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Fig. 5 Foraminifera. a-i in Upper Jurassic To Lowermost Cretaceous Microfossils From The Hăghimaş Mountains (Eastern Carpathians, Romania)

Fig. 5 Foraminifera. a-i Bramkampella arabica Redmond. Longitudinal (subaxial) (a, b), longitudinal-tangential (c), oblique (d, e, h), and transverse (f, g, i) sections; thin section FO4. j Textularia sp., thin section FO1-G(2). k-m Mayncina sp. k – thin section FO9B; l, m – thin section FO9A. n, o Protopeneroplis cf. ultragranulata (Gorbatchik). Subaxial (n) and subequatorial (o) sections; thin section FO1-H(2). p Nautiloculina cf. bronnimanni Arnaud-Vanneau & Peybernès, subaxial section; thin section FO1- H(2). q, r Reophax spp. q – thin section FO9-A; r – thin section FO5.

Fig. 4 Calcareous algae. a-e in Upper Jurassic To Lowermost Cretaceous Microfossils From The Hăghimaş Mountains (Eastern Carpathians, Romania)

Fig. 4 Calcareous algae. a-e Actinoporella/Clypeina sp. Different sections through laterals; a, d – thin section FO7-A; b, c – thin section FO7-C; e – thin section FO1-H. f-h Salpingoporella pygmaea (Gümbel). Oblique (f, g) and transverse (H) sections; f, g – thin section FO1-H(2); g – thin section FO1-H. i Charophyte gyrogonite; j, k Terquemella sp.; thin section FO8. l Rajkaella bartheli Bernier. Section of the distal part of the primary lateral and the secondary laterals; thin section FO4.

Fig. 3 in Upper Jurassic To Lowermost Cretaceous Microfossils From The Hăghimaş Mountains (Eastern Carpathians, Romania)

Fig. 3 Succession of the Upper Jurassic limestones in the FO2 profile with the stratigraphic range of the identified microfossils.

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Fig. 1a in New Species Of The Lower Cretaceous Genus Matheronia Munier-Chalmas (Bivalve Hippuritida) In Romania

Fig. 1a. Geographic distribution of Lower Cretaceous rudist bearing localities in Romania, with location of Matheronia beds. b. Geological map of the Nera valley area (Reşiţa-Moldova Nouă zone). c. Geological map of the Cornet area (Pădurea Craiului). d. Geological map of the area north of Dobreşti (Pădurea Craiului).

Fig. 7 Planktonic crinoids. a-w in Upper Jurassic To Lowermost Cretaceous Microfossils From The Hăghimaş Mountains (Eastern Carpathians, Romania)

Fig. 7 Planktonic crinoids. a-w Saccocoma sp. Different sections of secondibrachials. a, v – thin section FO2-B1C(2); b, u – thin section FO2-A1(2); c – thin section FO2-B10; d, i – thin section FO2-B9; e, k – thin section FO1-D; f, l, m, p, q, t, w – thin section FO1-F2(2); g, r – thin section FO1-F2; h, s – thin section FO2-B6(2); j – thin section FO1-G2.

Fig. 8 Incertae sedis microorganisms and agglutinated worm tubes. a-i in Upper Jurassic To Lowermost Cretaceous Microfossils From The Hăghimaş Mountains (Eastern Carpathians, Romania)

Fig. 8 Incertae sedis microorganisms and agglutinated worm tubes. a-i Crescentiella morronensis (Crescenti) in longitudinal-oblique (a, c, i), oblique (b, d, e, f), and transverse (e, h) sections; a, c – thin section FO1-B (c = closeup view of the middle part in a); b – thin section FO2-B8; d – thin section FO2-A1(3); e, f – thin section FO1-E (f = close-up view of the middle part in e). g – thin section FO1-A1; h – thin section FO2-A1; i – thin section FO1- F2(2). j-n Terebella lapilloides (Münster). Longitudinal (l), longitudinal-oblique (k, n), and transverse (j, m) sections; j – thin section FO2-B10; k – thin section FO1-B; l, m – thin sections FO1-A0; n – thin section FO2-A1.

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Fig. 4 in MITOCHONDRIAL 16S AND 12S rRNA SEQUENCE ANALYSIS IN FOUR SALMONID SPECIES FROM ROMANIA

Fig. 4. Majority with bootstrap support consensus trees for combined data (16S rRNA and 12S rRNA). (a) Combined data Neighbor Joining tree, distance model Kimura 2 Parameters, transition/transversion ratio 2.3; (b) combined data Maximum Parsimony tree; (c) combined data Maxi-

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Fig. 3. Majority with bootstrap support consensus trees for 12S in MITOCHONDRIAL 16S AND 12S rRNA SEQUENCE ANALYSIS IN FOUR SALMONID SPECIES FROM ROMANIA

Fig. 3. Majority with bootstrap support consensus trees for 12S rRNA. (a) 12S rRNA Maximum Parsimony tree; (b) 12S rRNA Neighbor Joining tree, distance model Kimura 2 Parameters, transi-

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Fig. 2. Majority with bootstrap support consensus trees for 16S in MITOCHONDRIAL 16S AND 12S rRNA SEQUENCE ANALYSIS IN FOUR SALMONID SPECIES FROM ROMANIA

Fig. 2. Majority with bootstrap support consensus trees for 16S rRNA. (a) 16S rRNA Neighbor Joining tree, distance model Kimura 2 Parameters, transition/transversion ratio 2.3; (b) 16S rRNA Maximum Parsimony tree; (c) 16S rRNA Maximum Likelihood tree

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Figure 1 in Edaphic Oniscidea, Diplopoda and Chilopoda from Pădurea Călugărească (South-Eastern Romania)

Figure 1. Sampling points locations in Pădurea Călugărească (purple circles) within the three habitats (H1-orange; H2- yellow; H3-red); inset: map of Romania showing the location of Pădurea Călugărească.

FIGURE 9 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 9. Fossil remains of Naja cf. romani from FP 1: A, venom fang (UBB V 969) in anterior view; B-G, presacral vertebrae (UBB V 970/1-4) in dorsal (B, F), ventral (C, G), lateral (D) and anterior (E) views; H-J, caudal vertebra (UBB V 970/5) in dorsal (H), anterior (I) and ventral (J) views. Scale bars (A; B-J) equal 2 mm.

FIGURE 8 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 8. Fossil snake vertebrae from FP 1: A-B, Scolecophidia indet. (UBB V 965/1-2) in dorsal (A) and ventral (B) views; C-I, Natrix sp. (UBB V 967/1-5) in dorsal (C, D, I), ventral (F), anterior (E) and lateral (G, H) views; J, Colubridae indet. (UBB V 968/1) in ventral view. Scale bars (A-B; C-J) equal 2 mm.

FIGURE 7 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 7. Fossil remains of Anguinae indet. sp. 2 from FP 1: A, fragmentary maxilla (UBB V 960/1) in lingual view; B-D, fragmentary dentaries (UBB V 960/2-4 in lingual views; E-F, osteoderms (UBB V 962/3-4) in dorsal view; G-H, presacral vertebra (UBB V 961/1) in dorsal and anterior views. Scale bar equals 2 mm.

FIGURE 6 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 6. Fossil remains of lacertids (A-F) and anguids (G-I) from FP 1: A-C, dentary fragments of Lacertidae indet. sp. 1 (UBB V 957/2-4) in lingual views; D, left dentary of Lacertidae indet. sp. 1 (UBB V 958) in lingual view; E-F, dentary fragments of Lacertidae indet. sp. 2 (UBB V 959/3-4) in lingual views; G-I, presacral vertebra of Anguinae indet. sp. 1 (UBB V 964/1) in ventral, lateral and anterior views; J, fragmentary osteoderm of Anguinae indet. sp. 1 (UBB V 964/2) in dorsal view. Scale bar equals 2 mm.

FIGURE 5 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 5. Fossil remains of Bufotes cf. viridis (A-F) and Pelophylax sp. (G-J) from FP 1: A, sacral vertebra (UBB V 950) in ventral view; B-C, distal fragments of humeri (UBB V 951/1-2) in ventral views; D-F, fragmentary ilia (UBB V 952/1-3) in lateral views; G-H, fragmentary frontoparietals (UBB V 953/1-2) in dorsal (G) and ventral (H) views; I, angulosplenial (UBB V 954/2) in dorsal view; J, fragmentary ilium (UBB V 956) in lateral view. Scale bar equals 2 mm.

FIGURE 4 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 4. Fossil remains of Latonia sp. (A, B) and Pelobates sp. (C-J) from FP 1: A-B, fragmentary ilia (UBB V 944/ 1-2) in lateral views; C, premaxilla (UBB V 945/1) in posterior view; D, angulosplenial (UBB V 946/3) in dorsal view; EF, fragmentary frontoparietal (UBB V 945/2) in dorsal (E) and ventral (F) views; G-H, fragmentary maxillae (UBB V 946/ 1-2 in lingual (G) and (H) labial views; I-J, presacral vertebra (UBB V 947) in ventral (I) and dorsal (J) views. Scale bar equals 2 mm.

FIGURE 3 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 3. Fossil remains of Triturus sp. from FP 1: A, atlas (UBB V 941) in ventral view; B-G, presacral vertebrae (UBB V 942/1-2) in dorsal (B, E), lateral (D, G) and ventral (C, D) views; H, proximal fragment of femur (UBB V 943/1); I, distal fragment of femur (UBB V 943/2). Scale bar equals 2 mm.

FIGURE 1. Geological setting. A in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 1. Geological setting. A, geological map of Moldova region, Romania and location of the Fălciu-Prut 1 fossil site (compiled after: Ionesi (1994) - geology; Săndulescu (1984), Răileanu et al. (2011) - tectonics; Haase et al. (2007) - loess cover); B, lithological log of the FP 1 fossil site.

FIGURE 2 in Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)

FIGURE 2. Fossil remains of Chelotriton sp. from FP 1: A-C, left oticooccipital (UBB V 939) in dorsal (A), ventral (B) and medial (C) views; D-E, fragmentary frontal (UBB V 940/1) in dorsal (D) and ventral (E) views; F-G, fragmentary dentary (UBB V 940/2) in labial (F) and lingual (G) views; H, rib fragment (UBB V 938/4) in lateral view; I-J, presacral vertebrae (UBB V 938/1-3) in ventral (I, J) and dorsal views (K). Abbreviations: coc, occipital condyle; fen, endolymphatic foramen; fov, fenestra ovalis; fpe, perilymphatic foramen; pb, basal process, VII, facial nerve foramen; VIII, auditory nerve foramina; IX + X, glossopharyngeal + vagus nerve foramen. Scale bar equals 2 mm.