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Granite inselbergs protrude from forest and savanna in the tropics. They are exposed to harsh climates (alternation of heavy rain and severe drought) and provide little nutrient for plants. Soil animals and humus components were investigated in cyanobacterial crusts close to patches of epilithic vegetation on the surface of the Nouragues inselberg (French Guiana). Three biological crust samples, corresponding to bromeliacean carpets of increasing size (supposed of increasing age), were sampled for faunal and micromorphological studies. Arthropods (mainly mites and insects) were abundant and highly diversified, the more so after enchytraeid worms ate and transformed the cyanobacterial mass. Below the superficial cyanobacterial crust, humus was made of a loose assemblage of enchytraeid faeces where these animals were present, or of a compact assemblage of cyanobacteria and amorphous organic matter where mites were the dominant animal group. Roots abounded in the humified part of the crust. We conclude that soil invertebrates, in particular enchytraeid worms, are important for the accumulation of organic matter on granite outcrops, and so therefore for the encroachment of plant succession.

International audience; The combined effects of isolation within an unfavourable matrix and vegetation development were studied in patches of scrub vegetation on a tropical inselberg (Nouragues, French Guiana). Three thickets similar to 10m2 area were sampled, located at similar to 30 m distance from each other, in which the same vegetation types were present at less than 3 m distance: canopies of Clusia minor (Clusiaceae) and Myrcia saxatilis (Myrticeae), two stages of thicket development, and zones of destruction by fire. The shallow organic soil was sampled over similar to 2 dm2 and down to 10 cm. The matrix was comprised of granite without any soil development. Arthropods were classified into morphospecies and their food diets were characterized by optical methods. The effect of isolation (between-thicket variation) on morphospecies composition was negligible, while that of vegetation type and fire (within-thicket variation) was prominent, as ascertained by principal component analysis and tested by partial redundance analysis. The importance of keystone structures (stages of vegetation development) was stressed, and interpreted to the light of taxonomic and foodweb knowledge.

International audience; A number of plant communities have been described on tropical inselbergs, known as hot spots of plant and animal biodiversity. However, few studies tried to question what drives seral processes in these harsh environments, submitted to natural hazards (violent storms, intense runoff and lightning strikes) which may destroy the vegetation cover and its accumulated organic matter. We analysed quantitative data from the granitic Nouragues inselberg (French Guiana) in order to discern how successional processes featured their variety. We showed that the transition from herbaceous carpets (bromeliaceous mats and grassy meadows) to woody vegetation (shrub thickets) was not conditioned by slope, but was truly successional. We also showed that there was a cycle of change in shrub thickets, reinitiated by the destruction of scrub vegetation by fire (lightnings), wood-destroying fungi and termites.

International audience; The aim of our study was to describe succession related changes in humus profiles on moderate slopes of a tropical inselberg (Nouragues, French Guiana). Nine humus profiles were collected in a stratified manner under two main communities on well-drained sites: carpets of Pitcairnia geyskesii (Bromeliaceae) and shrub thickets of Clusia minor (Clusiaceae), the latter including two stages of its dynamic development. The 53 sampled layers were analysed by an optical method, the volume ratio of 109 classes of litter/humus components being quantified by a count point method. Correspondence analysis (CA) revealed marked differences among humus forms. Pitcairnia carpets were characterized by the dominance of cyanobacteria which formed crusts with low faunal activity, except when they were colonized by enchytraeid worms. With advancing succession, we observed that leaf litter did not accumulate but rather was incorporated into organo-mineral excrements of macro-invertebrates under C minor. The late developmental stage of Clusia thickets, characterised by the establishment of Myrcia saxatilis (Myrtaceae), showed a thick layer of undecayed litter and near absence of organo-mineral aggregates. The humus form varied from mor in cyano-bacterial crusts to tropical moder (with a few mull features) in Clusia thickets, but comparisons among humus profiles revealed more complex successional processes than expected on the basis of the composition of plant and soil animal communities.

International audience; Tropical inselbergs are isolated rock outcrops with a special type of vegetation surrounded by rain forest. They are exposed to a harsh climate (alternation of heavy rain and severe drought) and provide few nutrients for plant growth. The aim of our study was to investigate a possible correlation between primary plant succession, size and diversity of soil arthropods. The study site was the Nouragues inselberg, in French Guiana (South America). Nine soil samples (three samples in each vegetation type) were taken for the study of soil arthropod communities and their food habits in three habitat types: Pitcairnia geyskesii (Bromeliaceae), Clusia minor (Clusiaceae) and Myrcia saxatilis (Myrtaceae), which represent three stages in a primary plant succession on this inselberg. Soil arthropods were classified into morphospecies under the dissecting microscope and their food habits were characterized by examining their gut contents under the light microscope. A variation in food habits was observed, cyanobacteria being found in arthropod guts only during the Pitcairnia stage, and were replaced by plant material at the Myrcia stage. Carnivory was prominent in oribatid mites, contrary to temperate records. All our samples contained large numbers of microarthropods, principally mites and collembolans. At the Myrcia stage arthropod density was significantly higher than at the two other stages. Macroinvertebrates are present only at late and intermediate successional stages. The number of macropredators increased by a factor of 10 in species richness and 100 in abundance along the succession. These results suggest that abundance and diversity of soil arthropods increased throughout the plant succession and show the importance of organic matter as a factor which can explain the observed phenomenon.