Back
Rhus asymmetrica
Rhus asymmetrica Tosal, J. Sanjuan, Mart.-Closas Rev. Palaeobot. Palynol., 2019, 261: 69. 28 Nov 2018
- Name
- Rhus asymmetrica
- Rank
- Species
- Generic Name
- [Genus] Rhus
- Authors (Pub.)
- Tosal A.
Sanjuan J.
Martín-Closas C.
- Publication
- Foliar adaptations of Rhus asymmetrica sp. nov. from the Oligocene
of Cervera (Catalonia, Spain). Palaeoclimatic implications [2018/11]
- Journal
- Review of Palaeobotany and Palynology
- Annee/Jahrgang
- 2019
- Volume
- 261
- Page number
- 69
- Year
- 2018
- Fossil Status
- leaves
- Stratigraphy
- Rupelian
- Strat. comment
- 32.4 Ma
- Location
- Sant Pere dels Arquells site, Cervera, eastern Ebro Basin, comarca of Segarra, Province of Lleida, Autonomous Community of Catalonia, Spain
- Paleoregion
- Eurasia (Europe)
Data for Holotypus
- Repository
- Sorbonne Université, Faculté des Sciences et Ingénierie, Paris, France
- Repository Number
- UPMC n5737a
Data for Paratypus
- Repository
- Museu de Ciències Naturals de Barcelona, Barcelona, Spain
- Repository Number
- MGB 84946–MGB 84948 (Plate I, 1–3); MGB 84964-MGB 84967 (Plate II, 1–4)
- Diagnosis
- Trifoliate leaves. Apical leaflet symmetric and elliptic in shapewith a
serrate margin, largely decurrent base, no petiolule and an acute apex.
Primary venation of the apical leaflet pinnate. Secondary vein framework
craspedodromous, without branching. Major secondary vein attachment
to the midvein decurrent. Intercostal tertiary vein fabric irregular reticulate. Exterior tertiary course andmarginal ultimate venation looped. Lateral leaflets basal asymmetric and ovate in shape, with an unequally
serrate margin, rounded base in the distal part and concave or straight base proximally, no petiolule and an acute apex. Primary vein framework of the lateral leaflet pinnate with only one basal vein. Secondary venation pattern craspedodromous. One of the first secondary vein pairs basal. Attachment of secondary veins to the midvein decurrent. Intercostal tertiary vein fabric irregular reticulate. Exterior tertiary course and marginal ultimate venation looped.