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Fig. 1 in Temporal variation of epi- and endofaunal assemblages associated with the red sponge Tedania ignis on a rocky shore (São Sebastião Channel), SE Brazil

Fig. 1. Temporal variation of sponge biomass, and density, taxon richness and Shannon diversity index of epifaunal (open symbols) and endofaunal (closed symbols) assemblages associated with Tedania ignis at Praia das Cigarras, São Sebastião, São Paulo, Brazil. Values are means ± SE.

Fig. 2 in Trophic relationships in fish assemblages of Neotropical floodplain lakes: selectivity and feeding overlap mediated by food availability

Fig. 2. Ordination by principal coordinate analysis (PCoA) of the food resource availability for six floodplain lakes along the Upper Paraná River, Paraná-Mato Grosso do Sul. AQI = aquatic insects; OAI = other aquatic invertebrates; OTI = other terrestrial invertebrates; PLA = plants; TRI = terrestrial insects.

Fig.5 in Trophic relationships in fish assemblages of Neotropical floodplain lakes: selectivity and feeding overlap mediated by food availability

Fig.5. Relationship between the mean of the proportional overlap Index (IS) and the scores of the first PCoA axis of resource availability in isolated floodplain lakes along the upper Paraná River.Values of IS closer to 1 indicates greater diet overlap. The mean IS was calculated based on individuals of 3 (ZÉ = ZÉ Marinho), 7 (Carioca = Car), 4 (TiÃo = Tia), 5 (Genipapo = Gen), 2 (CidÃo = Cid) and 5 species (Canal = Can).AQI = aquatic insects; PLA = plants.

Fig. 1 in Trophic relationships in fish assemblages of Neotropical floodplain lakes: selectivity and feeding overlap mediated by food availability

Fig. 1. Locations of the lakes on the upper Paraná River floodplain, Brazil: 1, Canal do Meio; 2, Carioca; 3, ZÉ Marinho; 4, CidÃo; 5, Genipapo; 6, TiÃo.

Fig. 4 in Trophic relationships in fish assemblages of Neotropical floodplain lakes: selectivity and feeding overlap mediated by food availability

Fig. 4. Relationship of the mean the Schoener's Index (O) between pairs of species and the scores of the first PCoA axis of resource availability in isolated floodplain lakes along the upper Paraná River. The mean O was calculated based on 10 (ZÉ = ZÉ Marinho), 28 (Carioca = Car), 6 (TiÃo = Tia), 21 (Genipapo = Gen), 3 (CidÃo = Cid) and 10 (Canal = Can) pairs of species. AQI = aquatic insects; PLA = plants.

Fig. 3 in Trophic relationships in fish assemblages of Neotropical floodplain lakes: selectivity and feeding overlap mediated by food availability

Fig. 3. Relationships between feeding selectivity by fish and the availability of food resources for six floodplain lakes along the Upper Paraná River, ParanáMato Grosso do Sul. Shape of data distribution (envelope effect) was significant.

Fig. 3 in Phyllostomidae assemblage (Chiroptera: Mammalia) in altitudinal forests at the Parque Estadual do Ibitipoca, Southeast of Minas Gerais, Brazil

Fig. 3. Species accumulation curve of phyllostomid bats captures based on sampling nights in the Parque Estadual do Ibitipoca, MG, Brazil. Dotted lines correspond to the 95% confidence interval obtained by the Mao Tau method.

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Fig 2 in Temporal variation in the spider assemblage (Arachnida, Araneae) in canopies of Callisthene fasciculata (Vochysiaceae) in the Brazilian Pantanal biome

Fig 2. Comparison of scores of the PCoA aXis generated from the distribution of nine groups in behavioral guilds of the assemblage of spiders in canopies of C. fasciculata between the different seasonal periods in the northern region of the Pantanal biome of Mato Grosso State, Brazil (z, High water; {, Receding water; …, Dry season; ", Rising water).

Fig. 2 in Phyllostomidae assemblage (Chiroptera: Mammalia) in altitudinal forests at the Parque Estadual do Ibitipoca, Southeast of Minas Gerais, Brazil

Fig. 2. Abundances of phyllostomid bat species recorded in Mata de Grota and Mata Grande in Parque Estadual do Ibitipoca, MG, Brazil.

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Figs 3, 4 in Temporal variation in the spider assemblage (Arachnida, Araneae) in canopies of Callisthene fasciculata (Vochysiaceae) in the Brazilian Pantanal biome

Figs 3, 4. Comparison between abundance (3) and richness (4) of the assemblage of spiders in canopies of C. fasciculata between the different seasonal periods in the northern region of the Pantanal biome of Mato Grosso State, Brazil.

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Fig 5 in Temporal variation in the spider assemblage (Arachnida, Araneae) in canopies of Callisthene fasciculata (Vochysiaceae) in the Brazilian Pantanal biome

Fig 5. Comparison between abundance of juveniles and adults (females and males) of spiders in canopies of C. fasciculata between the different seasonal periods in the northern region of the Pantanal biome of Mato Grosso State, Brazil (P 1, High water; P2, Receding water; P3, Dry season; P , Rising water; F, Females; M, Males; I, Immatures).

Fig. 1 in Phyllostomidae assemblage (Chiroptera: Mammalia) in altitudinal forests at the Parque Estadual do Ibitipoca, Southeast of Minas Gerais, Brazil

Fig. 1. Sampling sites in Parque Estadual do Ibitipoca, MG, Brazil: 1, Mata de Grota (Nanofloresta Nebular) and 2, Mata Grande (Floresta Nebular).

Fig. 4. Bancali Assemblage 1 in Ecomorphological and taphonomic gradients in clypeasteroid-dominated echinoid assemblages along a mixed siliciclastic-carbonate shelf from the early Miocene of northern Sardinia, Italy

Fig. 4. Bancali Assemblage 1 (A–E) and Bancali Assemblage 2 (F, G); early Miocene, Bancali, Sardinia, Italy. A. Amphiope sp. showing collapse of the central area of the test. B. Chaotically oriented test fragments of Amphiope sp. C. Encrustation by barnacles (arrow) on Amphiope sp. remains. D. Circular holes on Amphiope sp. fragment. E. Highly abraded fragment of Amphiope sp. F. Clypeaster (C. intermedius morphotype) encrusted by barnacles (arrow). G. Koehleraster sp. (MDLCA 23583).

Fig. 5 in Ecomorphological and taphonomic gradients in clypeasteroid-dominated echinoid assemblages along a mixed siliciclastic-carbonate shelf from the early Miocene of northern Sardinia, Italy

Fig. 5. Orientation data of complete tests. Early Miocene echinoids within Bancali Assemblage 1 (A), Bancali Assemblage 2 (B), and Usini Assemblage (C). N, number of counted specimens.

Fig. 3 in Ecomorphological and taphonomic gradients in clypeasteroid-dominated echinoid assemblages along a mixed siliciclastic-carbonate shelf from the early Miocene of northern Sardinia, Italy

Fig. 3. Stratigraphic sections of Bancali (A) and Usini (B) with distribution and relative abundance of recognized echinoids and associated macrofauna and flora. Abbreviations: A1, Bancali Assemblage 1; A2, Bancali Assemblage 2; A3, Usini Assemblage; c, conglomerate; cs, coarse sandstone; f, floatstone; fs, fine sandstone; gr, grainstone; ms, medium sandstone; p, packstone; r, rudstone; vfs, very fine sandstone; w, wackestone.

Fig. 9 in Ecomorphological and taphonomic gradients in clypeasteroid-dominated echinoid assemblages along a mixed siliciclastic-carbonate shelf from the early Miocene of northern Sardinia, Italy

Fig. 9. Distribution of clypeasteroid echinoids and associated echinoid taxa along a depth gradient as recognized in the Miocene sedimentary succession of northern Sardinia (based on Mancosu and Nebelsick 2013, 2015, 2017, and this paper).

Fig. 2 in Ecomorphological and taphonomic gradients in clypeasteroid-dominated echinoid assemblages along a mixed siliciclastic-carbonate shelf from the early Miocene of northern Sardinia, Italy

Fig. 2. Stratigraphy of the Miocene volcano-sedimentary succession of the Porto Torres Basin (based on Mazzei and Oggiano 1990; Martini et al. 1992; Francolini 1994; Funedda et al. 2000, 2003; Bossio et al. 2006).

Fig. 1. A in Ecomorphological and taphonomic gradients in clypeasteroid-dominated echinoid assemblages along a mixed siliciclastic-carbonate shelf from the early Miocene of northern Sardinia, Italy

Fig. 1. A. Map of the Mediterranean showing location of studied area B. Distribution of Miocene sedimentary rocks in northern Sardinia and location of echinoid assemblages cited within the text. C. Simplified geological map of the northern part of the Porto Torres Basin with the location of the clypeasteroid-echinoid assemblages of Bancali and Usini.

Fig. 6 in Ecomorphological and taphonomic gradients in clypeasteroid-dominated echinoid assemblages along a mixed siliciclastic-carbonate shelf from the early Miocene of northern Sardinia, Italy

Fig. 6. Taphonomic gradient recognized on complete tests and fragments of clypeasteroid echinoids by using the qualitative analysis of the surface characters.