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Fig. 1 in The oldest "intermetamorphic" larva of an achelatan lobster from the Lower Jurassic Posidonia Shale, South Germany

Fig. 1. Larva of Achelata gen. et sp. indet. (SMNS 70449), Toarcian, Lower Jurassic, Gomaringen, Southern Germany. A. Composite microscopic photograph under cross-polarised light. B. Colour-marked photograph indicating the visible structures. Abbreviations: ba, basipod; cx, coxa; e1–5, endopod element 1–5; m3, maxilliped 3; p2–6, pleon segment 2–6; t4–8, thoracic appendages 4–8 ("pereiopods" 1–5).

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Fig. 2 in The oldest "intermetamorphic" larva of an achelatan lobster from the Lower Jurassic Posidonia Shale, South Germany

Fig. 2. Larva of Achelata gen. et sp. indet. (SMNS 70449), Toarcian, Lower Jurassic, Gomaringen, Southern Germany. A. Stereo-image showing original relief of the fossil; based on virtual surface. B. Depth-inverted stereo-image showing morphologically correct relief in ventral view. Please use red-cyan glasses to view A and B. C. Non-stereo image; colour-marked are the elevations of the thoracic sternum.

Fig. 5 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 5. Metriorhynchid thalattosuchian Cricosaurus bambergensis sp. nov. (NKMB-P-Watt14/274) holotype, late Kimmeridgian of Wattendorf (southern Germany). Pectoral girdle and forelimb elements. Abbreviations: ca, carpal elements; co, coracoid; cv, cervical vertebra; dv, dorsal vertebra;?h, questionable humerus; mc, metacarpal elements; ph, phalanges; ru, radius and ulna; sc, scapula.

Fig. 4 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 4. Metriorhynchid thalattosuchian Cricosaurus bambergensis sp. nov. (NKMB-P-Watt14/274) holotype, late Kimmeridgian of Wattendorf (southern Germany). A. Dentition. B. Palatines showing the midline keel seperating symmetrical depressions (dashed outline). C. First cervical vertebrae. Abbreviations: aac, atlas-axis vertebrae; cv, cervical vertebra; hy, hyoid.

Fig. 8 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 8. Results of the phylogenetic analysis, simplified strict consensus topology of 2592 most parsimonious cladograms of Cricosaurus bambergensis sp. nov. within Metriorhynchinae (step number = 1.508; CI = 0.417; RI = 0.843; RC = 0.352; HI = 0.583).

Fig. 1 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 1. Metriorhynchid thalattosuchian Cricosaurus bambergensis sp. nov., NKMB-P-Watt14/274, holotype, late Kimmeridgian of Wattendorf (southern Germany). Skeleton in ventrolateral view.

Fig. 3 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 3. Metriorhynchid thalattosuchian Cricosaurus bambergensis sp. nov. (NKMB-P-Watt14/274) holotype, late Kimmeridgian of Wattendorf (southern Germany). A1, skull in ventrolateral view; A2, illustrates the preserved elements which can be unambiguously identified (please note that the dentary-surangular contact cannot be traced and is based upon the position in C. suevicus).

Fig. 2. A in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 2. A. Reduced stratigraphic table of the Kimmeridgian rock units of the northern Franconian Jurassic, based on Niebuhr and Pürner (2014). B, C. Maps showing the locality of NKMB-P-Watt14/274 at Wattendorf (asterisk) within the Bamberg district and its placement in Germany.

Fig. 7 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 7. Metriorhynchid thalattosuchian Cricosaurus bambergensis sp. nov. (NKMB-P-Watt14/274) holotype, late Kimmeridgian of Wattendorf (southern Germany). Hindlimb and pelvic girdle. Abbreviations: mt, metatarsals; ph, phalanges.

Fig. 9 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 9. Comparative images showing the ventral side of the skull and a close-up of the palatal region of metriorhynchid thalattosuchians Cricosaurus bambergensis sp. nov. (NKMB-P-Watt14/274, A) from the late Kimmeridgian of Wattendorf (southern Germany) and Cricosaurus elegans (BSPG AS I 504, B) from the lower Tithonian of Dating (southern Germany).

Fig. 6 in A new species of the metriorhynchid crocodylomorph Cricosaurus from the Upper Jurassic of southern Germany

Fig. 6. Metriorhynchid thalattosuchian Cricosaurus bambergensis sp. nov. (NKMB-P-Watt14/274) holotype, late Kimmeridgian of Wattendorf (southern Germany). Distal part of the tail showing the flexural and postflexural region.

Fig. 6. Echinocystitid echinoid Rhenechinus hopstaetteri Dehm, 1953, BSPG.1955 I 585 in Morphology and ecological setting of the basal echinoid genus Rhenechinus from the early Devonian of Spain and Germany

Fig. 6. Echinocystitid echinoid Rhenechinus hopstaetteri Dehm, 1953, BSPG.1955 I 585 (holotype), Hunsrück Slate, Lower Emsian, Lower Devonian; Gemünden, Rhineland−Palatinate, Germany. A. General view. B. Detail of ambulacral plating. C. Detail of oral region. Abbreviations: ps, peristomial membrane; t, tooth; 1, 2a, b, 3a–c, first three rows of interambulacral plates.

Fig. 1 in Morphology and ecological setting of the basal echinoid genus Rhenechinus from the early Devonian of Spain and Germany

Fig. 1. Map showing the geographical position and geological setting of the Aguión Formation and the echinoid bearing horizon (arrowed symbol), modified from García−Alcalde (1992).

Fig. 7. Echinocystitid echinoid Rhenechinus hopstaetteri Dehm, 1953 in Morphology and ecological setting of the basal echinoid genus Rhenechinus from the early Devonian of Spain and Germany

Fig. 7. Echinocystitid echinoid Rhenechinus hopstaetteri Dehm, 1953, DBM.HS 285, Hunsrück Slate, Lower Emsian, Lower Devonian; EschenbachBocksberg mine, Bundenbach, Rhineland−Palatinate, Germany. A. General view. B. Detail of adoral plating showing pedicellariae and spines. C. Detail of adoral ambulacral plating. Abbreviations: amb, ambulacral zone; ap, apical disc region; p, pedicellaria; ps, pedicellarial stalk element; pst, peristome.

Fig. 3 in Morphology and ecological setting of the basal echinoid genus Rhenechinus from the early Devonian of Spain and Germany

Fig. 3. Echinocystitid echinoid Rhenechinus ibericus (Hauser and Landeta, 2007). Aguión Formation, Emsian, Lower Devonian, Arnao, Asturias, NW Spain. A. UO DGO−23001 showing adoral plating and elements of the lantern. B. UO DGO−23000 showing partially articulated plating of the upper surface. Abbreviations: H, hemipyramid; t, tooth; 1, 2a, b, 3a–c, first three rows of interambulacral plates.

Fig. 3 in A new pleurocystitid blastozoan from the Middle Devonian of the Eifel (Germany) and its phylogenetic importance

Fig. 3. Interpretative camera lucida drawings of the pleurocystitid blastozoan Regulaecystis testudineus sp. nov., Nims Member of the Junkerberg Formation (Eifelian, Middle Devonian), Prüm Syncline (Rhenish Massif, Germany). A. Paratype GIK−2277, abanal face showing the plate names (A1) and anal face showing the shape of the periproct and the organisation of the primary opening area (A2). B. Holotype GIK−2276, anal face showing the insertion of the ornamented stem (B1) and lateral view showing the strengthening of the thecal margins due to strong ornamentation in thick ridges and thick granules (B2). C. Abanal face of the paratype GIK−2278 showing the dense granulation. Cup and isolated plates of Stylocrinus tabulatus (Goldfuss, 1839) are preserved in the anal face. Plate names abbreviations follow Kesling (1967). Scale bars 5 mm.

Fig. 2 in A new pleurocystitid blastozoan from the Middle Devonian of the Eifel (Germany) and its phylogenetic importance

Fig. 2. Pleurocystitid blastozoan Regulaecystis testudineus sp. nov., Nims Member of the Junkerberg Formation (Eifelian, Middle Devonian), Prüm Syncline (Rhenish Massif, Germany). A. Paratype GIK−2277, lateral view showing the flattened thecal flange and the rounded shape of the theca (A1), dorsal view showing the arched organisation of the plates (A2), lateral view showing the single pectinirhomb located at L3/L4 suture (A3), ventral view showing the organisation of the oral area (A4). B. Isolated plate GIK−2280, showing the slits of the pectinirhomb. C. Pluricolumnals adjacent to a reversed basal plate GIK−2279, showing the typical alternation of external and internal columnal in the proximal stem of the glyptocystitids. D. Paratype GIK−2278, dorsal view of the theca showing the reticulate ornamentation (D1), lateral view showing the intercalation of the circlets of plates (D2), aboral view showing the stem insertion and the organisation of the basals (D3). E. Holotype GIK−2276, lateral view showing the flattening of the theca, and the strong ornamentation (E1), ventral view showing the ornamentation at the margin of the theca and the elongate proximal portion and the thin ornamented distal portion of the stem (E2), and oblique dorsal view on the stem insertion and basal plates (E3). Scale bars 10 mm.

Fig. 1 in A new pleurocystitid blastozoan from the Middle Devonian of the Eifel (Germany) and its phylogenetic importance

Fig. 1. Geographical location of the fossiliferous sites near Prüm, Eifel (Rhenish Massif, Germany).

Fig. 4 in A new pleurocystitid blastozoan from the Middle Devonian of the Eifel (Germany) and its phylogenetic importance

Fig. 4. Pleurocystitida gen. et sp. indet. C from Hunsrückschiefer (Emsian, Lower Devonian), Bundenbach (Rhenish Massif, Germany). A. SMF−HS− 422, abanal face. B. SMF−HS−420, anal face. Scale bars 10 mm.

Fig. 5 in A new pleurocystitid blastozoan from the Middle Devonian of the Eifel (Germany) and its phylogenetic importance

Fig. 5. Strict consensus tree of the four shortest trees (45 steps) derived from PAUP and based on character data set in Appendix 2. The numbers adjacent to the nodes denote the respective support values: bold numbers being Bremer indices, italic numbers being bootstrap values> 50%. Major apomorphies have been reported on branches of the supported clades (see text and Appendix 1).