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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.

FIGURE 6. Shaded coloured 3D in Elongated theropod tracks from the Cretaceous Apenninic Carbonate Platform of southern Latium (central Italy

FIGURE 6. Shaded coloured 3D photogrammetric model of footprint F1 and F2 with relative section (S4) passing through the metatarsal impression and digit III.

FIGURE 5. Shaded coloured 3D in Elongated theropod tracks from the Cretaceous Apenninic Carbonate Platform of southern Latium (central Italy

FIGURE 5. Shaded coloured 3D photogrammetric model of footprint F3 and relative sections (S1, S2, S3).

FIGURE 2 in Elongated theropod tracks from the Cretaceous Apenninic Carbonate Platform of southern Latium (central Italy

FIGURE 2. Thin sections of the trampled block. 1, Nezzazata isabellae; 2, Cuneolina sliteri; 3, Aligned spathic calcite crystals suggesting emersive condition of the surface during trampling. Scale bar equals 0,5 mm (1 and 2) and 1,5 mm (3).

FIGURE 1 in Elongated theropod tracks from the Cretaceous Apenninic Carbonate Platform of southern Latium (central Italy

FIGURE 1. Map of provenance (black footprint) and present location of the track-bearing block (Lido di Porto Canale-Riomartino, grey spot).

FIGURE 4. 1, Shaded grey 3D in Elongated theropod tracks from the Cretaceous Apenninic Carbonate Platform of southern Latium (central Italy

FIGURE 4. 1, Shaded grey 3D photogrammetric model of the track-bearing block; 2, Shaded coloured 3D photogrammetric model.

FIGURE 3. 1 in Elongated theropod tracks from the Cretaceous Apenninic Carbonate Platform of southern Latium (central Italy

FIGURE 3. 1, The track-bearing block; 2, Close-up of the studied footprints; 3, Orthophoto of the trampled block; 4, Interpretative field drawing (scale bar equals 10 cm); F1, F2 and F3 indicate the three theropod tracks discussed in the text; A-D indicate poorly preserved traces, possibly produced by the trackmaker of F1, F2, and F3.