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Figure 6 from: Zhang Q, Zhang J (2019) Contribution to the knowledge of male and female eremochaetid flies in the late Cretaceous amber of Burma (Diptera, Brachycera, Eremochaetidae). Deutsche Entomologische Zeitschrift 66(1): 75-83. https://doi.org/10.3897/dez.66.33914
Figure 6 Zheniaburmensis sp. nov. Photomicrographs, paratype NIGP170826, female A habitus (lateral view) B antenna C wing D tarsus of hindleg E ovipositor (lateral view). Scale bars: 1mm (A, C); 0.1 mm (B, D, E).
Figure 1 from: Zhang Q, Zhang J (2019) Contribution to the knowledge of male and female eremochaetid flies in the late Cretaceous amber of Burma (Diptera, Brachycera, Eremochaetidae). Deutsche Entomologische Zeitschrift 66(1): 75-83. https://doi.org/10.3897/dez.66.33914
Figure 1 Zheniaxiai Q. Zhang et al., 2016. Photomicrographs (A–C) and Confocal microscopic photographs (D, E), topotype NIGP170824, male A habitus (right lateral view) B habitus (left lateral view) C antennae D male genitalia (right lateral view) E male genitalia (left lateral view). Scale bars: 1 mm (A, C); 0.1 mm (B, D, E).
Figure 3 from: Zhang Q, Zhang J (2019) Contribution to the knowledge of male and female eremochaetid flies in the late Cretaceous amber of Burma (Diptera, Brachycera, Eremochaetidae). Deutsche Entomologische Zeitschrift 66(1): 75-83. https://doi.org/10.3897/dez.66.33914
Figure 3 Difference and similarity between two sets of ovipositors. Photomicrographs (lateral view), AZheniaxiai Q. Zhang et al., 2016 (after Grimaldi and Barden 2016, AMNH BuSD-2) BZheniaxiai Q. Zhang et al., 2016 (after Q. Zhang et al. 2016, holotype BA02-15001). Scale bars: 0.1 mm (A, B).
Figure 5 from: Zhang Q, Zhang J (2019) Contribution to the knowledge of male and female eremochaetid flies in the late Cretaceous amber of Burma (Diptera, Brachycera, Eremochaetidae). Deutsche Entomologische Zeitschrift 66(1): 75-83. https://doi.org/10.3897/dez.66.33914
Figure 5 Zheniaburmensis sp. nov. Line drawings, holotype NIGP170825, A habitus (dorsal view) B male genitalia (ventral view) C tarsus of hindleg. Scale bar: 1mm (A); 0.1 mm (B, C).
Figure 4 from: Zhang Q, Zhang J (2019) Contribution to the knowledge of male and female eremochaetid flies in the late Cretaceous amber of Burma (Diptera, Brachycera, Eremochaetidae). Deutsche Entomologische Zeitschrift 66(1): 75-83. https://doi.org/10.3897/dez.66.33914
Figure 4 Zheniaburmensis sp. nov. Photomicrographs (A–C) and Confocal microscopic photograph (D), holotype NIGP170825, male A habitus (dorsal view) B habitus (ventral view) C male genitalia (ventral view) D male genitalia (ventral view). Scale bars: 1 mm (A, B); 0.1 mm (C, D).
Figure 8 from: Zhang Q, Zhang J (2019) Contribution to the knowledge of male and female eremochaetid flies in the late Cretaceous amber of Burma (Diptera, Brachycera, Eremochaetidae). Deutsche Entomologische Zeitschrift 66(1): 75-83. https://doi.org/10.3897/dez.66.33914
Figure 8 Difference and similarity between four sets of ovipositors. Line drawings (lateral view), ARhagoletispomonella (Walsh, 1867) (ovipositor extended, after Cumming and Wood 2009) BRhagoletispomonella (Walsh, 1867) (ovipositor not extended, after Norrbom 2010) CZheniaxiai Q. Zhang et al., 2016 DZheniaburmensis sp. nov. Scale bars: 1mm (C, D). ac gl – accessory gland; acul – aculeus; cerc – cercus; cloac op – cloacal opening; ev mem – eversible membrane; ovscp – oviscape; sg – segment; spmth – spermatheca; st – sternite; tg – tergite; v rep – ventral receptacle.
Figure 7 from: Zhang Q, Zhang J (2019) Contribution to the knowledge of male and female eremochaetid flies in the late Cretaceous amber of Burma (Diptera, Brachycera, Eremochaetidae). Deutsche Entomologische Zeitschrift 66(1): 75-83. https://doi.org/10.3897/dez.66.33914
Figure 7 Zheniaburmensis sp. nov. Line drawings, paratype NIGP170826, female A habitus (lateral view) B antenna C ovipositor (lateral view). Scale bar: 1mm (A); 0.1 mm (B, C).
Figure 2 from: Yang Q, Shi C, Ren D (2019) A new genus and species of berothids (Insecta, Neuroptera) from the Late Cretaceous Myanmar amber. ZooKeys 864: 99-109. https://doi.org/10.3897/zookeys.864.35271
Figure 2 Ansoberothajiewenae gen. et sp. nov., holotype CNU-NEU-MA2018072 A, B photograph of left forewing and line drawing C, D photograph of right forewing and line drawing E, F photograph of left hind wing and line drawing G, H photograph of right hind wing and line drawing. Scale bars 1 mm.
Figure 1 from: Yang Q, Shi C, Ren D (2019) A new genus and species of berothids (Insecta, Neuroptera) from the Late Cretaceous Myanmar amber. ZooKeys 864: 99-109. https://doi.org/10.3897/zookeys.864.35271
Figure 1 Ansoberothajiewenae gen. et sp. nov., holotype CNU-NEU-MA2018072 A photograph of holotype B detailed photograph of antenna, arrow shows the long scape C detailed photograph of abdomen, arrow shows the gonapophysis lateralis. Scale bars 2 mm (A) and 1 mm (B, C).
Text-fig. 1. Geographical position of the locality Předboj in the Bohemian Cretaceous Basin and in Europe. in Sabellid And Serpulid Worms (Polychaeta, Canalipalpata, Sabellida, Sabellidae, Serpulidae) From The Rocky Coast Facies (Late Cenomanian) At Předboj Near Prague
Text-fig. 1. Geographical position of the locality Předboj in the Bohemian Cretaceous Basin and in Europe.
Text-fig. 1. Geological map of the site Kučlín, Trupelník Hill. 1 – dumpsite body, exploitation faces, 2 – landslide body, 3 – occurrence of the basalt in the landslide body, 4 – tuff, tuffite with gneiss particles, 5 – 11 – Late Eocene rocks. 5 – basalts, 6 – tuff, tufite, 7 – diatomaceous cherts layer enclosing lenses of diatomaceous earth, 8 – diatomitic breccia, 9 – diatomaceous shale, 10 – diatomaceous clays to diatomites, 11 – calcareous diatomaceous clays to diatomaceous limestones and re-deposited Cretaceous material, 12 – Late Turonian marlstone to limestone, 13 – Middle Turonian marlstone, 14 – Middle Turonian organo-detritic limestone to conglomerate, 15 – Late Proterozoic orthogneiss, 16 – Syčivka creek, 17 – road, field drives, 18 – Kučlín village. in Geology Of The Site Kučlín, Trupelník Hill Near Bílina In North Bohemia
Text-fig. 1. Geological map of the site Kučlín, Trupelník Hill. 1 – dumpsite body, exploitation faces, 2 – landslide body, 3 – occurrence of the basalt in the landslide body, 4 – tuff, tuffite with gneiss particles, 5 – 11 – Late Eocene rocks. 5 – basalts, 6 – tuff, tufite, 7 – diatomaceous cherts layer enclosing lenses of diatomaceous earth, 8 – diatomitic breccia, 9 – diatomaceous shale, 10 – diatomaceous clays to diatomites, 11 – calcareous diatomaceous clays to diatomaceous limestones and re-deposited Cretaceous material, 12 – Late Turonian marlstone to limestone, 13 – Middle Turonian marlstone, 14 – Middle Turonian organo-detritic limestone to conglomerate, 15 – Late Proterozoic orthogneiss, 16 – Syčivka creek, 17 – road, field drives, 18 – Kučlín village.
Fig. 5 in Osteology of the dorsal vertebrae of the giant titanosaurian sauropod dinosaur Dreadnoughtus schrani from the Late Cretaceous of Argentina
Fig. 5. Comparison of lamina capture in dorsal vertebrae of titanosaurian sauropod Dreadnoughtus schrani Lacovara, Lamanna, Ibiricu, Poole, Schroeter, Ullmann, Voegele, Boles, Carter, Fowler, Egerton, Moyer, Coughenour, Schein, Harris, Martínez, and Novas, 2014, from Santa Cruz Province, Argentina; middle–late Campanian to early Maastrichtian (A–E, shown in non-standard views for best visualization) and "disconnection" (sensu Gallina 2011) in presacral vertebrae of Bonitasaura salgadoi Apesteguía, 2004 from Río Negro Province, Argentina; Santonian (F). A. Left side of MPM-PV 1156?-4, estimated as the ~4th dorsal vertebra. B. Left side of MPM-PV 1156?-5, ~5th. C. Right side of MPM-PV 1156-6 (mirrored), ~6th. D. Right side of MPM-PV 1156?-8 (mirrored), ~7th. E. Right side of MPM-PV 1156?-9 (mirrored), ~8th. Changes in the PODLs through the sequence are denoted by a dotted line. F. Presacral vertebrae reproduced from Gallina (2011) under a Creative Commons Attribution License (CC BY 4.0). F, F, estimated13th? cervical ver1 7 tebra; F, F, ~1st dorsal vertebra; F, F, ~2nd dorsal vertebra; F, F, ~3rd dorsal vertebra; F, F, 6th? dorsal vertebra; F, F, ~10th? dorsal vertebra. 2 8 3 9 4 10 5 11 6 12 Photographs (F1–F6) and explanatory drawings (F7–F12). Abbreviations: DI, diapophysis; PODL, postzygodiapophyseal lamina; "PODL", "new incipient horizontal lamina arises from the postzygapophysis pointing towards the diapophysis", as per Gallina (2011: fig. 6A); POZ, postzygapophysis.
Fig. 10 in A new ankylosaurid from the late Cretaceous Two Medicine Formation of Montana, USA
Fig. 10. Strict consensus tree based on 15 specimens—all of which were at one time referred to Euoplocephalus tutus—plus Pinacosaurus grangeri, generated using PAUP 4.0b10 (Swofford 2003). Nodes are discussed in the text. The tree has 29 steps, a Consistency Index of 0.793, and a Retention Index of 0.846.
Fig. 12 in Gastropods from Late Cretaceous Omagari and Yasukawa hydrocarbon seep deposits in the Nakagawa area, Hokkaido, Japan
Fig. 12. Gastropods from the Campanian (Upper Cretaceous) Omagari (B) and Yasukawa (A, C, D) seep sites in Hokkaido, Japan. A.?Sulcoactaeon sp. (UMUT MM30185) in apertural (A1), lateral (A2), and apical (A4) views; A3, close up of the aperture. B. Gastropoda indet. 1 (UMUT MM30186) in apertural (B1), lateral (B2), and apical (B3) views. C. Gastropoda indet. 2 (UMUT MM30187) in apertural (C3), lateral (C4), and apical (C5) views; C1, fibrous prismatic shell outer layer, C2, cross lamellar inner layer. D. Neogastropoda indet. (UMUT MM30188) in lateral (D1) and apical (D2) views.
Fig. 3. A in Stagodontid marsupials from the Late Cretaceous of Canada and their systematic and functional implications
Fig. 3. A. Didelphodon coyi Fox and Naylor, 1986, condyle and inflected angle of TMP 90.12.29, from the Horseshoe Canyon Formation, Edmontonian Land Mammal Age (early Maastrichtian), Michichi Creek (type locality), Alberta, in posterior view with ventral surface of inflected angle horizontal (A1) and dorsal surface of condyle horizontal (A2). B. Didelphodon coyi Fox and Naylor, 1986, incomplete right maxilla, TMP 94.125.125, from the Scollard Formation, Lancian Land Mammal Age (late Maastrichtian), KUA−1 locality, Red Deer River Valley, Alberta, containing P3, M1, M2 (broken) in occlusal view. C. Eodelphis cutleri (Smith Woodward, 1916), incomplete right maxilla, UALVP 43005, from the Dinosaur Park Formation, Judithian Land Mammal Age (late Campanian), Onetree Creek, Dinosaur Provincial Park, Alberta, containing M2–3 in occlusal view. D. Undescribed Alphadon−like marsupial, incomplete left maxilla, TMP 95.178.26, from the Oldman Formation, Judithian Land Mammal Age (late Campanian), Devil's Coulee, Alberta, containing P1–3, M1–4 in occlusal (D1) and labial (D2) views. B, C, and D1 stereophoto pairs. Scale bars 5 mm.
Fig. 19 in New Data On The Skull And Dentition In The Mongolian Late Cretaceous Eutherian Mammal Zalambdalestes
Fig. 19. Stereophotograph of the skull of Zalambdalestes lechei PSSMAE 130 in dorsal view, with accompanying line drawing. Gray pattern represents matrix. Abbreviations: ch, cerebral hemisphere; fr, frontal; ju, jugal; lac, lacrimal; mx, maxilla; na, nasal; naf, nasal facet on frontal; ob, olafactory bulb; pa, parietal; pal, palatine; pmx, premaxilla; sq, squamosal; ssf, subsquamosal foramen; sss, superior sagittal sinus; ts, transverse sinus; ver, vermis of cerebellum.
Fig. 43 in New Data On The Skull And Dentition In The Mongolian Late Cretaceous Eutherian Mammal Zalambdalestes
Fig. 43. Reconstruction of the skull of Zalambdalestes lechei in ventral view. Gray areas are holes. Abbreviations: as, alisphenoid; bo, basioccipital; bs, basisphenoid; ecpc, ectopterygoid crest; enpc, entopterygoid crest; eo, exoccipital; gf, glenoid fossa; inf, incisive foramen; ju, jugal; mapf, major palatine foramina; mpf, minor palatine foramen; mx, maxilla; pal, palatine; pe, petrosal; pmx, premaxilla; ppt, postpalatine torus; pr, promontorium; ps?, parasphenoid; pt, pterygoid; sq, squamosal; vo, vomer.
Fig. 4 in New Data On The Skull And Dentition In The Mongolian Late Cretaceous Eutherian Mammal Zalambdalestes
Fig. 4. Reconstructions of the skull of Zalambdalestes lechei in right lateral views (A, B) and in ventral views (C, D). Panels A and C are redrawn from Van Valen (1964: fig. 2), B is from Kielan Jaworowska (1975a: fig. 2A), and D is from KielanJaworowska (1984a: fig. 1). The basicranium in the last is based on Barunlestes butleri.
Fig. 38 in Late Campanian (Cretaceous) Heteromorph Ammonites From The Western Interior Of The United States
Fig. 38. Didymoceras cheyennense (Meek and Hayden, 1856a). A, B. USNM 482462, USGS Mesozoic locality D2740 (fig. 2, loc. 39). C, D. USNM 445099, USGS Mesozoic locality D221 (fig. 2, loc. 14). Figures are ×1.
Fig. 57 in Late Campanian (Cretaceous) Heteromorph Ammonites From The Western Interior Of The United States
Fig. 57. Spiroxybeloceras meekanum (Whitfield, 1877). A. USNM 482505, USGS Mesozoic locality D68 (fig. 2, loc. 43). B, C. USNM 482506, USGS Mesozoic locality D2740 (fig. 2, loc. 39). D, E. USNM 482507, USGS Mesozoic locality D1794 (fig. 2, loc. 37). F. USNM 482508, same locality as D, E. G. USNM 482509, same locality as D, E. H. USNM 12279, holotype of Ptychoceras meekanum Whitfield, 1877. I. BHMNH 2145, collected by N. L. Larson, Pierre Shale near center of sec. 4, T. 42 N., R. 47 W., Shannon County, S. Dak. J. USNM 411291, same locality as D, E.
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