Pseudotremia valga Loomis
publication ID |
https://doi.org/ 10.5281/zenodo.279260 |
DOI |
https://doi.org/10.5281/zenodo.6186459 |
persistent identifier |
https://treatment.plazi.org/id/03C47A60-FFC9-725E-60C0-5C9F7DEB7FFE |
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Pseudotremia valga Loomis |
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Pseudotremia valga Loomis View in CoL
Figs. 85–90 View FIGURES 80 – 85 View FIGURES 86 – 91
P. v a l g a Loomis 1943, p. 377. Shear, 1972, p. 173.
Type locality: “King Solomon’s Cave,” Lee Co., VIRGINIA. Male holotype in MCZ.
New records: VIRGINIA: Lee Co.: Smith Cave, 6 mi ESE of Rose Hill, 19 July 1979, J. Holsinger, 3, ƤƤ; 21 April 1973, D. Culver et al., 3; Cumberland Gap Saltpetre Cave, 1.4 mi NE Cumberland Gap, 15 July 1979, J. Holsinger, m.
Notes: “King Solomon’s Cave” was cited by Loomis in the original description as being located in Cumberland Gap, Claiborne Co., Tennessee. However, the former “King Solomon’s Cave” is now known as Cudjo’s Cave, or Gap Cave, and is located in Lee Co., Virginia. The town of Cumberland Gap is in Virginia. The cave is operated as a tourist attraction by Cumberland Gap National Historical Park. The first collection of this species was made in 1924 ( Loomis 1943) and Barr collected a male at the type locality in 1958 ( Shear 1972). Pseudotremia valga is a troglophile, well-pigmented and with 20–22 black ocelli. A typical metazonite (figs. 88, 90), the gonopods (figs. 86, 89) and right ninth leg (fig. 87) are illustrated here.
MCZ |
Museum of Comparative Zoology |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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