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Fig. 6 in A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration

Fig. 6. Spionid polychaete symbionts in the Recent cheilostome bryozoan Celleporaria brunnea (Hincks, 1884), Point Loma, San Diego, California. A. Living associations showing two long palps emerging from a spionid tube (arrowed), shorter tentacles of the bryozoan and black opercula. B. Spionid palps extending above level of bryozoan lophophores. C. Scanning electron microscope of bleached colony (NHM 2010.11.30.1) showing numerous spionid worm bioclaustrations varying in shape and size but consistently larger than the bryozoan orifices and new buds. D. Scanning electron micrograph of dried, unbleached colony showing mud tube constructed by a spionid worm surrounded by calcareous tube formed by the bioclaustrating bryozoan (NHM 2010.11.30.1).

Fig. 3 in A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration

Fig. 3. Fistuliporid bryozoan Stellatoides muellertchensis gen. et sp. nov., Middle Devonian (Lower Givetian, Ahbach Formation) of the abandoned "Müllertchen Quarry" (Hillesheim Syncline, Eifel, Rhenish Massif, northwestern Rhineland-Palatinate, Germany). A. Paratype SMF 21.115, goblet-shaped colony, side view. B. Paratype SMF 21.110, fragment of goblet-shaped colony showing maculae.

Fig. 2 in A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration

Fig. 2. Lowermost Lower Givetian stratigraphy of the "Type Eifelian Profile" sensu Struve (1982); light grey: biostratigraphic distribution of fistuliporid bryozoan Stellatoides muellertchensis gen. et sp. nov.; dark grey: maximum distribution.

Fig. 1 in A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration

Fig. 1. Map showing location of the abandoned Müllertchen Quarry within the Hillesheim Syncline. Geological overview of the Rhenish Massif (A), showing the studied area (taken from Bohatý et al. 2012; modified from Korn 2008 after Walter 1995) and detailed view of the Eifel Synclines (B) with the fossil locality 1 (modified after Struve 1996c).

Fig. 5 in A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration

Fig. 5. Cylindrical embedment trace (bioclaustration) Chaetosalpinx tapanilai ichnosp. nov., Middle Devonian (Lower Givetian) of the Rhenish Massif, north-western Rhineland-Palatinate, Germany. A. Paratype SMF 21.115, colony surface of fistuliporid bryozoan Stellatoides muellertchensis gen. et sp. nov. showing tubes of C. tapanilai. B. Paratype SMF 21.122, tangential section of tubes of C. tapanilai. C. Holotype SMF 21.118, longitudinal section of a tube.

Fig. 4 in A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration

Fig. 4. Fistuliporid bryozoan Stellatoides muellertchensis gen. et sp. nov., Middle Devonian (Lower Givetian) of the Rhenish Massif, north-western Rhineland-Palatinate, Germany. A. Holotype SMF 21.108, transverse section showing autozooecial chambers and vesicular skeleton (A), tangential sec1 tions showing autozooecial apertures with lunaria and vesicles (A 2 –A 5). B. Paratype SMF 21.113, longitudinal section showing multilayered secondary overgrowths.

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Fig. 1 in The taxonomy and anatomy of rauisuchian archosaurs from the Late Triassic of Germany and Poland

Fig. 1. Right maxilla of rauisuchian Teratosaurus suevicus Meyer, 1861 from Mittlerer Stubensandstein, Upper Triassic of Heslach, Germany, NHM 38646, holotype. Photographs in lateral (A), medial (B), and ventral (C) views. Designation "m" refers to maxillary tooth position.

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Fig. 2 in The taxonomy and anatomy of rauisuchian archosaurs from the Late Triassic of Germany and Poland

Fig. 2. Right maxilla of rauisuchian Teratosaurus suevicus Meyer, 1861 from Mittlerer Stubensandstein, Upper Triassic of Heslach, Germany, NHM 38646, holotype. Photographs in medial (A) and anterior (B) views. A is a close−up of the medial surface of the anterior end of the maxilla. Designation "m" refers to maxillary tooth position.

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Fig. 3 in The taxonomy and anatomy of rauisuchian archosaurs from the Late Triassic of Germany and Poland

Fig. 3. Left maxilla of rauisuchian Polonosuchus silesiacus (Sulej, 2005) from Late Carnian, Upper Triassic of Krasiejów Claypit, Poland, ZPAL AbIII/563, part of holotype. Photographs in lateral (A), medial (B), and ventral (C) views. Designation "m" refers to maxillary tooth position.

Fig. 5 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 5. Digital (A) and scanning electron microscope (B–E) photographies of the five larger specimens from the Langenberg quarry (Kimmeridgian, Late Jurassic): DFMMh/ FV658 (A), DFMMh/ FV707.1 (B), DFMMh/ FV383 (C), DFMMh/ FV 530 (D), and DFMMh/ FV 382 (E).

Fig. 4 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 4. Photographs of the five larger specimens from the Langenberg quarry (Kimmeridgian, Late Jurassic). A. DFMMh/FV 530 in lingual view. B. DFMMh/FV 383 in lingual view. C. DFMMh/FV707.1 in labial view. D. DFMMh/FV 382 in lingual view. E. DFMMh/FV658 in lingual view.

Fig. 1 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 1. Geographic location of Langenberg quarry ("Rohstoffbetriebe Oker") east of Oker (Goslar), Harz Mountains, Germany (from Mudroch and Thies 1996).

Fig. 2 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 2. The lithostratigraphic log of the Kimmeridgian of the Langenberg quarry near Oker, Harz Mountains, Germany. The examined theropod teeth were found in bed 83 together with skeletal remains of Europasaurus holgeri (modified after Thies et al. 2007).

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Fig. 3 in Plesiosoricids from early Oligocene fissure fillings in South Germany, with remarks on plesiosoricid phylogeny

Fig. 3. Strict consensus of the 96 most parsimonious trees resulting from the analysis of the data matrix given in Table 2. Only the 10 ingroup−species with character completeness of>35% are included in the analysis; 26 characters. Tree length = 33, consistency index (CI) = 0.8788, rescaled consistency index (RC) = 0.7030, CI excluding uninformative characters = 0.8000, retention index (RI) = 0.8000. Thin lines = European taxa; bold lines = North American species; dashed line = Asian species.

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Fig. 2 in Plesiosoricids from early Oligocene fissure fillings in South Germany, with remarks on plesiosoricid phylogeny

Fig. 2. Plesiosoricid mammal Butselia biveri Quinet and Misonne, 1965 from the Möhren Quarry (early Oligocene, southern Germany). A. Left dentary fragment with p1 and p3–m3, in occlusal (A1) and labial (A2) views, Möhren 12, BSP XI 1971 XXX 60. B. Left p2, in occlusal (B1) and labial (B2) views, Möhren 13, BSP 1972 XI 5908. C. Left dentary fragment with p3–p4, in occlusal view, Möhren 13, BSP 1972 XI 239. D. Left p4, in occlusal (D1) and labial (D2) views, Möhren 13, BSP 1972 XI 225. E. Left dentary fragment with m1, in occlusal view, Möhren 13, BSP 1972 XI 5604. F. Left m1, in labial view, Möhren 13, BSP 1972 XI 228. G. Right m2, reversed, in occlusal (G1) and labial (G2) views, Möhren 13, BSP 1972 XI 229. H. Left m3, in occlusal view, Möhren 13, BSP 1972 XI 5909. I. Right m3, reversed, in labial view, Möhren 13, BSP 1972 XI 5599. J. Left P3, in occlusal view, Möhren 13, BSP 1972 XI 217. K. Left P4, in occlusal view, Möhren 13, BSP 1972 XI 218. L. Left M1, in occlusal view, Möhren 13, BSP 1972 XI 220. M. Left M2, a. in occlusal view, Möhren 13, BSP 1972 XI 223. N. Left M3, in occlusal view, Möhren 13, BSP 1972 XI 243.

Fig. 3 in New middle Eocene formicid species from Germany and the evolution of weaver ants

Fig. 3. Weaver ant Oecophylla longiceps Dlussky sp. nov., Grube Messel, middle Eocene. A. Gyne, holotype MeI 3643. B. Gyne, paratype MeI 890. C. Male, paratype MeI 7636. Photographs (A1–C1) and drawings (A2–C2). Scale bars 5 mm.

Fig. 2 in New middle Eocene formicid species from Germany and the evolution of weaver ants

Fig. 2. Wings of weaver ant Oecophylla longiceps Dlussky sp. nov., drawing with nomenclature of wing venation.

Fig. 6 in New middle Eocene formicid species from Germany and the evolution of weaver ants

Fig. 6. Gynes of different species of Oecophylla weaver ants. A. Reconstruction of Oecophylla longiceps sp. nov., Grube Messel, middle Eocene. B. Reconstruction of Oecophylla atavina Cockerell, 1915, Bembridge Marls, Oligocene. C. Oecophylla smaragdina (Fabricius, 1775), Recent, Vietnam.

Fig. 1 in New middle Eocene formicid species from Germany and the evolution of weaver ants

Fig. 1. Distribution of extant and fossil weaver ants. Extant ranges are shaded grey, fossil sites are marked with an asterisk. Abbreviations: 1, Baltic amber; 2, Bournemouth and Isle of Wight; 3, Saxonian amber; 4, Brunstatt and Kleinkembs; 5, Sicilian amber; 6, Radoboj; 7, Mfwangano Island; 8, Montagne d'Andance; 9, Messel and Eckfeld. Distribution of extant species modified after Lokkers (1986).

Fig. 5 in New middle Eocene formicid species from Germany and the evolution of weaver ants

Fig. 5. Workers of different species of Oecophylla weaver ants. A. Dorsal view of Oecophylla crassinoda Wheeler, 1922, Baltic amber, middle to late Eocene, holotype GZG BST.4620. B. Side view of O. crassinoda Wheeler, 1922, Bitterfeld amber, middle to late Eocene, Humboldt Museum No 11/214. C. Side view of Oecophylla brischkei Mayr, 1868, Baltic amber, middle to late Eocene (from Wheeler 1915, with some changes). D. Head of O. brischkei Mayr, 1868, Baltic amber, middle to late Eocene, GZG.BST.04618. E. Side view of major worker of Recent Oecophylla smaragdina (Fabricius, 1775) from Vietnam. F. Frontal view of head of major worker of O. smaragdina (Fabricius, 1775). Scale bars 1 mm.