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94 results for “Troglobionts”
FIGURE 2. A in A new genus and two new species of the millipede family Chelodesmidae from Bahia state, northeastern Brazil, including a likely troglobiont (Diplopoda, Polydesmida)
FIGURE 2. A. Limestone landscape forms and Caatinga vegetation of the São Desidério region, Bahia state. B & C. Gruta Sumidouro do João Baio entrance zone. D & E. Conduit with subterranean drainage of different water levels, a natural phenomenon that occurs in the Gruta Sumidouro do João Baio cave. Photographs by Alexandre Lobo.
FIGURE 1 in A new genus and two new species of the millipede family Chelodesmidae from Bahia state, northeastern Brazil, including a likely troglobiont (Diplopoda, Polydesmida)
FIGURE 1. Location of the Gruta da Baixa Fria and Gruta Sumidouro do João Baio caves in Bahia, Brazil. Author: L. de Assis.
FIGURE 7 in A new genus and two new species of the millipede family Chelodesmidae from Bahia state, northeastern Brazil, including a likely troglobiont (Diplopoda, Polydesmida)
FIGURE 7. Strongylosomides troglobius sp. nov., male paratype. A-D. Right gonopod with prefemoral process (labeled PfP) highlighted and outlined in red, submesal, mesal, ventral and dorsal views, respectively. Photographs by K.V. Makarov, taken not to scale.
FIGURE 6 in A new genus and two new species of the millipede family Chelodesmidae from Bahia state, northeastern Brazil, including a likely troglobiont (Diplopoda, Polydesmida)
FIGURE 6. Strongylosomides troglobius sp. nov., male paratype. A-F. Right gonopod, submesal, mesal, ventral, dorsal, sublateral and lateral views, respectively. Abbreviations: A, acropodite; AP, acropodital process; c, cannula; Cx, gonocoxa; Pf, prefemoral region; PfP, prefemoral process; Sg, seminal groove; sl, solenomere; Te, telopodite. Photographs by K.V. Makarov, taken not to scale.
FIGURE 4 in A new genus and two new species of the millipede family Chelodesmidae from Bahia state, northeastern Brazil, including a likely troglobiont (Diplopoda, Polydesmida)
FIGURE 4. Strongylosomides troglobius sp. nov., male paratype. A-C. Habitus, dorsal, lateral and ventral views, respectively. Photographs by K.V. Makarov, taken not to scale.
FIGURE 3 in A new genus and two new species of the millipede family Chelodesmidae from Bahia state, northeastern Brazil, including a likely troglobiont (Diplopoda, Polydesmida)
FIGURE 3. Strongylosomides petropolites (Attems, 1901), male lectotype. A. Left gonopodal telopodite, mesal view (after Hoffman 1979), and Strongylosomides stercoriarius (Schubart, 1956), comb. nov., male syntype. B & C. Right gonopod and its tip, mesal and sublateral views, respectively (after Schubart 1956). Abbreviations: A, acropodite; AP, acropodital process; c, cannula; Cx, gonocoxa; Pf, prefemoral region; PfP, prefemoral process; Sg, seminal groove; sl, solenomere; T, telopodite. Scale bar: 0.1 mm (B) or drawn not to scale (A, C).
FIGURE 9 in A new genus and two new species of the millipede family Chelodesmidae from Bahia state, northeastern Brazil, including a likely troglobiont (Diplopoda, Polydesmida)
FIGURE 9. Rotundotergum elevatum sp. nov., male paratype. A. Incisura lateralis (I) beneath antenna, sublateral view. B. Body ring 7 with gonopods removed to show gonopod aperture, ventral view. C & D. Body ring 7 with intact gonopods, ventral and lateral views, respectively. Abbreviation: I, Incisura lateralis. Photographs by K.V. Makarov, taken not to scale.
Figure 3 in Temperature variation and the presence of troglobionts in terrestrial shallow subterranean habitats
Figure 3. Top panel, temperature profiles at hourly intervals for the La Guancha, 70 cm MSS site (black line) and Cueva del Mulo (grey line). Centre panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the MSS site. Note the absence of a 24 hour period even at very low spectral densities. Bottom panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the cave sites. Note the weak 24 hour period.
Figure 5 in Temperature variation and the presence of troglobionts in terrestrial shallow subterranean habitats
Figure 5. Top panel, temperature profiles at hourly intervals for an MSS (dark grey line), epikarst (black line) and cave (grey line) site in the doline where the entrance of Jama v Kovačiji is located. Upper centre panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the MSS site. Note the strong 24 hour period. Lower centre panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the epikarst site. Note the weak 24 hour period. Lower panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the cave site. Note the weak 24 hour period.
Figure 2 in Temperature variation and the presence of troglobionts in terrestrial shallow subterranean habitats
Figure 2. Top panel, temperature profiles at hourly intervals for an MSS site (black line) and nearby surface site (grey line) in a laurel forest in Teno in northwest Tenerife, Canary Islands (see Figure 1). Centre panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the surface site. Note the strong period at 24 hours. Bottom panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the MSS site. Note the absence of a 24 hour period even at very low spectral densities.
Figure 1 in Temperature variation and the presence of troglobionts in terrestrial shallow subterranean habitats
Figure 1. (A) Photographs of Teno MSS site on Tenerife in old volcanic rock. Note the stabilization of the habitat by moss on the surface. Photographs were taken at a road cut. The actual site was about 2 m from the cut. (B) Photograph of La Guancha clinker MSS site on Tenerife in volcanic rock. Structure of the rocks developed at the time of deposition of the lava. (C) Photograph of MSS site at Mašun, Slovenia in flysch. Note the similarity to the MSS site shown in panel A even though the rock is different. This site also has a moss layer stabilizing the habitat. (D) Photograph of MSS site at Jama v Kovačiji. Compared to other MSS sites, this had more dirt infilling.
Figure 4 in Temperature variation and the presence of troglobionts in terrestrial shallow subterranean habitats
Figure 4. Top panel, temperature profiles at hourly intervals for an MSS site at Mašun, Slovenia (see Figure 1), at depths of 20 cm (dark grey line), 50 cm (black line) and 80 cm (grey line). Upper centre panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the upper MSS site. Note the strong 24 hour period. Lower centre panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the intermediate MSS site. Note the weak 24 hour period. Lower panel, spectral densities (y-axis) for different cycle periods (x-axis) for cycles up to 100 days for the deep MSS site. Note the absence of any 24 hour period, even at low spectral densities.
FIGURE 1 in Insular species swarm goes underground: two new troglobiont Cylindroiulus millipedes from Madeira (Diplopoda: Julidae)
FIGURE 1. Sampling localities of subterranean Cylindroiulus spp. in Madeira Island, Portugal.
FIGURE 1 in Description of three new troglobiontic species of Cybaeodes (Araneae, Liocranidae) endemic to the Iberian Peninsula
FIGURE 1. Distribution of the genus Cybaeodes in the western Mediterranean.
Fig. 1 in Ecological Relocation of the Palaeoendemic Iberotrechus bolivari (Jeannel): from Troglobiont to Epigean (Coleoptera: Carabidae: Trechini)
Fig. 1. Iberotrechus bolivari from Puerto de la Braguía.
Fig. 5 in Assessing troglomorphic and phylogenetically informative traits in troglobionts: a new cave-dwelling centipede illuminates the evolution of a soil-dwelling lineage (Chilopoda: Geophilidae)
Fig. 5 Consensus tree obtained from the maximum parsimony phylogenetic analysis of Geophilidae s.l. under equal weighting of characters. Bootstrap and jackknife frequencies are indicated above nodes, in this order, when> 50%. Synapomorphies are indicated below nodes (see "Material and methods" for the character codes)
Fig. 3 Plutogeophilus jurupariquibaba gen.n in Assessing troglomorphic and phylogenetically informative traits in troglobionts: a new cave-dwelling centipede illuminates the evolution of a soil-dwelling lineage (Chilopoda: Geophilidae)
Fig. 3 Plutogeophilus jurupariquibaba gen.n. sp.n.: a anterior part of body, dorsal view; b–c head and forcipular segment, dorsal and ventral views, respectively; d–e posterior part of body, dorsal and ventral views, respectively. Photos: ♂, ISLA 11879, holotype. Scale bars: 0.4 µm
Figure 3 from: Reboleira ASPS, Enghoff H (2018) First continental troglobiont Cylindroiulus millipede (Diplopoda, Julida, Julidae). ZooKeys 795: 93-103. https://doi.org/10.3897/zookeys.795.27619
Figure 3 Cylindroiulusvillumi sp. n. female paratype, SEM. A midbody leg B detail of the claw C posterior view of the anal valves D lateral view of the telson. Scale bars: 10 μm (A, B); 100 μm (C, D).
Figure 2 from: Reboleira ASPS, Enghoff H (2018) First continental troglobiont Cylindroiulus millipede (Diplopoda, Julida, Julidae). ZooKeys 795: 93-103. https://doi.org/10.3897/zookeys.795.27619
Figure 2 Cylindroiulusvillumi sp. n. female paratype, SEM. A anterior view of the head B lateral view of the head C tip of the antenna D detail of a sensory cone of the antenna E tip of the sensory cone. Scale bars: 100 μm (A, B); 10 μm (C); 1 μm (D, E).
Figure 5 from: Reboleira ASPS, Enghoff H (2018) First continental troglobiont Cylindroiulus millipede (Diplopoda, Julida, Julidae). ZooKeys 795: 93-103. https://doi.org/10.3897/zookeys.795.27619
Figure 5 Cylindroiulusvillumi sp. n. vulva, lateral view. Abbreviations: bu: bursa, op: operculum, rs: receptaculum seminis. Scale bar: 100 μm.
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