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Fig. 5 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 5 Simplified global paleogeograhic reconstruction during the Late Jurassic, based on Scotese (2014: Map 35, Oxfordian) showing potential dispersal routes of caturoids through the Hispanic Corridor. Stars represent the only known records of caturoids outside Europe: 1, "Caturus" dartoni Eastman, 1899, from the lower Sundance Formation in South Dakota (Bathonian); 2, Caturus deani Gregory, 1923, from the Jagua Formation of Cuba (Oxfordian); 3, Catutoichthys olsacheri and Caturoidea sp. from the Vaca Muerta Formation of Argentina (Tithonian)

Fig. 2 Specimen MPCA 632 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 2 Specimen MPCA 632 from the Jurassic of Neuquén, Argentina: a, fossil of Caturidae sp., including disarticulated skull bones described in Bogan et al. (2013); b, corresponding inventory card of the Museo Carlos Ameghino (MPCA)

Fig. 1 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 1 Geographical setting: a, general location; b, simplified map showing outcrops of the Mendoza and Los Menucos groups in the provinces of Neuquén and Río Negro. Outcrops of the Mendoza Group are redrawn from the regional scheme in the geological map HG 3969-I Zapala (Leanza et al., 2001). Outcrops of the Los Menucos Group are redrawn from the regional scheme (esquema regional) in the geological map HG 4169-II Los Menucos (Cuchi et al., 2001)

Fig. 3 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 3 Nannoflora identified in the sediment of MPCA 632: Cyclagelosphaera margerelii (1–4), Crepidolithus sp. (5–6), Watznaueria barnesiae (7–8), Polycostella beckmannii (9–12), Watznaueria britannica (13), Watznaueria fossacincta (14), Watznaueria biporta (15–16)

FIGURE 2 in Late Jurassic jaw bones of Halecomorph fish (Actinopterygii: Halecomorphi) studied with X-ray microcomputed tomography

FIGURE 2. Panoramic view of the highest level of exploitation in Owadów-Brzezinki quarry (i.e., unit III and most fossiliferous 'Corbulomima horizon' occurring in the middle of the quarry wall).

FIGURE 4 in Late Jurassic jaw bones of Halecomorph fish (Actinopterygii: Halecomorphi) studied with X-ray microcomputed tomography

FIGURE 4. Maxillary bone of osteichthyan fish Caturus sp. (ZPAL P.16/O-B/2): 1-2. reconstruction of 3-D 'virtual fossils'— the same specimen after digital processing and analysis of tomographic data (scale bars equal 10 mm). 3. vertical sections of Caturus sp. teeth. 4. just after discovery.

FIGURE 1 in Late Jurassic jaw bones of Halecomorph fish (Actinopterygii: Halecomorphi) studied with X-ray microcomputed tomography

FIGURE 1. Map of Poland (1) with the location of the Owadów-Brzezinki Quarry (2B) near Tomaszów Mazowiecki.

FIGURE 3 in Late Jurassic jaw bones of Halecomorph fish (Actinopterygii: Halecomorphi) studied with X-ray microcomputed tomography

FIGURE 3. Jaw bone of osteichthyan fish Furo sp. (ZPAL P.16/O-B/1): 1-2. 3-D model of 'virtual fossils'—a different view of the same specimen after digital processing and analysis of tomographic data. 4. vertical sections of Furo sp. teeth. 5. 3-D printed dentary – 'virtual fossils'. 6. specimen in piece of limestone (scale bars equal 10 mm).

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Fig. 4 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 4 Stratigraphic distribution of the nannotaxa identified in MPCA 632. Plots von Nannotax 3