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:BDB6EAEC-0C87-79B6-B9D9-DE3F94B81388 species
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Mespilodaphne precoushatta

Mespilodaphne precoushatta E.W. Berry Profess. Pap. U.S. Geol. Surv., 132(E): 91. 10 Apr 1924
Name
Mespilodaphne precoushatta
Rank
Species
Generic Name
[Genus] Mespilodaphne
Authors (Pub.)
Berry E. W.  
Publication
An early Eocene florule from central Texas [1924/4]
Journal
Professional Papers / United States Geological Survey
Volume
132
Issue
E
Page number
91
Year
1924
Fossil Status
leaves
Stratigraphy
Ypresian
Location
Sayersville, Bastrop County, Texas, USA
Paleoregion
America (North)
Data for Not defined
Repository
National Museum of Natural History, Smithsonian Institution, Washington, USA
Repository Number
?
Diagnosis
Leaves of medium size; relatively broad, oval in general outline, widest medianly, and tapering about equally to the apex and base. Apex cuneate. Base acute. Margins entire, rather regularly and evenly rounded. Texture coriaceous. Length about 9.25 centimeters, maximum width about 4.1 centimeters. Petiole long and stout, about 2 centimeters in length. Midrib stout, prominent. Secondaries mediumly stout and prominent, eight or nine somewhat irregularly spaced pairs; closely spaced and opposite in the base, less closely spaced and subparallel to about the middle, above which they are about twice as far apart; they diverge from the midrib at angles of more than 45° and are camptodrome in the marginal region. Occasionally a subsecondary runs midway between and subparallel to the adjacent secondaries in the apical part of the leaf, where the true secondaries are more widely spaced, and one basal secondary shows abnormal branching. An apparently characteristic feature of this species is the crowding of the lower secondaries in the basal part of the leaf. The tertiaries are thin, transverse, and either percurrent or anastomosing.

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