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Dataset of "Synaptic Response of Fluidic Nanopores: The Connection of Potentiation with Hysteresis"

This dataset supports the article published in ChemPhysChem. "Synaptic Response of Fluidic Nanopores: The Connection of Potentiation with Hysteresis"   Raw data for the article "Synaptic Response of Fluidic Nanopores: The Connection of Potentiation with Hysteresis". For further details see the readme.txt file.

Fig. 2 in Influence of habitat connectivity and seasonality on the ichthyofauna structure of a riverine knickzone

Fig. 2. Non-metric multidimensional plots of the abundance of fish assemblage sampled in isolated (I) and connected (C) pools during the rainy and dry season in the Sapucaí-Mirim River knickzone, Southeast Brazil.

Fig. 5 in New brachyuran crabs from the Aptian-Albian Romualdo Formation, Santana Group of Brazil: Evidence for a Tethyan connection to the Araripe Basin

Fig. 5. Brachyura indet. (right cheliped) from the upper Aptian–lower Albian Romualdo Formation of the Santana Group, Araripe Basin, Pernambuco. DGEO-CTG-UFPE-7743, possibly akin to Araripecarcinus ferreirai Martins-Neto, 1987.

Fig. 2 in New brachyuran crabs from the Aptian-Albian Romualdo Formation, Santana Group of Brazil: Evidence for a Tethyan connection to the Araripe Basin

Fig. 2. Stratigraphic sections (A1–D1) and field photographs (A2–D2) of the upper Lower Cretaceous Romualdo Formation, Pernambuco, Brazil, where the new brachyuran crabs were discovered: Arrojado site (A), municipality of Araripina, Zé Gomes (B), Cedro (C), and Santo Antônio (D) sites, municipality of Exu. Scale bars 25 cm.

Fig. 4 in New brachyuran crabs from the Aptian-Albian Romualdo Formation, Santana Group of Brazil: Evidence for a Tethyan connection to the Araripe Basin

Fig. 4.?Eogeryonid brachyuran Romualdocarcinus salesi Prado and Luque gen. et sp. nov. from the upper Aptian–lower Albian Romualdo Formation of the Santana Group, Araripe Basin, Pernambuco, Brazil. A. Holotype DGEO-CTG-UFPE-8122; A1, dorsal view showing the two anterolateral spines, the epibranchial spine, and the outer orbital spine; A2, close-up of rostrum and left orbit showing the inner-, intra-, and outer- orbital spines; A3, inverted colour image of A2, showing the short and wide inner and outer orbital fissures. B. Paratype DGEO-CTG-UFPE-8119; B1, dorsal carapace; B2, inverted colour image of B1 showing the outer orbital spine and the two anterolateral spines. C. Paratype DGEO-CTG-UFPE-8137; C1, dorsal carapace; C2, inverted colour image of C1, showing the anterolateral spines and the short epibranchial spine. D. Paratype DGEO-CTG-UFPE- 8127; D1, SEM image of dorsal carapace; D2, inverted colour image of D1, showing the anterolateral spines and the short epibranchial spine. Abbreviations: as, anterolateral spines; ios, inner orbital spine; iof, innermost orbital fissure; its, intra-orbital spine; oof, outermost orbital fissure; oos, outer orbital spine. All specimens photographed dry and uncoated, except for C1, which was coated with ammonium chloride.

Fig. 1. A in New brachyuran crabs from the Aptian-Albian Romualdo Formation, Santana Group of Brazil: Evidence for a Tethyan connection to the Araripe Basin

Fig. 1. A. Map showing the known occurrences (stars) of orithopsid and eubrachyuran genera in the Early Cretaceous of South America: upper Aptian– lower Albian San Gil Inferior Formation, Boyacá and upper Aptian Paja Formation, Santander, Colombia and upper Aptian–lower Albian Romualdo Formation, Araripe Basin, Brazil. B. Sedimentary basins of northeast Brazil; arrows show the three possible routes of Cretaceous marine ingression into the Araripe Basin. C. New fossiliferous localities (stars) with brachyuran crabs from upper Aptian–lower Albian Romualdo Formation, Araripe Basin, Pernambuco, Brazil (base map modified from Assine 2007).

opencc-by-4.0Sep 2012View details →

Fig. 3 in Boine SnakeBavarioboafrom the Oligocene/Miocene of Eastern Turkey with Comments on Connections Between European and Asiatic Snake Faunas

Fig. 3. Two vertebrae of boine snake Bavarioboa sp. from the Mendikdere Formation, Kurucan, Turkey, Oligocene/Miocene. A. AUNHL IZ100401a, anterior trunk vertebra in right lateral view. B. AUNHL IZ100401b, middle trunk vertebra, in right lateral (B1), ventral (B2), anterior (B3), posterior (B4), and dorsal (B5) views.

opencc-by-4.0Sep 2012View details →

Fig. 1 in Boine SnakeBavarioboafrom the Oligocene/Miocene of Eastern Turkey with Comments on Connections Between European and Asiatic Snake Faunas

Fig. 1. Map of the Eastern Anatolia subbasins, and the location of snake fossil site (modified from Şenel et al. 1984; Bozkurt 2001; Sancay et al. 2006).

Fig. 5 in Connecting Hunter-Schreger Band microstructure to enamel microwear features: New insights from durophagous carnivores

Fig. 5. Box plots of microwear features across HSB categories in p4 (A–D) and m1 (E–H) specimens. Boxes represent inter−quartile ranges, horizontal lines within boxes are medians; vertical lines show upper and lower limits, and asterisks represent outliers. Abbreviations: a, acute−angled undulating HSB; u, undulating HSB; z, zig−zag HSB.

Fig. 1 in Connecting Hunter-Schreger Band microstructure to enamel microwear features: New insights from durophagous carnivores

Fig. 1. Tooth positions examined in the study, shown on a spotted hyena dentary. Black squares indicate the approximate size of the area examined during each trial. Note the exposed areas of dentine on the shear facet of m1; all trials were done on the enamel portion of the teeth only.

Fig. 3 in Connecting Hunter-Schreger Band microstructure to enamel microwear features: New insights from durophagous carnivores

Fig. 3. Method of enamel microstructure analysis. A. Three regions of the tooth crown were examined for Hunter−Schreger Bands (HSB), representing top, middle, and bottom thirds of the crown. One of three types of HSB was recorded for each region. B. Examples of a region with mostly (> 50%) zig−zag HSB. C. Region with acute−angled undulating HSB (note that some zig−zag HSB is also present, e.g., indicated by a dotted circle). D. Undulating HSB.

Fig. 6 in Connecting Hunter-Schreger Band microstructure to enamel microwear features: New insights from durophagous carnivores

Fig. 6. Plots of mean values and 95% confidence intervals for binned HSB categories in p4 (A–D) and m1 (E–H) specimens. Mean values are connected in fossil samples to show trend. Abbreviations: a, acute−angled undulating HSB; u, undulating HSB; z, zig−zag HSB.

Fig. 7 in Connecting Hunter-Schreger Band microstructure to enamel microwear features: New insights from durophagous carnivores

Fig. 7. Intra−dentition evolution of HSB microstructure in fossil Canidae (A) and Hyaenidae (B). Phylogenies for fossil canids based on Wang (1994) and Wang et al. (1999), and for hyaenids based on Werdelin and Solounias (1991). Progressively more derived HSB patterns are indicated by darker shades of grey. Abbreviations: a, acute−angled undulating HSB; u, undulating HSB; z, zig−zag HSB.

Fig. 2 in Connecting Hunter-Schreger Band microstructure to enamel microwear features: New insights from durophagous carnivores

Fig. 2. Examples of microwear features examined. A. Labial (buccal) wear facet on p4 of the extant spotted hyena Crocuta crocuta Erxleben, 1777 (cast of MVZ173771), showing a typical specimen with moderate tooth crown attrition. B. Examples of small (thin) scratches (MVZ173771). C. Examples of large (thick) scratches (C. crocuta, MVZ165179). D. Examples of small pits (Borophagus secundus VanderHoof, 1931, UCMP30479). E. Examples of large pits (C. crocuta, MVZ165160). F. p4 crown surface of the African hunting dog Lycaon pictus Temminck, 1820 (MVZ4842); note paucity of microwear features. Scale bars 1 mm.

opencc-by-4.0Jun 2009View details →

Fig. 1. Right I2 in First Tillodont from India: Additional Evidence for an Early Eocene Faunal Connection between Europe and India?

Fig. 1. Right I2 of esthonychine tillodonts. A. GU/RSR/VAS 1651, cf. Esthonyx sp., from Vastan Mine, in mesial (A1), lingual (A2), and distal (A3) views. B. USNM 533591, Esthonyx spatularius Cope, 1880, early Eocene Willwood Formation (Wasatchian zone Wa−0), Bighorn Basin, Wyoming, in mesial (B1), lingual (B2), and distal (B3) views.

opencc-by-4.0Jun 2009View details →

Fig. 2. Left M3 in First Tillodont from India: Additional Evidence for an Early Eocene Faunal Connection between Europe and India?

Fig. 2. Left M3 of esthonychine tillodonts. A. GU/RSR/VAS 1587, cf. Esthonyx sp., from Vastan Mine. B. USGS 25033, Esthonyx bisulcatus Cope, 1874, early Eocene Willwood Formation (Wasatchian zone Wa−6), Bighorn Basin, Wyoming. C. USNM 510865 (reversed), Esthonyx bisulcatus, early Eocene Willwood Formation (Wasatchian zone Wa−6), Bighorn Basin, Wyoming. Shown at same buccolingual width.

FIGURE 2 in Evidence on the paleodrainage connectivity during Pleistocene: Phylogeography of a hypoptopomatine endemic to southeastern Brazilian coastal drainages

FIGURE 2 | Phylogeny of Hisonotus leucofrenatus samples. A. Cytochrome Oxidase subunit 1; and B. rpS7 ribosomal protein gene intron 1 sequences. Numbers represent posterior probabilities of the respective node. Terminals collapsed into large and well supported group and colors represent paleodrainages according to Fig. 1. In (A) X axis represents time (Ma).

FIGURE 3 in Evidence on the paleodrainage connectivity during Pleistocene: Phylogeography of a hypoptopomatine endemic to southeastern Brazilian coastal drainages

FIGURE 3 | Haplotype network using Median-Joining for only cox1 sequences of Hisonotus leucofrenatus samples. A. Colors represent groups by paleodrainage; and B. Colors represent populations by current drainages. We use upper case in the first word of the noun for drainages (e.g., Tramandaí River system) to differentiate from the homonymous paleodrainages (e.g., tramandaí).

FIGURE 4 in Evidence on the paleodrainage connectivity during Pleistocene: Phylogeography of a hypoptopomatine endemic to southeastern Brazilian coastal drainages

FIGURE 4 | Linear regression plots of the relationship between genetic diversity (mean number of pairwise differences π) and physical characteristics of paleodrainage (contemporary land area, continental shelf area exposed and number of contemporary basins) as described by Thomaz, Knowles, 2018 (S2). A. Contemporary land area (R2 = 0.90); B. Continental shelf area exposed (R2 0.77); C. Number of contemporary basin (R2 = 0.21).

FIGURE 1 in Evidence on the paleodrainage connectivity during Pleistocene: Phylogeography of a hypoptopomatine endemic to southeastern Brazilian coastal drainages

FIGURE 1 | Map of geographic distribution and included samples of Hisonotus leucofrenatus from coastal drainages of southeastern Brazil. Colors of the circles represent groups sampled according limits of paleodrainage systems for the region and sample photo of Hisonotus leucofrenatus from Tramandaí River system, UFRGS 16528 (photo by L. R. Malabarba).