Wandella diamentina Gray 1994
publication ID |
https://doi.org/ 10.1080/00222933.2016.1181805 |
publication LSID |
lsid:zoobank.org:pub:327D7F9C-1ACC-4323-9D03-8D3A7B2E83D8 |
DOI |
https://doi.org/10.5281/zenodo.5195201 |
persistent identifier |
https://treatment.plazi.org/id/03E487C6-4C5C-6C50-FE0C-ECBEFDB71B24 |
treatment provided by |
Plazi |
scientific name |
Wandella diamentina Gray 1994 |
status |
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Wandella diamentina Gray 1994 View in CoL
( Figures 15 View Figure 15 , 30 View Figure 30 , 31 View Figure 31 )
Wandella diamentina View in CoL
Gray 1994, p. 56, figs 7, 87 – 91, 105, 106. Holotype female from Wyralah Station, southwest of Winton, Queensland, 22°46' S, 142°22' E, 15/VII/1981, A. Rozefelds, under rock, deposited in QM S6751, not examined.
Note
I have examined females from near the type locality with a similar somatic and genital morphology to the holotype, but bearing pores in the outer spermathecae. Judging by Gray ’ s illustrations (1994, figs. 105, 106) and his statement about the lack of glands in the outer spermathecae, it might be that the holotype is a not yet fully adult female. I here illustrate one of these females from near the type locality ( Figures 30 View Figure 30 C, 31A) in the hope that it might assist in recognizing the species, as it is hitherto known from a single female and two immatures.
Distribution
Southwestern
Australia.
Queensland
( Figure View Figure 15
15);
newly
recorded
from northeastern
South
Material examined
Australia. Queensland: 65 km northwest of Winton, sandstone outcrop, in moist lightly sheltered area on top of outcrop, under log and rocks (142.64005°, −21.95847°), J. Thompson, S. Cowan & M. Tio, 10/VII/1995, 2 ♀ 2 imm. (AM KS.44204). South Australia: Clifton Hills, O.S.E. Lake Eyre Basin, dunes under cowpats (139.48333°, −26.5°), D. Hirst, 18 – 20/XI/1993, 1 ♀ ( SAM NN 28348).
SAM |
South African Museum |
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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