Gleditsia aff. caspica DESF., 1809
publication ID |
https://doi.org/ 10.37520/fi.2022.009 |
persistent identifier |
https://treatment.plazi.org/id/03B187AD-FFB4-FFF8-CFB3-FA2AFD4A4A06 |
treatment provided by |
Felipe |
scientific name |
Gleditsia aff. caspica DESF., 1809 |
status |
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Gleditsia aff. caspica DESF., 1809 View in CoL
Text-figs 4h–k View Text-fig , 5a View Text-fig
M a t e r i a l. Oriolo MSF 787, 847, 910-1, 914-1, 915-1, 917-1, 918-1, 919-1, 920-1, 922-1, 923, 925, 926, 927, 928, 929, 931, 932, 933, 934, 935, Santa Lucia delle Spianate MSF n.n.
D e s c r i p t i o n. Leaflet, petiolate, petiole very short, lamina asymmetrical, broad to narrow elliptical, 12–27 mm long, 6–17 mm wide, secondary venation brochidodromous, small veins departing from secondary veins enter small crenulations, margin crenulate.
R e m a r k s. Givulescu (1979: 102, pl.41, fig.14) assigned a leaflet from Late Miocene strata of Chiuzbaia ( Romania), very similar to the material from Oriolo, to Gleditsia allemanica HEER, 1859 . According to Givulescu (1979), G. allemanica was present in middle and Late Miocene floras of Germany, Hungary, Romania and Ukraine. Recently, well-preserved leaflets of Gleditsia have been reported from Late Miocene and Pliocene localities in Poland and Germany. Worobiec and Worobiec (2019) reported Gleditsia europaea G. WOROBIEC, 2019 , from the Bełchatów Lignite Mine ( Poland), which they considered most closely related to the modern North American species G. aquatica MARSHALL, 1785 . From the Pliocene of Frankfurt, Kvaček et al. (2020) reported Gleditsia pliocaenica KVAČEK, TEODORIDIS et DENK, 2019 , which they compared to the western Eurasian G. caspica . The Pliocene specimens are very similar to the material from Oriolo.
Leaflets of Gleditsia differ from the Neogene extinct genus Podocarpium ( Herendeen 1992) by their crenulate margin.
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