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Text-fig. 5. Original material of Peziza sulphurea (syntype L 910,261-594), the substrate and schema with location of six apothecia and two fragments of apothecia. Apothecia marked with numbers 1–3 were examined microscopically. in A Revision Of Trichopeziza Lizonii, T. Sulphurea And T. Violascens (Ascomycota, Helotiales) From The Herbarium Prm With Notes On Type Material Of Peziza Sulphurea

Text-fig. 5. Original material of Peziza sulphurea (syntype L 910,261-594), the substrate and schema with location of six apothecia and two fragments of apothecia. Apothecia marked with numbers 1–3 were examined microscopically.

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Text-fig. 3. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. Above: assumed fragments of legs as seen in body cavity of holotype (Aa – in dorsal view, Ab – in ventral view) and paratype (B, only dorsal view available). Below: speculative reconstruction of legs, assumed segments leg IV in above rows (numbers 1, 3, 5, 7, 12, 13, 14), assumed segments of leg I below (numbers 6, 9, 10). Rest of the segments assumed to belong to legs II and III. Only trochanters III (nr. 8) and IV (nr. 7, 12) undoubtedly belonging to the new species. Bars indicating 50 µm, numbers indicate identity of segments. in Oribatid Mite Fossils From Quaternary And Pre-Quaternary Sediments In Slovenian Caves I.Two New Genera And Two New Species Of The Family Oppiidae From The Early Pleistocene

Text-fig. 3. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. Above: assumed fragments of legs as seen in body cavity of holotype (Aa – in dorsal view, Ab – in ventral view) and paratype (B, only dorsal view available). Below: speculative reconstruction of legs, assumed segments leg IV in above rows (numbers 1, 3, 5, 7, 12, 13, 14), assumed segments of leg I below (numbers 6, 9, 10). Rest of the segments assumed to belong to legs II and III. Only trochanters III (nr. 8) and IV (nr. 7, 12) undoubtedly belonging to the new species. Bars indicating 50 µm, numbers indicate identity of segments.

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Text-fig. 1. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. A – dorsal view of holotype (prodorsal setae largely missing except right lamellar seta, notogastral setae missing and their insertions not discernable); B – ventral view of holotype (genital and anal valves missing, only insertions of ventral setae visible, gnathosoma missing); C – lateral view of paratype (notogaster missing). Bar indicates 100 µm. For explanation of acronyms see page 31. in Oribatid Mite Fossils From Quaternary And Pre-Quaternary Sediments In Slovenian Caves I.Two New Genera And Two New Species Of The Family Oppiidae From The Early Pleistocene

Text-fig. 1. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. A – dorsal view of holotype (prodorsal setae largely missing except right lamellar seta, notogastral setae missing and their insertions not discernable); B – ventral view of holotype (genital and anal valves missing, only insertions of ventral setae visible, gnathosoma missing); C – lateral view of paratype (notogaster missing). Bar indicates 100 µm. For explanation of acronyms see page 31.

Fig. 10 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 10 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan (a) and Mandegan (all others) sections, Zagros Zone, SW Iran. a–c, h Oblique equatorial sections. d, f–g Equatorial sections. e Equatorial section of an uncoiling specimen. Thin-sections: NG 197-2 (a), Rt 72 (b), Rt 79 (c), Rt 113 (d, f–h), Rt 98 (e).

Fig. 12 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 12 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Mandegan (a, g, i–j) and Naghan sections (all others), Zagros Zone, SW Iran. a–e, h–i Oblique sections; note the rounded outline of the network in a and b. f Tangential section; note the rounded subepidermal network (lower part). g Almost centered axial section, holotype specimen. j Juvenile specimen showing protoconch connected to the following chamber (?deuteroconch) by numerous openings. Abbreviations: b = beam, p = proloculus, d? = possible deuteroconch, f = foramen, r = rafter, s = septum. Thin-sections: Rt 87 (a), NG 198 (b), 2NG 120-1 (c), 2NG 144 (d), 2NG 113 (e), 2NG 200-1 (f), Rt 113 (SNSB-BSPG 2016 V 16) (g), 2NG 200-1 (h), Rt 113-1 (i), Rt 72 (j).

Fig. 9 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 9 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Mandegan (a, e, g) and Naghan sections (all others), Zagros Zone, SW Iran. a–b Equatorial sections. c–d, g Oblique equatorial sections; note tendency to uncoil in the youngest chambers. e–f Oblique equatorial sections of uncoiling specimens. Abbreviations: p = proloculus, d = possible deuteroconch, f = foramen, s = septum. Thin-sections: Rt 113 (a, g), 2NG 191 (b), 2NG 186 (c), 2NG 49 (d), Rt 87-1 (e), NG 196 (f).

Fig. 8 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 8 Schematic drawing showing differences in the wall structure of Persiella n. gen. and Pseudocyclammina Yokoyama (without scale).

Fig. 7 Flabelloperforata tarburensis n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 7 Flabelloperforata tarburensis n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a Oblique section showing multiple foramina. b Detail from a showing pseudo-keriotheka-like wall structure. c Oblique section. d, e Details (d from c) showing multiple foramina. f Oblique section. Thin-sections: 2NG 8 (a–b), 2NG 86 (c–e), 2NGN (f). Scale bars: a–b = 0.2 mm, c, f = 1 mm, d–e = 0.3 mm.

Fig. 6 Flabelloperforata tarburensis n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 6 Flabelloperforata tarburensis n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a–e, g–l: Oblique sections; holotype specimen in a; multiple foramina depicted in i and k with arrows. f Oblique equatorial section. T: Tarburina zagrosiana Schlagintweit, Rashidi & Barani. m Slightly oblique subaxial section. Arrow: multiple foramina. Thin-sections: NG 85-2 (a), 2NG 81-2 (b), 2NG 85-1 (c), 2NG 83 (d), 2NG 84-1 (e, h), NG 49 (f), 2NG 81-4 (g), NG 83-2 (i), NG 81 (j), NG 61 (k), 2NG 87-2 (l), 2NG 197 (m).

Fig. 1 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 1 Lithostratigraphy of Upper Cretaceous strata of the Zagros Zone (redrawn from the Stratigraphic Chart of Iran, Geological Society of Iran, 1995).

Fig. 5 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 5 Neobalkhania bignoti Cherchi, Radoičić & Schroeder from the upper Maastrichtian of the Tarbur Formation of the Mandegan (a), and Naghan sections (all others). a Subaxial section of a large specimen (diameter ~7 mm). b Axial section of a megalospheric specimen. c Four specimens in (sub)axial sections, and Dicyclina sp. (D). d Tangential section showing subepidermal network with coarse primary partitions (right below) and finer secondary partitions (left below). e Oblique axial section of a megalospheric specimen. f Fragmentary equatorial section, P = Persiacyclammina maastrichtiana Schlagintweit & Rashidi. g Oblique section of a megalospheric specimen showing large embryo with opening to the second annular chamber. Scale bars: a–b, d, f–g = 0.3 mm; C, E = 0.6 mm. Thin-sections: Rt 113 (a), 2NG 109 (b), 2NG 128 (c), 2NG 201-1 (d), 2NG 120 (e), 2NG 81 (f–g).

Fig. 3 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 3 Typical microfacies of samples with Flabelloperforata tarburensis n. gen., n. sp (F in a–b), and Persiella pseudolituus n. gen., n. sp. (Ps in c–d), from the upper Maastrichtian Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a–b Wackestones/packstones with benthic foraminifera, among many porcelaneous and agglutinating taxa such as Dicyclina sp. (Di), Tarburina zagrosiana Schlagintweit, Rashidi & Barani (T), Dictyoconus bakhtiari Schlagintweit, Rashidi & Babadipour (D) and remains of dasycladalean algae (d in b). c Wackestone with small and larger benthic foraminifera and oblique longitudinal section of the dasycladale Pseudocymopolia cf. anadyomenea (Elliott) (P). d Grainstone/packstone with Omphalocyclus macroporus Lamarck (O), Dictyoconella? minima Henson (Dic), and slightly oblique axial section of Persiella pseudolituus n. gen., n. sp. (Ps). Thin-sections: 2NG 81-4 (a), 2NG 120 (b), 2NG 166 (c), 2NG 177 (d).

Fig. 2 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran

Fig. 2 Location of the Naghan and Mandegan sections, the type localities of Flabelloperforata tarburensis n. sp., and Persiella pseudolituus n. gen., n. sp. (taken from google maps)

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Fig. 6 in Biozonation And Correlation Of Two Wells In Niger Delta Using Calcareous Nannofossils

Fig. 6 Correlation of the MAY-01 and MAY-02 wells based on calcareous nannofossil zones, MFS and SB.

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Fig. 2 in Biozonation And Correlation Of Two Wells In Niger Delta Using Calcareous Nannofossils

Fig. 2 Stratigraphy and paleoenvironment of the Eocene-Pliocene interval of the Niger Delta (modified from Doust & Omatsola, 1990)

Fig. 5 in Disentangling Leucocytozoon parasite diversity in the neotropics: Descriptions of two new species and shortcomings of molecular diagnostics for leucocytozoids

Fig. 5. (A) A Bayesian phylogenetic hypothesis of Leucocytozoon species constructed only with partial mitochondrial genomes (5485 bp excluding gaps) and (B) partial cytb gene sequences of leucocytozoids. Branch colors indicate the parasite morphology, with green branches representing parasites in fusiform host cells, and blue branches correspond to a species that develops in roundish host cells. Notice that, since parasite mitochondrial genomes (mtDNA) corresponding to the partial cytb fragments of the MH909275 and MH909276 sequences could not be amplified, they were not included in the phylogenetic hypothesis constructed with mtDNA (Fig. 5A). (For interpretation of the references to color in this figure legend, the reader is referred to the Web version of this article.)

Fig. 2 in Disentangling Leucocytozoon parasite diversity in the neotropics: Descriptions of two new species and shortcomings of molecular diagnostics for leucocytozoids

Fig. 2. Leucocytozoon neotropicalis sp. nov. from the peripheral blood of its type vertebrate host Greenand-black Fruiteater (Pipreola riefferii) captured at Los Nevados NNP, Colombia. Macrogametocytes (A–E) and microgametocytes (F–I). Black arrows () indicate the deformed host cell nuclei. Parasite nuclei are indicated by white arrow () and nucleoli are shown by double white arrowtips (). Volutin granules are indicated by double black arrowtips () and vacuoles – by white arrowtips (). Uneven cytoplasmic processes may acquire a ribbon-like appearance (asterisk *). Giemsa-stained thin blood films. Scale bar = 10 μm. (For interpretation of the references to color in this figure legend, the reader is referred to the Web version of this article.)

Fig. 3 in Host biology and environmental variables differentially predict flea abundances for two rodent hosts in a plague-relevant system

Fig. 3. Cumulative distribution plots divided by year for (A) T. alpinus and (B) T. speciosus. For each species 2013 is shown in red, 2014 in teal, 2015 in pink. The x-axis represents each host individual, ordered from least to most flea infested, and the y-axis shows the cumulative proportion of total flea counts. The dotted line indicates individuals in the 90th percentile of flea abundances, illustrating that the top 10% most infected chipmunks usually account for close to 50% of all counted fleas. The proportion of individuals without fleas in each year is represented graphically as the proportion at which each colored line departs from the x-axis. (For interpretation of the references to color in this figure legend, the reader is referred to the Web version of this article.)

Fig. 4 in Host biology and environmental variables differentially predict flea abundances for two rodent hosts in a plague-relevant system

Fig. 4. Relationships between fecal glucocorticoid metabolite levels, sex, and flea abundance for (A) T. alpinus and (B) T. speciosus. Points show the mean ± S.E. number of fleas counted for female (white) and male (black) individuals within FGM categories (FGM values were rounded to the nearest 10). Lines of best fit (based on all raw data points) ± 95% confidence intervals are overlaid for each sex.

Fig. 2 in Host biology and environmental variables differentially predict flea abundances for two rodent hosts in a plague-relevant system

Fig. 2. Patterns of flea abundance across years, hosts, and flea species. Overall average flea abundances (A–B) and abundances of each flea species (C–D) in each year for T. alpinus (A, C) and T. speciosus (B, D). Abundances of each flea species on hosts of each sex (Males: closed circles, Females: open circles) on T. alpinus (E) and T. speciosus (F).