Pseudodiamesa branickii, Nowicki, 1873

Chamutiová, Tímea, Hamerlík, Ladislav & Bitušík, Peter, 2020, Subfossil chironomids (Diptera, Chironomidae) of lakes in the Tatra Mountains an illustrated guide, Zootaxa 4819 (2), pp. 216-264 : 223

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.4442621

persistent identifier

https://treatment.plazi.org/id/03F487F1-FFBA-FFA3-FF22-FBFFAAADFA78

treatment provided by

Plazi

scientific name

Pseudodiamesa branickii
status

 

Pseudodiamesa branickii View in CoL - type ( Figs 14–16 View FIGURES 9–14 View FIGURES 15–22 )

This is a new morphotype, not listed in Brooks et al. (2007).

Antennal ratio (length of basal segment/ length of flagellum) ˂ 2.5 ( Fig. 14 View FIGURES 9–14 ). Pecten epipharyngis consists of seven, weakly sclerotized scales. Labral lamellae absent. Premandible with 7–9 teeth ( Fig. 16 View FIGURES 15–22 ). Mandibular seta interna consists of 9–15 branches ( Fig. 15 View FIGURES 15–22 ). All teeth of mentum unicolored, black, fourth to seventh lateral teeth are hardly visible in unflatten mentum ( Fig. 14 View FIGURES 9–14 ).

Remarks: Subfossil remains have been recorded only in three lakes. In the Tatra Mts. lakes, the morphotype contains a single species, P. branickii Nowicki, 1873 ( Bitušík et al. 2006a; Novikmec et al. 2015).

Kingdom

Animalia

Phylum

Arthropoda

Class

Insecta

Order

Diptera

Family

Chironomidae

Genus

Pseudodiamesa

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