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Hemipatagus subrostratus
Taxonomy
Hemipatagus subrostratus was named by Clark and Twitchell (1915). It is a 3D body fossil. Its type locality is City quarry near cemetery, Wilmington, which is in an Eocene marine marl in the Jackson Formation of North Carolina.
It was recombined as Maretia subrostratus by Kier (1980).
It was recombined as Maretia subrostratus by Kier (1980).
Sister species lacking formal opinion data
Synonymy list
Year | Name and author |
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1915 | Hemipatagus subrostratus Clark and Twitchell p. 151 figs. Plate LXIX, Figs. 2a-b |
1942 | Hemipatagus subrostratus Cooke p. 53 |
1980 | Maretia subrostratus Kier p. 49 |
2007 | Hemipatagus subrostratus Kroh p. 190 |
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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.
†Hemipatagus subrostratus Clark and Twitchell 1915
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: o = order, c = class, p = phylum | |||||
References: Kiessling 2004, Aberhan 1992 |
Age range: base of the Bartonian to the top of the Late/Upper Eocene or 41.03000 to 33.90000 Ma
Collections (2 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Bartonian | USA (North Carolina) | Hemipatagus subrostratus (5436) | |
Late/Upper Eocene | USA (North Carolina) | Hemipatagus subrostratus (type locality: 142965) |