Lemna
publication ID |
https://doi.org/ 10.37520/fi.2023.004 |
persistent identifier |
https://treatment.plazi.org/id/4D2487A3-EF53-826F-FEEE-FB2B6BFBFED8 |
treatment provided by |
Felipe |
scientific name |
Lemna |
status |
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Genus Lemna View in CoL L.
Text-fig. 4e View Text-fig
M a t e r i a l. USNM PAL 620300.
L o c a l i t y. Park.
D e s c r i p t i o n. Leaves 0.9 mm long, 0.5–0.6 mm wide; elliptical; aerenchyma present; pseudoroot 0.4 mm long, 0.2 mm wide with slanted terminus.
R e m a r k s. The small size, elliptical leaves, presence of a pseudoroot and lack of venation are characters of the aquatic araceous subfamily, Lemnoideae. The lack of brown pigment cells, which we might expect to preserve in these cellularly preserved compressions (and which do preserve in the Spirodela fossils), rules out its placement in Spirodela or Landoltia and the broad elliptical shape of the fronds contrasts with the more narrow ellipses of Wolffia HORKEL ex SCHLEID and the narrow fronds of Wolfiella ( Armstrong 2021) . Note the name of the distinctive surficial cells is brown pigment cells. While they are brown in modern plants we would not necessarily be able to determine the color in the fossils. Thus, the leaf shape and lack of brown pigment cells support the placement of this specimen in Lemna . In North America, Lemna fossils are known from the Miocene of Mississippi ( McNair et al. 2019). The Kishenehn fossils are the oldest record of Lemna , predating Oligocene occurrences in Eurasia ( Dorofeev 1963). Another notable occurrence of Cenozoic Lemnoideae is that of the Limnobiophyllum leaf and root fossils from the Late Cretaceous through Oligocene of western North America ( Hoffman 1995, Kvaček 1995, McIver and Basinger 1993, Stockey et al. 1997). Limnobiophyllum differs from our fossils by having veined leaves, branching roots and size (leaves are 1–2 cm wide) ( Kvaček 1995, Stockey et al. 1997).
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