Mueggejapyx brehieri Sendra & Komericki 2021, gen. et sp. nov.
Creators: name: Sendra, Alberto
name: Komerički, Ana
name: Lips, Josiane
name: Luan, Yunxia
name: Selfa, Jesús
name: Jiménez-Valverde, Alberto
Publisher: name: Zenodo
Year: 2021
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Entognatha
Diplura
Japygidae
Mueggejapyx
Mueggejapyx brehieri

description: Mueggejapyx brehieri Sendra & Komerički gen. et sp. nov.
urn:lsid:zoobank.org:act: 8D581345-0B2E-4E5C-918C-DBF84F3B6978
Figs 2, 65–97; Tables 5–6
Etymology
This species is dedicated to Franck Brehier, French biospeleologist, who has dedicated himself to exploring and studying many karst areas and caves in Southeast Asia.
Type material
Holotype
MYANMAR • ♂; Shan State, Ywangan, Win Twin Cave; 21º11′51.47″ N, 96º32′40.34″ E, 16 Nov. 2018: Aung Lin leg.; labelled “♂4-holotype”; MZB (MCNB) 2020-1156.
Paratypes
MYANMAR • 1 ♂, 1 ♀; same collection data as for holotype; labelled “♂3-paratype” and “♀1– paratype”; MZB (MCNB) 2020-0626, MZB (MCNB) 2020-0627 • 1 ♀; same collection data as for holotype; labelled “♀2-paratype”; MZB (MCNB) 2020-1159 • 1 ♂; Shan State, Parpent Cave 1; 2 Dec. 2015; Franck Brehier leg; collected by hand; collector’s code BUR15-FB20; labelled “♂5-paratype”; MZB (MCNB) 2020-0628 • 1 ♂; same collection data as for preceding; collector’s code MY15–20.06; labelled “♂7-paratype”; MZB (MCNB) 2020-1158 • 1 ♀; Shan State, Kyauk Khaung [= Stone Cave]; 30 Nov. 2015; Franck Brehier leg.; collector’s codes: BUR15–FB17, MY15–17.03; labelled “♀6-paratype”; MZB (MCNB) 2020-1157.
Other material examined
MYANMAR • 2 specs; same collection data as for holotype; mounted on two separate aluminium stages and coated with palladium-gold; Coll. AS.
Description
BODY. Elongated (Fig. 2), length 23 mm in male holotype (19–26 mm in three paratype females, 15–23 mm in three paratype males). Greatest width at urotergite VII 2.6 mm. Epicuticle smooth under optical microscope, with numerous micropores at higher magnifications (Figs 72, 85). Cuticle unpigmented, except for slightly sclerotized areas on dorsal head, mandible tips, femoral and tibial condyles and segments VI–X (Fig. 2).
HEAD. Antennae with 36 antennomeres; antennae less than ½ body length; first antennomere short, followed by three longer and larger antennomeres (2 nd to 4 th antennomeres with reinforced borders) (Figs 65–68, 70; Table 5). All antennomeres with abundant setae including sM and sm setae, which appear more abundant on ventral side of 7 th to 16 th antennomeres under light microscope; trichobothria present on antennomeres 4–6 in a 3/5/5 pattern, in which a trichobothria in distal position; 1 or 2 placoid sensilla present on latero-interior ventral side on 17 th and more distal antennomeres; apical antennomere bearing 16–18 placoid sensilla distributed in three irregular whorls (Figs 65–66). Dorsal and ventral side of head with numerous uniformly distributed sM and sm, and several M, more obvious in young specimens (♂7- paratype); on dorsal side A1–3, S2,4,6, M2,3,5, I4,5, P2 and L1–5 (Fig. 69); on ventral side, submentum with large 1+1 M in posterior position, admentum with 4+4 M, mentum at base of labial palps with 1+1 M; external lobes of mentum with abundant sM; internal lobes with 1+1 short M. Elongated, conical labial palps almost 3 × as long as wide compared with sM and sm in addition to one
long, apical seta and a few shorter setiform sensilla (Figs 75–77). Lacinia falciform well sclerotized, all five laminae pectinate.
THORAX. Thoracic segments elongated (Figs 71, 75). Pronotum with 5+5 M and numerous uniformly distributed sM and sm; mesonotum with 5+5 M and a few sM and sm; metanotum with 2+2 M and a few sm; both prescuta have 1+1 M and scattered sM and sm; at high magnifications tiny, uniformly distributed micropores (0.10–0.15 µm diameter) visible on cuticle surface (Fig. 72). Thoracic sternites, intersternites, and presternites well defined with sm, sM, and M setae (Figs 75, 77–79). Pro-presternites and pro-, meso- and metasternites have strong internal Y-shaped cuticular structures (furcisternites) (Barlet & Carpentier 1962), and only in pro-presternites prolongation of posterior branch named spine clearly visible on surface (Denis 1949). Pro-presternum with 1+1 short M in anterior lateral position and 1+1 sM in medial anterior; prosternum with 1+1 medial anterior M; 3+3 lateral anterior M, 1+1 medial intermediate M and 2+2 lateral posterior M; meso-poststernum with 5+5 M; meso-intersternum with 5+5 M; mesosternum with 1+1 medial anterior M, 4+4 lateral anterior M, 1 M sagittal, 1+1 medial intermediate M, 1+0 medial posterior M and 3+3 lateral posterior M; metapoststernum with 5+5 M; meta-intersternum 4+4 M; and metasternum with 1+1 medial anterior M, 3+3 lateral anterior M; 1+1 sagittal M, 1+1 medial intermediate M, 3+3 lateral posterior M (Figs 75, 77–79). Legs elongated, hind legs reaching 5 th abdominal segment. Frictional setae between trochantercoxa-femora articulations; femora-tibia-tarsus articulations with row of long M or sM setae with large sockets, plus additional 1 M in coxa, 5 M in trochanter and 7 M in femora. Tibia and tarsus with M and sM; 5 M in tibia and 2 M in tarsus. Tibia also bearing one calcar seta at ventral apex, thicker and more robust than other tibial setae, and two rows of four or five thick setae along ventral side. Pretarsus with two unequal claws and sharp medial unguiculus.
ABDOMEN. Abdominal tergites with few sm and sM. Tergite I (prescutum and scutum) without M; tergite II with 0 or 1+1 M5; tergite III with 1+1 M (medial anterior macrosetae), 0 or 1+1 M1, 1+1 M4–5; tergites IV–VI with 1+1 M (ma), 0 or 1+1 M1, 1+1 M2–5; tergite VIII with 1+1 M4–5; tergite IX lacking M except (M1 present in specimens from Parpent Cave 1 (Fig. 88). Urite X (Figs 89, 92) nearly 1.5 × as long as wide, distinctly marked carinae present with subparallel margins slightly convergent towards posterior; 2+2 intracarinal D1 and D3 macrosetae and 3+3 macrosetae (L1, L3, L5) on carinae (Fig. 89); ventral side with four rows of 3+3 M, 3+3 M, 2+2 M, and 2+2 M from anterior to posterior position; acropygium rounded (Fig. 91). Tergites I–V with blunt, slightly rounded to pointed posterolateral angles; angles on tergites VI and VII more conspicuous, lobiform projection small to more prolonged and visibly sclerotized in largest specimens; tergite IX with projections (Fig. 88). Sternite I (Figs 80–85) with multiperforated surface and rounded protrusions covered by abundant sm and lesser sM and 3+3 or 3+4 M on prescutum and 11+11 M on scutum. Median glandular organ with 12 seta-shaped sensilla (Fig. 83). Lateral subcoxal organs invaginated below posterior margin or evaginated showing central opening protruding over margin of first urosternite (Figs 81–82). Each lateral subcoxal organ with one, two, or three rows of glandular setae (GS) (54–100 in males, 47–66 in females) and one row of sensory setae (SS) (11–24 in males, 13–15 in females) occupying 0.22–0.30 (males) and 0.23–0.25 (females) of interstyle width; GS/st1 (stylus of first sternite) = 0.1–0.23 (males) and 0.18–0.28 (females), SS/st1= 0.19 (male) and 0.16–0.26 (females); row of setae with large sockets anterior to glandular setae, 7–12 in males and 6–10 in females (Figs 80–85). Sternites have abundant sm and strong M; sternites II–VII with 7+7 A M, 5+5 (4+4) B M and 4+4 C M; sternite VIII with 3+3 (4+4) A M, 3+3 (2+2) B M and 3+3 C M (see Material and methods for terminology); sternite IX with 1+1 M (Figs 86–87). Cerci strong, well developed, elongated and rectilinear, becoming curved toward apex (Figs 89–92), length ranging from 2.8 mm in largest specimen (♀ 1- paratype) to 1.4 mm in the smallest (♂7- paratype); cerci always slightly longer than urite X, heavily sclerotized with external dorsal andventral carinae projecting from dorsal and ventral acetabular articulations running almost to apex ventrally and halfway dorsally. Cerci with medial tooth; right cercus with basal notch complementary in shape to round tooth at ventral side of basal portion of left cercus. Posterior to right notch and left tooth: in right cercus short row of 5 or 6 small, round denticles in line; and in left cercus two rows of small round denticles (4+4); these rows of denticles occupying 1/8 of total length of each cercus (Figs 89–95, 97). Each cercus with scattered sm, sM, and M setae and several conical sensilla throughout, more abundant distally (Figs 96–97). Dorsal side of each cercus with 6 or 7 D macrosetae, D1, D3 and D5 largest on both cerci; ventral side with 12 V-macrosetae, V3 and V8 being largest; intracarinal region with 5–7 L macrosetae, a pair of macrosetae in L1 being largest (Figs 91, 94–95).
Taxonomic affinities
Mueggejapyx gen. nov. is distinguished by its elongated, rectilinear, heavily sclerotized cerci curving subapically, and lacking a medial tooth but with one or two rows of basal small round denticles, its median glandular organ with seta-shaped sensilla, and short lateral subcoxal organs, each with a row of setae that have large sockets.
Remarks
Mueggejapyx brehieri gen. et sp. nov., was observed and collected along with A. ywangana sp. nov. in Win Twin Cave (Figs 1–4), as well as in two nearby caves: Parpent Cave 1 and Kyauk Khaung (synonyms: Sin Lae Ye Win, Stone Cave). The latter is the second longest cave so far explored in Myanmar. Kyauk Khaung Cave is over 4790 m long and also situated in the Ywangan karst area. Its entrance is located only 1240 m southeast of the entrance to Win Twin, and the cave itself extends mostly towards the northeast of the entrance. During the 2015 biological research of Kyauk Khaung, specimens of Campodeidae and Japygidae were found in the northernmost parts of the cave, which indicates the species is most likely distributed throughout the entire subterranean habitats of the Ywangan karst (unpublished data). The Ywangan karst covers 1050 ha, and at the moment hosts three other endemic troglobitic invertebrates: the carabid beetle Birmaphaenops brehieri Deuve, 2017 (Deuve 2017), the cave crab Shanphusa ywarngan Ng & Whitten, 2017 (Ng & Whitten 2017), and a woodlouse Bamaoniscus lobatus Taiti et al, 2020 as well as an endemic karst-adapted gecko, the Linn-Way bent-toed gecko Cyrtodactylus linnwayensis Grismer et al., 2017 (Grismer et al. 2017), and 17 species of bats (unpublished data). Due to its biodiversity, Ywangan karst is proposed as a karst Key Biodiversity Area and a subterranean Ramsar Site. Although cave tourism is being developed in the area, there are substantial efforts being made by the NGO sector (Fauna & Flora International Myanmar) to provide guidance for development of sustainable, low-impact tourism as well as cave and biodiversity conservation (unpublished data).
description: Published as part of Sendra, Alberto, Komerički, Ana, Lips, Josiane, Luan, Yunxia, Selfa, Jesús & Jiménez-Valverde, Alberto, 2021, Asian cave-adapted diplurans, with the description of two new genera and four new species (Arthropoda, Hexapoda, Entognatha), pp. 1-46 in European Journal of Taxonomy 731 on pages 29-37, DOI: 10.5852/ejt.2021.731.1199, http://zenodo.org/record/4422557