Pseudodiamesa nivosa, Goetgehebuer, 1928
publication ID |
https://doi.org/ 10.11646/zootaxa.4819.2.2 |
publication LSID |
lsid:zoobank.org:pub:2459A542-6CF2-4545-9E6F-262C68838D99 |
DOI |
https://doi.org/10.5281/zenodo.4442623 |
persistent identifier |
https://treatment.plazi.org/id/03F487F1-FFBA-FFA3-FF22-FA63AF1CF81C |
treatment provided by |
Plazi |
scientific name |
Pseudodiamesa nivosa |
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Pseudodiamesa nivosa View in CoL - type ( Figs 17–19 View FIGURES 15–22 )
This is a new morphotype, not listed in Brooks et al. (2007).
Antennal ratio ≥ 2.5 ( Fig. 17A View FIGURES 15–22 ). Pecten epipharyngis is characterized by even number (3–4 pairs) strongly sclerotized scales. Labral lamellae present between bases of SI setae. Premandible with more than 10 teeth ( Fig. 19 View FIGURES 15–22 ). Mandibular seta interna consists of 14–24 branches ( Fig. 18 View FIGURES 15–22 ).
Mentum with a lighter median tooth compared to the black lateral teeth; outermost lateral teeth are more visible in unflatten mentum ( Fig. 17 View FIGURES 15–22 ). However, be aware of the fact that first and second instar larvae of both morphotypes has broad median mental tooth that is lighter than the blackish lateral teeth ( Figs 20, 21 View FIGURES 15–22 ), thus young instars are not sufficient for morphotype identification.
Remarks: This morphotype was the most frequent Diamesinae remain in surface sediments of the Tatra Mts. lakes. Its distribution is consistent with the knowledge of the ecology of the nivosa species group. It is more coldadapted than the P. branickii group, which occurs under more moderate conditions ( Ilyashuk et al. 2010; Hamerlík et al. 2017). One species of the species group, P. nivosa Goetgehebuer, 1928 , was recorded in the Tatra Mts. ( Novikmec et al. 2015).
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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