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Journal of Insect Science logoLink to Journal of Insect Science
. 2019 Mar 27;19(2):18. doi: 10.1093/jisesa/iez026

Chemosystematics Using Cuticular Compounds: A Powerful Tool to Separate Species in Mediterranean Dung Beetles (Coleoptera: Geotrupidae)

Jerome Niogret 1,2,3,, Anne-Emmanuelle Felix 2,3, Antoine Nicot 2,3, Jean-Pierre Lumaret 2,3
PMCID: PMC6435918  PMID: 30915445

Abstract

The use of chemical characters to infer a phylogeny is known to be promising to ascertain phylogenetic relationships in controversial groups. Dung beetle classifications containing the Geotrupidae family, based on morphological characters and genes, are debated with respect to the subfamilies, such as the Bolboceratids. In our study, we used different approaches to generate and compare the Geotrupidae phylogenies based on genetics and chemotaxonomy. Cuticular compounds were analyzed for 12 species of Mediterranean dung beetles to build a chemical phylogeny. In addition, mitochondrial and nuclear marker concatenation have been used to elaborate the molecular phylogeny. Using the cuticular compound continuous data, our results showed that each species was associated with a specific chemical pattern and that all individuals belonging to the same species displayed a similar chemical blend. The most distant species was Bolbelasmus gallicus, with an evident distinction from the other species due to several compounds. The maximum parsimony tree showed that all genera belonging to a Geotrupidae subfamily were grouped in the same clade, with B. gallicus species isolated in another clade, similar to the chemotaxonomy grouping. A strong positive correlation between chemotaxonomy and genetic phylogeny has been demonstrated, underlying a genetic basis for cuticular hydrocarbon variations. Our results are congruent with previous studies using morphological or genetic data. Our results also showed that only 10 compounds can be used to distinguish at least six species of dung beetle and that chemotaxonomy could become a useful and affordable tool to determine phylogenetic relationships in insects.

Keywords: Geotrupidae, Bolboceratidae, chemotaxonomy, phylogeny


The cuticle of insects, including the Geotrupidae dung beetles (Coleoptera), is rich in various chemical compounds, primarily hydrocarbons. Several studies have reported the role of cuticular hydrocarbons in the intraspecific communication and mating behavior in Coleoptera (Peterson et al. 2007, Geiselhardt et al. 2009, Ming and Lewis 2010), including the recognition of sexual partners in dung beetles (Ortiz-Domínguez et al. 2006). Hydrocarbons are also used by phoretic mite species as chemical cues for host recognition (Krantz et al. 1991; Krantz and Royce 1994; Takaku et al. 1994; Niogret et al. 2006, 2010). Golden et al. (1992) and Nikolova et al. (1999) noted that the hydrocarbon composition of Coleopteran cuticle was not affected by their diet, excluding effects of environmental factors on the cuticle hydrocarbon variability.

Chemotaxonomy is the use of chemical characters, such as cuticular compounds (CCs), to infer phylogeny. These CCs were used to discriminate between different species in many social and solitary insects (Kaib et al. 1991; Chapman et al. 1995; Blum et al. 2000; Haverty et al. 2000, 2005; Page et al. 2002; Dronnet et al. 2006; Dapporto 2007; Baracchi et al. 2009). Jacob and Hanssen (1986) published one of the first studies demonstrating the use of CCs as taxonomic characters for the chemotaxonomy in Coleoptera. Since then, various studies on Coleoptera families showed that these cuticular characters were species specific within a family, such as in Tenebrionidae (Lockey 1992), Curculionidae (Page et al. 1997, Howard and Perez-Lachaud 2002), Staphylinidae (Lusebrink et al. 2007), and Scarabaeidae (Fletcher et al. 2008).

According to the World Scarabaeidae database, the Geotrupidae family Latreille, 1802 includes 27 genera and more than 360 species distributed in temperate, subtropical, and Asian tropical regions (Schoolmeesters 2010). Most Coleopteran classifications, including those for the Geotrupidae family, are based on adult and/or larval morphological characters, but there is still debate regarding the position of various subfamilies. According to some authors, the Geotrupidae family consists of three subfamilies: Geotrupinae, Lethrinae, and Taurocerastinae (Scholtz and Browne 1996, Browne and Scholtz 1999). However, the situation of the Bolboceratidae family is controversial, alternatively considered as a subfamily of the Geotrupidae (Lawrence and Newton 1995, Smith 2006) or as a separate clade (Browne and Scholtz 1999, Verdú et al. 2004). Since the 1950s, dung beetles belonging to the Geotrupidae family were more intensively studied, but only a few papers focused on phylogenetic classifications based on molecular tools (Carisio et al. 2004, Smith 2006, Cunha et al. 2011). To our knowledge, only one of these studies has considered the Bolboceratidae family in their sampling, and they supported its placement in the Geotrupidae family (Smith 2006).

In the present article, we studied 12 species of dung beetle from the Western Mediterranean Basin, including a Bolboceratid species, using cuticular chemical characters as a classification tool. We also compared this chemotaxonomy with a phylogeny based on more conventional genetic markers. To our knowledge, this is the first study to combine both chemotaxonomy and genetics to generate and to compare Coleoptera phylogenies.

Materials and Methods

Sampling

Insects were collected from multiple sites within the Mediterranean region using pitfall traps (CSR model according to Lobo et al. 1988 and Veiga et al. 1989) baited with fresh cattle dung (see Table 1 for locations). Twelve species of dung beetles were analyzed. Eleven species belonging to the Geotrupidae family were morphologically identified (Baraud 1992) as the following species: Anoplotrupes stercorosus (Scriba, 1791), Geotrupes mutator (Marsham, 1802), Geotrupes spiniger (Marsham, 1802), Geotrupes stercorarius (Linnaeus, 1758), Jekelius nitidus (Jekel, 1865), Sericotrupes niger (Marsham, 1802), Thorectes baraudi López-Colón, 1981, Thorectes lusitanicus (Jekel, 1865), Trypocopris pyrenaeus (Charpentier, 1825), Trypocopris vernalis (Linnaeus, 1758), and Typhaeus typhoeus (Linnaeus, 1758). Unfortunately, only Bolbelasmus gallicus (Mulsant, 1842) belonging to the Bolboceratidae family have been collected in our sampling area.

Table 1.

Locations and elevation of the pitfall traps used to catch the dung beetles in the Mediterranean region

Country and region Location name Location coordinates Elevation Collected species
France and Ariège Aulus-les-Bains (col d’Agnes) 42°47′N 01°22′E 1,570 m Geotrupes stercorarius
France and Gard Valleraugue (mont Aigoual) 44°07′N 03°35′E 1,500 m Trypocopris pyrenaeus
Anduze 44°03′N 03°59′E 250 m Typhaeus typhoeus
Junas 43°46′N 04°07′E 60 m Bolbelasmus gallicus
Souvignargues 43°48′N 04°07′E 100 m B. gallicus
France and Hérault Le Caylar 43°51′N 03°19′E 745 m Anoplotrupes stercorosus, Geotrupes mutator, Trypocopris vernalis
France and Lozère Florac 44°19′N 03°35′E 600 m Sericotrupes niger
France and Pyrénées-Orientales Font Romeu 42°30′N 02°03′E 1,600 m A. stercorosus, G. stercorarius, Teuchestes fossor
Mosset (col de Jau) 42°41′N 02°15′E 1,515 m A. stercorosus, G. stercorarius, Tr. pyrenaeus
Le Perthus 42°28′N 02°51′E 300 m G. mutator, Geotrupes spiniger, S. niger
Spain Algesiras 36°09′N 5°35′W 240 m Thorectes lusitanicus
Cabañeros National Park 39°24′N 0°35′W 800 m Jekelius nitidus, Thorectes baraudi

Chemical Analysis

Live beetles were cleaned with distilled water to remove potential dirt and then dried. To avoid cuticular modification induced by stress from trapping and cleaning protocols, the beetles were placed in small plastic containers and left undisturbed for 4 h after manipulation. Beetles were then frozen for 1 h at −25°C, and their abdomens were individually soaked in 2-ml pentane for 5 min. Gas chromatography linked to a mass spectrometer (GC–MS) was used to identify CCs extracted by the solvent. The GC–MS (Shimadzu QP2010 Plus MS coupled with a Shimadzu GC-2010 GC; Shimadzu, Kyoto, Japan) was set with the following parameters: electron impact: 70 eV, 40–330 amu, injector split-splitless at 270°C, oven temperature ramped from 100 to 300°C at 5°C/min and equipped with an SLB-TM-5-MS (Supelco) column, 30 m × 0.25 mm × 0.25 µm film thickness. CCs were identified by comparing mass spectrometers to NIST05 library, chemical standards, and retention index from ‘The Pherobase’ (El-Sayed 2012). The number of replicates varied per species: 7 A. stercorosus, 11 B. gallicus, 6 G. mutator, 4 G. spiniger, 12 G. stercorarius, 8 J. nitidus, 5 S. niger, 9 Th. baraudi, 11 Th. lusitanicus, 12 Tr. pyrenaeus, 4 Tr. vernalis, and 6 Ty. typhoeus. Compounds representing more than 0.1% of the chemical profile for at least one species were selected and ranked according to their retention index. The relative abundance of each compound was calculated by integrating the area of each peak.

Chemotaxonomy

To allow analysis of individual chemical profiles, the relative areas of peaks were converted to percentage of the total amount of the selected compounds. To visualize pattern differences among species and the 95% confidence ellipses around species, the relative areas of the 69 selected compounds were subjected to a non-metric multidimensional scaling (NMDS), and a cluster analysis using the average linkage (between individuals) method and Euclidean distance among chemicals as a dissimilarity measure using R 2.10.1 software (R Development Core Team 2010), with vegan function and Bray–Curtis index. The similarity percentage analysis (SIMPER) and the analysis of similarities (ANOSIM) were performed on Past 1.99 (Hammer et al. 2001).

DNA Extraction and PCR Amplifications

Total genomic DNA was extracted from one leg using DNeasy Blood and Tissue Kit (QIAGEN, Hombrechtikon, Switzerland) with slight modifications. After solvent extraction of the CCs, beetles were stored in dry conditions. With the intention of improving DNA extraction quality from dry tissues, and to enable more efficient lysis, we modified the conditions of the incubation step with proteinase K. The extracted tissues therefore were incubated for 10 min at 72°C with 20 µl of proteinase K and then kept overnight at 55°C.

Mitochondrial DNA

A 469-base pairs (bp) fragment of the gene encoding Cytochrome Oxidase I (COI) was amplified using primers C1-J-2441 and TL2-N-3014 described in Simon et al. (1994). Polymerase chain reactions (PCR) were performed using the following conditions: initial denaturation for 5 min at 95°C; 40 cycles of 94°C for 1 min, 45–50°C for 1 min, and 72°C for 40 s; and 10-min final extension at 72°C.

Nuclear DNA

An 822-bp fragment of the nuclear gene encoding 18 S Ribosomal marker was amplified with primers 5’18 S and 18 l described in Maddison et al. (1999). We obtained partial amplifications, so we used 500-bp fragment for the beginning of the gene (5’18 S primer) and 322 bp for the end of the gene (18 l primer) to build an 822-bp 18 S nuclear gene fragment. PCR was performed using the following conditions: initial denaturation for 5 min at 95°C; 35 cycles of 94°C for 30 s, 54–56°C for 30 s, and 72°C for 2 min 10 s, and 10-min final extension at 72°C.

Both amplifications (mitochondrial and nuclear fragments) were carried out on a thermocycler (Biometra, Archamps, France) and performed in a volume of 25 µl: 2.5 µl of 10× buffer, 2.5 µl MgCl2 (25 mM), 1 µl primers (10 µM), 0.3 µl dNTPs (20 nM), 1 µl DNA, and 1U of Promega Taq polymerase.

Sequencing and Phylogenetic Trees

PCR products were cleaned and sequenced either by a commercial facility (www.lgcgenomics.com) or by using exosapit purification: a blend of 15 µl PCR DNA and 2 µl exosapit solution was put in a Biometra thermocycler (15 min at 37°C following by 15 min at 80°C). All sequencing was performed in both directions. Sequence alignments were done with the BioEdit 7.0.5 software (Raleigh, NC; Hall 1999) by comparing with a previous sequence of COI gene fragment from G. stercorarius (AY039377Villalba et al. 2002) for the mitochondrial gene and a previous sequence of 18 S gene fragment from G. spiniger (AY745561.1Caterino et al. 2005) for the nuclear gene.

Phylogenetic analyses were carried out using an alignment of the concatenation of both sequenced fragments. All positions containing gaps were treated as missing data. Pairwise distances between haplotypes were obtained under the assumptions of the maximum composite likelihood model, and the distance-based tree was inferred using the neighbor-joining (NJ) method (MEGA 4.1 software; Tamura et al. 2007). Tree robustness was tested under bootstrap analysis (1,000 replicates). Numbers of replicates per sequenced species (n = 41 individuals) were the following: 5 A. stercorosus, 4 B. gallicus, 3 G. mutator, 3 G. spiniger, 4 G. stercorarius, 2 J. nitidus, 3 S. niger, 3 Th. baraudi, 3 Th. lusitanicus, 5 Tr. pyrenaeus, 1 Tr. vernalis, 3 Ty. typhoeus. Teuchestes fossor (Linnaeus, 1758) (Coleoptera: Aphodiidae) was selected as an outgroup to root our trees due to its relative distance to the Geotrupinae and the Bolboceratid species (our results have confirmed that those two groups were two distinct families).

Results

Chemical Analysis

In our analysis, we selected 69 CCs with substantial quantitative or qualitative differences providing enough information to discriminate between the species. Representative chromatograms for each species are shown in Fig. 1, and the identification and proportion of the 69 CCs are described in Table 2. We did not find any qualitative or quantitative chemical differences between males and females in any of the species studied. The ANOSIM allowed us to distinguish the species in 95.5% of the cases (P < 0.005; included 41% with P < 0.0001; data not shown), i.e., there is a significant separation between all the species but four, between A. stercorosus and G. stercorarius, between Tr. vernalis and G. mutator, and between Tr. vernalis and G. stercorarius. The estimated contribution of single compounds using a SIMPER analysis by pooling all species to the observed variation between species showed that the 10 first compounds responsible for 44% of the observed total variance were in the following order (Fig. 1): CC25 (pentacosene), CC54 (squalene), CC24 (5,9-pentacosadiene), CC36 (methylhexacosane), CC39 (ethylpentacosane), CC3 (heneicosene), CC40 (heptacosene), CC4 (heneicosane), CC44 (heptacosane), and CC27 (pentacosane; data not shown). CC25, CC24, CC39, CC44, and CC27 were present in all species, but at different ratios. CC25 was one of the major peaks in A. stercorosus, G. mutator, G. stercorarius, and Tr. vernalis; CC24 was the highest in Th. lusitanicus and predominant in J. nitidus; CC44 in both Trypocopris species; and CC27 was predominant in Tr. pyrenaeus. Three compounds, CC54, CC36, and CC40, were present in all species with the exception of B. gallicus. Moreover, CC54 was the major peak in S. niger and G. spiniger; CC36 and CC40 were the highest in Ty. typhoeus and Tr. pyrenaeus, respectively. CC3, the major peak in B. gallicus, was present only in three other species (J. nitidus, Tr. pyrenaeus, and Th. lusitanicus) and in a very low ratio. CC4, the second major peak in B. gallicus, was absent or present at a very low level in all the remaining species (see Table 2).

Fig. 1.

Fig. 1.

Representative gas chromatography spectra of cuticular compounds from the 12 studied species of dung beetles.

Table 2.

Cuticular compound composition of the 12 studied species of dung beetles

RI Name Anoplotrupes stercorosus Bolbelasmus gallicus Geotrupes mutator Geotrupes spiniger Geotrupes stercorarius Jekelius nitidus
CC1 2069 Heneicosanol 0.00 ± 0.00 4.78 ± 6.28 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.08 ± 0.19
CC2 2081 Heneicosene 0.23 ± 0.51 1.04 ± 0.35 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC3 2092 Heneicosene 0.00 ± 0.00 21.29 ± 4.60 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.01 ± 0.03
CC4 2103 Heneicosane 0.31 ± 0.35 16.68 ± 3.98 0.19 ± 0.24 0.00 ± 0.00 0.48 ± 0.44 0.40 ± 1.14
CC5 2118 (Z)-3,7,11,15-Tetramethyl-2-hexadecen-1-ol 0.00 ± 0.00 1.09 ± 0.87 0.00 ± 0.00 0.00 ± 0.00 0.37 ± 0.95 0.00 ± 0.00
CC6 2155 Ethyl octadecenoate 0.00 ± 0.00 8.77 ± 5.16 0.00 ± 0.00 0.00 ± 0.00 0.15 ± 0.54 0.02 ± 0.07
CC7 2200 Docosane 0.03 ± 0.08 0.32 ± 0.10 0.26 ± 0.41 0.19 ± 0.27 0.20 ± 0.31 0.00 ± 0.00
CC8 2228 Docosene 0.00 ± 0.00 0.00 ± 0.00 0.07 ± 0.18 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC9 2233 Methyldocosane 0.00 ± 0.00 4.27 ± 3.13 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.01 ± 0.03
CC10 2240 Methyldocosane 0.00 ± 0.00 4.06 ± 2.07 0.07 ± 0.16 0.00 ± 0.00 0.09 ± 0.20 0.12 ± 0.38
CC11 2249 Methyldocosane 0.00 ± 0.00 1.00 ± 0.44 0.09 ± 0.22 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC12 2269 Methyldocosane 0.98 ± 0.50 0.63 ± 0.31 0.63 ± 1.53 0.00 ± 0.00 0.99 ± 1.67 1.34 ± 1.00
CC13 2275 9-Tricosene 0.27 ± 0.25 0.10 ± 0.19 0.00 ± 0.00 0.00 ± 0.00 0.77 ± 0.96 0.03 ± 0.08
CC14 2280 Methyldocosane 0.90 ± 0.59 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.68 ± 1.09 0.02 ± 0.07
CC15 2292 (Z)-5-Tricosene 0.07 ± 0.18 2.77 ± 1.14 0.00 ± 0.00 0.00 ± 0.00 0.11 ± 0.38 0.43 ± 0.92
CC16 2302 Tricosane 2.55 ± 1.41 1.84 ± 0.59 1.08 ± 0.85 1.14 ± 0.90 4.48 ± 1.56 1.31 ± 2.55
CC17 2320 Trimethyl docosane 0.00 ± 0.00 1.71 ± 1.74 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.02 ± 0.07
CC18 2348 Methyl tricosane 0.64 ± 0.48 0.00 ± 0.00 0.07 ± 0.17 0.08 ± 0.17 0.18 ± 0.21 0.34 ± 0.44
CC19 2378 Dimethyltricosane 0.66 ± 0.33 0.19 ± 0.11 0.34 ± 0.48 0.00 ± 0.00 0.72 ± 0.59 0.21 ± 0.15
CC20 2386 Trimethyl docosane 2.40 ± 1.06 0.00 ± 0.00 0.32 ± 0.37 0.08 ± 0.18 1.45 ± 0.69 0.33 ± 0.18
CC21 2393 Trimethyl tricosane 0.22 ± 0.38 0.03 ± 0.03 0.00 ± 0.00 0.00 ± 0.00 0.15 ± 0.22 0.31 ± 0.25
CC22 2402 Tetracosane 1.39 ± 1.37 0.37 ± 0.16 0.80 ± 0.48 0.54 ± 0.42 1.67 ± 0.75 1.03 ± 0.28
CC23 2414 Ethyl tricosane 0.00 ± 0.00 0.04 ± 0.03 0.25 ± 0.61 2.77 ± 2.51 1.48 ± 1.62 0.15 ± 0.14
CC24 2472 5,9-Pentacosadiene 6.72 ± 1.38 0.35 ± 0.12 4.66 ± 2.14 4.06 ± 1.24 4.84 ± 2.02 11.10 ± 4.47
CC25 2477 Pentacosene (Z7 ou Z9) 16.02 ± 7.94 0.02 ± 0.02 17.83 ± 12.89 0.71 ± 0.60 21.85 ± 12.38 0.82 ± 0.55
CC26 2484 5-Pentacosene 8.15 ± 3.41 0.03 ± 0.03 1.33 ± 1.51 0.20 ± 0.28 5.38 ± 3.79 0.49 ± 0.32
CC27 2502 Pentacosane 6.93 ± 3.03 6.87 ± 1.81 5.72 ± 2.22 5.81 ± 1.69 9.33 ± 2.43 3.71 ± 2.60
CC28 2507 Methyl-tetracosane 0.61 ± 0.45 0.00 ± 0.00 0.73 ± 0.60 0.70 ± 0.48 0.69 ± 0.58 1.22 ± 0.67
CC29 2535 13-Methylpentacosane 2.27 ± 1.00 0.16 ± 0.08 0.99 ± 0.38 4.30 ± 2.27 1.60 ± 0.63 4.60 ± 1.20
CC30 2540 Methylpentacosane 0.50 ± 0.41 0.02 ± 0.02 0.00 ± 0.00 2.16 ± 0.85 0.26 ± 0.22 2.03 ± 1.33
CC31 2551 5-Methylpentacosane 0.55 ± 0.46 0.00 ± 0.00 0.11 ± 0.28 0.28 ± 0.40 0.09 ± 0.24 1.66 ± 1.05
CC32 2569 5-Methylpentacosane 2.02 ± 0.62 0.11 ± 0.06 3.19 ± 1.42 1.84 ± 0.63 1.78 ± 0.55 2.45 ± 0.96
CC33 2574 3-Methylpentacosane 4.03 ± 1.14 0.06 ± 0.06 0.48 ± 1.18 2.32 ± 0.90 3.06 ± 1.21 3.78 ± 0.95
CC34 2580 Methylpentacosane 2.20 ± 1.45 0.04 ± 0.07 0.59 ± 0.35 3.82 ± 2.57 0.67 ± 0.34 3.04 ± 1.13
CC35 2600 Hexacosane 1.35 ± 0.53 0.33 ± 0.10 2.40 ± 1.01 1.90 ± 1.90 1.42 ± 0.65 4.38 ± 1.30
CC36 2611 Methyl-hexacosane 1.75 ± 1.34 0.00 ± 0.00 0.95 ± 1.26 8.15 ± 6.60 2.21 ± 1.44 5.71 ± 2.03
CC37 2632 Unidentified hydrocarbon 0.13 ± 0.25 0.03 ± 0.05 0.00 ± 0.00 2.90 ± 1.66 0.08 ± 0.16 0.03 ± 0.11
CC38 2640 Methyl-hexacosane 1.19 ± 1.27 0.17 ± 0.14 2.02 ± 1.83 0.83 ± 0.69 1.40 ± 0.69 1.11 ± 0.68
CC39 2670 Ethylpentacosane 6.33 ± 2.65 1.02 ± 0.50 10.57 ± 3.62 5.11 ± 2.94 3.47 ± 1.49 11.77 ± 2.24
CC40 2684 Heptacosene 3.69 ± 1.26 0.00 ± 0.00 9.63 ± 6.12 4.20 ± 6.31 5.17 ± 4.23 1.02 ± 0.46
CC41 2692 Heptacosene 1.04 ± 0.64 0.38 ± 0.60 3.15 ± 1.34 2.33 ± 3.83 2.37 ± 1.33 0.29 ± 0.21
CC42 2694 Dimethylhexacosane 0.00 ± 0.00 0.00 ± 0.00 0.06 ± 0.10 0.00 ± 0.00 0.17 ± 0.26 2.52 ± 2.08
CC43 2696 Dimethylhexacosane 0.28 ± 0.32 0.00 ± 0.00 0.06 ± 0.15 0.22 ± 0.49 0.11 ± 0.18 3.55 ± 2.39
CC44 2700 Heptacosane 4.04 ± 2.58 3.06 ± 1.15 5.52 ± 1.25 2.97 ± 1.08 5.27 ± 4.99 1.28 ± 2.76
CC45 2716 Unidentified hydrocarbon 0.07 ± 0.13 0.00 ± 0.00 0.55 ± 0.75 0.16 ± 0.35 0.10 ± 0.21 0.33 ± 0.34
CC46 2739 Methylheptacosane 2.26 ± 1.24 0.05 ± 0.06 1.32 ± 1.15 1.65 ± 0.45 0.99 ± 0.50 2.84 ± 1.31
CC47 2737 Methylheptacosane 0.25 ± 0.27 0.30 ± 0.54 0.94 ± 0.45 0.57 ± 0.75 0.27 ± 0.25 0.87 ± 0.61
CC48 2742 Methylheptacosane 0.00 ± 0.00 0.00 ± 0.00 0.10 ± 0.24 0.08 ± 0.19 0.00 ± 0.00 1.04 ± 0.60
CC49 2750 Methylheptacosane 0.09 ± 0.15 0.30 ± 0.59 0.71 ± 1.74 0.00 ± 0.00 0.08 ± 0.25 0.00 ± 0.00
CC50 2770 Methylheptacosane 1.02 ± 0.26 0.10 ± 0.12 1.51 ± 1.20 1.94 ± 0.84 0.73 ± 0.54 1.14 ± 0.65
CC51 2780 Methylheptacosane 1.49 ± 0.26 0.07 ± 0.12 3.49 ± 0.66 1.37 ± 1.02 1.21 ± 0.83 7.65 ± 2.37
CC52 2786 Methylheptacosane 0.65 ± 0.52 0.10 ± 0.21 0.00 ± 0.00 0.20 ± 0.19 0.21 ± 0.16 2.87 ± 0.67
CC53 2800 Octacosane 0.28 ± 0.27 0.41 ± 0.15 0.60 ± 0.64 0.34 ± 0.21 0.15 ± 0.23 2.54 ± 1.65
CC54 2816 Squalene 7.35 ± 5.42 0.00 ± 0.00 8.38 ± 8.35 17.55 ± 9.80 5.61 ± 3.38 1.57 ± 1.93
CC55 2858 Methyloctacosane 1.13 ± 0.96 0.11 ± 0.16 1.13 ± 1.52 0.27 ± 0.59 0.75 ± 0.74 0.65 ± 0.34
CC56 2864 Methyloctacosane 1.09 ± 1.07 3.86 ± 2.18 1.83 ± 2.18 4.73 ± 1.37 1.35 ± 1.34 0.29 ± 0.62
CC57 2893 Nonacosene 0.19 ± 0.49 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC58 2900 Nonacosane 1.88 ± 1.10 3.14 ± 0.82 2.68 ± 0.40 2.40 ± 1.69 1.63 ± 1.65 2.69 ± 2.36
CC59 2932 11,13-Dimethyloctacosane C30 0.96 ± 1.09 0.38 ± 0.13 0.72 ± 0.85 2.83 ± 3.13 0.32 ± 0.21 0.93 ± 1.72
CC60 2974 Methylnonacosane 0.33 ± 0.39 0.21 ± 0.15 0.28 ± 0.43 1.24 ± 0.36 0.19 ± 0.48 0.60 ± 0.47
CC61 2981 Methylnonacosane 0.00 ± 0.00 0.72 ± 0.42 0.30 ± 0.41 1.04 ± 0.67 0.05 ± 0.14 0.59 ± 0.35
CC62 2984 Methylnonacosane 0.00 ± 0.00 0.12 ± 0.10 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC63 3000 Triacontane 0.00 ± 0.00 0.22 ± 0.16 0.00 ± 0.00 0.20 ± 0.27 0.01 ± 0.02 0.07 ± 0.21
CC64 3039 Methyltriacontane 0.00 ± 0.00 0.25 ± 0.27 0.07 ± 0.18 0.00 ± 0.00 0.17 ± 0.30 0.00 ± 0.00
CC65 3064 Methyltriacontane 0.00 ± 0.00 0.16 ± 0.24 0.00 ± 0.00 0.00 ± 0.00 0.11 ± 0.29 0.00 ± 0.00
CC66 3079 Methyltriacontane 0.09 ± 0.16 4.25 ± 2.05 0.00 ± 0.00 1.88 ± 2.67 0.16 ± 0.25 0.02 ± 0.06
CC67 3101 Methyltriacontane 0.11 ± 0.19 0.47 ± 0.62 0.22 ± 0.35 1.16 ± 0.77 0.12 ± 0.30 0.13 ± 0.43
CC68 3107 Hentriacontane 0.00 ± 0.00 0.25 ± 0.37 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC69 3129 13-Methylhentriacontane 0.30 ± 0.31 0.90 ± 0.88 0.92 ± 0.27 0.79 ± 0.50 0.57 ± 0.60 0.46 ± 0.42
CC1 2069 Heneicosanol 0.00 ± 0.00 0.00 ± 0.00 1.35 ± 1.45 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC2 2081 Heneicosene 0.00 ± 0.00 0.00 ± 0.00 0.58 ± 0.36 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC3 2092 Heneicosene 0.00 ± 0.00 0.00 ± 0.00 0.07 ± 0.17 0.02 ± 0.06 0.00 ± 0.00 0.00 ± 0.00
CC4 2103 Heneicosane 0.07 ± 0.15 0.00 ± 0.00 2.47 ± 0.87 0.58 ± 0.25 0.00 ± 0.00 0.00 ± 0.00
CC5 2118 (Z)-3,7,11,15-Tetramethyl-2-hexadecen-1-ol 1.98 ± 3.02 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC6 2155 Ethyl octadecenoate 0.00 ± 0.00 0.00 ± 0.00 0.03 ± 0.11 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC7 2200 Docosane 0.13 ± 0.29 0.00 ± 0.00 0.00 ± 0.00 0.47 ± 0.27 0.00 ± 0.00 0.33 ± 0.38
CC8 2228 Docosene 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.21 ± 0.34
CC9 2233 Methyldocosane 0.00 ± 0.00 0.00 ± 0.00 0.07 ± 0.13 0.00 ± 0.00 0.00 ± 0.00 0.08 ± 0.20
CC10 2240 Methyldocosane 0.00 ± 0.00 0.00 ± 0.00 3.60 ± 3.17 0.00 ± 0.00 0.00 ± 0.00 0.08 ± 0.19
CC11 2249 Methyldocosane 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00 0.19 ± 0.33
CC12 2269 Methyldocosane 0.33 ± 0.49 1.33 ± 1.17 10.05 ± 2.77 1.00 ± 0.54 0.38 ± 0.44 0.05 ± 0.13
CC13 2275 9-Tricosene 0.00 ± 0.00 0.00 ± 0.00 0.30 ± 0.35 0.64 ± 0.54 0.38 ± 0.50 0.00 ± 0.00
CC14 2280 Methyl docosane 0.00 ± 0.00 0.12 ± 0.16 0.51 ± 0.52 5.31 ± 2.42 1.29 ± 1.91 0.00 ± 0.00
CC15 2292 (Z)-5-Tricosene 0.27 ± 0.59 0.01 ± 0.04 0.23 ± 0.28 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC16 2302 Tricosane 1.30 ± 0.84 1.79 ± 0.64 3.16 ± 1.68 5.15 ± 1.77 1.91 ± 1.42 0.13 ± 0.33
CC17 2320 Trimethyl docosane 0.00 ± 0.00 0.00 ± 0.00 0.09 ± 0.23 0.00 ± 0.00 0.00 ± 0.00 0.00 ± 0.00
CC18 2348 Methyl tricosane 0.50 ± 0.73 0.75 ± 0.46 1.08 ± 0.73 0.13 ± 0.14 0.00 ± 0.00 0.10 ± 0.24
CC19 2378 Dimethyltricosane 0.13 ± 0.29 0.22 ± 0.14 0.39 ± 0.52 1.39 ± 0.64 0.54 ± 0.62 0.16 ± 0.40
CC20 2386 Trimethyl docosane 0.48 ± 0.69 0.75 ± 0.31 0.40 ± 0.61 1.25 ± 0.53 1.76 ± 2.00 0.26 ± 0.41
CC21 2393 Trimethyl tricosane 0.00 ± 0.00 0.69 ± 0.51 1.46 ± 1.15 0.00 ± 0.00 0.50 ± 0.68 0.00 ± 0.00
CC22 2402 Tetracosane 0.24 ± 0.33 0.70 ± 0.15 2.03 ± 0.58 2.26 ± 0.79 1.81 ± 0.67 0.11 ± 0.17
CC23 2414 Ethyl tricosane 0.13 ± 0.28 1.06 ± 0.56 1.75 ± 0.50 0.36 ± 0.23 0.47 ± 0.54 0.49 ± 0.44
CC24 2472 5,9-Pentacosadiene 1.74 ± 2.39 8.21 ± 2.56 10.70 ± 2.08 1.84 ± 0.85 5.13 ± 2.49 1.26 ± 0.76
CC25 2477 Pentacosene (Z7 ou Z9) 0.79 ± 0.78 0.42 ± 0.48 0.79 ± 0.52 1.03 ± 0.33 14.53 ± 8.26 0.05 ± 0.13
CC26 2484 5-Pentacosene 0.25 ± 0.35 1.48 ± 0.61 0.43 ± 0.50 0.92 ± 0.35 1.99 ± 1.50 0.00 ± 0.00
CC27 2502 Pentacosane 3.68 ± 1.10 5.79 ± 2.21 2.81 ± 1.50 9.47 ± 1.97 7.84 ± 3.62 3.43 ± 0.80
CC28 2507 Methyl-tetracosane 0.00 ± 0.00 0.36 ± 0.23 0.18 ± 0.24 0.00 ± 0.00 0.14 ± 0.28 3.41 ± 1.08
CC29 2535 13-Methylpentacosane 0.66 ± 0.75 2.42 ± 0.98 2.65 ± 0.78 1.77 ± 0.73 0.51 ± 0.60 3.55 ± 1.55
CC30 2540 Methylpentacosane 0.14 ± 0.32 1.75 ± 0.59 0.59 ± 0.36 0.87 ± 0.41 0.46 ± 0.53 2.09 ± 1.06
CC31 2551 5-Methylpentacosane 0.00 ± 0.00 1.67 ± 0.65 0.21 ± 0.32 0.32 ± 0.30 0.08 ± 0.16 0.34 ± 0.39
CC32 2569 5-Methylpentacosane 0.55 ± 0.60 0.59 ± 0.09 2.80 ± 0.60 1.01 ± 0.22 0.39 ± 0.56 0.96 ± 0.86
CC33 2574 3-Methylpentacosane 1.74 ± 0.38 2.97 ± 0.49 1.73 ± 1.07 3.42 ± 0.57 3.93 ± 1.10 5.61 ± 2.98
CC34 2580 Methylpentacosane 0.67 ± 1.14 1.07 ± 0.57 5.23 ± 3.10 0.84 ± 0.36 0.76 ± 0.51 1.61 ± 0.99
CC35 2600 Hexacosane 0.42 ± 0.43 9.70 ± 3.59 3.05 ± 2.56 2.56 ± 0.63 2.30 ± 0.82 0.75 ± 0.42
CC36 2611 Methyl-hexacosane 1.97 ± 0.59 4.78 ± 1.40 2.75 ± 1.57 4.13 ± 1.50 2.96 ± 1.09 20.74 ± 5.89
CC37 2632 Unidentified hydrocarbon 0.00 ± 0.00 0.03 ± 0.06 6.55 ± 4.73 0.00 ± 0.00 0.35 ± 0.41 0.19 ± 0.47
CC38 2640 Methyl-hexacosane 2.28 ± 0.78 2.65 ± 2.37 3.75 ± 0.72 1.30 ± 0.45 1.55 ± 1.12 7.47 ± 1.98
CC39 2670 Ethylpentacosane 3.55 ± 3.05 10.71 ± 3.40 3.90 ± 2.09 3.67 ± 1.50 4.29 ± 2.06 5.10 ± 2.27
CC40 2684 Heptacosene 2.38 ± 1.35 1.56 ± 0.98 1.84 ± 0.88 10.81 ± 2.07 4.25 ± 0.72 0.17 ± 0.41
CC41 2692 Heptacosene 0.67 ± 1.10 0.70 ± 0.24 0.36 ± 0.32 1.43 ± 0.61 1.12 ± 0.77 0.36 ± 0.40
CC42 2694 Dimethylhexacosane 0.21 ± 0.48 0.54 ± 0.14 0.17 ± 0.25 0.00 ± 0.00 0.00 ± 0.00 0.34 ± 0.41
CC43 2696 Dimethylhexacosane 0.00 ± 0.00 2.24 ± 1.74 1.17 ± 0.99 1.61 ± 1.10 1.59 ± 1.59 3.24 ± 1.74
CC44 2700 Heptacosane 5.14 ± 1.08 1.30 ± 0.91 0.89 ± 0.69 8.92 ± 2.26 7.42 ± 5.00 3.21 ± 2.32
CC45 2716 Unidentified hydrocarbon 0.00 ± 0.00 0.45 ± 0.38 0.61 ± 0.55 0.00 ± 0.00 0.12 ± 0.24 3.35 ± 1.89
CC46 2739 Methylheptacosane 3.00 ± 2.42 3.37 ± 0.69 0.99 ± 0.36 1.75 ± 0.51 0.38 ± 0.76 2.20 ± 2.28
CC47 2737 Methylheptacosane 0.43 ± 0.69 2.22 ± 0.45 0.19 ± 0.20 0.00 ± 0.00 0.24 ± 0.48 3.97 ± 2.16
CC48 2742 Methylheptacosane 0.19 ± 0.42 0.86 ± 0.62 0.11 ± 0.15 0.38 ± 0.18 0.38 ± 0.76 0.14 ± 0.35
CC49 2750 Methylheptacosane 0.08 ± 0.18 0.12 ± 0.13 0.00 ± 0.00 0.17 ± 0.14 0.00 ± 0.00 0.48 ± 0.53
CC50 2770 Methylheptacosane 4.03 ± 1.79 0.29 ± 0.18 1.83 ± 0.54 1.34 ± 0.35 0.81 ± 1.07 0.70 ± 0.78
CC51 2780 Methylheptacosane 5.06 ± 2.95 2.47 ± 0.52 0.79 ± 0.39 2.20 ± 0.46 2.86 ± 1.04 4.78 ± 1.37
CC52 2786 Methylheptacosane 0.37 ± 0.82 2.45 ± 0.45 0.95 ± 0.66 0.47 ± 0.20 0.13 ± 0.25 2.31 ± 0.95
CC53 2800 Octacosane 1.12 ± 0.41 0.48 ± 0.48 0.04 ± 0.13 1.09 ± 0.54 1.06 ± 0.79 0.00 ± 0.00
CC54 2816 Squalene 21.25 ± 8.14 5.78 ± 0.80 4.12 ± 1.27 8.81 ± 5.58 5.25 ± 1.33 10.22 ± 3.19
CC55 2858 Methyloctacosane 2.32 ± 0.74 5.27 ± 1.67 1.92 ± 0.56 3.99 ± 2.29 1.91 ± 1.30 3.44 ± 0.89
CC56 2864 Methyloctacosane 10.97 ± 2.25 2.67 ± 2.12 1.56 ± 0.82 0.74 ± 0.34 2.54 ± 1.54 0.66 ± 0.67
CC57 2893 Nonacosene 0.36 ± 0.51 0.00 ± 0.00 0.57 ± 0.67 0.20 ± 0.22 0.14 ± 0.29 0.15 ± 0.24
CC58 2900 Nonacosane 6.32 ± 5.31 0.77 ± 0.55 0.76 ± 0.83 3.67 ± 1.08 5.31 ± 4.74 0.33 ± 0.40
CC59 2932 11,13-Dimethyloctacosane C30 2.77 ± 2.72 1.07 ± 0.70 0.49 ± 0.34 0.37 ± 0.24 0.25 ± 0.50 0.00 ± 0.00
CC60 2974 Methylnonacosane 0.71 ± 0.75 0.00 ± 0.00 0.21 ± 0.30 0.37 ± 0.23 1.66 ± 3.33 0.00 ± 0.00
CC61 2981 Methylnonacosane 1.93 ± 1.49 0.86 ± 0.27 0.00 ± 0.00 0.00 ± 0.00 2.80 ± 5.34 0.00 ± 0.00
CC62 2984 Methylnonacosane 0.25 ± 0.55 0.00 ± 0.00 0.14 ± 0.48 0.00 ± 0.00 0.00 ± 0.00 0.05 ± 0.11
CC63 3000 Triacontane 0.27 ± 0.37 0.87 ± 0.65 0.14 ± 0.36 0.01 ± 0.05 0.14 ± 0.28 0.00 ± 0.00
CC64 3039 Methyltriacontane 0.17 ± 0.38 0.00 ± 0.00 0.03 ± 0.11 0.00 ± 0.00 1.16 ± 1.91 0.00 ± 0.00
CC65 3064 Methyltriacontane 0.66 ± 0.91 0.00 ± 0.00 0.58 ± 0.94 0.95 ± 0.47 0.20 ± 0.41 0.05 ± 0.11
CC66 3079 Methyltriacontane 3.46 ± 3.60 0.60 ± 0.53 0.94 ± 0.92 0.31 ± 0.35 0.43 ± 0.86 0.37 ± 0.58
CC67 3101 Methyltriacontane 0.94 ± 1.46 0.00 ± 0.00 0.30 ± 0.55 0.00 ± 0.00 0.60 ± 0.69 0.37 ± 0.45
CC68 3107 Hentriacontane 0.00 ± 0.00 0.28 ± 0.64 0.00 ± 0.00 0.04 ± 0.10 0.00 ± 0.00 0.00 ± 0.00
CC69 3129 13-Methylhentriacontane 0.94 ± 0.95 0.73 ± 0.96 0.55 ± 0.43 0.71 ± 0.33 0.99 ± 1.30 0.22 ± 0.40

The compounds responsible for 44% of the observed total variance between the species are in bold.

NMDS analysis (Fig. 2) on quantitative variations of CCs revealed that the individuals were regrouped by species (Fig. 2a), and all species were clustered by genus (Fig. 2b) with low individual variability (stress = 0.14). Each species was associated with a specific chemical pattern, even within the same genus. For instance, within the genus Trypocopris, several differences could be described between the two studied species. The major compound of Tr. vernalis, CC25 (14.5%), represented only 1% of the chemical profile of Tr. pyrenaeus, whereas the major compound of Tr. pyrenaeus, CC40 (10.8%), was only present at 4.3% in Tr. vernalis. Moreover, qualitative differences were also species characteristic. Several compounds, e.g., CC3, CC4, and CC7, were absent in Tr. vernalis, but present in Tr. pyrenaeus.

Fig. 2.

Fig. 2.

Non-metric multidimensional scaling (stress value = 0.14) of the 69 cuticular compounds in the 12 studied species (a) and eight studied genius (b) of dung beetles using R 2.10.1 software.

According to NMDS analysis, the most distant species was B. gallicus with an evident distinction from other species. Indeed, the lighter compounds, CC3 and CC4, were responsible for an average of 21.1% of the divergence between B. gallicus and the other species (SIMPER analysis, data not shown). Typhaeus typhoeus and J. nitidus were also among the most divergent species in NMDS results. The two Thorectes species and S. niger were easily distinguishable from the others. The two Trypocopris species were very close. Geotrupes stercorarius and G. mutator were undistinguishable species in the Geotrupes genus, whereas G. spiniger (considered to be a close relative of G. stercorarius) was well distinct.

The cluster analysis (Fig. 3) provided a dendrogram, in which relative distances among the 12 studied species were determined by the average distances among their chemical profiles. We observed the same topology using the NMDS analysis. Bolbelasmus gallicus was very distant from all the other species. As in the NMDS analysis, several species can be dissociated from each other, with all their specific individuals in the same cluster: Ty. typhoeus, J. nitidus, Th. lusitanicus, and Th. baraudi. Also, individuals of Tr. pyrenaeus were recovered as a distinct and separate clade, whereas individuals of Tr. vernalis were distantly scattered across the topology.

Fig. 3.

Fig. 3.

Dendrogram for the 12 studied species of dung beetle species resulting from cluster analysis performed by average linkage between groups and using Euclidean distance and R 2.10.1 software. The relative distances among the individuals were determined by the distances among their chemical profiles.

Moreover, using only the 10 compounds responsible for 44% of the observed total variance described earlier, we could still distinguish 6 of the 12 using either NMDS or cluster analysis: B. gallicus, Ty. typhoeus, J. nitidus, Tr. pyrenaeus, Th. lusitanicus, and Th. baraudi (data not shown).

Sequence Analysis

The sequence alignment was done on the concatenation of gene fragments encoding for both mitochondrial COI and nuclear 18S, with a total 1,291 bp. Interestingly, sequences from individuals B. gallicus were distinguishable by the presence of indels (18 bp) with respect to all the remaining analyzed species. The mean base composition of the concatenation of both genes was as follows: T = 28.8%; C = 22.2%; A = 26.7%; G = 22.3%. For the mitochondrial marker, sequence divergence within species ranged from 0 to 4.7% (data not shown). Inside the Geotrupidae family, excluding B. gallicus, the divergence among species averaged 14.5%. Moreover, between Geotrupidae and Bolboceratidae, the latter represented by B. gallicus, this divergence was high (32.3% on average), which was even higher than sequence divergence with the outgroup (Te. fossor; Aphodiidae; 27.1%). Sequence divergences were weaker for the nuclear marker (data not shown) than for the mitochondrial marker: they ranged from 0 to 1.6% within species, averaged at 0.3% inside Geotrupidae family, and were 2.7 and 2.1% between Geotrupidae and Bolboceratidae and between Geotrupidae and outgroup, respectively.

Phylogenetic Tree

Using the concatenation of the mitochondrial CO1 and the nuclear 18S genes, and a maximum parsimony analysis, the consistency index and the retention index were 0.55 and 0.86, respectively. There were a total of 1,270 positions in the final data set, of which 212 resulted to be informative. The phylogenetic tree inferred using the NJ and maximum parsimony methods yielded the same topology (NJ tree on Fig. 4).

Fig. 4.

Fig. 4.

Neighbor-joining analysis phylogenetic tree for the concatenation of mitochondrial and nuclear used markers. Numbers at nodes indicate the statistical support as obtained from 1,000 bootstrap replicates.

The monophyly of all analyzed genera was tested by bootstrap values (BV) varying from 15 to 100% (Fig. 4). All species, but two Geotrupes (G. stercorarius and G. spiniger), were recovered as monophyletic. Our results suggest that B. gallicus is the most divergent, being highly separated from the other species (BV 100%). Furthermore, the Bolboceratidae family, represented in this study only by B. gallicus, occupied a basal position not only with respect to the remaining ingroup species (family Geotrupidae), but also in relation to the outgroup species (family Aphodiidae).

Discussion

The present study shows that the 12 studied species of dung beetle have distinct chemical profiles of CCs, and their use as systematic characters has demonstrated to be very useful to distinguish genera and species in this specific group of Coleoptera. These CCs are similar to those observed in other groups of insects (Gongyin et al. 2007, Fletcher et al. 2008, Baracchi et al. 2009). Our results demonstrated that the cuticular hydrocarbon profile of 7 of the 12 dung beetle species included in this study (namely, B. gallicus, G. spiniger, J. nitidus, Ty. typhoeus, Tr. pyrenaeus, Th. baraudi, and Th. lusitanicus) had a high taxonomic and diagnostic power. Moreover, only 10 compounds are sufficient to affiliate individuals to the correct species for at least six studied species. Our results also demonstrate that the chemotaxonomy is consistent with the mitochondrial and nuclear phylogenies for the majority of studied species.

Some authors consider the Bolboceratidae family to be a subfamily within the Geotrupidae (Lawrence and Newton 1995, Smith 2006). However, our chemical and molecular results support the separation of Geotrupidae and Bolboceratidae as distinct families (the latter family being represented by only one species in our study), which is in agreement with morphological studies (Browne and Scholtz 1999, Verdú et al. 2004). In addition, our molecular results support that the Bolboceratidae family, represented by B. gallicus, is the most divergent with respect to the Aphodiidae family. The sequence divergence and the phylogenetic distance in tree reconstructions showed that B. gallicus diverged from a common ancestral population at the same time than the Aphodiidae family and a long time before the Geotrupidae family. Our study demonstrates that chemical characters corroborate the genetic divergence for B. gallicus. Therefore, chemotaxonomy can be expected to be used as an important tool for evolutionary studies too. An unsophisticated extraction by solvent of compounds from an insect cuticle will straightforwardly allow to get species affinities when compare with the more time-consuming and expensive DNA extraction and analysis.

The chemotaxonomic model presented in this study was unable to discriminate between some species when the whole chemical profile was considered. For instance, our chemotaxonomic model was unable to distinguish between individuals of G. stercorarius from G. mutator, probably due to their close phylogenetic relationship. This observation underlined the fact that the use of chemical profiles for taxonomic and phylogenetic purpose is rapid, efficient, and cost-effective, but should be used as a consolidate with molecular tools as well. However, some single compounds by themselves can serve as a chemotaxonomic tool to distinguish between close species. For instance, the ratio of two compounds (CC39 and CC40) is higher, whereas the ratio of three other compounds (CC16, CC26, and CC33) is lower in G. mutator compared with G. stercorarius, allowing separation between both species. From a chemical point of view, G. mutator individuals appeared to be closer to G. stercorarius individuals than to G. spiniger, but G. spiniger and G. stercorarius individuals are closer and present in the same clade in the molecular phylogeny. This molecular result is in contradiction with the phylogeny by Cunha et al. (2011), where all Geotrupes species were monophyletic. However, using only the mitochondrial marker, we obtained a strong monophyly for all Geotrupes species (data not shown). We used the 18S nuclear gene, which seems to be less affected by Geotrupes speciation than the neurofibromin gene, used by Cunha et al. (2011).

Our chemotaxonomy and molecular phylogenies are congruent with the morphological taxonomy by Verdú et al. (2004) based on larval morphology. More than 30 morphological characters are needed to establish a phylogeny based on larvae. Thereby, to simplify the approach, it could be interesting to study the dung beetle chemotaxonomy using larval cuticular profiles.

The CCs are known to have a functional role as kairomones to trigger phoretic interactions: they are used by phoretic mites to discriminate their host-carrier among several candidates, even within the same genus (Niogret et al. 2006, 2010). However, mating behavior in dung beetles is not well documented, most probably because males and females are primarily attracted by food resources and do not require other chemical cues to find a mate (Price and May 2009). However, in the field, some dung pats attract many individuals of the same species as, e.g., the case of G. spiniger or G. stercorarius, whereas nearby similar pats contain no beetles (J.-P. Lumaret, personal observation). This aggregation effect may be due to chemical cues other than a food resource, as shown by Ortiz-Domínguez et al. (2006). Our study has shown that each of the studied species can be differentiated by their cuticular profile.

Conclusion

Our study demonstrated that CC profiles are powerful diagnostic tools for species separation among dung beetles. Moreover, CC extraction and analysis could be a simplified and less expensive way to distinguish species when compared with current molecular techniques. Chemical ecology and molecular biology are two main scientific approaches to study insect interactions. The combination of those different techniques can improve our ability to clarify complex hypotheses and evolutionary scenarios that single techniques fail to resolve.

Acknowledgments

We thank Alexandre Larnac and Bruno Buatois (CNRS, Montpellier) for their technical assistance, and Alan Scarlett (Faculty of Science and Technology of Plymouth, UK) and Paul Kendra (USDA, ARS, Miami, FL) for all valuable comments and revision of English. We also thank Jose Ramon Verdú (CIBIO, Alicante University) who provided beetles from Spain.

References Cited

  1. Baracchi D., Dapporto L., Teseo S., Hashim R., and Turillazzi S.. . 2009. Medium molecular weight polar substances of the cuticle as tools in the study of the taxonomy, systematics and chemical ecology of tropical hover wasps (Hymenoptera: Stenogastrinae). J. Zool. Syst. Evol. Res. 48: 109–114. [Google Scholar]
  2. Baraud J. 1992. Coléoptères Scarabaeoidea d’Europe. Faune de France et régions limitrophes, 78. Fédération Française des Sociétés de Sciences Naturelles & Société Linnéenne de Lyon, Paris, France: pp. 856. [Google Scholar]
  3. Blum M. S., Fales H. M., Morse R. A., and Underwood B. A.. . 2000. Chemical characters of two related species of giant honeybees (Apis dorsata and A. laboriosa): Possible ecological significance. J. Chem. Ecol. 26: 801–807. [Google Scholar]
  4. Browne J., and Scholtz C. H.. . 1999. A phylogeny of the families of Scarabaeoidea (Coleoptera). Syst. Entomol. 24: 51–84. [Google Scholar]
  5. Carisio L., Cervella P., Palestrini C., DelPero M., and Rolando A.. . 2004. Biogeographical patterns of genetic differentiation in dung beetles of the genus Trypocopris (Coleoptera, Geotrupidae) inferred from mtDNA and AFLP analyses. J. Biogeogr. 31: 1149–1162. [Google Scholar]
  6. Caterino M. S., Hunt T., and Vogler A. P.. 2005. On the constitution and phylogeny of Staphyliniformia (Insecta: Coleoptera). Mol. Phylogenet. Evol. 34: 655–672. [DOI] [PubMed] [Google Scholar]
  7. Chapman R. F., Espelie K. E., and Sword G. A.. . 1995. Use of cuticular lipids in grasshopper taxonomy – a study of variation in Schistocerca shoshone (Thomas). Biochem. Syst. Ecol. 23: 383–398. [Google Scholar]
  8. Cunha R. L., Verdú J. R., Lobo J. M., and Zardoya R.. 2011. Ancient origin of endemic Iberian earth-boring dung beetles (Geotrupidae). Mol. Phylogenet. Evol. 59: 578–586. [DOI] [PubMed] [Google Scholar]
  9. Dapporto L. 2007. Cuticular lipid diversification in Lasiommata megera and Lasiommata paramegaera: the influence of species, sex, and population (Lepidoptera: Nymphalidae). Biol. J. Linn. Soc. 91: 703–710. [Google Scholar]
  10. Dronnet S., Lohou C., Christides J. P., and Bagnères A. G.. 2006. Cuticular hydrocarbon composition reflects genetic relationship among colonies of the introduced termite Reticulitermes santonensis Feytaud. J. Chem. Ecol. 32: 1027–1042. [DOI] [PubMed] [Google Scholar]
  11. El-Sayed A. 2012. The pherobase: database of insect pheromones and semiochemicals (http://www.pherobase.com) (accessed 2012).
  12. Fletcher M. T., Allsopp P. G., McGrath M. J., Chow S., Gallagher O. P., Hull C., Cribb B. W., Moore C. J., and Kitching W.. . 2008. Diverse cuticular hydrocarbons from Australian canebeetles (Coleoptera: Scarabaeidae). Aust. J. Entomol. 47: 153–159. [Google Scholar]
  13. Geiselhardt S., Otte T., and Hilker M.. 2009. The role of cuticular hydrocarbons in male mating behavior of the mustard leaf beetle, Phaedon cochleariae (F.). J. Chem. Ecol. 35: 1162–1171. [DOI] [PubMed] [Google Scholar]
  14. Golden K. L., Meinke L. J., and Stanleysamuelson D. W.. . 1992. Cuticular hydrocarbon discrimination of Diabrotica (Coleoptera, Chrysomelidae) sibling species. Ann. Entomol. Soc. Am. 85: 561–570. [Google Scholar]
  15. Gongyin Y., Kai L., Jiaying Z., Guanghui Z., and Cui H.. . 2007. Cuticular hydrocarbon composition in pupal exuviae for taxonomic differentiation of six necrophagous flies. J. Med. Entomol. 44: 450–456. [DOI] [PubMed] [Google Scholar]
  16. Hall T. A. 1999. BioEdit: a user-friendly biological sequence alignment editor and analysis program for Windows 95/98/NT. Nucleic Acids Symp. Ser. 41: 95–98. [Google Scholar]
  17. Hammer O., Harper D. A. T., and Ryan P. D.. . 2001. PAST: Paleontological Statistics Software Package for education and data analysis. Paleontol. Electron. 4: 1–9. [Google Scholar]
  18. Haverty M. I., Woodrow R. J., Nelson L. J., and Grace J. K.. . 2000. Cuticular hydrocarbons of termites of the Hawaiian Islands. J. Chem. Ecol. 26: 1167–1191. [Google Scholar]
  19. Haverty M. I., Woodrow R. J., Nelson L. J., and Grace J. K.. 2005. Identification of termite species by the hydrocarbons in their feces. J. Chem. Ecol. 31: 2119–2151. [DOI] [PubMed] [Google Scholar]
  20. Howard R. W., and Perez-Lachaud G.. . 2002. Cuticular hydrocarbons of the ectoparasitic wasp Cephalonomia hyalinipennis (Hymenoptera: Bethylidae) and its alternative host, the stored product pest Caulophilus oryzae (Coleoptera: Curculionidae). Arch. Insect Biochem. Physiol. 50: 75–84. [DOI] [PubMed] [Google Scholar]
  21. Jacob J., and Hanssen H. P.. . 1986. Distribution and variability of cuticular hydrocarbons within the Coleoptera. Biochem. Syst. Ecol. 14: 207–210. [Google Scholar]
  22. Kaib M., Brandl R., and Bagine R. K. N.. . 1991. Cuticular hydrocarbon profiles – a valuable tool in termite taxonomy. Naturwissenschaften 78: 176–179. [Google Scholar]
  23. Krantz G. W., and Royce L. A.. . 1994. Observations on the biology and behavior of Macrocheles mycotrupetes Krantz and Mellott (Acari: Macrochelidae). Int. J. Acarol. 20: 115–121. [Google Scholar]
  24. Krantz G. W., Royce L. A., Lowry R. R., and Kelsey R.. . 1991. Mechanisms of phoretic specificity in Macrocheles (Acari: Macrochelidae), pp. 561–569. InDusbabek F. and Bukva V. (eds.), Modern acarology. Volume II. Proceedings of the VIII International Congress of Acarology, Ceske Budejovice, Czechoslovakia. Springer Science+Business Media, Dordrecht, The Netherlands. [Google Scholar]
  25. Lawrence J. F., and Newton A. F.. . 1995. Families and subfamilies of Coleoptera (with selected genera, notes, references and data on family-group names), pp. 779–1006. In Pakaluk J. and Slipinski S. A. (eds.), Biology, phylogeny and classification of Coleoptera: papers celebrating the 80th birthday of Roy A. Crowson. Muzeum i Instytut Zoologii PAN, Warsaw, Poland. [Google Scholar]
  26. Lobo J. M., Martin-Piera F., and Veiga C. M.. . 1988. Dung-baited pitfall traps for studying coprophagous Scarabaeoidea (Col) communities. 1. Characteristics determining capacity of capture. Revue d’Ecol. Biol. Sol. 25: 77–100. [Google Scholar]
  27. Lockey K. H. 1992. Insect hydrocarbon chemotaxonomy – cuticular hydrocarbons of adult and larval Epiphysa species Blanchard and adult Onymacris unguicularis (Haag) (Tenebrionidae, Coleoptera). Comp. Biochem. Physiol. B Biochem. Mol. Biol. 102: 451–470. [Google Scholar]
  28. Lusebrink I., Burkhardt D., Gedig T., Dettner K., Mosandl A., and Seifert K.. 2007. Intrageneric differences in the four stereoisomers of stenusine in the rove beetle genus, Stenus (Coleoptera, Staphylinidae). Naturwissenschaften 94: 143–147. [DOI] [PubMed] [Google Scholar]
  29. Maddison D. R., Baker M. D., and Ober K. A.. . 1999. Phylogeny of carabid beetles as inferred from 18S ribosomal DNA (Coleoptera: Carabidae). Syst. Entomol. 24: 103–138. [Google Scholar]
  30. Ming Q. L., and Lewis S. M.. . 2010. Mate recognition and sex differences in cuticular hydrocarbons of the diurnal firefly Ellychnia corrusca (Coleoptera: Lampyridae). Ann. Entomol. Soc. Am. 103: 128–133. [Google Scholar]
  31. Nikolova N., Rezanka T., Nikolova-Damyanova B., and Kalushkov P.. . 1999. Hydrocarbons in adult Chrysomela vigintipunctata (Scopoli) (Coleoptera: Chrysomelidae). Comp. Biochem. Physiol. B Biochem. Mol. Biol. 123: 67–77. [Google Scholar]
  32. Niogret J., Lumaret J.-P., and Bertrand M.. . 2006. Review of the phoretic association between coprophilous insects and macrochelid mites (Acari: Mesostigmata) in France. Elytron (Barc.) 20: 99–121. [Google Scholar]
  33. Niogret J., Lumaret J.-P., and Bertrand M.. . 2010. Generalist and specialist strategies in macrochelid mites (Acari: Mesostigmata) phoretically associated with dung beetles (Coleoptera: Scarabaeidae), pp. 343–347. InSabelis M. W. and Bruin J. (eds.), Trends in acarology. Springer, Dordrecht, The Netherlands. [Google Scholar]
  34. Ortiz-Domínguez M., Favila M. E., Mendoza-López M. R., García-Barradas O., and Cruz-Sánchez J. S.. . 2006. Epicuticular compounds and sexual recognition in the ball-roller scarab, Canthon cyanellus cyanellus. Entomol. Exp. Appl. 119: 23–27. [Google Scholar]
  35. Page M., Nelson L. J., Blomquist G. J., and Seybold S. J.. . 1997. Cuticular hydrocarbons as chemotaxonomic characters of pine engraver beetles (Ips spp.) in the grandicollis subgeneric group. J. Chem. Ecol. 23: 1053–1099. [Google Scholar]
  36. Page M., Nelson L. J., Forschler B. T., and Haverty M. I.. 2002. Cuticular hydrocarbons suggest three lineages in Reticulitermes (Isoptera: Rhinotermitidae) from North America. Comp. Biochem. Physiol. B Biochem. Mol. Biol. 131: 305–324. [DOI] [PubMed] [Google Scholar]
  37. Peterson M. A., Dobler S., Larson E. L., Juarez D., Schlarbaum T., Monsen K. J., and Francke W.. . 2007. Profiles of cuticular hydrocarbons mediate male mate choice and sexual isolation between hybridising Chrysochus (Coleoptera: Chrysomelidae). Chemoecology 17: 87–96. [Google Scholar]
  38. Price D. L., and May M. L.. . 2009. Behavioral ecology of Phanaeus dung beetles (Coleoptera: Scarabaeidae): review and new observations. Acta Zool. Mex. 25: 211–238. [Google Scholar]
  39. R Development Core Team 2010. R: a language and environment for statistical computing, reference index version 2.10.1. R Foundation for Statistical Computing, Vienna, Austria: (http://www.R-project.org). [Google Scholar]
  40. Scholtz C. H., and Browne D. J.. . 1996. Polyphyly in the Geotrupidae (Coleoptera: Scarabaeoidea): a case for a new family. J. Nat. Hist. 30: 597–614. [Google Scholar]
  41. Schoolmeesters P. 2010. World Scarabaeidae database. InBisby F. A., Ruggiero M. A., Roskov Y. R., Cachuela-Palacio M., Kimani S. W., Kirk P. M., Soulier-Perkins A., and Hertum J. V. (eds.), Catalogue of life: 2006 Annual checklist. Species 2000 and ITIS, Reading, United Kingdom. [Google Scholar]
  42. Simon C., Frati F., Beckenbach A., Crespi B., Liu H., and Flook P.. . 1994. Evolution, weighting, and phylogenetic utility of mitochondrial gene-sequences and a compilation of conserved polymerase chain reaction primers. Ann. Entomol. Soc. Am. 87: 651–701. [Google Scholar]
  43. Smith A. B. T. 2006. An overview of the classification and evolution of the major scarab beetle clades (Coleoptera: Scarabaeoidea) based on preliminary molecular analyses. Coleopterists Bull. 60: 35–46. [Google Scholar]
  44. Takaku G., Katakura H., and Yoshida N.. . 1994. Mesostigmatic mites (Acari) associated with ground, burying, roving carrion and dung beetles (Coleoptera) in Sapporo and Tomakomai, Hokkaido, Northern Japan. Zool. Sci. 11: 305–311. [Google Scholar]
  45. Tamura K., Dudley J., Nei M., and Kumar S.. 2007. MEGA4: Molecular Evolutionary Genetics Analysis (MEGA) software version 4.0. Mol. Biol. Evol. 24: 1596–1599. [DOI] [PubMed] [Google Scholar]
  46. Veiga C. M., Lobo J. M., and Martín-Piera F.. . 1989. Use of dung-baited pitfall traps for studying coprophagous Scarabaeoidea (Col) communities. 2. Effectiveness. Rev. Ecol. Biol. Sol. 26: 91–109. [Google Scholar]
  47. Verdú J. R., Galante E., Lumaret J.-P., and Cabrero-Sañudo F. J.. . 2004. Phylogenetic analysis of Geotrupidae (Coleoptera, Scarabaeoidea) based on larvae. Syst. Entomol. 29: 509–523. [Google Scholar]
  48. Villalba S., Lobo J. M., Martín-Piera F., and Zardoya R.. 2002. Phylogenetic relationships of Iberian dung beetles (Coleoptera: Scarabaeinae): insights on the evolution of nesting behavior. J. Mol. Evol. 55: 116–126. [DOI] [PubMed] [Google Scholar]

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