic crustose lichen fossil from the Lower Devonian, nor to presumed lichen-like organisms such as the Cambrian Farghera robusta or to the Lower Devonian Spongiophyton minutissimum.