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Asymmetric dark matter may alter the evolution of very low-mass stars and brown dwarfs
<p>MESA inlists and data files for "<a href="https://ui.adsabs.harvard.edu/?#abs/2011PhRvD..84j1302Z">Asymmetric dark matter may alter the evolution of very low-mass stars and brown dwarfs</a>"</p>
First Results from ABRACADABRA-10 cm: A Search for Sub-$\mu$eV Axion Dark Matter — 2018 Data
<p>Extracted limits from the Axion Dark Matter search associated with the article: <em>First Results from ABRACADABRA-10 cm: A Search for Sub-μeV Axion Dark Matter </em>(To be published in Phys. Rev. Lett. 2019)</p>
Casting about in the Dark - Artifact Evaluation
<p>Companion dataset artifact used in the paper "Casting about in the Dark".</p> <p>This version incorporates some additional minor changes to the artifact, related to the additionally sampled cast instances. This version is the one used in the final version of the paper.</p> <p>---</p> <p>Abstract:</p> <p>The main goal of a static type system is to prevent certain kinds of errors from happening at run time. A type system is formulated as a set of constraints that gives any expression or term in a program a well-defined type. Yet mainstream programming languages are endowed with type systems that provide the means to circumvent their constraints through <em>casting</em>.</p> <p>We want to understand how and when developers escape the static type system to use dynamic typing. We empirically study how casting is used by developers in more than seven thousand Java projects. We find that casts are widely used (8.7% of methods contain at least one cast) and that 50% of casts we inspected are not guarded locally to ensure against potential run-time errors.</p> <p>To help us better categorize use cases and thus understand how casts are used in practice, we identify 25 cast-usage patterns, recurrent programming idioms using casts to solve a specific issue. This knowledge can be: (a) a recommendation for current and future language designers to make informed decisions (b) a reference for tool builders, <em>e.g.</em>,<br> by providing more precise or new refactoring analyses, (c) a guide for researchers to test new language features, or to carry out controlled programming experiments, and (d) a guide for developers for better practices.</p>
Figures 5–10 in Scopaeus saotomensis spec. nov., a flightless rove beetle from the Island of São Tomé (Coleoptera: Staphylinidae: Paederinae: Lathrobiini) - Isolation and adaptation in a dark, humid, tropical forest environment
Figures 5–10. Scopaeus saotomensis, holotype, República Democrática de São Tomé e Príncipe, São Tomé, Lagoa Amelia; aedeagus in lateral (5), ventral (6), dorsal (7) view; abdominal sternite VII (8); abdominal sternite VIII in ventral (9) and lateral (10) view. Abbreviations: dl – distal lobes (apical lobes and dorsal lobe not distinguishable), f – flagellum, ll – lateral lobes, mf – median foramen, mtf – median tooth of flagellum, p – parameres, sl – groups of setae of lateral lobes, sp – setae of phallobase, vdl – ventrodextral, lobiform enlargement of distal lobes, vl – ventral lobe.
Figure 1 in Scopaeus saotomensis spec. nov., a flightless rove beetle from the Island of São Tomé (Coleoptera: Staphylinidae: Paederinae: Lathrobiini) - Isolation and adaptation in a dark, humid, tropical forest environment
Figure 1. Habitus of Scopaeus saotomensis, holotype, República Democrática de São Tomé e Príncipe, São Tomé, Lagoa Amelia.
Figures 2–4 in Scopaeus saotomensis spec. nov., a flightless rove beetle from the Island of São Tomé (Coleoptera: Staphylinidae: Paederinae: Lathrobiini) - Isolation and adaptation in a dark, humid, tropical forest environment
Figures 2–4. Scopaeus saotomensis, lateral aspect exhibiting basal depressions of abdominal tergites (upper arrows), basal constrictions of abdominal sternites (lower arrows), and stridular file on dorsolateral surface of metaventrite (2); enlarged view of stridular file (3); plectral ridges on posterior surface of base of mesothoracic leg (4).
Fig. 5 in Argulus coregoni (Crustacea: Branchiura: Argulidae) Parasitic on a Dark Chub Nipponocypris temminckii (Cypriniformes: Xenocyprididae) in a Stream, Central Japan, with a List of Its Known Hosts in East Asia
Fig. 5. Argulus coregoni, adult male, NSMT-Cr 31596. A, Habitus, fresh specimen, dorsal view; B, C, habitus, ethanol-preserved specimen, dorsal and ventral views, respectively. The specimen was fixed in 70% ethanol on 21 September 2021 and photographed on 20 July 2022. Scale bars: 1 mm.
Fig. 4 in Argulus coregoni (Crustacea: Branchiura: Argulidae) Parasitic on a Dark Chub Nipponocypris temminckii (Cypriniformes: Xenocyprididae) in a Stream, Central Japan, with a List of Its Known Hosts in East Asia
Fig. 4. Argulus coregoni, adult male, NSMT-Cr 31596. A, First leg, ventral view; B, distal part of endopod of first leg, ventral view; C, second leg, ventral view; D, coxa of second leg, ventral view; E, third leg, ventral view; F, coxa, base, and part of exopod of third leg, dorsal view; G, fourth leg, ventral view, H, base (with peg) and part of endopod of fourth leg, anteroventral view. Scale bars: A, C, E, G, 0.3 mm; B, D, F, H, 0.1 mm.
Fig. 2 in Argulus coregoni (Crustacea: Branchiura: Argulidae) Parasitic on a Dark Chub Nipponocypris temminckii (Cypriniformes: Xenocyprididae) in a Stream, Central Japan, with a List of Its Known Hosts in East Asia
Fig. 2. Argulus coregoni, adult male, NSMT-Cr 31596. A, Habitus, dorsal view; B, habitus, ventral view. Scale bar: 1 mm.
Fig. 1. Argulus coregoni and its collection site. A in Argulus coregoni (Crustacea: Branchiura: Argulidae) Parasitic on a Dark Chub Nipponocypris temminckii (Cypriniformes: Xenocyprididae) in a Stream, Central Japan, with a List of Its Known Hosts in East Asia
Fig. 1. Argulus coregoni and its collection site. A, Middle reaches of the Takase River where dark chub were collected; B, a dark chub (ca. 70 mm total length) infected with an adult male of A. coregoni (arrowhead) on the dorsal body surface at the boundary between the head and trunk. Scale bar: 5 mm.
Text-fig. 4. Platanaceae 1–3. Macginitiea gracilis (LESQUEREUX) J. WOLFE et WEHR leaves and associated reproductive structures 1. Holotype of Aralia gracilis LESQUEREUX from Bridger Pass, Wyoming, USNM 330. 2. Specimen showing the typical configuration of five lobes, Killpecker Creek flora, Wyoming. UF 18126-13242. 3. Silicified M. gracilis leaf from Almont, North Dakota; arrow indicates adjacent Macginicarpa infructescence, UF 15722-29202a. 4. Macginicarpa infructescence from Almont, UF15722-35493. 5. Platananthus sp., Almont, UF 15722-62019. 6. Macginicarpa glabra MANCHESTER infructescence, enlarged from fig. 3, UF 15722-29202b. Specimens in figs 3-6 collected and donated by John Curtis. Scales = 1 cm. Images 3–6 light-dark inverted. in Revisions To Roland Brown'S North American Paleocene Flora
Text-fig. 4. Platanaceae 1–3. Macginitiea gracilis (LESQUEREUX) J. WOLFE et WEHR leaves and associated reproductive structures 1. Holotype of Aralia gracilis LESQUEREUX from Bridger Pass, Wyoming, USNM 330. 2. Specimen showing the typical configuration of five lobes, Killpecker Creek flora, Wyoming. UF 18126-13242. 3. Silicified M. gracilis leaf from Almont, North Dakota; arrow indicates adjacent Macginicarpa infructescence, UF 15722-29202a. 4. Macginicarpa infructescence from Almont, UF15722-35493. 5. Platananthus sp., Almont, UF 15722-62019. 6. Macginicarpa glabra MANCHESTER infructescence, enlarged from fig. 3, UF 15722-29202b. Specimens in figs 3-6 collected and donated by John Curtis. Scales = 1 cm. Images 3–6 light-dark inverted.
Text-fig. 3. 1, 2. Ensete goldianum (LESQUEREUX) comb. nov, Holotype, USNM 494, Golden Colorado. 1. Numerous seeds on a slab. 2. Detail of seed molds and casts. 3-5 "Sagittaria" megasperma R. W. BROWN. 3. Infructescence head. USNM 167488, lectotype selected by Watt 1971. 4. Isolated fruit showing veins of wing, and longitudinally striate central body and single style, USNM 313282, 5. Additional isolated fruit, USNM 313283. Images 4, 5 light-dark inverted. Scale = 1 cm. in Revisions To Roland Brown'S North American Paleocene Flora
Text-fig. 3. 1, 2. Ensete goldianum (LESQUEREUX) comb. nov, Holotype, USNM 494, Golden Colorado. 1. Numerous seeds on a slab. 2. Detail of seed molds and casts. 3-5 "Sagittaria" megasperma R. W. BROWN. 3. Infructescence head. USNM 167488, lectotype selected by Watt 1971. 4. Isolated fruit showing veins of wing, and longitudinally striate central body and single style, USNM 313282, 5. Additional isolated fruit, USNM 313283. Images 4, 5 light-dark inverted. Scale = 1 cm.
Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011). in Feather Palm Foliage From The Messinian Of Italy (Capo Di Fiume, Palena And Pollenzo Near Alba) Within The Framework Of Northern Mediterranean Late Miocene Flora
Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011).
Text-fig. 2: Microscopic photo of the wood from Kučlín (specimen No. G 4723, NM, transverse section) shoving growth ring boundary with markedly rounded tracheids and abundant axial parenchyma (dark cells) present both in late- and earlywood (scale bar = 100 µm). in Silicified Stem From The Late Eocene Fossil Locality Of Kučlín (Czech Republic): Overview And New Remarks
Text-fig. 2: Microscopic photo of the wood from Kučlín (specimen No. G 4723, NM, transverse section) shoving growth ring boundary with markedly rounded tracheids and abundant axial parenchyma (dark cells) present both in late- and earlywood (scale bar = 100 µm).
Text-fig. 8. Basalts, agglomerates and coarse tuffs (dark) and plant-bearing coarse tuffaceous sandstones with fossil plants (light) on the Nitusi Cape, Siziman locality. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)
Text-fig. 8. Basalts, agglomerates and coarse tuffs (dark) and plant-bearing coarse tuffaceous sandstones with fossil plants (light) on the Nitusi Cape, Siziman locality.
Text-fig. 3 Pollen diagram from the locality of Bohutín. 0-0.01 m – sandy soil mixed with humus, slightly clayey, sample B11; 0.05 m – grey-blue strongly sandy clay, sample B10; 0.10-0.25 m – brown-grey sandy clay with plant remains and mixed with a small amount of peat, sample B9, sample B8 (0.15 m), sample B7 (0.20 m), sample B6 (0.25 m); 0.30-0.35 m – dark sandy clay mixed with peat and plant remains, sample B5, sample B4 (0.35 m); 0.40 m – grey strongly sandy clay mixed with peat, sample B3; 0.45-0.50 m – grey-blue strongly sandy clay, sample B2, sample B1 (0.50 m). in Reconstruction Of Vegetation Development On The Floodplain Of The Litavka River In The Holocene (Central Bohemia, Brdy Mts.)
Text-fig. 3 Pollen diagram from the locality of Bohutín. 0-0.01 m – sandy soil mixed with humus, slightly clayey, sample B11; 0.05 m – grey-blue strongly sandy clay, sample B10; 0.10-0.25 m – brown-grey sandy clay with plant remains and mixed with a small amount of peat, sample B9, sample B8 (0.15 m), sample B7 (0.20 m), sample B6 (0.25 m); 0.30-0.35 m – dark sandy clay mixed with peat and plant remains, sample B5, sample B4 (0.35 m); 0.40 m – grey strongly sandy clay mixed with peat, sample B3; 0.45-0.50 m – grey-blue strongly sandy clay, sample B2, sample B1 (0.50 m).
Figure 2 in Scarabs in the dark: occurrence of Scarabaeoidea beetles (Insecta: Coleoptera) in Brazilian caves
Figure 2. Proportion of Scarabaeoidea families sampled in Brazilian caves. Numbers inside the figure represent the species numbers in each Scarabaeoidea family.
Figure 1 in Scarabs in the dark: occurrence of Scarabaeoidea beetles (Insecta: Coleoptera) in Brazilian caves
Figure 1. Some Scarabaeoidea beetle species and the localization where they are found in Brazilian caves. A) Polynoncus gemmingeri (Trogidae) found in Andrelândia, MG (Quartzite cave); B) Gymnetis pantherina (Cetoniidae) found in Curionópolis, PA (Iron ore cave); C) Agaocnemis pruina (Melolonthidae) found in Carrancas, MG (Quartzite cave); D) Rhinaspis aenea (Melolonthidae) found in Santa Teresa, ES (Granite cave); E) Dichotomius aff. carbonarius (Scarabaeidae) found in Lassance, MG (Limestone cave) and F) Dicrania sp. (Melolonthidae) found in Montalvânia, MG (Limestone cave).
Fig. 3 in Like phoenix from the ashes: How modern baleen whales arose from a fossil "dark age"
Fig. 3. Patterns and potential drivers of the early Miocene "dark age". A. Extinction of toothed mysticetes and eomysticetids at the beginning of the early Miocene "dark age", and subsequent reinvasion of coastal habitats by larger, toothless filter feeding mysticetes during the middle Miocene. The occurrence of eomysticetids in the earliest Miocene is based on a single, fragmentary specimen from New Zealand (Boessenecker and Fordyce 2017b). B. Global oxygen isotope curve, showing the timing of the mid-Miocene Climatic Optimum (Zachos et al. 2008). C. Global sea-level change (Miller et al. 2005). D. Global diatom abundance as derived from Deep-Sea Drilling Programme/Ocean Drilling Programme smear slides (Renaudie 2016). Highlighted events potentially relevant to the "dark age": 1, a 0.5 shift in δ18O; 2, a 40 m sea-level fall; and 3, an early Miocene decrease in global diatom abundance. Reconstructions of mysticetes by Carl Buell.
Fig. 2 in Like phoenix from the ashes: How modern baleen whales arose from a fossil "dark age"
Fig. 2. Comparison of Australasian late Oligocene baleen whale assemblages: south-eastern Australia (A1, B1) and New Zealand (A2, B2). A. Late Oligocene palaeogeographical reconstruction. B. Differences in mysticete assemblage composition. Note the widespread inundation of New Zealand. Dashed lines in A delineate the modern coastline without compensating for late Neogene Alpine Fault movement. Palaeogeographical reconstructions are based on King et al. (1999), King (2000), Holdgate and Gallagher (2003). Drawings of whales by Carl Buell.
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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.