Carya cf. minor SAPORTA , 1873
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https://doi.org/10.37520/fi.2022.009 |
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https://treatment.plazi.org/id/03B187AD-FFAD-FFE2-CD67-FB0DFBDD495D |
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Felipe (2022-10-08 21:08:06, last updated by Plazi 2023-11-07 16:12:01) |
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Carya cf. minor SAPORTA , 1873 |
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Text-fig. 9a–e View Text-fig
1873 Carya minor SAPORTA , p. 217.
1876 Juglans minor (SAPORTA) SAPORTA et MARION , p. 166, pl. 37, figs 1–6.
1970 Carya cf. minor SAPORTA ; Pavia, pl. 3, fig. 5.
2001 Carya cf. minor SAPORTA ; Martinetto and Sami, p. 17, textfig. 10.
M a t e r i a l. Oriolo MSF 631, 631-1, 631-2, 634, 634-1, 635, 639, 690, 691, 755, 756, 757-1, 758, 759, 760, 761, 762, 763, 764, 765, 766, 767, 768, 769, 770, 771, 772, 773, 774, 775, 777.
D e s c r i p t i o n. Leaflet, petiolate, petiole <2 mm long, lamina elliptic, ovate or obovate, 39–124 mm long, 18–57 mm wide, base cuneate decurrent, acute rounded, apex acute or acuminate, secondary venation mixed brochidodromous, semicraspedodromous, secondary veins branching close to leaf margin or rarely close to primary vein, secondary veins and intersecondary veins spaced 2–4 per 1 cm primary vein, margin sharply serrate.
R e m a r k s. The material from Oriolo is closely similar to leaves/leaflets of C. minor from the Pliocene of Meximieux ( France) and Willershausen ( Germany) in some instances (densely spaced, regular secondaries forming a brochidodromous pattern of loops), while other leaflets have a more irregular pattern of secondary veins. From Miocene strata of France and Crete, Kvaček et al. (2011) and Zidianakis et al. (2020) described dispersed leaves and leaflets of Carya as Carya sp. , accounting for differences in secondary venation with known western Eurasian Neogene species of Carya . Pavia (1970) reported a very similar leaflet from Arboschio (Pliocene).
Kvacek, Z., Teodoridis, V., Roiron, P. (2011): A forgotten Miocene mastixioid flora of Arjuzanx (Landes, SW France). - Palaeontographica, Abt. B, 285: 3 - 111. https: // doi. org / 10.1127 / palb / 285 / 2011 / 3
Pavia, G. (1970): Resti di Anancus arvernensis e flore ad affinita plioceniche nel Villafranchiano inferiore della cava Arboschio (Villafranca d'Asti) [Remains of Anancus arvernensis and floras with Pliocene affinities in the lower Villafranchian of the Arboschio quarry (Villafranca d'Asti)]. - Memorie della Societa Geologica Italiana, 9: 157 - 176. (in Italian)
Saporta, G. de (1873): Sur les caracteres propres a la vegetation pliocene, a propos des decouvertes de M. J. Rames, dans le Cantal. - Bulletin de la Societe Geologique de France, 3 (1): 212 - 231.
Zidianakis, G., Iliopoulos, G., Zelilidis, A., Kovar-Eder, J. (2020): Three (middle to) late Miocene plant macroremain assemblages (Pitsidia, Kassanoi and Metochia) from the Messara-Gavdos region, southern Crete. - Acta Palaeobotanica, 60: 333 - 437. https: // doi. org / 10.35535 / acpa- 2020 - 0018
Text-fig. 9. a–e: Carya aff. minor. a: Terminal leaflet, Oriolo MSF 755. b: Oriolo MSF 755. c: Oriolo MSF 766. d: Oriolo MSF 768. e: Oriolo MSF 635. f, g: Pterocarya aff. fraxinifolia. f: Fruit, Oriolo MSF 632. g: Leaflet, Oriolo MSF 632a. h–j: Alnus aff. glutinosa subsp. barbata. h: Oriolo MSF 852. i: Oriolo MSF 850. j: Seed cone, Oriolo MSF 987. k–o: Corylus aff. avellana. k: Leaf, Oriolo MSF 841. l: Fruit, Oriolo MSF 1001. m: Fruit, Oriolo MSF 1022. n: Fruit, Oriolo MSF 1003. o: Fruit, Oriolo MSF 1022. Scale bars 50 mm (a–e, g–i), 10 mm (f, j–o).
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