Pristiphora breadalbanensis (Cameron, 1882)

Prous, Marko, Kramp, Katja & Liston 1, Veli VikbergAndrew, 2017, North-Western Palaearctic species of Pristiphora (Hymenoptera, Tenthredinidae), Journal of Hymenoptera Research 59, pp. 1-190 : 36-37

publication ID

https://dx.doi.org/10.3897/jhr.59.12565

publication LSID

lsid:zoobank.org:pub:598C5BB3-2136-4D91-B522-FA14D8874A52

persistent identifier

https://treatment.plazi.org/id/893CA72E-7FAC-FE60-E494-F72A72DD8D26

treatment provided by

Journal of Hymenoptera Research by Pensoft

scientific name

Pristiphora breadalbanensis (Cameron, 1882)
status

 

Pristiphora breadalbanensis (Cameron, 1882) Fig. 214

Nematus breadalbanensis Cameron, 1882: 531-532. Syntypes possibly in BMNH, not examined. Type locality: Scotland, United Kingdom.

Lygaeonematus tromsöensis [sic!] Kiær, 1898: 48-49. 2 ♀ syntypes in TROM, not examined. Type locality: Flöifjeld and Mauken, Troms, Norway. Synonymised with Lygaeonematus breadalbanensis by Lindqvist (1952).

Lygaeonematus corpulentus Konow, 1904a: 196 (key). Syntype ♀ (GBIF-GISHym3909) in SDEI, examined. Type locality: Norway and Sweden ( Konow 1904b).

Lygaeonematus arcticola Enslin, 1916: 514-515.1 ♀ and 1 ♂ syntype in ZSM, examined. Type locality: North Ural, Russia.

Similar species.

Species limits in the carinata group are still unclear.

Genetic data.

Based on COI barcode sequences, specimens of the carinata group are divided between four BIN clusters (BOLD:AAF4995, BOLD:ABU8603, BOLD:ACL1744, BOLD:ACL1745), which form a monophyletic group (Fig. 5). Minimal distances between these clusters are 1.2%-4.48%. Because of unresolved taxonomy, it is not yet clear how different species are divided among these BIN clusters. Based on nuclear data, maximum divergence within the group is 2.2% (based on ten specimens and TPI) and the nearest neighbour is 1.5% ( P. pseudocoactula , both genes combined) or 1.0% different ( P. wesmaeli , only NaK).

Host plants.

Unknown.

Distribution and material examined.

West Palaearctic, Nearctic. Specimens studied are from Norway, Russia (North Ural), and United Kingdom.