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Euproteaciphyllum pinnatum
Taxonomy
Euproteaciphyllum pinnatum was named by Carpenter et al. (2012). It is considered to be a form taxon. Its type specimen is Holotype: OU33344, Geology Museum, University of Otago, Dunedin, NZ, a leaf (Cuticle), and it is a compression fossil. Its type locality is F45/f0394, middle Gore Lignite Measure, Newvale Mine, which is in an Oligocene/Miocene mire/swamp lignite in New Zealand.
Synonymy list
Year | Name and author |
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2012 | Euproteaciphyllum pinnatum Carpenter et al. p. 383 fig. 5 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Euproteaciphyllum pinnatum Carpenter et al. 2012
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Diagnosis
Reference | Diagnosis | |
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R. J. Carpenter et al. 2012 | Foliage pinnately lobed. Lobes small, more-or-less triangular or falcate. Stomatal distribution more-or-less parallel, subsidiary cells typically appearing butterfly-winged. Anticlinal epidermal wall cuticle variably buttressed and sinuous at junctions with periclinal walls. Trichome bases common on both leaf surfaces, associated with two or more epidermal cells. |
Measurements
No measurements are available
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Source: p = phylum | |||||
Reference: Kiessling 2009 |
Age range: base of the Late/Upper Oligocene to the top of the Early/Lower Miocene or 28.40000 to 15.97000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Late/Upper Oligocene - Early/Lower Miocene | New Zealand (Southland) | Euproteaciphyllum pinnatum (type locality: 169981) |