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BRAIN Journal-A Repeated Signal Difference for Recognising Patterns-Figure 2. Schematic of the same neuron N1, shared between 2 different patterns P1 and P2.
<p>It can be assumed that only one pattern fires during each time unit, where Rule 1 of the Introduction states that if a neuron fires a stronger signal for a pattern, it sends feedback to ask it to fire again, the next time unit. If it fires a weaker signal, the request is not to fire next time. Stronger and weaker relates to a more variable type of on or off. As the mechanism is not final yet, there could be some flexibility with it. Rule 1 also states that if the neuron does not fire for the current pattern, it receives the switch command from the last pattern it did fire for. Note that the actual firing event can produce either zero or some input and so an earlier event can also force a weak feedback signal. Rule 2 states that this particular feedback is only the on/off switch command and does not affect the size of the output value. A schematic of the idea is illustrated in Figure 2, which relates to the same neuron shared between 2 pattern events, at times t1 and t2. The schematic is described further in section 0. </p>
Data, analysis scripts, simulations, and schematics files for "Position Sensitive Alpha Detector for an Associate Particle Imaging System"
<p>Measured data and analysis script, as well as, simulated data, input scripts, as well as, schematics for the readout board for our publication "Position Sensitive Alpha Detector for an Associate Particle Imaging System"</p>
Icepack schematic
<p>Column based physical processes that affect the area and volume of sea ice, which are represented or accounted for within the Icepack software package.</p>
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified). in A Review Of The Early Miocene Mastixioid Flora Of The Kristina Mine At Hrádek Nad Nisou In North Bohemia (The Czech Republic)
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified).
Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided) in A Late Upper Palaeolithic Skull From Moča (The Slovak Republic) In The Context Of Central Europe
Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided)
Text-fig. 3. Schematic section through the Żyttawa (Zittau) Basin, on the Czech and Polish boundary; Hrádek n. Nisou and Turów parts of the basin. Explanation of the symbols. 1 – Overlying strata with the upper coal seam, 2 – middle and lower strata with the coal seam (Miocene), 3 – first sedimentary setting with basal coal seam (Miocene / Oligocene), 4 – alcalic volcanism (Tertiary), 5 – Upper Cretaceous deposits, 6 - underlying rocks of the basin. (Adapted after Václ 1967, Václ and Čadek, 1962, modified). in Some Monocot Pollen Taxa From The Lower Miocene Basal Coaly Deposits Of The Czech And Polish Parts Of The Żytawa (Zittau) Basin
Text-fig. 3. Schematic section through the Żyttawa (Zittau) Basin, on the Czech and Polish boundary; Hrádek n. Nisou and Turów parts of the basin. Explanation of the symbols. 1 – Overlying strata with the upper coal seam, 2 – middle and lower strata with the coal seam (Miocene), 3 – first sedimentary setting with basal coal seam (Miocene / Oligocene), 4 – alcalic volcanism (Tertiary), 5 – Upper Cretaceous deposits, 6 - underlying rocks of the basin. (Adapted after Václ 1967, Václ and Čadek, 1962, modified).
Fig. 2. Schematic drawing showing measured parameters and descriptive terminology used for sclerite types A–H in Trachyplax arctica, a new multiplated problematic fossil from the lower Cambrian of North Greenland
Fig. 2. Schematic drawing showing measured parameters and descriptive terminology used for sclerite types A–H. Abbreviations: A, apical angle; Ai, apex interarea; L, length; Lr, length of rostrum; Ls, length of shield; H, height; W, width; Wai, width of apex interarea; Wr, width of rostrum; Ws, width of shield. Not to scale.
Рис. 1. Схематическое ΑеΛение АзербайΑжана: ZQ, SH, KU, AP – БоΛьшой Кавказ; AR – Куро-Араксинская низменность; GN, KB, NH – МаΛый Кавказ; LK – ТаΛыш (вкΛючая ЗуванΑ и Αенкоранскую низменность). Fig. 1. Schematic division of Azerbaijan:ZQ, SH, KU, AP – the Greater Caucasus; AR – the Kura-Aras lowland; GN, KB, NH – the Lesser Caucasus; LK – Talysh (including Zuvand and the Lenkoran lowland). in The fauna of lamellicorn beetles (Coleoptera: Scarabaeoidea) of Azerbaijan
Рис. 1. Схематическое ΑеΛение АзербайΑжана: ZQ, SH, KU, AP – БоΛьшой Кавказ; AR – Куро-Араксинская низменность; GN, KB, NH – МаΛый Кавказ; LK – ТаΛыш (вкΛючая ЗуванΑ и Αенкоранскую низменность). Fig. 1. Schematic division of Azerbaijan:ZQ, SH, KU, AP – the Greater Caucasus; AR – the Kura-Aras lowland; GN, KB, NH – the Lesser Caucasus; LK – Talysh (including Zuvand and the Lenkoran lowland).
FIGURE 2. Schematic showing hypothesized flow patterns within the hydrospire folds. 2.1 in Visualizing the fluid flow through the complex skeletonized respiratory structures of a blastoid echinoderm
FIGURE 2. Schematic showing hypothesized flow patterns within the hydrospire folds. 2.1, In Hypothesis 1, the flow has an adoral component representing respiratory leakage. 2.2, In Hypothesis 2, the flow is entirely radial, without leakage. See text for further discussion.
Fig.. 3. Simocyon batalleri, MNCN B−3458, Batallones−1, Madrid Province, Spain, cranium in left lateral view. A. Photograph. B. Schematic drawing showing the main anatomical features of this view (artwork by M. Antón). in Ailurid carnivoran mammal Simocyon from the late Miocene of Spain and the systematics of the genus
Fig.. 3. Simocyon batalleri, MNCN B−3458, Batallones−1, Madrid Province, Spain, cranium in left lateral view. A. Photograph. B. Schematic drawing showing the main anatomical features of this view (artwork by M. Antón).
Figure 9. Schematic 3D in Morphology and spatial constraints in a dorso-ventrally flattened skull, with a revised species description of Platyallabes tihoni (Poll, 1944)
Figure 9. Schematic 3D reconstruction of the lower jaw-suspensorium articulation area. (a) Overview of the lower jaw, suspensorium and part of skull at level of articulation with suspensorium. Solid lower jaw indicates closed mouth, transparent lower jaw indicates open mouth. Black arrow shows displacement of lower jaw according to the black axis indicated at the jaw articulation. The grey arrows indicate the movements of the lower jaw halves if they were rotated along the grey axis at the articulation. (b) Detail from a postero-ventral view of the lower jaw articulation, showing the two rotation axis: black rod represents the axis which allows a proper mouth opening, grey rod represents the axis of rotation which has shifted together with the suspensorium. Rotation along the black axis results in the medial position of the retroarticular process; with respect to the suspensorium (transparent lower jaw indicates the closed mouth, solid lower jaw the open mouth).
Fig. 33. a, b. Hortipes architelones, new species. a. Vulva, ventral view. b. Vulva, schematic representation. c, d. Hortipes bosmansi, new species. c. Vulva, ventral view. d. Vulva, schematic representation. e, f. Hortipes sceptrum, new species. e. Vulva, ventral view. f in Hortipes, A Huge Genus Of Tiny Afrotropical Spiders (Araneae, Liocranidae)
Fig. 33. a, b. Hortipes architelones, new species. a. Vulva, ventral view. b. Vulva, schematic representation. c, d. Hortipes bosmansi, new species. c. Vulva, ventral view. d. Vulva, schematic representation. e, f. Hortipes sceptrum, new species. e. Vulva, ventral view. f. Vulva, schematic representation. Scale line: 0.1 mm.
Fig. 26. a, b. Hortipes lejeunei, new species. a. Vulva, ventral view. b. Vulva, schematic representation. c in Hortipes, A Huge Genus Of Tiny Afrotropical Spiders (Araneae, Liocranidae)
Fig. 26. a, b. Hortipes lejeunei, new species. a. Vulva, ventral view. b. Vulva, schematic representation. c. Hortipes chrysothemis, new species, vulva, ventral view. d. Hortipes angariopsis, new species, vulva, ventral view. e. Hortipes puylaerti, new species, vulva, ventral view. f. Hortipes machaeropolion, new species, vulva, ventral view. Arrow indicates ID entrance. Scale line: 0.1 mm.
Fig. 29. a, b. Hortipes centralis, new species. a. Vulva, ventral view. b. Vulva, schematic representation. c in Hortipes, A Huge Genus Of Tiny Afrotropical Spiders (Araneae, Liocranidae)
Fig. 29. a, b. Hortipes centralis, new species. a. Vulva, ventral view. b. Vulva, schematic representation. c. Hortipes robertus, new species, vulva, ventral view. Arrow indicates gland associated with widened portion of ID. d. Hortipes abucoletus, new species, vulva, ventral view. Arrow indicates gland associated with widened portion of ID. e–g. Hortipes tarachodes, new species. e, f. Vulva, left half, ventral and dorsal views. g. Vulva, left half, schematic representation. Scale line: 0.1 mm.
Fig. 8. Hortipes genitalia, labeled schematics. a. H in Hortipes, A Huge Genus Of Tiny Afrotropical Spiders (Araneae, Liocranidae)
Fig. 8. Hortipes genitalia, labeled schematics. a. H. falcatus, new species, ventral view of vulva, left half. b. H. silvarum Ledoux and Emerit, ventral view of vulva, right half. c. H. falcatus, new species, male palp, ventral view. d. H. machaeropolion, new species, male palp, retrolateral view.
Text-fig. 1. Location of Ivanovce Pliocene primate site in Slovakia within the wider area of the Carpathians-Pannonian Basin (white circle). The northern wall of the former limestone quarry at Ivanovce near Trenčín in western Slovakia. Several karst fillings provided a rich early Pliocene vertebrate assemblage. a: schematic sketch of the site showing the location of different karst fillings, b: photo of the same site during the palaeontological research in 1960s. in Allosorex Stenodus Fejfar, 1966 (Eulipotyphla, Soricidae): Re-Description Of Type Material And Re-Interpretation Of Its Fossil Record
Text-fig. 1. Location of Ivanovce Pliocene primate site in Slovakia within the wider area of the Carpathians-Pannonian Basin (white circle). The northern wall of the former limestone quarry at Ivanovce near Trenčín in western Slovakia. Several karst fillings provided a rich early Pliocene vertebrate assemblage. a: schematic sketch of the site showing the location of different karst fillings, b: photo of the same site during the palaeontological research in 1960s.
Text-fig. 2. Field photograph of the sampling locality, together with a schematic profile. Stratigraphic horizon from which the fossil wood fragment was extracted (white arrow) (Modified from Pires and Da Rosa 2000). in A New Fossil Fabaceae Wood From The Pleistocene Touro Passo Formation Of Rio Grande Do Sul, Brazil
Text-fig. 2. Field photograph of the sampling locality, together with a schematic profile. Stratigraphic horizon from which the fossil wood fragment was extracted (white arrow) (Modified from Pires and Da Rosa 2000).
Text-fig. 1. Schematic drawing, demonstrating the basic endoskeletal elements of the craniate head. Sclerotomic derivatives red and pharyngoqualar derivatives yellow. b: basal pharyngoqualar segment; c: ceratal pharyngoqualar segment; ct: cartilago teniformis (blue); e: epal pharyngoqualar segment; gr: gill rays; h: hypal pharyngoqualar segment; la: lower arcual element; lt: laterotectal element; mt: mediotectal element; n: notochord (green); s: summital pharyngoqualar segment; t: telical pharyngoqualar segment; ua: upper arcual element. in Cartilago Teniformis And Its Derivatives: Additional Information On The Basic Composition And Evolution Of The Skull
Text-fig. 1. Schematic drawing, demonstrating the basic endoskeletal elements of the craniate head. Sclerotomic derivatives red and pharyngoqualar derivatives yellow. b: basal pharyngoqualar segment; c: ceratal pharyngoqualar segment; ct: cartilago teniformis (blue); e: epal pharyngoqualar segment; gr: gill rays; h: hypal pharyngoqualar segment; la: lower arcual element; lt: laterotectal element; mt: mediotectal element; n: notochord (green); s: summital pharyngoqualar segment; t: telical pharyngoqualar segment; ua: upper arcual element.
Text-fig. 6. Comparative analysis of the three genera (Prynadaeopteris RADCZ., Geperapteris S.V.MEYEN, Tumidopteris NAUGOLNYKH) with possible affinity to Gleicheniaceae from the Permian deposits of Angaraland. a–c: Tumidopteris NAUGOLNYKH; d–f: Prynadaeopteris RADCZ. (based on Radczenko 1955, 1956, Naugolnykh 2013); g–i: Geperapteris S.V.MEYEN (based on Meyen 1982, Naugolnykh 2013). Left column – sori in plan (frontal view); central column – leaves; right column – sori in cross-section; FL – flattened sori; HS – hemispherical sori. Scale 1 cm (b, h), 5 mm (e), 1 mm (a, d), 0.5 mm (g); c, f, i – figures schematically drawn without scale. in A New Species Of The Genus Tumidopteris Naugolnykh From The Permian Of The Pechora Cis-Urals, Russia
Text-fig. 6. Comparative analysis of the three genera (Prynadaeopteris RADCZ., Geperapteris S.V.MEYEN, Tumidopteris NAUGOLNYKH) with possible affinity to Gleicheniaceae from the Permian deposits of Angaraland. a–c: Tumidopteris NAUGOLNYKH; d–f: Prynadaeopteris RADCZ. (based on Radczenko 1955, 1956, Naugolnykh 2013); g–i: Geperapteris S.V.MEYEN (based on Meyen 1982, Naugolnykh 2013). Left column – sori in plan (frontal view); central column – leaves; right column – sori in cross-section; FL – flattened sori; HS – hemispherical sori. Scale 1 cm (b, h), 5 mm (e), 1 mm (a, d), 0.5 mm (g); c, f, i – figures schematically drawn without scale.
Text-fig. 3. Schematic position of the human modifications (cut marks, impact marks, ochre traces, inserted bones) recognised on the canid remains from Předmostí, indicated on a wolf skeleton; the frequencies of the modifications are not shown. Modified after © 2003 ArcheoZoo.org / Michel Coutureau (Inrap). in Consumption Of Canid Meat At The Gravettian Předmostí Site, The Czech Republic
Text-fig. 3. Schematic position of the human modifications (cut marks, impact marks, ochre traces, inserted bones) recognised on the canid remains from Předmostí, indicated on a wolf skeleton; the frequencies of the modifications are not shown. Modified after © 2003 ArcheoZoo.org / Michel Coutureau (Inrap).
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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.
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DANDI Archive for NWB datasets
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International Brain Laboratory public data
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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.