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Cave millipede diversity with the description of six new species from Guangxi, China

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We synthesized the current knowledge of cave-dwelling millipede diversity from Guangxi Zhuang Autonomous Region (Guangxi), South China Karst, China and described six new millipede species from four caves from the Guilin area, northeastern Guangxi. Fifty-two cave-dwelling millipedes are known for the region consisting of 38 troglobionts and 14 troglophiles. Of the troglobionts, 24 are presently considered single-cave endemics. New species described here include Hyleoglomerisrukouqu sp. nov. and Hyleoglomerisxuxiakei sp. nov. (Family Glomeridae), Hylomusyuani sp. nov. (Family Paradoxosomatidae), Eutrichodesmusjianjia sp. nov. (Family Haplodesmidae), Trichopeltisliangfengdong sp. nov. (Family Cryptodesmidae), and Glyphiulusmaocun sp. nov. (Family Cambalopsidae). Our work also resulted in range expansions of Pacidesmustrifidus Golovatch & Geoffroy, 2014, Blingulussinicus Zhang & Li, 1981 and Glyphiulusmelanoporus Mauriès & Nguyen Duy-Jacquemin, 1997. As with many hypogean animals in Southeast Asia, intensive human activities threaten the persistence of both cave habitats and species. We provide both assessments on the newly described species’ distributions and recommendations for future research and conservation efforts.
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Cave-dwelling millipedes, Guangxi, China 57
Cave millipede diversity with the description
of six new species from Guangxi, China
Weixin Liu1, J. Judson Wynne2
1 Department of Entomology, College of Agriculture, South China Agricultural University, 483 Wushanlu,
Guangzhou 510642, China 2 Department of Biological Sciences, Merriam-Powell Center for Environmental
Research, Northern Arizona University, Box 5640, Flagsta, AZ 86011, USA
Corresponding author: J. Judson Wynne (jut.wynne@nau.edu); Weixin Liu (da2000wei@163.com)
Academic editor: O. Moldovan | Received 19 April 2019 | Accepted 3 June 2019 | Published 02 July2019
http://zoobank.org/19205CA6-4680-45D4-A3A0-F1640752D41B
Citation: Liu WX, Wynne JJ (2019) Cave millipede diversity with the description of six new species from Guangxi,
China. Subterranean Biology 30: 57–94. https://doi.org/10.3897/subtbiol.30.35559
Abstract
We synthesized the current knowledge of cave-dwelling millipede diversity from Guangxi Zhuang Au-
tonomous Region (Guangxi), South China Karst, China and described six new millipede species from
four caves from the Guilin area, northeastern Guangxi. Fifty-two cave-dwelling millipedes are known
for the region consisting of 38 troglobionts and 14 troglophiles. Of the troglobionts, 24 are presently
considered single-cave endemics. New species described here include Hyleoglomeris rukouqu sp. nov. and
Hyleoglomeris xuxiakei sp. nov. (Family Glomeridae), Hylomus yuani sp. nov. (Family Paradoxosomati-
dae), Eutrichodesmus jianjia sp. nov. (Family Haplodesmidae), Trichopeltis liangfengdong sp. nov. (Family
Cryptodesmidae), and Glyphiulus maocun sp. nov. (Family Cambalopsidae). Our work also resulted in
range expansions of Pacidesmus tridus Golovatch & Georoy, 2014, Blingulus sinicus Zhang & Li, 1981
and Glyphiulus melanoporus Mauriès & Nguyen Duy-Jacquemin, 1997. As with many hypogean animals
in Southeast Asia, intensive human activities threaten the persistence of both cave habitats and species. We
provide both assessments on the newly described species’ distributions and recommendations for future
research and conservation eorts.
Keywords
Single cave endemic, disturbance relict, cave conservation
Subterranean Biology 30: 57–94 (2019)
doi: 10.3897/subtbiol.30.35559
http://subtbiol.pensoft.net
Copyright Weixin Liu, J. Judson Wynne . This is an open access article distributed under the terms of the Creative Commons Attribution License
(CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
RESEARCH ARTICLE
Subterranean
Biology Published by
The International Society
for Subterranean Biology
A peer-reviewed open-access journal
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
58
Introduction
Southeast Asia is considered the most biologically diverse for troglomorphic animals
among the well-sampled tropical regions of the globe (Clements et al. 2006). Yet despite
research conducted over the past three decades, few areas in Southeast Asia have been
suciently investigated and knowledge of cave biological diversity and ecological pro-
cesses is limited (Deharveng and Bedos 2000). e expansive South China Karst rep-
resents one of these regions (Clarke 2006, Chen et al. 2001). Among the four admin-
istrative units in China where this formation occurs, Guangxi is considered the most
taxonomically well-studied region. At least 100 troglomorphic (subterranean-adapted)
arthropods have been identied from Guangxi (Wynne, unpublished data). Most have
been identied as short-range endemic species (Tian 2011, Deharveng et al. 2008) with
more than half (or 58 species) considered single cave endemics (Gao et al. 2018).
Common in cave-arthropod communities, millipedes represent a dominant and
widespread group in southern China (Golovatch 2015, Liu et al. 2017a). Approxi-
mately 150 cave-dwelling millipedes have been described from China (Golovatch
2015, Liu unpublished data) with 52 species known from Guangxi. Of these, 38 spe-
cies are troglobionts with 24 identied as single-cave endemics (Table 1). Fig. 1 sum-
marizes millipede diversity by family with Cambalopsidae (14 species), Glomeridae
(11) and Paradoxosomatidae (10) being among the most speciose groups.
In the paper, we describe six new species (representing ve families, Glomeridae,
Paradoxosomatidae, Haplodesmidae, Cryptodesmidae and Cambalopsidae), as well as
discuss range expansions of three additional cave-dwelling species. We have also sum-
marized the cave-dwelling millipedes known to Guangxi, their known distributions,
and provide recommendations to guide future research and management eorts.
Material and methods
Study area
Located in southwest China, Guangxi encompasses 236,700 km2. Once an ancient
shallow sea during the middle Cambrian to Late Triassic periods, this region is now
largely characterized by a massive karst (limestone) stratum over 10,000 m thick (Cao
et al. 2007) with steep-sided mountains called fenglin or “tower karst” protruding sky-
ward. As a result of the subtropical climate and rock stratum, Guangxi supports at least
564 known caves (Yuanhai Zhang, pers. comm. 2019).
We sampled four caves in the northeastern most extent of Guangxi within a 30 km
radius of the city of Guilin, China (Fig. 2). Caves were selected based upon two cri-
teria – sucient length to support deep zone conditions, and the availability of a cur-
rent cave map. Cave deep zones are dened as completely dark region with relatively
stable temperature, low to no airow, and a near water saturated atmosphere with a
Cave-dwelling millipedes, Guangxi, China 59
Figure 1. Species richness (total number of species provided in parentheses) for the eight known families
of subterranean-dwelling millipedes from Guangxi, China.
negligible evaporation rate (Howarth 1980, 1982). While we recognize other factors
may contribute to the occurrence of cave deep zones (e.g., mazy and/or constricted
passageways, small or partially rock-fall obstructed entrances, and cave structure in
general), we used this criterion because logistics prevented us from selecting study sites
based upon site visit evaluations. is work represents the rst eort to sample these
caves for subterranean-adapted arthropods.
All caves occurred at low elevations within tower karst formations. While extensive
agriculture, as well as rural village and suburban habitation characterized the surround-
ing lowlands, vegetation on the tower karst represented a marginally disturbed combi-
nation of native and introduced plant and tree species.
Literature review and synthesis
Based on our knowledge of the South China Karst (SCK) cave-dwelling millipede
literature, we summarized the total number of caves sampled and cave-dwelling mil-
lipedes detected for Guangxi. For selected species occurring within two or more caves,
we determined maximum distances between caves and, in some cases, average dis-
tances across all caves using ArcGIS 10.6.1.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
60
Figure 2. Study area with general locations of the four study caves (black triangles). Locator map depicts
the Guilin area (red dot), Guangxi (bold black outline), China.
Field sampling
We hand collected cave-dwelling arthropods at four caves from 15 to 18 November
2016. Approximately eight hours (2 observers at 4 hours per observer) was spent con-
ducting direct intuitive searches within estimated deep zones of each cave. We ex-
amined bat guano, dead insects, mud banks and oors, ood detritus, or vegetation
Cave-dwelling millipedes, Guangxi, China 61
brought in by humans and deposited within the cave. Given the four caves varied in
size and the diversity of arthropods encountered, the areal extent sampled varied. We
also sampled the vegetation within the entrance of Liangfeng Cave applying a direct
intuitive search approach. For all four caves, we also opportunistically collected arthro-
pods as encountered while transiting from entrance to estimated deep zones. Sampling
methods were applied sensu stricto Wynne et al. (2019).
Analysis and preparation
All specimens examined in this study were collected by the second author in the Guilin
area, Guangxi, southern China and preserved in 95% ethanol. Holotypes and para-
types are deposited in the Zoological Collection of the South China Agricultural Uni-
versity, Guangzhou, Guangdong Province, China (SCAU). Detailed examination of
characters and dissections were performed using a Leica S8 APO stereo micro scope.
Line drawings were prepared with a ZEISS Axioskop40 microscope with a camera lu-
cida attached. Photographs were taken using a Keyence VHX-5000 digital mi croscope,
and further edited using Adobe Photoshop CS5.
Cave locations
We recognize standard practice for new species description is to provide sample locality
information including geographical data to facilitate future collecting, interpretation
and research. Because caves often represent sensitive resources, we provided general
geographical information and oset the latitude and longitude coordinates by ~1 km.
is level of detail is sucient for future comparative studies, while protecting the
precise location of our study caves.
Terminology
Cave ecosystems typically consist of four zonal environments (Howarth 1980, 1983):
(1) entrance zone – combination of surface and cave environmental conditions; (2)
twilight zone – both diminished light conditions and inuence of surface environ-
ment; (3) transition zone – aphotic, yet barometric and diurnal shifts are observed at a
signicantly diminished rate approaching near stable climatic conditions; and, (4) deep
zone – complete darkness, high environmental stability, constant temperature, and
near water-saturated atmosphere with low to no airow (typically occurs in the deepest
portion of the cave). While there are four primary cave specic functional groups gen-
erally recognized, the specimens discussed are troglomorphic (subterranean-adapted)
organisms known as troglobionts (Sket 2008). ese animals are obligate cave dwellers
that require the stable environmental conditions of the deep zone to complete their life
cycle and exhibit morphological characteristics indicative of cave adaptation. We also
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
62
Table 1. Fifty-two known cave-dwelling millipede species from Guangxi, South China Karst, China. ‘Or-
der: Family: Species’, ‘Functional Group’ (TB=presumed troglobiont, TP=troglophile), number of caves
(# Caves) to suggest a level of potential endemism), and main Reference(s) are provided. As troglophiles
are expected to have regional distributions, the number of caves where TPs were detected is not included.
Order: Family: Species Functional group # Caves Reference(s)
Glomerida: Glomeridae
Hyleoglomeris baxian Liu & Tian, 2015 TB 1 Liu and Tian 2015a
Hyleoglomeris curtisulcata Golovatch, Liu & Georoy, 2012 TB 1 Golovatch et al. 2012a
Hyleoglomeris grandis Liu & Tian, 2015 TB 1 Liu and Tian 2015a
Hyleoglomeris heshang Golovatch, Liu & Georoy, 2012 TB 1 Golovatch et al. 2012a
Hyleoglomeris kunnan Golovatch, Liu & Georoy, 2012 TB 1 Golovatch et al. 2012a
Hyleoglomeris lii Golovatch, Liu & Georoy, 2012 TP Golovatch et al. 2012a
Hyleoglomeris mashanorum Golovatch, Liu & Georoy,
2012
TB 1 Golovatch et al. 2012a
Hyleoglomeris mulunensis Golovatch, Liu & Georoy, 2012 TB 1 Golovatch et al. 2012a
Hyleoglomeris rukouqu sp. nov. TP is study
Hyleoglomeris xueju Golovatch, Liu & Georoy, 2012 TB 1 Golovatch et al. 2012a
Hyleoglomeris xuxiakei sp. nov. TB 1 is study
Polydesmida: Cryptodesmidae
Trichopeltis liangfengdong sp. nov. TB 1 is study
Haplodesmidae
Eutrichodesmus distinctus Golovatch, Georoy, Mauriès &
VandenSpiegel, 2009
TB 1 Golovatch et al. 2009a
Eutrichodesmus jianjia sp. nov. TB 1 is study
Eutrichodesmus latus Golovatch, Georoy, Mauriès &
VandenSpiegel, 2009
TB 4 Golovatch et al. 2009b
Eutrichodesmus lipsae Golovatch, Georoy, Mauriès &
VandenSpiegel, 2015
TB 1 Golovatch et al. 2015
Eutrichodesmus planatus Liu & Tian, 2013 TB 1 Liu and Tian 2013
Eutrichodesmus similis Golovatch, Georoy, Mauriès &
VandenSpiegel, 2009
TB 2 Golovatch et al. 2009b
Paradoxosomatidae
Piccola golovatchi Liu & Tian, 2015 TB 1 Liu and Tian 2015b
Hylomus longispinus (Loksa, 1960) TB 1 Loksa 1960, Golovatch et al. 2010a,
Srisonchai et al. 2018
Hylomus lui (Golovatch, Li, Liu & Georoy, 2012) TB 1 Golovatch et al. 2012b, Srisonchai et
al. 2018
Hylomus nodulosus (Liu, Golovatch & Tian, 2014) TP Liu et al. 2014, Srisonchai et al. 2018
Hylomus phasmoides (Liu, Golovatch & Tian, 2016) TB 1 Liu et al. 2016, Srisonchai et al. 2018
Hylomus scolopendroides Golovatch, Georoy & Mauriès,
2010
TB 4 Golovatch et al. 2010a, Liu et al.
2014, Srisonchai et al. 2018
Hylomus scutigeroides Golovatch, Georoy & Mauriès,
2010
TB 6 Golovatch et al. 2010a, Liu et al.
2014, Srisonchai et al. 2018
Hylomus spinissimus (Golovatch, Li, Liu & Georoy, 2012) TB 1 Golovatch et al. 2012b, Srisonchai et
al. 2018
Hylomus variabilis (Liu, Golovatch & Tian, 2016) TP Liu et al. 2016, Srisonchai et al. 2018
Hylomus yuani sp. nov. TB 1 is study
Polydesmidae
Epanerchodus orientalis Attems, 1901 TP Golovatch et al. 2012c
Pacidesmus armatus Golovatch, Georoy & Mauriès, 2010 TB 3 Golovatch et al. 2010b
Pacidesmus bedosae Golovatch, Georoy & Mauriès, 2010 TB 3 Golovatch et al. 2010b
Pacidesmus bidus Golovatch & Georoy, 2014 TB 1 Golovatch and Georoy 2014
Pacidesmus tiani Golovatch, Georoy & Mauriès, 2010 TB 2 Golovatch et al. 2010b
Pacidesmus tridus Golovatch & Georoy, 2014 TB 4 Golovatch and Georoy 2014, is
study
Cave-dwelling millipedes, Guangxi, China 63
Order: Family: Species Functional group # Caves Reference(s)
Callipodida: Paracortinidae
Paracortina yinae Liu & Tian, 2015 TP Liu and Tian 2015c
Spirostreptida: Pericambalidae
Bilingulus sinicus Zhang & Li, 1981 TP Zhang and Li 1981, is study
Parabilingulus aramulus Zhang & Li, 1981 TP Zhang and Li 1981
Parabilingulus simplicius Mauriès & Nguyen Duy-
Jacquemin, 1997
TP Mauriès and Nguyen Duy-Jacquemin
1997
Cambalopsidae
Hypocambala polytricha Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB 1 Golovatch et al. 2011a
Glyphiulus acutus Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB? 2 Golovatch et al. 2011b
Glyphiulus calceus Jiang, Guo, Chen & Xie, 2018 TP Jiang et al. 2018
Glyphiulus dicilis Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB 2 Golovatch et al. 2011b
Glyphiulus echinoides Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TP Golovatch et al. 2011c
Glyphiulus foetidus Jiang, Guo, Chen & Xie, 2018 TP Jiang et al. 2018
Glyphiulus impletus Jiang, Guo, Chen & Xie, 2018 TP Jiang et al. 2018
Glyphiulus maocun sp. nov. TB 1 is study
Glyphiulus melanoporus Mauriès & Nguyen Duy-
Jacquemin, 1997
TP Mauriès and Nguyen Duy-Jacquemin
1997, This study
Glyphiulus mulunensis Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB 2 Golovatch et al. 2011b
Glyphiulus paramulunensis Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB 2 Golovatch et al. 2011b
Glyphiulus proximus Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB 2 Golovatch et al. 2011b
Glyphiulus speobius Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB 2 Golovatch et al. 2011b
Glyphiulus tiani Golovatch, Georoy, Mauriès &
VandenSpiegel, 2011
TB 1 Golovatch et al. 2011b
reference troglophiles (or troglophilous organisms) – non-troglomorphic animals that
occur facultatively within caves and complete their life cycles there, but also exist in
similar cave-like habitats on the surface (Barr 1967, Howarth 1983, Sket 2008). Terms
used for taxonomic descriptions follow Minelli (2015).
Results
Since ~1960, at least 49 caves have been sampled for cave-dwelling millipedes. Of
these, nearly half (24 caves) supported single-cave endemic troglobionts, nine caves
supported at least two troglobitic millipede species, and three caves (present study;
Table 2) contained three troglobionts. For species occurring in two or more caves,
maximum distance between caves ranged from 11.22 km for Glyphiulus speobius to
137.27 km for Hylomus scutigeroides (Table 3).
A total of nine cave-dwelling millipede species were collected from four caves near
Guilin (Table 2). Four millipede species were detected in Liangfeng Cave, the other
three caves contained three species each. Of the six undescribed species, four are troglo-
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
64
Table 2. Nine cave-dwelling millipedes including both troglobitic and potentially relict species from four
caves near Guilin, Guangxi, South China Karst, China.
Species Maomaotou cave Guanshan No. 4 cave Shangshuiyan cave Liangfeng cave
Hyleoglomeris rukouqu sp. nov. ×
Hyleoglomeris xuxiakei sp. nov. ×
Hylomus yuani sp. nov. ×
Eutrichodesmus jianjia sp. nov. ×
Trichopeltis liangfengdong sp. nov. ×
Pacidesmus tridus × × ×
Blingulus sinicus × × ×
Glyphiulus melanoporus ×
Glyphiulus maocun sp. nov. ×
Table 3. Fourteen troglomorphic millipede species detected in more than one cave, Guangxi, South
China Karst, China. ‘Order: Family: Species’, number of caves (# Caves) to suggest a level of potential
endemism), and maximum distance between caves in kilometers (Max Dist.) are provided. *Indicates
coordinate data for all caves was unavailable for that species. ‘?’ denotes maximum distance was indeter-
minable due to lack of cave coordinate data. ‘Landscape features’ potentially aecting distribution of caves
separated by more than 10 km.
Order: Family: Species # Caves Max dist. (km) Landscape features
Polydesmida: Haplodesmidae
*Eutrichodesmus latus 4 14.32 Maximum distance between two caves provided, the third
cave occurs in between the two.
*Eutrichodesmus similis 2 ?
Paradoxosomatida
Hylomus scolopendroides 4 81.27 ree caves clustered within 21.24 km; one cave separated by
Diaojiang, Hongshui and Jincheng Rivers and lowland areas
Hylomus scutigeroides 6 137.6 One cave separated from others by Hongshui River; others
may occur in same formation
Polydesmidae
*Pacidesmus armatus 3 12.4 Two of three caves separated by lowland areas
*Pacidesmus bedosae 3 2.67
Pacidesmus tiani 2 1.88
Pacidesmus tridus 4 59.7 Separated by lowland areas
Spirostreptida: Cambalopsidae
Glyphiulus acutus 2 8.85
Glyphiulus dicilis 2 9.32
Glyphiulus mulunensis 2 7.77
Glyphiulus paramulunensis 2 6.67
Glyphiulus proximus 2 2.67
Glyphiulus speobius 2 11.22 Separated by lowland areas
morphic and may represent single cave and/or short-range endemics. One undescribed
epigean species, Hyleoglomeris rukouqu sp. nov., was identied within cave entrance
vegetation, and may represent a ‘disturbance relict’ species (sensu stricto Wynne et al.
2014). Glyphiulus maocun sp. nov., a troglophile, was detected in one cave, but likely
has a more regional distribution. For known troglophiles, Blingulus sinicus Zhang &
Li, 1981 were more widely distributed occurring in three caves each, while Glyphiulus
melanoporus Mauriès & Nguyen Duy-Jacquemin, 1997 was detected in one cave.
Cave-dwelling millipedes, Guangxi, China 65
Class Diplopoda
Order Glomerida Leach, 1814
Family Glomeridae Leach, 1815
Genus Hyleoglomeris Verhoe, 1910
Type species. Hyleoglomeris multilineata Verhoe, 1910.
Remarks. e genus can be characterized by the telopods, which with frontomesal tri-
chosteles on the prefemur and femur, and the caudomesal femoral process forming a dis-
tinct angle to femur proper (Golovatch et al. 2006, Liu and Tian 2015a). It encompasses
over 90 species distributed in Eurasia from Japan and Sulawesi to the Balkans (Engho et
al. 2015). At present, 30 species of this genus occur in China, 25 are subterranean-adapted.
Hyleoglomeris rukouqu sp. nov.
http://zoobank.org/EFA33915-ECD8-4B25-B874-28D0354B907C
Figs 3A, 5, 6
Type material. Holotype male (SCAU), China, Guangxi Zhuang Autonomous Re-
gion, Yangshou County, Shangshuiyan Cave [24°57'43.6"N, 110°20'37.21"E], 191
m elevation (el.), cave entrance, ferns and other vegetation (refer to habitat section
below), direct intuitive search, 17 November 2016, J.J. Wynne leg. Paratype, 1 female
(SCAU), same data as holotype.
Etymology. e species name, rukouqu, is used as a noun in apposition from the
Mandarin phrase, rùkǒu qū (入口区). When translated to English it means “entrance
zone” or “entrance area” to denote the area in the cave where this species was collected.
Diagnosis. Adult male of H. rukouqu sp. nov. is distinct from other Hyleoglomeris
species based on the following combination of characters: (1) peculiar color pattern
(Fig. 5); (2) telopods with a large, rectangular, central syncoxital lobe (Fig. 6D). is
new species is similar to H. lii (a troglophile from a cave in Guangxi), but is distin-
guished by (1) 2+2 dark brown spots on the thoracic shield (Fig. 5B, C) vs. 1+1 light
grey-yellow spots in H. lii; (2) sycoxital lobe of telopods being high, large and rectan-
gle-shaped (Fig. 6D) vs. low, linguiform, apically evidently concave in H. lii.
Description. Based on type specimens. Length ca 8.0 mm (holotype), 11.0 mm
(paratype), width 5.0 mm (holotype), 7.0 mm (paratype). Coloration: pattern vivid (Fig.
3A). With the exception of the brown dorsal spots, this species had similar coloration as
that of the limestone rock and sediment within the entrance. General coloration in alco-
hol (Fig. 5) light yellowish with contrastingly dark spots, latter absent on rings 3 and 11.
Head only brownish caudal margin, antennae and ommatidia dark-brownish. Collum
mostly marbled dark-brown except frontal margin part. oracic shield with 2+2 dark
brown spots, but lateral ones smaller than middle ones. Terga 4 with 1+1 brownish spots,
smaller than the above. Terga 5–7 and pygidium with 1+1 large, oblong, transverse, para-
median, marbled, dark spots. Terga 8–10, these paramedian spots increasingly separated
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
66
Figure 3. A Hyleoglomeris rukouqu sp. nov. from Shangshuiyan Cave B Hyleoglomeris xuxiakei sp. nov.
from Guanshan No. 4 Cave C Hylomus yuani sp. nov. from Liangfeng Cave D Eutrichodesmus jianjia sp.
nov. from Guanshan No. 4 Cave.
into 2+2, but lateral ones smaller than middle ones. Head: Ommatidium at least 7+1,
lenses rather convex. Tömösváry’s organ transverse-oval, parallel to the body, only slightly
wider than long. Antennae with four apical cones, antennomere 6 ca 2.5 times as long as
Cave-dwelling millipedes, Guangxi, China 67
Figure 4. A Trichopeltis liangfengdong sp. nov. from Liangfeng Cave B Pacidesmus tridus Golovatch &
Georoy, 2014 from Maomaotou Cave C Glyphiulus maocun sp. nov. from Liangfeng Cave.
Figure 5. Hyleoglomeris rukouqu sp. nov., holotype. A–C Habitus, dorsal, lateral and ventral views, respectively.
wide. Exoskeleton: Collum with two transverse striae (Fig. 5C). oracic shield (Fig. 5B)
with a narrow hyposchism, the latter not reaching behind caudal tergal margin; 7 trans-
verse striae: 3 starting below, 1 level to, 3 above schism; 5 striae (never the rst and last
from below) crossing the dorsum. Following terga 3–11 with two striae above lateral edge
(Fig. 5B). Pygidium (last tergite) of both sexes slightly concave medially at caudal mar-
gin. ♂ leg 17 with a low, rounded, outer coxal lobe; telopodite 4-segmented (Fig. 6A). ♂
leg 18 with a subtrianglar syncoxital notch; telopodite 4-segmented (Fig. 6B). Telopods:
(Fig. 6C–E) with a large, subrectanglar, central syncoxital lobe anked by high setose
horns, each of the latter with a small lobe on top. Prefemur micropapillate laterally, with
a long, digitiform, frontomesal trichostele. Femur with a smaller, digitiform, frontomesal
trichostele. Caudomedial femoral process prominent, apically with an evident lobe. Tibia
with a frontomesal seta. Caudomesal tibial process evident, recurved; an indistinct, papil-
late tubercle at base on caudal face. Tarsus strongly sigmoid, narrowly rounded apically.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
68
Figure 6. Hyleoglomeris rukouqu sp. nov., holotype. A leg 17, anterior view B leg 18; anterior view
Cright half of telopods, posterior view D right half of telopods, anterior views E tip of syncoxital horn,
anterior view.
Habitat. Specimens were collected within a vegetation association that may be
limited to the cave entrance zone and similar geographic features (e.g., sinkholes and
ssures in rock). At least three plant species occurred within the entrance including
Gesneriaceae sp., Adiantum sp., and one other fern species, which cannot be identied
without examining the sorii (A. Monro, pers. comm. 2018).
Notes. Based on the vivid color pattern and well-developed ommatidia, as well as
the location where it was detected within the cave, this animal represents an epigean
species and may be functioning as an obligate troglophile (sensu Peck 1970). While it
is likely H. rukouqu sp. nov. either occurred or still occurs in similar habitats on the
surface, the importance of relict plant species restricted to cave entrances has been
discussed for southern China (Monro et al. 2018). Additionally, several arthropod spe-
cies globally are restricted to cave entrances in Polynesia (Mockford and Wynne 2013,
Wynne et al. 2014, Bernard et al. 2015, Taiti and Wynne 2015) and North America
(Benedict 1979, Wynne and Shear 2016) due to either extensive surface disturbance
and glacial interglacial cycles, respectively. us, it is possible this species is a ‘distur-
bance relict’ restricted to the entrance of Shangshuiyan Cave and potentially other area
cave entrances with similar vegetation.
Hyleoglomeris xuxiakei sp. nov.
http://zoobank.org/D3CA0855-76FD-4683-8A7C-3F0505DC3D8E
Figs 3B, 7, 8
Type material. Holotype male (SCAU), China, Guangxi Zhuang Autonomous Re-
gion, Yangshuo County, Guanshan No. 4 Cave [24°56'58.34"N, 110°20'53.52"E],
Cave-dwelling millipedes, Guangxi, China 69
186 m el., deep zone, direct intuitive search, 16 November 2016, J.J. Wynne leg.
Paratype, 1 male (SCAU), same data as holotype. 3 females (SCAU), same data as
holotype, but deep zone, slightly muddy at area.
Etymology. e species name, xuxiakei, was Latinized using a combination of the
surname and forename of Xu Xiake (徐霞客). Xu was a traveler, explorer, and the rst
speleologist of China, who studied caves and karst geology during the decline of the
Ming Dynasty. He conducted a four-year expedition (1636–1640) across southern
China where he examined over 300 caves (including more than 100 from the Guilin
area; Sweeting 1995, Ravbar 2016). In his book, Xu Xiake’s Travels (rst published in
1642), he described underground streams and ponds, provided sketch maps of caves,
as well as proposed terminology for karst features; many of his speleological terms are
still used today (Ravbar 2016).
Figure 7. Hyleoglomeris xuxiakei sp. nov., holotype. A–C Habitus, dorsal, lateral and ventral views,
respectively.
Figure 8. Hyleoglomeris xuxiakei sp. nov., holotype. A Leg 17, anterior view B leg 18; anterior view
Cright half of telopods, posterior view D right half of telopods, anterior views.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
70
Diagnosis. Adult male of H. xuxiakei sp. nov. is distinct from other Hyleoglomeris
species based on the following combination of characters: (1) nearly pallid color (Fig.
7); (2) leg 17 with 3-segmented telopodite (Fig. 8A); (3) telopods with a low, oval-
shaped, central syncoxital lobe; (4) horns of syncoxital lobe without any structure on
top (Fig. 8D). is new species is clearly distinguished by the depigmented body (Fig.
3B) vs. vivid color pattern in H. rukouqu sp. nov. (Fig. 3A).
Description. Based on type specimens. Lengths of body ca 3.8–4.5 mm, width 2.5
–3.0 mm in both sexes. Coloration: entirely pallid (Figs 3B, 7). Head: Ommatidium
at least 5(6) + 1, translucent, barely visible (Fig. 7C). Tömösváry’s organ transverse-ov-
al, parallel to the body, only slightly wider than long. Antennae with four apical cones,
antennomere 6 ca 2.0 () or 1.8 () times as long as wide. Exoskeleton: Collum with
two transverse striae (Fig. 7C). oracic shield with a narrow hyposchism, the latter
reaching behind caudal tergal margin; 8–9 transverse striae: 4(5) starting below, one
level to, 3(4) above schism; 5 striae (never the rst and last from below) crossing the
dorsum. Following terga 3–11 with two striae above lateral edge. Pygidium of both
sexes regularly rounded at caudal margin. leg 17 with a low, subrounded, outer
coxal lobe; telopodite 3-segmented (Fig. 8A). leg 18 with an arch-shaped syncoxital
notch; telopodite 4-segmented (Fig. 8B). Telopods: (Fig. 8C–D) with a rather low,
oval-shaped, transverse, central syncoxital lobe anked by high setose horns, each of
the latter without any structure on top. Prefemur micropapillate laterally, with a well-
developed frontomesal trichostele. Femur with a smaller frontomesal trichostele. Cau-
domesal femoral process prominent, apically with an evident lobe strongly curved to
frontad. Tibia with a frontomesal seta. Caudomesal tibial process evident, recurved; a
distinct, papillate tubercle at base on caudal face. Tarsus strongly sigmoid, narrowly
rounded apically.
Habitat. is species was collected from a chamber within the estimated cave deep
zone, approximately 50 m from the cave entrance. Cave sediment was compact mud
with a small amount of rock breakdown from the ceiling.
Notes. Based on a depigmented habitus and translucent ommatidia, we consider
this species is a troglobiont.
Order Polydesmida Leach, 1815
Family Paradoxosomatidae Daday, 1889
Genus Hylomus Cook & Loomis, 1924
Type species. Hylomus draco Cook & Loomis, 1924.
Remarks. e genus is often referred to as “dragon millipedes” because of the para-
terga is antler-like, wing-shaped or spiniform. It can be characterized by the collum and
metaterga often with granulate, tuberculate and/or speculate; male femora (5, 6, 7 and/
or 9) often humped ventrally; and gonopods mostly suberect, some subfalcated, a short-
ened solenomere mostly sheathed by a usually condensed, rather simple solenophore
Cave-dwelling millipedes, Guangxi, China 71
(Liu et al. 2014, 2016). is genus encompasses 33 species distributed from China,
Laos, Vietnam and ailand (Srisonchai et al. 2018). At present, 19 species are known
in China and 13 are subterranean-adapted (Liu et al. 2016; Srisonchai et al. 2018).
Hylomus yuani sp. nov.
http://zoobank.org/89255A98-84A8-4D57-ADF4-F7B4F0BDBE48
Figs 3C, 9–12
Material examined. Holotype male (SCAU), China, Guangxi Zhuang Autonomous
Region, Lingchuan County, Liangfeng Cave [25°12'34.86"N, 110°31'56.8"E], 184 m
el., deep zone, direct intuitive search, 18 November 2016, J.J. Wynne leg. Paratypes, 1
male, 3 females (SCAU), same data as holotype.
Etymology. is species is named for Dr. Yuan Daoxian (袁道先), a preeminent
and globally recognized Chinese hydrologist. He has made numerous signicant con-
tributions in advancing both the science and management of karst and karst waters in
southern China since the 1960s.
Diagnosis. Adult males of H. yuani sp. nov. are distinct from other Hylomus spe-
cies based on the following combination of characters: (1) paraterga long and spini-
form only on collum and rings 2–6, short and coniform thereafter (Figs 9, 10A, B);
(2) collum with 8+8 frontal, 3+3 in the middle, 3+3 caudal, setigerous spinules; (3)
femur 6 strongly inated in distal 1/4 (Fig. 10D); (4) gonopod with a agelliform sole-
nomere and a strongly condensed solenophore (Figs 9–12). is new species is similar
to H.lui (a troglobiont from a cave in Guilin), but is distinguished by (1) paraterga
long and spiniform on collum and rings 2–6 (Fig. 9) vs. on collum and rings 2–5 in
H. lui; (2) collum and following metaterga with three transverse rows of spinules (Fig.
10A–B) vs. two transverse rows of spinules in H. lui.
Description. Based on type specimens. Lengths of body ca 27–28 (), 30–35 mm
(); width of mid-body pro- and metazonae 1.5–1.6 and 2.0 (), 2.0–2.2 and 2.5–2.6
mm (). Coloration: light brownish to nearly pallid (Figs 3C, 9–10). Antennomere
7 dark brown. Body: with 20 rings. In width, head < ring 2 < collum < 4–5 < 3 = 6–7
< 8–9 < 10–13; thereafter body gradually tapered posteriorly towards telson. Head:
densely setose, but more sparsely on vertex, epicranial suture conspicuous (Fig. 10A).
Antennae long and slender, reaching past ring 8 () or 7 () when extended posteri-
orly. Exoskeleton: Collum with 8+8 evident setigerous spinules arranged in a row at
front margin, behind it with 3+3 in the middle and 3+3 similarly spinules at posterior
margin. Metaterga 2–4 each with 5+5, 3+3 and 5+5(6) similarly setigerous spinules ar-
ranged in three transverse rows (Fig. 9A). Following metaterga with same sculpture, but
7–9+7–9 setigerous spinules at posterior margin, 2–4 spinules of them extended to the
lateral side (Figs 9C, 10B). Paraterga clearly spiniform, but well-developed only in para-
terga 1–6, directed more dorsad than laterad (Fig. 9A). Following paraterga increasingly
stout and short, paraterga 7–14 directed dorsolaterad, thereafter directed clearly caudad
(Figs 9C, 10A–B). Tegument shining, prozonae delicately microalveolate, metaterga
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
72
Figure 9. Hylomus yuani sp. nov., paratype. A Anterior part of body, dorsal view B anterior part of
body, ventral view C posterior part of body, dorsal view D posterior part of body, ventral view.
Cave-dwelling millipedes, Guangxi, China 73
Figure 10. Hylomus yuani sp. nov., paratype. A Mid-body rings, dorsal view B mid-body rings, lateral
views C sternite V, ventral view D femora 6 and 7, subventral view.
and surface below paraterga nely microgranulate. Constriction between pro- and
metazonae broad and shallow (Fig. 10A–B). Pore formula normal; transverse sulcus
usually very vague, but traceable in rings 5–19 (Fig. 10A). Ozopores inconspicuous,
located near the base on lateral side of pore-bearing paraterga (Fig. 10B). Pleurosternal
carinae evident only on rings 2 and 3 in both sexes, absent thereafter. Epiproct simple,
lateral pre-apical papillae distinct (Fig. 9C). Hypoproct subtrapeziform, caudal margin
emarginate, setigerous cones at caudal edge large, widely separated (Fig. 9D). Sterna
sparsely setose, cross-shaped impressions weak. A paramedian pair of short, rounded,
independent tubercles between coxae 4 (Figs 9B, 10C). Legs long and slender, ca
5.0 () or 3.5 () times as long as mid-body ring height. femur 6 strongly inated
ventrally in distal 1/4 (Fig. 10D). Gonopods: (Figs 11, 12) Coxite short, subcylindrical,
densely setose distodorsally, about 1/3 as long as telopodite. Prefemur densely setose
and about half as long as acropodite. Femorite elongate, slightly curved, with seminal
groove running entirely on mesal face. Solenophore (sph) strongly condensed; soleno-
mere (sl) agelliform, evidently separated at base from solenophore.
Habitat. is species was collected within the estimated cave deep zone, approximate-
ly 20 m from the cave entrance. Cave sediment was compact mud and the passageway was
swaddled by a slightly visible fog. is species and cave crickets (family Rhaphidophoridae)
were among the most abundant species within this portion of cave deep zone.
Notes. Based on the slender elongate antennae and legs, a depigmented cuticle, the
species is considered a troglobiont.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
74
Figure 11. Hylomus yuani sp. nov., paratype. A Right gonopod, lateral view B right gonopod, mesal views.
Figure 12. Hylomus yuani sp. nov., paratype. A Right gonopod, lateral view B right gonopod, mesal
views. Designations: sl = solenomere; sph = splenophore.
Cave-dwelling millipedes, Guangxi, China 75
Family Haplodesmidae Cook, 1895
Genus Eutrichodesmus Silvestri, 1910
Type species. Eutrichodesmus demangei Silvestri, 1910.
Remarks. e genus can be characterized by the body often capable of volvation,
with or without mid-dorsal projections; paraterga 2 strongly enlarged; and gonopod
femorite with a more or less distinct process or outgrowth laterally (Golovatch et al.
2009a, b). It encompasses 53 species distributed from south Japan, southern China, and
Southeast Asia to Vanuatu, Melanesia (Engho et al. 2015, Liu et al. 2017b). At pre-
sent, 23 species have been known in continental China, 20 are subterranean-adapted.
Eutrichodesmus jianjia sp. nov.
http://zoobank.org/403323E4-C776-4DC8-8795-9C53C3B64E02
Figs 3D, 13, 14
Type material. Holotype male (SCAU), China, Guangxi Zhuang Autonomous Re-
gion, Yangshuo County, Guanshan No. 4 Cave [24°56'58.34"N, 110°20'53.52"E],
186 m el., deep zone, direct intuitive search, 16 November 2016, J. J. Wynne leg.
Paratypes, 4 females, 1 juv. (SCAU), same data as holotype; 1 male (SCAU), same data
as holotype, but collected on mud bank.
Etymology. e species name, jianjia (肩甲), is used as a noun in apposition. is
phrase was used to denote the well-developed paraterga, which covers the millipede’s
legs much like the pauldrons of body armor cover the shoulder of the warrior.
Diagnosis. Adult males of E. jianjia sp. nov. is distinct from other Eutrichodesmus
species based on the following combination of characters: (1) collum with ve, and
metaterga 2–19 with three transverse rows of round microvillose tubercles (Fig. 13).
(2) gonopod acropodite with a dorsolateral tooth (t) at midway and apical with a large
tube-shaped lobe (l) (Fig. 14). is new species is clearly distinguished from E. lipsae (a
troglobiont from a cave in Guilin) by (1) metaterga without mid-dorsal projections vs.
most metaterga with mid-dorsal projections; (2) gonopod acropodite with a triangular,
ventral process (p) at about basal 1/3 (Fig. 14) vs. without this process in E. lipsae.
Description. Based on type specimens. Lengths of adult body ca 6.0–7.0 mm,
widths of mid-body pro- and metazonae 0.6–1.0 and 1.2–1.3 mm in both sexes. Col-
oration: generally light-yellowish to pallid (Fig. 3D). Body: subcylindrical, congloba-
tion complete, adults with 20 rings (Fig. 10A). Head: frons densely setose, nely micro-
granulate on vertex, with a paramedian pair of rounded knobs above antennal sockets.
Epicranial suture conspicuous. Antennae short, slightly clavate. Exoskeleton: Collum
subtrapeziform, slightly broader than head, not covering the latter from above, with ve
transverse rows of round microvillose tubercles (Fig. 13B). Metaterga 2–19 each with
three transverse mixostictic rows of similar tubercles extending onto paraterga, about
6–8+6–8 per row. e middle row of tubercles slightly larger than others. Pre-anal ring
short, with four transverse rows of small tubercles (Fig. 13D, E). Paraterga with evident
shoulders anteriorly, strongly declivous, broad and usually triobate laterally, evidently
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
76
Figure 13. Eutrichodesmus jianjia sp. nov., paratype. A Habitus, lateral view B anterior part of body,
ventral view C anterior part of body, dorsal view D posterior part of body, ventral view E posterior part
of body, lateral view.
Figure 14. Eutrichodesmus jianjia sp. nov., paratype. A Left gonopod, lateral view B left gonopod,
mesal view. Designations: dp = distofemoral process; l = lobe; p = process; t = tooth.
extending down below level of venter; caudolaterally at base with two distinct lobula-
tions (Fig. 13A). Paraterga 2 strongly enlarged. Tergal setae and ozopores invisible. Ozo-
pores hardly visible. Prozonae nely alveolate; constriction between pro- and metazoan
Cave-dwelling millipedes, Guangxi, China 77
narrow and shallow. Epiproct apically with four spinnerets. Hypoproct subtrapeziform,
with two long setae. Sterna narrow, but much broader between coxae 6–7 and 9.
Gonopod aperture suboval. Legs long and slender, but hardly reaching tips of paraterga.
Gonopods: (Fig. 14) Coxite large, abundantly setose and micropapillate ventrolaterally.
Telopodite subfalcate, distinctly curved ventrad, setose in its basal part, with a promi-
nent, denticulate, lateral, distofemoral process (dp) at midway. Acropodite with a trian-
gular, ventral process (p) at about basal one-third and a dorsolateral tooth (t) at midway;
apical with a large tube-shaped lobe (l). Seminal groove long, terminating without hair.
Habitat. Specimens were collected in the same general location as H. xuxiakei sp.
nov. specimens. us, refer to the H. xuxiakei sp. nov. habitat description.
Notes. Based on the long slender legs and a depigmented cuticle, we consider this
species a troglobiont.
Family Cryptodesmidae Karsch, 1880
Genus Trichopeltis Pocock, 1894
Type species. Cryptodesmus bicolor Pocock, 1894.
Remarks. e genus can be characterized by the metaterga distinctly several trans-
verse rows of tuberculations, usually setose, and gonopod usually foliate, with a tri-
partite or deeply notched telopodite. It encompasses 12 species distributed from the
Himalayas of India, through Bangladesh, Myanmar to southern China, Laos, Viet-
nam, Cambodia and Indonesia (Likhitrakarn et al. 2017). At present, 5 species have
been known in China, 4 are subterranean-adapted.
Trichopeltis liang fengdong sp. nov.
http://zoobank.org/7E972E70-ADDA-4CA1-924F-3016EF5E3FA7
Figs 4A, 15–17
Type material. Holotype male (SCAU), China, Guangxi Zhuang Autonomous Re-
gion, Lingchuan County, Liangfeng Cave [25°12'34.86"N, 110°31'56.8"E], 184 m
el., deep zone, steam bank, direct intuitive search, 18 November 2016, J.J. Wynne leg.
Paratypes, 4 females (SCAU), same data as holotype.
Etymology. is species name, liangfengdong, is used as a noun in apposition and
is the name of the type locality.
Diagnosis. Adult male of T. liangfengdong sp. nov. is distinct from other Trichopeltis
species based on the following combination of characters: (1) metaterga 2–15 with four
transverse rows of small, setigerous tubercles (Fig. 15B); (2) gonopod coxae without
seta and acropodite with several small subapical lobules (los) (Fig. 17). is new species
is similar to T. reexus (a troglobiont from a cave in Hunan), but is distinguished by (1)
metaterga 2–15 with four transverse rows of setigerous tubercles vs. two transverse rows
in T. reexus; (2) tip of acropodite bid (Fig. 17) vs. distorted in T. reexus.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
78
Description. Based on type specimens. Length of both sexes ca 14.0–15.0 mm,
widths of mid-body pro- and metazonae 1.5–2.0 and 4.8–5.0 mm. Coloration: gener-
ally pallid (Fig. 4B). Body: with 20 rings (Fig. 15). In width, collum < ring 2 < 3 = 4
< 5 < 6 < 7–16; thereafter body gradually tapered posteriorly towards telson. Head:
densely pilose and microgranulate, epicranial suture present (Fig. 16A). Antennae
long, reaching past ring 3 when extended posteriorly; in length, antennomere 6 = 5 >
4 = 3 > 2 > 7 > 1. Exoskeleton: Collum fan-shaped (Fig. 15A), covering the head from
above, dorsal surface with irregular several small, round, setigerous tubercles. Marginal
lobules on collum: 13+13 small, setigerous, rounded anteriorly, 7+7 relative larger,
laterally and 5+5 very small caudally. Mid-dorsal regions on rings 2–15 with four more
or less regular, transverse rows of similarly small, setigerous tubercles, 4–5 + 4–5 per
row (Figs 15B, 16B). Several tubercles extending onto paraterga. Following metaterga
with ve rows of smaller tubercles, 6–7 + 6–7 per row (Fig. 15B). Paraterga strong-
ly developed, clearly upturned dorsally above the dorsum only on the collum, other
paraterga at. Each with 5–6 small, dentiform, lateral and 7–8 much larger, squarish
caudolateral lobules, all evident, setigerous and microvillose (Figs 15, 16A, B). Cau-
Figure 15. Trichopeltis liangfengdong sp. nov. holotype. A Habitus, ventral view B habitus, sublateral view.
Cave-dwelling millipedes, Guangxi, China 79
Figure 16. Trichopeltis liangfengdong sp. nov., holotype. A anterior part of body, ventral view B anterior part
of body, dorsal view C sterna 6 and 7, ventral view D right gonopod, mesal view E right gonopod, lateral view.
dolateral lobules on paraterga mostly oblong, relatively large, and well separated from
one another (Fig. 16A). Caudolateral corner of paraterga projecting behind rear ter-
gal margin on rings 15–19 (Fig. 15). Integument clearly microgranulate throughout,
prozonae nely alveolated. Limbus regularly crenulated. Stricture between pro- and
metazonae broad, shallow and nely microgranulated. Tergal setae simple and short
(Fig. 16A, B). Ozopores invisible, pore formula untraceable. Epiproct short, with four
spinnerets apically. Hypoproct subtrapeziform, 1+1 caudal setigerous papillae clearly
separated. Pleurosternal carinae present on rings 2 and 3 in both sexes. Sterna mod-
estly setose, cross-shaped impressions moderate, broadened between coxae 9 (Fig.
16C). Legs long and slender, unmodied, produced beyond paratergal lateral margin
(Fig. 15), about 1.8 times as long as mid-body ring height in both sexes. Gonopods:
(Figs 16D, E, 17) Coxite short and squarish, without seta. Prefemur densely setose and
a particularly long setae; nearly half the length of telopodite. Femorite strongly at-
ten, pie-shaped, with a small lobe (l) ventrally. Acropodite folded, with several small
subapical lobules (los), tip bid. Seminal groove terminating with a hairy pulvillus,
forming no distinct solenomere.
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80
Habitat. Specimens were collected in the same general location as H. yuani sp.
nov. specimens. us, refer to the H. yuani sp. nov. habitat description.
Notes. Based on the long slender antennae and legs and a depigmented cuticle, the
species is considered a troglobiont.
Family Polydesmidae Leach, 1815
Genus Pacidesmus Golovatch, 1991
Type species. Pacidesmus shelleyi Golovatch, 1991
Remarks. e genus can be characterized by metaterga often with three transverse
rows of 3+3 sculpture, and gonopod structure showing no prominent clivus to recurve
laterad of the seminal groove (Golovatch and Georoy 2006). It encompasses 9 spe-
cies, only the type species from a mountain in Chiengmai, ailand, all other 8 species
have been known from caves in China.
Figure 17. Trichopeltis liangfengdong sp. nov., holotype. A Left gonopod, mesal view B left gonopod,
lateral view. Designations: l = lobe; los = lobules.
Cave-dwelling millipedes, Guangxi, China 81
Pacidesmus tridus Golovatch & Georoy, 2014
Fig. 4B
Material examined. 6 males, 3 females (SCAU), China, Guangxi Zhuang Autonomous
Region, Yangshuo County, Guanshan No. 4 Cave [24°56'58.34"N, 110°20'53.52"E],
186 m el., deep zone, direct intuitive search, 16 November 2016, J.J. Wynne leg. 1
male, 1 juv. (SCAU), China, Guangxi Zhuang Autonomous Region, Xiufeng District,
Maomaotou Cave [25°18'46.12"N, 110°16'12.64"E], 225 m el., deep zone, direct in-
tuitive search, 15 November 2016, J. J. Wynne leg. 2 males, 1 female, 4 juv. (SCAU),
China, Guangxi Zhuang Autonomous Region, Yangshou County, Shangshuiyan Cave
[24°57'43.6"N, 110°20'37.21"E], 191 m el., deep zone, direct intuitive search, 17
November 2016, J. J. Wynne leg.
Notes. is troglobiont was rst found in Skeleton Cave [25°17'13"N, 110°13'26"E],
el. 186 m (Golovatch and Georoy 2014). We later conrmed P. tridus within three caves
with the furthest cave (Guanshan # 4) approximately ~13 km to the south of type locality.
e three caves where we detected P. tridus are separated by a distance of ~41 km. e
northernmost cave, Maomaotou Cave occurs 39.6 km north from Guangshan No. 4 Cave
and Shangshuiyan Cave, which are co-located occurring within 1 km of each other. As it
is currently morphologically described as one species, it now has a regional distribution.
Habitat. is species was collected from the estimated deep zones of the three
caves. For Maomaotou cave, we collected it within bamboo detritus at mid-cave. In
Shangshuiyan Cave, specimens were collected within decomposing detritus and along
muddy cave sediment deposits within a sinuous passageway. For Guangshan No. 4
Cave, refer to habitat descriptions of H. xuxiakei sp. nov.
Order Spirostreptida Brandt, 1833
Family Pericambalidae Silvestri, 1909
Genus Bilingulus Zhang & Li, 1981
Type species. Bilingulus sinicus Zhang & Li, 1981.
Remarks. e genus can be characterized by the lingular lamellae divided into two
parts. legs 1 with a syncoxite carry a pair of long, band-like coxal process; femur
with a nger-shaped process at the end protruding posteriorly, tarsus without claw at
the end. Anterior gonopod with a very broad coxa; telopodite of posterior gonopod
slender, devoid of branch (Zhang and Li 1981).
Bilingulus sinicus Zhang & Li, 1981
Material examined. 3 males, 3 females, 5 juv. (SCAU), China, Guangxi Zhuang
Autonomous Region, Yangshou County, Shangshuiyan Cave [24°57'43.6"N,
110°20'37.21"E], 191 m el., deep zone, cartography station #19, direct intuitive
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
82
search, 17 November 2016, J.J. Wynne leg. 4 females (SCAU), China, Guangxi
Zhuang Autonomous Region, Xiufeng District, Maomaotou Cave [25°18'46.12"N,
110°16'12.64"E], 225 m el., deep zone, direct intuitive search, 15 November 2016,
J.J. Wynne leg. 1 juv. (SCAU), China, Guangxi Zhuang Autonomous Region, Ling-
chuan County, Liangfeng Cave [25°12'34.86"N, 110°31'56.8"E], 184 m el., deep
zone, direct intuitive search, 18 November 16, J.J. Wynne leg.
Notes. is species lacked characters suggestive of troglomorphy. It had a pigment-
ed cuticle and ommatidia were present. us, B. sinicus is considered a troglophile. It
was rst described by Zhang and Li (1981) from a cave in Guilin; no cave name or
coordinate data were provided. While we detected this species in three dierent Guilin
caves, we’re unable to determine a distance from the type locality. e caves where we
detected P. tridus is separated by an average distance of 34.1 km. Maomaotou Cave
occurs to the north-northwest and is 45 km from Liangfeng Cave and 40.4 km to the
north of Shangshuiyan Cave. Based upon its epigean characteristics and that this spe-
cies is regionally distributed on the landscape, we consider it a troglophile.
Family Cambalopsidae Cook, 1895
Genus Glyphiulus Gervais, 1847
Type species. lulus (recte: Julus) granulatus Gervais, 1847.
Remarks. e genus has been divided into two groups, granulatus-group and ja-
vanicus-group. Both groups shared the same gonopods characters as the anterior gono-
pods usually with a plate-like coxosternum, 1-segmented telopodite. Posterior gonop-
ods highly compressed, showing a plumose, subagelliform, distal process (Golovatch
et al. 2007). It encompasses over 60 species distributed in Southeast Asia and southern
China. At present, 42 species have been known in China, 34 are subterranean-adapted.
e below two species belong to granulatus-group because legs 1 strongly reduced,
sternum devoid of median structures.
Glyphiulus melanoporus Mauriès & Nguyen Duy-Jacquemin, 1997
Material examined. 1 male, 1 female, 1 juv. (SCAU), China, Guangxi Zhuang Autono-
mous Region, Xiufeng District, Maomaotou Cave, [25°18'46.12"N, 110°16'12.64"E],
225 m el., deep zone, direct intuitive search, 15 November 2016, J. J. Wynne leg.
Notes. G. melanoporus is considered a troglophile. e type locality for this species
is Skeleton Cave [25°17'13"N, 110°13'26"E] (Mauriès and Nguyen Duy-Jacquemin
1997). We collected this species from Maomaotou Cave, which represents a 21.1 km
range expansion to the south of the type locality.
Habitat. For our specimens, we collected them within the deep zone of Maomao-
tou Cave. Sediment where specimens were collected was compacted and wet.
Cave-dwelling millipedes, Guangxi, China 83
Glyphiulus maocun sp. nov.
http://zoobank.org/5CDE1D3A-71A2-48EA-B4BB-F9FDD20D860D
Figs 4C, 18–20
Type material. Holotype male, China, Guangxi Zhuang Autonomous Region, Ling-
chuan County, Maocun Village, Liangfeng Cave [25°12'34.86"N, 110°31'56.8"E],
184 m el., deep zone, direct intuitive search, 18 November 2016, J.J. Wynne. Para-
types, 4 females, 4 juv. (SCAU), same data as holotype.
Etymology. e species name, maocun, is used as a noun in apposition and is the
name of the village nearest to the type locality.
Diagnosis. is new species is similar to G. melanoporus (from caves in Guilin)
in showing carinotaxy formula of collum I–IV+5c+6a+pc+ma. However, G. maocun
sp. nov. is distinct from G. melanoporus by (1) carinotaxy formula of metaterga 2/2+I/
Figure 18. Glyphiulus maocun sp. nov., holotype. A , B Anterior part of body, sublateral views C mid-
body rings, dorsal view D posterior part of body, ventral view.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
84
Figure 19. Glyphiulus maocun sp. nov., holotype. A Head and collum, dorsal view B head, collum, and
legs 1, ventral view C legs 1, anterior view D leg 2, caudal view E legs 3, frontal view F anterior gonopods,
caudal view G posterior gonopods, anterior view H posterior gonopods, caudal view.
i+3/3; (2) anterior gonopod with a conspicuous, high, curved downward process on
coxosternum (Figs 19F, 20A); (3) posterior gonopod tip branch plumose agellum
(Figs 19G–I, 20B, C).
Cave-dwelling millipedes, Guangxi, China 85
Figure 20. Glyphiulus maocun sp. nov., holotype. A Anterior gonopods, caudal view B posterior gonop-
ods, anterior view C posterior gonopods, caudal view.
Description. Based on the type specimens. Lengths of both sexes ca 26–32 mm,
mid-body rings round in cross-section, their widths and heights similar, 1.2–1.8 mm.
Coloration: yellow-brown to brownish in alcohol. Ommatidia blackish (Fig. 18A).
Body: with 46–54 podous rings + 2–1 apodous one(s) + telson. Head: clypeus with
4 teeth anteromedially. Each eye patch with about 8–12 ommatidium arranged in
three irregular vertical rows (Figs 18A, 19A). Antennae long, antennomere 7 with
four short apical cones (Fig. 18A, B). Gnathochilarium usually, with a separate pro-
mentum (Fig.19B). Exoskeleton: Carinotaxy formula of collum I–IV+5c+6a+pc+ma,
anterior margin crests lower (Fig. 19A). Subsequent metaterga strongly crested, cari-
notaxy formula 2/2+I/i+3/3. Ozoporiferous tubercles round (Fig. 18). Prozonae deli-
cately alveolate; strictures and metazonae ne longitudinal striations. Rings 2 and 3
with long pleural aps. Epiproct simple, with a short, low, rounded tubercle medially.
Paraprocts rather regularly convex. Hypoproct broadly emarginated (Fig. 18D).
legs 1 very strongly reduced, represented only by a sternum devoid of any median or
paramedian structures but carrying 1+1 strongly separated prongs both curved ante-
riad and bearing several strong setae (Fig. 18B, C). legs 2 with large coxae; penes
oblong, each with two strong setae distolaterally (Fig. 19D). legs 3 with slender
and elongate coxae (Fig. 19E). Legs slender, about 1.2 times as long as mid-body ring
height. Claw simple, without any spine at base. Anterior gonopods: (Figs 19F, 20A)
with a conspicuous, high, lobe-shaped, curved downward process on coxosternum,
which is much higher than telopdite; telopodite slightly coiled, 1-segmented, lateral
in position, with 2 or 3 strong apical setae. Posterior gonopods: (Figs 19G–I, 20B, C)
laterally with a low, lateral lobe carrying a dozen of long setae, tip branch very slender
and high, plumose agellum.
Habitat. Specimens were collected within or at proximity to ood detritus.
Notes. Specimens exhibited no characteristics suggestive of cave adaptation. It had
a pigmented cuticle and well-developed blackish ommatidia. We consider this species
to be troglophillic within Liangfeng Cave. Subsequently, this species may have a larger,
more regional distribution.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
86
Discussion
Our work increased the number of subterranean-adapted millipedes from 34 to 38
species. With 564 known caves in Guangxi (Yuanhai Zhang, pers. comm. 2019), but
a fraction (8.7% or 49 caves) of these caves have been examined for troglomorphic
millipedes. e identication of six new species of millipedes from four caves in the
Guilin area underscores the potential for many additional discoveries. For millipede-
specic surveys, direct intuitive searches of selected cave deep zones (sensu Wynne et
al. 2019) has been identied as the best technique; Mesibov et al. (1995) reported that
four weeks of hand collecting during the fall was more ecient than an intensive pitfall
trapping eort involving trapping seven days per month for over one year.
Conversely, while advancing our knowledge of regional troglomorphic millipede
diversity stands to contribute signicantly to the conservation value of the SCK, a more
comprehensive understanding (i.e., for all cave-dwelling taxa) of regional diversity, as
well as advancing procedures to assessing the vulnerability of cave systems to anthro-
pogenic impact should be considered. Wynne et al. (2018, 2019) provides a system-
atic framework and guidance for sampling cave-dwelling arthropods using a repeatable
framework, which can be modied for application in the SCK. Using such an approach,
these data may be then be examined by applying principles similar to the cave vulner-
ability assessment developed by Tanalgo et al. (2018). rough such an eort, system-
atic techniques may be used to assemble robust and comparable landscape scale data,
and each cave subsequently be evaluated for its vulnerability due to human activities.
Moreover, for conservation biologists and resource managers to best evaluate the
importance of SCK cave biological diversity, we will require a more robust understand-
ing of the distributional ranges of troglomorphic species (as well as other subterranean-
restricted taxa). Specically, while nearly 40 percent of troglomorphic millipedes were
identied as single cave endemics, 14 troglobionts (including one whose range was
expanded from this work) occurred within two or more caves. One species, P. tridus,
was conrmed within three caves in the Guilin region (two caves from this work, plus
the type locality); the maximum distance between caves for this species was 59.7 km.
ree additional subterranean-adapted species occurred in multiple caves with maxi-
mum distances ranging from 81.27 and 137.6 km (Table 3). As many troglomorphic
arthropods are identied as short-range endemic species, occurring in a single cave
or geological formation (Reddell 1994, Culver et al. 2000, Christman et al. 2005,
Deharveng et al. 2008, Tian 2011, Harvey and Wynne 2014, Gao et al. 2018, Nitzu
et al. 2018) and that rivers and valleys/ lowland areas often result in vicariance (Barr
1985, Faille et al. 2015, Katz et al. 2018), the genetic relatedness of at least these three
species should be further examined using genetic techniques. While these species may
be morphological similar, we suggest they may be genetically distinct – potentially
representing dierent subspecies or lineages.
We also reported a possible ‘disturbance relict’, H. rukouqu sp. nov., discovered
within a cave entrance vegetation community. As similar cave entrance vegetation
Cave-dwelling millipedes, Guangxi, China 87
communities have been identied as either supporting distinct relict plant communi-
ties and/or plant species in southern China (Monro et al. 2018), Easter Island, Chile
(Wynne et al. 2014), and west-central New Mexico, USA (Lindsey 1951, Northup and
Welbourn 1997, Wynne 2013), their importance in supporting cave-restricted arthro-
pod populations demonstrated (Northup and Welbourn 1997, Wynne 2013, Wynne
et al. 2014, Wynne and Shear 2016), and widespread land cover conversion of both
lowlands and uplands has occurred in China since 1958, this nding warrants both
additional research into this species distribution, as well as a larger scale examination
of other potential ‘disturbance relict’ arthropod species within cave entrance vegetation
communities of the SCK.
Although caves are often considered distinct from the surface environment, cave
ecosystems are inextricably linked to surface processes. Caves require an allochthonous
energy supply, which may include ood detritus, guano deposition from bats, birds and
crickets, and dissolved organic materials that percolate from the surface. us, when
humans adversely change the surface environment, the cave ecosystem may change as
well. Deforestation (Trajano 2000, Ferreira and Horta 2001, Clements et al. 2006,
Stone and Howarth 2007), intensive agriculture and water diversion (van Beynen
and Townsend 2005, Stone and Howarth 2007, Harley et al. 2011), livestock grazing
(Stone and Howarth 2007), alien species introductions (Elliott 1992, Reeves 1999,
Taylor et al. 2003, Howarth et al. 2007, Price 2016), heavy metals and agrochemicals
(Whitten 2009), and global climate change (Chevaldonné and Lejeune 2003, Mam-
mola et al. 2018) have negatively aected both cave organisms and ecological processes.
Despite the impressive biological diversity found in China, there are no govern-
ment regulations, nor is any government agency responsible for managing and protect-
ing cave resources. Development projects typically progress in caverniferous regions
and tourist caves are developed without consideration for subterranean resources and
the rich biodiversity they often support (Whitten 2009). While we recognize environ-
mental conditions are improving and environmental regulations have strengthened in
China, Whitten (2009) and Cao et al. (2007) identied most of the aforementioned
impacts continue to expand and severely stress both epigean and hypogean ecosystems
in southern extent of the country. us, we recommend monitoring environmental
conditions of the surface and subsurface of caves identied as supporting rare endemic
species populations and/or sensitive ecosystems.
is paper revealed that at least 38 troglomorphic millipede species occur in
Guangxi. Other examples of SCK’s high cave diversity includes at least 19 species of
troglomorphic pseudoscorpions (Gao et al. 2018), 29 vascular plant species believed
restricted to cave entrances (Monro et al. 2018), and the richest globally diversity of
caveshes with at least 154 species and nearly half of these species considered single
cave endemics (Zhao et al. in press). As this work continues, we anticipate the number
of subterranean-adapted millipedes, as well as other arthropod species will increase.
rough ours and other eorts, we believe the SCK will ultimately emerge as a global
hotspot for cave biological diversity.
Weixin Liu & J. Judson Wynne / Subterranean Biology 30: 57–94 (2019)
88
Acknowledgements
Dr. Wang Jietao at the Wuhan Center, China Geological Survey provided eldwork and
logistical support and developed part of gure 1. We thank International Research Cent-
er on Karst in Guilin for additional logistical support. Mr. Zhang Yuanhai provided us
with information regarding regional caves while Dr. Qiang Li provided cave coordinates
for some of the caves examined in this study. Dr. Wu Zhuoting oered additional assis-
tance with some of the Mandarin names. Dr. Sergei Golovatch provided us with invalu-
able peer-review comments leading to the improvement of this manuscript. Fieldwork
was recognized as an Explorers Club ag expedition. e lead author was sponsored by
the National Natural Science Foundation of China (Grant no. 31801956 and Grant no.
41871039) for work related to species’ descriptions and manuscript preparation.
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... Jeekel 2004;Shear 2011;Enghoff et al. 2015) or an independent family (e.g. Wang and Mauriès 1996;Ying 1998;Shelley 2003;Liu and Wynne 2019;Golovatch and Liu 2020). ...
... Information on the type locality of this species is ambiguous, only described as Guilin, Guangxi . Liu and Wynne (2019) collected this from three caves. Specimens used in this research were collected from Juzi Cave that is very close to the Shangshuiyan Cave reported in Liu and Wynne (2019). ...
... Liu and Wynne (2019) collected this from three caves. Specimens used in this research were collected from Juzi Cave that is very close to the Shangshuiyan Cave reported in Liu and Wynne (2019). In addition, with morphology mostly identical to that of the original description, these were identified as Pericambala sinica (Zhang & Li, 1981), comb. ...
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The millipede subfamily Pericambalinae Silvestri, 1909 is poorly understood and the taxonomic status remains controversial. Pericambalinae was regarded as either a subfamily of Cambalopsidae or an independent family. To address this issue, we conducted a molecular phylogenetic analysis and a morphological revision, and the genera and species from China are also revised. The results support the recovery of the family status, Pericambalidae, stat. nov. The morphological differences between Bilingulus Zhang & Li, 1981 and Parabilingulus Zhang & Li, 1981 are shown to be caused by post-embryonic development (anamorphosis and non-systemic metamorphosis) and both of these should be junior synonyms of Pericambala Silvestri, 1909 (Pericambala = Bilingulus, syn. nov. = Parabilingulus, syn. nov.). Three new combinations are proposed: Pericambala simplicia (Mauriès & Nguyen Duy-Jacquemin, 1997), comb. nov., Pericambala aramula (Zhang & Li, 1981), comb. nov. and Pericambala sinica (Zhang & Li, 1981), comb. nov. The mature specimens of Pericambala simplicia, comb. nov. and Pericambala aramula, comb. nov. were collected from the type localities and are described for the first time. A new species, Pericambala cordata, sp. nov. is described. After revision, Pericambalidae contains two genera and six species with one genus and four species recorded from China. Due to a deficiency in outgroup sampling, the phylogenetic status of Pericambalidae in the suborder Cambalidea remains uncertain. Variation of the gnathochilarium in Cambalidea is discussed and a key to the species of Pericambala in China is also provided. This research lays a foundation for further revision of Cambalidea in the future. ZooBank: urn:lsid:zoobank.org:pub:BDA46BCE-102B-45FE-A963-47F029A09E76.
... Vascular and bone-related outcomes as well as increased mortality are a direct effect of sHPT. [5] After renal transplantation, renal function increases and the mineral metabolism dramatically improves. Renal function increases and mineral metabolism significantly improves following renal transplantation. ...
... The benefits of PTX on mortality rates observed in dialysis patients have not been demonstrated in patients receiving a kidney transplant. [4,5] First Point. The endocrine system comprises four small glands called parathyroid glands, which are typically located behind the thyroid's left and right lobes. ...
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Background: Persistent secondary hyperparathyroidism after renal transplantation is common, and risk factors for posttransplant secondary hyperparathyroidism are pre-transplant levels of PTH and calcium, time spent on dialysis before transplantation, and nodular hyperplasia of the parathyroid glands. Purpose: This study aimed to determine the frequency and risk factors of persistent hyperparathyroidism one-year post-kidney transplant. Methodology: Cross-Sectional Hospital-based study was conducted in a period from September 2018 to March 2019 in Ibn Sina Hospital and Ahmed Gasim Hospital and covered 81 study participants. Results: Pre-kidney transplantation PTH level, (58%) reported mild increase in PTH level, (37.1%) reported moderate increase while only (4.9%) had a severe increase. Post-kidney transplant PTH, (60.5%) reported normal levels of PTH, (34.6%) a mild increase while (4.9%) reported a moderate decrease in PHT. After three months of PKT, serum calcium was high in (38.3%) and low phosphate (2.5%). After one year of PKT, serum calcium was high in (8.6%) and low phosphate (2.5%). a significant reduction in the PTH after KT compared with PTH levels before KT (p-value < 0.001) and the association between PKT level of PTH with age, gender and duration of dialysis before KT (P value < 0.05). Conclusion: Obtaining a level of PTH adequate to the graft function and to normalize levels of calcium, and phosphorus as a primary clinical objective for patients with secondary HPT after renal transplantation in Sudan. Risk factors such as age, duration of dialysis, and pre-transplantation level of PTH should be taken into account in the management policy after renal transplantation. Keywords: frequency; risk; factors; persistent; Hyperparathyroidism; post-kidney; transplan
... South-East Asia is an important biodiversity hotspot (Sodhi et al. 2004, Clements et al. 2006, and the high species' richness of millipedes, including dragon millipedes, is indeed remarkable. Intensive field surveys in several areas in mainland South-East Asia have been made in the past 10 years and have revealed numerous species of spectacular dragon millipedes (Liu et al. 2014, Likhitrakarn et al. 2015, Srisonchai et al. 2016, 2018a-d, 2020, Liu and Wynne, 2019, Nguyen and Sierwald 2019. All dragon millipede genera are generally considered as locally endemic for the region, and with a few exceptions, such as the widespread and in part synanthropic D. planata, they have limited dispersal capacity (Srisonchai et al. 2018a, Liu andWynne 2019). ...
... Intensive field surveys in several areas in mainland South-East Asia have been made in the past 10 years and have revealed numerous species of spectacular dragon millipedes (Liu et al. 2014, Likhitrakarn et al. 2015, Srisonchai et al. 2016, 2018a-d, 2020, Liu and Wynne, 2019, Nguyen and Sierwald 2019. All dragon millipede genera are generally considered as locally endemic for the region, and with a few exceptions, such as the widespread and in part synanthropic D. planata, they have limited dispersal capacity (Srisonchai et al. 2018a, Liu andWynne 2019). Their distribution patterns are thus likely to have been affected by ancient events and could reveal important insights into the historical biogeography of mainland South-East Asia. ...
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Recent taxonomic revision of the strikingly ornamented millipedes known as ‘dragon millipedes’ in the family Paradoxosomatidae, has revealed generic division into six genera. The majority of species are distributed in mainland South-East Asia and each genus is restricted to a well-delimited area. However, their evolutionary history has remained poorly understood, particularly the relationships among genera and their biogeographic distribution. We present a comprehensive and well-resolved molecular phylogeny based on mitochondrial and nuclear genes. A dataset of 256 sequences representing 40 dragon millipede species was newly generated and analysed in order to reveal the relationships and to explore the origin using ancestral range reconstruction. All dragon millipedes were retrieved together as monophyletic, each genus except Hylomus forming a distinct clade with strong statistical values, supporting the previous classification using morphology. A new monotypic genus and new species, Siamaxytes bifurca Srisonchai and Panha gen. nov. et sp. nov., was revealed based on distinct morphological and DNA data. The Tenasserim mountain range was inferred to be the centre of origin of dragon millipedes with a series of subsequent diversifications across mainland South-East Asia. Our analysis provides evidence that both dispersal and vicariance presumably played a role in shaping these millipedes’ distribution and diversification.
... Glyphiulus Gervais, 1847 is the largest genus in the millipede family Cambalopsidae, currently comprising 70 species (Likhitrakarn et al. 2017;Liu and Wynne 2019;Jiang et al. 2021Jiang et al. , 2022. They range from southern China in the north to Java and Borneo in the south and southeast, being particularly common in caves and usually very narrow in distribution, except for G. granulatus (Gervais, 1847) which is pantropical (Likhitrakarn et al. 2021). ...
... Photographs of specimens were taken with a Keyence VHX-5000 digital microscope and edited using Adobe Photoshop CS6 software. The terminology used in the text is after Golovatch et al. (2007aGolovatch et al. ( , b, 2011a, Liu and Wynne (2019), Jiang et al. (2017Jiang et al. ( , 2018Jiang et al. ( , 2020 and Likhitrakarn et al. (2017Likhitrakarn et al. ( , 2021. The distribution map was created using QGIS 3.20.1 software. ...
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The javanicus -group of Glyphiulus is re-assessed and its Chinese component species are presently divided between the following two newly-circumscribed species groups, i.e. the formosus - and the sinensis -group. The two can be differentiated, based on the diagnostic characters of the first pair of legs in the male. In addition, metatergal crests being complete and the carinotaxy formula on the collum being I–III+P+M are only characteristic of the formosus -group. A molecular phylogeny of the genus, based on DNA sequencing of four gene fragments of four genes, allows for Glyphiulus to be recovered as a monophyletic group, the phylogenetic relationship being ((Clade A, Clade B), Clade C). Molecular evidence is fully congruent with the morphological one. In addition, based on barcoding data, interspecific p-distances between Glyphiulus species amount to 11.2–24.9%, vs. 0–8.2% for intraspecific p-distances. Five new species of Glyphiulus , all cavernicolous, are described from China: G. sinuatoprocessus Zhao & Liu, sp. nov. , G. conuliformis Zhao & Liu, sp. nov. (both from Guangdong Province), G. xiniudong Zhao & Liu, sp. nov. , G. scutatus Zhao & Liu, sp. nov. and G. portaliformis Zhao & Liu, sp. nov. (all three from Guangxi Zhuang Autonomous Region). The known Chinese species of the formosus -group appear to mainly be confined to the South China region.
... While the species checklist published in 2018 mentioned 29 Juliformia (9 Spirobolida, 20 Spirostreptida), only four species of the extinct Cambalidea (a suborder of Spirostreptida) family Electrocambalidae have been described so far (Moritz & Wesener, 2021). Based on this result, the currently known fossil Cambalidea are not related to the megadiverse extant family Cambalopsidae (Golovatch et al., 2007a(Golovatch et al., , 2007b(Golovatch et al., , 2009Jeekel, 2004;Jiang et al., 2021;Likhitrakarn et al., 2024;Liu & Wynne, 2019). In order to get a better understanding about the evolution of a megadiverse group of soil arthropods, we describe here the first fossil and oldest known representative of the Spirostreptida family Cambalopsidae with a detailed 3D reconstruction of the male gonopods. ...
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Micro computed tomography (µCT) scans allow a 3D reconstruction of characters otherwise hidden in fossil amber specimens. In this study we reveal the male copulatory legs (gonopods) retracted into the body, and other important morphological characters, for a fossil Juliformia millipede. Characters of the male gonopods are essential for the classification of numerous recent millipede groups. This made it previously almost impossible to correctly assign fossil millipedes to a recent taxon, especially in the Juliformia, where the gonopods are often retracted into the body. The millipede specimen analyzed here is preserved in Myanmar amber dating back to the Cretaceous, 98 MYA (± 0.63 MY). Gonopod and mouthpart characters identify the millipede as a member of the order Spirostreptida, family Cambalopsidae, the first known fossil of one of the most diverse extant SE Asians millipede groups. While the gonopods show similarities to the extant genera Hypocambala Silvestri, 1897, Plusioglyphiulus Silvestri, 1923 and Glyphiulus Gervais, 1847, the presence of neither carinate body rings, nor longitudinally striate metazona, nor a flattened leg pair 2, absence of both an enlarged collum and an enlarged leg pair 2 allows us to describe it as a new genus and species, Laeviglyphiulus patrickmuelleri n. gen., n. sp.
... Cavernas são ambientes únicos do ponto de vista ecológico, com habitats fisicamente diferenciados do meio externo e com características estáveis do ponto de vista climático quando comparado aos ambientes epígeos, com poucas variações dentro da mesma estação ou anualmente (GÖKTÜRK et al., 2011;LIANG et al., 2019;ZHU et al., 2020). Além de estáveis, os habitats subterrâneos são caracterizados pela escassez total ou baixa luminosidade, afetando significativamente a disponibilidade de recursos para os seres vivos fotodepedentes, como as espécies vegetais, selecionando espécies que adotam estratégias adaptativas fascinantes de sobrevivência nestes ambientes (LIU et al., 2019;KIEW, RAHMAN, 2021;SIEVERS et al., 2022). ...
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The subterranean environment of caves is unique from an ecological perspective. In this environment, a fascinating and adapted flora can occur under subterranean conditions. Therefore, this study investigated how the species Cupania vernalis Cambess. (Sapindaceae), occurring in different environments with distinct characteristics (subterranean to full sunlight), may be affected in its morpho-physiological traits. For this purpose, the specific leaf mass of each individual was determined, and the concentrations of chlorophylls a, b, and total carotenoids were quantified by UV/Vis Absorption Spectroscopy, considering the absorbances at 470, 646, and 663 nm, respectively. The concentrations of photosynthetic pigments and specific leaf mass of the species underwent changes according to their occurrence in locations with different incident light availability in the environment. The species possesses a capacity for phenotypic and biochemical plasticity for physiological adjustments, enabling its occurrence under different light conditions, which makes it a potential candidate for use in the restoration of cave environments.
... Trichopeltis Pocock, 1894 is one of the tropical or subtropical genera of Asian Cryptodesmidae. Currently, this genus encompasses 13 species, mainly documented in Indonesia, Myanmar, Laos, Vietnam, Cambodia, southern China, and the Himalayas (Golovatch 2015(Golovatch , 2016Golovatch and VandenSpiegel 2017;Likhitrakarn et al. 2017;Liu et al. 2017;Liu and Wynne 2019). This genus is well defined and characterized by a tripartite or deeply notched gonopod telopodite, including a small middle to caudal solenomere branch (Golovatch et al. 2010). ...
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A new species of Cryptodesmidae, Trichopeltis jiyuesp. nov., is described from the Ailaoshan National Nature Reserve in Yunnan Province, southwest China. The new species is distinguished from its congeners by the gonopodal coxae with two conspicuous wing-like processes, the relatively long, stout setae on the gonopodal coxae, gonopodal telopodites glabrous and four-branched, and the acropodite curved caudolaterad. The new species is the second record of an epigean species of genus Trichopeltis Pocock, 1894 in China. An updated key is provided to all 14 presently known species.
... Limestone karsts in Southeast Asia are referred to as 'arks of biodiversity' and as such are a priority for biodiversity conservation (Clements et al. 2006). Karst hills usually are relatively small, scattered and isolated, but nonetheless may support large numbers of endemic organisms (Schilthuizen 2011;Tolentino et al. 2020), including a wide variety of millipede species (Golovatch 2015;Liu et al. 2017;Liu and Wynne 2019). ...
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A new species of the giant pill millipede genus Sphaerobelum is described: Sphaerobelum turcosa sp. nov. from the northeastern part of Thailand. Species delimitation is based on morphological characters and COI sequence data. The new species can be clearly discriminated from congeners by its greenish-blue body color, the face mask-like appearance of the thoracic and anal shields jointly when rolled up, and the combination of the following four characters: (1) the coxa of the second leg laterally with a sharp and long process, (2) the tarsi of legs 4–21 with 6–7 ventral spines, (3) the anterior telopods consisting of four conspicuous telopoditomeres, and (4) the immovable, slender (not strongly humped) and distally curved finger of the posterior telopods without a membranous spot. The interspecific COI sequence divergence between the new species and other Sphaerobelum species ranges from 17% to 23% (mean 20%). The intergeneric COI sequence divergence between the new species and Zephronia species ranges from 18% to 21% (mean 20%). The relationships among Sphaerobelum and Zephronia species based on the COI sequence data were not resolved in this study. Sphaerobelum turcosa sp. nov. is restricted to limestone habitat in Loei province and is probably endemic for the Thai fauna.
... Glyphiulus deharvengi ( Figure 8A) and Eutrichodesmus sketi ( Figure 8B) are widespread in the cave. The presence of these species was expected, as both genera are very frequently found and highly diversified in South China caves [11,14,39]. Eutrichodesmus sketi is eyeless. ...
Article
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China is a country with abundant karst landscapes, but research on cave biodiversity is still limited. Currently, only Ganxiao Dong, located in Huanjiang, Guangxi, has been reported as a hotspot for cave biodiversity. Many of the world’s most troglomorphic species in the major groups of cave animals have been recently discovered in China, making the existence of many more hotspots in the country likely. Feihu Dong, one of these potential hotspot caves, has been systematically investigated to complement a preliminary species list of 1995, leading to the discovery of 62 species of animals from the cave. Among them, 27 are considered troglobionts or stygobionts, 26 are considered troglophiles or stygophiles, and nine are classified as trogloxenes or stygoxenes. Research on the cave biodiversity of Feihu Dong has demonstrated that it currently holds the highest number of known cave animal species in China. Among the most remarkable features of this fauna is the co-occurrence of five species of cave-obligate beetles, all modified for cave life. The biological survey was limited to a small part of the cave. Several habitats (like guano) have not been investigated so far, and several important cave groups have been insufficiently or not sampled (like Ostracoda). Meanwhile, the system increases in length with each new caving expedition. Further discoveries of cave organisms in Feihu Dong are therefore expected. As Feihu Dong and Ganxiao Dong are the only caves in China that have been extensively studied for a large range of organisms, and as they are located in karstic areas that are similar in richness to other regions of southern China, it can be confidently assumed that several other caves of high biodiversity will be discovered in the coming years.
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In order to provide a reassessment of the Neotropical genus Pseudonannolene Silvestri, 1895, a cladistic analysis, biogeographic analysis, and taxonomic review were conducted in the present work. For the cladistic approach, 91 morphological characters were scored for 53 terminals as the ingroup and 10 as the outgroup. Three synapomorphies support the monophyly of the genus: presence of a longitudinal suture on the promentum, penial bases partially fused, and the internal branch of the gonopods surrounding the telopodite; and two homoplastic transformations: the lateral lobe of the collum densely striated and setae present up to the apical portion of the prefemoral process on the first leg-pair of males. The genus Pseudonannolene is recovered as sister-group of Epinannolene Brölemann, 1903 (Pseudonannoleninae). A total of 226 occurrence points were recorded for Pseudonannolene, with the majority of records from the Chacoan subregion, composed by Araucaria Forest, Atlantic, and Parana Forest provinces. The biogeographical searches using the Geographically explicit Event Model recovered two biogeographic reconstructions (cost of 79 000), with the vicariance events occurring more frequently in the deep clades, whereas sympatry and points of sympatry occurred in more inclusive clades. The first reconstruction recovered four vicariances, 13 sympatries, 4 points of sympatry, and 21 founder events, and the second reconstruction recovered four vicariances, 12–13 sympatries, 4–5 points of sympatry, and 21 founder events. The genus Pseudonannolene comprises 56 species, including 8 new species herein described: P. alata sp. nov., P. aurea sp. nov., P. bucculenta sp. nov., P. curvata sp. nov., P. granulata sp. nov., P. insularis sp. nov., P. morettii sp. nov., and P. nicolau sp. nov.; P. brevis Silvestri, 1902 and P. rugosetta Silvestri, 1897 are regarded as species inquirendae; a neotype of P. alegrensis Silvestri, 1897 is here proposed with male described for the first time. The following taxa are synonymized: P. canastra Gallo & Bichuette, 2020 and P. saguassu Iniesta & Ferreira, 2013 with P. ambuatinga Iniesta & Ferreira, 2013; P. marconii Iniesta & Ferreira, 2013 with P. longicornis (Porat, 1888); P. chaimowiczi Fontanetti, 1996, P. gogo Iniesta & Ferreira, 2013, P. rosineii Iniesta & Ferreira, 2014, P. taboa Iniesta & Ferreira, 2014, and P. longissima Iniesta & Ferreira, 2014 with P. microzoporus Mauriès, 1987; P. tricolor gracilis Brölemann, 1902 and P. tricolor rugosus Schubart, 1945 with P. tricolor Brölemann, 1902; P. auguralis Silvestri, 1902 with P. rocana Silvestri, 1902; and P. abbreviata Silvestri, 1902 with P. typica Silvestri, 1895. P. inops Brölemann, 1929 is proposed here as new status from P. bovei inops. A dichotomous identification key is presented to facilitate the species identification.
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