Gaylussacia sp.

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-D2E0-3E9DFC21FCEA

treatment provided by

Felipe

scientific name

Gaylussacia sp.
status

 

Gaylussacia sp.

Figure 2.5 View FIGURE 2

Description. One simple, 2.4 cm long, 1.0 cm wide, petiolate leaf displays characteristics of Gaylussacia . The petiole is very short (~ 1 mm long) with a significant expansion near the stem. The blade is obovate, symmetrical. Margin is unlobed and entire. Base is acute, cuneate. Apex is obtuse, rounded. Primary venation is pinnate. Secondary venation is brochidodromous and decurrent. Secondaries form long and irregularly spaced loops that depart the midvein at angles of 20–30°, the angles increasing to approximately 45° distally. Tertiary venation is reticulate.

Site occurrence. Scarborough School.

Remarks. Of the approximately 50 species of Gaylussacia worldwide, most of the North American species occur on the southeastern coastal plain, including G. baccata , G. dumosa , G. frondosa ( Figure 2.6 View FIGURE 2 ), G. mosieri , G. nana , and G. tomentosa . The Citronelle Formation leaf described here is the first report of fossil Gaylussacia in North America. The unique, disjunct biogeographical pattern of Gaylussacia (it is present in eastern portions of North America and South America) is most commonly explained as a probable origination in South America with subsequent migration into North America during the Paleogene via the Caribbean islands. However, molecular approaches suggest that the genus originated in North America and subsequently expanded into South America ( Floyd, 2002).

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF