Bennelongia mcraeae, Martens & Halse & Schön, 2013
publication ID |
https://doi.org/ 10.5852/ejt.2013.66 |
publication LSID |
lsid:zoobank.org:pub:5270B024-84C1-4CD5-BC18-4AF37D2E1045 |
DOI |
https://doi.org/10.5281/zenodo.3846918 |
persistent identifier |
https://treatment.plazi.org/id/DFD1A720-E602-46CC-AABF-C6EDD63CD70E |
taxon LSID |
lsid:zoobank.org:act:DFD1A720-E602-46CC-AABF-C6EDD63CD70E |
treatment provided by |
Carolina |
scientific name |
Bennelongia mcraeae |
status |
sp. nov. |
Bennelongia mcraeae sp. nov.
urn:lsid:zoobank.org:act:DFD1A720-E602-46CC-AABF-C6EDD63CD70E
Diagnosis
Valves ( Fig. 16 View Fig A-B, E-F) high and rounded, with greatest height situated on or close to the middle, dorsal margins almost evenly rounded; ventral margin weakly sinuous. LV ( Fig. 16A, E View Fig ) with anteroventral il large, reaching over half of the anterior margin; dorsal il descending along ca. 4/5 of anterior margin, both lists thus clearly overlapping. RV ( Fig. 16B, F View Fig ) with antero-ventral lapel fairly ventrally inserted, large and pronounced, with rounded, weakly crenulated margin ( Fig. 16D View Fig , I-L). Carapace in lateral view ( Fig. 16 View Fig C- D) pitted, especially along anterior and posterior margins, and set with few setae.
Hemipenes ( Fig. 17A, F View Fig ) largely symmetrical, ls with broad base, ventrally bluntly beak-shaped, only protruding significantly beyond ventral tip of ms. Right prehensile palp ( Fig. 17C, E View Fig ) with distal segment stout, but of somewhat variable shape, either strongly subquadrate or with rounded dorsal and anterior
margins. Left prehensile palp ( Fig. 17B, D View Fig ) with distal segment long and slender, reaching beyond ventro-apical margin of proximal segment with at least half of its length.
Etymology
The species is named in honour of Jane McRae (Perth, WA) in acknowledgement of her vast knowledge of the taxonomy and morphology of many invertebrate groups of Western Australia. She also collected the type material of the present species and has unrelentingly provided technical help towards the present revision of Bennelongia since 2006.
Measurements (all measurements in µm – see Table 1 View Table 1 for measurements of all specimens illustrated with SEM)
Holotype ♂ ( WAMC52286 ): RV: L = 1480, H = 878. LV: L = 1560, H = 896.
Allotype ♀ ( WAMC52287 ): RV: L = 1608, H = 1002. LV: L = 1663, H = 1033.
Type locality
Arro Lake, ca. 11 km NW of Eneabba, WA. Approximate coordinates: 29º44’11” S, 115º09’58” E (WGS 84). All specimens collected by J. McRae & A. Pinder (voucher OST14B; locality code SPS182) on 23 Sep. 1999 with a sweep net. Arro Lake is an open lake with a Melaleuca / Casuarina fringe. Water chemistry at the time of collecting: Salinity = 0.15 g /l, pH = 7.32. Nutrient levels were fairly high: total N = 1700 µg /l; total P = 220 µg /l. The milky-white colour of the water equates to a high level of turbidity (2200 NTU).
Type material
Holotype
♂ ( WAMC52286 ), with soft parts dissected in a sealed slide and valves stored dry in a micropalaeontological slide.
Allotype
♀ ( WAMC52287 ), with soft parts dissected in a sealed slide, and valves stored dry in a micropalaeontological slide.
Paratypes
Two ♂♂ (dissection: OC.3328; valves: WAMC 52288) and one ♀ carapace ( WAMC 52289). Three females in bulk in EtOH ( WAMC 52290).
Differential diagnosis
The species is characterised especially by the large and stout lapel on the RV but also by the large anteroventral il on the LV.
Ecology and distribution
Lake Arro (ca. 300 km N of Perth) is a large flat-bottomed body of water with episodic inflow that holds water for about 4-24 months after inflow. The lake has a clay base and sediment-driven turbidity. This species is known only from the type locality. From the same sample as the one that yielded B. macraeae sp. nov., Timms (2002) described a new species of Anostraca , Branchinella complexidigitata Timms, 2002 .
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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