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Text-fig. 4. Porechye open pit coal mine. a: photography of the Lipovtsy Formation section; b: stratigraphic column, 1 – sandstone, 2 – conglomerate, 3 – coal, 4 – tuff dated by U-Th-Pb geochronology, 5 – siltstone, 6 – mudstone, 7 – palynological samples with angiosperm pollen, 8 – dispersed angiosperm cuticles. in Angiosperm Diversification In The Early Cretaceous Of Primorye, Far East Of Russia

Text-fig. 4. Porechye open pit coal mine. a: photography of the Lipovtsy Formation section; b: stratigraphic column, 1 – sandstone, 2 – conglomerate, 3 – coal, 4 – tuff dated by U-Th-Pb geochronology, 5 – siltstone, 6 – mudstone, 7 – palynological samples with angiosperm pollen, 8 – dispersed angiosperm cuticles.

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Text-fig. 2. Moderately dipping Oligocene layers of the Mány Member in the eastern part of the Strázsa Hill quarry, SW of Zsámbék. The claymarl and siltstone layers cover sandstone and conglomerate. The arrow indicates the position of fossiliferous layers. Photo: László Fodor. in The Late Oligocene Macroflora Of Zsámbék, Central Hungary

Text-fig. 2. Moderately dipping Oligocene layers of the Mány Member in the eastern part of the Strázsa Hill quarry, SW of Zsámbék. The claymarl and siltstone layers cover sandstone and conglomerate. The arrow indicates the position of fossiliferous layers. Photo: László Fodor.

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Text-fig. 2. Stratigraphic column of the Govone section with a detail of the sampled intervals on the right. CCS – Cassano Spinola Conglomerates; Gm and Gg – sedimentary cycles, respectively marl-dominated or gypsum-dominated; MES – Messinian Erosional Surface; MSC – Messinian Salinity Crisis; PLG – Primary Lower Gypsum; RLG – Resedimented Lower Gypsum. in Remains Of A Subtropical Humid Forest In A Messinian Evaporitebearing Succession At Govone, Northwestern Italy - Preliminary Results

Text-fig. 2. Stratigraphic column of the Govone section with a detail of the sampled intervals on the right. CCS – Cassano Spinola Conglomerates; Gm and Gg – sedimentary cycles, respectively marl-dominated or gypsum-dominated; MES – Messinian Erosional Surface; MSC – Messinian Salinity Crisis; PLG – Primary Lower Gypsum; RLG – Resedimented Lower Gypsum.

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Text-fig. 3. "Rzehakia beds" at Líšeň-Neklež locality. 1 – topsoil, 2 – greenish-gray clay, locally yellow-brown, 3 – ochre-brown coarse sand, 4 – conglomerate with clasts of granodiorite, 5 – grey-brown medium-grained sand, 6 – light yellowish fine sand, 7 – re-sedimented red-brown eluvium of granodiorite, 8 – re-sedimented red-brown granodiorite debris, 9 – granodiorite, 10 – fossil macroflora. in A New Early Miocene (Ottnangian) Flora Of The "Rzehakia Beds" From Brno-Líšeň

Text-fig. 3. "Rzehakia beds" at Líšeň-Neklež locality. 1 – topsoil, 2 – greenish-gray clay, locally yellow-brown, 3 – ochre-brown coarse sand, 4 – conglomerate with clasts of granodiorite, 5 – grey-brown medium-grained sand, 6 – light yellowish fine sand, 7 – re-sedimented red-brown eluvium of granodiorite, 8 – re-sedimented red-brown granodiorite debris, 9 – granodiorite, 10 – fossil macroflora.

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Text-fig. 5. a: coal seam "Rabochy" with three tuff layers in upper part of Lipovtsy Formation in Porechye open pit coal mine; b: same section, enlarged view, upper tuff layer, sample 160/4 site; c: tuff layer in upper part of Frentsevka Formation below conglomerate at Palets Cape; d: same section, enlarged view, sample 1 site. in Angiosperm Diversification In The Early Cretaceous Of Primorye, Far East Of Russia

Text-fig. 5. a: coal seam "Rabochy" with three tuff layers in upper part of Lipovtsy Formation in Porechye open pit coal mine; b: same section, enlarged view, upper tuff layer, sample 160/4 site; c: tuff layer in upper part of Frentsevka Formation below conglomerate at Palets Cape; d: same section, enlarged view, sample 1 site.

Figure 8 in Washington State (USA) trigoniids (Bivalvia) from the conglomerate of Patterson Lake (Early Cretaceous)

Figure 8 (left). Parvitrigonia cooperi n. gen. et sp. A, B. UWBM 112557 from UWBM loc. B-9487. Paratype. Natural mudstone cast, RV, complete except for posterior terminus (dotted area). A. Flank view showing general outline. Costae mildly eroded. B. Dorsal view showing fine growth lines on area/escutcheon. C, D. UWBM 112558 from UWBM loc. B-9486. Holotype. Slightly crushed natural mudstone cast of articulated valves. Missing area and escutcheon (dotted area). C. RV with some shell remaining, flank view, showing wavy costae anteriorly. D. LV, flank view, showing flattopped costae. Scale bar = 5 mm

Figure 10. Earlpackardia methowensis n in Washington State (USA) trigoniids (Bivalvia) from the conglomerate of Patterson Lake (Early Cretaceous)

Figure 10. Earlpackardia methowensis n. sp., holotype UWBM 112559 from UWBM loc. 9486. A. Flank view. Dotted line indicates proposed reconstruction of missing shell based on growth lines. B. Oblique view demonstrating the umbo, marginal carina, unornamented area, and escutcheon. C. Dorsal view demonstrating the pointed beak and degree of inflation. D. Oblique dorsal view showing the incurved umbo, unornamented area, and escutcheon. Scale bar = 1 cm.

Figure 7 in Washington State (USA) trigoniids (Bivalvia) from the conglomerate of Patterson Lake (Early Cretaceous)

Figure 7. Notoscabrotrigonia oregana (Packard, 1921) UWBM 112553 from UWBM loc. 9486. Silicone cast of an external mold. Flank view of RV. Scale bar = 10 mm.

Figure 9. Parvitrigonia cooperi n in Washington State (USA) trigoniids (Bivalvia) from the conglomerate of Patterson Lake (Early Cretaceous)

Figure 9. Parvitrigonia cooperi n. gen. et sp. UWBM 115724 from UWBM loc. B-9541. Paratype. Complete natural sandstone cast of undistorted RV. Because of coarse matrix, fine detail is not well-shown. A. Flank view showing general outline of entire shell. B. Dorsal view showing overall shape of area/escutcheon and degree of shell inflation. Scale bar = 5 mm.

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Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011). in Feather Palm Foliage From The Messinian Of Italy (Capo Di Fiume, Palena And Pollenzo Near Alba) Within The Framework Of Northern Mediterranean Late Miocene Flora

Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011).

Text-fig. 11. Geological map south of the Nel'ma Bay. 1 - granodiorite (Early Palaeogene); 2 – Eocene andesitic and dacitic tuff with plant-bearing argillitic lenses; 3 – Late Eocene to Early Miocene andesite-basalt (Kizi Volcanic Group); 4 – tuffogenous sedimentary plant-bearing lenses with plant fossils; 5 – Dacite neck (Early Oligocene) 1 km south of the Dembi Bay; 6 – Pliocene pebbles and conglomerates; 7 – Plateaubasalts (Sovgavan' Formation, Late Neogene–Quaternary); 8 – Quaternary alluvial deposits; 9 – localities with fossil plants: a – Sonje, b – Bui, c – Dembi. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)

Text-fig. 11. Geological map south of the Nel'ma Bay. 1 - granodiorite (Early Palaeogene); 2 – Eocene andesitic and dacitic tuff with plant-bearing argillitic lenses; 3 – Late Eocene to Early Miocene andesite-basalt (Kizi Volcanic Group); 4 – tuffogenous sedimentary plant-bearing lenses with plant fossils; 5 – Dacite neck (Early Oligocene) 1 km south of the Dembi Bay; 6 – Pliocene pebbles and conglomerates; 7 – Plateaubasalts (Sovgavan' Formation, Late Neogene–Quaternary); 8 – Quaternary alluvial deposits; 9 – localities with fossil plants: a – Sonje, b – Bui, c – Dembi.

Text-fig. 6. Geological plan of Malo-Mikhaylovka. 1 – andesito-dacite; 2 – coarse-grained tuff; 3 – argillitic tuffite; 4 – tuffitic sandstone; 5 – lignite, coal clay; 6 – lenses of tuffitic conglomerate; 7 – acidic tuff; 8 – dacite; 9 – andesito-basalt; 10 – basalt; 11 – sandstone; 12 – andesite; 13 – break; 14 – inclination/direction of beds; 15 – plant-bearing levels; 16 – talus. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)

Text-fig. 6. Geological plan of Malo-Mikhaylovka. 1 – andesito-dacite; 2 – coarse-grained tuff; 3 – argillitic tuffite; 4 – tuffitic sandstone; 5 – lignite, coal clay; 6 – lenses of tuffitic conglomerate; 7 – acidic tuff; 8 – dacite; 9 – andesito-basalt; 10 – basalt; 11 – sandstone; 12 – andesite; 13 – break; 14 – inclination/direction of beds; 15 – plant-bearing levels; 16 – talus.

Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)

Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level.

Text-fig. 12. Geological plan of the Velikaya Kema plant-bearing locality (4 km north of Velikaya Kema village). 1 – basalt with flaggy flows; 2 – massive basalt; 3 – andesite with flaggy flows; 4 – andesite-basalt; 5 – trachyte, 6 – felsite; 7 – agglomerate, basalt and andesite; 8 – tuff coarse-grained; 9 – conglomerate; 10 – thin layers of andesitic tuff; 11 – tuffite, tuffaceous argillite, diatomite; 12 – plant bearing levels. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)

Text-fig. 12. Geological plan of the Velikaya Kema plant-bearing locality (4 km north of Velikaya Kema village). 1 – basalt with flaggy flows; 2 – massive basalt; 3 – andesite with flaggy flows; 4 – andesite-basalt; 5 – trachyte, 6 – felsite; 7 – agglomerate, basalt and andesite; 8 – tuff coarse-grained; 9 – conglomerate; 10 – thin layers of andesitic tuff; 11 – tuffite, tuffaceous argillite, diatomite; 12 – plant bearing levels.

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Text-fig. 3. Borehole section in the Blansko Graben with lithology, distribution of palynomorphs, macroflora and macrofauna (modified after Čech, unpublished report). 1 – Spesovicornea pacltovae, 2 – Platanus sp., 3 – Myrtophyllum angustum (VEL.) KNOBOCH, 4 – Gleichenia sp.), 5 – percentage of land-derived palynomorphs, 6 – percentages of marine palynomorphs, 7 – glauconite, 8 – pyrite nodules, 9 – macrofauna, 10 – productive palynological samples, 11 – carbonized roots, 12 – conglomerate, 13 – sandstone, 14 – claystone, 15 – coal, 16 – granite and granodiorite of the Brno pluton. in Spesovicornea Pacltovae Gen. Nov. Et Sp. Nov., A New Elateroid Sporomorph From The Bohemian Cenomanian (Czech Republic)

Text-fig. 3. Borehole section in the Blansko Graben with lithology, distribution of palynomorphs, macroflora and macrofauna (modified after Čech, unpublished report). 1 – Spesovicornea pacltovae, 2 – Platanus sp., 3 – Myrtophyllum angustum (VEL.) KNOBOCH, 4 – Gleichenia sp.), 5 – percentage of land-derived palynomorphs, 6 – percentages of marine palynomorphs, 7 – glauconite, 8 – pyrite nodules, 9 – macrofauna, 10 – productive palynological samples, 11 – carbonized roots, 12 – conglomerate, 13 – sandstone, 14 – claystone, 15 – coal, 16 – granite and granodiorite of the Brno pluton.

Fig. 12 in Shelly fossils from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia

Fig. 12. Shell microstructures of Cordatia erinae Brock and Claybourn gen. et sp. nov. from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia. A. SAM P57308, ventral valve in oblique internal view (A1); A2–A4, details of laminar shell microstructure. B. SAM P57309, dorsal valve in oblique internal view (B1); B2, detail of laminar shell microstructure. C. SAM P57310, shell fragment in oblique internal view (C1); C2, detail of laminar shell microstructure.

Fig. 8 in Shelly fossils from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia

Fig. 8. The lingulid brachiopod Curdus pararaensis Holmer and Ushatinskaya in Gravestock et al., 2001 from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia. Dorsal (A, B, E, G, H) and ventral (C, D, F) valves. A. SAM P57262 in external view. B. SAM P57263 in external view. C. SAM P57264 in external (C1) and oblique (posterior) (C2) views; C3 shows external ornament of faint concentric growth lines. D. SAM P57265 in internal view. E. SAM P57266 in internal view. F. SAM P57267 in internal view. G. SAM P57268 in internal view. H. SAM P57269 in internal view.

Fig. 5 in Shelly fossils from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia

Fig. 5. Spines of the bradoriid arthropod Mongolitubulus squamifer Missarzhevsky, 1977 from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia. A. SAM P57227. B. SAM P57228. C. SAM P57229. D. SAM P57230. E. SAM P57231. F. SAM P57232, fragment with flared base. G. SAM P57233. H. SAM P57234, close-up of rhomboid scales.

Fig. 11 in Shelly fossils from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia

Fig. 11. The lingulid brachiopod Cordatia erinae Brock and Claybourn gen. et sp. nov. from the lower Cambrian of South Australia, Ajax Limestone, Flinders Ranges (AJX-M/415) (A–E) and White Point Conglomerate, Kangaroo Island (F–S). Ventral (A, D, G) and dorsal (B, C, E, F, H–S) valves. A. SAM P53644, holotype in internal (A1) and oblique (A2) views; A3, detail of the delthyrium, propareas, and muscle field. B. SAM P57290 in internal view. C. SAM P57291 in external view (C1); C1, detail of the metamorphic shell. D. SAM P57292 in external view. E. SAM P57293, detail of external ornament. F. SAM P57294 in oblique internal view. G. SAM P57295 in internal view. H. SAM P57296 in external oblique view. I. SAM P57297 in external view. J. SAM P57298 in internal view. K. SAM P57299 in internal view. L. SAM P57300 in internal view. M. SAM P57301 in internal view. N. SAM P57302 in internal view. O. SAM P57303 in external view. P. SAM P57304 in external view. Q. SAM P57305 in external view. R. SAM P57306 in external view. S. SAM P57307 in external view.