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Lobonotus brazosensis
Taxonomy
Lobonotus brazosensis was named by Stenzel (1935). It is a 3D body fossil. Its type locality is Whiskey Bridge Decapods, which is in an Eocene carbonate marl in the Crockett Formation of Texas.
It was corrected as Lobonotus brazoensis by Schweitzer et al. (2002); it was misspelled as Lobonotus brazoensis by Schweitzer et al. (2007) and Schweitzer et al. (2010).
It was corrected as Lobonotus brazoensis by Schweitzer et al. (2002); it was misspelled as Lobonotus brazoensis by Schweitzer et al. (2007) and Schweitzer et al. (2010).
Synonymy list
Year | Name and author |
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1935 | Lobonotus brazosensis Stenzel p. 384 |
2002 | Lobonotus brazoensis Schweitzer et al. p. 19 |
2007 | Lobonotus brazoensis Schweitzer et al. p. 7 |
2010 | Lobonotus brazosensis Schweitzer et al. p. 116 |
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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.
†Lobonotus brazosensis Stenzel 1935
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: o = order, c = class | |||||
References: Aberhan 1992, Turnsek 1997 |
Age range: Middle Eocene or 47.80000 to 37.71000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Middle Eocene | USA (Texas) | Lobonotus brazosensis (type locality: 133577) |