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Figure 7 in Preliminary study on Acropora (Scleractinia: Astrocoeniina: Acroporidae) of the Persian Gulf, with emphasis on the north and northeastern areas

Figure 7. Acropora mossambica: a) portion of colony; b) top view of plate; c) portion of branch; d) SEM micrograph showing terminal part of branch; e) SEM micrograph showing close up view of radial corallites; f) SEM micrograph showing coenosteum on radial corallite; g) top view of axial corallite; h) SEM micrograph showing coenosteum between radial corallites.

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Figure 6 in Preliminary study on Acropora (Scleractinia: Astrocoeniina: Acroporidae) of the Persian Gulf, with emphasis on the north and northeastern areas

Figure 6. Acropora arabensis: a) live colony, note the distinct white branch tips; b) portion of the colony; c) portion of branch; d) SEM micrograph showing close up view of radial corallites; e) SEM micrograph showing broken costae ornamentation on radial corallite; f) top view of axial corallite; g) SEM micrograph showing coenosteum between radial corallites.

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Figure 3 in Preliminary study on Acropora (Scleractinia: Astrocoeniina: Acroporidae) of the Persian Gulf, with emphasis on the north and northeastern areas

Figure 3. Acropora aspera: a) portion of colony; b) portion of branch; c) SEM micrograph showing terminal part of branch; d) SEM micrograph from lateral view of radial corallites, note the gutter-shaped appearances formed by the outer walls; e) SEM micrograph showing coenosteum on a radial corallite; f) top view of axial corallite showing extent of primary and secondary septa; g) SEM micrograph showing coenosteum between radial corallites.

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Text-fig. 4. Dendrogram (Ward's method, squared Euclidean distance) showing the relationship between the studied fossil vegetation assemblages of Hrádek/N. (48), Wackersdorf (49), Berzdorf and Wiesa (50) and the Mydlovary Fm. (51) and the studied modern vegetation units from SE China and Japan (Teodoridis et al. 2011a, 2012, Appendix – this volume). 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. 4. Dendrogram (Ward's method, squared Euclidean distance) showing the relationship between the studied fossil vegetation assemblages of Hrádek/N. (48), Wackersdorf (49), Berzdorf and Wiesa (50) and the Mydlovary Fm. (51) and the studied modern vegetation units from SE China and Japan (Teodoridis et al. 2011a, 2012, Appendix – this volume).

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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).

Fig. 9 Drumul lui Lehman. a in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 9 Drumul lui Lehman. a The stratigraphic contact between the Valanginian limestones and the monomictic Aptian breccia (marked by white line). b Detail from the contact area. c, d Monomictic breccia. 567, 620 = sample numbers. Scale bar for c and d = 2 cm.

Fig. 8 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 8 Microfossils from the Aptian breccia and conglomerate pebbles in the Padinile Frumoase area. a-c, f, g Unidentified orbitolinids. d Rectodyctioconus giganteus Schroeder. e Mesorbitolina parva (Douglass). h Unidentified?involutinid foraminifer. i Montsalevia salevensis (Charollais, Brönnimann & Zaninetti). j unidentified biserial foraminifer. k Pfenderina neocomiensis (Pfender). l Palorbitolina lenticularis (Blumenbach); m Terebella lapilloides Münster. n Neomeris cretacea Steinmann. o Griphoporella sp. p Carpathoporella occidentalis Dragastan. q Clypeina parasolkani Farinacci & Radoičić. r Lithocodium aggregatum Elliott. s Coscinophragma cribrosa (Reuss). a, b, sample 266; c, e, m, n, p, s, sample 271; d, i, j, k, q, r, sample 275; f, h, o, sample 279; g, sample 272; l, sample 568. Scale bar = 1 mm (a-c, f); 0.5 mm (d, e, g, h, o, q); 0.25 mm (i-m, p).

Fig. 7 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 7 Facies and microfacies from the upper Valanginian (a-b) and Aptian (c-h). a-b Bioclastic intraclastic floatstone. Intraclasts consist of peloidal packstone with echinoderms (a1, b1), bioclastic packstone with sponge spicules and coral fragments (a2), and peloidal packstone with small foraminifera (b2). The matrix (m) contains calpionellids and calcispheres. The arrows in a are delineating the shape of the intraclasts. c Limestone-rich breccia. Clasts are embedded in a micritic/clay-rich matrix that contains silt-sized quartz. The matrix contains orbitolinids (indicated by the small yellow arrows). d Marly clast with bioclasts and glauconite. e Coral-rich bioconstruction with dissolved corals. f Clast containing abundant sponge and Lithocodium crusts (center). In the upper right corner the carbonate components of the clast are dissolved. g Clasts from an orbitolinid-rich peloidal bioclastic grainstone; orbitolinids are present both in the matrix and the clasts. h Clast composed of an orbitolinid/green algae-bearing packstone (left) and clast that contains peloidal fenestral wackestone (right) (detail from photo g). a, b, sample 258; c-f, sample 266; g, h, sample 272. Scale

Fig. 6 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 6 Microfossils from the lower Valanginian limestones and the upper Valanginian limestones/marly-limestones. a-c Pseudocyclammina lituus (Yokoyama); d Coscinoconus cf. cherchiae (Arnaud-Vanneau, Boisseau & Darsac); e-j Montsalevia salevensis (Charollais, Brönnimann & Zaninetti); k-o Meandrospira favrei (Charollais, Brönnimann & Zaninetti); p-s Unidentified calpionellids; t, u Cadosina fusca Wanner; v, w Crustocadosina semiradiata Wanner; x, y Stomiosphaera echinata Nowak. a, h, sample 12817; b, i, sample 256; c, d, sample 257; e, sample 260; f, g, p, u, sample 12818; j, x, y, sample 249; k, r, sample 252; l,q, v, w, sample 12816; m, n, o, s, t, sample 258. Scale bar = 0.5 mm (a-b); 0.25 mm (c-o); 0.125 mm (p-y).

Fig. 3 Padinile Frumoase outcrop a in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 3 Padinile Frumoase outcrop a The lower Valanginian-upper Valanginian unconformity (yellow line) and the transgressive contact between the Valanginian limestones and the Aptian deposits (breccia and conglomerates) (white line). b Monomictic breccia. c The first outcrop located above the contact area (~3m). d Monomictic orthoconglomerates with common carbonate pebbles. e Monomictic paraconglomerates with carbonate pebbles. 272, 280, 291 = sample numbers. Scale bar for b, d, e = 2 cm.

Fig. 5 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 5 Lower Valanginian limestones and upper Valanginian limestones/marly-limestones (enlargement view of the left area in Fig. 3a). a The unconformity between the lower Valanginian limestones and upper Valanginian limestones/marly limestones (yellow line). The thin-bedded upper Valanginian carbonate beds are lying over thick-bedded shallow-water lower Valanginian limestones. b Bioclastic intraclastic grainstone; note the presence of dissolution structures filled with vadous silt. c Peloidal bioclastic packstone with dissolution structures. d Bioclastic wackestone passing to a peloidal bioclastic packstone. e, f Peloidal bioclastic packstone, with sintaxial overgrowth cement being developed on the echinoderm plates. g Peloidal bioclastic packstone/grainstone with Lithocodium nodules. b, c, sample 12817; d, e, sample 12816; f, sample 11827; g, sample 12819. Scale bar = 1 mm (b-g).

Fig. 10 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 10 Microfacies and microfossils identified in the limestone pebbles of the Aptian breccia and conglomerates from the Drumul lui Lehman section. a Bioclastic intraclastic floatstone with intraclasts of bioclastic wackestone; the matrix contains orbitolinids, echinoderm plates and silt-sized quartz extraclast. b Intraclasts composed of fenestral wackestone and peloidal fenestral grainstone. c Pebbles originating form reefal bioconstructions. The corals are encrusted by microproblematic organisms. d Rudist fragment and sponges (chaetetids). e Pebble consisting of a peloidal bioclastic packstone with?Vercorsella sp. (indicated by the arrows). f Carbonate pebble with dissolution structures; cavities are bordered by fine crystalline, schalenoedric cements. The interior is filled with clay minerals and iron oxides. g Pebble consisting of a peloidal fenestral packstone; the fenestral structures are filled with vadous silt and sediment derived from the breccia's matrix. h Intensely dissolved carbonate clasts; the clasts and the cavities are bordered by fine crystalline, schalenoedric cement. a,

Fig. 1 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 1 Location of the Aptian deposits on the geological map of the northern part of the Piatra Craiului Massif [based on the maps 1:50000, sheets110a to 110d (Dimitrescu et al., 1971; Patrulius et al., 1971; Săndulescu et al., 1972; Dimitrescu et al., 1974), redrawn with minor changes]

Fig. 2 in A review of sarcoptic mange in North American wildlife

Fig. 2. Microscopic lesions of a bear with sarcoptic mange. (A) Close-up view of hyperkeratotic and crusted skin showing a mite tunnel. (B) Histological section with cross-section of S. scabiei within the epidermis. (Asterisks: mite tunnels; arrowheads: epidermis; arrow pointing to S. scabiei).

Fig. 1 in A review of sarcoptic mange in North American wildlife

Fig. 1. Life stages of S. scabiei. Top left: Egg; Top middle: Larva; Top right: Protonymph; Bottom left: Tritonymph; Bottom middle: Adult Male; Bottom right: Adult Female.

Fig. 4 in A community analysis approach to parasite transmission in multi-host systems: Assemblages of small mammal prey and Echinococcus multilocularis in an urban area in North America

Fig. 4. Map showing the geographic distribution of three small mammal assemblage types predicted for the City of Calgary area by a multinomial logistic regression (MLR) model associating the environmental variables to assemblage types, developed from data collected in 2012 and 2013 (Liccioli et al., 2014). Note how large portion of BWM and NHP were classified as assemblage 1 as expected, but also large portion of FCPP, where it was not expected.

Fig. 1 in A community analysis approach to parasite transmission in multi-host systems: Assemblages of small mammal prey and Echinococcus multilocularis in an urban area in North America

Fig. 1. Study sites for the characterization of the small mammal assemblages in urban Calgary, AB, Canada in 2012–2013, showing the location of five areas in Urban Calgary and detailed map of Bowmont, Southland Lowlands, and Weaselhead. Bowmont (BM), Fishcreek Provincial Park (FCPP), Nose Hill Park (NHP), Southland Lowlands (SL), and Weaselhead (WSH).

Fig. 2 in A community analysis approach to parasite transmission in multi-host systems: Assemblages of small mammal prey and Echinococcus multilocularis in an urban area in North America

Fig. 2. Dendrograms derived from the Bray-Curtis similarity of small mammal assemblages in five parks and natural areas in urban Calgary, AB, Canada, 2012–2013. a) Dendrogram using abundance data and group-average clustering algorithm. The dashed line indicates the cluster cut-off line of 45% similarity. Symbols for each site indicate the prevalence of definitive hosts (EmDH) and presence (1) or absence (0) of infected small mammals (EmIH). b) Dendrogram using abundance data and complete-linkage clustering algorithm. Note how it is similar to the dendrogram using group-average algorithm. c) Dendrogram using proportion data and group-average clustering algorithm. Note how all BM sites are in single cluster and all NHP sites and most sites are in another cluster, similar to the dendrogram using abundance data.

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Figure 4 in New record of an oyster species from Chilika Lagoon, Odisha, north-western Bay of Bengal

Figure 4. Ligament area, hinge dentition and white layer showing layer of mother pearl in I. ephippium.