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Figure 2 in Clonal mechanisms that matter in Agave fourcroydes and A. sisalana invasions in drylands: implications for their management
Figure 2. Flowering, aerial bulbil, and shoot from rhizomes phenology of Agave fourcroydes (AF) and A. sisalana (AS) in the study zone. Wilcoxon signed-rank tests showed no statistical differences between species in any variable. Mean % floral buds: W = 29.0, p-value = 0.141; Mean % flowers: W = 2.0, p-value = 0.789; Mean % bulbils: W = 49.0, p-value = 0.834; Mean % fallen bulbils: W = 13.0, p-value = 0.083; Mean % new shoots from rhizomes: W = 16.0, p-value = 0.834. W = Wilcoxon statistic.
Figure 1 in Clonal mechanisms that matter in Agave fourcroydes and A. sisalana invasions in drylands: implications for their management
Figure 1. Diagram of a rosette of Agave fourcroydes or A. sisalana showing their clonal ramet types. BS: basal shoots, born directly from the rosette; RS: shoots from rhizomes, and aerial bulbils from floral scapes.
Figure 1 in Effects of Palmer Amaranth (Amoronthus polmeri) Establishment Time and Distance from the Crop Row on Biological and Phenological Characteristics of the Weed: Implications on Soybean Yield
Figure 1. Schematic representation of the experimental setup depicting the distance of Amoronthus polmeri (AMAPA) from the crop (i.e., 0, 24, and 48 cm from the soybean row) and the sequence of A. polmeri establishment time (i.e., 0, 1, 2, 4, 6, and 8 wk after soybean emergence [WAE] or AMAPA-0, AMAPA-1, AMAPA-2, AMAPA-4, AMAPA-6, and AMAPA-8, respectively). Each treatment combination (i.e., establishment time × distance from the crop) was applied only to one randomly selected experimental plot per replication.
Paleoseismology of the Northern Kongur Shan Extensional System, NE Pamir: Implications for Potential Irregular Earthquake Recurrence
<p>Data and code used in the manuscript submitted to JGR: Solid Earth, including:</p> <p>1. 0.1-m resolution DEM at the Alasai site</p> <p>2. Photomosaics of the lacustrine section and fault exposure</p> <p>3. Dataset on earthquake magnitude and liquefaction distance</p> <p>4. Matlab code for scarp degradation modeling</p> <p>5. Matlab code for Monte Carlo simulation of earthquake cycles</p>
Diagramms and Figures for a Bachelor Thesis: "Morphological Diversity of Bryophytes: Methodological Approaches and Ecological Implications"
<p>This depository holds all diagramms and figures that were created with the collected data used in the Bachelor's Thesis using R Version 4.4.0 or Python Version 3.12.4. <br><br></p>
Fig. 7 in A new Late Ordovician bubble-headed trilobite species from South West Wales and its implications for biostratigraphy
Fig. 7. Chart showing the frequency distribution of numbers of denticles on lateral margins of complete librigenae of Staurocephalus oliveae sp. nov. from the upper Katian (Upper Ordovician) Sholeshook Limestone Formation at Talfan Farm, Llanddowror, Carmarthenshire, Wales, UK. n = 36.
Fig. 3 in A new Late Ordovician bubble-headed trilobite species from South West Wales and its implications for biostratigraphy
Fig. 3. Encrinurid trilobite Staurocephalus oliveae sp. nov. from the upper Katian (Upper Ordovician) Sholeshook Limestone Formation at Talfan Farm, Llanddowror, Carmarthenshire, Wales, UK. A. Holotype, NMW 2013.11G.1, cephalon in dorsal (A1), oblique anterolateral (A2), and frontal (A3) views. B. Paratype, NMW 2013.11G.2, cephalon in dorsal (B1), oblique anterolateral (B2), and dorsolateral (B3) views. C. Paratype, NMW 2013.11G.6, cranidium in dorsal view. D. Paratype, NMW 2013.11G.7, partial cranidium, dorsal view of internal mould (D1), ventral view of external mould (D2), and latex cast of external mould (D3). E. Paratype, NMW 2013.11G.8, cephalon, external mould in ventral view (E1) and latex cast of external mould (E2). F. Paratype, NMW 2013.11G.9, genal angle of cranidium, showing marginal denticles decreasing in size posteriorly. Scale bars 2 mm, except F 1 mm.
Fig. 6 in A new Late Ordovician bubble-headed trilobite species from South West Wales and its implications for biostratigraphy
Fig. 6. Historic specimens of the encrinurid trilobite Staurocephalus from museum collections. A. SM A31592, cranidium in dorsal view labelled Staurocephalus cf. murchisoni Barrande" from the Sholeshook Limestone Formation (upper Katian, Upper Ordovician) in the Sholeshook railway cutting, Haverfordwest area, herein assigned to S. oliveae sp. nov.? B. BIRUG 48862, cranidium in dorsal view labelled "Staurocephalus cf. murchisoni" from the lower Tre-wylan Beds (Cautleyan) (upper Katian, Upper Ordovician) in the Llansantffraid-ym-Mechain district of the south-eastern Berwyn Hills, Mid Wales (Whittington 1938: 451, locality 42), herein assigned to S. oliveae sp. nov.? C, D. Specimens from the King collection, Sedgwick Museum, from the (locally) basal Ashgill mudstones (lower Rawtheyan, Ashgill Zone 5) (upper Katian, Upper Ordovician) of Aber Marchnant, Berwyn Hills, Mid Wales, originally identified as Staurocephalus cf. murchisoni by King (1923) and assigned to S. clavifrons by Whittington (1968), herein assigned to S. aff. oliveae. C. SM A39813, incomplete cranidium in dorsal view. D. SM A39814.A, incomplete cranidium in dorsal view (D1) and close up of left genal area (D2) to show large lateral denticles (arrowed). E. SM A31589, dorsal view of incomplete cranidium labelled "Staurocephalus globiceps" from the Marr collection, Sedgwick Museum, from the Slade and Redhill Mudstone Formation at Pelcomb Cross, Haverfordwest, herein assigned to S. cf. clavifrons. Note the prominent genal spine on the right side. Scale bars 1 mm, except D2 0.5 mm.
Fig. 2 in A new Late Ordovician bubble-headed trilobite species from South West Wales and its implications for biostratigraphy
Fig. 2. Stratigraphical column showing the age of the Sholeshook Limestone Formation (in blue) and the underlying and overlying formations together with the shelly and chitinozoan biozonations of the Anglo-Welsh succession. Asterisk shows approximate age of the Talfan Farm locality, in the lower part of the formation (equivalent to Cautleyan Zone 1).
Fig. 5 in A new Late Ordovician bubble-headed trilobite species from South West Wales and its implications for biostratigraphy
Fig. 5. Reconstruction drawings of the encrinurid trilobite Staurocephalus oliveae sp. nov. A. Cephalon, in anterior (A1), left lateral (A2), ventral (A3), and dorsal (A4) views. B. Pygidium, in ventral (B1) and dorsal (B2) views. Cephalon has a mean maximum width (tr.) of 10.15 mm; pygidium has a mean maximum width (tr.) of 3.96 mm.
Fig. 4 in A new Late Ordovician bubble-headed trilobite species from South West Wales and its implications for biostratigraphy
Fig. 4. Encrinurid trilobite Staurocephalus oliveae sp. nov. from the upper Katian (Upper Ordovician) Sholeshook Limestone Formation at Talfan Farm, Llanddowror, Carmarthenshire, Wales, UK. A. Paratype, NMW 2013.11G.5, rostral plate in ventral view. B. Paratype, NMW 2013.11G.3, right librigena in lateral view. C. Paratype, NMW 2013.11G.10, left librigena in lateral view. D. Paratype, NMW 2013.11G.12, right librigena in lateral view. E. Paratype, NMW 2013.11G.13, thoracic segment in dorsal view. F. Paratype, NMW 2013.11G.4, pygidium in dorsal view. G. Paratype, NMW 2013.11G.11, pygidium in dorsal view. H. Paratype, NMW 2013.11G.15, pygidium in ventral view of external mould (H1) and latex cast of external mould (H2). Scale bars 2 mm.
Fig. 8 in A new Late Ordovician bubble-headed trilobite species from South West Wales and its implications for biostratigraphy
Fig. 8. Graph showing the number of lateral denticles on librigenae of various Staurocephalus species through time. Circle represents the mean, vertical lines the range where one was observed in that species. Chatterton and Campbell (1980) described S. struszi as having "twelve (possibly eleven on some specimens)" denticles. Species names in black font represent occurrences in England and Wales, those in red font occur outside Avalonia. Note that Cautleyan and Rawtheyan are regional stages from the AngloWelsh chronostratigraphy and belong in the upper part of the international Katian Stage. The remaining stages are international. The Telychian is approximately twice the length of the other stages (e.g., Ogg et al. 2008: fig. 1.1), hence the wider spacing allocated to it.
Fig. 5 in Evidence for parallel development of ever-growing molars in Early Pleistocene rodents from southern Spain and their paleoenvironmental implications
Fig. 5. ESEM images (all in occlusal view) of murids from Lower Pleistocene, Barranco de los Conejos, Guadix-Baza Basin, Spain.. A–D. Apodemus atavus Heller, 1936. A. Right M1, IPHES-BC-11. B. Left M1, IPHES-BC-5. C. Right m1, IPHES-BC-6. D. Left m1, IPHES-BC-13. E–O. Castillomys gracilis Weerd, 1976. E. Right M1, IPHES-BC-1. F. Right M1, IPHES-BC-2. G. Left M1, IPHES-BC-15. H. Left M1, IPHES-BC-16. I. Right M2, IPHES-BC-20. J. Left M3, IPHES-BC-19. K. Left m1, IPHES-BC-7. L. Left m1, IPHES-BC-9. M. Right m2, IPHES-BC-8. N. Right m2, IPHES-BC-10. O. Right m2, IPHES-BC-21.
Fig. 4 in Evidence for parallel development of ever-growing molars in Early Pleistocene rodents from southern Spain and their paleoenvironmental implications
Fig. 4. ESEM images (all in occlusal view) of Tibericola vandermeuleni (Agustí, 1992), from Lower Pleistocene, Barranco de los Conejos, Guadix-Baza Basin, Spain. A. Right m1, IPHES-BC-135. B. Right m1, IPHES-BC-34. C. Right m1, holotype, IPHES-BC-36. D. Right m1, IPHES-BC-114. E. Right m1, IPHES-BC-115. F. Right m1, IPHES-BC-116. G. Left m1, IPHES-BC-29. H. Left m1, IPHES-BC-40. I. Left m1 (the posterior lobe is missing), IPHES-BC-136. J. Right M3, IPHES-BC-141. K. Right M3 (part of the posterior lobe is missing), IPHES-BC-142. L. Left M3, IPHES-BC-121. M. Right M3, IPHES-BC-140.
Fig. 1 in Evidence for parallel development of ever-growing molars in Early Pleistocene rodents from southern Spain and their paleoenvironmental implications
Fig. 1. Nomenclature and measurements of arvicoline molars. A, B. Left m1 of Manchenomys (nomenclature (A) and measurements (B). C. Right M3 of Manchenomys. Abbreviations: A, ACC length; AC2, anteroconid cap; AL1, anterior lobe; B, shortest distance between BRA3 and LRA4; BRA, buccal re-entrant angle; BSA, buccal salient angle; C, shortest distance between LRA3 and BRA3; L, occlusal surface length; LRA, lingual re-entrant angle; LSA, lingual salient angle; PC, posterior cap; PL, posterior lobe; T1–T7, triangles 1–7; W, width.
Fig. 3 in Evidence for parallel development of ever-growing molars in Early Pleistocene rodents from southern Spain and their paleoenvironmental implications
Fig. 3. ESEM images (all in occlusal view) of Manchenomys oswaldoreigi (Agustí, Castillo, and Galobart, 1993), from Lower Pleistocene, Barranco de los Conejos, Guadix-Baza Basin, Spain. A. Left m1, IPHES-BC-28. B. Left m1, IPHES-BC-33. C. Right m1 (the posterior lobe is missing), IPHES-BC-38. D. Left M3, IPHES-BC-145.
Fig. 2 in Evidence for parallel development of ever-growing molars in Early Pleistocene rodents from southern Spain and their paleoenvironmental implications
Fig. 2. ESEM images (all in occlusal view, except A2, B2, C) of Early Pleistocene arvicolines from Spain. A–G. Orcemys giberti Martin, Tesakov, Agustí, and Johnston, 2018, from Barranco de los Conejos, Guadix-Baza Basin. A. Left m1 in occlusal (A1) and lateral (A2) views, holotype, IPHES-BC-30. B. Right m1 in occlusal (B1) and lateral (B2) views, IPHESA-BC-118. C. Right m1 in basal view, IPHES-BC-31. D. Right M2, IPHES-BC-32. E. Right M2, IPHES-BC-117. F. Right M3, IPHES-BC-120. G. Posterior fragment of right M3, IPHES-BC-119. H. Mimomys sp. from Cortijo de Don Alfonso, Guadix-Baza Basin; left m1, IPHES-CDA-01. I. Mimomys sp. from Cementerio de Orce, Guadix-Baza Basin; anterior fragment of right m1, IPHES- CO-B-01. J–L. Mimomys medasensis Michaux, 1971, from Almenara-Casablanca 1, eastern Spain. J. Left m1, IPHESA-ACB-1-CS-4. K. Left m1, IPHESA-ACB-1-CS-3. L. Left m1, IPHESA-ACB-1-CS-5. The white arrows indicate the mimomyan ridge.
Fig. 12 in A comparison of teeth in Tithonian, Late Jurassic, predatory actinopterygian fishes from Owadów-Brzezinki Lägerstatte and its palaeoecological implications
Fig. 12. Comparison of generalized teeth vertical cross sections of the studied taxa. A. Caturoidea. B. Pachycormidae. Not to scale.
Fig. 8 in A comparison of teeth in Tithonian, Late Jurassic, predatory actinopterygian fishes from Owadów-Brzezinki Lägerstatte and its palaeoecological implications
Fig. 8. SEM overview of tooth of caturoid fish Strobilodus sp. ZPAL P. 16/O-B/2 from Tithonian, Upper Jurassic Kcynia Formation, Corbulomima Limestone (Unit III), Owadów-Brzezinki, Poland. A. Mid-crown section with visible layer of enameloid (en). B. Basal section with exposed orthodentin (ort). C, D. Overview in apical-mid-crown surface. E–H. Changes in enameloid structure from linear through irregular to scale-like in basal direction.
Fig. 5 in A comparison of teeth in Tithonian, Late Jurassic, predatory actinopterygian fishes from Owadów-Brzezinki Lägerstatte and its palaeoecological implications
Fig. 5. Vertical cross-section of tooth of pachycormid fish Orthocormus teyleri Lambers, 1988, NG/PAL/VERT/OB/O1 thin section from ZPAL P. 16/OB/3 from Tithonian, Upper Jurassic Kcynia Formation, Corbulomima Limestone (Unit III), Owadów-Brzezinki, Poland. Basal (A1), mid-crown (A2), and apical (A3) planes, with visible acrodin cap. Internal structure (A4), with visible denteonal canals (white arrows) and inter-denteonal dentin (black arrows).
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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.