The INTERNATIONAL FOSSIL PLANT NAMES INDEX
Global registry of scientific names of fossil organisms covered by the International Code of Nomenclature for Algae, Fungi, and Plants and the International Code of Zoological Nomenclature © 2014-2024

IDNAME urn:idName:ifpni.org:species:5DDC4F23-6CFA-1304-5334-8D47767E0FCC species
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Filicites peruanus

Filicites peruanus E.W. Berry Amer. J. Sci., Series 5, 5(27): 244. Mar 1923
Name
Filicites peruanus
Rank
Species
Generic Name
[Genus] Filicites
Authors (Pub.)
Berry E. W.  
Publication
Tertiary plants from the Andes of Cajamarca, Peru [1923/3]
Journal
American Journal of Science
Annee/Jahrgang
Series 5
Volume
5
Issue
27
Page number
244
Year
1923
Fossil Status
foliage
Stratigraphy
Pliocene
Location
tuff outcropping near Jadibamba on the trail between Celendin and Yanacancha, Department of Cajamarca, northern Peru (about Lat. 6°45’ South, Long. 78°25’ West)
Paleoregion
America (South)
Data for Not defined
Repository
National Museum of Natural History, Smithsonian Institution, Washington, USA
Repository Number
USNM PAL 320702
Diagnosis
Fronds at least bipinnate inferring from the inequilateral base of the pinnules, variable in size, somewhat coriaceous in texture. Pinnules ovate, with an acuminate apex and a rounded inequilateral base. Margins entire, regular in the limited amount of material seen. Length ranging from 5 to 15 em. Maximum width, below the middle, ranging from 1 to 4 em. Midvein stout, channeled above and prominent on the under side. Laterals thin but well marked, regularly and closely spaced, subparallel; they diverge from the midvein at acute angles, curving rapidly outward, and pursue nearly straight courses to the margins. In the larger specimens their general angle of divergence from the midvein is about 80°. In the smaller specimens they are more ascending. They are invariably once forked and rarely show a second dichotomy. The forking is usually near the base but there is considerable variation in this feature, frequently the fork is quite a distance above the base, and more rarely it is half way to the margin.

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