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Fig. 8 in Priabonian, late Eocene chronostratigraphy, depositional environment, and paleosol-trace fossil associations, Pipestone Springs, southwest Montana, USA

Fig. 8. Correlation of Pipestone Springs and Flagstaff Rim upper Eocene lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. → A. Location of Flagstaff Rim (Wyoming) and Pipestone Springs (Montana). B. Pipestone Springs reference section and Flagstaff Rim section showing its lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. Sections are correlated based upon Pipestone Spring's 40Ar/39Ar age of 36.00±0.20 Ma tuff and Flagstaff Rim's Ash B, and on middle Chadronian vertebrate assemblages in the PSMP and between Flagstaff Rim's Ash B to Ash G. 40Ar/39Ar age controls for Pipestone Springs strata are from this study; Flagstaff Rim tuff ages are from Swisher and Prothero (1990), Obradovich et al. (1995), and Sahy et al. (2015) Abbreviations: An, anorthoclase; Bi, biotite; S, sanidine (denote minerals used for single crystal 40Ar/39Ar age analyses of tuffs).

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Fig. 3 in The oldest diving anseriform bird from the late Eocene of Kazakhstan and the evolution of aquatic adaptations in the intertarsal joint of waterfowl

Fig. 3. The intertarsal joint of Recent Anatidae (exemplified by Somateria spectabilis (Linnaeus, 1758), PIN 41-2-2; A) and fossil wading bird (PIN 3104-65; early Eocene of Tsagaan-Khushu locality; southern Mongolia; B) as related to the swimming locomotion. Two types of the general structure of the distal tibiotarsus (A1, B), illustrating the difference in the shape of the condylus medialis (cm1, cm2). Maximal anatomically possible dorsiflexion of the tarsometatarsus in Anatidae, in craniomedial view (A2, showing full contact between the condylus medialis type 2 and the articular surface of the tarsometatarsus), in medial view (A3). Position of the tarsometatarsus relative to the tibiotarsus at the beginning of the propulsive phase of the stride in swimming duck (C) and walking wader (D); note the strongly dorsiflexed tarsometatarsus in the former (modified after Provini et al. 2012; Killbourne et al. 2016). Abbreviations: cm1, cm2; condylus medialis in type 1 and type 2 intertarsal joints (see text). Scale bars 10 mm.

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Fig. 2 in The oldest diving anseriform bird from the late Eocene of Kazakhstan and the evolution of aquatic adaptations in the intertarsal joint of waterfowl

Fig. 2. Tarsometatarsi of anseriform bird Cousteauvia kustovia gen. et sp. nov. and selected modern Anseriformes. A. Cousteauvia kustovia gen. et sp. nov., holotype PIN 2612/4, latest Eocene of Kusto-Kyzylkain, Eastern Kazakhstan, in dorsal (A1), medial (A2), lateral (A3), plantar (A4), angled disto-dorsal (A5), and proximal (A6) views, and distal view on the cross-section (A7). B. Melanitta perspicillata Linnaeus, 1758 (Anatidae), PIN 41-9-1, Recent, in dorsal (B1), medial (B2), plantar (B3), and proximal (B4) views. C. Anas undulata Dubois, 1839 (Anatidae), PIN 40-32-2, Recent, in dorsal (C1) and lateral (C2) views. D. Anseranas semipalmata (Latham, 1798) (Anseranatidae), USNM 621019, Recent, in dorsal (D1) and proximal (D2) views. E. Anhima cornuta (Linnaeus, 1766) (Anhimidae), USNM 345208, Recent, in dorsal (E1) and proximal (E2) views. F. Anas platyrhynchos Linnaeus, 1758 (Anatidae), PIN 40-30-3, Recent, in distal view on the cross-section. G. Clangula hyemalis (Linnaeus, 1758) (Anatidae), PIN 41-7-8, Recent, in distal view on the cross-section. Abbreviations: cdl, dorsolateral crest of the shaft; cdm, dorsomedial crest of the shaft; cl, cotyla lateralis; cm, cotyla medialis; cmh, crista medialis hypotarsi; cpm, crista plantaris medialis; ei, eminentia intercotylaris; fdl, canal for tendon of m. flexor digitorum longus; fic, fossa infracotylaris; fpm, fossa parahypotarsalis medialis; fvp, foramina vascularia proximalia; itc, impressio m. tibialis cranialis; se, sulcus extensorius; sfdl, sulcus for tendon of m. flexor digitorum longus; l, lip-like distal extension of the cotyla lateralis. Scale bars: A1–A5, B1–B3, C, D1, 10 mm; A6, B4, D2, E2, 5 mm; A7, F, G, 2 mm.

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Fig. 1 in The oldest diving anseriform bird from the late Eocene of Kazakhstan and the evolution of aquatic adaptations in the intertarsal joint of waterfowl

Fig. 1. General outline map showing the geographical position of Kazakhstan (A) and Kusto-Kyzylkain locality (asterisk) at Zaysan Basin (B).

Figure 6 in A new Late Eocene cassiduloid (Echinoidea) from Yorke Peninsula, South Australia

Figure 6. Comparative drawings of A, Late Eocene Rhynchopygus? janchrisorum sp. nov. from Yorke Peninsula, South Australia; B, Late Cretaceous (Late Maastrichtian) R. donetzensis from the Severny Donetz Basin, Ukraine (adapted from Smith and Jeffery, 2000); C1, Late Cretaceous (Late? Santonian) R. marmini from La Richardière, Dissay, France; C2, posterior profile of Late Cretaceous (Late Campanian) R. marmini from near Royan and St Palais-sur-Mer, France. Based on published illustrations, latter profile typical of Maastrichtian R. marmini specimens in general. Scale bars 5 mm.

Figure 4 in A new Late Eocene cassiduloid (Echinoidea) from Yorke Peninsula, South Australia

Figure 4. Rhynchopygus? janchrisorum sp. nov. A–C, reconstruction of adapical, right lateral and posterior characteristics of holotype NMV P145616 (actual specimen outline shown with broken line). Scale bar 10 mm.

Figure 2 in A new Late Eocene cassiduloid (Echinoidea) from Yorke Peninsula, South Australia

Figure 2. Rhynchopygus? janchrisorum sp. nov. A–C, adapical, right lateral and posterior views of holotype NMV P145616; D, adoral view of paratype NMV P312115; E, adoral view of paratype NMV P312114; F, adapical view of paratype NMV P312113. All specimens form the Late Eocene Muloowurtie Formation, Yorke Peninsula, South Australia. Scale bar 10 mm.

Figure 1. A and B in A new Late Eocene cassiduloid (Echinoidea) from Yorke Peninsula, South Australia

Figure 1. A and B, general location maps; C, map of St Vincent Basin in relation to Yorke Peninsula, Kangaroo Island and the Fleurieu Peninsula (Maslin Bay), South Australia; D, location of the northernmost exposure (1), and southernmost exposure (2), of the Muloowurtie Formation, west side of Gulf St Vincent.

Figure 5 in A new Late Eocene cassiduloid (Echinoidea) from Yorke Peninsula, South Australia

Figure 5. Rhynchopygus? janchrisorum sp. nov. Drawing of adapical surface of NMV P312113 showing plate structure distal to petals. Scale bar 10 mm.

Fig. 4 - Palinurellusa bericus n in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)

Fig. 4 - Palinurellusa bericus n. sp., es. MSNM i28011, holotype / olotipo. A) Dorsal view / visione dorsale. B) Lateral view / visione laterale. Scale bar equal: 10 mm.

Fig. 2 in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)

Fig. 2 - Quarry at San Feliciano hill. / Cava di SAn Feliciano. A) Calcarenitic levels including corals and decapod crustaceans / visione dei livelli calcarenitici contenenti coralli e crostacei. B) Detail of one calcarenitc level with branched corals (Plocophyllia sp.) / dettaglio di un livello calcarenititco con colonia di coralli ramificati (Plocophyllia sp.). C) Calcarenitic level with coral in section (Plocophyllia sp.) / livello calcarenitico con sezioni di coralli (Plocophyllia sp.).

Fig. 3 - A in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)

Fig. 3 - A) Palinurellus bericus n. sp., reconstruction of the carapace/ Palinurellusa bericus n. sp., ricostruzione del carapace. B) Palinurellus wieneckii (De Man, 1881) (after Holthuis, 1991).

Fig. 1 in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)

Fig. 1 - Berici Mounts with location of the fossiliferous site. / Mappa dei Monti Berici con localizzazione della località fossilifera.

FIG. 11 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 11. — Distribution in percent of specimens by order and species from Mas de Gimel and Naples elaborated from data of Tables 2 and 3: A, color pie chart of Mas de Gimel collection; B, color pie chart of Naples collection. White sections correspond to specimens of indeterminate order or, within an order, of indeterminate specific attribution. Each identified species presents a color variation of the order color section. Percentage number are indicated when superior to one.

FIG. 9 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 9. — Upper deciduous (DP4), premolar (P4) and molars (M1-2-3) of Hartenbergeromys pailladensis n. sp. from the two closely related localities: MGL, Mas de Gimel (Hérault), and NAP, Naples (Hérault): A, UM-MGL-647, right DP4; A1, occlusal view; A2, lingual view; B, UM-NAP-57, enamel cover of a left DP4, unworn: B1, lingual view; B2, occlusal view; C, UM-NAP-59, left P4: C1, occlusal view; C2, labial view; D, UM-NAP-58, left P4, occlusal view; E, MicroCTScan of UM-MGL-601, holotype, unworn left M1: E1, occlusal view; E2, lingual view; E3, labial view; E', same as E (UM-MGL-601), but drawings, to compare both figurations; F, UM-MGL-639, worn right M1: F1, occlusal view; F2, lingual view; G, UM-NAP-47, unworn left M1: G1, occlusal view; G2, lingual view; H, UM-NAP-55, right M1-2, moderately worn, roots partially preserved, occlusal view; I, UM-NAP-48, left M2, moderately worn, roots partially preserved: I1, occlusal view; I2, lingual view; I3, labial view; J, UM-NAP-56, left M3, weakly worn, roots broken; J1, occlusal view; J2, lingual view; J3, labial view; K, UM-NAP-52, right M3, nearly unworn: K1, occlusal view; K2, lingual view; K3, labial view; L, UM-NAP-64, right M3, nearly unworn, roots absent, occlusal view. Scale bar: 1 mm. The background of the profiles is greyed out. On Fig. F open cracks are filled with horizontal stripes.

FIG. 8 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 8. — Equoidea from Mas de Gimel, Naples and Naples 2: A-F, teeth of Propalaeotherium gaudryi (Lemoine, 1878) in occlusal views: left m1-m2 UM-MGL-77 (A), right M1 UM-NAP-103 (B), left M1 UM-NAP2-72L (C), right p4 UM-MGL-26 (D), left p4 UM-MGL-32 (E) and left p3 UM-MGL-73 (F); G-J, teeth of Pachynolophus cf. ruscasseriensis Remy, Krasovec, Lopez, Marandat & Lihoreau, 2019 in occlusal views: broken left M3 UM-MGL-361 (G), right M3 UM-NAP-99 (H), left m2 UM-MGL-369 (I) and right p3 UM-MGL-372 (J). Scale bar: 5 mm.

FIG. 7 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 7. — Large perissodactyl taxa from Mas de Gimel, Naples and Naples 2: A-C, teeth of Hyrachyus stehlini (Depéret, 1904) in occlusal view: right M1 UM-NAP-110 (A), right P3 UM-MGL-515 (B) and right m2 UM-MGL-513 (C); D-F, dental row of Lophiodon cf. leptorhynchum Filhol, 1888: mandible with right and left p2-m3 UM-NAP2-09 in lateral view (D) and occlusal focus on left side (F), right P2-M3 UM-NAP2-73 (E). Scale bars: A-C, 10 mm; D-F, 50 mm.

FIG. 3 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 3. — Apatotheria, Chiroptera, Pantolesta, and Plesiadapiformes from Mas de Gimel and Naples: A, B, molars of Heterohyus sp.: left m1 UM-NAP-16 in occlusal (A1) and labial (A2) views, left m2 UM-MGL-810 in occlusal (B1) and labial (B2) views; C, D, molars of Palaeochiropterygidae gen. et sp. indet.: left m3 UM-MGL-107 in occlusal (C1) and labial (C2) views, right M1 or M2 UM-NAP-19 in occlusal (D1) and lingual (D2) views; E, left P4 UM-MGL-456 of?Icaronycteridae sp. indet. in lingual (E1) and occlusal (E2) views; F, right m1-2 UM-MGL-449 of Palaeochiropteryx cf. tupaiodon Revilliod, 1917 in occlusal (F1) and labial (F2); G, H, molars of Icaronycteris sp.: right m1 or m2 UM-NAP-20 in occlusal (G1) and labial (G2) views, left UM-NAP-21 in occlusal (H1) and labial (H2) views; I, left M1 or M2 UM-MGL-424 of Pantolestidae gen. et sp. indet. in occlusal view; J, left M3 UM-NAP-1 of?Pantolestes sabatieri Smith, 2001 in occlusal view; K, right m2 UM-MGL-741 of Arcius lapparenti in occlusal (K1) and labial (K2) views. Scale bars: A-H, K, 0.5 mm; I, J, 1 mm.

FIG. 6 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 6. — Artiodactyla from Mas de Gimel, Naples and Naples 2: A, B, molars of Protodichobune oweni Lemoine, 1878: right M3 UM-MGL-27 in occlusal view (A), left m1 UM-NAP-78 in occlusal view (B); C-F, teeth in occlusal view of Cuisitherium lydekkeri (Lemoine, 1891): left M1 UM-NAP-82 (C), right p4 UM-NAP2-73L (D), right m3 UM-NAP-76 (E) and right m1 UM-NAP-77 (F); G, right p4 of Eurodexis cf. russelli Sudre & Erfurt, 1996 UM-MGL-491 in occlusal (G1) and lingual (G2) views; H, I, molars of Diacodexis cf. varleti Sudre, Russel, Louis & Savage, 1983: right m2 UM-MGL-811 in occlusal view (H) and left M2 UM-NAP-84 in occlusal view (I); J, talonid of a left m3 UM-MGL-33 of cf. Haplobunodontidae indet. in occlusal view. Scale bar: 2 mm.

FIG. 5 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 5. — Hyaenodontidae and Carnivoraformes from Mas de Gimel: A, trigonid of right lower m1? of Matthodon peignei Solé, Marandat & Lihoreau, 2020 UM-MGL-70 in occlusal (A1) lingual (A2) and labial (A3) views; B, left m3 of Leonhardtina meridianum Solé, Marandat & Lihoreau, 2020 UM-MGL-707 in lingual (B1) and occlusal (B2) views; C, talonid of a left m1 of Lesmesodon gunnelli Solé, Morlo, Schaal & Lehmann, 2021 UM-MGL-36 in occlusal (C1) and lingual (C2) views; D, left M3 of Uintacyon cf. hookeri Solé, 2014 UM-MGL-108 in occlusal (D1) and labial (D2) views. Scale bars: A, 2 mm; B, C, 1 mm; D, 0.5 mm.