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zenodo28/100

FIGURE 3 in Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications

FIGURE 3. (Continued)

opennotspecifiedDec 2016View details →
zenodo28/100

FIGURE 3 in Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications

FIGURE 3. (Continued)

opennotspecifiedDec 2016View details →
zenodo28/100

FIGURE 3 in Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications

FIGURE 3. (Continued)

opennotspecifiedDec 2016View details →
zenodo28/100

TABLE 1 in Systematics, palaeoecology and taphonomy of Turonian oysters from the northern Gabon Coastal Basin

TABLE 1. — List of oyster fauna of Libreville.After Lombard (1930),Dartevelle & Freneix (1957), Musavu Moussavou et al. (2013a, 2014a) and the present study.

opennotspecifiedJul 2017View details →
zenodo28/100

Fig. 6 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication

Fig. 6. Stromatoporoid Clathrocoilona spissa (Lecompte, 1951), from the Jiwozhai reef, Jiwozhai Member, Dushan Formation, Givetian, Middle Devonian; Dushan, Guizhou, South China. A. NIGP 177048; A1, longitudinal section showing the contemporarily encrusting layers, with black and white rectangles illustrating details; A2, A3, enlargement of A1, note the obvious discrepancy between different areas in the same stromatoporoid: the condensed skeletons of A2 are similar to Clathrocoilona spissa (Lecompte, 1951) and thin laminae of A3 are consistent with Clathrocoilona obliterata (Lecompte, 1951). B. NIGP 177049; B1, longitudinal section, note the intra-specific variations (white arrows) of the lower irregular layers similar to Clathrocoilona crassitexta (Lecompte, 1951) and the upper regular layers identical to Clathrocoilona obliterata (Lecompte, 1951); B2, tangential section.

opencc-by-4.0Jul 2022View details →
zenodo28/100

Fig. 9 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 9. Neritariid gastropods Dentineritaria neritina (Münster, 1841) from Lago Antorno (A) and Misurina Landslide (B, C), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12801, in apertural (A1) and apical (A2) views; A3, end of smooth larval shell well visible in oblique lateral view. B. PZO 12683, in apertural (B1) and abapertural (B2) views. C. PZO 12684 in apical view.

opencc-by-4.0Jan 2021View details →
zenodo28/100

FIGURE 4 in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 4. Google Earth© (2020) image showing approximate positions of the three caves on the peninsula surveyed by Veth.

opencc-by-4.0Dec 2021View details →
zenodo28/100

FIGURE 1 in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 1. Map of the northwest coast of Western Australia showing the relation between the Montebello and Barrow Islands and Cape Range peninsula.

opencc-by-4.0Dec 2021View details →
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FIGURE 7 in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 7. Spindle plot of the relative abundances of the species present in three or more spits in the Morgan's Cave deposit, plus all the species recorded in the Barrow Island owl pellet sample, showing the decrease in abundance of sand plain specialists such as Notomys alexis, and the increase in non-sand plain specialists such as Pseudomys nanus.

opencc-by-4.0Dec 2021View details →
zenodo28/100

FIGURE 2. A in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 2. A close-up map of Barrow and Montebello Islands, showing bathymetry of the area around the islands. The 10 m isohyet shows the outline of the "super-island", created when sea levels cut off the islands from the mainland and discussed below.

opencc-by-4.0Dec 2021View details →
zenodo28/100

FIG. 6 in The Pleistocene Conidae (Mollusca: Gastropoda) from the island of Rhodes (Greece) and their palaeoecological significance

FIG. 6. — Conus (Lautoconus) sp. from the Pleistocene of Tsampika, Rhodes (Greece) under natural (A1, A2, A5, A6) and UV (A3, A4, A7) light: A, MNHN.F. A88169. Lines on A5 indicate the subsutural flexure. Scale bar: 1 cm.

opencc-zeroJul 2024View details →
zenodo28/100

FIG. 12 in The Pleistocene Conidae (Mollusca: Gastropoda) from the island of Rhodes (Greece) and their palaeoecological significance

FIG. 12. — Distribution of the various species of Conidae found in the Mediterranean regions, during the late Pleistocene and their current distribution: A, Atlantic Ocean; W, western Mediterranean; C, central Mediterranean; E, eastern Mediterranean.

opencc-zeroJul 2024View details →
zenodo28/100

Text-fig. 2. Studied section at the Ďurkovec quarry. Note the co-occurrence of bryozoans and decapod crustaceans. in The Priabonian Bryozoan-Decapod Association From The Borové Formation (The Ďurkovec Quarry, Ne Slovakia) And Its Palaeoecological Implications

Text-fig. 2. Studied section at the Ďurkovec quarry. Note the co-occurrence of bryozoans and decapod crustaceans.

opencc-by-4.0Jul 2012View details →
zenodo28/100

FIG. 5 in Early Eocene Caenogastropods (Mollusca, Gastropoda) from Haymana-Polatl Basin, Central Anatolia (Turkey): taxonomy and palaeoecology

FIG. 5. — Caenogastropods (deposited in the repositories of the General Directorate of Mineral Research and Exploration, Ankara): A, B, N, "Ampullina" cf. vapincana (d'Orbigny, 1850); C, D, "Ampullina" cf. vulcani (Brongniart, 1823); E, F, "Ampullinid" indet.; G, Campanile giganteum (Lamarck, 1804); H-K, Cerithium puigcercosensis (Cossmann, 1897) n. comb.; L, M, "Crommium" sp. 1. Scale bars: 1 cm.

opencc-zeroJun 2011View details →
zenodo28/100

Text-fig. 5. Fossils of some mammalian taxa from Gánovce-Hrádok Neanderthal site. a) Castor fiber – mandible dext. et sin. with incisors and p4 – m3 in lateral (mandible) and occlusal (cheek teeth) views (OF 6664–6665); b) Ursus ex gr. spelaeus – right mandible fragment with m1 – m3 in lateral view (P-unnumbered); c) Coelodonta antiquitatis – p2 sin. in buccal view (OF 7188); d) Equus sp. I (cf. taubachensis) – P3 – M3 dext. in travertine, buccal view (P-14302); e) Equus sp. II (cf. germanicus) – Mt sin. fragment in anterior view (OF unnumbered); f) Alces alces – left maxilla fragment with M1 – M3 in occlusal view (P-14303); g) Mammuthus primigenius – m2 sin. in occlusal view (P-14312); h) Palaeoloxodon antiquus – palate fragment with M3 dext. et sin. in occlusal view (P-14281). 50 mm scale is for a–c, 100 mm scale is for d–h. in Revised Floral And Faunal Assemblages From Late Pleistocene Deposits Of The Gánovce-Hrádok Neanderthal Site -Biostratigraphic And Palaeoecological Implications

Text-fig. 5. Fossils of some mammalian taxa from Gánovce-Hrádok Neanderthal site. a) Castor fiber – mandible dext. et sin. with incisors and p4 – m3 in lateral (mandible) and occlusal (cheek teeth) views (OF 6664–6665); b) Ursus ex gr. spelaeus – right mandible fragment with m1 – m3 in lateral view (P-unnumbered); c) Coelodonta antiquitatis – p2 sin. in buccal view (OF 7188); d) Equus sp. I (cf. taubachensis) – P3 – M3 dext. in travertine, buccal view (P-14302); e) Equus sp. II (cf. germanicus) – Mt sin. fragment in anterior view (OF unnumbered); f) Alces alces – left maxilla fragment with M1 – M3 in occlusal view (P-14303); g) Mammuthus primigenius – m2 sin. in occlusal view (P-14312); h) Palaeoloxodon antiquus – palate fragment with M3 dext. et sin. in occlusal view (P-14281). 50 mm scale is for a–c, 100 mm scale is for d–h.

opencc-by-4.0Aug 2017View details →
zenodo28/100

Figure 9 in The skull and the palaeoecological significance of Labidosaurus hamatus, a captorhinid reptile from the Lower Permian of Texas

Figure 9. Labidosaurus hamatus opisthotics. Right opisthotic of MCZ 8727 in dorsal (A), ventral (B), posterior (C), anterior (D), distal (E), and proximal (F) views. Left opisthotic of CM 73370 in dorsal (G), ventral (H), posterior (I), anterior (J), and proximal (K) views.

opencc-by-4.0Feb 2007View details →
zenodo28/100

Fig. 1 in The geological setting and palaeoenvironmental and palaeoecological reconstructions of the Upper Permian insect beds at Belmont, New South Wales, Australia

Fig. 1. (A) Outline map of Australia; (B) Outline map of New South Wales; (C) Map of Lake Macquarie area. The study area is enclosed in the rectangle.

opencc-by-4.0Apr 2007View details →
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Fig. 8 in The geological setting and palaeoenvironmental and palaeoecological reconstructions of the Upper Permian insect beds at Belmont, New South Wales, Australia

Fig. 8. Analysis of insect orders by number and percentage of individual insects (not total specimen numbers), Belmont insect beds, based upon new Beattie collection (2002–2004).

opencc-by-4.0Apr 2007View details →
dryad28/100

Data from: Palaeoecological implications of the preservation potential of soft-bodied organisms in sediment-density flows: testing turbulent waters

Open the record for dataset details and reuse information.

publicMay 2017View details →
dryad28/100

Data from: Palaeoecological inferences for the fossil Australian snakes Yurlunggur and Wonambi (Serpentes, Madtsoiidae)

Open the record for dataset details and reuse information.

publicFeb 2018View details →

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