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Text-fig. 20. Carnivore puncture mark on tibia 97-597-C-Př82, for the metrics of this bone see Table 12. in Consumption Of Canid Meat At The Gravettian Předmostí Site, The Czech Republic

Text-fig. 20. Carnivore puncture mark on tibia 97-597-C-Př82, for the metrics of this bone see Table 12.

Text-fig. 5. Disarticulation marks on the head of humerus 98- 594-B-P (1) to disarticulate the shoulder joint, for the metrics of this bone see Table 12. in Consumption Of Canid Meat At The Gravettian Předmostí Site, The Czech Republic

Text-fig. 5. Disarticulation marks on the head of humerus 98- 594-B-P (1) to disarticulate the shoulder joint, for the metrics of this bone see Table 12.

Text-fig. 3. Schematic position of the human modifications (cut marks, impact marks, ochre traces, inserted bones) recognised on the canid remains from Předmostí, indicated on a wolf skeleton; the frequencies of the modifications are not shown. Modified after © 2003 ArcheoZoo.org / Michel Coutureau (Inrap). in Consumption Of Canid Meat At The Gravettian Předmostí Site, The Czech Republic

Text-fig. 3. Schematic position of the human modifications (cut marks, impact marks, ochre traces, inserted bones) recognised on the canid remains from Předmostí, indicated on a wolf skeleton; the frequencies of the modifications are not shown. Modified after © 2003 ArcheoZoo.org / Michel Coutureau (Inrap).

Text-fig. 1. Map of northern Eurasia with the most important sites discussed in the text: 1: Předmostí, 2: Pavlov, 3: Dolní Věstonice, 4: Krems Wachtberg, 5: Braives, 6: Trou des Nutons, 7: Jaurens, 8: Maldidier, 9: Lokomotiv, 10: Geographical Society cave. in Consumption Of Canid Meat At The Gravettian Předmostí Site, The Czech Republic

Text-fig. 1. Map of northern Eurasia with the most important sites discussed in the text: 1: Předmostí, 2: Pavlov, 3: Dolní Věstonice, 4: Krems Wachtberg, 5: Braives, 6: Trou des Nutons, 7: Jaurens, 8: Maldidier, 9: Lokomotiv, 10: Geographical Society cave.

Text-fig. 1. Schematic maps showing location of the Prague Basin in the Barrandian area of the Czech Republic (a), the Koněprusy area (b), quarries in the Koněprusy area (c) and Jirásek's and Preisler's quarries (d). The exact location of the section described by Hladil et al. (1993) (1) and the new sections where the brachiopods were extracted (2) are figured. Abbreviations: UDI – upper dark interval, VČS-E – Velkolom Čertovy schody – východ quarry. in Rhynchonelliform Brachiopods And Trilobites Of The 'Upper Dark Interval' In The Koněprusy Area Devonian, Eifelian, Kačák Event; The Czech Republic

Text-fig. 1. Schematic maps showing location of the Prague Basin in the Barrandian area of the Czech Republic (a), the Koněprusy area (b), quarries in the Koněprusy area (c) and Jirásek's and Preisler's quarries (d). The exact location of the section described by Hladil et al. (1993) (1) and the new sections where the brachiopods were extracted (2) are figured. Abbreviations: UDI – upper dark interval, VČS-E – Velkolom Čertovy schody – východ quarry.

Text-fig. 3. Eastern wall of Jirásek's Quarry with studied section, with light-grey Acanthopyge Limestones in lower half of the wall, the UDI (in brown) in upper half followed by bioclastic breccia (Bed 46 sensu Hladil 1993) near the edge of the wall (a) and detail of UDI and adjacent limestones with the most productive beds (b). Photo January, 2019. in Rhynchonelliform Brachiopods And Trilobites Of The 'Upper Dark Interval' In The Koněprusy Area Devonian, Eifelian, Kačák Event; The Czech Republic

Text-fig. 3. Eastern wall of Jirásek's Quarry with studied section, with light-grey Acanthopyge Limestones in lower half of the wall, the UDI (in brown) in upper half followed by bioclastic breccia (Bed 46 sensu Hladil 1993) near the edge of the wall (a) and detail of UDI and adjacent limestones with the most productive beds (b). Photo January, 2019.

Text-fig. 2. Studied section in Jirásek's Quarry with essential data on lithology and samples studied on rhynchonelliform brachiopods and trilobites (black dots – productive, white dots – barren). in Rhynchonelliform Brachiopods And Trilobites Of The 'Upper Dark Interval' In The Koněprusy Area Devonian, Eifelian, Kačák Event; The Czech Republic

Text-fig. 2. Studied section in Jirásek's Quarry with essential data on lithology and samples studied on rhynchonelliform brachiopods and trilobites (black dots – productive, white dots – barren).

Text-fig. 2. General geological map of the Emsian (Suchomasty Limestone) and Eifelian (Acanthopyge Limestone) rocks at Zadní Kobyla ridge with marked Calceola- and trilobite-bearing locality. Modified after Svoboda and Prantl (1949) and Mergl (2014). in Trilobite Assemblage Of Calceola -Bearing Beds In Acanthopyge Limestone (Choteč Formation, Middle Devonian, Eifelian, Prague Basin, The Czech Republic)

Text-fig. 2. General geological map of the Emsian (Suchomasty Limestone) and Eifelian (Acanthopyge Limestone) rocks at Zadní Kobyla ridge with marked Calceola- and trilobite-bearing locality. Modified after Svoboda and Prantl (1949) and Mergl (2014).

Text-fig. 5. A pie chart of trilobite taxa abundance at Zadní Kobyla – small quarry outcrop (Calceola-bearing locality). in Trilobite Assemblage Of Calceola -Bearing Beds In Acanthopyge Limestone (Choteč Formation, Middle Devonian, Eifelian, Prague Basin, The Czech Republic)

Text-fig. 5. A pie chart of trilobite taxa abundance at Zadní Kobyla – small quarry outcrop (Calceola-bearing locality).

Text-fig. 1. Sketch map of the Devonian of the Prague Basin, and generalised stratigraphy of the Koněprusy Limestone (Pragian), Suchomasty Limestone (Upper Emsian), Acanthopyge Limestone (Eifelian) and the top of the Acanthopyge Limestone and the Srbsko Formation (transition Eifelian-Givetian) in the Koněprusy area (with marked neptunian dykes and approximate positions of Calceola-bearing limestone beds). Modified after Chlupáč et al. (1986), Hladil et al. (1992) and Mergl (2014). in Trilobite Assemblage Of Calceola -Bearing Beds In Acanthopyge Limestone (Choteč Formation, Middle Devonian, Eifelian, Prague Basin, The Czech Republic)

Text-fig. 1. Sketch map of the Devonian of the Prague Basin, and generalised stratigraphy of the Koněprusy Limestone (Pragian), Suchomasty Limestone (Upper Emsian), Acanthopyge Limestone (Eifelian) and the top of the Acanthopyge Limestone and the Srbsko Formation (transition Eifelian-Givetian) in the Koněprusy area (with marked neptunian dykes and approximate positions of Calceola-bearing limestone beds). Modified after Chlupáč et al. (1986), Hladil et al. (1992) and Mergl (2014).

Fig. 4 in Sand martin (Riparia riparia) in the Czech Republic at the turn of the millenium

Fig. 4. So far increasing colony size compensates decreasing number of localites. Colony size increased currently from 130 holes per colony to current 314 holes per colony.

Fig. 5 in Sand martin (Riparia riparia) in the Czech Republic at the turn of the millenium

Fig. 5. Distribution of altitude of sand martin nestplaces in the Czech Republic. In discordance with previously published results, sand martins created numerous colonies in altitudes over 400 m a.s.l.

Fig. 3 in Sand martin (Riparia riparia) in the Czech Republic at the turn of the millenium

Fig. 3. Number of disappeared colonies outnumbered the number of newly emerging localities occupied by sand martins in all years except of 1999 and 2004. It signalizes the rising limitation in the number of available localities during last years.

Fig. 2 in Sand martin (Riparia riparia) in the Czech Republic at the turn of the millenium

Fig. 2. Relative share of unoccupied localities found during the sand martin monitoring. Amount of unoccupied localities appropriate for nesting of sand martins according to HJERTAAS (1984) was compared with the total amount of all appropriate localities available.

Fig. 1 in Sand martin (Riparia riparia) in the Czech Republic at the turn of the millenium

Fig. 1. Population trends of the sand martin in the Czech Republic during 1992-2005. "Index of interseasonal changes" shows the relative change in the number of holes in the relation to the previous year. Included are holes from all the colonies monitored for at least two subsequent years. "Index 1993" shows the rapid decrease of sand martin population during the period surveyed. Amount of holes in 1993 is marked as 100 %; included are all the colonies monitored for at least two subsequent years. All discontinuously occupied localities are also included in both indexes.

Text-fig. 1. Lithostratigraphic scheme for Most Basin (edited according to Kvaček et al. 2019 and Hilgen et al. 2012) with fossiliferous horizons of Holešice and Libkovice members in its west part. Stratigraphic position of fish remnants is highlighted. in New Ichthyofauna From The Holešice And Libkovice Members In The Western Part Of Most Basin (Early Miocene), The Czech Republic

Text-fig. 1. Lithostratigraphic scheme for Most Basin (edited according to Kvaček et al. 2019 and Hilgen et al. 2012) with fossiliferous horizons of Holešice and Libkovice members in its west part. Stratigraphic position of fish remnants is highlighted.

Fig. 11 in Catalogue of type specimens of braconid wasps (Hymenoptera: Braconidae) deposited in the National Museum, Prague, Czech Republic

Fig. 11. Holotype of Apanteles murinanae Čapek & Zwölfer, 1957 with its labels (scale bar = 2.5 mm).

Fig. 34 in Catalogue of type specimens of braconid wasps (Hymenoptera: Braconidae) deposited in the National Museum, Prague, Czech Republic

Fig. 34. Characteristic determination labels used by Maximilian Fischer which are under the type material deposited in NMPC.

Fig. 33 in Catalogue of type specimens of braconid wasps (Hymenoptera: Braconidae) deposited in the National Museum, Prague, Czech Republic

Fig. 33. Different types of locality labels used by P. Starý in 1950s and locality label used by A. Hoffer with paratype labels by A. Taeger.

Fig. 8 in Catalogue of type specimens of braconid wasps (Hymenoptera: Braconidae) deposited in the National Museum, Prague, Czech Republic

Fig. 8. Paratype of Ropalophorus wisconsinensis Shenefelt, 1960 with its labels (scale bar = 2.5 mm).