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Temporal coexistence of dung-dweller and soil-digger dung beetles (Coleoptera, Scarabaeoidea) in contrasting Mediterranean habitats

Published online by Cambridge University Press:  07 February 2008

P. Jay-Robert*
Affiliation:
UMR 5175 Centre d'Écologie Fonctionnelle et Évolutive – Laboratoire de Zoogéographie, Université Montpellier IIIroute de Mende, F-34199 Montpellier cedex 5, France
F. Errouissi
Affiliation:
Institut Supérieur des Sciences Biologiques Appliquées de Tunis (ISSBAT), 9 avenue Zohaïr Essefi, TN-1007 Tunis, Tunisie
J.P. Lumaret
Affiliation:
UMR 5175 Centre d'Écologie Fonctionnelle et Évolutive – Laboratoire de Zoogéographie, Université Montpellier IIIroute de Mende, F-34199 Montpellier cedex 5, France
*
*Author for correspondence Fax: +33 467 142 459 E-mail: pierre.jay-robert@univ-montp3.fr
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Abstract

The western part of the Mediterranean basin is a transitional biogeographical region for the distribution of the representatives of the main guilds of dung beetles; towards the south, Aphodiinae (dung-dwellers) become scarce, whereas northwards Scarabaeinae (soil-diggers) progressively disappear. The number of species in local dung beetle assemblages is enhanced by this double faunistic contribution. Annual dung beetle assemblages were sampled in two sub-Mediterranean sites, which differed by 600 m in elevation, in order to determine the phenological dynamics related to the way of using dung (dung-dwellers/Aphodiinae vs. soil-diggers/Scarabaeinae and Geotrupinae). Aphodiids were active all year round, although they were affected by summer drought and, at high elevation, by the length of the cold season. This reduced activity was related to an impoverishment of Aphodiinae and to reduced temporal segregation between species. In contrast, soil-diggers were not active all year round and showed different species assemblages in the two sites. An extension of the activity period of these beetles was observed due to the occurrence of cold resistant species at high elevation. Our results suggested that the occurrence of soil-diggers seemingly did not affect the seasonality of dung-dwellers; their local abundance showed no negative correlation and, most importantly, phenological differences between dung-dwellers were always significantly higher than the seasonal differences between dwellers and diggers.

Information

Type
Research Paper
Copyright
Copyright © 2008 Cambridge University Press
Figure 0

Fig. 1. Monthly temperatures and precipitations at the two sampled sites. LES, low elevation site (Garrigue); MES, medium elevation site (Causse); Rs, Spearman rank correlation between LES and MES data sets (–●–, LES (14.2°C mean); –○–, MES (10.7°C mean); ■, LES (1396.8 mm cumul.); □, MES (1098.3 mm cumul).

Figure 1

Table 1. Monthly variation of dung beetle assemblages at the Low Elevation Site (January 2000 to June 2001 period); mean value per trap.

Figure 2

Table 2. Monthly variation of dung beetle assemblages at the Medium Elevation Site (April 2000 to June 2001 period); mean value per trap.

Figure 3

Fig. 2. Distribution of species abundance in ecological groups designed with the Preston method (Preston, 1948, 1962; Lobo & Favila, 1999) in low elevation (Garrigue) and medium elevation sites (Causse) (, Scarabaeinae rollers;, Scarabaeinae tunnellers; □, Geotrupinae tunnellers; ■, Aphodiinae dwellers).

Figure 4

Table 3. Distribution of rare (<64 specimens) and abundant (>64 specimens) species according to ecological groups at both sites (64 is the inter-class limit, see fig. 2, approximating one specimen per trap).

Figure 5

Fig. 3. Plot of species sampled at LES on axes 1–2 of correspondence analysis. For each ecological group (Aphodiinae dwellers (AD), Scarabaeinae tunnellers (ST), Scarabaeinae rollers (SR) and Geotrupinae tunnellers (GT)) the barycentre and the standard deviation along axes are represented by an ellipse (the barycentre is the centre of the ellipse, the standard deviation for axis 1 is the axis of the ellipse that is parallel to axis 1, the SD for axis 2 is the axis of the ellipse parallel to axis 2). See table 1 for species name abbreviations (◊, Aphodiinae dwellers (AD); △, Scarabaeinae tunnellers (ST); +, Scarabaeinae rollers (SR); ×, Geotrupinae tunnellers (GT); ●, Month/Year).

Figure 6

Fig. 4. Plot of species sampled at MES on axes 1–2 of correspondence analysis. For each ecological group (Aphodiinae dwellers (AD), Scarabaeinae tunnellers (ST), Scarabaeinae rollers (SR), Geotrupinae tunnellers (GT)) the barycentre and the standard deviation along axes are represented by an ellipse (the barycentre is the centre of the ellipse, the standard deviation for axis 1 is the axis of the ellipse that is parallel to axis 1, the SD for axis 2 is the axis of the ellipse parallel to axis 2). See table 2 for species name abbreviations (◊, Aphodiinae dwellers (AD); △, Scarabaeinae tunnellers (ST); +, Scarabaeinae rollers (SR); ×, Geotrupinae tunnellers (GT); ●, Month/Year).

Figure 7

Fig. 5. Correlation between standard errors (SE) along axis 1 calculated at LES and MES for species sampled in both sites. Rs, Spearman rank correlation between LES and MES data sets (◊, Aphodiinae dwellers; △, Scarabaeinae tunnellers; +, Scarabaeinae rollers; ×, Geotrupinae tunnellers).

Figure 8

Table 4. Position and scattering of the four ecological groups: Aphodiinae dwellers (AD), Scarabaeinae tunnellers (ST), Scarabaeinae rollers (SR) and Geotrupinae tunnellers (GT) in the plane (1–2) of CA for sampled sites LES and MES (details in the text).

Figure 9

Table 5. Distance between species in the plane (1–2) of CA.