Trigonobalanopsis rhamnoides (ROSSMÄSSLER) KVAČEK et WALTHER
publication ID |
https://doi.org/ 10.5281/zenodo.13183351 |
persistent identifier |
https://treatment.plazi.org/id/C64487CC-FFDC-FF99-FCB7-FE6B310518DD |
treatment provided by |
Felipe |
scientific name |
Trigonobalanopsis rhamnoides (ROSSMÄSSLER) KVAČEK et WALTHER |
status |
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Trigonobalanopsis rhamnoides (ROSSMÄSSLER) KVAČEK et WALTHER
Pl. 7, fig. 7
1988 Trigonobalanopsis rhamnoides (ROSSMÄSSLER) KVAČEK et WALTHER , p. 405, pl. 2, figs 1-8, pls 50-54, pl. 55, figs 2-7, pl. 56, figs 1-4, pl. 57, text-figs 2-4.
Leaves petiolate, incompletely preserved, lamina narrow elliptical, base cuneate, margin entire, venation brochidodromous, midrib straight, secondaries very regularly disposed, bent, subparallel, at an angle of ca. 35°. Higher-order venation not preserved.
D i s c u s s i o n: This extinct member of the Fagaceae has been usually recognized mainly according to its rhamnoid venation ( Phyllites rhamnoides ROSSM. ). Its occurrences in the Eocene are rare ( Knobloch et al 1996). In the volcanic facies Trigonobalanopsis was usually poorly represented (Rott, as Rhamnus dechenii WEBER ) while it was a dominant element in the Miocene mastixioid floras ( Kvaček and Walther 1988). The occurrence of rare specimens at Kučlín is quite exceptional outside the Late Eocene riparian vegetation in the Bohemian Massif.
M a t e r i a l: KIN 372.
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