Sassafras albidum ( Nuttal, 1818 ) Nees von Esenbeck, 1836

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 : 12-14

publication ID

https://doi.org/10.26879/550

persistent identifier

https://treatment.plazi.org/id/039E0517-F667-FFB2-D01C-3DEEFDF9FB57

treatment provided by

Felipe (2024-08-11 01:53:16, last updated 2024-08-12 13:25:36)

scientific name

Sassafras albidum ( Nuttal, 1818 ) Nees von Esenbeck, 1836
status

 

Sassafras albidum ( Nuttal, 1818) Nees von Esenbeck, 1836 View in CoL

Figure 4.4 View FIGURE 4

Description. One bilobed leaf is attributed to Sassafras albidum . The overall outline is ovate with one lateral lobe. The original leaf was> 7 cm long. The main lobe has a width of 3 cm, whereas the lateral lobe is 1.5 cm wide. The base is missing. The apex of the central lobe is missing, but was probably rounded or acute. The apex of the lateral lobe is acute. It is difficult to categorize the primary venation, since the major veins to the lobes often do not diverge at the same point in other extant and fossil Sassafras specimens. The majority of S. albidum leaves are suprabasalactinodromous regardless of the number of lobes (usually from 1– 3) (personal observation). In the Citronelle Formation fossil, the primary vein of the lateral lobe is smaller than the primary vein in the main lobe. Secondary veins are brochidodromous, forming long arches departing the midvein at angles of approximately 50–55°. There are many intersecondary veins perpendicular to the midvein in the basal half of the leaf, becoming parallel to the major secondaries in the apical portion. Tertiary veins are mixed percurrent. Quaternary veins are irregular reticulate. A fimbrial vein is evident.

Site occurrence. Perdido Park.

Remarks. There are only two or three modern species of Sassafras , S. albidum being the only species currently in North America. It has a wide distribution over much of the eastern portion of the continent. Sassafras albidum probably diverged from Asian counterparts in the middle Miocene ( Chanderbali et al., 2001; Nie et al., 2008). Fossils of Sassafras have been reported from the western Miocene Clarkia and Succor Creek floras ( Smiley and Rember, 1985; Fields, 1996).

Chanderbali, A. S., van der Werff, H., and Renner, S. S. 2001. Phylogeny and historical biogeography of Lauraceae: evidence from the chloroplast and nuclear genomes. Annals of the Missouri Botanical Garden, 88: 104 - 134.

Fields, P. F. 1996. The Succor Creek Flora of the Middle Miocene Sucker Creek Formation, southwestern Idaho and eastern Oregon: systematics and paleoecology. Unpublished PhD Dissertation. Michigan State University, East Lansing, Michigan, USA.

Nees von Esenbeck, C. G. D. 1836. Systema Laurinarum. Berolini.

Nie, Z-L, Wen, J., Azuma, H., Qui, Y-L, Sun, H., Meng, Y., Sun, W-B, and Zimmer, E. A. 2008. Phylogenetic and biogeographic complexity of Magnoliaceae in the Northern Hemisphere inferred from three nuclear data sets. Molecular Phylogenetics and Evolution, 48: 1027 - 1040.

Nuttal, T. 1818. The Genera of North American Plants and a catalogue of the species, to the year 1817. G. Heartt, Philadelphia.

Smiley, C. J. and Rember, W. C. 1985. Composition of the Miocene Clarkia Flora, p. 175 - 184. In Smiley, C. J. (ed.), Late Cenozoic History of the Pacific Northwest. Pacific Division of the American Association for the Advancement of Science, San Francisco.

Gallery Image

FIGURE 4. Representative Lauraceae from the Citronelle Formation. 1. Lindera sp. leaf (UF 19210–062072), scale bar equals 1 cm. 2. Extant Lindera leaf from USAM herbarium for comparison with Figure 4.1, scale bar equals 1 cm. 3. Persea sp. leaf (UF 19210–062073), scale bar equals 1 cm. 4. Sassafras albidum leaf (UF 19210–062074), scale bar equals 1 cm. 5. Close-up of Figure 4.1 Lindera leaf showing high order venation, scale bar equals 2.5 mm. 6. Close-up of Figure 4.3 Persea leaf showing high order venation, scale bar equals 2.5 mm.

Kingdom

Plantae

Phylum

Tracheophyta

Class

Magnoliopsida

Order

Laurales

Family

Lauraceae

Genus

Sassafras