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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in the Blansko Graben with lithology, distribution of palynomorphs, macroflora and macrofauna (modified after Čech, unpublished report). 1 – Spesovicornea pacltovae, 2 – Platanus sp., 3 – Myrtophyllum angustum (VEL.)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in the Blansko Graben with lithology, distribution of palynomorphs, macroflora and macrofauna (modified after Čech, unpublished report). 1 – Spesovicornea pacltovae, 2 – Platanus sp., 3 – Myrtophyllum angustum (VEL.)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.

Figure 6 in Rove beetle communities (Coleoptera: Staphylinidae) in the rock dumps after coal mining

Figure 6. Factors "Temperature" (A), "Year" (B) and environmental factors (C) contribution into rove beetles abundance on the study sites.

Figure 5 in Rove beetle communities (Coleoptera: Staphylinidae) in the rock dumps after coal mining

Figure 5. Dynamic density of rove beetles (A) and their dominant subfamilies (B) on the dumps of the Kedrovsky coal mine (mean ± SD).

Figure 3 in Rove beetle communities (Coleoptera: Staphylinidae) in the rock dumps after coal mining

Figure 3. Rank distribution of Staphylinidae species (the rank of species is along the abscissa axis; abundance, % is along the ordinate axis) in the rock dumps of the Kedrovsky coal mine for the entire period of research.

Figure 2 in Rove beetle communities (Coleoptera: Staphylinidae) in the rock dumps after coal mining

Figure 2. Numerical characteristics of some taxonomic categories of rove beetles in the studied area of the Kedrovsky coal mine (general number).

Figure 4 in Rove beetle communities (Coleoptera: Staphylinidae) in the rock dumps after coal mining

Figure 4. Similarity (according to Jaccard, IJ) of the rove beetle population in the sites of the Kedrovsky coal mine (the number at the nodes mean the bootstrap confidence intervals obtained based on 999 iterations are indicated).

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Figure 6 in Diversity of ground-dwelling arthropods on overburden dumps after coal mining

Figure 6. The ratio of beetle families in the study site (with the exception of Carabidae and Staphylinidae).

Fig. 13 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 13. Niutoushania (A, B) and Edriosteges (C–G) from the 1st member of the Lungtan Formation of Daijiagou. A, B. Niutoushania chongqingensis Chen sp. nov., anteroventral (A1), posterior (A2), and dorsal (A3) views of holotype NMV P309641 (A). B. Fragment of a ventral external mold NMV P309642 showing regularly spaced costae and fine spine bases. C–G. Edriosteges poyangensis (Kayser, 1883), dorsal (C, D2, E, F), anterodorsal (D1), and ventral (G) views of four dorsal external molds NMV P309632 (C), NMV P309630 (D), NMV P309629 (E), NMV P309631 (F), and a ventral valve NMV P309633 (G).

Fig. 11 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 11. Ventral interior of Transennatia gratiosa (Waagen, 1884); based on a ventral internal mold NMV P309639.

Fig. 14 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 14. Cardinal process of Chengxianoproductus cf. changxingensis Liao and Meng, 1986 (based on specimen NMV P309640).

Fig. 12 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 12. Interiors of Niutoushania chongqingensis Chen sp. nov. (based on specimen NMV P309641); ventral valve (A) and dorsal valve (B).

Fig. 15 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 15. Ventral interior of Permophricodothyris grandis (Huang, 1933) showing well−developed muscle scars (based on specimen NMV P309621).

Fig. 9 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 9. Selected serial sections of the ventral umbo of Meekella beipeiensis Chen sp. nov. (based on specimen NMV P309627) showing closely situated, parallel dental plates. The numbers are distance from the ventral beak; the orientation of the sections is with ventral surfaces upward.

Fig. 10. A in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 10. A. Meekella kueichowensis (Huang, 1933), dorsal (A1), ventral (A2), and lateral (A3) views of NMV P309622. B. Chengxianoproductus cf. changxingensis Liao and Meng, 1986, ventral (B1), posterior (B2), lateral (B3), and dorsal (B4) views of NMV P309640 (B); B5, enlargement of fine, densely arranged spine bases of B1. C, D. Spinomarginifera alpha Huang, 1932, lateral (C1), posterior (C2), ventral (C3), and dorsal (D) views of a complete specimen NMV P309643 and a dorsal external mold NMV P309644. E–H. Transennatia gratiosa (Waagen, 1884), ventral (E1, G, H1), anteroventral (E2, H2), posterior (E3, H3), lateral (E4, H4), and internal (F) views of a ventral internal mold NMV P309639 (E), and latex replica NMV P309638 (F) of the ventral internal mold (E –E), a ventral internal mold NMV P309636 (G) and a dorsal external mold NMV P309637 (H –H). A, E, F, G, from the 4th member of the Lungtan For1 4 1 4 mation of Daijiagou; B, from the 1st member of the Lungtan Formation of Daijiagou; C, D, H, from the 5th member of the Lungtan Formation of Daijiagou.

Fig. 6 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 6. Global stratigraphic distributions of the Lungtan brachiopod faunas. Permian chronostratigraphic framework follows International Union of Geological Sciences (2002). Conodont zones are after Mei et al. (1994) and Jin et al. (1998). The G/L mass extinction horizon corresponds to the biostratigraphic G/L boundary. The extinction interval is defined by the late Capitanian conodonts Jinogondolella granti Zone and the earliest Wuchiapingian Clarkina postbitteri Zone. Brachiopod genera include 1, Spinomarginifera; 2, Edriosteges; 3, Meekella; 4, Transennatia; 5, Perigeyerella; 6, Permophricodothyris; 7, Paraspiriferina; 8, Magniderbyia; 9, Niutoushania; 10, Chengxianoproductus; 11, Peltichia. Brachiopod species include 12, Edriosteges poyangensis; 13, Transennatia gratiosa; 14, Permophricodothyris grandis; 15, Magniderbyia sp. indet.; 16, Meekella pusilloplicata; 17, Me. kueichowensis; 18, Me. beipeiensis; 19, Spinomarginifera lopingensis; 20, Niutoushania chongqingensis; 21, Chengxianoproductus cf. changxingensis; 22, Paraspiriferina sp.; 23, Perigeyerella costellata; 24, Peltichia zigzag; 25, Spinomarginifera alpha.

Fig. 8 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 8. Reconstruction of ventral interior of Perigeyella costellata Wang, 1955 (based on specimen NMV P309620).

Fig. 5 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 5. Abundance of the Edriosteges poyangensis–Spinomarginifera lopingensis Association. A total of 51 specimens were collected from a shell bed at the basal Lungtan Formation.

Fig. 3 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 3. Correlations of the described faunas with previously published brachiopod assemblages from South China. The dashed lines indicate that the zonal boundaries are not well defined.

Fig. 2 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China

Fig. 2. Composite stratigraphy of the Lungtan Formation at the Daijiagou and Chuanmu sections, showing lithology, microfacies and fossil horizons. A. Daijiagou section. B. Chuanmu section. Lithology: 1, coarse sandstone; 2, alternating mudstone and sandstone; 3, siltstone; 4, fine sandstone; 5, clay; 6, coal seam; 7, cherty limestone; 8, bioclastic limestone; 9, limestone. Microfacies: 1, low−angle cross bedding; 2, wavy bedding; 3, bimodal cross bedding; 4, brackish water ironstone concretions; 5, black shale; 6, coal seam; 7, sandy mudstone; 8, siltstone; 9, quartz sandstone; 10, alternating siliceous shale and cherty limestone; 11, sparite; 12, grainstone−packstone; 13, roots (coal seats); 14, weathered clay; 15, cherty limestone.