Find research datasets worth reusing

Fig. 9 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 9. The buccinid neogastropod Colus? sp. from the middle Eocene Satsop Weatherwax seep deposit, Washington State, USA. A. NRM Mo 185029, small specimen with well-preserved aperture and siphonal canal. B. NRM Mo 185030, larger specimen.

Fig. 14 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 14. The provannid gastropod Provanna fortis sp. nov. from the middle Eocene Satsop Weatherwax seep deposit, Washington State, USA. A. NRM Mo 185027, teleoconch with 2.5 whorls (A1); basal view showing spiral cords and aperture with siphonal notch (A2). B. NRM Mo 185028 (holotype); part of protoconch and teleoconch with 3 strongly angular whorls with spines (B2); close-up on protoconch (B1); spiral suture and fading axial rib (B3); growth increments (B4).

Fig. 2 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 2. Scanned polished slab of carbonate from the middle Eocene Satsop Weatherwax seep deposit showing its main petrographic features.

Fig. 3 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 3. Cross-plot of carbon and oxygen isotope data of the middle Eocene Satsop Weatherwax seep deposit; all values are given relative to the PDB standard.

Fig. 13 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 13. The provannid gastropod Desbruyeresia belliatus sp. nov. from the middle Eocene Satsop Weatherwax seep deposit, Washington State, USA. A. NRM Mo 185022; almost complete specimen showing protoconch with 3 whorls (A1); close-up on protoconch (A2); spire with 2.5 whorls and the spire base with short siphonal notch, arrows pointing to spiral cords (A3). B. NRM Mo 185023; protoconch with 3.5 whorls showing the protoconch-teleoconch transition (B1); close-up of protoconch sculpture (B2); close-up of protoconch-teleoconch transition (arrow) (B3). C. NRM Mo 185024; decollated protoconch and calcareous plug (C1); close-up on protoconch (C2). D. NRM Mo 185025 (holotype) showing protoconch with 3 whorls and teleoconch with 3.5 whorls and an oval aperture. E. NRM Mo 185026, Close-up of specimen with protoconch-teleoconch transition (arrow).

Fig. 12 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 12. The nuculanid bivalve Nuculana acutilineata sp. nov. from the middle Eocene Satsop Weatherwax seep deposit, Washington State, USA. A. NRM Mo 185010, almost complete young specimen with initial part intact (A1); close-up on initial part (A2). B. NRM Mo 185008, left valve in lateral view. C. NRM Mo 185009 (holotype), right valve in lateral view showing interior features. D. NRM Mo 185012, right valve specimen showing interior with hinge, faint muscle scar and pallial line. E. NRM Mo 185011; almost complete adult specimen (E1); close-up of escutcheon and dentition (E2).

Fig. 5 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 5. Unidentified vesicomyid bivalve from the middle Eocene Satsop Weatherwax seep deposit, Washington State, USA. A. NRM Mo 185002; left valve of young specimen showing hinge disrupted by a crack (A1); close-up on hinge and dentition (A2). B. NRM Mo 185005; right valve of young specimen showing hinge and ligament nymph (B1); close-up on hinge and dentition (B2).

Fig. 6 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 6. Gastropod limpets from the middle Eocene Satsop Weatherwax seep deposit, Washington State, USA. A, B. Limpet 1, possibly belonging to the Cocculiniformia. A. NRM Mo 185019 slightly oval specimen in apical (A1) and oblique (A2) views. B. NRM Mo 185020 more rectangular specimen in apical (B1) and oblique (B2) views; close-up of sculpture (B3). C. NRM Mo 185021, limpet 2 in lateral (C1) and apical (C2) views.

Fig. 8 in A middle Eocene seep deposit with silicified fauna from the Humptulips Formation in western Washington State, USA

Fig. 8. The neritimorph gastropod Thalassonerita eocenica Squires and Goedert, 1996a from the middle Eocene Satsop Weatherwax seep deposit, Washington State, USA. A. NRM Mo 185015, specimen with nicely preserved aperture. B. NRM Mo 185016, juvenile specimen; apertural view B1); apical view showing spiral sculpture and outline of protoconch (B2); side view showing spiral sculpture (B3). C. NRM Mo 185017, moderately sized specimen; oblique view showing dissolved interior of shell (C1); apical view showing spiral and reticulate sculpture (C2), note that the distinct, fine ribbing near the aperture is most likely the result of dissolution and not sculpture; close-up of protoconch (C3). D. NRM Mo 185018, juvenile specimen in which the protoconch is preserved as internal mold, showing that its internal walls were dissolved; note also reticulate sculpture.

Fig. 3 in New serpulid polychaetes from the Permian of western Sicily

Fig. 3. Serpulid polychaete "Serpula" calannai sp. nov. (holotype MSNC 4549-33) from the Wordian to upper Permian, "Pietra di Salomone" Limestone, Sicily, Italy. A. Tube fragment before assembling. Growth direction, inferred from the slightly flaring peristomes, marked by an arrow. B. Detail of a peristome and growth lines. C. Longitudinal fracture of tube displaying wall section and inner surface covered by secondary crystals. D. Oblique view of tube showing prominence of ornamentations. E. Detail of C showing layered structure of tube wall, only locally preserved. F. Circular cross section of tube, with relatively thick wall locally showing its likely original layering. All SEM images.

Fig. 2 in New serpulid polychaetes from the Permian of western Sicily

Fig. 2. New serpulid polychaetes from the Wordian to upper Permian, "Pietra di Salomone" Limestone, Sicily, Italy. A. "Serpula" calannai sp. nov. (holotype MSNC 4549-33); general views (A1–A3), cross section of tube, white limestone partly filling lumen (A4). B. "Serpula" prisca sp. nov. (holotype PMC.S5.15.09.2017); general view of anterior end, partially embedded in rock. Arrow indicates growth directions for all tubes.

Fig. 4 in New serpulid polychaetes from the Permian of western Sicily

Fig. 4. Serpulid polychaete "Serpula" prisca sp. nov. (holotype PMC. S 5.15.09.2017) from the Wordian to upper Permian, "Pietra di Salomone" Limestone, Sicily, Italy. A. Central portion of the tube glued together, with only feeble growth lines on its outer surface. B. Tube wall with large secondary calcite crystals pointing to complete recrystallization. C. Close-up of outer surface showing very thin and smooth growth lines. D. Magnification of C, with closely spaced, relatively prominent growth lines, crossed by nearly imperceptible longitudinal striations. All SEM images.

Fig. 3 in Synopsis of the terrestrial vertebrate faunas from the Middle Kura Basin (Eastern Georgia and Western Azerbaijan, South Caucasus)

Fig. 3. Fossil terrestrial mammal sites in Middle Kura Foreland Basin. 1, Iagluja; 2, Tetri Udabnos Seri; 3, Udabno; 4, Kushkuna; 5, Dzedzvtakhevi; 6, Kvabebi; 7, Zemo Melaani; 8, Chachuna; 9, Kotsakhuri; 10, Taribana; 11, Dzhaparidze; 12, Eldari; 13, Palantokan; 14, Yenikend; 15, Vashlovani; 16, Qirmizi Samukh; 17, Kvemo Kedi; 18, Duzdag; 19, Almaly; 20, Karadja.

Fig. 2 in Synopsis of the terrestrial vertebrate faunas from the Middle Kura Basin (Eastern Georgia and Western Azerbaijan, South Caucasus)

Fig. 2. The scheme of migration of the lithofacies of the Miocene deposits of South Kakheti (Middle Kura Basin), adapted from Buleishvili (1960). The Khersonian continental facies, variegated clay of the Eladri Formation, are the thickest in the south-western part of the area; the transition of this continental formation into marine deposits can be traced starting from the Ravine Dibzis; and the marine deposits are the thickest at the mountain EllyarOyugi. Abbreviations: N p, Pontian; N m, Meotian; N s 2, upper Khersonian (upper part of the upper Sarmatian); N s 1, lower Khersonian (lower part 1 1 1 3 1 3 of the upper Sarmatian); N s, Bessarabian (middle Sarmatian); N s, Volhynian (lower Sarmatian); N 2, Tarkhanian, Chokrakian, Karaganian, Konkian 1 2 1 1 1 (middle Miocene).

Fig. 1 in Synopsis of the terrestrial vertebrate faunas from the Middle Kura Basin (Eastern Georgia and Western Azerbaijan, South Caucasus)

Fig. 1. Map of the Caucasus region showing the Tertiary foreland basins. Modified after Mauvilly et al. (2016); Mauvilly (2017). Topographic map from the United States Geological Survey (USGS) earth explorer web-based platform https://earthexplorer.usgs.gov. FB, foreland basin.

Fig. 1 in Crinoids from the Silurian of Western Estonia

Fig. 1. Silurian stratigraphy of Estonia. The majority of the new fossil material is from the West−Estonian islands, represented in the middle of the chart of lithostratigraphic units (based on Hints 2008). D1, Lower Devonian; O, Ordovician; O3, Upper Ordovician.

Fig. 5 in Crinoids from the Silurian of Western Estonia

Fig. 5. Camerate, disparid, and flexible crinoids from the Silurian of Estonia. A. Myelodactylus? sp., TUG 1395−7, Ohesaare Formation (Pridoli), Ohesaare Cliff. Articular facet of columnal. B. Saaremaacrinus estoniensis gen. et sp. nov., holotype, TUG 1395−3, middle Äigu Beds, Kaugatuma Formation (Pridoli), Kaugatuma Cliff. B1, lateral view of theca, interpretation of plates in Fig. 4; B2, tegmen view of theca. C, D. Cicerocrinus osiliensis (Jaekel, 1900), Ohesaare Formation (Pridoli), Ohesaare Cliff. C. TUG 1376−1. C−ray lateral view of calyx. D. GIT 405−242. C−ray lateral view of calyx. E. Protaxocrinus salteri? (Angelin, 1878), TUG 1395−4, Ninase Member, Jaani Formation (Wenlock), Suuriku Cliff. E1, CD interray view of crown and proximal column; E2, CD interray view of calyx, proximal arms and column, note badly beach−worn preservation. F. Caleocrinus balticensis sp. nov., GIT 405−12, Juuru Stage (Llandovery), Heltermaa. D−Ray lateral view of crown. G, H. Desmidocrinus laevigatus sp. nov., middle Äigu Beds, Kaugatuma Formation (Pridoli), Kaugatuma Cliff. G. TUG 1395−1, holotype. G1, oblique D−ray lateral view of calyx; G2, CD−interray lateral view of calyx; G3, D−ray lateral view of incomplete crown. H. TUG 1395−2, paratype. D−ray lateral view of calyx.

Fig. 4 in Crinoids from the Silurian of Western Estonia

Fig. 4. Plate diagrams of Estonian crinoids. A. Saaremaacrinus estoniensis gen. et sp. nov., TUG 1395−3, middle Äigu Beds, Kaugatuma Formation (Pridoli), Kaugatuma Cliff. Normal interray plating (A1), C−ray plating (A2), CD−interray plating(A3), and lateral outline of theca (A4). B. Calceocrinus baliticensis sp. nov, GIT 405−212, Juuru Stage (Llandovery), Heltermaa. D−ray view of crown. C. Protaxocrinus salteri? (Angelin, 1878), TUG 1395−4, Ninase Member, Jaani Formation (Wenlock), Suuriku Cliff. Lateral outline. Plate designations: black, radial plate; ruled, inferradial plate; cross−ruled, radianal plate; stippled, interradial plates or anal plates; P, primanal; X, anal X plate; grey, openings into theca. Scale bars 1 mm.

Fig. 3 in Crinoids from the Silurian of Western Estonia

Fig. 3. Camerate crinoids from the Silurian of Estonia. A, B. Middle Äigu Beds, Kaugatuma Formation (Pridoli), Kaugatuma Cliff. A. Eucalyptocrinites tumidus sp. nov., GIT 405−243. A1, lateral view of crown, note modestly expanding partition plates; A2, basal view of calyx, note nodose calyx plates; A3, tegmen view of crown, note flat tegmen top. B. Calliocrinus sedgwickianus sp. nov., TUG 1395−8. Basal view of a portion of the basal and radial circlets, all circular pits are the trace fossil Oichnus. C. Eucalyptocrinites sp., GIT 405−238, Jaani Formation (Wenlock), Suuriku Cliff. Lateral view of calyx. D. Eucalyptocrinites sp. 2., TUG 1395−13, Ninase Member, Jaani Formation (Wenlock), Panga Cliff. D1, tegmen view of crown; D2, B−ray view of partial crown, note deep elongate groove on well−preserved partition plate. E. Periechocrinus longimanus (Angelin, 1878), GIT 405−4−1, Jaani Formation (Wenlock), Janni Cliff. Lateral view of partial calyx, calyx sutures very indistinct. F. Eucalyptocrinites sp. 1, TUG 1375−3, Jaani Formation (Wenlock), Undva Cliff. Lateral view of broken crown. G. Calliocrinus sp., TUG 1395−6, Ninase Member, Jaani Formation (Wenlock), Suuriku Cliff. Broadly bifurcating spine. H. Eucalyptocrinites sp. 1, TUG 1375−2, Jaani Formation (Wenlock), Undva Cliff. Lateral view of crown of juvenile. Scale bars 10 mm.

Fig. 6 in Crinoids from the Silurian of Western Estonia

Fig. 6. Crinoids from the Silurian of Estonia, middle Äigu Beds, Kaugatuma Formation (Pridoli, Silurian), Kaugatuma Cliff. A. Cladida indet., TUG 1395−9, lateral view of badly disarticulated calyx. B. Enallocrinus sp. holdfast, TUG 1395−39, column of Enallocrinus holdfasts lacking the rhizoids. C. Field photograph of an uncollected in situ Enallocrinus holdfast. Note wide, pentalobate lumen and long radices of holdfast. Scale bars 10 mm.