Vaccinium, Linnaeus, 1753

Stults, DZ & Axsmith, BJ, 2015, New plant fossil records and paleoclimate analyses of the late Pliocene Citronelle Formation flora, U. S. Gulf Coast, Palaeontologia Electronica (New York, N. Y.: 1991) 2 (6), pp. 1-35 : 9

publication ID

https://doi.org/ 10.26879/550

persistent identifier

https://treatment.plazi.org/id/039E0517-F664-FFB7-D0CA-3876FBE6F8C1

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Felipe

scientific name

Vaccinium
status

 

Genus VACCINIUM Linnaeus, 1753 View in CoL Vaccinium sp.

Figure 2.7–2.8 View FIGURE 2

Description. One mostly complete, simple, petiolate, elliptic, symmetrical leaf, 4 cm long, 1.7 cm wide (L:W ratio 2:1) is attributed to Vaccinium . Margin is unlobed, apically serrate. The base and apex are acute. Primary framework is pinnate. Secondary venation is brochidodromous. The secondary veins are regularly spaced, noticeably thickened, and form angles approximately 45° from the midrib. Veins of a gauge between secondary and tertiary thicknesses (but not intersecondaries) form loops off the secondary veins toward the basal end, a common feature in extant Vaccinium species. Tertiary veins are irregular, reticulate. Teeth on the apical portion of the leaf are few and small, sinuses angular, straight proximally and distally. The presence of these few, small apical teeth occur in several extant species of Vaccinium (such as some morphotypes of V. corymbosum and V. tenellum ).

Site occurrence. Scarborough School.

Remarks. Vaccinium has 25 recognized species in North America, most of which occur in the west. However, five species occur in the warmer southeastern portion of the continent ( V. crassifolia , V. darrowii , V. hirsutum , V. myrsinites , and V. tenellum ). Fossil leaves of Vaccinium were listed as a possible component of the Miocene Clarkia flora of Idaho ( Smiley and Rember, 1985) and have been identified from the Miocene Succor Creek flora of Oregon ( Fields, 1996).

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