“…This plant material includes well-preserved, decimetrelong foliage, shoots, stem fragments, fructifications, cuticle sheets and dispersed seeds. The plant taxa consist of ginkgophytes (50%: Baiera Braun, 1843, Sphenobaiera Florin, 1936), conifers (40%: Ortiseia Florin, 1964, Quadrocladus Schweitzer, 1960, Pseudovoltzia Florin, 1927, Dolomitia Clement-Westerhof, 1987, taeniopterids (2%: Taeniopteris Brongniart, 1828), seed ferns (1%: Germaropteris Kustatscher et al, 2014, Sphenopteris (Brongniart) Sternberg, 1825), and sphenophytes (< 1%) (Clement-Westerhof, 1984, 1987Poort and Kerp, 1990;Visscher et al, 2001;Bauer et al, 2014;Kustatscher et al, 2012Kustatscher et al, , 2014Kustatscher et al, , 2017. The fossiliferous horizon above the marine horizon ('Flora B' in Kustatscher et al, 2017) yielded fragmentary plant remains (debris), but with exceptionally well-preserved cuticles mostly of gymnosperms (conifers, seed ferns).…”