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Policies, systemic factors, trade-offs and synergies for agroecological transitions
<table> <tbody> <tr> <td>In order to identify the existing policies, systemic factors, trade-offs and synergies for agroecological transition we collected data via desk research, interviews with policy-makers and focus groups. This dataset presents the interview outcomes for 39 policy-makers from our focal countries</td> </tr> </tbody> </table>
Fig. 1. Multilure trap baited with 300 in Myrmecological fauna (Hymenoptera: Formicidae) collected with Multilure-type traps in a Neotropical transitional region from northeastern Mexico
Fig. 1. Multilure trap baited with 300 mL of Strepha Trap® on a tree in the biosphere reserve "El Cielo."
Fig. 1 in A new basal eusauropod from the Middle Jurassic of Yunnan, China, and faunal compositions and transitions of Asian sauropodomorph dinosaurs
Fig. 1. Geographical information on the locality of Nebulasaurus. A. Map of China showing Yunnan Province (shaded black). B. Map of Yunnan Province showing the locality indicated by a silhouette of a sauropod.
Fig. 4 in A new basal eusauropod from the Middle Jurassic of Yunnan, China, and faunal compositions and transitions of Asian sauropodomorph dinosaurs
Fig. 4. Comparison of non-neosauropod eusauropod braincases illustrates general conditions against unique features of the braincase of Nebulasaurus taito gen. et sp. nov. (e.g., frontoparietal fenestra larger than postparietal foramen, supraoccipital not expanding laterally, and supraoccipital contributing little to foramen magnum). A. Shunosaurus lii Dong, Zhou and Zhang, 1983; China, Xiashaximiao Formation, Middle Jurassic (ZDM 65430), in dorsal (A 1) and posterior (A 2) views (modified after Chatterjee and Zheng 2002; supraoccipital was redrawn based on Zhang 1988). B. Mamenchisaurus youngi Pi, Ouyang and Ye, 1996; China, Shangshaximiao Formation, Middle Jurassic (ZDM 83), in dorsal (B 1) and posterior (B 2) views (modified after Ouyan and Ye 2002). C. Omeisaurus tianfuensis He, Li, Cai and Gao, 1984; China, Xiashaximiao Formation, Middle Jurassic; ZDM 5702, in dorsal view (C 1); ZDM 5703 in posterior view (C 2) (modified after He et al. 1988). D. Spinophorosaurus nigerensis Remes, Ortega, Fierro, Joger, Kosma, Ferrer, PALDES, SNHM, Ide, and Maga, 2009; Niger, Irhazer Group, Middle Jurassic (GCP-CV-4229), in dorsal (D 1) and posterior (D 2) views (modified after Knoll et al. 2012). Arrows indicate wide participation of supraoccipital in the margin of foramen magnum. Asterisks indicate lateral expansion of supraoccipital along exoccipital-parietal contact. Scale bars 5 cm.
Fig. 3 in A new basal eusauropod from the Middle Jurassic of Yunnan, China, and faunal compositions and transitions of Asian sauropodomorph dinosaurs
Fig. 3. Photographs of the holotype of the sauropodomorph dinosaur Nebulasaurus taito gen. et sp. nov., Xiabanjing, Zhanghe Formation, Middle Jurassic LDRC-v.d.1). A. The braincase (holotype) in right lateral view. B. Details of the metotic region in left lateral view.
Fig. 10 in Patterns of spatio-temporal distribution as criteria for the separation of planktic foraminiferal species across the Danian-Selandian transition in Spain
Fig. 10. Lower/higher (L/H) latitude taxa ratio and quantitative stratigraphic distribution of planktic foraminiferal genera across the Danian–Selandian transition at Caravaca. Asterisks indicate climate warming events identified here.
Fig. 9 in Patterns of spatio-temporal distribution as criteria for the separation of planktic foraminiferal species across the Danian-Selandian transition in Spain
Fig. 9. Cluster analyses based on Morisita's index for relative abundance data of species from Caravaca in the Acarinina uncinata Zone (4a) and in the Morozovella cf. albeari Zone (4b); l1 = Simpson's diversity index in sample j; l2 = Simpson's diversity index in sample k; xij = percentage of species i in sample j; xik = percentage of species i in sample k.
Fig. 2 in Patterns of spatio-temporal distribution as criteria for the separation of planktic foraminiferal species across the Danian-Selandian transition in Spain
Fig. 2. Comparison of some planktic foraminiferal zonations proposed for the D–S transition in low and middle latitudes. Correlation with the chronostratigraphic and magnetostratigraphic scales based on data from the Zumaia stratotype. (*) Probable biostratigraphic position of the base of the Igorina pusilla Zone by Toumarkine and Luterbacher (1985), and Canudo and Molina (1992), based on data from Zumaia. (**) Biostratigraphic position of the P3a/P3b boundary by Berggren and Pearson (2005), assuming that their species concept of I. albeari includes Morozovella crosswicksensis by Blow (1979) and Arenillas and Molina (1997) and/or M. cf. albeari by Arenillas et al. (2008). FOD, first occurrence data; L/H, lower/higher latitude, LOD, last occurence data.
Fig. 3 in Patterns of spatio-temporal distribution as criteria for the separation of planktic foraminiferal species across the Danian-Selandian transition in Spain
Fig. 3. Quantitative stratigraphic distribution of planktic foraminiferal species across the Danian–Selandian transition at Caravaca. The shown stratigraphic interval does not include the lower part of the A. uncinata Zone, where Globoconusa species were found (see Arenillas and Molina 1997).
Fig. 4 in New dryolestidan mammal from the Hauterivian-Barremian transition of the Iberian Peninsula
Fig. 4. Drawings of Dryolestida left upper−molar, modified from the original descriptions. A–C, Kimmeridgian; D–F, Tithonian–Berriasian; G–H, early Barremian; I, late Barremian. A. Left M4 or M5 of Comotherium richi Prothero, 1981, from the Upper Jurassic Morrison Formation, Como Bluff locality, Wyoming, USA. B. Right M5, reversed, of Dryolestes leiriensis Martin, 1999, from Guimarota, Portugal. C. Left M6 of Krebsotherium lusitanicum Martin, 1999, from Guimarota, Portugal. D. Right M4 or M 6 (reversed) of Portopinheirodon asymmetricus Martin, 1999, Porto Pinheiro, Lourinha, Portugal. E. Right M5 (reversed) of Laolestes andresi Martin, 1999, from Porto Pinheiro, Lourinha, Portugal. F. Right upper molar of Donodon perscriptoris Sigogneau−Russell, 1991, Anoual, Morocco. G. Left M4 or M 5 of Crusafontia amoae sp. nov., holotype, Cuesta Corrales 2, El Castellar Formation, Galve, Teruel, Spain. H. Right M6 or M 7 (reversed) of Crusafontia amoae sp. nov., first described as upper molar of Crusafontia cuencana by Krebs (1993), P−2 H4 Pelejón 2, Galve, Teruel, Spain. I. Left M2 or M3, of Crusafontia cuencana Henkel and Krebs, 1969, Uña, La Huérguina Formation, Cuenca, Spain, (from Krebs 1993). Scale bars 1 mm.
Fig. 1 in New dryolestidan mammal from the Hauterivian-Barremian transition of the Iberian Peninsula
Fig. 1. Geographical and geological setting of Galve (Teruel, Spain). A. Simplified geological map of the Iberian Peninsula. B. Palaeogeographic subbasins within the Maestrazgo Basin and active faults during Early Cretaceous sedimentation, modified from Salas et al. (2001), and the palaeogeographical—and geographical—relationship with the Uña area (Cuenca, Spain). C. Litho− and chronostratigraphy of the Mesozoic mammal record from the areas of Galve and Uña. Abbreviations: Ga, Galve; Mo, Morella; Ol, Oliete; Pa, Las Parras; Pe, Perelló; Pg, Peñagolosa; Sa, Salzedella.
Fig. 6 in New dryolestidan mammal from the Hauterivian-Barremian transition of the Iberian Peninsula
Fig. 6. Drawings of premolars modified and assigned to dryolestids in Martin (1998). A. Nomenclature of the "peramuran" premolars. B. Left P4 and P5 of Peramus tenuirostris modified after Clemens and Mills (1971). C. Right P4 here assigned to Pocamus pepelui Galve Th 23, reversed, modified after Martin (1998). D. Right P5 of Pocamus pepelui (holotype) from Poca, modified after Canudo and Cuenca−Bescós (1996). E. Left upper molar of Afriquiamus nessovi, modified after Sigogneau−Russell (1999). F–H. Deciduous premolars (dP) and premolars of Dryolestida for comparison with those of "Peramurans". F. Right dP3–4 of Dryolestes leiriensis (reversed) modified after Martin (1997, 1999). G. Right P4 of Dryolestes leiriensis (reversed) modified after Martin (1999). H. Left P3 and P4 of Krebsotherium lusitanicum modified after Martin (1999). Note that the molars are all drawn with the mesial side to the left; thus some are reversed drawings.
Fig. 3 in New dryolestidan mammal from the Hauterivian-Barremian transition of the Iberian Peninsula
Fig. 3. Dryolestidan mammal Crusafontia amoae sp. nov., MPZ CC2−1 M4 or M5, holotype, from the site of Cuesta Corrales 2, Colladico Blanco level, El Castellar Formation, Galve, Teruel, Spain in, occlusal (A), mesial (B), labial (C), distal (D), and lingual (E) views. The schematic drawing of C. amoae, in the box in the lower left−hand corner shows the main anatomical elements of the occlusal surface of a dryolestidan.
Fig. 2 in New dryolestidan mammal from the Hauterivian-Barremian transition of the Iberian Peninsula
Fig. 2. Geological setting of the Mesozoic mammal fossil sites from the Galve area. Stratigraphy of the Wealden facies and geological mapping of the Galve syncline (modified from Díaz Molina and Yébenes 1987).
Dataset of Northern Khanty transitive clauses, version 1.0
<table> <tbody> <tr> <td><span>This dataset is created for a study of morphosyntactic variation in Northern Khanty.</span></td> </tr> <tr> <td><span>The research is conducted in terms of the project ”Verb agreement and voice in Northern Khanty discourse” supported by the Alexander von Humboldt Foundation.</span></td> </tr> <tr> <td><span>The results of my study are to appear in an article "The emergence of hierarchical alignment in Northern Khanty: a comparative dialectal corpus study" submitted to the journal "Linguistica Uralica".</span></td> </tr> <tr> <td><span>The dataset contains mannualy annotated transitive clauses from four Northern Khanty dialects: Kazym, Obdorsk, Shuryshkary, and Tegi.</span></td> </tr> <tr> <td><span>Transitive clauses here are active and passive clauses containing at least two overtly and/or pronominally expressed core arguments</span></td> </tr> <tr> <td><span>Parameters: voice, conjugation, person, animacy, uniqueness/maximality, familiarity</span></td> </tr> <tr> <td><span>The sources are: </span></td> </tr> <tr> <td><span>(1) an unpublished corpus of Northern Khanty (Kazym, Tegi, Shuryshkary) compiled by Egor Kashkin, </span></td> </tr> <tr> <td><span>(2) an online corpus of Obdorsk Khanty from the database "Endangered Languages and Cultures of Siberia".</span></td> </tr> <tr> <td> </td> </tr> <tr> <td><span>Warning!!! The annotation is a product of my own work and has not been reviewed by third party, thus it may contain errors</span></td> </tr> <tr> <td><span>Glosses are only partially available, translations and glosses from (1) are available only in Russian</span></td> </tr> <tr> <td><span>Parameters of uniqueness/maximality and familiarity were only annotated separately for Obdorsk and Kazym dialects, in Tegi and Shuryshkary annotation all instances of familiar referents had been treated as unique/maximal </span></td> </tr> <tr> <td> </td> </tr> <tr> <td><span>This version was published on 9.08.2024, it is recommended to check if a newer version is available</span></td> </tr> <tr> <td><span>Should you have any questions, do not hesitate to contact me at nikita.muraviev@gmail.com</span></td> </tr> </tbody> </table>
Fig. 2 in Molecular detection of Cryptosporidium parvum in wild rodents (Phyllotis darwini) inhabiting protected and rural transitional areas in north-central Chile
Fig. 2. Phylogram representing analysis of the 18 rRNA region. The evolutionary history was inferred with maximum likelihood method and the Tamura 3-parameter (T92) model with a discrete Gamma distribution (5 categories (+G)). Analysis contains sequences uploaded from GenBank (with Cryptosporidium species, host, country, and accessions numbers in brackets) and those obtained in the present study are shown in triangles (with ID isolate, host, site of sampling and country, and accessions numbers in brackets). Bootstrap values are represented as per cent of internal branches (1000 replicates), and values lower than 50 are hidden. The tree is drawn to scale, with branch lengths measured in the number of substitutions per site. Cryptosporidium muris was used to root the tree.
Fig. 1 in Molecular detection of Cryptosporidium parvum in wild rodents (Phyllotis darwini) inhabiting protected and rural transitional areas in north-central Chile
Fig. 1. Map of the Coquimbo region in Chile showing the two types of areas (i.e., Bosque Fray Jorge National Park - BFPNP [in green]; El Tangue Farm [in blue]) in which Darwin's leaf-eared mice (Phyllotis darwini) were sampled. In each area, 4 grids were established, and 200 capture points were allocated per grid. (UTM projection. Datum WGS84, Zone 19J).
Fig. 4 in New and previously known ectoparasitic monogenoids (Platyhelminthes) on native and non-native fishes from tributaries of the Usumacinta River basin (southern Mexico), a Neotropical transition zone
Fig. 4. Copulatory complexes of Ligictaluridus mirabilis (Mueller 1937; Klassen and Beverley-Burton (1985) on Southern blue catfish Ictalurus meridionalis (Ictaluridae) from the Usumacinta river basin (southern Mexico). A – copulatory complex in ventral view; B – copulatory complex in dorsal view. Abbreviations: mco – male copulatory organ; ap – accessory piece.
Fig. 1. Icelanonchohaptor tropicalis n in New and previously known ectoparasitic monogenoids (Platyhelminthes) on native and non-native fishes from tributaries of the Usumacinta River basin (southern Mexico), a Neotropical transition zone
Fig. 1. Icelanonchohaptor tropicalis n. sp. on the Usumacinta buffalo Ictiobus meridionalis (Catostomidae) from the Usumacinta river basin (southern Mexico). A – whole mount (composite, dorsal view); B – vagina; C – copulatory complex (ventral view); D – egg; E – Haptor; F – Hook. Abbreviations: mco – male copulatory organ; ap – accessory piece; sv – seminal vesicle.
Fig. 3 in New and previously known ectoparasitic monogenoids (Platyhelminthes) on native and non-native fishes from tributaries of the Usumacinta River basin (southern Mexico), a Neotropical transition zone
Fig. 3. Haptoral and copulatory complex sclerites of Heteropriapulus heterotylioides n. sp. on Pterygoplichthys pardalis (Loricariidae) from the Usumacinta river basin (southern Mexico). A, B, and C – copulatory complexes (A and C in dorsal view; B in ventral view); D – ventral anchor; E – hook; F, G and H – dorsal anchors; I and J – ventral bars; K and L – dorsal bars; M – vaginal tube.
ScienceDex guides
Understand access before you commit
These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
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.