MEM INST OSWALDO CRUZ, RIO DE JANEIRO, 107(8) December 2012
PAGES: 1016-1020 DOI: 10.1590/S0074-02762012000800009 Full paper
Sandflies (Diptera: Psychodidae) from caves of the quartzite Espinhaço Range, Minas Gerais, Brazil

Ricardo Andrade Barata+; Estefânia Conceição Apolinário

Laboratório de Parasitologia, Departamento de Ciências Biológicas, Universidade Federal dos Vales do Jequitinhonha e Mucuri, Diamantina, MG, Brasil

Abstract

This study investigated the sandfly fauna of two quartzite caves in the Espinhaço Mountain Range, located in the municipality of Diamantina, state Minas Gerais. From August 2010-July 2011, entomological sampling was performed in the caves of Salitre and Monte Cristo with two HP light traps exposed in the photic and aphotic zones of each cave. The sandfly fauna consisted of 17 species, among which Lutzomyia cipoensis was predominant (54.76%). The male/female ratio in the total captures was 1:2.5. The aphotic zone showed the highest frequency of specimens captured (65%). A greater density of sandflies occurred during the summer (January-February), coinciding with the period of higher temperatures, humidity and rainfall. The presence of Lutzomyia longipalpis, Lutzomyia whitmani and Lutzomyia pessoai, proven or suspected vectors of leishmaniasis, is of concern because the area is visited by many tourists.

The Espinhaço mountain range belongs to an extensive and continuous Precambrian orogenic zone (Almeida-Abreu & Renger 2002) consisting of a group of mountains and plateaus located in the states of Minas Gerais (MG) and Bahia, Brazil. The range extends approximately 1.200 km in a predominantly north-south direction (Saadi 1995). In 2005, this group of mountains was considered by the United Nations Educational, Scientific and Cultural Organization as the seventh Brazilian biosphere reserve due to its enormous diversity and biological importance. This area is valuable due to its great number of caves and because it separates three important watersheds (Rio São Francisco, Rio Doce and Rio Jequitinhonha) and divides the savannah (Cerrado), Atlantic Forest and Caatinga biomes (Gontijo 2008).

Although MG has the largest number of caves in the country, studies regarding the survey of cave fauna have been concentrated in the state of São Paulo (SP) and conducted mainly in limestone caves. However, studies involving surveys of cave fauna have been concentrated in SP and have been conducted primarily in limestone caves (Gomes et al. 2000, Ferreira & Horta 2001).

Furthermore, data on the sandflies of limestone, sandstone or quartzite caves are even less common and literature on sandflies is nonexistent for non-limestone caves, particularly quartzite caves. Given the recent expansion of ecotourism, regular monitoring of the cave areas that are used by visitors is crucially needed to facilitate preventive management of the transmission of leishmaniasis.

Therefore, this study aimed to identify the sandfly fauna of two quartzite caves, to investigate the relationship of the sandflies to climatic factors, to specify the seasonal distribution of the fauna and the transmission of leishmaniasis and to contribute to the knowledge of Brazilian biodiversity.

 

MATERIALS AND METHODS

Study area - The caves are located in the quartzite rocks of the Espinhaço Range, in the municipality of Diamantina, MG (Fig. 1). The caves named Gruta do Salitre (18º16'47"S 43º32'10"W) and Gruta Monte Cristo (18º17'49"S 43º33'30"W) (Fig. 2A, B) are located 10 km from the city centre and 3 km from each other. They are predominantly horizontal, with two entrances and sandy soil with fallen overlapping rocks. The caves also contain perennial watercourses. These caves are constantly visited by tourists, researchers and other sightseers. Therefore, human activities, such as soil trampling, the removal of the neighbouring native forest, graffiti on the walls, fly ash resulting from fires, garbage accumulation and traces of recent saltpetre extraction, are evident.

 

 

 

 

Methods - Insects were captured with HP light traps (Pugedo et al. 2005) from August 2010-July 2011. The traps were exposed continuously for 40 h/month between 04:00 pm (day 1) and 08:00 am (day 3). Two traps were placed in each cave: one at its entrance (photic zone) and the other in the darkness (aphotic zone), approximately 50 m from the entrance. The specimens captured were transported to the Parasitological Laboratory of the Federal University of Jequitinhonha and Mucuri Valleys and then sacrificed by freezing. The males and females were placed in haemolytic tubes containing ethanol (70%) and prepared and assembled on slides according to the technique of Langeron (1949). The taxonomic keys of Young and Duncan (1994) and Forattini (1973) were used to identify the sandfly species. The specimens with missing or damaged characters that prevented identification at the species level were identified as Lutzomyia spp. The females belonging to the genus Brumptomyia were not identified to the species level. The temperature and humidity were measured with a thermohygrometer at the capture site. The rainfall data were obtained from the Brazilian Meteorology Institute (inmet.gov.br/sim/sonabra/convencionais.php).

Statistical analysis - We used the means of the climatic variables for the months of capture. A Shapiro-Wilk test was used to evaluate the normality of the data distribution (GraphPad Prism software v.5). The Spearman correlations between the climatic variables and the density of the sandflies were calculated and their statistical significance assessed (p < 0.05).

 

RESULTS

The sandfly fauna of the Gruta do Salitre and the Gruta Monte Cristo consists of 17 species: Brumptomyia avellari (Costa Lima, 1932), Brumptomyia cunhai (Mangabeira, 1942), Lutzomyia carmelinoi Ryan, Fraiha, Lainson and Shaw, 1986, Lutzomyia cipoensis Martins, Falcão and Silva, 1964, Lutzomyia evandroi (Costa Lima & Antunes, 1936), Lutzomyia goiana Martins, Falcão and Silva, 1962, Lutzomyia ischyracantha Martins, Falcão and Silva, 1962, Lutzomyia longipalpis (Lutz & Neiva, 1912), Lutzomyia longispina (Mangabeira, 1942), Lutzomyia oliveirai Martins, Silva and Falcão, 1970, Lutzomyia pessoai (Coutinho & Barretto, 1940), Lutzomyia quinquefer (Dyar, 1929), Lutzomyia ramirezi Martins, Falcão, Silva and Miranda, 1982, Lutzomyia renei (Martins, Falcão & Silva, 1957), Lutzomyia sordellii (Shannon & Del Ponte, 1927), Lutzomyia whitmani (Antunes & Coutinho, 1939) and one undescribed species. In total, 2,248 specimens were identified, of which 633 were males (28%) and 1,615 females (72%), with a ratio of one male to 2.5 females. The predominant species was Lu. cipoensis, representing 54.76% of the total sandflies collected (Table).

The distribution of the sandflies captured in each cave and the climatic variables are represented in Fig. 3. The density of the sandflies in both caves showed positive correlations with the temperature, humidity and rainfall, with values of p = 0.085, p = 0.931 and p = 0.378, respectively. These values were not statistically significant at a level of p < 0.05.

 

 

DISCUSSION

Cave ecotopes are commonly used by sandflies for shelter or as breeding sites (Galati et al. 2006) and a few studies have investigated the abundance and richness of sandflies in cave environments in Brazil. In the state of Amazonas (AM), Alves et al. (2011) identified 15 species of sandfly in three sandstone caves. Galati et al. (2010) examined the diversity of sandflies in caves in SP, consisting of 11 species. In Mato Grosso do Sul, Galati et al. (2003, 2006) captured many sandfly specimens in limestone caves in the Serra da Bodoquena. In MG, Barata et al. (2008) identified 14 species of sandfly in a limestone cave located in Cavernas do Peruaçu National Park.

According to the results shown in Table, captures of insects in the aphotic zone (65%) were predominant. However, almost all of the species considered were captured both in the photic and aphotic zones. Considerations of the behaviour that enables the completion of the life cycle either within or outside the caves suggest that these species are troglophiles in terms of Schinner-Racovitza's system (Holsinger & Culver 1988) for cave organisms. This hypothesis was also suggested by Galati et al. (2003).

In general, the presence of sandflies in these caves appears to be related to the presence of bats, rodents, birds and lizards, which can serve as blood sources for the sandflies. Analyses of the gut contents of engorged females will be performed to identify the blood sources. Moreover, the large amount of guano inside the caves may serve as a breeding site for sandflies, as shown by Alves et al. (2011).

Caves have unique characteristics, including high humidity, stable temperatures and the risk of starvation due to scarce food resources (Auler & Zogbi 2005, White & Culver 2005). These features most likely influence the distribution of organisms in the cave environment. The two caves showed a greater number of sandflies in the summer (January-February), coinciding with the period of higher temperatures, humidity and rainfall. In contrast, a decrease in the density of these insects was found during the coldest and driest months. This pattern of seasonality has also been reported in most of the studies on sandflies in the endemic areas for leishmaniasis in MG (Barata et al. 2004, 2011).

The analysis of both caves showed that the distribution of sandflies in Gruta Monte Cristo was more nearly homogeneous during the study period than in Gruta do Salitre (Fig. 3). The reason for this finding may be that the former cave is less known and less accessible than the latter. The anthropogenic influence on Gruta Monte Cristo would also be lower for this reason. Consequently, trampling and vandalism appear to cause less disturbance to the sandfly breeding sites in Gruta Monte Cristo throughout the year. These factors can most likely explain the lower number of species found in Gruta do Salitre (11 species) than in Gruta Monte Cristo (13 species).

Although Lu. longipalpis is considered highly urbanised, with a high degree of synanthropy, this species has also been collected in the wild environment of caves in Diamantina, as observed by Galati et al. (2003). Lu. whitmani, a vector of Leishmania braziliensis in southeastern Brazil (Mayrink et al. 1979, Rocha et al. 2010), was recorded in small numbers in this study, as was Lu. pessoai, a species suspected of transmitting the agent of cutaneous leishmaniasis (Forattini et al. 1972). The other species collected in this study are not currently of epidemiological interest in terms of the transmission of leishmaniasis.

Several recent studies have contributed to the knowledge of the biodiversity of Brazilian caves. Alves et al. (2008) described Lutzomyia maruaga, which was captured in the aphotic zone of a sandstone cave in AM. Carvalho et al. (2010) described Martinsmyia reginae, captured in a cave in the state of Tocantins, and Carva-lho et al. (2011a) described Evandromyia spelunca, found in a cave in Lassance, MG. In the present study, an undescribed species (Lutzomyia sp.) was also captured in large numbers (16.9%), as shown in Table.

In this context, it is essential to implement educational programs and to conduct increased monitoring of the cave environment in association with a management plan to assure conservation actions and define regulations for access to caves, particularly during the months of higher sandfly densities. The presence of vectors of the leishmaniasis agent is of concern due to the increased volume of tourists and requires greater attention from the local ecotourism organisations.

 

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Received 15 June 2012
Accepted 8 August 2012

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