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Fig. 6 in The Alvarez impact theory of mass extinction; limits to its applicability and the "great expectations syndrome"

Fig. 6. The Late Triassic cratering record plotted against extinction events (based on Lucas and Tanner 2008: fig. 8; crater dates modified after Schmieder and Buchner 2008 and Martin Schmieder personal communication, 2011) and two alternative time scales. Note that the 100 km−sized and precisely dated Manicouagan crater (214.56±0.05 Ma; see ottawa−rasc.ca/wiki/index.php?title=Odale−Articles− Manicouagan) is within the age range of the end−Carnian extinction only in the ICS 2009 geochronologic scheme (see also Lucas et al. 2012). Carbon isotope events compiled from Tanner (2010) and Ruhl and Kürschner (2011: fig.1). Vertical lines correspond to possible temporal ranges. J., Jurassic.

Fig. 5 in Short-term survival of ammonites in New Jersey after the end-Cretaceous bolide impact

Fig. 5. Ammonite aptychi (= jaws) in the matrix of the Burrowed Unit. A, D. Lower jaws attributed to Eubaculites. A. AMNH 69496, right valve. D. AMNH 69492, view of right valve (D1), close−up of aptychus at the anterior end (D2). B, C. Lower jaws attributed to Discoscaphites. B. AMNH 69497, left valve. C. AMNH 69498, left valve.

Fig. 4 in Short-term survival of ammonites in New Jersey after the end-Cretaceous bolide impact

Fig. 4. Clay pods in the matrix of the Burrowed Unit adjacent to burrows, Monmouth County, New Jersey, probably reworked from the Pinna Layer, and piped down into the Burrowed Unit. A–D. Single pod adjacent to a burrow. A. Overview. B. Eubaculites latecarinatus (Brunnschweiler, 1966), AMNH 66312 in left lateral view (B1); whorl cross−section at adoral end showing a specimen of Eubaculites telescoped inside (B2). C. Heteropora americana Richards, 1962, AMNH 51309; without any sediment in the zooids. D. Eubaculites sp., hollow specimen, AMNH 66313; view of hollow chambers (D1), close−up of septum (D2). E. Eubaculites sp. in another clay pod adjacent to a burrow, AMNH 66314; septal face (E1), close−up of septal neck (E2).

Fig. 1 in Short-term survival of ammonites in New Jersey after the end-Cretaceous bolide impact

Fig. 1. Stratigraphic section in the Manasquan River Basin, Monmouth County, New Jersey. A. The top of the Tinton Formation consists of the Pinna Layer overlain by the Burrowed Unit, which is overlain, in turn, by the Hornerstown Formation. An enriched concentration of iridium occurs at the base of the Pinna Layer (indicated by the stars). The position of the Cretaceous/Paleogene boundary in this figure is based on the assumption that the enriched concentration of iridium is in place. B. Iridium profile from two sites (represented by the solid and dashed lines) in the Manasquan River Basin (Landman et al. 2007a). C. Map of part of New Jersey showing localities mentioned in the text: 1, Manasquan River Basin; 2, Buck's Pit; 3, Ivanhoe Creek.

Fig. 10 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 10. Bar graphs showing the ratio of life stages and sexes in each sample. A- Procamallanus (Procamallanus) pseudolaeviconchus Moravec and van As, 2015. B- Paracamallanus cyathopharynx (Baylis, 1923). Prevalence of each group in each month is given in the line graphs. F = female, M = male, L = larvae, US = unknown sex.

Fig. 8 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 8. Lateral view of isolated buccal capsules of Paracamallanus specimens, morphotypes A and B. (i). Brightfield. (ii). Epifluorescence [Filter-set 09 (Ex. 470/40)]. (iii). SEM. 1 = anterior part of posterior capsule; 2 = posterior part of posterior capsule; t = trident; ellipse = elliptical shape of capsule; rectangle = rectangular shape of capsule.

Fig. 9 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 9. Principal Component Analyses (PCA) of Paracamallanus morphometry collected from Clarias gariepinus (Burchell, 1822). A- PCA using morphometric ratios for both males and females. B- PCA using buccal capsule ratios for both males and females. Each parasite is indicated as a dot, with the fill, shape and colour corresponding to morphotype and lineage (refer to key). F = female; M = male.

Fig. 5 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 5. Scanning electron micrographs of male Paracamallanus cyathopharynx (Baylis, 1923) from Clarias gariepinus (Burchell, 1822). A-posterior end, ventrolateral view, arrows show precloacal papillae; Bposterior end, ventral view, solid arrow shows right spicule, dashed arrow shows pair of adcloacal papillae, double arrows show postcloacal papillae; Cisolated right spicule, ventrolateral view, arrow shows shaft; D-right spicule tip, dorsal view; E– right spicule tip, ventral view, arrow shows ventral barb; Fisolated left spicule.

Fig. 3 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 3. Scanning electron micrographs of Procamallanus (Procamallanus) pseudolaeviconchus Moravec and van As, 2015 from Clarias gariepinus (Burchell, 1822). A-postequatorial region of female, vulva, ventral view; B- vulva, lateral view, arrows show lips; C- first-stage larva exiting vulva; D-posterior end of male, ventral view, solid arrows show pre-cloacal papillae, dashed arrows show post-cloacal papillae, circles show adcloacal papillae; D(i)- pedunculate papilla; E– isolated right spicule, lateral view, solid arrow shows shaft, dashed arrow shows spicule tip; E (i)- right spicule tip, arrow shows velum; F- posterior end of male, ventrolateral view, arrow shows right spicule; G-isolated left spicule, lateral view; G(i)- left spicule tip, arrow shows velum.

Fig. 2 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 2. Scanning electron micrographs of Procamallanus (Procamallanus) pseudolaeviconchus Moravec and van As, 2015 from Clarias gariepinus (Burchell, 1822). A-anterior end, lateral view; B- anterior end, apical view, solid arrow shows smooth peribuccal flange, dashed arrow shows marginal elevation; Cisolated buccal capsule, lateral view, arrow shows oesophagus; D-isolated buccal capsule, apical view, solid arrows show marginal elevations; E– buccal capsule interior, apical view, dashed arrow shows narrow ring, solid arrow shows basal ring; F- microdissected buccal capsule, lateral view, dashed arrow shows narrow ring, solid arrow shows basal ring; Ganterior region, lateral view, arrow shows excretory pore; G(i)- excretory pore, lateral view; H- lateral deirid, lateral view; I- lateral deirid, apical view. a = amphid; s = submedian papilla.

Fig. 7 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 7. Phylogram of Camallanidae based on CO1 mtDNA, with Spirocerca lupi (Rudolphi, 1809) as the outgroup. Procamallanus data and Paracamallanus lineage one (LI1) and two (LI2) from the present study are indicated in purple, orange and green, respectively. Nodal support presented for Bayesian inference and Maximum Likelihood approaches (BI/ML), with support lower than 0.75/75% excluded and support above 0.9/90% indicated by an asterisk (*).

Fig. 6 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 6. Phylogram of Camallanidae based on 18S rDNA, with Spirocerca lupi (Rudolphi, 1809) as the outgroup. Procamallanus and Paracamallanus data from the present study are indicated in purple and orange, respectively. Nodal support presented for Bayesian inference and Maximum Likelihood approaches (BI/ML), with support lower than 0.75/75% excluded and support above 0.9/90% indicated by an asterisk (*).

Fig. 4 in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 4. Scanning electron micrographs of Paracamallanus cyathopharynx (Baylis, 1923) from Clarias gariepinus (Burchell, 1822). A-anterior end, apical view; B- anterior end, apical view, arrow shows oesophagus; C- isolated buccal capsule, lateral view, arrow shows oesophagus; C(i)- isolated buccal capsule, lateral view, double arrow shows isthmus; D-microdissected anterior buccal capsule, ventral view of longitudinal ridges. E- lateral view of deirid; F, G, G(i)- posterior end of female, apical view, digit-like processes. a = amphid; s = submedian papilla; sc = sclerotised plate; t = trident; 1 = anterior buccal capsule; 2 = anterior part of posterior buccal capsule; 3 = posterior part of buccal capsule.

Fig. 1 in Epidemiology of Trichinella infection in wild boar from Spain and its impact on human health during the period 2006-2019

Fig. 1. Prevalence of Trichinella infection in wild boar from several Spanish autonomous communities.

Fig. 1. Maps indicating the sampling locality within South Africa. A in Camallanid nematodes from Clarias gariepinus (Burchell, 1822) in the Crocodile River, Gauteng, South Africa: Exploring diversity and divergence in an acid-mine drainage impacted environment

Fig. 1. Maps indicating the sampling locality within South Africa. A- Map of Africa. B- Map of South Africa; red square highlighting area of interest. C- Map of Crocodile River flowing from Lake Heritage (sampling site) to Hartbeespoort Dam further downstream.

Fig. 4 in Epidemiology of Trichinella infection in wild boar from Spain and its impact on human health during the period 2006-2019

Fig. 4. Box-plot and post hoc pairwise comparison via Dunn's test of the incidence. Box-plot with different letters indicate a statistically significant difference.

Fig. 3 in Epidemiology of Trichinella infection in wild boar from Spain and its impact on human health during the period 2006-2019

Fig. 3. Three-dimensional plots for the interaction effects of the total number of wild boars hunted and the prevalence of the Trichinella infection in wild boar on incidence of trichinellosis in humans.

opencc-by-4.0Aug 2022View details →

Fig. 1 in The impact of mass-flowering crops on bee pathogen dynamics

Fig. 1. Chronological trend (1961–2019) of the global land area (ha) used for crops; red: almonds; ochre: rapeseed; green: seed cotton; light blue: soybeans; dark blue: sunflower; purple: the sum of 5 MFCs with biggest global land area used in 2019 (see Table 1); data from the Food and Agriculture Organization of the United Nations (2021). (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)

opencc-by-4.0Apr 2022View details →

Fig. 4 in Habitat associations and impacts on a juvenile fish host by a temperate gnathiid isopod

Fig. 4. Significant abiotic parameters (lunar illumination and wave height) vs. gnathiid density per trap. Lines represent negative binomial linear regressions with standard error margins.