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Staminate inflorescences with in situ pollen from Eocene Baltic amber reveal high diversity in Fagaceae (oak family)

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WILLDENOWIA
卷 50, 期 3, 页码 405-517

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BOTANISCHER GARTEN & BOTANISCHE MUSEUM BERLIN-DAHLEM
DOI: 10.3372/wi.50.50303

关键词

Baltic amber forest; Castaneoideae; Eotrigonobalanus; Fagaceae; Formanodendron doichangensis; Quercus sect; Lobatae; Quercus sect; Protobalanus; palaeobotany; palaeoecology; palynology; Trigonobalanus verticillata

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Eocene Baltic amber forms the largest amber deposit worldwide; however, its source vegetation and climate are much debated. Representatives of the oak family (Fagaceae) were abundant in the Baltic amber source area based on numerous inclusions of staminate inflorescences or individual florets, previously assigned to Castanea and Quercus. However, the actual generic and infrageneric diversity of Fagaceae from Baltic amber remained unknown. Using flower characteristics and section-diagnostic in situ pollen of staminate inflorescences and detached floret inclusions, we describe 18 fossil-species of Fagaceae making this family by far the most diverse plant family preserved in Baltic amber. We substantiate the occurrence of the Castaneoideae, Quercoideae (Quercus sect. Cyclobalanopsis/Lobatae; Q. sect. Lobatae; Q. sect. Protobalanus), Trigonobalanoideae and the extinct genus Eotrigonobalanus. Among the 18 fossil-species, six are described as new: Q. aimeeana, Q. casparyi, Q. multipilosa, E. campanulata, E. conwentzii, E. longianihera; and one new combination is published: Q. brachyandra ( Castanea brachyandra). In addition, a lectotype is designated for the name Quercites meyerianus and neotypes arc designated for the names Castanea inclusa and Quercus longistaminea ( C. longistaminea). Members of the Fagaceae probably inhabited azonal and zonal vegetation types of the amber source area, including bottomland flood-plains and stream banks (Q. sect. Lobatae), dry habitats (Q. sect. Lobatae, Q. sect. Protobalanus), peaty soils, riparian and swamp forests (Castanopsis, Eotrigonobalanus), as well as mixed mesophytic forests (castaneoids, Quercoideae, trigonohalanoids). Affinities to extant North American and E to SE Asian floras support the recent notion that late Eocene Baltic amber (38-34 Ma) was formed in a warm-temperate climate.

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