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Figs 1-11 in Contribution to the knowledge of the Xantholini from China. XV. New species collected by Michael Schülke in Zhejiang and Yunnan (Coleoptera, Staphylinidae)¹

Figs 1-11: Mahavana gaoligonggaoligong n. sp.: 1 head (right half omitted); 2 antenna; 3 tergite of the male genital segment; 4 sternite of the same; 5 aedeagus. Mahavana daliana n. sp.: 6 head (right half omitted); 7 antenna; 8 6° visible sternite; 9 male genital segment; 10 sternite of the same; 11 aedeagus (bar scale: 0,1 mm).

Figs 19-22 in Contribution to the knowledge of the Xantholini from China. XV. New species collected by Michael Schülke in Zhejiang and Yunnan (Coleoptera, Staphylinidae)¹

Figs 19-22: Atopolinus uncinatus n. sp.: 19 sternite of male genital segment. Atopolinus inusualis n. sp.: 20 tergite of male genital segment. 21 sternite of the same; 22 aedeagus (bar scale: 0,1 mm).

Figs 27-31 in Contribution to the knowledge of the Xantholini from China. XV. New species collected by Michael Schülke in Zhejiang and Yunnan (Coleoptera, Staphylinidae)¹

Figs 27-31: Atopolinus schuelkeischuelkei n. sp.: 27 6° visible tergite; 28 6° visible sternite; 29 male

Figs 12-18 in Contribution to the knowledge of the Xantholini from China. XV. New species collected by Michael Schülke in Zhejiang and Yunnan (Coleoptera, Staphylinidae)¹

Figs 12-18: Yunna fungicolafungicola n. sp.: 12 male genital segment; 13 sternite of the same; 14 aedeagus. Atopolinus uncinatusuncinatus n. sp.: 15 6° visible tergite; 16 6° visible sternite; 17 male genital segment; 18 aedeagus (bar scale: 0,1 mm).

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FIG, 1. John William Daly (1933–2008) on the upper Río San Juan. This paper is dedicated to John Daly, our late friend and colleague, who helped collect three of the new species here described. In addition to his globally acclaimed discoveries in chemistry and pharmacology, John was an accomplished field herpetologist who contributed importantly to the systematics and natural history of dendrobatoid frogs (see Grant et al., 2006; Myers, 2009). This photograph shows John at age 37, with the upper Río San Juan behind him and branches overhead of a madroño tree (probably Garcinia magnifolia, syn. Rheedia chocoensis, Clusiaceae). When in South America, John was never far from a dendrobatid frog—this time, in the tree above his head, a tiny, undescribed semiarboreal species (also collected and later named "Dendrobates fuguritus" by our colleague Philip Silverstone). Other dendrobatids found nearby included Phyllobates aurotaenia (Boulenger, 1913), which was then being used for poisoning blowgun darts, and also the nontoxic species that we name Silverstoneia dalyi herein. (Photograph by C. W. Myers, 2 km above Playa de Oro, Chocó, February 16, 1971.) in Review of the Frog Genus Silverstoneia, with Descriptions of Five New Species from the Colombian Chocó (Dendrobatidae: Colostethinae)

FIG, 1. John William Daly (1933–2008) on the upper Río San Juan. This paper is dedicated to John Daly, our late friend and colleague, who helped collect three of the new species here described. In addition to his globally acclaimed discoveries in chemistry and pharmacology, John was an accomplished field herpetologist who contributed importantly to the systematics and natural history of dendrobatoid frogs (see Grant et al., 2006; Myers, 2009). This photograph shows John at age 37, with the upper Río San Juan behind him and branches overhead of a madroño tree (probably Garcinia magnifolia, syn. Rheedia chocoensis, Clusiaceae). When in South America, John was never far from a dendrobatid frog—this time, in the tree above his head, a tiny, undescribed semiarboreal species (also collected and later named "Dendrobates fuguritus" by our colleague Philip Silverstone). Other dendrobatids found nearby included Phyllobates aurotaenia (Boulenger, 1913), which was then being used for poisoning blowgun darts, and also the nontoxic species that we name Silverstoneia dalyi herein. (Photograph by C. W. Myers, 2 km above Playa de Oro, Chocó, February 16, 1971.)

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Figures 1–11 in Contribution to the knowledge of Chinese Phasmatodea IX: First report of Xeroderinae (Phasmatodea: Phasmatidae) from China

Figures 1–11. Sinoxenophasmina abbreviatum gen. & sp. nov. 12. Xenophasmina fimbriatum (Redtenbacher, 1908). 1. Female apex of abdomen, lateral view. 2. Female apex of abdomen, dorsal view. 3. Male apex of abdomen, lateral view. 4. Male apex of abdomen, dorsal view. 5. Male vomer, ventral view. 6. Female habitus. 7. Male habitus. 8. Female head and thorax, dorsolateral view. 9. Male head and thorax, dorsolateral view. 10. Egg, lateral view. 11. Egg, dorsal view. 12. Female habitus. Scale bars: 1–4, 6–9, 12 = 5 mm; 5, 10–11= 1 mm.

FIG. 5. — A in Contribution to the systematics and phylogeny of Bouvrain, 1982 (Mammalia, Bovidae)

FIG. 5. — A, One of the 32 most parsimonious trees with length 38, ECI: 0.60 that is preferred here. A delayed transformation scenario has been chosen for characters Oc and Bo2 (see text). Character changes supporting nodes 1-6 are: Node 1 = *Hc4(1), *Pe(1) and obviously Hc7(1); Node 2 = Hc3(1), Hc7(2), Hc8(1); Node 3 = Hc9(1), Hc10(1), Oc(1), Bo1(2), Bo2(1); Node 4 = Hc3(0), *Hc4(0), Hc7(1), Hc8(0); Node 5 = *Hc2(1), *Hc1(1), Bo2(1), Oc(1), Cr(1); Node 6 = *Hc1(2), *Hc5(1), *Hc11(1), Bo1(1), *Su(1). Unambiguous character changes supporting the same nodes on both trees are marked with an asterisk. Characters supporting terminal taxa are all the same in the favored and most parsimonious trees except for Cr(1). Character coding as in Figure 4. Numbers in squares represent % values of bootstrapping support with 1000 pseudoreplicates; B, Distribution of cladogram lengths. Abbreviations: P., Prostr., Prostrepsiceros; h., houtumschindleri.

FIG. 3 in Contribution to the systematics and phylogeny of Bouvrain, 1982 (Mammalia, Bovidae)

FIG. 3. — Scatter diagram comparing the horn-core basal dimensions of several late Miocene spiral-horned antelopes. Prostepsiceros libycus Lehman & Thomas, 1987 is placed outside the present metrical frame; ●, P. vallesiensis Bouvrain, 1982 holotype; ○, P. vallesiensis RP1 114n, 115n; ◆, Dytikodorcas longicornis Bouvrain & Bonis, 2007; ■, P. vinayaki (Pilgrim, 1939) holotype; □, P. aff. vinayaki Baynunah; ▲, P. vallesiensis M. Sinap Loc. 40; ▲, Prostrepsiceros sp. M. Sinap Loc. 91; △, P. aff. vallesiensis Middle Sinap. Abbreviations: APD, anteroposterior diameter; DT, transverse diameter.

FIG. 2 in Contribution to the systematics and phylogeny of Bouvrain, 1982 (Mammalia, Bovidae)

FIG. 2. — Prostepsiceros vallesiensis Bouvrain, 1982 from RPl: A, B, C, lateral; D, posterior views. Scale bar: 4 cm.

FIG. 1 in Contribution to the systematics and phylogeny of Bouvrain, 1982 (Mammalia, Bovidae)

FIG. 1. — Prostrepsiceros vallesiensis Bouvrain, 1982, holotype skull RPl234: A, dorsal; B, lateral; C, occipital; D, ventral views. Scale bar: 4 cm.

FIG. 10 in Contributions biostratigraphiques et paléoenvironnementales de l'étude des nannofossiles calcaires des dépôts tortonomessiniens du bassin du Chélif (Algérie)

FIG. 10. — Variations verticales de l'abondance des principales espèces de nannofossiles calcaires dans la coupe de Djebel Ben Dourda, bassin du Bas Chélif (Algérie).

FIG. 5 in Contributions biostratigraphiques et paléoenvironnementales de l'étude des nannofossiles calcaires des dépôts tortonomessiniens du bassin du Chélif (Algérie)

FIG. 5. —Distribution des principaux marqueurs de nannofossiles calcaires de la coupe de Djebel Ben Dourda, bassin du Bas Chélif (Algérie). Les astérisques indiquent des zones modifiées: * par Berggren et al. (1995); ** par Raffi & Flores (1995).

FIG. 6 in Contributions biostratigraphiques et paléoenvironnementales de l'étude des nannofossiles calcaires des dépôts tortonomessiniens du bassin du Chélif (Algérie)

FIG. 6. — Nannofossiles calcaires du Dahra (Algérie): A, Amaurolithus amplificus (éch. 52); B, A. delicatus (éch. 28); C, A. primus (éch. 28); D, A. tricorniculatus (éch. 28); E, Discoaster loeblichii (éch. 19); F, D. quinqueramus (éch. 29); G, D. brouweri (éch. 28); H, D. neohamatus (éch. 29); I, D. surculus (éch. 28); J, D. variabilis (éch. 50); K, D. deflandrei (éch. 28); L, M, D. misconceptus (éch. 29); N, O, Triquetrorhabdulus rugosus (éch. 28); P, Q, Coccolithus pelagicus (éch. 1); R, S, Reticulofenestra pseudoumbilicus (éch. 4); T, R. rotaria (flèche) (éch. 28); U, V, Helicosphaera carteri (éch. 20); W, X, Rhabdosphaera procera (éch. 59); Y, coccosphère de Coccolithus pelagicus au MEB (éch. 19); L, N, P, R, U, W, lumière naturelle; M, O, Q, S, T, V, X, lumière polarisée. Échelles: 5 µm.

FIG. 2 in Contributions biostratigraphiques et paléoenvironnementales de l'étude des nannofossiles calcaires des dépôts tortonomessiniens du bassin du Chélif (Algérie)

FIG. 2. — Biozonation dans la série type des bassins miocènes de l'Algérie nord-occidentale (Chélif, Tafna). Cycles eustatiques miocènes et leur correspondance avec les cycles de Haq et al. (1987) d'après Belkebir et al. (1996) modifié. 1, conglomérats; 2, grès; 3, marnes; 4, diatomites (Tripoli); 5, calcaires; 6, cinérites; 7, gypse; 8, algues et coraux; 9, discontinuités.

FIG. 3 in Contributions biostratigraphiques et paléoenvironnementales de l'étude des nannofossiles calcaires des dépôts tortonomessiniens du bassin du Chélif (Algérie)

FIG. 3. — Répartition verticale des différents taxons de nannofossiles calcaires dans la coupe du Djebel Ben Dourda, bassin du Bas Chélif (Algérie).

FIG. 1. — A in Contributions biostratigraphiques et paléoenvironnementales de l'étude des nannofossiles calcaires des dépôts tortonomessiniens du bassin du Chélif (Algérie)

FIG. 1. — A, Carte simplifiée du bassin du Bas Chélif (Algérie); B, localisation de la coupe de Djebel Ben Dourda, situation par rapport à la wilaya de Mostaganem. Abréviations: Dj., Djebel; O., oued.

FIG. 2 in Controverses géologiques sur le Cambro-Ordovicien de la Montagne Noire (France) à l'aube du siècle: les contributions de Jean Miquel (1859-1940)

FIG. 2. — Schéma synthétique de l'évolution des termes stratigraphiques utilisés dans la corrélation du Cambrien et de l'Ordovicien inférieur en Grande-Bretagne au cours de la deuxième moitié du XIXe siècle.

FIG. 5 in Controverses géologiques sur le Cambro-Ordovicien de la Montagne Noire (France) à l'aube du siècle: les contributions de Jean Miquel (1859-1940)

FIG. 5. — Trilobites déposés au Laboratoire de Géologie du Muséum national d'Histoire naturelle, Paris (acronyme Gs); A, cranidium de Parabailiella languedocensis Thoral, 1946 (Gs 2000/13); B, cranidium de Conocoryphe heberti Munier-Chalmas & Bergeron, 1889 (Gs 2000/14); C, cranidium de Ctenocephalus (Ctenocephalus) bergeroni Thoral, 1946 (Gs 2000/15); D, cranidium de Pardailhania hispida Thoral, 1945 (Gs 2000/16); E, cranidium de Badulesia granieri (Thoral, 1935) (Gs 2000/17); F, cranidium de Solenopleuropsis (Manublesia) ribeiro (Verneuil & Barrande, 1860) (Gs 2000/18); G, cranidium de Solenopleuropsis (Manublesia) levisilimbata Thoral, 1948 (Gs 2000/19); H, cranidium de Solenopleuropsis (Solenopleuropsis) multigranifera Thoral, 1948 (Gs 2000/20); I, cranidium de Solenopleuropsis (Solenopleuropsis) rouayrouxi Munier-Chalmas & Bergeron, 1889 (Gs 2000/21); J, cranidium de Velieuxia couloumana (Miquel, 1905) (Gs 2000/22). Échelles: A, F, H-J, 2 mm; B, E, 1 cm; C, G, 5 mm; D, 6 mm.

FIG. 4 in Controverses géologiques sur le Cambro-Ordovicien de la Montagne Noire (France) à l'aube du siècle: les contributions de Jean Miquel (1859-1940)

FIG. 4. — Trilobites déposés au Laboratoire de Géologie du Muséum national d'Histoire naturelle, Paris (acronyme Gs); A, cranidium de Calodiscus foveolatus Howell, 1935 (Gs 2000/1); B, cranidium de Pseudoperonopsis sallesi (Munier-Chalmas & Bergeron, 1889) (Gs 2000/2); C, pygidium de Pseudoperonopsis sallesi (Munier-Chalmas & Bergeron, 1889) (Gs 2000/3); D, cranidium de Leiagnostus thorali (Howell, 1935) (Gs 2000/4); E, pygidium de Eccaparadoxides mediterraneus Pompeckj, 1901 (Gs 2000/5); F, céphalon et une partie du thorax de Eccaparadoxides brachyrhachis Linnarsson, 1883 (Gs 2000/6); G, cranidium de Eccaparadoxides rouvillei (Miquel, 1905) (Gs 2000/7); H, pygidium de Eccaparadoxides rouvillei (Miquel, 1905) (Gs 2000/8); I, exemplaire complet de Corynexochus delagei Miquel, 1905 (Gs 2000/9); J, cranidium de Agraulos longicephalus (Hicks, 1872) (Gs 2000/10); K, cranidium de Bailiella levyi Munier-Chalmas & Bergeron, 1889 (Gs 2000/11); L, pygidium de Bailiella levyi Munier- Chalmas & Bergeron, 1889 (Gs 2000/12). Échelles: A, G, I, L, 5 mm; B-D, J, K, 2 mm; E, 4 mm; F, H, 1 cm.

FIG. 3 in Controverses géologiques sur le Cambro-Ordovicien de la Montagne Noire (France) à l'aube du siècle: les contributions de Jean Miquel (1859-1940)

FIG. 3. — Diagramme de corrélation des unités stratigraphiques du Cambrien et de l'Ordovicien inférieur (Tremadoc-Arenig) du versant sud de la Montagne Noire jusqu'en 1935.