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FIGURE 3 in A new paper wasp from Late Eocene of France (Hymenoptera: Vespidae: Polistinae)

FIGURE 3. Wing venation patterns of Agelaia myrmecophila (Duke), Parapolybia varia (Fabricius), Angiopolybia paraensis (Spinosa) and of the two specimens of Palaeopolistes jattioti sp. nov.. Venation nomenclature is explained in the text.

FIGURE 1 in A new paper wasp from Late Eocene of France (Hymenoptera: Vespidae: Polistinae)

FIGURE 1. Palaeopolistes jattioti sp. nov. Print and counterprint of the holotype (A, B) and paratype (C, D) Scale bars 1 mm.

FIGURE 2 in A new paper wasp from Late Eocene of France (Hymenoptera: Vespidae: Polistinae)

FIGURE 2. Palaeopolistes jattioti sp. nov., holotype. Drawing of the counterprint. For more clarity, only one pair of wings was represented. Scale bar 1 mm.

FIGURE 7 in A new late Eocene Bicornucythere species (Ostracoda, Crustacea) from Myanmar, and its significance for the evolutionary history of the genus

FIGURE 7. Early Miocene (A) and late Eocene (B) localities of Bicornucythere are represented by solid black symbols. The paleogeography was generated using the online service of the Ocean Drilling Stratigraphic Network (http://www.odsn.de), accessed on September 11, 2013. The late Eocene and early Miocene paleogeographies represent configurations at 35 Ma and 22 Ma, respectively. The grey shading indicates plate fragments. The black line shows today's shoreline. Open white circles represent localities of fossil ostracodes without Bicornucythere. Numbers are references to the localities: 1, Gramann (1975); 2, Bera & Banerjee (1996); 3, Khosla & Nagori (1989); 4, Khosla (1978), Singh (1988); 5, Ahmad et al. (1991); 6, Yeşilyurt et al. (2009); 7, Nazik (1993); 8, Honigstein et al. (2002); 9, Bosboom et al. (2011); 10, Bhandari (1991); 11, Bhandari (1992); 12, This study.

FIGURE 5 in A new late Eocene Bicornucythere species (Ostracoda, Crustacea) from Myanmar, and its significance for the evolutionary history of the genus

FIGURE 5. Measurements of Bicornucythere bisanensis and Bicornucythere concentrica sp. nov. A, SEM images of B. bisanensis in the A, A-1, and A-2 stages. Scale bars = 100 µm. B, Measurements used in the study: valve length (L), valve height (H), and width of marginal infold (WM). Scale bar = 100 µm. C, The 95% confidence intervals of L, H, and WM/L of B. bisanensis and B. concentrica sp. nov. The bars in the A and A-1 stages indicate 95% confidence intervals of the measurements, while the bars in the A-2 stage indicate ranges of the measurements. The open diamonds indicate mean values. The horizontal dotted lines indicate the WM/L ratios of B. concentrica sp. nov. "n" indicates the number of measurements. The measurements and detailed information about B. bisanensis specimens are given in the Appendix.

FIGURE 3 in A new late Eocene Bicornucythere species (Ostracoda, Crustacea) from Myanmar, and its significance for the evolutionary history of the genus

FIGURE 3. Columnar section of the Yaw Formation in the Kyauktakha section (Fig. 2B and 2C) and horizons of the examined samples.

FIGURE 4 in A new late Eocene Bicornucythere species (Ostracoda, Crustacea) from Myanmar, and its significance for the evolutionary history of the genus

FIGURE 4. SEM images of ostracodes and benthic foraminifer from sample 69-1. The arrows point anteriorly. A–I, Bicornucythere concentrica Yamaguchi sp. nov. (A–D), UMUT-CA31128, holotype, carapace, left external view (A), right external view (B), dorsal view (C), and anterior view (D). E–H, UMUT-CA31129, paratype, right valve, external view (E), internal view (F), dorsal view (G), and hingement (H). I, UMUT-CA31131, paratype, carapace, left external view. J, Trachyleberididae gen. et sp. indet.1, right external view of carapace. K, Buntoninae gen. et sp. indet., left external view of carapace. L, Cytheromorpha? sp., right valve, external view. M–O, Ammonia subgranulosa (Jacob and Sastri, 1950), spiral view (K), umbilical view (L), and apertural view (M). Scale bars =100 µm.

FIGURE 1. A in A new late Eocene Bicornucythere species (Ostracoda, Crustacea) from Myanmar, and its significance for the evolutionary history of the genus

FIGURE 1. A, Geological map and the study area. Modified after Morley (2009) and Mitchell et al. (2012). B, Late Eocene geography of Myanmar, simplified from Licht et al. (2013). Abbreviations: Kb = Kabaw fault, IBR = Indo-Burman Ranges.

FIGURE 2. A in A new late Eocene Bicornucythere species (Ostracoda, Crustacea) from Myanmar, and its significance for the evolutionary history of the genus

FIGURE 2. A, Geological map in the vicinity of the Kyauktakha section (B and C). B and C, traverse maps and sample localities.

FIGURES 4–6 in Revision of the genus Metoisops (Hemiptera: Heteroptera, Miridae, Isometopinae) from late Eocene European amber

FIGURES 4–6. Metoisops punctatus holotype, ♂, in Baltic amber, nr. 364/2; Borissiak Paleontological Institute Russian Academy of Sciences (Arthropod laboratory), Moscow—dorsal views, antennal segments.

FIGURES 7–8 in Revision of the genus Metoisops (Hemiptera: Heteroptera, Miridae, Isometopinae) from late Eocene European amber

FIGURES 7–8. Metoisops punctatus specimen from Rovno (Ukraine), macropterous ♂, in Baltic amber, nr. K-7057, Schmalgausen Institute of Zoology, National Academy of Sciences of Ukraine, Kiev—dorsal views.

FIGURE 23 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 23. 'Fibla' exusta (Cockerell et Custer, 1925). Holotype UCM 4923. A, specimen as preserved. B, hind wing venation. Scale bar = 4 mm.

FIGURE 13 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 13. Archiraphidia tranquilla (Scudder, 1890). Wing venation of the holotype MCZ 246. A, right forewing. B, right hind wing. C, left forewing. D, left hind wing. Scale bar = 4 mm (all to scale).

FIGURE 21 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 21. Florissantoraphidia funerata (Engel, 2003). Holotype NHM In. 26922. A, the specimen as preserved (wetted with ethanol). B, the same (dry). Scale bar = 4 mm (both to scale).

FIGURE 18 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 18. Archiraphidia? somnolenta (Scudder, 1890). Wing venation of the holotype MCZ 488. A, left forewing. B, right forewing as preserved. C, right forewing, reconstruction. D, left hind wing. E, right hind wing. Scale bar = 4 mm (all to scale).

FIGURE 16 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 16. Archiraphidia tranquilla (Scudder, 1890) (paralectotype of A. eventa (Scudder, 1890), MCZ 253). A, the specimen as preserved (covered by Canada balsam). B, right forewing, C, right hind wing. D, left forewing. E, left hind wing. Scale bar = 4 mm (all to scale).

FIGURE 8 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 8. Megaraphidia sp. Specimen MCZ 3641. A, part (converted to right). B, counterpart. C, hind wing venation. Scale bar = 4 mm (all to scale).

FIGURE 7 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 7. Megaraphidia exhumata (Cockerell, 1909). Holotype MCZ 3640. A, part (converted to right). B, counterpart. C, forewing venation. Scale bar = 4 mm (all to scale).

FIGURE 4 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 4. Dictyoraphidia veterana (Scudder, 1890). Wing venation of the holotype PU 6385, EM 1.385. A, forewing. B, hind wing. Scale bar = 4 mm.

FIGURE 22 in A revision of the late Eocene snakeflies (Raphidioptera) of the Florissant Formation, Colorado, with special reference to the wing venation of the Raphidiomorpha

FIGURE 22. Florissantoraphidia funerata (Engel, 2003). Wing venation of the holotype NHM In. 26922. A, left forewing. B, apical portion of right forewing. C, left hind wing. Scale bar = 4 mm (all to scale).