Arcellites punctatus E.M.Friis, K.R.Pedersen et Marone
Plant Fossil Names Registry Number: PFN002844
Act LSID: urn:lsid:plantfossilnames.org:act:2844
Authors: E. M. Friis, K. R. Pedersen & F. Marone
Rank: species
Genus: Arcellites E.L.Miner
Reference: Friis, E. M., Pedersen, K. R. & Marone, F. (2014): Arcellites punctatus sp. nov.: a new megaspore from the Early Cretaceous of Portugal studied using high resolution synchrotron radiation X-ray tomographic microscopy (SRXTM). – Grana 53(2): 91–102.
Page of description: 93
Illustrations or figures: figs 1–5
Types
Holotype S170173, Palaeobotanical Collections, Department of Palaeobiology, the Swedish Museum of Natural History, Stockholm, Sweden
Figures: figs 1A, 6A, B
Note: Holotype from sample Torres Vedras 43.
Paratypes: S170218, S170219, S171531–S171533, S174135–S174140 (sample Torres Vedras 38); S174141 (sample Torres Vedras 39); S174142 (sample Torres Vedras 40); S170169–S170172, S174097 (sample Torres Vedras 43); S174134 (sample Torres Vedras 46); S174133 (sample Torres Vedras 143); S174123–S174132 (sample Torres Vedras 144).
Original diagnosis/description
Arcellites megaspore with prominent six-parted acrolamella. Megaspore trilete. Megaspore body spherical with an open, coarsely rugulate surface formed from broad, rounded ridges; outer megaspore wall smooth lacking body appendages. Segments of acrolamella laminar with membranous, crenulate or serrate outer margin. Megaspore wall over the megaspore body three-layered; inner layer thin, of even thickness; middle layer granular-fibrous of uneven thickness causing the rugose surface pattern; outer layer solid, of more or less even thickness, perforated by short, narrow canals that extend almost to the middle layer. Canals straight, of uneven length and distribution with most canals in the valleys between and along the flanks of the rounded ridges; canals absent or scattered over the ridges. Acrolamella extends from outer layer. Microspores adhering to the acrolamellae are trilete with raised proximal region, more or less circular outline, and a psilate-perforate, sometimes faintly rugulate surface.
Etymology
From the distinctive punctate, perforated wall ultrastructure.
Stratigraphy
Cretaceous, Lower Cretaceous
Fluviatile cross-bedded sands with intercalated clay beds and darker organic rich horizons (Almargem Formation); Late Barremian–Aptian
Locality
Portugal
Torres Vedras (39° 06′ 13″ N; 009° 06′ 44″ W)
Plant fossil remain
pollen and spores
Comments
Use comments to notify PFNR administrators of mistakes or incomplete information relevant to this record.