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Figure 24. Bulungamayine P3s and p3s. a, b in A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia

Figure 24. Bulungamayine P3s and p3s. a, b, occlusal stereopair of NTMAG P2786-1, LP3; c, d, occlusal stereopair of NTMAG P8663-3, Rp3; e, f, occlusal stereopair of NTMAG P9272-11, Lp3. Scale bar = 12 mm for a and b, 6 mm for c-f.

Figure 20 in A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia

Figure 20. Molars referred to Phalangerida incertae sedis. a, b, occlusal stereopair of NTMAG P9215-12, Rm1; c, d, occlusal stereopair of NTMAG 9215-11, Rm2; e, lingual view of NTMAG P9215-11; f, lingual view of NTMAG P9215-12; g, buccal view of NTMAG P9215-11. Scale bar = 2 mm.

Figure 13 in A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia

Figure 13. Slabbed face of Microsite sample, showing oncoids and cross-sections of the gastropods Glyptophysa and Melanoides. Scale bar is 1 cm.

Figure 25. Bulungamayine molariform teeth. a, b in A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia

Figure 25. Bulungamayine molariform teeth. a, b, occlusal stereopair of NTMAG P8697-8, RM2/3; c, d, occlusal stereopair of NTMAG P874-1, LM3; e, f, occlusal stereopair of NTMAG P9464-190, Lm2; g, h, occlusal stereopair of NTMAG P9464-217, Rm2; i, j, occlusal stereopair of NTMAG P9272-10, Ldp3. Scale bar = 3 mm.

Figure 5 in A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia

Figure 5. Stratigraphic chart for Small Hills showing units from which fossil sites derive and their relationships.

opencc-by-4.0Mar 2024View details →

FIGURE 1 Paleogeographic and geological setting. A in New Miocene fossil taxa illuminate the evolution and paleobiogeography of the Ponto-Caspian gammaroid amphipod radiation

FIGURE 1 Paleogeographic and geological setting. A) Map of the Ponto-Caspian region. The area marked with transparent white indicates the maximum extent of the Paratethys 11 Ma ago (Palcu et al., 2021). The green dot represents the newly discovered fossil amphipod sites from Romania, while the black dots indicate previously known fossiliferous locations from the Caucasus (Azerbaijan and Russia). B) Close-up map of Iași City, Romania, (https://www.openstreetmap.org /#map=12/47.1449/27.6062) showing the location of the study sites (Site 1 – construction site in Iași City; Site 2 – Vlădiceni quarry). C) Upper part shows a chronostratigraphic chart of the Eastern Paratethys and its correlation to the Global Time Scale (Raffi et al., 2020). The stratigraphic age of the sites from this study are indicated with green, while the previously known sites from the Caucasus are indicated with black. The lower part is a geological cross section of the focal area indicating the lithostratigraphic context and altitude (modified after Ionesi et al. 2005). Sampling sites are indicated with green dots. D) Photographs of the two study sites from the current study. PHOTO BY IONESI V.

opencc-by-4.0Jun 2022View details →

Fig. 2 Geological section across the S in Valanginian Radiolarians Of Ne Sardinia (Italy) In The Frame Of The Weissert Event

Fig. 2 Geological section across the S'Ozzastru area (trace A-A' in the geological map of Fig. 1). Legend: a - Recent and present alluvial deposits (Holocene). b - Cuccuru 'e Flores Conglomerate: sandstone and breccia (middle Eocene). c - Siniscola Marl: marl (1) and marly limestone (2) (late Valanginian). d - Schiriddè Limestone: cherty limestone (early Valanginian). e - Monte Bardia Limestone: limestone (early Tithonian - late Berriasian). f - S'Adde Limestone: limestone and cherty limestone (latest Bathonian - earliest Tithonian). g - Dorgali Formation: dolostone (middle-late Bathonian). h - Metamorphic basement (Palaeozoic). i - Fault (modified from Bottini et al., 2018).

Figure 24 in A description of Echinorhynchus baeri Kostylew, 1928 (Acanthocephala: Echinorhynchidae) from Salmo trutta in Turkey, with notes on synonymy, geographical origins, geological history, molecular profile, and X-ray microanalysis

Figure 24. The printout for the elemental scan (EDXA) for the miniature apical hook at the apex of the E. baeri proboscis. Note the drop in calcium and phosphorus peaks compared to that of normal hooks (Fig. 23).

Figure 1 in A description of Echinorhynchus baeri Kostylew, 1928 (Acanthocephala: Echinorhynchidae) from Salmo trutta in Turkey, with notes on synonymy, geographical origins, geological history, molecular profile, and X-ray microanalysis

Figure 1. Collection site of Echinorhynchus baeri from Salmo trutta in the Kilise Stream, Murat River, Turkey.

Figure 23 in A description of Echinorhynchus baeri Kostylew, 1928 (Acanthocephala: Echinorhynchidae) from Salmo trutta in Turkey, with notes on synonymy, geographical origins, geological history, molecular profile, and X-ray microanalysis

Figure 23. The printout of the elemental scan (EDXA) for the common large hooks for E. baeri. Note height of calcium and phosphorus peaks.

Figures 11–16 in A description of Echinorhynchus baeri Kostylew, 1928 (Acanthocephala: Echinorhynchidae) from Salmo trutta in Turkey, with notes on synonymy, geographical origins, geological history, molecular profile, and X-ray microanalysis

Figures 11–16. SEM of mature specimens of Echinorhynchus baeri from S. trutta in Turkey. 11. Proboscis of a female specimen. Note variation in hook size; smaller hooks at base 12. Anterior hooks. Note indentation at the base of the hooks (arrow). 13. Double miniature hooks at apical end of proboscis (arrow); occasionally one miniature apical hook present. 14. Higher magnification of an apical hook; note perforations. This hook has a low Ca reading (see EDAX data). 15. A gallium cut normal hook from the mid-proboscis. Note prominent calcified root. 16. A gallium cut miniature apical hook. Note the hollow base and absence of roots.

Figures 3–10 in A description of Echinorhynchus baeri Kostylew, 1928 (Acanthocephala: Echinorhynchidae) from Salmo trutta in Turkey, with notes on synonymy, geographical origins, geological history, molecular profile, and X-ray microanalysis

Figures 3–10. Specimens of Echinorhynchus baeri collected from Salmo trutta in Turkey and proboscis hook rows of specimens of E. sevani and E. baeri, respectively, collected from Salmo ischchan in Lake Sevan, Armenia. 3. A male specimen. Note the unique amoeboid, lobulated giant nuclei in the long lemnisci (arrow), the prominent retractor muscles, and the near contiguous ovoid-elongate testes. Proboscis is usually bent ventrad. 4. A gravid female with typically long lemnisci. The reproductive system is obscured by eggs. 5. The female reproductive system. Note the very long and slender uterus and the longitudinal bulge near its distal end (upper arrow). Also note the laterally extending uterine glands at the base of the uterine bell (lower arrow). 6. The proboscis of the male specimens in Fig. 3. Note the uninucleated round cells (arrow). 7. A ripe egg with prominent polar prolongation of the fertilization membrane. 8. A ventral row of proboscis hooks from a male specimen. Note the lack of root manubria anteriorly and the gradual development of manubria with decreasing size of roots posteriorly. 9. Lateral view of hooks of E. sevani after Dinnik (1932) showing variable manubriation in all hook roots ''A = first two hooks. B & C = middle hooks, D & E = last two hooks of the vertical row.'' Measurement bars were not provided. 10. Lateral view of hooks of E. baeri after Kostylew (1928) showing the absence of manubria in all hook roots and the virtual absence of roots of the basal hook; measurement bars were not provided.

Figures 17–22 in A description of Echinorhynchus baeri Kostylew, 1928 (Acanthocephala: Echinorhynchidae) from Salmo trutta in Turkey, with notes on synonymy, geographical origins, geological history, molecular profile, and X-ray microanalysis

Figures 17–22. SEM of mature specimens of Echinorhynchus baeri from S. trutta in Turkey. 17. Sensory pore (arrow) at the base of the proboscis. No micropores here. 18. Epidermal micropores at midtrunk. 19. The posterior end of a female specimen showing terminal gonopore. 20. Egg mass from a dissected female specimen. 21. Bursa of a male specimen. 22. The opening of the bursa showing one ring of sensory knobs (arrow).

Figure 2 in A description of Echinorhynchus baeri Kostylew, 1928 (Acanthocephala: Echinorhynchidae) from Salmo trutta in Turkey, with notes on synonymy, geographical origins, geological history, molecular profile, and X-ray microanalysis

Figure 2. The drainage system of the historic Inner Anatolian freshwater Lake of the Middle Miocene-Pliocene period based on Demirsoy (2008). The drainage is shown to include the Aras, Murat, and Euphrates rivers. Striped lines mark the present borders and coasts of Turkey.

opencc-by-4.0Dec 2021View details →

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.

opencc-by-4.0Dec 2020View details →

FIGURE 1. General geological settings. 1 in Bone histology reveals the first record of titanosaur (Dinosauria: Sauropoda) from the Late Cretaceous of Bulgaria

FIGURE 1. General geological settings. 1, Tectonic map of Bulgaria (after Ivanov, 2017); 2, Geological scheme for part of the Western Srednogorie zone and position of the dinosaur bone locality (after Sinnyovsky et al., 2012; simplified).

Fig. 13 - A in The Unnamed Plateau (Western Desert of Egypt). New geological and geoarchaeological data from an exploration in a remote area

Fig. 13 - A) Bottom of the basin; in the background, the damming dunes. / Fondo del bacino formatosi alla base delle dune; le dune di sbarramento sullo sfondo. B) Cemented sands cropping out at the bottom of the basin. / Sabbie cementate sul fondo del bacino. C) Bleached sand. / Sabbia sbiancata. D) Thin rhizocretions. / Sottili rizoconcrezioni. E) A fine-grained conglomerate grinding slab. / Macina in conglomerato fine. F) Quartz artifacts. / Manufatti in quarzo. G-I) Blade industry on quartzite and a core. / Industria laminare su arenaria silicizzata e nucleo.

Fig. 8 - A in The Unnamed Plateau (Western Desert of Egypt). New geological and geoarchaeological data from an exploration in a remote area

Fig. 8 - A) The well-defined mountain pass. / Passo di montagna ben evidente. B) View of the western valley (Area 5) from the pass. The downhill path is visible on the left. / Vista sulla vallata occidentale (Area 5) dal passo. Il sentiero di discesa è visibile sulla sinistra.

Fig. 12 - A in The Unnamed Plateau (Western Desert of Egypt). New geological and geoarchaeological data from an exploration in a remote area

Fig. 12 - A) Some artifacts found at our camp. / Alcuni manufatti rinvenuti presso il nostro campo. B) Quartz vein in the red granite. / Vena di quarzo nel granito rosso.

Fig. 14 - A in The Unnamed Plateau (Western Desert of Egypt). New geological and geoarchaeological data from an exploration in a remote area

Fig. 14 - A) Rock panel with three engraved giraffes, plus an undefined quadruped, perhaps another giraffe. / Pannello su roccia raffigurante tre giraffe martellinate, più altro quadrupede indecifrabile, forse una quarta giraffa. B) Imprint of fossil macroflora, possibly Cordaites sp. (30-35 cm). / Impronta di macroflora fossile, probabilmente Cordaites sp. C) Contact between two alternating metamorphic rocks pertaining to the Anatexite Formation. / Contatto tra due unità metamorfiche che si alternano nell'ambito della Anatexite Formation. D) Stone line crossing the riverbed of a tributary of the western valley. /Allineamento di pietre che attraversa l'alveo di un affluente della vallata occidentale. E) Thick playa deposits incised by a tributary; the author for scale. / Spessi depositi di playa erosi da un affluente; l'autrice come scala.