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Fig. 1 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 1 Location of the Aptian deposits on the geological map of the northern part of the Piatra Craiului Massif [based on the maps 1:50000, sheets110a to 110d (Dimitrescu et al., 1971; Patrulius et al., 1971; Săndulescu et al., 1972; Dimitrescu et al., 1974), redrawn with minor changes]

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. 12 Supratidal limestones. a in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 12 Supratidal limestones. a Algal-microbial mats; they contain alternations of calcified cyanobacteria and very fine micritic lamine. b Detail from the image a; the cyanobacteria laminae with agglutinated fine peloids and ostracods (indicated by arrows). c, d Fenestral algal/cyanobacterial bindstone; micro-lamination is formed by calcified cyanobacteria filaments; the lower part is composed of rivulariacean-type cyanobacteria; detail at left;

Fig. 5 Pedogenetically altered granular limestones. a, b in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 5 Pedogenetically altered granular limestones. a, b Peloidal-bioclastic grainstone bearing vadoids and black pebbles, micritised intraclasts and meniscus cements. c-d Dissolution features associated with microstalactitic and equigranular cements which are developed arround cavities and grains; cavities are filled with vadose silt in association with large crystals of equigranular calcite.

Fig. 8 a-d in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 8 a-d Normal marine subtidal limestones. Bioturbated bioclastic packstone with dasycladalean algae [Selliporella neocomiensis (Radoičić), Terquemella sp.]; miliolids, ostracods and bivalve fragments.

Fig. 3 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 3 Intraclastic/bioclastic-dominated shoals. a-f Coarse intraclastic-bioclastic grainstone and rudstone containing intraclasts, oncoids, peloids, normal and incipient ooids. g-h Intraclastic-bioclastic grainstone and rudstone with vadoids. Bioclasts are represented by large benthic foraminifera (a, c-d), coral fragments (b, d-e), rivulariacean-type cyanobacteria (e.g. Diversocalis sp.) (c), bivlave fragments, echinoderm fragments, dasycladalean algae [Clypeina sulcata (Alth)] (a) and gastropods (f); intraclasts and blackened bioclasts (black pebbles) (a, c, d, f, h).

Fig. 15 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 15 Limestones from the Padina Brașoavei outcrop (Urdărița horst). The arrows indicate the discontinuity surface.

Fig. 4 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 4 Contact between the intraclastic/bioclastic-dominated shoals (A) and peritidal limestones (B) in the Dâmbovicioara Gorges.

Fig. 11 a in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 11 a Intertidal carbonates (micro-cycles delimitated by firmground type surfaces) (thin section in panorama). Fenestral peloidal-oncoidic grainstone; Millimeter-scale firmgrounds are composed of micritic laminae (arrowed).

Fig. 7 a, b in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 7 a, b Well bedded, decimetre- to meter-thick limestones from the peritidal succession of the Cheile Dâmbovicioarei; c fenestral structures and millimeter to centimeter-thick sets of laminae are present.

Fig. 9 Restricted marine subtidal limestones. a-d in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 9 Restricted marine subtidal limestones. a-d Oncoidal-bioclastic packstone with cyanobacteria nodules.

Fig. 17 Carbonate facies from the breccia levels. a-d in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania

Fig. 17 Carbonate facies from the breccia levels. a-d Peloidal-bioclastic packstone with cyanobacteria, ostracods and foraminifera (d); cavities are filled with vadose silt and gravitational terrigenous material. e-f Breccia with horizontal (e), circumgranular and vertical (f) cracks. Scale-bar = 1 mm.

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Fig. 2 in Comparative microbiomes of ticks collected from a black rhino and its surrounding environment

Fig. 2. (a) The distribution of bacterial taxa at the species level in tick samples collected from Eliska's body and from the field. Each bar depicts the mean relative abundance value of independent replicates. Species comprising more than 1% of reads are shown. Each bar depicts the mean relative abundance value of independent replicates (n = 4 ticks collected from the field; n = 3 ticks collected from Eliska's body). (b) LEfSe analysis of differentially abundant bacterial taxa between ticks collected from Eliska's body and ticks collected from the field. Only taxa meeting an LDA significant threshold of> 2 are shown.

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Fig. 1 in Comparative microbiomes of ticks collected from a black rhino and its surrounding environment

Fig. 1. Box plots showing the alpha diversities (measurement of species richness and evenness within a habitat unit) of: (a) the number of operational taxonomic units (OTUs) found in microbiome taxonomic profiling (MTP); and (b) phylogenetic diversity (abundance); (c) Pielou diversity (equity); and (d) Shannon diversity (measurement of richness and equity in the distribution of species) among the samples from Eliska. Bars indicate the median, and the hinges represent the lower and upper quartiles. In panel (a), there are no statistically significant differences between the two groups. However, in panels (b), (c), and (d), there are statistically significant differences between the two groups. (e) Unweighted pair group method with arithmetic mean (UPGMA) clustering, and (f) principal-coordinate analysis depicting differences in taxonomic compositions of bacterial communities in Amblyomma gemma samples collected from Eliska's body and from the field. * indicates statistical differences between the two groups of ticks (Wilcoxon rank-sum test, p <0.05).