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FIG. 3 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 3. — Spatial distribution of identified vertebrate bodyfossil remains of Angeac-Charente recovered from 2013 to 2018: A, aerial view of the Angeac-Charente site with the location of the manual (R1-3 and CG1-8) excavation plots and some remarkable fossils (drone picture ©D. Abit, July 2017); B, diagram of the Angeac-Charente locality with the position of vertebrate body fossil remains according to taxon type. Each point represents the position of one specimen (3-D SIG data measured from 2013 to 2018 projected with ArcGIS Desktop 10.3.1.). SIG data from the CG1 plot (2010-1012) are lacking (in grey) (See Rozada et al. 2021).

FIG. 1 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 1. — Geographical distribution of the three continental fossil localities documenting the Late Jurassic to Early Cretaceous transition in Western France: Chassiron (Tithonian, Department of Charente-Maritime), Cherves-de-Cognac (Berriasian, Department of Charente) and Angeac-Charente (Berriasian, Department of Charente).

FIG. 4 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 4. — Angeac-Charente synthetic log based on the lithostratigraphic sections of R3, CG3 and CG9, of Rozada et al. (2021), and the main corresponding depositional events. The thickness is measured above and below the Unit 1/Unit 2 limit, which marks the base of the bonebed. Abbreviations: DE, Depositional Event; U, Unit.

FIG. 16 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 16. — Choristoder remains from Angeac-Charente: A-C, anterior dorsal vertebra of cf. Cteniogenys sp. (ANG M-20) in dorsal (A), ventral (B) and posterior (C) views; D, E, juvenile dorsal vertebral centrum (ANG M-47) in ventral (D) and oblique anterior (E) views. Scale bar: A-C, 1 mm; D, E, 200 µm.

FIG. 2 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 2. — Views of the Angeac-Charente gravel quarry: A, CG1 plot at the end of the 2010 excavation campaign; B, CG1 and CG3 plots at the beginning of the 2013 excavation campaign; C, CG4, CG6, CG7 plots (on the left), and CG9 plot (on the right) during the 2018 excavation campaign.

FIG. 14 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 14. — Rhynchocephalian right dentary fragment from Angeac-Charente: A-C, cf. Opisthias sp. (ANG M-120) in labial (A), lingual (B) and dorsal (C) views. Scale bar: 2.5 mm.

FIG. 11 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 11. — Vertebra of Caudata indet. from Angeac-Charente: A-F, (ANG M-71) in anterior (A), posterior (B), left lateral (C), right lateral (D), dorsal (E) and ventral (F) views. Scale bar: 2 mm.

FIG. 13 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 13. — Pleurosternid turtle from the Berriasian of Angeac-Charente: A, carapace of Pleurosternon bullockii (Owen, 1842) (ANG14 R-454) in dorsal view; B, plastron and right peripheral plates 1 and 2 of Pleurosternon bullockii (ANG14 R-474 & ANG15 R-1082) in ventral view. Scale bar: 10 cm.

FIG. 8 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 8. — Actinopterygian remains from the Berriasian of Angeac-Charente: A, isolated tooth of Amiiformes indet. (ANG M-39); B, C, isolated tooth of Amiiformes indet. (ANG M-110); D, dentulous vomerine element of Amiiformes indet. (ANG M-56); E-G, isolated tooth of Ionoscopiformes indet. (ANG M-111); H, jaw frag- ment of Actinopterygii indet. (ANG M-38) in lingual view; I, vertebra of Actinopterygii indet. (ANG M-069). Scale bar: A-C, E-H, 500 µm; D, 250 µm; I, 2 mm.

FIG. 21 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 21. — Ornithischian teeth from Angeac-Charente: A, B, Heterodontosaurid premaxillary tooth of Echinodon sp. (ANG15-R671) in lingual (A) and labial (B) views; C, D, Heterodontosaurid premaxillary tooth of Echinodon sp. (ANG14-3368) in lingual (C) and labial (D) views; E, F, hypsilophodontid premaxillary tooth (ANG M-119) in lingual (E) and labial (F) views; G, H, hypsilophodontid dentary tooth (ANG15-R927) in labial (G) and lingual (H) views; I-L, hypsilophodontid maxillary tooth (ANG 10-153) in lingual (I), distal (J), labial (K) and mesial (L) views. Scale bars: A-D, I-L, 5 mm; E-H, 3 mm.

FIG. 25 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 25. — Sauropod embryonic or hatchling teeth from Angeac-Charente: A, tooth of Macronaria indet. (ANGM-18) in lingual view; B, C, tooth of Turiasauria indet. (ANGM-118) in labial (B) and lingual (C) views. Scale bar: 500 µm.

FIG. 20 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 20. — Pterosaur teeth from Angeac-Charente: A, Pterodactyloidea indet. A (ANG M-24) in labial view; B, Pterodactyloidea indet. A (ANG M-10) in lingual view; C, D, Pterodactyloidea indet. A, (ANG M-42) in lingual (C) and mesial (D) views; E, F, Pterodactyloidea indet. B, (ANG M-43) in lingual (E) and mesial (F) views; G, H, Pterodactyloidea indet. B, (ANG M-112) in lingual (G) and mesial (H) views; I, Pterodactyloidea indet. B, (ANG M-40) in lingual view; J, K, Pterosauria indet. (ANG M-41) in labial (J) and distal (K) views; L, M, Pterosauria indet. (ANG M-113) in lingual (L) and mesial (M) views. Scale bar: 500 µm.

FIG. 24 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 24. — Sauropod teeth from Angeac-Charente: A-D, posterior left maxillary tooth of Turiasauria indet. (ANG11-837) in labial (A), mesial (B), lingual (C) and distal (D) views; E-H, left maxillary tooth of Turiasauria indet. (ANG15-R905) in labial (E), mesial (F), lingual (G) and distal (H) views; I-L, left maxillary tooth of Turiasauria indet. (ANG13-2330) in labial (I), mesial (J), lingual (K) and distal (L) views; M-P, left premaxillary tooth of Turiasauria indet. (ANG14-R289) in labial (M), mesial (N), lingual (O) and distal (P) views; Q-T, dentary tooth of Turiasauria indet. (ANG14-3495) in labial (Q), mesial (R), lingual (S) and distal (T) views; U-X, left dentary tooth of Turiasauria indet. (ANG14- R435) in labial (U), mesial (V), lingual (W) and distal (X) views; Y-AA, maxillary tooth of Macronaria indet. (ANG R-1732) in labial (Y), distal (Z) and lingual (AA) views. Scale bar: A-X, 2 cm; Y-AA, 1 cm.

FIG. 30 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 30. — Ornithomimosaur remains from Angeac-Charente: A-C, proximal end of right tibia (ANG12-1893) in posterior (A), anterior (B) and lateral (C) views; D, distal end of right tibia (ANG10-56) in anterior view; E, proximal end of right fibula (ANG11-696) in medial view; F-H, Left astragalus and calcaneum (ANG12- 1803) in anterior (F), posterior (G) and dorsal (H) views. Scale bar: A-E, 4 cm; F-H, 2 cm.

FIG. 26 in Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary

FIG. 26. — Sauropod caudal vertebrae from Angeac-Charente: A-C, anterior caudal vertebra of Turiasauria indet. (ANG15-R679) in left lateral (A), posterior (B) and dorsal (C) views; D-F, anterior caudal vertebra of Turiasauria indet. (ANG15-R698) in right lateral (D), posterior (E) and dorsal (F) views; G-I, anterior caudal vertebra of Turiasauria indet. (ANG15-R921) in right lateral (G), posterior (H) and dorsal (I) views; J-L, middle caudal vertebra of Turiasauria indet. (ANG15-R652) in right lateral (J), posterior (K) and dorsal (L) views. Scale bar: 10 cm.

Fig. 9 Drumul lui Lehman. a in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 9 Drumul lui Lehman. a The stratigraphic contact between the Valanginian limestones and the monomictic Aptian breccia (marked by white line). b Detail from the contact area. c, d Monomictic breccia. 567, 620 = sample numbers. Scale bar for c and d = 2 cm.

Fig. 8 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 8 Microfossils from the Aptian breccia and conglomerate pebbles in the Padinile Frumoase area. a-c, f, g Unidentified orbitolinids. d Rectodyctioconus giganteus Schroeder. e Mesorbitolina parva (Douglass). h Unidentified?involutinid foraminifer. i Montsalevia salevensis (Charollais, Brönnimann & Zaninetti). j unidentified biserial foraminifer. k Pfenderina neocomiensis (Pfender). l Palorbitolina lenticularis (Blumenbach); m Terebella lapilloides Münster. n Neomeris cretacea Steinmann. o Griphoporella sp. p Carpathoporella occidentalis Dragastan. q Clypeina parasolkani Farinacci & Radoičić. r Lithocodium aggregatum Elliott. s Coscinophragma cribrosa (Reuss). a, b, sample 266; c, e, m, n, p, s, sample 271; d, i, j, k, q, r, sample 275; f, h, o, sample 279; g, sample 272; l, sample 568. Scale bar = 1 mm (a-c, f); 0.5 mm (d, e, g, h, o, q); 0.25 mm (i-m, p).

Fig. 7 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 7 Facies and microfacies from the upper Valanginian (a-b) and Aptian (c-h). a-b Bioclastic intraclastic floatstone. Intraclasts consist of peloidal packstone with echinoderms (a1, b1), bioclastic packstone with sponge spicules and coral fragments (a2), and peloidal packstone with small foraminifera (b2). The matrix (m) contains calpionellids and calcispheres. The arrows in a are delineating the shape of the intraclasts. c Limestone-rich breccia. Clasts are embedded in a micritic/clay-rich matrix that contains silt-sized quartz. The matrix contains orbitolinids (indicated by the small yellow arrows). d Marly clast with bioclasts and glauconite. e Coral-rich bioconstruction with dissolved corals. f Clast containing abundant sponge and Lithocodium crusts (center). In the upper right corner the carbonate components of the clast are dissolved. g Clasts from an orbitolinid-rich peloidal bioclastic grainstone; orbitolinids are present both in the matrix and the clasts. h Clast composed of an orbitolinid/green algae-bearing packstone (left) and clast that contains peloidal fenestral wackestone (right) (detail from photo g). a, b, sample 258; c-f, sample 266; g, h, sample 272. Scale

Fig. 6 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 6 Microfossils from the lower Valanginian limestones and the upper Valanginian limestones/marly-limestones. a-c Pseudocyclammina lituus (Yokoyama); d Coscinoconus cf. cherchiae (Arnaud-Vanneau, Boisseau & Darsac); e-j Montsalevia salevensis (Charollais, Brönnimann & Zaninetti); k-o Meandrospira favrei (Charollais, Brönnimann & Zaninetti); p-s Unidentified calpionellids; t, u Cadosina fusca Wanner; v, w Crustocadosina semiradiata Wanner; x, y Stomiosphaera echinata Nowak. a, h, sample 12817; b, i, sample 256; c, d, sample 257; e, sample 260; f, g, p, u, sample 12818; j, x, y, sample 249; k, r, sample 252; l,q, v, w, sample 12816; m, n, o, s, t, sample 258. Scale bar = 0.5 mm (a-b); 0.25 mm (c-o); 0.125 mm (p-y).

Fig. 3 Padinile Frumoase outcrop a in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 3 Padinile Frumoase outcrop a The lower Valanginian-upper Valanginian unconformity (yellow line) and the transgressive contact between the Valanginian limestones and the Aptian deposits (breccia and conglomerates) (white line). b Monomictic breccia. c The first outcrop located above the contact area (~3m). d Monomictic orthoconglomerates with common carbonate pebbles. e Monomictic paraconglomerates with carbonate pebbles. 272, 280, 291 = sample numbers. Scale bar for b, d, e = 2 cm.