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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. 8. Basalts, agglomerates and coarse tuffs (dark) and plant-bearing coarse tuffaceous sandstones with fossil plants (light) on the Nitusi Cape, Siziman locality. 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. 8. Basalts, agglomerates and coarse tuffs (dark) and plant-bearing coarse tuffaceous sandstones with fossil plants (light) on the Nitusi Cape, Siziman locality.

Text-fig. 5. Malo-Mikhaylovka village. The view on outcrops of the Malo-Mikhaylovka plant-bearing sedimentary strata. 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. 5. Malo-Mikhaylovka village. The view on outcrops of the Malo-Mikhaylovka plant-bearing sedimentary strata.

Text-fig. 7. Tuffitic argillites and coaly argillites with plant fossils near the bottom of the plant-bearing beds at the MaloMikhaylovka locality. 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. 7. Tuffitic argillites and coaly argillites with plant fossils near the bottom of the plant-bearing beds at the MaloMikhaylovka locality.

Text-fig. 3. Distribution of main types of volcanoes in the NearShore Volcanic Belt of Eastern Sikhote-Alin' (Eocene–Neogene). 1 – Central volcanoes (partly preserved); 2 – Central volcanoes (destructed); 3 – Shield and gentle sloping volcanoes with a dolerite or trachy-basaltic neck on the top; 4 – Lava and scoria cones; 5 – Pyroclastic, tuffaceous coarse- and fine-grained terrigenous sedimentary rocks, partly with plant-bearing levels; 6 – Eruption centers of plateau-basalts and the direction of lava flows; 7 – Main Late Cenozoic basaltic plateaus; 8 – Fumarol fields; 9 – Hot springs. 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. 3. Distribution of main types of volcanoes in the NearShore Volcanic Belt of Eastern Sikhote-Alin' (Eocene–Neogene). 1 – Central volcanoes (partly preserved); 2 – Central volcanoes (destructed); 3 – Shield and gentle sloping volcanoes with a dolerite or trachy-basaltic neck on the top; 4 – Lava and scoria cones; 5 – Pyroclastic, tuffaceous coarse- and fine-grained terrigenous sedimentary rocks, partly with plant-bearing levels; 6 – Eruption centers of plateau-basalts and the direction of lava flows; 7 – Main Late Cenozoic basaltic plateaus; 8 – Fumarol fields; 9 – Hot springs.

Text-fig. 4. A typical Oligocene–Early Miocene gentle-sloping Central volcano with an eruptive dolerite neck near the top – Nevelskoy "Cap". 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. 4. A typical Oligocene–Early Miocene gentle-sloping Central volcano with an eruptive dolerite neck near the top – Nevelskoy "Cap".

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. Simplified geological map of the Krkonoše Piedmont Basin (based on Blecha et al. 1997) with the palaeogeographic outline of the Rudník lake deposits. The site of Vrchlabí – road cut represents the complete Rudník "Horizon" sequence with record of various developmental stages of the lake. Numbers of sites are simplified. in Permian Fauna Of The Krkonoše Piedmont Basin (Bohemian Massif, Central Europe)

Text-fig. 3. Simplified geological map of the Krkonoše Piedmont Basin (based on Blecha et al. 1997) with the palaeogeographic outline of the Rudník lake deposits. The site of Vrchlabí – road cut represents the complete Rudník "Horizon" sequence with record of various developmental stages of the lake. Numbers of sites are simplified.

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Text-fig. 1. Sketch of the Bohemian Massif and the Czech Republic (dash-and-dot line) with marked position of the Krkonoše Piedmont Basin (grey). Modified after Martínek et al. 2006. in Permian Fauna Of The Krkonoše Piedmont Basin (Bohemian Massif, Central Europe)

Text-fig. 1. Sketch of the Bohemian Massif and the Czech Republic (dash-and-dot line) with marked position of the Krkonoše Piedmont Basin (grey). Modified after Martínek et al. 2006.

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Text-fig. 4. Simplified geological map of the Krkonoše Piedmont Basin (based on Blecha et al. 1997) with the palaeogeographic outline of the Kalná lake deposits. Numbers of sites are simplified. in Permian Fauna Of The Krkonoše Piedmont Basin (Bohemian Massif, Central Europe)

Text-fig. 4. Simplified geological map of the Krkonoše Piedmont Basin (based on Blecha et al. 1997) with the palaeogeographic outline of the Kalná lake deposits. Numbers of sites are simplified.

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Supplementary material to: "Formation of low-pressure reaction textures during near-isothermal exhumation of hot orogenic crust (Bohemian Massif, Austria)"

<p>Supplemantary material to "Sorger, D.,  Hauzenberger, C. A., Finger, F., Linner, M., Skrzypek, E., & Schorn, S. (2024). Formation of low-pressure reaction textures during near-isothermal exhumation of hot orogenic crust (Bohemian Massif, Austria). Journal of Metamorphic Geology, 42(1), 3–34."</p>

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Fluid-rock interaction of metamorphic fluids caused base metal mineralization in the Moldanubian domain, Bohemian Massif, Czech Republic – a fluid inclusion study - Supplementary data + measuring conditions

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FIG. 8. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 8. — Igornichthys bohemicus n. sp., holotype MHK 30866: A, scales with one spine sharply pointing in posterior direction and slightly downwards on each scale; B, scale with two sharply pointed tubercles. Scale bars: 1 mm.

FIG. 7. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 7. — Igornichthys bohemicus n. sp., holotype MHK 30866, scales on the left lateral side of the body: A, scales from rows 23-27 with conspicuous spines; B, detail of the scales from rows 25-27 with single spine; C, scales with two spines; D, detail of the scale with single spine in medial view; E, detail of the scale from row 27 with microsculpture of spines, whereas the surrounding scale surface is rough, which indicates bony surface; F, detail of the microsculpture on the spine of the previous scale. Scale bars: A, B, C, 500 µm; D, E, F, 100 µm.

FIG. 6. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 6. — Igornichthys bohemicus n. sp., holotype MHK 30866: A, general view of the teeth of upper and lower jaws; B, detail of the teeth of the upper and lower jaws, which interlock, when the jaws are closed; C, detail of the teeth of the anterior region of the lower jaw; D, detail of the teeth of the lower jaw. Scale bars: A, B, 500 µm; C, D, 100 µm.

FIG. 5. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 5. — Igornichthys bohemicus n. sp., reconstruction of the body in left lateral view. Posterior part of the body which is not preserved is grey. Scale bar: 5 mm.

FIG. 4. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 4. — Igornichthys bohemicus n. sp., reconstruction of the skull in left lateral view. The outlines of the bones, which are ill-defined, are marked with dashed lines. Abbreviations: see Methods. Scale bar: 5 mm.

FIG. 10 in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 10. — Reconstructions of the skull in dorsal view of some Aeduellidae and Igornichthyidae. The outlines of the bones, which are ill-defined, are marked with dashed lines: A, Aeduella blainvillei (Agassiz, 1833), after Heyler (1969); B, Neslovicella rzehaki Štamberg, 2007, after Štamberg (2007); C, Setlikia bohemica Štamberg & Zajíc, 1994, after Štamberg & Zajíc (1994); D, Igornichthys bohemicus n. sp. Abbreviations: see Methods. Scale bars: 1 cm.

FIG. 3. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 3. — Igornichthys bohemicus n. sp., holotype MHK 30866: A, left view of the whole specimen; B, detail of the skull in left lateral view. Scale bars: 5 mm.

FIG. 2. — Igornichthys bohemicus n in A new actinopterygian species of Igornichthys Heyler, 1972 from the Permian of the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic), and its relationship to the actinopterygians of other European Permo- Carboniferous basins

FIG. 2. — Igornichthys bohemicus n. sp., outprint of the skull in left lateral view, holotype MHK 30866. The outlines of the bones, which are ill-defined, are marked with dashed lines. Abbreviations: see Methods. Scale bar: 5 mm.