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FIGURE 6 in Anticyphon gen. nov., a new genus of Scirtidae (Coleoptera: Scirtoidea) inhabiting high altitude Andean cloud forests and páramo formation
FIGURE 6. Anticyphon davidsoni sp. nov., male genitalia. A) male genitalia, B) penis, C) tegmen, D) sternite VIII, E) sternite IX, F) tergite VIII, G) tergite IX. Scale bar = 0.5 mm. Abbreviations: dpp—dorsal process of penis, pe—penis, pm—paramere, pmd—parameroid, s—sternite, t—tergite, tg—tegmen, trg—trigonium.
FIGURE 2 in Anticyphon gen. nov., a new genus of Scirtidae (Coleoptera: Scirtoidea) inhabiting high altitude Andean cloud forests and páramo formation
FIGURE 2. Anticyphon gen. nov., mandibles (A, D, G), maxillae (B, E, H), labia (C, F, I). A – C) A. davidsoni sp. nov., D – F) A. oyonensis sp. nov., G – I) A. paramoensis sp. nov.
FIGURE 1. Anticyphon gen. nov., habitus. A in Anticyphon gen. nov., a new genus of Scirtidae (Coleoptera: Scirtoidea) inhabiting high altitude Andean cloud forests and páramo formation
FIGURE 1. Anticyphon gen. nov., habitus. A) A. davidsoni sp. nov., B) A. ecuadorensis sp. nov., C) A. oyonensis sp. nov., female, D) A. oyonensis sp. nov., male E) A. paramoensis sp. nov., light form, F) A. paramoensis sp. nov., dark form, G) A. peruvianus sp. nov., H) A. santanderensis sp. nov. Scale bars = 1.0 mm.
FIGURE 3. Terrapotamon longitarsus n in A new species of long-legged terrestrial Terrapotamon Ng, 1986 (Crustacea: Brachyura: Potamidae) from limestone formations in Satun, southern Thailand
FIGURE 3. Terrapotamon longitarsus n. sp. Overall habitus. A, male (35.0 × 29.5 mm) (ZRC 2016.0162 a); B, paratype male (28.4 × 23.8 mm) (PSUZC 20150611 - 01.01); C, female (23.8 × 20.2 mm) (ZRC 2016.0162 b).
FIGURE 2. Terrapotamon longitarsus n in A new species of long-legged terrestrial Terrapotamon Ng, 1986 (Crustacea: Brachyura: Potamidae) from limestone formations in Satun, southern Thailand
FIGURE 2. Terrapotamon longitarsus n. sp. Holotype male (47.4 × 38.6 mm) (ZRC 2016.0161). A, right third maxilliped; B, ventral view of cephalothorax showing posterior thoracic sternum and pleon (right margin of somite 3 damaged); C, right ambulatory legs; D, dorsal view of right cheliped; E, outer view of right chela.
Star Formation In Nearby Clouds (SFiNCs): X-ray And Infrared Source Catalogs And Membership. SPCM Atlas Dataset.
<p>The SPCM (SFiNCs Possible Cluster Member) Atlas dataset accompanies the article entitled ``Star Formation In Nearby Clouds (SFiNCs): X-ray And Infrared Source Catalogs And Membership,'' by Getman, Broos, Kuhn, Feigelson, Richert, Ota, Bate, and Garmire, to appear in The Astrophysical Journal Supplement Series. The paper is also available on-line on astro-ph at: https://arxiv.org/abs/1612.05282 . SPCM Atlas is a collection of 25 PDF files. Four pdf files are associated with the SFiNCs star forming region (SFR) Cep OB3b, and 21 pdf files are associated with the remaining 21 SFiNCs SFRs. Full description of SPCM Atlas is given in the Appendix B section of the article. This upload is superseded by a new version, http://doi.org/10.5281/zenodo.345398 .</p>
Pattern formation in skyrmionic materials with anisotropic environments
<p>Magnetic Skyrmions have attracted broad attention during recent years because they are regarded as promising candidates as bits of information in novel data storage devices. A broad range of theoretical and experimental investigations have been conducted with the consideration of axisymmetric Skyrmions in isotropic environments. However, one naturally observes a huge variety of anisotropic behavior inmany experimentally relevant materials. In the present work, we investigate the influence of anisotropic environments onto the formation and behavior of the noncollinear spin states of skyrmionic materials by means of Monte Carlo calculations. We find skyrmionic textures which are far from having an axisymmetric shape. Furthermore, we show the possibility to employ periodic modulations of the environment to create skyrmionic tracks.</p>
Raw data used for COI delineation of the Eupolybothrus species: Authors: Stoev et al. 2013 Data type: genomic The archive contains the following data: 1) fasta-Alignment as the basis for all analyses (.FASTA), 2) mega-file for the calculation of the genetic distances and the NJ tree (.MDSX), 3) NJ-tree in Newick format (.NWK), 4) graph of the TCS Software for the Statistical Parsimony method (.GRAPH) File: E_cavernicolus.rar from: Eupolybothrus cavernicolus Komerički & Stoev sp. n. (Chilopoda: Lithobiomorpha: Lithobiidae): the first eukaryotic species description combining transcriptomic, DNA barcoding and micro-CT imaging data - Biodiversity Data Journal 1: e1013 (28 October 2013) https://doi.org/10.3897/BDJ.1.e1013
<p>Authors: Stoev et al. 2013 Data type: genomic The archive contains the following data: 1) fasta-Alignment as the basis for all analyses (.FASTA), 2) mega-file for the calculation of the genetic distances and the NJ tree (.MDSX), 3) NJ-tree in Newick format (.NWK), 4) graph of the TCS Software for the Statistical Parsimony method (.GRAPH) File: E_cavernicolus.rar</p>
Character coding comparisons: matrices of 115 traits for hominoids in TNT format.
<p>TNT_character_matrix_positions.csv: provides descriptions of the 115 characters and their positions in the character matrices.</p> <p>TNT_95CI_character_matrix.tnt: TNT format character matrix with 115 traits. Each trait value is a 95% confidence interval for the species mean.</p> <p>TNT_DVC_character_matrix.tnt: TNT format character matrix with 115 traits. Each trait value is coded using divergence coding.</p> <p>TNT_GWC_character_matrix.tnt: TNT format character matrix with 115 traits. Each trait value is coded using generalized gap weighting.</p> <p> TNT_HSC_character_matrix.tnt: TNT format character matrix with 115 traits. Each trait value is coded using homogeneous subset coding.</p> <p>TNT_IDO_character_matrix.tnt: TNT format character matrix with 115 traits. Each trait value is coded using identification of overlap coding.</p> <p>TNT_Mean_character_matrix.tnt: TNT format character matrix with 115 traits. Each trait value is a species mean.</p> <p> </p>
FIG. 8 in Les forages de Juzanvigny (Aube, France): lithobiostratigraphie des formations du Barrémien à l'Albien moyen dans l'est du bassin de Paris et datations par les ammonites
FIG. 8. — Position stratigraphique du forage AUB 111 dans l'Albien-type de l'Aube et organisation géométrique des dépôts entre l'Albien en grande partie sableux de l'Yonne et celui essentiellement argileux de l'Aube et du Perthois (modifié d'après Amédro & Matrion 2014). Le forage AUB 111 recoupe un intervalle équivalent aux principaux affleurements suivants: berges de la rivière Aube à Unienville, carrière de Montreuil-sur-Barse, fosse creusée au fond du réservoir Aube à Pogains et carrière de Courcelles, mais dans une suite lithologique continue, dépourvue de lacunes d'observation.
FIG. 2 in A revised heterostracan-based ichthyostratigraphy of the Wood Bay Formation (Lower Devonian, Spitsbergen), and correlation with Russian Arctic archipelagos
FIG. 2. — Stratigraphical section of the Andrée Land Block of northern Spitsbergen, after Harland (1997) and Blomeier et al. (2003a). Ages after Blieck et al. (2000, 2002) and McCann (2000). Note that: 1) it is common to subdivide the lowermost part of the Red Bay Group into Wulffberget, Rabotdalen (locally present) and Princesse Alicefjellet formations instead of only the Rivieratoppen Formation, according to Murashov & Mokin (1976, 1979) – this subdivision being applicable throughout the Devonian of northern Spitsbergen (Blomeier et al. 2003a, b); and 2) the Grey Hoek and Wijde Bay formations are considered as lateral equivalents and Eifelian in age by Schweitzer (1999); however, Schweitzer's idea that the Grey Hoek and Wijde Bay formations are of equal age is certainly not true along Wijdefjorden, where one lies on top of the other with a depositional boundary; upper parts of the Grey Hoek Formation in the Woodfjorden area may be coeval with the Wijde Bay Formation farther east (Blomeier et al. 2003a, b; W. Dallmann, pers. comm. 2007).
Text-fig. 3. Progonomys morganae molars from the upper part of the Nagri Formation. a) YGSP 33180, holotype, from Y 450 and b) 54091 from Y 450; both left M1 with buccal side upward. c) 34159 from Y259; and d) 36168 from Y 311, left and right m1, respectively, with lingual side upward. Scale for all is 1 mm. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 3. Progonomys morganae molars from the upper part of the Nagri Formation. a) YGSP 33180, holotype, from Y 450 and b) 54091 from Y 450; both left M1 with buccal side upward. c) 34159 from Y259; and d) 36168 from Y 311, left and right m1, respectively, with lingual side upward. Scale for all is 1 mm.
FIG. 3 in Hypsodont Myomiminae (Gliridae, Rodentia) from five new localities in the Lower Miocene Tudela Formation (Bardenas Reales, Ebro Basin, Spain) and their bearing on the age of the Agenian-Ramblian boundary
FIG. 3. — Distribution chart of the Myomiminae species studied in this paper and in Daams (1990). The succession of the localities from Daams (1990) is, though in stratigraphical order, not calibrated.
Fig. 1 in Pseudocyclammina Sarvakensis Sp. Nov. And Pseudotextulariella Brevicamerata Sp. Nov.: Further Evidence For The Cenomanian Megadiversity Of Larger Benthic Foraminifera From The Sarvak Formation Of Sw Iran
Fig. 1 Number of agglutinated foraminiferal genera (small and large taxa) in each geological stage (modified from Kaminski et al., 2008, fig. 1).
Fig. 5 in Pseudocyclammina Sarvakensis Sp. Nov. And Pseudotextulariella Brevicamerata Sp. Nov.: Further Evidence For The Cenomanian Megadiversity Of Larger Benthic Foraminifera From The Sarvak Formation Of Sw Iran
Fig. 5 Lower and Upper Cretaceous (Cenomanian) species of Pseudotextulariella Barnard, 1953. a-i, k Pseudotextulariella brevicamerata sp. nov., middle Cenomanian Sarvak Formation of SW Iran, Tang-e Darbast section (a-i) and Arman well-1 (k), thin-sections RAP 188 and AMN 3173.49 m. a, h-i Tangential sections. b, d-e, g Subaxial section, holotype specimen in e. c, k Oblique sections. f Fragmentary transverse section. j, l Pseudotextulariella courtionensis Brönnimann, 1967, Valanginian of Switzerland (from Brönnimann, 1967, pl. 1, figs. 1 and 5). m-n Pseudotextulariella cretosa (Cushman, 1932), transverse and axial sections (from Brönnimann, 1967, pl. 3, figs. 2 and 5). Abbreviations: b = beam, cha = chamber, fo = foramen, ib = intercalary beam, r = rafter, s = septum.
Fig. 3 in Pseudocyclammina Sarvakensis Sp. Nov. And Pseudotextulariella Brevicamerata Sp. Nov.: Further Evidence For The Cenomanian Megadiversity Of Larger Benthic Foraminifera From The Sarvak Formation Of Sw Iran
Fig. 3 Lithostratigraphic log of the Tang-e Darbast section, the type locality of Pseudocyclammina sarvakensis sp. nov and Pseudotextulariella brevicamerata sp. nov., showing the distribution of some (larger) benthic foraminifera. a Neoiraqia insolita (Decrouez & Moullade), b Orbitolinopsis cenomaniensis Schlagintweit & Yazdi-Moghadam, c Conicorbitolina cf. conica (d'Archiac), d Mesorbitolina aperta (Erman), e Orbitolina ex gr. concava (Lamarck), f Rotorbinella mesogeensis (Tronchetti), g Nezzazata gr. gyra-conica (Smout), h Decastroia cf. serrakieli Vicedo & Piuz, i Myriastyla omanensis Piuz, Meister & Vicedo, j Chrysalidina gradata Orbigny, k Iraqia ultima Yazdi-Moghadam & Schlagintweit.
Fig. 4 in Pseudocyclammina Sarvakensis Sp. Nov. And Pseudotextulariella Brevicamerata Sp. Nov.: Further Evidence For The Cenomanian Megadiversity Of Larger Benthic Foraminifera From The Sarvak Formation Of Sw Iran
Fig. 4 Upper Cretaceous species of Pseudocyclammina Yabe & Hanzawa, 1926; note the different scales. a-g Pseudocyclammina sarvakensis sp. nov., middle Cenomanian Sarvak Formation of SW Iran, Tang-e Darbast section, thin-section RAP 181 (b, d-f), and Shahneshin section, thin-section AKHS 97 (c, g). a Equatorial section, microspheric specimen? (from Sampò,1969 illustrated as Cyclammina sp. (?) in pl. XLV, fig. 2). b Equatorial section, holotype. c, e Oblique sections. d Subaxial section. f Oblique tangential section. g Oblique equatorial section, megalospheric specimen? h Pseudocyclammina massiliensis Maync, early-middle Campanian of Brač Island, Croatia. i Pseudocylammina rugosa (Orbigny), equatorial section, Cenomanian of W France (from Maync, 1952, pl. 12, fig. 10). j-m Pseudocyclammina sphaeroidea Gendrot, Upper Cretaceous (?Coniacian) of Austria (from Schlagintweit, 1992, pl. 1, figs. 13-16). Subaxial section (j), equatorial section of a specimen with uncoiling final stage (k), equatorial section (l), equatorial section slightly oblique (m).
Fig. 2 a in Pseudocyclammina Sarvakensis Sp. Nov. And Pseudotextulariella Brevicamerata Sp. Nov.: Further Evidence For The Cenomanian Megadiversity Of Larger Benthic Foraminifera From The Sarvak Formation Of Sw Iran
Fig. 2 a Simplified geological map of Iran (after Schlagintweit & Yazdi-Moghadam, 2021) showing the main tectonic subdivisions. b Road map of the Tang-e Darbast section (type-locality of Iraqia ultima Yazdi-Moghadam & Schlagintweit, 2022 and Simplorabanitina simplex Consorti, Schlagintweit, and Yazdi-Moghadam, 2022). c Road map of the Shahneshin section. d Position of Arman well-1. e Tectono-stratigraphic units of the Zagros belt (modified after Yazdi-Moghadam & Schlagintweit, 2021). The position of the studied sections is marked by an asterisk. Abbreviations: BF Balarud Fault, CEIM Central East Iran Microplate, HZF High Zagros Fault, KZF Kazerun Fault, MFF Mountain Front Fault, MZRF Main Zagros Revers Fault, MZT Main Zagros Thrust, SSZ Sanandaj-Sirjan Zone, UDMA Uromia Dokhtar Magmatic Arc, ZFTB Zagros Fold
Fig 1 in A new Cambrian catillicephalid trilobite from the Shallow Bay Formation of western Newfoundland, Canada
Fig 1. Cranidia of catillicephalid trilobite Catillicephala cifellii sp. nov. from the Downes Point Member, Shallow Bay Formation, Guzhangian, Miaolingian, Cambrian; boulder BPS 467, Broom Point South, western Newfoundland, Canada. A. GSC 142512, holotype; dorsal (A1), lateral (A2), and anterior (A3) views. B. GSC 142513, paratype; dorsal view. C. GSC 142514, paratype; dorsal (C1), lateral (C2), and anterior (C3) views. D. GSC 142515, paratype; dorsal view. Scale bars 1 mm.
Fig. 3 in New Eocene South American native ungulates from the Quebrada de los Colorados Formation at Los Cardones National Park, Argentina
Fig. 3. New fossil specimens of Typotheria and Toxodontia from the Quebrada de Los Colorados Formation exposed at Quebrada Grande locality, Los Cardones National Park (Salta Province), Casamayoran SALMA. A, B. Colbertiasp. A. IBIGEO-P 58a, left maxillary fragment with M2–M3 in occlusal view. B. IBIGEO-P 58b, left maxillary fragment with P4–M3 in occlusal view. C–E. Pampahippus secundus Deraco and García-López, 2016. C. IBIGEO-P 62, right trigonid and incomplete talonid of a lower right molar in occlusal view. D. IBIGEO-P 63, fragmented left p3 or p4 in occlusal view. E. IBIGEO-P 64, left m1? in occlusal (E1), labial (E2), and lingual (E3) views. Photographs (A1–E1, E3, E4), explanatory drawings (A2–E2). Dashed area indicates broken or missing dental areas.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.