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Fig. 1 in Non-invasive detection of Orthohalarachne attenuata (Banks, 1910) and Orthohalarachne diminuata (Doetschman, 1944) (Acari: Halarachnidae) in free-ranging synanthropic South American sea lions Otaria flavescens (Shaw, 1800)

Fig. 1. Sampling area of Orthohalarachne spp. of South American sea lions in Valdivia, Chile. The exact sampling location is shown in the section (upper-left) as a red-framed black star. Map created with QGIS (https://qgis.org/en/site/) and map data used from OpenStreetMap (openstreetmap.org/copyright). (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)

Fig. 5 in Non-invasive detection of Orthohalarachne attenuata (Banks, 1910) and Orthohalarachne diminuata (Doetschman, 1944) (Acari: Halarachnidae) in free-ranging synanthropic South American sea lions Otaria flavescens (Shaw, 1800)

Fig. 5. Haplotype (TCS) networks of Orthohalarachne diminuata and Orthohalarachne attenuata based on 16S rDNA sequences. (A) Network analysis based on countries of origin, (B) network analysis based on the pinniped host species (CSL=California sea lion, GFS = Guadalupe fur seal, NFS=Northern fur seal, SAS=South American sea lion). For better visualization a combined network analysis of Or. attenuata and Or. diminuata sequences is shown, however, the calculated distance (48 mutations) between species was clipped. Or. attenuata haplotypes are encircled in black boxes with dashed lines, whereas Or. diminuata haplotypes are encircled in light grey boxes with dashed lines based on estimated MOTUs by ABGD.

Fig. 2 in Non-invasive detection of Orthohalarachne attenuata (Banks, 1910) and Orthohalarachne diminuata (Doetschman, 1944) (Acari: Halarachnidae) in free-ranging synanthropic South American sea lions Otaria flavescens (Shaw, 1800)

Fig. 2. Nasal discharge in three individuals (A, B, C) of the "urban" colony of South American sea lions Otaria flavescens in Valdivia, Chile.

Fig. 4 in Non-invasive detection of Orthohalarachne attenuata (Banks, 1910) and Orthohalarachne diminuata (Doetschman, 1944) (Acari: Halarachnidae) in free-ranging synanthropic South American sea lions Otaria flavescens (Shaw, 1800)

Fig. 4. Larval stages of (A) Orthohalarachne attenuata and (B) Orthohalarachne diminuata showing distinct differences in idiosoma length.

opencc-by-4.0Nov 2022View details →

F I G U R E 4 in A low-density single nucleotide polymorphism panel for brown trout (Salmo trutta L.) suitable for exploring genetic diversity at a range of spatial scales

F I G U R E 4 Correlation between geographic distance (km) against genetic distance (linear FST) for the trout samples from the River Camel. The red points represent those between the De Lank and all other sites, the black points for all pair-wise comparisons excluding the De Lank. Linear regression for all sites including the De Lank is given by the red line (r2 = 0.321, P = 0.231), and linear regression for all pair-wise sites excluding the De Lank is given by the black line (r2 = 0.658, P = 0.0671)

Fig. 4 in The oldest post-Paleozoic (Ladinian, Triassic) brachiopods from the Betic Range, SE Spain

Fig. 4. Internal structure of zeillerid brachiopod Misunithyris goyi gen. et sp. nov. (BQ-AH2.2) from the lower Ladinian of the South-Iberian Triassic platform, the Arroyo Hurtado section. A. Transverse serial sections through the specimen (distance from the beak in mm). B. Microphotographs of acetate peels showing the hinge plates-crural bases relationship: crural bases are located in the ventral part of the hinge plates but a dorsal thickening emerges towards an early dorsal development. Section at 4.10 mm (B1) and 4.30 mm (B2) from the apex. Abbreviations: cb, crural bases; dp, deltidial plates; ld, dental lamellae; ms, median septum; pc, cardinal process; sp, septalium.

Fig. 6 in The oldest post-Paleozoic (Ladinian, Triassic) brachiopods from the Betic Range, SE Spain

Fig. 6. Paleogeographical map of the Ladinian times (modified after Pérez-López and Pérez-Valera 2007), showing the distribution of taxa highly related to, or common with the brachiopod fauna inhabiting the Middle Triassic peri-Iberian platforms system. Color of arrows and taxa symbolizes the inferred paleobiogeographical affinities. ACP, Apennine Carbonate Platform; AM, Armorican Massif; BM: Bohemian Massif; CM, Central Massif; EM, Ebro Massif; MM, Meso-Mediterranean Massif; Mi, Misunithyris; Me, Menathyris; Mz, Mentzelia; Co, Coenothyris. Occurrences mainly based on Schmidt (1935), Siblík (1972, 1988, 2001), Popiel-Barczyk and Senkowiczowa (1989), Dagys (1993), Török (1993), Kaim (1997), Torti and Angiolini (1997), Pálfy (2003), Feldman (2005, 2013), Ruban (2010), Escudero-Mozo et al. (2015), among others (see text for details). Dotted line shows palaeogeographic position of the currently emerged land.

Fig. 3 in The oldest post-Paleozoic (Ladinian, Triassic) brachiopods from the Betic Range, SE Spain

Fig. 3. Intraspecific variability of zeillerid brachiopod Misunithyris goyi gen. et sp. nov. of the lower Ladinian from the South-Iberian Triassic platform, the Arroyo Hurtado (A, B), Calasparra (C, E), Talave (D, F) sections; in dorsal (A1–F1), anterior (A2–F2), and lateral (A3–F3) views. A. BQ-AH2.1. B. BQ-AH2.2, sectioned in the present work. C. BQ-CL1.1. D. BQ-TA1.1. E. BQ-CL1.2. F. BQ-TA1.2, holotype. All specimens were coated with magnesium oxide.

Fig. 5 in The oldest post-Paleozoic (Ladinian, Triassic) brachiopods from the Betic Range, SE Spain

Fig. 5. Microphotographs of acetate peels from zeillerid brachiopod Misunithyris goyi gen. et sp. nov. (BQ-AH2.2) from the lower Ladinian of the South-Iberian Triassic platform, the Arroyo Hurtado section. A. Section at 1.00 mm from the apex showing dental lamellae enveloped in a thick-shelled wall. B. Section at 2.60 mm from the apex showing the disposition of deltidial plates. C, D. Sections at 3.30 and 3.50 mm from the apex, respectively, showing the first stages of hinge plates and earlier cardinalia and the evolution of the cardinal process, clearly striated and raised by a high cardinal platform. E, F. Sections at 4.10 and 4.30 mm from the apex, respectively, showing the cardinal area with the position of crural bases and the articulation system. G–I. Partial sections at 4.90, 5.70, and 7.10 mm from the apex, respectively, showing the evolution of the crural architecture and dorsal median septum development.

Fig. 1 in The oldest post-Paleozoic (Ladinian, Triassic) brachiopods from the Betic Range, SE Spain

Fig. 1. Geographical and geological setting of the localities studied yielding Ladinian brachiopods in the Betic Range context emphasizing the South-Iberian Triassic outcrops. AH, Arroyo Hurtado section; CL, Calasparra section; TA, Talave section.

opencc-by-4.0Apr 2017View details →

Geographic range maps for Mammal Diversity Database v1.3 taxonomy

Update of mammal maps based on the taxonomy of the Mammal diversity database. These maps are different from the original, have been downscaled and are distributed under the R package mdd (github.com/alrobles/mdd).

opencc-by-4.0Nov 2024View details →

Seasonal orographic effect of North American Mountain Range at different levels and its remote control on tropical climate

<a name="OLE_LINK36"></a><a name="OLE_LINK37"></a><a name="OLE_LINK81"></a><a name="OLE_LINK6"></a>Orography significantly influences global climate patterns. <a name="OLE_LINK32"></a><a name="OLE_LINK33"></a>Previous studies show the North American Mountain Range (NAMR) impacts regional climates seasonally but have not thoroughly illustrated the seasonally different atmospheric responses in the lower and upper troposphere, respectively. Using the Community Earth System Model version 1.2 with a slab ocean configuration, we investigate the NAMR’s seasonal impacts by simulating scenarios with and without the mountain range. Our findings reveal that the NAMR induces contrasting responses in sea surface temperature (SST) and precipitation off California in different seasons, indicating different underlying mechanisms. Through analysis of large-scale circulation and local energy budgets, we find that in summer, the NAMR reinforces the North Pacific High causing SST cooling and drying off California. This cooling propagates to the equatorial Pacific via anomalous northeasterlies, influencing the Intertropical Convergence Zone and initiating a climatic signal through the Pacific Meridional Mode, which crosses the equator and affects Southern Hemisphere temperatures. In winter, the NAMR reduces wind speed and evaporation, leading to SST warming off California, amplified by SST-cloud feedback. In the upper troposphere, we observe seasonal shifts in jet stream patterns: during winter, a weakened, equatorward-shifted jet over the Pacific and a strengthened, poleward-shifted branch over the Atlantic; in summer, the jet stream intensifies over and downstream of the mountains while weakening upstream. Our research highlights distinct seasonal mechanisms by which the NAMR influence climate patterns, linking mid-latitude climate variations to equatorial, cross-hemispheric and global changes.

opencc-by-4.0Nov 2024View details →

Raw data to "Quantum-critical and dynamical properties of the XXZ bilayer with long-range interactions"

<div> This directory contains the data used to generate the numerical results in the work "Quantum-critical and dynamical properties of the XXZ bilayer with long-range interactions [1]". To get an overview of the organization of the directory and a description of the data we recommend the README.md file. [1]: P. Adelhardt, A. Duft and K. P. Schmidt, Quantum-critical and dynamical properties of the XXZ bilayer with long-range interactions, <a href="https://arxiv.org/abs/2408.13145">arXiv:2408.13145</a>     </div>

openapache2.0Sep 2024View details →

Computational generation of long-range axonal morphologies

This repository contains both the data and scripts to reproduce all figures of the related article. Usually, one should download all the files in a directory and read the README.md file.

opencc-by-4.0Dec 2024View details →

Datasets and R codes used for the analyses in "Seasonal variation in home range size of White-Backed Woodpeckers"

Abstract Knowing a species’ area requirements is fundamental for species conservation. For the nominate subspecies of the White-backed Woodpecker Dendrocopos leucotos, a species of high conservation concern in Europe, estimates of the seasonal and year-round area requirements based on telemetry are missing. In the present study, we radio-tracked adult White-backed Woodpeckers in Central Europe and investigated bi-monthly home range sizes based on three home range estimators in relation to season, sex, body weight, and year. Home range size of 49 radio-tracked individuals varied depending on the used home range estimator, with minimum convex polygons (MCP) and autocorrelated kernel density estimation (AKDE) producing 1.6 – 1.8 and 2 – 3.3 times larger seasonal home ranges than traditional kernel density estimation (KDE). Moreover, home range sizes varied between seasons. Home ranges were smallest in February/March (predicted median home range sizes ranged from 35 ha with KDE to 88 ha with AKDE) and April/May (KDE: 30 ha, AKDE: 55 ha) and larger during the rest of the year (KDE: 48 – 67 ha, AKDE: 136 – 184 ha). The mean home range size of six individuals tracked in all seasons (calculated with all locations per individual) was 116 ha with KDE, 304 ha with MCP and 350 ha with AKDE. Our results highlight the importance of considering the full annual cycle when addressing area requirements of White-backed Woodpeckers and likely also of other species. Furthermore, our study shows that using multiple methods for home range estimation may be useful to obtain results that are both comparable with those of other studies and capture the range in which the true home range size is likely to be. For the conservation of the White-backed Woodpecker, we conclude that at least 116 to 350 ha of forest should be present for a pair.

opencc-by-4.0Nov 2024View details →

Dataset of the publication: Probing Short-Range Correlations in the van der Waals Magnet CrSBr by Small-Angle Neutron Scattering

Dataset of the publication: Probing Short-Range Correlations in the van der Waals Magnet CrSBr by Small-Angle Neutron Scattering DOI: 10.1002/smsc.202400244 A. Rybakov, C. Boix-Constant, D. Alba Venero, H. S. J. van der Zant, S. Mañas-Valero, E. Coronado Small Science, 4, 8, 2400244 (2024)

opencc-by-nc-nd-4.0Aug 2024View details →

ForestSemantic: A Dataset for Semantic Learning of Forest from Close-Range Sensing

ForestSemantic is a dataset for forest semantic studies at both tree- and plot-levels. The dataset supports both instance and semantic segmentation, such as the tree detection and segmentation and the classification of ground, trunk, branches, and foliage components at both tree- and plot-levels. Also, the instance of each first-order branch is provided, For each plot, three files are provided, i.e., "Plot_x.las", "Plot_x_Tree_Reference.xlsx" and "Plot_x_Branch_Reference.txt", where x means the x-th plot. 1) "Plot_x.las" is the data file, which includes the point coordinates and intensity, as well as tree-, classification-, and First-order branch IDs. The tree-, classification-, and First-order branch IDs are stored in the field of "Point Source ID", "Classification" and "GPS Time", respectively. 2) "Plot_x_Tree_Reference.xlsx" includes the reference of the tree structure traits for each tree in the plot. The reference of each tree takes up one row. The tree-ID, position_x, position_y, tree height (m), DBH (m), First-order branch (m), Crown Projection area (m2), Crown Surface area (m2), Crown Volume (m3) are in the column 1 to 9, respectively. 3) "Plot_x_Branch_Reference.txt" includes the reference of the First-order branch in the plot, including the tree ID, branch ID, the start and end point positions of each branch. The record of each individual First-order branch takes up one row, and the column 1 to 9 are tree-ID, First-order Branch ID, Start_x, Start_y, Start_z, End_x, End_y, End_z, and Length. 4) The calculation of the reference of the tree structure traits can be found in <a href="https://doi.org/10.1080/10095020.2024.2313325">https://doi.org/10.1080/10095020.2024.2313325.</a> 5) For more details about the data, readers are referred to "Read me.pdf". If you used this dataset, please cite the following paper: Liang, Xinlian, Hanwen Qi, Xuejie Deng, Jianchang Chen, Shangshu Cai, Qingjun Zhang, Yunsheng Wang, Antero Kukko, and Juha Hyyppä. 2024. “ForestSemantic: A Dataset for Semantic Learning of Forest from Close-Range Sensing.” Geo-Spatial Information Science, March, 1–27. doi:10.1080/10095020.2024.2313325.

opencc-by-4.0Aug 2016View details →

Fig. 2 in Novelties from the Northern Mountains Complex of Madagascar IV: A new Rinorea Aubl. (Violaceae) of restricted range from the Galoko and Kalabinono massifs

Fig. 2. – Distribution map of Rinorea callmanderi Wahlert (stars) in Madagascar plotted on a map of forest cover in 2000 (grey)

opencc-by-4.0Dec 2014View details →

Fig. 2 in On The Geographic Distribution Of Nemognatha Plaumanni Borchmann, 1942 (Coleoptera: Meloidae): New Records From Venezuela, With A 4500 Km Range Extension

Fig. 2. Latero-dorsalvieWofaspecimenof Nemognathaplaumanni BorcHmann, 1942, from tHeCordilleradelaCostaintHeStateofAragua (Venezuela), locatedabout 4500 kmnortH