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Fig. 10 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 10. Ostracods from Bálvány North section, Bükk Mountains, Hungary. Right lateral views of complete carapaces. A–J. Acratia? jeanvannieri Forel sp. nov., Griesbachian, Lower Triassic. A. Holotype, UPMC P6M2803, sample 08BAN61. B. Paratype, UPMC P6M2804, sample 08BAN63. C. UPMC P6M2805, sample 08BAN63. D. UPMC P6M2806, sample 08BAN63. E. UPMC P6M2807, sample 08BAN61. F. UPMC P6M2808, sample 08BAN61. G. UPMC P6M2809, sample 08BAN63. H. UPMC P6M2810, sample 08BAN63. I. UPMC P6M2811, sample 08BAN62. J. UPMC P6M2812, sample 08BAN62. K–O. Acratia nagyvisnyoensis Forel sp. nov., Changhsingian, Upper Permian. K. Holotype, UPMC P6M2813, sample 08BAN47. L. Paratype, UPMC P6M2814, sample 08BAN47. M. UPMC P6M2815, sample 08BAN47. N. UPMC P6M2816, sample 08BAN47. O. UPMC P6M2817, sample 08BAN54. P, T. Acratia sp. A, Changhsingian, Upper Permian. P. UPMC P6M2818, sample 08BAN47. T. UPMC P6M2819, sample 08BAN47. Q. Acratia sp. B, Changhsingian, Upper Permian. UPMC P6M2820, sample 08BAN47. R, S. Acratia sp. C, Changhsingian, Upper Permian. R. UPMC P6M2821, sample 08BAN50. S. UPMC P6M2822, sample 08BAN52. Scale bars 100 µm.
Fig. 18 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 18. Ostracods from Bálvány North section, Bükk Mountains, Hungary. Right (A, B, D, E, G–P) and left (C, F) lateral views of complete carapaces. A–H. Callicythere? balvanyseptentrioensis Forel sp. nov., Griesbachian, Lower Triassic. A. Holotype, UPMC P6M2900, sample 08BAN62. B. Paratype, UPMC P6M2901, sample 08BAN61. C. UPMC P6M2902, sample 08BAN62. D. UPMC P6M2903, sample 08BAN62. E. UPMC P6M2904, sample 08BAN62. F. UPMC P6M2905, sample 08BAN63. G. UPMC P6M2906, sample 08BAN64. H. UPMC P6M2907, sample 08BAN62. I–L. Eumiraculum desmaresae Forel sp. nov., Changhsingian, Upper Permian. I. UPMC P6M2908, sample 08BAN47. J. Holotype, UPMC P6M2909, sample 08BAN47. K. Paratype, UPMC P6M2910, sample 08BAN47. L. UPMC P6M2911, sample 08BAN47. M. Sulcella? sp., UPMC P6M2916, sample 08BAN67, Griesbachian, Lower Triassic. N. Eumiraculum cf. Eumiraculum desmaresae Forel sp. nov., UPMC P6M2912, sample 08BAN67, Griesbachian, Lower Triassic. O, P. Cetollina? sp. A. O. UPMC P6M2913, sample 08BAN59, Changhsingian, Upper Permian. P. UPMC P6M2914, sample 08BAN66, Griesbachian, Lower Triassic. Scale bars 100 µm.
Fig. 6 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 6. Ostracods from Bálvány North section, Hungary (except A–D from Bulla section, Northern Italy). Right (A, E, G–W) and left (B, C, D, F) lateral views of complete carapaces. A–G. Langdaia bullabalvanyensis Crasquin sp. nov., Griesbachian, Lower Triassic. A. Holotype, UPMC P6M2762, sample 05BU19. B. Paratype, UPMC P6M2763, sample 05BU19. C. UPMC P6M2232, sample 05BU19. D. UPMC P6M2764, sample 05BU19. E. UPMC P6M2765, sample 08BAN67. F. UPMC P6M2766, sample 08BAN67. G. UPMC P6M2767, sample 08BAN67. H, I. Bairdia baudini nom. nov. H. UPMC P6M2785, sample 08BAN48, Changhsingian, Upper Permian. I. UPMC P6M2786, sample 08BAN61, Griesbachian, Lower Triassic. J–M. Bairdia wailiensis Crasquin−Soleau, 2006, Griesbachian, Lower Triassic. J. UPMC P6M2770, sample 08BAN62. K. UPMC P6M2771, sample 08BAN47. L. UPMC P6M2772, sample 08BAN62. M. UPMC P6M2773, sample 08BAN62. N–P. Bairdia anisongae Forel sp. nov. N. Holotype, UPMC P6M2774, sample 08BAN55, Changhsingian, Upper Permian. O. Paratype, UPMC P6M2775, sample 08BAN62, Grisbachian, Lower Triassic. P. UPMC P6M2776, sample 08BAN47, Changhsingian, Upper Permian. Q–U. Bairdia davehornei Forel sp. nov., Griesbachian, Lower Triassic. Q. Holotype, UPMC P6M2777, sample 08BAN61. R. Paratype, UPMC P6M2778, sample 08BAN62. S. UPMC P6M2779, sample 08BAN62. T. UPMC P6M2780, sample 08BAN62. U. UPMC P6M2781, sample 08BAN62. V, W. Bairdia cf. Bairdia davehornei Forel sp. nov., Griesbachian, Lower Triassic. V. UPMC P6M2782, sample 08BAN62. W. UPMC P6M2783, sample 08BAN61. Scale bars 100 µm.
Fig. 12 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 12. Ostracods from Bálvány North section, Bükk Mountains, Hungary. Right lateral (A, D–H, J–U) and dorsal (B, C, I) views of complete carapaces. A–K. Liuzhinia venninae Forel sp. nov., Griesbachian, Lower Triassic. A. Holotype, UPMC P6M2842, sample 08BAN63. B. UPMC P6M2843, sample 08BAN63. C. Dorsal view of a complete carapace, UPMC P6M2844, sample 08BAN63. D. Paratype, UPMC P6M2845, sample 08BAN61. E. UPMC P6M2846, sample 08BAN63. F. UPMC P6M2847, sample 08BAN63. G. UPMC P6M2848, sample 08BAN62. H. UPMC P6M2849, sample 08BAN61. I. UPMC P6M2850, sample 08BAN63. J. UPMC P6M2851, sample 08BAN61. K. UPMC P6M2852, sample 08BAN63. L–R. Liuzhinia bankutensis Forel sp. nov. L. Holotype, UPMC P6M2853, sample 08BAN67, Giresbachian, Lower Triassic. M. Paratype, UPMC P6M2854, sample 08BAN69, Griesbachian, Lower Triassic. N. UPMC P6M2915, sample 08BAN47, Changhsingian, Upper Permian. O. UPMC P6M2855, sample 08BAN63, Giresbachian, Lower Triassic. P. UPMC P6M2856, sample 08BAN67, Griesbachian,Lower Triassic. Q. UPMC P6M2857, sample 08BAN67, Griesbachian, Lower Triassic. R. UPMC P6M2858, sample 08BAN67, Griesbachian, Lower Triassic. S. Liuzhinia sp. A. UPMC P6M2859, sample 08BAN62, Griesbachian, Lower Triassic. T. Liuzhinia sp. B. UPMC P6M2768, sample 08BAN47, Changhsingian, Upper Permian. U. Bairdiacypris fornicata Shi, 1982. UPMC P6M2860, sample 08BAN62, Griesbachian, Lower Triassic. Scale bars 100 µm.
Fig. 1 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 1. Location map of the northern part of the Bükk Mountains (after Less et al. 2002) with Bálvány North P–T boundary section. Fm., Formation.
Fig. 23 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 23. Ostracods from Bálvány North section, Bükk Mountains, Hungary. Right lateral views of complete carapaces. A, B. Microcheilinella cf. rectodorsata Forel, 2010, Changhsingian, Upper Permian. A. UPMC P6M2889, sample 08BAN47. B. UPMC P6M2890, sample 08BAN47. C, D. Microcheilinella sp. C, Griesbachian, Lower Triassic. C. UPMC P6M2891, sample 08BAN61. D. UPMC P6M2892, sample 08BAN61. E, F. Microcheilinella sp. D, Changhsingian, Upper Permian. E. UPMC P6M2893, sample 08BAN 59. F. UPMC P6M2894, sample 08BAN59. G, I. Microcheilinella sp. E, Griesbachian, Lower Triassic. G. UPMC P6M2896, sample 08BAN61. I. UPMC P6M2897, sample 08BAN61. H. Microcheilinella sp. F, UPMC P6M2898, sample 08BAN47, Changhsingian, Upper Permian. J. Microcheilinella sp. G, UPMC P6M2899, sample 08BAN47, Changhsingian, Upper Permian. Scale bars 100 µm.
Fig. 4 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 4. Ostracods from Bálvány North section, Bükk Mountains, Hungary. Left (A, D–G, N–O) and right (B, M, P–S) lateral views of complete carapaces, external views of a left (J, L, V) and right (I, K, U) valves. A–H. Reviya praecurukensis Forel sp. nov., Changhsingian, Upper Permian. A. Holotype, UPMC P6M2742, sample 08BAN47. B. Paratype, UPMC P6M2743, sample 08BAN47. C. UPMC P6M2744, sample 08BAN47. D. UPMC P6M2745, sample 08BAN47. E. UPMC P6M2746, sample 08BAN47. F. UPMC P6M2747, sample 08BAN47. G. UPMC P6M2748, sample 08BAN47. H. UPMC P6M2749, sample 08BAN52. I–L. Hollinella fengqinglaii Crasquin sp. nov., Changhsingian, Upper Permian. I. Holotype, UPMC P6M2750, sample 08BAN50. J. Paratype, UPMC P6M2751, sample 08BAN60. K. UPMC P6M2752, sample 08BAN56. L. UPMC P6M2753, sample 08BAN60. M–O. Samarella meishanella Forel, 2010, Changhsingian, Upper Permian. M. UPMC P6M2754, sample 08BAN56. N. UPMC P6M2755, sample 08BAN63. O. UPMC P6M2756, sample 08BAN63. P.?Samarella victori Crasquin, 2010a, UPMC P6M2757, sample 08BAN56, Changhsingian, Upper Permian. Q–T. Shemonaella? olempskaella Forel sp. nov., Changhsingian, Upper Permian. Q. Holotype, UPMC P6M2758, sample 08BAN48. R. Paratype, UPMC P6M2759, sample 08BAN47. S. UPMC P6M2760, sample 08BAN47. T. UPMC P6M2761, sample 08BAN47. U, V. Reviya curukensis Crasquin−Soleau, 2004, Griesbachian, Lower Triassic. U. UPMC P6M2862, sample 08BAN65. V. UPMC P6M2862, sample 08BAN65. Scale bars 100 µm.
Fig. 22 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 22. Ostracods from Bálvány North section, Bükk Mountains, Hungary. Right lateral view of complete carapaces, except B. A. Acratia cf. sp. C. UPMC P6M2823, sample 08BAN53. B. Acratia sp. D. UPMC P6M2824, sample 08BAN47. C. Acratia? sp. E. UPMC P6M2825, sample 08BAN55. D. Acratia sp. F. UPMC P6M2826, sample 08BAN67. E. Kempfina? sp. A. UPMC P6M2827, sample 08BAN47. F. Baschkirina cf. huzhouensis Forel, 2010. UPMC P6M2828, sample 08BAN47. G, H.?Bairdiacypris caeca Shi, 1987. G. UPMC P6M2829, sample 08BAN59. H. UPMC P6M2830, sample 08BAN59. I–L. Fabalicypris parva Wang, 1978. I. UPMC P6M2835, sample 08BAN47. J. UPMC P6M2832, sample 08BAN47. K. UPMC P6M2833, sample 08BAN47. L. UPMC P6M2834, sample 08BAN47. M. Fabalicypris arcuata Wang, 1978. UPMC P6M2831, sample 08BAN51. N. Fabalicypris cf. parva Wang, 1978. UPMC P6M2836, sample 08BAN61. O. Fabalicypris reniformis (Chen, 1958) sensu Wang, 1978. UPMC P6M2837, sample 08BAN48. P, R. Fabalicypris cf. elliptica rotunda Kozur, 1985. P. UPMC P6M2839, sample 08BAN47. R. UPMC P6M2840, sample 08BAN62. Q. Fabalicypris? sp. UPMC P6M2841, sample 08BAN53. Scale bars 100 µm.
Fig. 21 in Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary
Fig. 21. Ostracods from Bálvány North section, Bükk Mountains, Hungary. Right lateral views of complete (A–I, L–T) and broken (J, K) carapaces. A. Bairdia cf. broutini Crasquin, 2010a. UPMC P6M2784, sample 08BAN62, Griesbachian, Lower Triassic. B–C. Bairdia cf. urodeloformis Chen, 1987, Changhsingian, Upper Permian. B. UPMC P6M2768, sample 08BAN47. C. UPMC P6M2769, sample 08BAN47. D. Bairdia sp. A sensu Crasquin et al. (2010), UPMC P6M2787, sample 08BAN47, Changhsingian, Upper Permian. E. Bairdia sp. F, UPMC P6M2788, sample 08BAN62, Griesbachian, Lower Triassic. F. Bairdia sp. G, UPMC P6M2838, sample 08BAN54, Changhsingian, Upper Permian. G. Bairdia sp. H, UPMC P6M2789, sample 08BAN47, Changhsingian, Upper Permian. H. Bairdia sp. I, UPMC P6M2790, sample 08BAN50, Changhsingian, Upper Permian. I. Bairdia sp. J, UPMC P6M2791, sample 08BAN50, Changhsingian, Upper Permian. J. Bairdia sp. K, UPMC P6M2792, sample 08BAN59, Changhsingian, Upper Permian. K. Bairdia sp. L, UPMC P6M2793, sample 08BAN54, Changhsingian, Upper Permian. L. Bairdia sp. M, UPMC P6M2794, sample 08BAN47, Changhsingian, Upper Permian. M. Bairdia? sp. N, UPMC P6M2795, sample 08BAN52, Changhsingian, Upper Permian. N. Bairdia sp. O, UPMC P6M2796, sample 08BAN47, Changhsingian, Upper Permian. O. Bairdia sp. P, UPMC P6M2797, sample 08BAN48, Changhsingian, Upper Permian. P. Bairdia sp. Q, UPMC P6M2798, sample 08BAN59, Changhsingian, Upper Permian. Q. Bairdia sp. R, UPMC P6M2799, sample 08BAN60, Changhsingian, Upper Permian. R. Bairdia sp. S, UPMC P6M2800, sample 08BAN62, Griesbachian, Lower Triassic. S. Bairdia? sp. T, UPMC P6M2801, sample 08BAN61, Griesbachian, Lower Triassic. T. Bairdia sp. U, UPMC P6M2802, sample 08BAN65, Griesbachian, Lower Triassic. Scale bars 100 µm.
FIG. 1. — A in Biodiversity in mountain groundwater: the Mercantour National Park (France) as a European hotspot
FIG. 1. — A, Study area and location of sampling sites. Sites are numbered as in Table 1; B, Map of groundwater habitats (extracted from Cornu et al. 2013) with the limits of the Mercantour National Park in white.
FIG. 2 in Biodiversity in mountain groundwater: the Mercantour National Park (France) as a European hotspot
FIG. 2. — Some representative species collected in the Mercantour National Park:A, Troglochaetus beranecki Delachaux,1921, length 0.6 mm; B, Parabathynella sp., length 1.5 mm; C, Nipargus foreli Humbert, 1877, length 8 mm; D, Proasellus sp., length 4 mm. Photographs: A-C, M.-J. Dole-Olivier; D, F. Malard.
Fig. 6 in Areas of endemism in Thailand: has historical partitioning between seasonally dry lowland and aseasonal moist mountain forests shaped biodiversity in Southeast Asia?
Fig. 6. Relationship between elevation and geographical range of Hybos spp. in Thailand. The number of 1° grids in which a species was recorded is plotted against the median elevation of all records. Line fitted by linear regression in PAST (r2=0.1026).
Fig. 5 in Areas of endemism in Thailand: has historical partitioning between seasonally dry lowland and aseasonal moist mountain forests shaped biodiversity in Southeast Asia?
Fig. 5. EZPAE down-weighted against homoplasy, using altitudinally zoned mountain ranges as OGU, 'characters' made additive. Strict consensus tree of two equally parsimonious trees (CI = 0.716, RI = 0.534) produced by maximum parsimony analysis with weighted 'characters' and TBR branch swapping in TNT. Symmetrical resampling support is given under the nodes. Alphabetic codes of termini correspond with mountain ranges as abbreviated in Fig. 3; the suffixes 'low' & 'high' refer to low (<1,250m) and high (>1,250m) elevation sample data.
Fig. 4 in Areas of endemism in Thailand: has historical partitioning between seasonally dry lowland and aseasonal moist mountain forests shaped biodiversity in Southeast Asia?
Fig. 4. EZPAE down-weighted against homoplasy, using altitudinally zoned mountain ranges as OGU, 'characters' made non-additive. Strict consensus tree of four equally parsimonious trees (CI = 0.674, 0.580) produced by maximum parsimony analysis with weighted 'characters' and TBR branch swapping in TNT. Symmetrical resampling support is given under the nodes. Alphabetic codes of termini correspond with mountain ranges as abbreviated in Fig. 3; the suffixes 'low' & 'high' refer to low (<1,250m) and high (>1,250m) sample data.
Fig. 2. PAE using 1 in Areas of endemism in Thailand: has historical partitioning between seasonally dry lowland and aseasonal moist mountain forests shaped biodiversity in Southeast Asia?
Fig. 2. PAE using 1° grids as OGU. Strict consensus tree of 760 equally parsimonious trees (CI = 0.501, RI = 0.557) produced by maximum parsimony analysis with unweighted 'characters' and TBR branch swapping in TNT. Symmetrical resampling support is given under the nodes (see Fig 1A for explanation of alphabetic codes).
Fig. 3 in Areas of endemism in Thailand: has historical partitioning between seasonally dry lowland and aseasonal moist mountain forests shaped biodiversity in Southeast Asia?
Fig. 3. PAE using mountain ranges as OGU. Strict consensus tree of nine equally parsimonious trees (CI = 0.745, RI = 0.722) produced by maximum parsimony analysis with weighted 'characters' and implicit enumeration in TNT. Symmetrical resampling support is given under the nodes. Abbreviations. – CM, Cardamom Mountains; DK, Dong Paya Yen – Khao Yai Forest Complex; DL, Daen Lao Range; LP, Luang Prabang Range; NST, Nakhon Si Thammarat Range; PM, Petchabun Mountains; PR, Phuket Range; PPR, Phu Pan Range; TH, Tenasserim Hills; TT, Thanon Thongchai Range. Grid-B and Grid-L refer to 1° grids (B and L in Fig. 1A) that were not assigned to any mountain range.
Fig. 1 in Areas of endemism in Thailand: has historical partitioning between seasonally dry lowland and aseasonal moist mountain forests shaped biodiversity in Southeast Asia?
Fig. 1. Maps of Thailand showing: A, Grid of 1° of latitude and longitude denoted by single-letters A–W. Mountain ranges are indicated by two- or three letter codes (CD, DK, DL, LP, NST, PM, PPR, PR, TH & TT) and the grids that comprise each range are colour-coded. Grids B and L were not assigned to any mountain range; B, Species richness (number of species) of Hybos present in 1° grids; C, reciprocal weighted endemicity of Hybos spp. calculated for 1° grids.
Fig. 5 in Two new species of the genus Deuteraphorura Absolon, 1901 (Hexapoda, Collembola, Onychiuridae) from Georgian caves with remarks on the subterranean biodiversity of the Caucasus Mountains
Fig. 5. Deuteraphorura kozmani Parimuchová, Barjadze & Kováč sp. nov. a. Dorsal chaetotaxy. b. AOIII. c. MVO (enlargment of modified chaeta). d. Tita and claw of leg III (DIC contrast image; chaeta in C-row not visible from this view).
Fig. 3 in Two new species of the genus Deuteraphorura Absolon, 1901 (Hexapoda, Collembola, Onychiuridae) from Georgian caves with remarks on the subterranean biodiversity of the Caucasus Mountains
Fig. 3. Histogram of COI K2P distances between specimens of Deuteraphorura Absolon, 1901. The red line indicates the threshold distance above which specimens are considered to belong to different species, according to ASAP method.
Fig. 2. A in Two new species of the genus Deuteraphorura Absolon, 1901 (Hexapoda, Collembola, Onychiuridae) from Georgian caves with remarks on the subterranean biodiversity of the Caucasus Mountains
Fig. 2. A neighbour-joining tree (NJ) with species delimitation of Georgian cave populations of Deuteraphorura Absolon, 1901 based on COI molecular marker, morphology and geographic location in karst areas. Numbers and coloured columns indicate groups (species) identified by particular methods ASAP (Assemble Species by Automatic Partitioning) and bPTP (Bayesian Poisson tree processes). The question mark (?) indicates ambiguous result in Shvilobisa Cave due to low number of studied specimens. For abbreviations of caves in the NJ tree see Table 1.
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