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Text-fig. 3. 1, 2. Ensete goldianum (LESQUEREUX) comb. nov, Holotype, USNM 494, Golden Colorado. 1. Numerous seeds on a slab. 2. Detail of seed molds and casts. 3-5 "Sagittaria" megasperma R. W. BROWN. 3. Infructescence head. USNM 167488, lectotype selected by Watt 1971. 4. Isolated fruit showing veins of wing, and longitudinally striate central body and single style, USNM 313282, 5. Additional isolated fruit, USNM 313283. Images 4, 5 light-dark inverted. Scale = 1 cm. in Revisions To Roland Brown'S North American Paleocene Flora
Text-fig. 3. 1, 2. Ensete goldianum (LESQUEREUX) comb. nov, Holotype, USNM 494, Golden Colorado. 1. Numerous seeds on a slab. 2. Detail of seed molds and casts. 3-5 "Sagittaria" megasperma R. W. BROWN. 3. Infructescence head. USNM 167488, lectotype selected by Watt 1971. 4. Isolated fruit showing veins of wing, and longitudinally striate central body and single style, USNM 313282, 5. Additional isolated fruit, USNM 313283. Images 4, 5 light-dark inverted. Scale = 1 cm.
Text-fig. 2. Cyclurus macrocephalus, scales. a-i – isolated scales: a – specimen IGP 2011/14; b – specimen IGP 2011/22, scale 2; c – specimen IGP 2011/18, scale 2; d – specimen NMP Pc 2868; e – specimen IGP 2011/17; f – specimen NMP Pc 2867; g – specimen IGP 2011/18, scale 3; h – specimen IGP 2011/16; i – specimen IGP 2011/18, scale 1. e-g – scales from the postanal area of the body; i – scale from the lateral line. Head should be in the left. Scale bars represent 1 mm. in Lepidological Review On The Fish Fauna Of The Kučlín Locality (Upper Eocene, Czech Republic)
Text-fig. 2. Cyclurus macrocephalus, scales. a-i – isolated scales: a – specimen IGP 2011/14; b – specimen IGP 2011/22, scale 2; c – specimen IGP 2011/18, scale 2; d – specimen NMP Pc 2868; e – specimen IGP 2011/17; f – specimen NMP Pc 2867; g – specimen IGP 2011/18, scale 3; h – specimen IGP 2011/16; i – specimen IGP 2011/18, scale 1. e-g – scales from the postanal area of the body; i – scale from the lateral line. Head should be in the left. Scale bars represent 1 mm.
Text-fig. 3. Thaumaturus furcatus, scales. a – reconstruction according to Obrhelová (1975); b – specimen NMP Pc 164, scales in situ; c – detail of the postanal part of the specimen NMP Pc 164 with the preserved scale covering. d – specimen NMP Pc 191, scales in situ; e – h isolated scales: e – NMP Pc 185; f – NMP Pc 239, scale 1; g – NMP Pc 239, scale 2; h – NMP Pc 241. Head should be in the left (excluding d). Scale bars represent 5 mm (b, d) 1 mm (c) and 0.5 mm (e-h). in Lepidological Review On The Fish Fauna Of The Kučlín Locality (Upper Eocene, Czech Republic)
Text-fig. 3. Thaumaturus furcatus, scales. a – reconstruction according to Obrhelová (1975); b – specimen NMP Pc 164, scales in situ; c – detail of the postanal part of the specimen NMP Pc 164 with the preserved scale covering. d – specimen NMP Pc 191, scales in situ; e – h isolated scales: e – NMP Pc 185; f – NMP Pc 239, scale 1; g – NMP Pc 239, scale 2; h – NMP Pc 241. Head should be in the left (excluding d). Scale bars represent 5 mm (b, d) 1 mm (c) and 0.5 mm (e-h).
Text-fig. 4. Cyclurus macrocephalus REUSS. Isolated skull bones. Specimen NMP Pc 2848. Dent: dentary; Dpal: dermopalatine; Mx: maxillary; Vo: vomer. [Photograph D. Serrette] in Complements To The Anatomical Knowledge Of Reuss (Pisces, Actinopterygii) From The Eocene Of Kučlín, Bohemia, Czech Republic
Text-fig. 4. Cyclurus macrocephalus REUSS. Isolated skull bones. Specimen NMP Pc 2848. Dent: dentary; Dpal: dermopalatine; Mx: maxillary; Vo: vomer. [Photograph D. Serrette]
Text-fig. 10. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 26. Lateral plates on undersurface of arm segment in Hunsrück Slate articulated specimen. Short thin groove spines on ventral edge of lateral arm plates protect undersurface of vertebra and partially cover ambulacral groove. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 10. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 26. Lateral plates on undersurface of arm segment in Hunsrück Slate articulated specimen. Short thin groove spines on ventral edge of lateral arm plates protect undersurface of vertebra and partially cover ambulacral groove.
Text-fig. 11. Eospondylus cf. primigenius (STÜRTZ) "Prastav" quarry at Praha-Holyně, Třebotov Limestone, Lower Devonian, Dalejan, NM L 36905, x 65. Overlay of proximal and distal articulations. Upper photo is proximal surface with distal bird-like articulation knobs superposed in ink. Lower photo is distal surface with proximal articulation knobs superposed in ink. The architecture of articulation surfaces is both zygospondylous and auluroid. This architecture occurs also in vertebrae of Furcaster and indicates that families Eospondylidae and Furcasteridae are closely related. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 11. Eospondylus cf. primigenius (STÜRTZ) "Prastav" quarry at Praha-Holyně, Třebotov Limestone, Lower Devonian, Dalejan, NM L 36905, x 65. Overlay of proximal and distal articulations. Upper photo is proximal surface with distal bird-like articulation knobs superposed in ink. Lower photo is distal surface with proximal articulation knobs superposed in ink. The architecture of articulation surfaces is both zygospondylous and auluroid. This architecture occurs also in vertebrae of Furcaster and indicates that families Eospondylidae and Furcasteridae are closely related.
Text-fig. 2. Condylopyge cf. rex (BARRANDE, 1846), middle Cambrian, latest Cambrian Stage 5 and lower Drumian, Jince Formation, Příbram-Jince Basin. a. internal mould of isolated cephalon (Specimen CGS CW 17), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. b. latex cast of external mould of isolated pygidium (Specimen CGS FK 63), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. c. internal mould of isolated cephalon (Specimen CGS CW 18), foot of the slope known as Vinice near Jince (locality 20 in Fatka and Kordule 1992) in lower levels of the Onymagnostus hybridus Zone. Condylopyge rex (BARRANDE, 1846), middle Cambrian, lower Drumian, Buchava Formation, Paradoxides (Eccaparadoxides) pusillus Zone, Skryje-Týřovice Basin. d. internal mould of isolated cephalon (NM-L43011a), Karáskovská rokle - nad chatami. e. internal mould of isolated pygidium (NM-L43014), Lůmek u Týřovic. f. internal mould of isolated cephalon (NM-L43013), Lůmek u Týřovic. Whitened with ammonium chloride sublimate. All scale bars are 1 mm. Photographs by Martin Valent (National Museum Prague). in Condylopyge Hawle Et Corda, 1847 In The Příbram-Jince Basin (Barrandian Area, The Czech Republic, Agnostida)
Text-fig. 2. Condylopyge cf. rex (BARRANDE, 1846), middle Cambrian, latest Cambrian Stage 5 and lower Drumian, Jince Formation, Příbram-Jince Basin. a. internal mould of isolated cephalon (Specimen CGS CW 17), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. b. latex cast of external mould of isolated pygidium (Specimen CGS FK 63), Potůček near Rejkovice locality (= locality 12 in Fatka and Kordule 1992) in lower levels of the Paradoxides (Eccaparadoxides) pusillus Zone. c. internal mould of isolated cephalon (Specimen CGS CW 18), foot of the slope known as Vinice near Jince (locality 20 in Fatka and Kordule 1992) in lower levels of the Onymagnostus hybridus Zone. Condylopyge rex (BARRANDE, 1846), middle Cambrian, lower Drumian, Buchava Formation, Paradoxides (Eccaparadoxides) pusillus Zone, Skryje-Týřovice Basin. d. internal mould of isolated cephalon (NM-L43011a), Karáskovská rokle - nad chatami. e. internal mould of isolated pygidium (NM-L43014), Lůmek u Týřovic. f. internal mould of isolated cephalon (NM-L43013), Lůmek u Týřovic. Whitened with ammonium chloride sublimate. All scale bars are 1 mm. Photographs by Martin Valent (National Museum Prague).
Text-fig. 7B. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, BMNH E3358, x 4. Hunsrück Slate articulated specimen. Underside of arm showing two contrasting appearances of lateral arm plates in a single arm. The arm is rolled slightly. Of the left lateral arm plates the lateral surface is extensively exposed. The spine ridge faces distally (posteriorly). Of the right lateral arm plates only the ventral edge that borders the ambulacral groove is exposed. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 7B. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, BMNH E3358, x 4. Hunsrück Slate articulated specimen. Underside of arm showing two contrasting appearances of lateral arm plates in a single arm. The arm is rolled slightly. Of the left lateral arm plates the lateral surface is extensively exposed. The spine ridge faces distally (posteriorly). Of the right lateral arm plates only the ventral edge that borders the ambulacral groove is exposed.
Text-fig. 8. Eospondylus cf. primigenius (STÜRTZ) "Červený lom" quarry near Praha-Klukovice, Loděnice Limestone, Lower Devonian, Pragian, NM L 36910, x 25. Left lateral plate, outer view. The surface leading to the vertical ridge flairs outward. The height profile leaves uncovered part of the side of the arm vertebra. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 8. Eospondylus cf. primigenius (STÜRTZ) "Červený lom" quarry near Praha-Klukovice, Loděnice Limestone, Lower Devonian, Pragian, NM L 36910, x 25. Left lateral plate, outer view. The surface leading to the vertical ridge flairs outward. The height profile leaves uncovered part of the side of the arm vertebra.
Text-fig. 6. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 12.5. Undersurface of arm segments in Hunsrück Slate articulated specimen. A few lateral plates are displaced and expose details of vertebrae. The canal for radial water vessel is in center of zygosphene knob and zygotreme pit, like spout and funnel. At distal outer edges of vertebrae is cupola for tube feet. There are no under arm plates. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 6. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 12.5. Undersurface of arm segments in Hunsrück Slate articulated specimen. A few lateral plates are displaced and expose details of vertebrae. The canal for radial water vessel is in center of zygosphene knob and zygotreme pit, like spout and funnel. At distal outer edges of vertebrae is cupola for tube feet. There are no under arm plates.
Text-fig. 2. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate,, NM S 4764, x 3. Specimen with ventral arm coiling. The specimen is on its dorsum in slate with all five rays curled ventrally inward toward mouth area on underside of disk. Barely visible are tips of two jaws; slightly exposed are proximal parts of rays in oral view extending outward from disk. The location of abrupt ventral bending of rays is indicated by emergence from slate of five rays in aboral view that point inward toward buried disk. Based on ventral bending of rays and intimate association with crinoids Eospondylus has been interpreted as stratigraphic first occurrence of Order Euryalida, which contains epizoic gorgonocephalid and euryalid basket-stars of modern oceans. This status is rejected using new evidence from isolated vertebrae. [Photo by Alexander Glass]. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 2. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate,, NM S 4764, x 3. Specimen with ventral arm coiling. The specimen is on its dorsum in slate with all five rays curled ventrally inward toward mouth area on underside of disk. Barely visible are tips of two jaws; slightly exposed are proximal parts of rays in oral view extending outward from disk. The location of abrupt ventral bending of rays is indicated by emergence from slate of five rays in aboral view that point inward toward buried disk. Based on ventral bending of rays and intimate association with crinoids Eospondylus has been interpreted as stratigraphic first occurrence of Order Euryalida, which contains epizoic gorgonocephalid and euryalid basket-stars of modern oceans. This status is rejected using new evidence from isolated vertebrae. [Photo by Alexander Glass].
Figure 12 in Morphological, ultrastructural, and molecular identification of a new microsporidian pathogen isolated from Crepidodera aurata (Coleoptera, Chrysomelidae)
Figure 12. Phylogenetic relationships among microsporidium species isolated from different hosts based on SSUrRNA. The tree was constructed by maximum likelihood method using Kimura two-parameter distance and evaluated by 1000 bootstrap replications with the MEGA.6 program. Thelonia contejeani and Thelonia parastaci were used as outgroups in the analysis.
Figure 2 in Inbreeding tolerance in two isolated populations of Harting's vole Microtus hartingi (Rodentia, Arvicolinae)
Figure 2. Odour choice between kin vs. nonkin individuals of the opposite sex in Microtus hartingi populations (%), regarding duration of approaches to odour samples in seconds. Females A) and males B) at the age of 35–40 days; females C) and males D) — at the age of 53–58 days.
Figure 1 in Inbreeding tolerance in two isolated populations of Harting's vole Microtus hartingi (Rodentia, Arvicolinae)
Figure 1. Differences in female aggressive behaviour with deadly outcome in polygynous groups in two populations of M. hartingi voles: O-groups (60–70 days of age), Y-groups (49–52 days of age) and control pairs. CAP analogous groups compared to RP; O-groups and Y-groups compared to each other and to control within populations; sisters compared to nonkin in all groups, by Fisher's exact test
Fig. 1 in Effect of four multiple nucleopolyhedrovirus isolates on the larval mortality and development of Spodoptera exigua (Lepidoptera: Noctuidae): determination of virus production and mean time to death
Fig. 1. Mean time of death calculated for third-instar larvae of Spodoptera exigua. The numbers above the columns indicate the values calculated for 3 replications. The columns headed by the same letter are not significantly different (Weibull analysis, α = 1.96).
Fig. 2 in Evaluation of isolates of entomopathogenic fungi in the genera Metarhizium, Beauveria, and Isaria, and their virulence to Thaumastocoris peregrinus (Hemiptera: Thaumastocoridae)
Fig. 2. Daily mean survival curves for adult Thaumastocoris peregrinus exposed to entomopathogenic fungal isolates of the genera Beauveria, Metarhizium, and Isaria for a period of 10 d. The horizontal dotted line indicates insect mortality of 50%.
Fig. 1 in Evaluation of isolates of entomopathogenic fungi in the genera Metarhizium, Beauveria, and Isaria, and their virulence to Thaumastocoris peregrinus (Hemiptera: Thaumastocoridae)
Fig. 1. Percentage of confirmed mortality of Thaumastocoris peregrinus, treat- ed with suspensions of 1 × 108 conidia per mL of entomopathogenic fungal isolates. Different letters above the bars indicate differences between treatments by Tukey's test (P <0.05). Bars represent the error ± 1 × SEM (df = 100).
Fig. 1 in Isolation of Metarhizium guizhouense and Metarhizium robertsii strains from soil-exposed Amblyomma americanum (Acarina: Ixodidae) from northwest Arkansas, USA
Fig. 1. Metarhizium robertsii (A-C, E) and Metarhizium guizhouense (D, F) from Amblyomma americanum ticks collected from northwest Arkansas (Washington County). (A) Sporulating M. robertsii (Savoy P2AM1/ARSEF 14332) growing on an infected adult male tick. (B) Inset of infected tick showing sporulating conidia in addition to mouthparts and coxal spurs diagnostic of A. americanum. (C, D) Metarhizium robertsii (Savoy P2AM1/ARSEF 14432) and M. guizhouense (West Fork P9N2/ ARSEF 14330), respectively, 10 d old colony on Sabouraud Dextrose Agar (plate diam = 60 mm). (E, F) Conidia of M. robertsii (Savoy P2AM1/ARSEF 14332) and M. guizhouense (West Fork P9N2/ARSEF 14330), respectively, viewed at 200× magnification (scale = 20 µm). Photos: Austin Goldsmith (A, B) and Louela Castrillo (C-F).
Fig. 3 in Isolation of native strains of entomopathogenic fungi from agricultural soils of northeastern Mexico and their virulence on Spodoptera exigua (Lepidoptera: Noctuidae)
Fig. 3. Changes in the metamorphosis of Spodoptera exigua caused by isolates (HEB1, HIB-12) and collection strains (GHA, Ma) of entomopathogenic fungi under laboratory conditions (26 °C, 65 ± 5% RH, 14:10 h [L:D] photoperiod). (A) HEB1 (Beauveria bassiana); (B) GHA (Beauveria bassiana); (C) HIB-12 (Metharizium anisopliae); (D) Ma (Metharizium anisopliae). Lines in the bars indicate the standard error.
Fig. 2 in Isolation of native strains of entomopathogenic fungi from agricultural soils of northeastern Mexico and their virulence on Spodoptera exigua (Lepidoptera: Noctuidae)
Fig. 2. Interruption of the metamorphosis of Spodoptera exigua caused by isolates (HEB1, HIB-12) and collection strains (GHA, Ma) of entomopathogenic fungi under laboratory conditions (26 °C, 65 ± 5% RH, 14:10 h [L:D] photoperiod). Lines in the bars indicate the standard error.
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