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opencc-by-4.0Dec 2015View details →

Fig. 3 in A new species of montane gymnophthalmid lizard, genus Cercosaura (Squamata: Gymnophthalmidae), from the Amazon slope of northern Peru

Fig. 3. Holotype of Cercosaura doanae sp. nov. in life: dorsolateral (upper) and ventral (bottom) views. Photographs by P.J. Venegas.

opencc-by-4.0Dec 2015View details →

Fig. 2 in A new species of montane gymnophthalmid lizard, genus Cercosaura (Squamata: Gymnophthalmidae), from the Amazon slope of northern Peru

Fig. 2. Head of the holotype (CORBIDI 00651) of Cercosaura doanae sp. nov. in lateral (A), dorsal (B), and ventral (C) views. Photographs by G. Chávez.

Fig. 8 in A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska

Fig. 8. Comparison of line−drawing reconstructions of skulls of Pachyrhinosaurus perotorum (A), Pachyrhinosaurus canadensis (B), and Pachyrhinosaurus lakustai (C) in left lateral and dorsal views. A. Based on DMNH 21200 and DMNH 22558. B. Based upon NMC 9485, NMC 9602 as shown in Langston (1975), and from Sampson and Loewen (2010). C. Derived from Currie et al. (2008). Gray fill indicates hypothetical morphology not preserved in currently known specimens of P. perotorum. Drawings not to scale.

Fig. 4 in A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska

Fig. 4. Centrosaurine ceratopsid Pachyrhinosaurus perotorum sp. nov., holotype (DMNH 21200); parietal in dorsal (A), ventral (B), and right lateral (C) views. D. Reconstruction of the posterior parietal frill based upon DMNH 21200 and a yet to be catalogued partial parietal with a P3 horn. Scale bars 10 cm.

Fig. 3 in A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska

Fig. 3. Labelled line drawings of Pachyrhinosaurus perotorum paratype (DMNH 22558) skull in left lateral (A), right lateral (B), dorsal (C), ventral (D), and anterior (E) views. Scale bars 10 cm.

Fig. 7 in A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska

Fig. 7. Results of phylogenetic analysis. One of three equally most parsimonious trees (length = 107, C.I. (consistency index) = 0.8131, R.I. (retention index) = 0.8291) from our analysis set upon the Late Cretaceous timescale. Ranges of ceratopsian taxa other than Pachyrhinosaurus perotorum from Sampson and Loewren (2010). Timescale dates derived from Walker and Geissman (2009). Solid thick bars indicate well constrained range of a taxon. Open thick bars indicate poorly constrained or estimated range of a taxon. Open circles at nodes indicate named node−defined clades. Arcs on branches indicate stem−defined lineage names. Divergence points on tree are arbitrarily drawn, and are not based on calculations of lineage divergence dates. Abbreviations: Cen., Cenomanian; Con., Coniacian; Dan., Danian; Pal., Paleocene; Sa., Santonian; Tur., Turonian.

Fig. 2 in A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska

Fig. 2. Centrosaurine ceratopsid Pachyrhinosaurus perotorum sp. nov., paratype (DMNH 22558); skull in left lateral (A), right lateral (B), dorsal (C), ventral (D), and anterior (E) views. Scale bars 10 cm.

Fig. 6 in A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska

Fig. 6. Results of phylogenetic analysis. Strict consensus of the three equally most parsimonious trees generated by our analysis (length = 107, C.I. (consistency index) = 0.8131, R.I. (retention index) = 0.8291). Numbers at nodes are Bremer support values / Bootstrap percentages recovered from 1000 replicates.

Fig. 5 in A new Maastrichtian species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope of Alaska

Fig. 5. Centrosaurine ceratopsid Pachyrhinosaurus perotorum sp. nov., paratype (DMNH 21201); partial parietal preserving portion of right transverse parietal bar and anterior rim horn in dorsal (A), ventral (B), and right lateral (C) views. Scale bars 5 cm.

opencc-by-4.0Dec 2019View details →

Рис. 1. Распространение виΑов Dorcadion (s. str.) Dalman, 1817 в Восточном Казахстане. 1 – южные преΑгорья хр. Тарбагатай, типовое местонахожΑение D. urdzharicum; 2 – северные преΑгорья и скΛоны Тарбагатая и Саура, местонахожΑение D. songaricum; 3 – степи северо-запаΑнее оз. СасыккоΛь, местонахожΑение D. cephalotes; 4 – преΑгорья у югозапаΑного берега оз. АΛакоΛь, типовое местонахожΑение D. alakoliense; 5 – 47 км юго-восточнее Маканчи, типовое местонахожΑение D. natali sp. n. Fig. 1. Localities of species of Dorcadion (s. str.) Dalman, 1817 in East Kazakhstan. 1 – southern foothills of the Tarbagatai Ridge, type locality of D. urdzharicum; 2 – northern foothills and slopes of the Tarbagatai and Saur, locality of D. songaricum; 3 – steppes NW of Sasykkol Lake, locality of D. cephalotes; 4 – foothills at the SW shore of Alakol Lake, type locality of D. alakoliense; 5 – 47 km SE Makanchi, type locality of D. natali sp. n. in A new species of Dorcadion Dalman, 1817 (Coleoptera: Cerambycidae) from East Kazakhstan

Рис. 1. Распространение виΑов Dorcadion (s. str.) Dalman, 1817 в Восточном Казахстане. 1 – южные преΑгорья хр. Тарбагатай, типовое местонахожΑение D. urdzharicum; 2 – северные преΑгорья и скΛоны Тарбагатая и Саура, местонахожΑение D. songaricum; 3 – степи северо-запаΑнее оз. СасыккоΛь, местонахожΑение D. cephalotes; 4 – преΑгорья у югозапаΑного берега оз. АΛакоΛь, типовое местонахожΑение D. alakoliense; 5 – 47 км юго-восточнее Маканчи, типовое местонахожΑение D. natali sp. n. Fig. 1. Localities of species of Dorcadion (s. str.) Dalman, 1817 in East Kazakhstan. 1 – southern foothills of the Tarbagatai Ridge, type locality of D. urdzharicum; 2 – northern foothills and slopes of the Tarbagatai and Saur, locality of D. songaricum; 3 – steppes NW of Sasykkol Lake, locality of D. cephalotes; 4 – foothills at the SW shore of Alakol Lake, type locality of D. alakoliense; 5 – 47 km SE Makanchi, type locality of D. natali sp. n.

FIGURE 1 in Variation in patterns of fish assemblage and their environmental correlates in a tropical river basin from the Gulf of Mexico slope

FIGURE 1 | Study area and sampling sites in the Usumacinta River basin (shaded area in figure box), Mexico. Site number and names of the main rivers in the region are enclosed in boxes (see Tab. 1 for names of watercourses). Black arrow indicates flow direction.

FIGURE 2 in Variation in patterns of fish assemblage and their environmental correlates in a tropical river basin from the Gulf of Mexico slope

FIGURE 2 | Relative contribution of common species to total fish abundance by seasons (left panel) and years (right panel). Species shown had a contribution above the 50% quantile for abundance. Refer to Tab. 1 for species acronyms.

FIGURE 5 in Variation in patterns of fish assemblage and their environmental correlates in a tropical river basin from the Gulf of Mexico slope

FIGURE 5 | Plots for the redundancy analysis of fish communities and environmental data, displaying weighted averages of species scores (A), fitted site scores (B), and species scores of significant species (C). Centroids of factor "ORD" are indicated by a "×". Convex hulls (A, C) and point shape (A, B) show cluster affiliation. DO, dissolved oxygen; DU, distance to the confluence with the Usumacinta River; FC, forest cover; ORD, stream order; TC, water temperature.

FIGURE 4 in Variation in patterns of fish assemblage and their environmental correlates in a tropical river basin from the Gulf of Mexico slope

FIGURE 4 | Multivariate regression tree of transformed species abundances and environmental data. Percentage of improvement in the model is shown under each node; discriminating environmental variables and threshold values are shown at each split. DO, dissolved oxygen; ORD, stream order; n, number of samples.

FIGURE 3 in Variation in patterns of fish assemblage and their environmental correlates in a tropical river basin from the Gulf of Mexico slope

FIGURE 3 | Principal component analysis plot of environmental data. DO, dissolved oxygen; DU, distance to the confluence with the Usumacinta River; EC, electric conductivity; FC, forest cover; ORD, stream order.

opencc-by-4.0Sep 2024View details →

Complementary data for Iqbal et al. (2024): Slopes along Apollo EVAs: Astronaut experience as input for future mission planning

Complementary data for Iqbal et al. (2024): Slopes along Apollo EVAs: Astronaut experience as input for future mission planning Data contains shapefiles that can be used in any geoinformation system (GIS). If you use these data, please cite BOTH the JOURNAL NAME publication and the Zenodo dataset. Iqbal, W., Head III, J. W., van der Bogert, C. H., Frueh, T., Henriksen, M., Bickel, V., Kring, D., Hiesinger, H., Scott, D. R., & Heyer, T. (2024). Slopes along Apollo EVAs: Astronaut experience as input for future mission planning. Acta Astronautica, 223, 184-196. <a title="Persistent link using digital object identifier" href="https://doi.org/10.1016/j.actaastro.2024.07.006" target="_blank" rel="noreferrer noopener">https://doi.org/10.1016/j.actaastro.2024.07.006</a> Iqbal, W., Head, J. W., van der Bogert, C., Frueh, T., Henriksen, M., Bickel, V., Kring, D., Hiesinger, H., Scott, D. R., & Heyer, T. (2024). Complementary data for Iqbal et al. (2024): Slopes along Apollo EVAs: Astronaut experience as input for future mission planning [Data set]. In Acta Astronautica (Bd. 223, S. 184–196). Zenodo. <a href="https://doi.org/10.5281/zenodo.13790204" target="_blank" rel="noopener">https://doi.org/10.5281/zenodo.13790204</a> -------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------- Structure -> File "Apollo_Traverses_Iqbal_24" - It includes six subfolders for each landing site that contain the shapefiles of traverses. -------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------- For further questions contact <a href="mailto:lwueller@uni-muenster.de" rel="noopener noreferrer nofollow">iqbalw@uni-muenster.de</a> Wajiha Iqbal, Institut für Planetologie, Universität Münster, Germany.

opencc-by-4.0Sep 2024View details →

Files for the numerical results shown in "Far-from-equilibrium travelling pulses in sloped semi-arid environments driven by autotoxicity effects" by Gabriele Grifò, Annalisa Iuorio, and Frits Veerman

This folder contains the code used to produce Fig. 1 and Fig. 8-10 in the paper: "Far-from-equilibrium travelling pulses in sloped semi-arid environments driven by autotoxicity effects" by Gabriele Grifò, Annalisa Iuorio, and Frits Veerman. The preprint version of this paper is available at <a href="https://arxiv.org/abs/2405.1560">https://arxiv.org/abs/2405.1560</a>. In the subfolder "Direct_simulations", the code (to obtain Fig. 1) is based on a MATLAB routine which uses finite differences for spatial discretization with periodic boundary conditions together with MATLAB’s ode15s routine for time integration. The continuation procedure (to obtain Fig. 8-10) is shown in the subfolder "Continuation" based on the software AUTO to analyse the dependence of the constructed travelling pulse solutions of Eq. (3.2) with respect to three system parameters, i.e. A, D, and H. Correspondingly, in each folder 'Continuation_X' where X=A, D, H, the results can be obtained by running the file 'AUTO_script_cont_X', based on the two files 'parab_X.f90' and 'c.parab_X'. Selected solutions for each continuation are stored in the corresponding subfolders 'solutions_X', whereas the tables resulting from the continuation procedure in the scripts are shown in the files 'bifdiag_X.dat'. In each script file further details are provided in order to clarify how to extract the solutions used for the plots.

opencc-zeroJan 2024View details →

Linked collectors and determiners for: A new species of Hyloscirtus (Anura, Hylidae) from the Colombian and Venezuelan slopes of Sierra de Perijá, and the phylogenetic position of Hyloscirtus jahni (Rivero, 1961).

Natural history specimen data linked to collectors and determiners held within, "A new species of Hyloscirtus (Anura, Hylidae) from the Colombian and Venezuelan slopes of Sierra de Perijá, and the phylogenetic position of Hyloscirtus jahni (Rivero, 1961)". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/266ff2b3-8358-436f-ad80-e07c70f2203f">https://bionomia.net/dataset/266ff2b3-8358-436f-ad80-e07c70f2203f</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/266ff2b3-8358-436f-ad80-e07c70f2203f">https://gbif.org/dataset/266ff2b3-8358-436f-ad80-e07c70f2203f</a>. Formatted as a Frictionless Data package.

opencc-zeroOct 2024View details →

Linked collectors and determiners for: Amalophyllon miraculum (Gesneriaceae), an exceptionally small lithophilous new species from the western Andean slopes of Ecuador.

Natural history specimen data linked to collectors and determiners held within, "Amalophyllon miraculum (Gesneriaceae), an exceptionally small lithophilous new species from the western Andean slopes of Ecuador". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/fdfff9a9-0826-442b-90b3-2f82699c9bbf">https://bionomia.net/dataset/fdfff9a9-0826-442b-90b3-2f82699c9bbf</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/fdfff9a9-0826-442b-90b3-2f82699c9bbf">https://gbif.org/dataset/fdfff9a9-0826-442b-90b3-2f82699c9bbf</a>. Formatted as a Frictionless Data package.