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Text-fig. 1. Photograph of the studied outcrop with wide bedding planes on the Loděnice – vinice above the topmost step of the vineyard. in Early Complex Tiering Pattern: Upper Ordovician, Barrandian Area, The Czech Republic

Text-fig. 1. Photograph of the studied outcrop with wide bedding planes on the Loděnice – vinice above the topmost step of the vineyard.

Text-fig. 9. a: Arenicolites isp., BK 13, Layer No. 6; b–f: Bifungites isp., a set of specimens showing variability in chamber shape, b – field photograph, Layer No. 23, c – field photograph, Layer No. 23, d – field photograph, Layer No. 23, e – parallel-orientated specimens, field photograph, Layer No. 23, f – field photograph, Layer No. 23; g: Didymaulichnus isp., convex epirelief, field photograph, Layer No. 1. Scale bar = 1 cm. in Early Complex Tiering Pattern: Upper Ordovician, Barrandian Area, The Czech Republic

Text-fig. 9. a: Arenicolites isp., BK 13, Layer No. 6; b–f: Bifungites isp., a set of specimens showing variability in chamber shape, b – field photograph, Layer No. 23, c – field photograph, Layer No. 23, d – field photograph, Layer No. 23, e – parallel-orientated specimens, field photograph, Layer No. 23, f – field photograph, Layer No. 23; g: Didymaulichnus isp., convex epirelief, field photograph, Layer No. 1. Scale bar = 1 cm.

Text-fig. 8. a, b: Bifungites isp. with fragments of vertical shafts, a – concave hyporelief BK 20, Layer No. 26, b – full relief BK 33, Layer No. 23; c–e: Palaeophycus sulcatus (MILLER et DYER, 1878), c – BK 29, Layer No. 22, d – BK 18, Layer No. 16, e – BK 31, Layer No. 6; f: Palaeophycus cf. tubularis HALL, 1847, BK 25, Layer No. 22; g: Megagrapton isp., concave hyporelief, BK 32, Layer No. 16; h: Teichichnus isp. (bottom) crossing Zoophycos isp. (centre to right bottom), BK 16, Layer No. 22. Scale bar = 1 cm. in Early Complex Tiering Pattern: Upper Ordovician, Barrandian Area, The Czech Republic

Text-fig. 8. a, b: Bifungites isp. with fragments of vertical shafts, a – concave hyporelief BK 20, Layer No. 26, b – full relief BK 33, Layer No. 23; c–e: Palaeophycus sulcatus (MILLER et DYER, 1878), c – BK 29, Layer No. 22, d – BK 18, Layer No. 16, e – BK 31, Layer No. 6; f: Palaeophycus cf. tubularis HALL, 1847, BK 25, Layer No. 22; g: Megagrapton isp., concave hyporelief, BK 32, Layer No. 16; h: Teichichnus isp. (bottom) crossing Zoophycos isp. (centre to right bottom), BK 16, Layer No. 22. Scale bar = 1 cm.

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CATCH-EyoU: Processes in Youth's Construction of Active EU Citizenship: Cross-national Wave 1 Questionnaires: Italy, Sweden, Germany, Greece, Portugal, Czech Republic, UK, and Estonia: EXTRACT: Identification with Europe and Home Country

It is a well-established fact that forming a mature and coherent political identity is one developmental task in adolescence and young adulthood. However, given different degrees of commitment on the regional, national, and European level, the question remains whether young people’s identification varies among those spheres? Drawing on data from the European Catch-EyoU-project, it was the goal of this study to examine whether young people can be classified according to their identification toward their home country and Europe and how these types are associated with age, gender, country as well as political interest, tolerance, and political participation. The study is based on adolescents and young adults from the Czech Republic, Germany, Great Britain, Greece, Estonia, Italy, Portugal, and Sweden (N = 9,339; Mage=19.62; 59.1% female). Cluster analysis revealed five types of young people’s identification with country and Europe which showed significant associations between group membership and tolerance, political interest, and participation. The implications of distinguishing types of identification and their associations with political outcomes are discussed.

Fig. 4 in Evidence of two lineages of metriorhynchid crocodylomorphs in the Lower Cretaceous of the Czech Republic

Fig. 4. Metriorhynchid crocodylomorph tooth crowns from Štramberk, Czech Republic; Valanginian (Lower Cretaceous. A. Torvoneustes? sp., NHMW 2020/0025/0002. B. Plesiosuchina? indet., NHMW 2020/0025/ 0001. SEM micrographs of the carinae (A1, A2, B1, B2) showing the denticle morphologies. General views (A3, B3) indicating the sections where SEM micrographs were obtained. Scale bars 1 mm.

Fig. 5 in Evidence of two lineages of metriorhynchid crocodylomorphs in the Lower Cretaceous of the Czech Republic

Fig. 5. Metriorhynchid crocodylomorph tooth crown of Torvoneustes? sp., NHMW 2020/0025/0002 (A, B) and Plesiosuchina? indet., NHMW 2020/0025/0001 (C) from Štramberk, Czech Republic; Valanginian (Lower Cretaceous). A. SEM micrograph showing split carina (arrows). B, C. SEM micrograph showing lingual crown surface texture. Scale bars 5 mm.

Fig. 1. A in Evidence of two lineages of metriorhynchid crocodylomorphs in the Lower Cretaceous of the Czech Republic

Fig. 1. A. Geographic location of the studied area. B. Tectonic map of the Outer Western Carpathian area in the eastern part of the Czech Republic showing the location of Štramberk.

Fig. 3 in Evidence of two lineages of metriorhynchid crocodylomorphs in the Lower Cretaceous of the Czech Republic

Fig. 3. Tooth crown of the metriorhynchid crocodylomorph Torvoneustes? sp. (NHMW 2020/0025/0002) from Štramberk, Czech Republic; Valanginian Lower Cretaceous); in mesial (A1), apical (A2), labial (A3), basal (A4), lingual (A5), and distal (A6) views.

Fig. 2 in Evidence of two lineages of metriorhynchid crocodylomorphs in the Lower Cretaceous of the Czech Republic

Fig. 2. Tooth crown of the metriorhynchid crocodylomorph Plesiosuchina? indet. (NHMW 2020/0025/0001) from Štramberk, Czech Republic; Valanginian (Lower Cretaceous); in mesial (A1), apical (A2), labial (A3), basal (A4), lingual (A5), and distal (A6) views.

Fig. 6 in Evidence of two lineages of metriorhynchid crocodylomorphs in the Lower Cretaceous of the Czech Republic

Fig. 6. Morphospace occupation of Plesiosuchina? indet. (NHMW 2020/0025/0001) and Torvoneustes? sp. (NHMW 2020/0025/0002) among the thalattosuchian crocodylomorphs using principal coordinates 1 and 2. See SOM 1 and 2 for extended results of the principal coordinates analysis. Silhouettes obtained from phylopic.org: Geosaurinae (Dmitry Bogdanov, CC BY 3.0), Metriorhynchinae and Teleosauroidea (Gareth Monger, CC BY 3.0).

FIG. 5 in Expressed sex ratio in populations of the moss Hamatocaulis vernicosus (Mitt.) Hedenäs (Scorpidiaceae) in the Czech Republic with consideration of its cryptic species

FIG. 5. — The sex ratio in mixed population at locality Zhůří 1. Unbordered pie charts refer to clade 1, bordered ones represent clade 2. The patch in the larger circle contained plants of both clades, so this patch must be excluded from evaluating sex ratio in separated clades.

FIG. 3 in Expressed sex ratio in populations of the moss Hamatocaulis vernicosus (Mitt.) Hedenäs (Scorpidiaceae) in the Czech Republic with consideration of its cryptic species

FIG. 3. — Rates of male (blue), female (red) and non-expressing (green) plants at studied localities of Hamatocaulis vernicosus (Mitt.) Hedenäs clade 1 and 2.

FIG. 2 in Expressed sex ratio in populations of the moss Hamatocaulis vernicosus (Mitt.) Hedenäs (Scorpidiaceae) in the Czech Republic with consideration of its cryptic species

FIG. 2. — The expressed sex ratio at studied localities of H. vernicosus (Mitt.) Hedenäs. In mixed populations,only single-clade patches were used for the assessment.

FIG. 4 in Expressed sex ratio in populations of the moss Hamatocaulis vernicosus (Mitt.) Hedenäs (Scorpidiaceae) in the Czech Republic with consideration of its cryptic species

FIG. 4.— Sex ratio at localities with co-occurring cryptic species. All, without distinguished clades; cl. 1, clade 1; cl. 2, clade 2; Šimanov, Šimanovské rašeliniště. Only barcoded shoots were used to create this graph.

FIG. 1 in Expressed sex ratio in populations of the moss Hamatocaulis vernicosus (Mitt.) Hedenäs (Scorpidiaceae) in the Czech Republic with consideration of its cryptic species

FIG. 1.— The sex expression of Hamatocaulis vernicosus (Mitt.) Hedenäs in the Czech Republic at individual localities assessed at two levels of pooling hierarchy ("shoots at localities" and "patches at localities").

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FIGURE 3 in A multicarpellate fruit from Late Cretaceous sediments of South Bohemia, Czech Republic

FIGURE 3. Schematic line drawings of the gynoecium of Covidifructus multicarpellatus. (A) Longitudinal median section through the gynoecium showing its complex internal morphology with a remaining floral apex and an empty space (asterisk) in the centre of the ovary; arrowheads indicate stigma positions; grey shaded areas indicate potential stigmatic secretion forming an extra-gynoecial compitum across neighbouring stigmas; pollen grains and hypothetical pathways of pollen tubes are given in orange; dashed orange line indicates hypothetical pathway of pollen tube reaching a stigma via growth through the extra-gynoecial compitum; dashed black line indicates area of postgenital carpel union in the centre of the ovary (symplicate region); arrows indicate area of irregular ovary closure shown in (B); placentation is axile with the seeds (green) attached in the distalmost part of the ovary. (B) Line drawing showing zone ovary closure (see also Figure 1C, F) as seen from above, radial lines correspond to ventral slits of individual carpels; carpel flanks meet in an irregular pattern in the centre of the gynoecium; the area of closure is flattened (compressed; indicated by dashed ellipse), and the 10 carpels are roughly arranged in a double row facing each other (dashed line in centre of figure) rather than in a smooth circle.

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FIGURE 2 in A multicarpellate fruit from Late Cretaceous sediments of South Bohemia, Czech Republic

FIGURE 2. Covidifructus multicarpellatus gen. et sp. nov. specimen No. NMP F3200, scale bars equal 300 µm in all figures, series of microCT sections of premature capsular fruit. (A) Volume rendering of fruit in lateral view; lines B-F indicate approximate levels of transverse sections shown in the following images. (B) Transverse section at the level of styles and stigmas. (C) Transverse section at the level of the symplicate zone of the gynoecium where the carpels are postgenitally united in the centre of the ovary; distalmost parts of locules and seeds are visible. (D) Transverse section at the level of the empty space (asterisk) where carpels do not meet in the centre of the ovary. (E) Transverse section at the level of the synascidiate zone of the gynoecium, i.e., below the enclosed floral apex and the empty space. (F) Transverse section through the very base of the fruit showing the basal-most parts of the locules. (G) Longitudinal median section showing empty space in the centre of the ovary (asterisk) and axile ovule/seed attachment (arrow) in the distalmost part of the ovary. (H) Longitudinal tangential section with one seed rendered and coloured in green. (I) Transverse section at the level of seed attachment in the distal part of the ovary, with one seed rendered and coloured in green.

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FIGURE 1 in A multicarpellate fruit from Late Cretaceous sediments of South Bohemia, Czech Republic

FIGURE 1. Covidifructus multicarpellatus gen. et sp. nov.; specimen No. NMP F3200; scale bars equal 100 µm in all figures. (A) Small premature capsular fruit in lateral view, semi-globose in overall shape; SEM. (B) Fruit seen in apical view; note preformed dorsal lines of fruit dehiscence; SEM. (C) Close-up of fruit apex showing styles and stigmatic areas (asterisks); note irregular closure of ovary in the very centre; SEM. (D) MicroCT volume rendering, lateral view, showing 10 elongate seeds (green), one seed per carpel. (E) MicroCT volume rendering, apical view, showing regular arrangement of carpels and seeds. (F) Detail of central ovary closure (dashed line); note that some of the carpel flanks (arrowheads) do not extend to the very centre of the closure zone; SEM.

FIGURE 1 in Putative Ordovician green alga Krejciella reinterpreted as enteropneust hemichordate tube (Czech Republic)

FIGURE 1. Location map of the study area, showing the location of each of the studied localities within the Ordovician of the Prague Basin. A. Map of the Czech Republic and the Bohemian Massif showing the distribution of Ordovician rocks in the Prague Basin. B. Ordovician of the Prague Basin with the location of five outcrops that yielded the studied specimens.

FIGURE 2 in Putative Ordovician green alga Krejciella reinterpreted as enteropneust hemichordate tube (Czech Republic)

FIGURE 2. Type material of Krejciella putzkeri Obrhel 1968. Three-dimensionally preserved fragments of tubeshaped fossils. All specimens are in lateral view and are housed in the National Museum Prague. A. Holotype, NML D497a. B. Counterpart of the holotype, NML 497b. C. Paratype, NML 498.