Research Article |
Corresponding author: Hannelore Hoch ( hannelore.hoch@mfn-berlin.de ) Academic editor: Dávid Rédei
© 2016 Hannelore Hoch, Rodrigo Ferreira.
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.
Citation:
Hoch H, Ferreira RL (2016) Iuiuia caeca gen. n., sp. n., a new troglobitic planthopper in the family Kinnaridae (Hemiptera, Fulgoromorpha) from Brazil. Deutsche Entomologische Zeitschrift 63(2): 171-181. https://doi.org/10.3897/dez.63.8432
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A new obligate cavernicolous (troglobitic) species in the planthopper family Kinnaridae is described from Brazil, and a new genus is established, as it could not be placed in any of the existing genera. Information on distribution and ecology is given. This is the second record of a troglobitic representative of this family from Brazil, and only the 6th cavernicolous kinnarid species worldwide.
Taxonomy, troglobite, troglomorphy, caves, Neotropics
A recent survey of limestone caves in the Iuiú municipality (Bahia state, Brazil) by a team of the Centro de estudos em Biologia Subterrânea, Federal University of Lavras, Brazil, revealed the existence of a previously unknown species belonging to the planthopper family Kinnaridae (Figs
With currently 111 species in 21 genera, Kinnaridae is one of the smaller families within the Hemipteran group of Fulgoromorpha (
The epigean Kinnaridae fauna of Brazil, like that of South America in general, must be considered virtually unknown: hitherto only a single species has been documented, Oeclidius parallelus Muir, 1934 from Brazil.
Although information on the biology and ecology of Kinnaridae is largely lacking, the majority of the world’s species are epigean and display well-developed compound eyes, vivid colouration of the body and tegmina, and are capable of flight. A few lineages, however, have colonized caves. Apart from Kinnapotiguara troglobia, described only recently from a limestone cave in Rio Grande do Norte State, NE Brazil (
The classification of Kinnaridae is still under debate. Even Kinnaridae as a family has not yet been established as a monophyletic group.
Kinnarinae were subdivided by
Unambiguous synapomorphies have not been identified for any of the established genera or tribes. Thus the accommodation of the new species within any of the existing supraspecific taxa is inherently problematic.
Following the key provided by
In characters of the male genitalia, the new cavernicolous species does not share any similarities with any species of the known kinnarid genera (in or outside Kinnocciini) which could be interpreted as synapomorphies. We thus opted for the establishment of a new genus which is described below.
Collecting, preservation, permanent storage. The specimens were collected by hand, and transferred immediately into vials containing 96% ethanol. For permanent storage, after dissection and examination, the abdomen and genitalia were transferred to polyethylene vials, and individually associated with the specimen vial.
Morphological examination techniques, visualization. Measurements and examinations of external body features were made from the specimen in ethanol, without further manipulation. To prepare male genitalia for dissection, the genital capsule was removed from the specimen, macerated for 24h in 10% KOH at room temperature, washed in water, transferred to glycerine for storage, or to glycerine-jelly for drawings. Examinations and drawings were made using a Leitz stereomicroscope with a camera lucida attachment.
Habitus photographs. The photograph in Fig.
Depository. ES: Laboratório de Ecologia Subterrânea/ISLA: Coleção de Invertebrados Subterrâneos da UFLA–Universidade Federal de Lavras, Brazil.
Kinnaridae Muir, 1925: 158
Prosotropinae Fennah, 1945: 449
Kinnocciini Emeljanov, 2006: 1
Iuiuia caeca sp. n. (type locality: Brazil, Bahia State, Iuiu municipality).
Small kinnarid (ca. 3 mm body length), strongly troglomorphic: compound eyes absent, tegmina reduced, wings vestigial, body pigmentation reduced (Fig.
Head. Vertex trapezoidal, short, ca. 3 × wider posteriorly than medially long, with a very faint median carina; anterior and posterior margin of vertex parallel. Frons narrow, ca. 1.8–2.0 × longer than maximally wide, widest between level of antennae and frontoclypeal suture, ca. 1.3 × longer than post- and anteclypeus together, surface medially smooth, devoid of a median carina, lateral margins distinctly ridged. Frontoclypeal suture nearly straight. Post- and anteclypeus with a distinct median carina. Rostrum elongate, in repose well surpassing hind coxae, third joint shorter than second. Compound eyes absent, their former position recognizable by a shallow, vaulted area. Median (frontal) ocellus absent, lateral ocelli vestigial. Antennae with scape short, subcylindrical, slightly expanding distally; pedicel subcylindrical, ca. 2.4 × as long as wide, with distinct sensory plaque organs; arista ca. 2.8 × as long as pedicel.
Thorax. Pronotum tricarinate, ca. 3 × wider than vertex posteriorly, short, posterior margin medially shallowly concave; carinae distinct, median carina attaining but not surpassing anterior margin of pronotum; lateral carinae medially more or less parallel to posterior margin, and joining posterior margin laterally. Mesonotum faintly tricarinate, ca. 1.3 × wider than medially long. Tegulae vestigial. Hind tibiae laterally unarmed, distally with 7 slender teeth, arranged in a shallow arc. First metatarsal joint distally with 4/5 and 5/6, 2nd metatarsal joint with 3/4 or 4/5 teeth (individually and bilaterally variable). Pretarsal claws and arolia small, inconspicuous. Tegmina (Fig.
Male genitalia. Genital segment bilaterally symmetrical, in lateral aspect short, ca. 3 × as high as medially long; in caudal aspect approximately figure-8-shaped, in upper third laterally constricted, with a narrow transversal bridge; anterior margin of genital segment smooth, without any conspicuous median apodemes; medioventral process prominent, broadly subtriangular, in lateral aspect distinctly exceeding caudal margin. Anal segment bilaterally symmetrical, short, stout, ventrally on each side with a compressed wing-shaped process. Parameres slender, narrow throughout, medially converging. Connective straight, narrow, almost terete.
Aedeagus bilaterally symmetrical, tubular, stout; periandrium with two large lateral lobes; proximal apodeme of aedeagus (= „tectiform structure“: term applied by
Females with abdominal tergites VI, VII and VIII bearing wax-fields. Female genitalia as in other Kinnaridae of the non-piercing type; sternite VII broadly rectangular, caudal margin straight; caudal margin of sternite VIII medially deeply incised; gonocoxae VIII bilobate, both lobes well developed, apically converging.
The genus name refers to Iuiú, the name of the municipality were the cave (type locality) is situated. The gender is feminine.
Habitus (Fig.
Body length. Measurements refer to distance between anterior margin of head to tip of abdomen (= caudal margin of parameres), those in brackets to distance of anterior margin of head to distal margin of tegmina.
Males. 2.8 (3.4)–3.8 (3.8) mm (n = 8). Females. 4.4 (4.0)–4.5 (4.1) mm (n = 2).
Colouration. Frons, vertex, pronotum yellowish, carinae contrasting dark brown; mesonotum more or less uniformly sordid yellowish; antennae and tegulae sordid light brown; tegmina translucent, uniformly yellowish-brown, veins slightly darker, without any conspicuous pattern. Metanotum, legs, as well as abdominal tergites and sternites pale yellow.
Configuration, shape and proportions of head and thorax as described for the genus.
Male genitalia (Fig.
Iuiuia caeca sp. n. Male genitalia (paratype). a genital segment, left lateral aspect; b same, caudal aspect; c anal segment, left lateral aspect; d same, caudal aspect; e parameres, caudal aspect; f left paramere, left lateral aspect; g aedeagus with connective, left lateral aspect; h same, ventral aspect; j same, dorsal aspect. Scale bars: 0.1 mm.
External female genitalia (Fig.
Female abdomen and external genitalia. a ventral aspect, b right ventrolateral aspect. Abbreviations: s VII = Vll. sternite, gx VIII = gonocoxae VIII; as (X) = anal segment (X. segment); ast (XI) = anal style (XI. segment); t VI, t VII, t VIII = tergites of segments VI-VIII. Scale bar 0.1 mm.
The species is only known from the “Lapa do Baixão” cave in Iuiú municipality, Bahia State, Brazil. The external vegetation in the area corresponds to the “Caatinga” formation, the only xeric biome of the country, with xeromorph, decidual vegetation (Fig.
The “Lapa do Baixão” cave formed within limestones from the “Bambuí” geological group, from the Neoproterozoic, with ages ranging from 650-850 Myr. This group comprises the largest limestone formation in Brazil, embracing most of the known Brazilian limestone caves (Fig.
The Baixão cave possesses dozens of roots, mainly observed in the first portion of the cave (Fig.
Unfortunately, it was not possible to associate the roots to any particular plant species in the surface vegetation, but considering the distance between the surface and the cave, it appears likely that such roots belong to substantial trees with pivotant roots systems, capable of penetrating deep inside the cracks into the soil and rock until reaching the cave chambers.
Such roots shelter a variety of invertebrate species which feed especially in their decomposing parts. However, also many non-troglomorphic Cixiidae (Pintalia spp.) feed on them, especially in those roots located nearer the entrance (but also in aphotic zones). These are supposedly accidentals to the cave, but eventually can become troglophiles. Specimens of Iuiuia caeca were observed only on roots within the labyrinthic part in the deep cave zone.
They were only rarely observed on the same roots where the non-troglomorphic Cixiidae occur. The root mats where Iuiuia occur are mainly placed in the final portion of this labyrinthic part of the cave, near the connection with the inner single vadose and semi- meandrine passage. Such root mats are considerably smaller than those found in other parts of the cave. During a visit to the cave on 7.viii.2013, most of the observed specimens were nymphs, and only three adult males were found. During this visit, one of the males was found on a small root, near the cave floor, while the other two were found in an upper chamber, without roots, where they were freely walking on speleothems. During our last visit to the cave (9.vii.2014), seven adults and many nymphs were observed, but their spatial distribution was even more restricted. All observed specimens were associated with roots in a single part of the conduit, and no specimens were found in other chambers, as in the previous visit. Since both visits occurred in the dry period of the area, such differences observed on their abundance and distribution cannot be primarily related to seasonal changes. Potential predators include spiders (especially Ochyroceratidae), Amblypygi (Charinus iuiu Vasconcelos & Ferreira, 2016) and a relatively large troglobitic pseudoscorpion species, with a body size of around 5 mm (Spelaeobochica iuiu Ratton, Mahnert & Ferreira, 2012); the latter is well distributed throughout the cave, but less common in the areas where I. caeca occurs.
The species epithet “caeca” (blind, Lat.) refers to the complete reduction of compound eyes in this species. The gender is feminine.
Holotype male. Brazil. Bahia State, Iuiu municipality, Toca Lapa do Baixão (14°23’8.13”S, 43°37’35.06”W), 7.viii.2013, R.L. Ferreira leg., in coll. Universidade Federal de Lavras, ISLA.
Paratypes: 2 males, same data as holotype. 5 males, 2 females, same data as holotype, except 9.vii. 2014, in coll. Universidade Federal de Lavras, ISLA.
In the cave, several 4th and 5th instar nymphs of Kinnaridae were collected which, due to substantial morphological differences, apparently represent two species. However, none of these nymphs could be associated with certainty to Iuiuia caeca. Thus it is likely that the cave Toca Lapa do Baixão houses at least two, if not three, kinnarid species.
The placement of Iuiuia into Kinnocciini ought to be considered preliminary as the characters observed in Iuiuia caeca do not fully coincide with those given by
Thus it cannot be excluded that the closest epigean relative (whether extant yet unknown or extinct) displayed a median carinae of the frons and a darkly pigmented integument.
The genera currently featured in Kinnocciini, Kinnoccia Remane, 1985 and Kinnocana Remane, 1985 (as listed in
No close epigean relatives could be identified for Iuiuia caeca in Brazil, or elsewhere. The only epigean kinnarid species documented from Brazil is Oeclidius parallelus Muir, 1934, described from a single female from „Bahia; Iguassú“ (
It is certainly difficult to formulate a well-supported hypothesis regarding the evolution of the subterranean lineages of the Brazilian planthoppers, mainly due to the lack of knowledge on the epigean Fulgoromorpha fauna of Brazil. Different scenarios are conceivable, and may not be mutually exclusive. Initial cave adaptation may have occurred as a consequence of allopatric speciation following the extinction of epigean ancestral species as was postulated in the climatic relict hypothesis (
However, the structure and age of the rocks housing cave environments seem to be important factors acting on the evolution or at least on the distribution pattern of the cavernicolous Kinnaridae and Cixiidae of Brazil. Three biogeographic-geological constellations are observed:
1. Iuiuia caeca appears to be restricted to a single cave, which consists of a deep cave, which is possibly not connected to a larger system of mesocaverns.
2. Populations of the kinnarid Kinnapotiguara troglobia are known from many caves in the Apodi group in the Rio Grande do Norte State (
3. Ferricixius davidi, the only troglobitic Cixiidae known for Brazil, is found in a single iron ore cave, located in an area where hundreds of caves are known. This cave is very close to the surface, and roots penetrate into the subterranean macrocaverns. The cave is also interconnected with other caves in the surroundings by small canaliculi present on the topmost ferrugineous breccia, which would theoretically allow migration between caves, so long as a suitable microhabitat (e.g., high relative humidity, food resources) is maintained.
The external area surrounding the cave is heavily impacted, mainly by human activities such as agriculture and extensive breeding of cattle and goats. Moreover, the area is currently being evaluated for its potential for limestone extraction. Hence, although there are no mining activities yet in the area, such activities will probably start in a near future, posing a potential risk to the cave environment. A new railway (FIOL–Ferrovia de Integração Oeste-Leste) that is being constructed connecting the Brazilian coastal area to this inner portion of Bahia state will favour the outflow of feedstock (especially agricultural products and ore), which will certainly contribute to arising the interest of exploiting the limestone in the area. Fortunately, the cave did not show any indication of human visitation, thus we consider the best option for the moment in order to preserve the cave may be to not publicly disclose the precise GPS data of its location.
It is worth mentioning that the Lapa do Baixão cave has many other troglobitic species (12 species) from which only two are currently described: Spelaeobochica iuiu Ratton, Mahnert & Ferreira, 2012 (Pseudoscorpiones, Bochicidae) and Iuiuniscus iuiuensis Souza, Ferreira & Senna, 2015 (Isopoda, Styloniscidae). Therefore, Iuiuia caeca comprises the third troglobitic species described from this cave, which certainly deserves attention regarding its conservation. Many hotspots of subterranean biodiversity (those caves or cave systems with 20 or more cave obligate species) (Culver and Sket 2010) occurs around the world, but currently there are no such hotspots in South America. In most cases, the high number of troglobitic/stygobitic species depends on the sampling efforts spent in a given cave.
Accordingly, Toca do Baixão cave certainly has potential to become a hotspot in the future, since only a few samplings were conducted there. Therefore, it is crucial that Brazilian government earmark some conservation efforts to preserve this unique cave and its endemic inhabitants.
The discovery of Iuiuia caeca not only represents the 3rd obligate cavernicolous Fulgoromorpha species in Brazil, but also provides evidence of three separate evolutionary lineages which have invaded caves, two within the Kinnaridae, and one within the Cixiidae. All three species were discovered within a few years and are the result of the exploration efforts of a single, but active team of speleologists. Given the vast extension of cavernous substrate in Brazil and the availability of suitable planthopper habitat, Brazil may soon join Hawaii (e.g.,
We would like to express our sincere thanks to our colleagues Marconi Souza Silva (UFLA) and Luiz Felipe Moretti Iniesta for helping with collections, and to our colleagues at the Museum für Naturkunde, Berlin: Manfred Uhlig for the male habitus photograph (Fig.