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Fig. 3 Upper Jurassic foraminifers from the Ardeu Unit. a-c in Foraminiferal Assemblages And Facies Associations In The Upper Jurassic Carbonates From Ardeu Unit (Metaliferi Mountains, Romania)

Fig. 3 Upper Jurassic foraminifers from the Ardeu Unit. a-c Bramkampella arabica Redmond (a - Sample 65, b - Sample 172, c - Sample 146). d Undetermined lituolid (Sample 41). e Kaminskia-type foraminifer with fine canaliculated wall (Sample 66). f-h Everticyclammina praekelleri Banner & Highton (Sample 65). i Alveosepta jaccardi (Schrodt) (Sample 49). j-l Ammobaculites sp. (j - Sample 65, k - Sample 110, l - Sample 95). m-n Charentia evoluta (Gorbachik) (m - Sample 32, n - Sample 45). o-p Protopeneroplis striata Weynschenk (o - Sample 153, p - Sample 212).

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Fig. 4 Upper Jurassic foraminifers from the Ardeu Unit. a-c in Foraminiferal Assemblages And Facies Associations In The Upper Jurassic Carbonates From Ardeu Unit (Metaliferi Mountains, Romania)

Fig. 4 Upper Jurassic foraminifers from the Ardeu Unit. a-c Mohlerina basiliensis (Mohler) (a - Sample 31, b - Sample 14, c - Sample 7). d-e Coscinoconus alpinus Leupold (d - Sample 17, e - Sample 21). f Coscinoconus sp. (Sample 110). g-h Troglotella incrustans Wernli & Fookes (g - Sample 10, h - Sample 85). i Troglotella incrustans associated with a Lithocodium aggregatum oncoid (Sample 85). j-k Redmondoides lugeoni (Septfontaine) (j - Sample 138, k - Sample 45). l Lenticulina sp. (Sample 145). m Nautiloculina bronnimanni Arnaud-Vanneau & Peybernès (Sample 174). n Coscinophragma sp. (Sample 182). o Haddonia sp. (Sample 53). p Neokilianina rahonensis (Foury & Vincent) (Sample 115).

Fig. 2 a in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments

Fig. 2 a Lithostratigraphic succession from Strâmturii Valley and Cioroi-Negru Brook, Cornițel village, Borod Basin (redrawn after MureȘan et al., 1974) showing the units (I, II, III, and IV) defined by Șuraru (1972) and MureȘan et al. (1974). b Detailed studied section near the top of the unit II. Legend: 1 tuffs and tuffites; 2 marls; 3 siltic marls; 4 sandy marls; 5 sandstones; 6 conglomerates; 7 limestones with charophytes; 8 hippuritid-bearing limestones; 9 "hippurites reefs"; 10 corals; 11 gastropods; 12 bivalves; 13 foraminifera; 14 rudists; 15 charophytes; 16 palynomorphs.

Fig. 7 a, b Bournonia excavata d in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments

Fig. 7 a, b Bournonia excavata d'Orbigny, 1847, (inventory no. 24078 BBU-MPS =no.1246 sample field); a transverse section through RV close to the commissure, showing the myocardinal elements: anterior and posterior tooth and myophores (am, pm) of the opposite valve; b view of flat posteroventral side of RV; c Gorjanovicia endrissi (Böhm)(24079 BBU-MPS) – transverse section of RV showing compact layer, concave ventral band (Vb); Ib- narrow and wide Pb with 3 fine rounded costae; d, e Praeradiolites subtoucasi (Toucas): d transverse section through RV (24080-BBU-MPS), unknown commissure. The outer shell layer from ventral side is eroded thus the radial bands are missing. e transverse section on other specimen (24081-BBUMPS) having outer shell layer partially broken but preserve the myocardinal apparatus. f, g Radiolites squamosus (d'Orbigny): f specimen with both valves showing convex LV, very eroded and the ornamentations of RV consist in dense growth lamellae (sample no. 24082 BBU-MPS); g ventral side of RV of the same specimen showing radial bands (Vb and Pb) with folds upward to commissure and the narrow interband (Ib). h-i Radiolites nouleti (Bayle)(sample no. 24083 BBU-MPS): h large conical RV, thick-shelled, with dense folded growth lamellae, slightly ondulated in large interband (Ib); i transverse section in RVof the same specimen, showing thick cellular outer shell layer, ligamental ridge and accessory cavities. j, k Sphaerulites boreaui (Toucas)(sample no. 24084 BBU-MPS), j specimen with both valves, top view, showing LV, thin and smaller than lower valve and large RV with expanded, sub-horizontal growth lamellae; k transverse section through RV, showing thickness of cellular

Fig. 4 a, b Microfacies from the first rudist-bearing lithosome. a-e, g in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments

Fig. 4 a, b Microfacies from the first rudist-bearing lithosome. a-e, g bioclastic-intraclastic floatstone/rudstone; bioclasts are poorly sorted with angular to subangular shapes. f bioclastic-extraclastic grainstone. h bioclastic-extraclastic packstone/wackestone.

Fig. 6 a, b in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments

Fig. 6 a, b Extraclastic sediments from the rudist-bearing lithosomes; they are represented by metamorphic lithoclasts (quartzite, crystalline schists), monomineral quartz, muscovite and biotite (crossed polars). c, d Tuffites with altered volcanic glass and various crystalloclasts, angular quartz, biotite and calcite (c- plane-polarized light; d - crossed polars).

Fig. 5 a, b Microfacies from the second rudist-bearing lithosome. a, c-e in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments

Fig. 5 a, b Microfacies from the second rudist-bearing lithosome. a, c-e Bioclastic-extraclastic floatstone; frequent bioclasts are represented by rudist fragments, echinoderm fragments and bivalves fragments; the rudist shells are fragment- ed and perforated (a, d). b Bioclastic-extraclastic rudstone/grainstones with rudist, echinoderm fragments and red algae fragments.

Fig. 8 a-g in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments

Fig. 8 a-g Hippuritella lapeirousei (Goldfuss)(nos. 24085, 24086, 24087, 24088-BBU-MPS). a Transverse section made close to the beak of right valve (RV), the outer shell layer is thick, reaching 3 mm. b RV showing the position of the pillars (P1 and P2) as shallow longitudinal furrows (24085 BBU-MPS). c thin and nearly flat LV very eroded showing remains of radial canals (24085 BBU-MPS). d ventral area of conical, slightly curved RV (24086 BBUMPS) showing the position of the pillars as two shallow longitudinal furrows; e transverse section of RV showing short and rounded pillars (P1 and P2) with the same size (24086 BBU-MPS). f, g transverse sections through specimens (nos. 24087, 24088 BBU-MPS) that have the first pillar (P1) slightly smaller than the second pillar (P2). Note the erosion of the outer shell layer in f) (24087 BBU-MPS). h-i Vaccinites gosaviensis (Douvillé)- transverse section made on two RVs (nos. 23503, 24089 BBU-MPS) showing truncated ligamental ridge (L) and characteristic shape of the pillars. j Vaccinites archiaci (Douvillé), transverse section on RV (no. 24090 BBU-MPS) showing triangular in base and lamelliform ligamental ridge (L), first pillar (P1) thick and shorter and slightly pinched P2. k Vaccinites sulcatus (Defrance) – transverse section on lower valve (no. 23504 BBU-MPS) in which ligamental ridge (L) is wide and short having the same length with first pillar (P1) and second pillar is slightly pinched at its base and curved anteriorly.

Fig. 9 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 9 Geologic cross sections in the northern area of the Ciuc Mountains. The location of cross sections is marked on Fig. 1.

Fig. 5 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 5 Diagram of the lithologic types in the Bistra Sandstone (= Ugra Sandstone) showing binary depositional rhythms, as occurring in the Jandarmului and Ugra valleys.

Fig. 2 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 2 Stratigraphic column of the Cretaceous flysch in the Ciuc Digitation of the Ceahlău Nappe, between the TrotuȘ River and Șulța Streamlet. Legend: 1, marl; 2, marly limestone; 3, sandy limestone; 4, calcarenite; 5, sandstone; 6, marly clay; 7, calcareous breccia; 8, macrofossil occurrence.

Fig. 12 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 12 Peregrinella multicarinata (Lamarck, 1819) [= peregrina von Buch, 1835], Ciugheş Valley, Cădăreşti; 1 well-preserved specimen (LPBIII 376) in 1a – ventral; 1b – lateral; 1c - dorsal views; 2 rock slab with broken shells (LPBIII 376); scale bars represent 2 cm.

Fig. 11 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 11 Geologic cross sections in the GhimeȘ-Palanca region: A – Cross section at the GhimeȘ Pass, at the confluence of the Șanț Streamlet with the TrotuȘ River. B – Cross section at the Palanca Railway Station, at the confluence of the CiugheȘ Valley with the TrotuȘ River; Legend: 1, coarse-grained micaceous sandstone; 2, convolute calcareous fine-grained sandstone; 3, sideritic fine-grained sandstone; 4, red clay with pelosiderites; 5, marly clay; 6, convolute micaceous sandstone; 7, rusty marly limestone.

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Fig. 3 in Gastrointestinal parasite infestation in the alpine mountain hare (Lepus timidus varronis): Are abiotic environmental factors such as elevation, temperature and precipitation affecting prevalence of parasite species?

Fig. 3. Parasite infestation in faeces and ambient temperature. Correlation between parasite infestation in Alpine mountain hare faeces (n = 52) and average, minimal, and maximal temperature found in Vorarlberg (Austria) during the years 2014 and 2015. Count visualises the number of faecal samples. See text for details on statistics.

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Fig. 2 in Gastrointestinal parasite infestation in the alpine mountain hare (Lepus timidus varronis): Are abiotic environmental factors such as elevation, temperature and precipitation affecting prevalence of parasite species?

Fig. 2. Number of parasite types per faeces and severity of parasitic infestation. Correlation between number of parasite types per Alpine mountain hare faeces and severity of parasitic infestation (n = 28) found in Vorarlberg (Austria) during the years 2014 and 2015. Count visualises the number of faecal samples. The severity of infestation is indicated by scattered ((+)), low (+), intermediate (++), and high (+++) infestation. See text for details on statistics.

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Fig. 1. A in Translocation a potential corridor for equine piroplasms in Cape mountain zebra (Equus zebra zebra)

Fig. 1. A map of south-western South Africa, showing the localities of the 3 reserves from which samples were obtained (black circles) namely Mountain Zebra National Park (MZNP), De Hoop Nature Reserve (DHNR) and Karoo National Park (KNP). The grey diamonds show other known municipal nature reserves and national parks which contain Cape Mountain zebra sourced from Cradock, Eastern Cape, South Africa.

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Text-fig. 18. Geographical position of the main palaeobotanical localities in the České středohoří Mountains. 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. 18. Geographical position of the main palaeobotanical localities in the České středohoří Mountains.

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Text-fig. 12. Cladogram showing the systematic position of Protothymallus within the Cyprinidae (for the character states see Tab. 1). in Revision Of The Cyprinids From The Early Oligocene Of The České Středohoří Mountains, And The Phylogenetic Relationships Of Protothymallus Laube, 1901 (Teleostei, Cyprinidae, Gobioninae)

Text-fig. 12. Cladogram showing the systematic position of Protothymallus within the Cyprinidae (for the character states see Tab. 1).

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Text-fig. 4. Protothymallus elongatus (KRAMBERGER, 1885): ventral detail of the neurocranium (SMMGD SaT-168). in Revision Of The Cyprinids From The Early Oligocene Of The České Středohoří Mountains, And The Phylogenetic Relationships Of Protothymallus Laube, 1901 (Teleostei, Cyprinidae, Gobioninae)

Text-fig. 4. Protothymallus elongatus (KRAMBERGER, 1885): ventral detail of the neurocranium (SMMGD SaT-168).