Sphenopteris mira KIDST., 1923

Cleal, Christopher J., Strullu-Derrien, Christine & Spencer, Alan R. T., 2024, Early Coal Swamp Vegetation From The Serpukhovian Lower Clackmannan Group Of Scotland, Fossil Imprint 80 (1), pp. 35-67 : 49

publication ID

https://doi.org/10.37520/fi.2024.006

persistent identifier

https://treatment.plazi.org/id/03A187BC-B037-FFAE-74C0-FF2F52D2FCAD

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Felipe (2025-01-20 01:33:08, last updated 2025-01-23 01:21:11)

scientific name

Sphenopteris mira KIDST., 1923
status

 

Sphenopteris mira KIDST., 1923

Text-fig. 7d

1923 Sphenopteris mira KIDST. , p. 138, pl. 30, fig. 2.

D e s c r i p t i o n. A single specimen showing part of a bipinnate segment. Pinnules alternately attached to ultimate rachis; pinnules small, subrhomboidal, 3‒5 mm long, each with 3‒6 narrow linear segments. A single vein enters each pinnule segment.

R e m a r k s. Only one specimen of this small-pinnuled species is known from Scotland ( Kidston 1923: pl. 30, fig. 2) but it has also been described from the Serpukhovian of Upper Silesia ( Purkyňová 1970). There are no distinctive features that allow it to be definitely placed in a particular fossil-genus and so provisionally it has been retained in its original fossil-genus.

O c c u r r e n c e. Rare in Upper Limestone Formation, only reported from below the Orchard Limestone at New Braidbar Quarry, Renfrewshire.

Kidston, R. (1923): Fossil plants of the Carboniferous rocks of Great Britain. Parts 1 - 4. - Memoirs of the Geological Survey of Great Britain, Palaeontology, 2: 1 - 376.

Purkynova, E. (1970): Die Unternamurflora des Beckens von Horni Slezsko (CSSR). - Palaontologische Abhand- lungen, Abt. B, 3: 129 - 268.