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Fig. 5 in Rediscovery of the rare Star Mountains Worm-eating Snake, Toxicocalamus ernstmayri O'Shea et al., 2015 (Serpentes: Elapidae: Hydrophiinae) with the description of its coloration in life

Fig. 5. Distinguishing Toxicocalamus from Micropechis. (A, A')Holotype of T. ernstmayri (MCZ R-145946) from Wangbin, Western Province, PNG. (B, B') Holotype of T. grandis (BMNH 1946.1.18.34) from Setakwa River, Papua Province, Indonesian New Guinea. (C, C') Yellow phase of Micropechis ikaheka (BMNH 1909.4.30.12) from the FakFak Peninsula, West Papua Province, Indonesian New Guinea. Color-coding of head scalation includes six supralabials (orange), a single anterior temporal (yellow), two posterior temporals (blue), and a temporolabial (red). The individual we report here clearly has the same head scute arrangement as T. ernstmayri.

Fig. 2 in Rediscovery of the rare Star Mountains Worm-eating Snake, Toxicocalamus ernstmayri O'Shea et al., 2015 (Serpentes: Elapidae: Hydrophiinae) with the description of its coloration in life

Fig. 2. The first live individual of Toxicocalamus ernstmayri, observed and photographed in broad daylight at the Ok Tedi Mine, North Fly District, Western Province, Papua New Guinea. (A) The individual's serendipitous crossing of a 747 mm wide tire track allowed an approximation of its total length as near 850 mm. (B) The snake moves in a straight line across open ground. (C) Slower movement across a rubble pile allowed a more detailed examination of head and body scales (see Fig. 4). (D) The individual moving under the tracks of a stationary digger. Photos by Blaise Paivu.

Fig. 3 in Rediscovery of the rare Star Mountains Worm-eating Snake, Toxicocalamus ernstmayri O'Shea et al., 2015 (Serpentes: Elapidae: Hydrophiinae) with the description of its coloration in life

Fig. 3. View of an actively worked area of the Ok Tedi Mine. The observed individual of Toxicocalamus ernstmayri eventually disappeared into the vegetation on the slope in the top left of the photograph. Photo by Blaise Paivu.

Fig. 1 in Rediscovery of the rare Star Mountains Worm-eating Snake, Toxicocalamus ernstmayri O'Shea et al., 2015 (Serpentes: Elapidae: Hydrophiinae) with the description of its coloration in life

Fig. 1. Satellite map (derived from Google Earth) of the southern Star Mountains, North Fly District, Western Province, Papua New Guinea, with yellow dots on the larger map indicating two localities (Wangbin and Ok Tedi Mine), approximately 13 km apart, where Toxicocalamus ernstmayri has been recorded. The main town is Tabubil at the confluence of the Ok Tedi and Ok Mani, which flow into the Fly River. Scale = 5 km. The inset map illustrates the location of the larger map in relationship to the rest of New Guinea.

Fig. 4 in Rediscovery of the rare Star Mountains Worm-eating Snake, Toxicocalamus ernstmayri O'Shea et al., 2015 (Serpentes: Elapidae: Hydrophiinae) with the description of its coloration in life

Fig. 4. Confirming the individual's identification as Toxicocalamus ernstmayri. (A) Close-up of the snake shown in Fig. 2C with insets B, C, and D indicated. (B, B') Head and neck in extreme close-up. Color coding of head scalation includes six supralabials (orange), one anterior temporal (yellow), and two posterior temporals (blue), but no temporolabial (see Fig. 5). The head scutes appear to comply with the colubrid-elapid nine dorsal scute arrangement (i.e., two internasals, two prefrontals, one frontal, two supraoculars, and two parietals; therefore lacking any head scute fusion, although this is difficult to discern from the magnified image with accuracy. (C, C') Based on the visible dorsal scales, the dorsal scale count on the anterior body is 15. The count is achieved by locating the vertebral scale row and counting down to the lowest dorsal scale row (eight scales), doubling the count, and subtracting one scale to account for the single vertebral scale row. (D, D') The dorsal scale count at midbody, performed as described for the previous panel, is also 15.

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Figs. 7–14 in A new species of Heteraphorura Bagnall, 1948 (Collembola, Poduromorpha, Onychiuridae) from Apennine Mountains (Tuscany, Italy).

Figs. 7–14.- Heteraphorura steineri sp. nov. 7.- Chaetotaxy of central part of Abd. sternum IV, male ventral organ, remnant of furca. 8.- Chaetotaxy of central part of Abd. sternum IV, female, remnant of furca. 9.- Dorsal pso on Th. II. 10.- Dorsal pso on Abd. V. 11.- Dorsal pso on Abd. II. 12.- Maxillary palp. 13.- Distal part of leg I. 14.- Distal part of leg III. Scales¡ 0.05 mm.

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Figs. 1–6 in A new species of Heteraphorura Bagnall, 1948 (Collembola, Poduromorpha, Onychiuridae) from Apennine Mountains (Tuscany, Italy).

Figs. 1–6.- Heteraphorura steineri sp. nov. 1.- Chaetotaxy and localization of pseudocelli on dorsal side of body. 2.- Postantennal organ. 3.- Antennal III sensory organ. 4.- Labium and postlabial chaetae. 5.- Ventral chaetotaxy of abdomen, male. 6.- Ventral chaetotaxy of abdomen, female. Scales¡ 0.2 mm (1, 5, 6), 0.05 mm (2, 3, 4).

Figure 9 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 9. Schematic diagram illustrating the genesis of the dykes and their sediments in the Rösenbeck quarry. (a) Early Late Devonian: end of reef limestone sedimentation. (b) Late Devonian to Tournaisian: collapse of the carbonate platform, formation of fissures and dykes. (c) Late Tournaisian to Viséan: accumulation of carbonates on top of the reef ruin, widening of the dykes. (d) Late Viséan: begin of filling of the dykes by shales. (e) Latest Viséan to early Serpukhovian: transport of eroded sediment blocks from the top of the reef ruin into the dykes. (f) Serpukhovian to Recent: complete filling of the dykes with mud, erosion of the reef complex.

Figure 8 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 8. Chondrichthyan teeth from the Early Carboniferous dyke sediments of Rösenbeck. (a–c) Thrinacodus cf. gracia (Grogan and Lund, 2008). A, C, in lingual views, sample C; B, in lingual view, sample C. (d)?Squatinactis sp., in occlusal (D1), lingual (D2), and labial (D3) views, sample C. (e–j) Denaea cf. fournieri Pruvost, 1922, in lingual (E1, F1, G1, H2, I1, J1), occlusal (E2, F2, G2, I2, J2), and labial (E3, F3, G3, H1, I3) views, sample C. (k) Holocephali gen. et sp. indet. in lingual view, sample C. Scale bars: 0.4 mm.

Figure 7 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 7. Conodonts from the Early Carboniferous dyke sediments of Rösenbeck. (a) Gnathodus girtyi girtyi Haas, 1953, sample C. (b) Lochriea commutata (Branson and Mehl, 1941), sample C. (c) Lochriea nodosa (Bischoff, 1957), sample C. (d) Gnathodus praebilineatus Belka, 1985, sample E. (e) Gnathodus bilineatus Roundy, 1926, sample E. (f) "Gnathodus"homopunctatus (Ziegler, 1960), sample E. (g) Lochriea nodosa (Bischoff, 1957), sample F. (h) Gnathodus bilineatus Roundy, 1926, sample F. (i) Gnathodus girtyi girtyi Haas, 1953, sample F. (j) Gnathodus girtyi girtyi Haas, 1953, sample F. (k) Gnathodus bilineatus Roundy, 1926, sample H. (l) "Gnathodus"homopunctatus (Ziegler, 1960), sample H.

Figure 5 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 5. Carbonate microfacies of selected samples from the Rösenbeck quarry; all ×2. A – Middle Devonian reef limestone; B–F – Early Carboniferous dyke sediments. (a) Sample A: Stromatopora–Tabulata rudstone. Bioclast- and lithoclast-supported facies with fragments of stromatoporoids, tabulate corals (Thamnopora), and fragments of rugose corals and bivalves without preferred orientation. (b) Sample B: ammonoid packstone. Densely packed fragments of ammonoids within micritic matrix; some areas are filled with pseudosparite. Bioclast voids are filled with sparry calcite and displaying geopetal orientation. Ammonoids of various sizes from the initial stage (1 mm in diameter) up to 20 mm (but then fragmentary) are packed without preferred orientation. Numerous mollusc shell fragments (probably also mostly from ammonoids); less abundant are remains of ostracods, trilobites, and foraminifera. (c) Sample C: thin section with two successive carbonate facies. The lower part is a mollusc packstone with micritic matrix in which particularly small ammonoids up to 2 mm diameter are present; larger specimens are fragmented. Separated by a sharp boundary follows (in the upper part of the thin section) an ammonoid rudstone with densely packed ammonoids up to approximately 8 mm conch diameter. (d) Sample C: densely packed bioclastic and lithoclastic packstone with strongly fragmented mollusc shells and well-rounded clasts of phosphoritic nodules up to 10 mm length. Further biogens include ostracods, foraminifera, and conodonts. (e) Sample E: mollusc packstone with micritic matrix, which in some places is replaced by pseudosparite. Bioclast voids are filled with sparry calcite and show geopetal orientation. Most of the bioclasts are probably ammonoid shell remains; only one specimen is rather well preserved with internal whorls (Calygirtyoceras sp.). Further biogens are orthoconic cephalopods, ostracods, and trilobites. (f) Sample G: wackestone with occasionally occurring ammonoid conchs.

Figure 6 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 6. Stratigraphic column for the Viséan with the ammonoid stratigraphy and the presumed positions of the samples (timescale after Korn and Kaufmann, 2009).

Figure 4 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 4. Polished slab of sample E showing a breccia structure with various carbonate and phosphorite components; ×1.

Figure 2 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 2. Examples of neptunian dykes in the Middle Devonian limestone in the Rösenbeck quarry. (a) Funnel-shaped dyke largely filled with debris and mud. (b) Cave-like dyke filled with Early Carboniferous shales.

Figure 3 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 3. The position of the studied samples in the outcrop at the south-eastern margin of the limestone quarry. Sample A is from the top of the Middle Devonian reef limestone, and samples B to G are Early Carboniferous dyke sediments.

Figure 1 in Facies, origin, and palaeontological inventory of an Early Carboniferous neptunian dyke in the Devonian reef limestone near Rösenbeck (Brilon Anticline, Rhenish Mountains)

Figure 1. Geological map of the Brilon Syncline (after Bär, 1968) with the position of the Rösenbeck locality (marked by a star) at the eastern margin of the Brilon carbonate complex.

Figure 5 in It's a Trap! An evaluation of different passive trap types to effectively catch and control the invasive red swamp crayfish (Procambarus clarkii) in streams of the Santa Monica Mountains

Figure 5. Mean crayfish counts by size (cm) class across twelve trap types with standard error bars.

Figure 2 in It's a Trap! An evaluation of different passive trap types to effectively catch and control the invasive red swamp crayfish (Procambarus clarkii) in streams of the Santa Monica Mountains

Figure 2. Six standard, base trap types used in this study; a = Steel silver Gee Minnow trap, b = Vinyl coated black Promar Minnow trap, c = Mountain Restoration Trust custom design pyramid trap, d = Collapsible red square mesh Promar 501 trap, e = Colapsible cylindrical black mesh Promar 503 trap, and f = Mountain Restoration Trust custom PVC tube/refuge traps. Specific modifications to these traps to create the 12 types tested are provided in Table 1.

Figure 1 in It's a Trap! An evaluation of different passive trap types to effectively catch and control the invasive red swamp crayfish (Procambarus clarkii) in streams of the Santa Monica Mountains

Figure 1. Placement of traps compared in study in Las Virgenes Creek within Malibu Creek State Park. Inset shows specific study location within a regional context. Section locations were selected based on their representativeness of habitat types occurring over the entire reach (i.e. amount of riffle, runs and pools being comparable) and presence of suitable habitat for trap placement and visual observance of crayfish, tadpoles and native chub.

Figure 7 in It's a Trap! An evaluation of different passive trap types to effectively catch and control the invasive red swamp crayfish (Procambarus clarkii) in streams of the Santa Monica Mountains

Figure 7. Mean catches by stream habitat type. Differences in mean catches between stream Pools vs. Runs was evaluated using Wilcoxon rank-sum tests. * P-value <0.05.