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Falcatifolium eocenica
Taxonomy
Falcatifolium eocenica was named by Hill and Scriven (1999). It is considered to be a form taxon. Its type specimen is Holotype: 2350, 2351., a sterile axis (Cuticle), and it is a compression fossil. Its type locality is ALCOA Anglesea Site II coal mine, which is in an Eocene channel mudstone/sandstone in the Demon Bluff Formation of Australia.
Synonyms
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Synonymy list
Year | Name and author |
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1987 | Dacrycarpus eocenica Greenwood p. 116 figs. 6C, 8, 9, 14, 15 |
1999 | Falcatifolium eocenica Hill and Scriven |
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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.
†Falcatifolium eocenica Hill and Scriven 1999
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Invalid names: Dacrycarpus eocenica Greenwood 1987 [objective synonym]
Diagnosis
Reference | Diagnosis | |
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D. R. Greenwood 1987 (Dacrycarpus eocenica) | Foliage dimorphic; distichous leaves bilateral, falcate, decurrent, loosely imbricate leaves strongly keeled, hypostomatic, sto-mata paratetracytic, in orderly rows, non-stomata1 cells rectangular, length : width (L : W) of cells never greater than 1:3. | |
R. S. Hill and L. J. Scriven 1999 | Foliage narrow, bilaterally flattened, curved. Cuticle robust, stomatal polar extensions connect to polar epidermal cells. |
Measurements
No measurements are available
No ecological data are available
Age range: Late/Upper Eocene or 37.71000 to 33.90000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Late/Upper Eocene | Australia (Victoria) | Dacrycarpus eocenica, Falcatifolium eocenica (type locality: 166825) |