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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. 5 in Deep-water fossorial shrimps from the Oligocene Kiscell Clay of Hungary: Taxonomy and palaeoecology
Fig. 5. Minor chelae of fossorial shrimp Ctenocheles rupeliensis (Beurlen, 1939), Óbuda in Budapest, Late Kiscellian. A. Left minor propodus (HNHM M.59.4700). B. Right minor propodus (HNHM M.59.4869). C. Minor propodus articulated with dactylus (HNHM M.59.4691). D. Articulated left minor chela (HNHM M.59.4682). All specimens are paralectotypes selected herein. All specimens are figured to the same scale and were covered with ammonium chloride (except D) prior to photography. Photographs by MH.
Fig. 2 in Deep-water fossorial shrimps from the Oligocene Kiscell Clay of Hungary: Taxonomy and palaeoecology
Fig. 2. Fossorial shrimp Lepidophthalmus crateriferus (Lőrenthey in Lőrenthey and Beurlen, 1929) comb. nov., Óbuda in Budapest, Late Kiscellian. A. Left major cheliped of presumed male (HNHM M.59.4684b). B. Isolated left major propodus (HNHM M.59.4690). C. Left major cheliped of presumed male (C 1); neotype herein designated (lectotype of Callianassa brevimanus Beurlen, 1939) (HNHM M.59.4684a). Detail of C 1 under different light angle showing carpus and merus (C 2). Line drawing of merus depicted in C 2 (C 3). Note presence of distal meral hook and blade (see also white arrows in A and C 1). D. Presumed female specimen with both chelae (HNHM M.59.4720). E. Imprint of mesial surface of right major propodus (HNHM M.59.4683). Note setal pits close to upper margin of the chela. All specimens except HNHM M.59.4684a are paralectotypes of C. brevimanus selected herein. All specimens are figured to the same scale and were covered with ammonium chloride (except C ) prior to photography. Photographs by MH.
Fig. 3 in Deep-water fossorial shrimps from the Oligocene Kiscell Clay of Hungary: Taxonomy and palaeoecology
Fig. 3. Fossorial shrimp Lepidophthalmus crateriferus (Lőrenthey in Lőrenthey and Beurlen, 1929) comb. nov., Óbuda in Budapest, Late Kiscellian; presumed male morphotypes unless stated otherwise. A. Right major propodus (KGP-MH OT-007). B. Left major propodus articulated with dactylus of presumed female (KGP-MH OT-003). C. Left major propodus (KGP-MH OT-009). D. Left major propodus (KGP-MH OT-006). E. Fragmentary left major propodus (KGP-MH OT-008). F. Right major propodus (KGP-MH OT-010). G. Right major propodus (KGP-MH OT-001). H. Right major propodus of presumed female (KGP-MH OT-002). I. Right minor propodus of indeterminate sex (KGP-MH OT-011). J. Left major propodus of presumed female KGP-MH OT-005). K. Right minor propodus of indeterminate sex (KGP-MH OT-004). L. Left major dactylus (KGP-MH OT-017). M. Right major dactylus (KGP-MH OT-013). N. Right minor(?) dactylus (KGP-MH OT-012). O. Left major dactylus (KGP-MH OT-016). All elements are depicted in lateral aspect except D–F and J which are depicted in mesial view. All specimens are figured to the same scale and were covered with ammonium chloride prior to photography. Photographs by MH.
Fig. 5 in A proposed ectochory of Galba truncatula snails between wallow sites enhances transmission of Fascioloides magna at gemenc, in Hungary
Fig. 5. Some intact shells and fragments of snails which were recovered from dry mud adhering to a tree trunk near a wallowing site. A relatively fresh and intact shell of G. truncatula (X) can be seen among the brownish pieces of only recently deceased (R) and old, whitish shells of snails.
Fig. 3. G in A proposed ectochory of Galba truncatula snails between wallow sites enhances transmission of Fascioloides magna at gemenc, in Hungary
Fig. 3. G. truncatula snails are foraging adjacent to a fresh faecal ball of red deer. In consequence of their intense foraging activity, they transform the smooth surface of mud rough. (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)
Fig. 4 in A proposed ectochory of Galba truncatula snails between wallow sites enhances transmission of Fascioloides magna at gemenc, in Hungary
Fig. 4. Collection of dry mud-cover from a roadside tree trunk on the bank of a wallow. Thicker trees than the trunk of the bushes are regularly used by wild boars as rubbing poles. The edge of the puddle was trampled by animals.
Fig. 2. Several G. truncatula within a in A proposed ectochory of Galba truncatula snails between wallow sites enhances transmission of Fascioloides magna at gemenc, in Hungary
Fig. 2. Several G. truncatula within a shrinking puddle. The amphibious snails are distributed more or less evenly on the wettest parts of mud but not in the water. A footprint of red deer is on the left. (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)
Fig. 1. A in A proposed ectochory of Galba truncatula snails between wallow sites enhances transmission of Fascioloides magna at gemenc, in Hungary
Fig. 1. A) The 57 sample sites, black circles, for the malacological survey performed at Gemenc. The sites were selected upon discussions with the hunters for water bodies that had known animal water contact. B) A typical puddle on a forest road in Gemenc flood area. Several footprints of game are immersed into the soft mud and the deepest center of the wallowing site rainwater last for month.
Fig. 1 in Threat of cercarial dermatitis in Hungary: A first report of Trichobilharzia franki from the mallard (Anas platyrhynchos) and European ear snail (Radix auricularia) using molecular methods
Fig. 1. Proved occurrence of R. auricularia snails in Hungarian habitats based on museum collections and own investigations. The species was detected in artificial ponds or canals (yellow dots: living specimens; green dots: shells) and also in natural habitats (red dots: living specimens; blue dots: shells). (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)
Fig. 8. a, b in Threat of cercarial dermatitis in Hungary: A first report of Trichobilharzia franki from the mallard (Anas platyrhynchos) and European ear snail (Radix auricularia) using molecular methods
Fig. 8. a, b. Maximum likelihood tree of the samples of Trichobilharzia franki and Bilharziella polonica from the present study (a COI, b 28S) in relation to other schistostomatid sequences deposited in GenBank. Bootstrap values are given at the nodes; posterior probabilities for Bayesian inference are shown behind the bootstrap values. Unsupported nodes by BI are marked with a hyphen. Samples from the present study are in bold. The scale bar indicates the expected number of substitutions per sit.
Fig. 6. A in Threat of cercarial dermatitis in Hungary: A first report of Trichobilharzia franki from the mallard (Anas platyrhynchos) and European ear snail (Radix auricularia) using molecular methods
Fig. 6. A hemalaun-stained Dendritobilharzia male from the liver of a mallard. Every scale under the specimen is equal to a millimetre.
Fig. 3. A in Threat of cercarial dermatitis in Hungary: A first report of Trichobilharzia franki from the mallard (Anas platyrhynchos) and European ear snail (Radix auricularia) using molecular methods
Fig. 3. A complete specimen of native Trichobilharzia male in cell suspension from the liver of a mallard.
Fig. 2 in Threat of cercarial dermatitis in Hungary: A first report of Trichobilharzia franki from the mallard (Anas platyrhynchos) and European ear snail (Radix auricularia) using molecular methods
Fig. 2. The shape of bursa copulatrix of the adult R. auricularia is spherical and the stalk is long (A), while the bursa copulatrix of Radix balthica is oval and stalk is short (B). This anatomical structure seems the most reliable morphological difference to distinguish of the two most common Radix species in Hungary, but can only be studied on sexually mature and non-trematode infected specimens (Juh´asz, 2018) The length of the dissected organs is about 1 cm.
FIGURE 4 in Talpa fossilis or Talpa europaea? Using geometric morphometrics and allometric trajectories of humeral moles remains from Hungary to answer a taxonomic debate
FIGURE 4. Boxplot of the centroid sizes. Bottom and top of the boxes are the first and third quartiles; horizontal solid black lines represent the median; whiskers represent the minimum and maximum values.
FIGURE 3. 1 in Talpa fossilis or Talpa europaea? Using geometric morphometrics and allometric trajectories of humeral moles remains from Hungary to answer a taxonomic debate
FIGURE 3. 1, Scatterplot of the first two axes of the PCA. Deformation grids refer to axes extremes (positive and negative values). 2, Scatterplot of the first and third axes of PCA. Deformation grids refer to axes extremes (positive and negative values).
FIGURE 5. 1 in Talpa fossilis or Talpa europaea? Using geometric morphometrics and allometric trajectories of humeral moles remains from Hungary to answer a taxonomic debate
FIGURE 5. 1, CCA scatterplot of the shape and size variables. 2, Plot of the Euclidean distances between the predicted shape values of Talpa fossilis and T. europaea against 10 discrete CS intervals.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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