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Structure and Interactions in a Cave Guano-Soil Continuum Community

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Structure and Interactions in a Cave Guano-Soil Continuum Community European Journal of Soil Biology 57 (2013) 19e26 Contents lists available at SciVerse ScienceDirect European Journal of Soil Biology journal homepage: http://www.elsevier.com/locate/ejsobi Original article Structure and interactions in a cave guanoesoil continuum community Thais Giovannini Pellegrini a,1, Rodrigo Lopes Ferreira b,* a PPG-Applied Ecology, Department of Biology (DBI), Federal University of Lavras (UFLA), Minas Gerais CEP 37200-000, Brazil b Laboratory of Underground Ecology, Department of Biology (DBI), Federal University of Lavras (UFLA), Minas Gerais CEP 37200-000, Brazil article info abstract Article history: Bat guano represents an important food resource for cave-dwelling organisms, hosting up to entire Received 30 November 2012 communities in a single deposit. Sampling conducted in guano and its interface with the adjacent soil Received in revised form revealed a wide variation in physicochemical parameters (nitrogen, phosphorus, organic matter, pH and 22 February 2013 moisture) along that continuum. The invertebrate orders that showed the greatest abundance and Accepted 8 March 2013 species richness were: Mesostigmata, Sarcoptiformes and Trombidiformes, all belonging to subclass Available online 3 May 2013 Acari. The results clearly showed that mite species are the most abundant group in guano deposits. Such Handling editor: Stefan Schrader species can directly or indirectly feed on this food resource. The abiotic factors of the guano significantly explained some community parameters. Furthermore, moisture was the parameter that best explained Keywords: the abundance distribution for the most common mite species. Lastly, a trophic web of the most Subterranean realm abundant species in the guano was devised based on literature data, interspecies correlation, preferences Feeding resource for microhabitats and abundance rates of the populations. It was possible to observe that the temporal Invertebrates changes in the guano deposit determine a successional process in the community, including the trophic Mites web structure. Bat guano Ó 2013 Elsevier Masson SAS. All rights reserved. Physio-chemical parameters 1. Introduction more acidic [5,6]. However, studies by Ferreira et al. [3] demon- strated that moisture and pH data alone are not sufficient to infer The condition of total absence of light and the resulting inex- the age of a guano deposit. According to those authors, guano de- istence of photosynthetic organisms require cave environments to posits are open systems and are therefore affected by chemical, depend on resources from the outside. That condition gives rise to a physical and biological processes, such as percolating water, tendency toward oligotrophy in most of these systems [1]. Never- physical and biological movement, and incorporation of animal theless, that condition is not always prevalent in caves, especially bodies and exuviae. those in which guano deposits can be found. Guano from birds, Guano deposits have a strong influence on the distribution invertebrates and most commonly bats, can form extensive de- pattern of certain cave-dwelling populations, sometimes hosting posits in caves; in those cases, it represents the main food resource large communities at different successional stages [7,6]. These for cave-dwelling organisms [2,3]. communities include such diverse organisms as bacteria, fungi, Bats can produce considerably large deposits. Guano deposits protozoa, nematodes, mites, coleopterans, dipterans, lepidopterans, vary with regard to dietary quality and microclimate, characterized collembola and spiders [4]. Among those, mites are the most by the high variability of microhabitats, with variable pH, moisture abundant organisms in guano [6]. and organic matter percentage [4]. This heterogeneity in the The majority of studies on the communities associated with chemical conditions of guano deposits mainly takes place due to guano deposits in caves have been food chain descriptions and the variations this substrate undergoes over time. Fresher guano is species lists e.g., [4,7e9]. Few studies consider the interrelations generally more alkaline and moist; as it ages, it becomes drier and with the physicochemical parameters of the substrate under study [10]. Moreover, there have been no studies taking into consideration the continuums of variation in the physicochemical parameters of * Corresponding author. Tel.: þ55 (35) 3829 1884. the substrate in the guanoesoil interface area. Therefore, there is a E-mail addresses: [email protected] (T.G. Pellegrini), drops@ dbi.ufla.br (R.L. Ferreira). need to understand the interference of this change in the substrate 1 Tel.: þ55 (35) 8826 8647. properties on associated invertebrate communities. As such, in 1164-5563/$ e see front matter Ó 2013 Elsevier Masson SAS. All rights reserved. http://dx.doi.org/10.1016/j.ejsobi.2013.03.003 20 T.G. Pellegrini, R.L. Ferreira / European Journal of Soil Biology 57 (2013) 19e26 order to understand the structure of a given community associated oxidation in acidic medium, and organic matter determination was with bat guano, it is important to relate richness and abundance performed by colorimetry [15]. The Soils Laboratory of the Federal patterns to abiotic parameters of those organic deposits. University of Lavras performed those last three analyses. The objective of the present study was to determine the composition of the invertebrate community associated with a large 2.3. Statistics guano deposit and its interface with the adjacent soil in a Neotropical cave. Furthermore, the study aimed to assess whether In order to confirm the efficiency of the sampling of the deposit abiotic factors of the guano and soil (pH, organic matter percentage, under study, a collection curve was calculated along with its con- moisture content, total nitrogen and total phosphorus) influence fidence interval, with 100 simulations of cumulative richness the structure of the invertebrate community associated with those observed throughout the 25 sampling points, using EstimateS substrates. Finally, the possible existing interactions were repre- software. Using the same program, the richness and abundance sented in a trophic web of the most abundant species in the guano. expected in the guano deposit were calculated using the average of Jackknife 1 and 2 and Chao 1 and 2 estimators. 2. Materials and methods The similarity between the fauna at the different points in the guano was compared using non-metric multidimensional scaling e 2.1. Study area n-MDS. The n-MDS was built based on the abundances of the invertebrate fauna, using the BrayeCurtis index. The aim of the The work was carried out in a large bat guano deposit located in analysis was basically to compare possible differences in the Lapa Nova cave. This dolomitic cave is located in the municipality of composition of organisms in guano, in the guanoesoil interface and Vazante, northwestern Minas Gerais state, Brazil (UTM-23 299811 in the soil. The existence of significant differences between n-MDS e 8010693) [11]. Although it is not set up for mass tourism, Lapa groups was evaluated by ANOSIM. Lastly, SIMPER analysis was used Nova has been visited annually by pilgrims for several decades, to evaluate which species were responsible for those differences. thereby serving as local tourist hub. All above-mentioned analyses were carried out using Primer The guano under study is located in an area far from the main software. entrance to the cave. It is in continuous deposition and is charac- The relationship between abiotic parameters (pH, moisture, terized as guano from omnivorous bats of the genus Phyllostomus. levels of nitrogen and phosphorus, and organic matter availability) The deposit is, on average, 15 m long and 5 m wide, representing an and biotic variables (richness, equitability and invertebrates di- important source of feeding resources for the organisms of that versity) were evaluated by General Linear Models (GLM) using Sta- cave. tistica software. The relationship between the abundance of the most representative species and the abiotic parameters was eval- 2.2. Experiment layout uated through Canonical Correlation Analysis (CCA) using PC-ORD 5.0 software. Lastly, a correlation matrix was obtained between the First, a linear transect was established in the direction of the most abundant/best distributed species and environmental pa- greatest length of the deposit until reaching an area with no visible rameters using BioEstat 5.0 software. Next, a correlation matrix was guano. Next, two samples were collected every meter of that built only among the most abundant species in the guano using transect. The same volume of guano was collected at all points for Statistica. biological analyses. The samples were taken from 400 cm2 squares, The possible interactions between the most abundant species 5 cm deep. For the analysis of community structure, the samples present in the guano deposit were also assessed. That task was were individually placed in plastic jars, which were then sealed, performed using information on the biology of each group found in labeled and taken to the lab. The other set of samples were used to the literature [16,17], the correlations among the species, the quantify the percentage of organic matter, moisture level, pH, ni- abundance rates and their preferences for microhabitats obtained trogen and phosphorus. from CCA. The first set of samples was previously triaged to remove the larger organisms. Next, those samples were place in Berlesee
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