New methods reveal oldest known fossil epiphyllous moss: Bryiidites utahensis gen. et sp. nov. (Bryidae)

• Published in: American journal of botany Vol. 100; no. 12; pp. 2450 - 2457
• Main Authors: Barclay, Richard S., McElwain, Jennifer C., Duckett, Jeffrey G., van Es, Maarten H., Mostaert, Anika S., Pressel, Silvia, Sageman, Bradley B.
• Format: Journal Article
• Language: English
• Published: United States Botanical Society of America, Inc 01.12.2013; Botanical Society of America
• Subjects: atomic force microscopy; Biological Evolution; Botany; Bryidae; Bryophyta; Bryophyta - growth & development; Bryophytes; Bryopsida - growth & development; Cretaceous; Dakota Formation; epiphyll; Forests; Fossils; Fungal spores; Geology; Germination; Lauraceae; Microscopy - methods; Mosses; North America; Paleobotany; Phylogeny; Plant cells; Plant Leaves; Plants; protonema; Scanning electron microscopy; Spore germination; Spores; Trees; Tropical Climate; North America; paleobotany; Bryophyta; Dakota Formation; epiphyll; Cretaceous; Lauraceae; atomic force microscopy; protonema
• ISSN: 0002-9122; 1537-2197
• DOI: 10.3732/ajb.1300209

Premise of the study: Epiphyllous bryophytes are a highly characteristic feature of many humid tropical forest ecosystems. In contrast to the extensive fossil record for the leaves of their host plants, the record is virtually nonexistent for the epiphylls themselves, despite a fossil record for mosses that begins in the Middle Carboniferous Period, 330 million years ago. Methods: Epifluorescence optical microscopy, scanning electron microscopy, and atomic force microscopy were employed to investigate an intimate association between a newly discovered epiphyllous moss and a Lauraceae plant host from the middle Cretaceous. Key results: We describe the oldest fossil specimen of an epiphyllous moss, Bryiidites utahensis gen. et sp. nov., identified from an individual specimen only 450 μm long, situated on an approximately one millimeter square fossil leaf fragment. The moss epiphyll is exquisitely preserved as germinating spores and short-celled protonemata with transverse and oblique cross-walls closely matching those of extant epiphyllous mosses on the surface of the plant-leaf hosts. Conclusions: The extension of the epiphyll record back to the middle Cretaceous provides fossil evidence for the appearance of epiphyllous mosses during the diversification of flowering plants, at least 95 million years ago. It also provides substantive evidence for a tropical maritime climate in central North America during the middle Cretaceous.