Research Article |
Corresponding author: Ivanklin Soares Campos-Filho ( ivanklin.filho@gmail.com ) Academic editor: Spyros Sfenthourakis
© 2022 Ivanklin Soares Campos-Filho, Jéssica S. Gallo, Jonas E. Gallão, Dayana F. Torres, Yesenia M. Carpio-Díaz, Carlos Mario López-Orozco, Ricardo Borja-Arrieta, Stefano Taiti, Maria Elina Bichuette.
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Citation:
Campos-Filho IS, Gallo JS, Gallão JE, Torres DF, Carpio-Díaz YM, López-Orozco CM, Arrieta RB, Taiti S, Bichuette ME (2022) Expanding the knowledge on the diversity of the cavernicolous Styloniscidae Vandel, 1952 (Oniscidea, Synocheta) from Brazil, with descriptions of two new species from the semiarid karst regions. In: De Smedt P, Taiti S, Sfenthourakis S, Campos-Filho IS (Eds) Facets of terrestrial isopod biology. ZooKeys 1101: 35-55. https://doi.org/10.3897/zookeys.1101.79043
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Two new species of Pectenoniscus from two caves in karst areas of the Brazilian semiarid region are described. Pectenoniscus pankaru Campos-Filho, Torres & Bichuette, sp. nov. from Gruna do Govi cave, Serra do Ramalho karst area, state of Bahia, and Pectenoniscus fervens Campos-Filho, Taiti & Bichuette, sp. nov. from Toca Coroa do Frade cave, Barra Bonita karst area, state of Piauí. In addition, specimens of Cylindroniscus flaviae from Gruta da Tapagem (= Caverna do Diabo), Açungui karst area were also recorded. An updated diagnosis of Pectenoniscus and a distribution map of the species examined herein are given.
Açungui geomorphological group, Bambuí geomorphological group, Casa Nova geomorphological group, Cylindroniscus, Neotropical, Pectenoniscus
Terrestrial isopods (Oniscidea) comprise approximately 4,000 species and more than 500 genera distributed in 38 families (
The family Styloniscidae comprises 120 species distributed in 18 genera (WoRMS 2021). The family has a worldwide distribution, with species inhabiting many terrestrial environments, including caves (
To date, in Brazil, 26 species of the family distributed in nine genera have been recorded from caves, i.e., Chaimowiczia (2 spp.), Clavigeroniscus (1 sp.), Cordioniscus (1 sp.), Cylindroniscus (2 spp), Iuiuniscus (1 sp.), Pectenoniscus (8 spp.), Spelunconiscus (1 sp.), Styloniscus (2 spp.), and Xangoniscus (8 spp.) (
Two new species of Pectenoniscus from caves of two distinct Brazilian karst regions are described here. The first species comes from Gruna do Govi, Serra do Ramalho karst region, inserted in the Bambuí geomorphological group, state of Bahia, and the second from Toca Coroa do Frade, Barra Bonita karst region, Casa Nova geomorphological group, state of Piauí. In addition, specimens of Cylindroniscus flaviae Campos-Filho, Araujo & Taiti, 2017 from Gruta da Tapagem (also known as Caverna do Diabo), Açungui geomorphological group, are recorded here. An updated diagnosis of the genus Pectenoniscus is given to include the species described by
Specimens were collected by hand with the aid of tweezers and brushes and stored in 70% and 100% ethanol. Information about the microhabitat (entrance, twilight or aphotic zones) and environmental variables (temperature and relative air humidity) of the caves was also recorded. Descriptions are based on morphological characters with the use of micro-preparations in Hoyer’s medium (
The material is deposited in the scientific collection of cave fauna of the Laboratório de Estudos Subterrâneos (LES), Universidade Federal de São Carlos, São Carlos, Brazil.
The Açungui geomorphological group comprises the metamorphic limestone and dolomite rocks of ~ 600 million years ago, extending from south of the São Paulo state to north of the Paraná state (
This region includes the Caverna do Diabo State Park (PECD, in Portuguese, Parque Estadual da Caverna do Diabo), state of São Paulo (Fig.
The Bambuí geomorphological group has the largest limestone area (ca. 146,000 km²) and the highest number of caves in Brazil (
The Gruna do Govi (Figs
A Gruta da Tapagem (Caverna do Diabo), Açungui geomorphological group B Cylindroniscus flaviae Campos-Filho, Araujo & Taiti, 2017 foraging in the organic matter C surrounding area outside Gruta Toca Coroa do Frade, Casa Nova geomorphological group D aphotic zone of the Toca Coroa do Frade.
Gruna do Govi, Bambuí geomorphological group A surrounding area outside the cave B cave entrance C, D outside cave illustrating the anthropic impacts E Pectenoniscus pankaru Campos-Filho, Torres & Bichuette, sp. nov. foraging in the organic matter F cave habitat where the specimens were collected.
The Barra Bonita karst region is inserted in the Casa Nova geomorphological group, and it is formed by quartzites, mica schists, and limestones of ~ 740 Myr (
The Gruta Toca Coroa do Frade (Figs
Cylindroniscus seurati Arcangeli, 1929 by monotypy (see
Cylindroniscus flaviae
Campos-Filho, Araujo & Taiti, in
Cylindroniscus flaviae;
Brazil●1♀, Gruta da Tapagem (Caverna do Diabo), Eldorado, Parque Estadual Caverna do Diabo, Açungui geomorphological group, state of São Paulo, 24°38'17.00"S, 48°24'4.00"W, leg. ME Bichuette, T Zepon, JE Gallão, 24.III.2021, LES 27755●1♀, same locality and collectors as for preceding, 24.III.2021, LES 27756●1♂, 1♀, same locality and collectors as for preceding, 24.III.2021, LES 27757●1♀, same locality and collectors as for preceding, 24.III.2021, LES 27758●2♀♀, same locality and collectors as for preceding, 24.III.2021, LES 27759●1♂, same locality and collectors as for preceding, 25.III.2021, LES 27760.
Cylindroniscus flaviae shows preference for organic matter deposits and highly humid areas in the aphotic zone (Fig.
This species is recorded from several caves in the Açungui geomorphological group (see Campos-Filho et al. 2017).
Pectenoniscus angulatus Andersson, 1960 by monotypy (see
After
The genus Pectenoniscus was created by
Brazil●1♂, holotype, Gruna do Govi, Feira da Mata, Serra do Ramalho karst area, Bambuí geomorphological group, state of Bahia, 13°56'43.30"S, 44°14'25.94"W, 12.X.2020, leg. ME Bichuette, DF Torres, JS Gallo, LS Horta and JE Gallão, LES 27761●1♂ (parts in micropreparations), paratype, same data as for holotype, LES 27762●2 ♀♀, paratypes, same data as for holotype, LES 27763.
Maximum length: ♂ 2.2 mm, ♀ 3.5 mm. Dorsal surface slightly granulated, granules on pereonites 1–7 in two transverse rows, pleon smooth (Fig.
Male. Pereopods 1–6 (Fig.
Pectenoniscus pankaru Campos-Filho, Torres & Bichuette, sp. nov. (♀, LES 27763) A habitus, dorsal view B habitus, lateral view C cephalon, dorsal view. Pectenoniscus fervens Campos-Filho, Taiti & Bichuette, sp. nov. (♀, LES 27764) D habitus, dorsal view E habitus, lateral view F cephalon, dorsal view.
The new species is named for the indigenous people Pankaru, who inhabited the northern portion of Serra do Ramalho region.
Pectenoniscus pankaru sp. nov. differs from all other species of the genus in the shape of the male pleopod 2 endopod. Moreover, it differs in having the antennal flagellum composed of four articles (vs. five in P. angulatus, three in P. carinhanhensis, P. iuiuensis, P. juveniliensis, P. lilae, P. montalvaniensis, P. morrensis and P. santanensis), antennula bearing 12 aesthetascs (vs. six in P. morrensis and P. santanensis, eight in P. angulatus and P. montalvaniensis, nine in P. juveniliensis and P. lilae, ten in P. iuiuensis, and 11 in P. carinhanhensis) (see also
Specimens of Pectenoniscus pankaru sp. nov. were found only in the aphotic zone associated to the sediment banks close to a small subterranean stream (Fig.
Brazil●1♂ (parts in micropreparations), holotype, Gruta Toca Coroa do Frade, Coronel José Dias, Barra Bonita karst region, Casa Nova geomorphological group, state of Piauí, 8°47'51.58"S, 42°25'1.47"W, 8.I.2018, leg. DM Schimonsky, DF Torres and JE Gallão, LES 22421●6♀♀ (one with parts in micropreparations), paratypes, same data as for holotype, LES 27764.
Maximum length: ♂ and ♀ 3 mm. Dorsal surface granulated, granules on pereonites 1–7 in two transverse rows, on pleonites 3–5 in one row (Fig.
Male. Pereopods 1–7 (Fig.
Latin. fervens for very hot, boiling hot. The new species name refers to the very hot temperatures of the Brazilian state of Piauí.
Pectenoniscus fervens sp. nov. differs from all other species of the genus in the shape of the male pleopod 2 endopod. Moreover, it differs from P. pankaru sp. nov. in having the antennula bearing six aesthetascs, the dactylar seta stout and in the different shape of the male pleopod 1 and pleopod 3–5 exopods. The new species shows the same number of aesthetascs of the antennula as in P. morrensis and P. santanensis, from which it differs in the antennal flagellum composed of four articles (three in P. morrensis and P. santanensis), male pleopod 1 protopod with the distal margin concave (vs. straight in P. morrensis, almost straight in P. santanensis), male pleopod 4 exopod triangular (vs. subrectangular in P. morrensis, subquadrangualar in P. santanensis), and male pleopod 5 exopod rhomboid and longer than wide (vs. triangular and as long as wide in P. morrensis, subquadrangular in P. santanensis).
The specimens of Pectenoniscus fervens sp. nov. were found only in the aphotic zone (Fig.
The new species of Pectenoniscus described here showed strict dependence on high humidity. Their occurrence in the caves present in semiarid regions, where the external temperatures are high and the humidity is low, reinforce the idea that these caves are probably important refuges for these animals due to their favourable conditions. Moreover, both species show remarkable troglomorphism, such as absent body pigments and eyes, which reinforces the classification of both species as troglobites.
A preliminary evaluation of the conservation status of the new species described here was carried out following the IUCN (International Union of Conservation of Nature) classification. Pectenoniscus pankaru sp. nov. and Pectenoniscus fervens sp. nov. were classified as Critically Endangered (CR) by the criteria B2ab(iii). The surrounding areas of the caves (Gruna do Govi and Gruta Toca Coroa do Frade) are impacted by deforestation and the remaining native vegetation is present only close to their entrances. The Serra do Ramalho karts area is historically threatened by agricultural activities and potential mining projects (
Our thanks go to ICMBio/CECAV (Instituto Chico Mendes para Conservação da Biodiversidade/Centro Nacional de Pesquisa e Conservação de Cavernas) for financial support of the project “Estudos para definição de áreas prioritárias para a Conservação de Proteção Espeleológico na Serra do Ramalho – BA”, under execution by the GBPE (Grupo Bambuí de Pesquisas Espeleológicas), coordinated by Ezio Rubbioli and integrated by MEB; to the members of GBPE, L. Horta, E. Rubbioli, F. Chaimowicz, A. Lobo and R. Brandi for all support in the occasion of the discovery of the new species from Serra do Ramalho karst area; special thanks to GBPE for sharing speleological information of Serra do Ramalho karst area with MEB and for all contribution to the knowledge of Brazilian caves; to D.M. von Schimonsky for his assistance on sampling trip in the state of Piauí; to T. Zepon and V.F. Sperandei for their assistance in sampling at Gruta da Tapagem (Caverna do Diabo), PECD; to SISBIO (Sistema de Autorização Informação em Biodiversidade) for collection permit to MEB (28992 and 75338); to Fundação Florestal for collection permit to MEB at Gruta da Tapagem - PECD (number 004738/2020-15); to FAPESP (Fundação de Amparo à Pesquisa do Estado de São Paulo) for financial support to MEB (Gruta da Tapagem project; number 2019/19520-0); to Vicerrectoría de Investigaciones of the University of Cartagena for the financial support to the Grupo de Investigación en Biología Descriptiva y Aplicada (Project Redes de Investigación Científica, Acta de Compromiso N° 017–2020); to CAPES (Coordenação de Aperfeiçoamento de Pessoal de Nível Superior) for financial support to ISC-F during his postdoctoral fellowship at UFCG (CAPES/PNPD/UFCG/CTRN/PPGRN/201713705) (Finance Code 001); to CNPq (Conselho Nacional de Desenvolvimento Científico e Tecnológico) for financial support and productivity fellowship to MEB (457413/2014-0 and 310378/2017-6); to Research Project titled “Biodiversity of terrestrial isopods (Crustacea, Isopoda, Oniscidea) from Cyprus in the light of integrative taxonomy”, funded by the “ONISILOS Research Program – 2018”, University of Cyprus, for the postdoctoral fellowship granted to ISC-F. We would like also to thank Jana Bedek and Paula B. Araujo for their critiques and suggestions.