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Fig. 4 in The castorid Steneofiber from NW Germany and its implications for the taxonomy of Miocene beavers

Fig. 4. Occlusal pattern of lower cheek teeth of the castorid Steneofiber depereti from the middle Miocene of Hambach 6C, northwestern Germany. Mandibular tooth rows (A–E), deciduous teeth (F, G), premolars (H–J), molars (K–R); left p4–m3, IPB−HaH 6408 (A); right p4–m3, IPB−HaH 6409 (B); left p4–m3, IPB−HaH 5149 (C); right m1–m3, IPB−HaH 5150 (D); left p4–m2, IPB−HaH 5167 (E); left dp4, IPB−HaH 6392 (F); right dp4, IPB−HaH 6393 (G); right p4, IPB−HaH 6396 (H); right p4, IPB−HaH 6395 (I); left p4, IPB−HaH 6397 (J); left m1/2, IPB−HaH 6399 (K); right m1/2, IPB−HaH 5100 (L); right m1/2, slightly worn with a lingually open metaflexid, IPB−HaH 5043 (M); right m1/2, IPB−HaH 5106 (N); right m1/2, IPB−HaH 6400 (O); right m3, IPB−HaH 5110 (P); left m3, IPB−HaH 6404 (Q); right m3, IPB−HaH 6402 (R).

Fig. 3 in The castorid Steneofiber from NW Germany and its implications for the taxonomy of Miocene beavers

Fig. 3. Incisors of the castorid Steneofiber depereti from the middle Miocene of Hambach 6C, northwestern Germany. A. Tip of right I (IPB−HaH 6418) in oblique−lateral (A1) and lingual (A2) views. B. Tip of left I (IPB−HaH 6419) in lateral view.

Fig. 4 in Taxonomy, nomenclature, and evolution of the early schubertellid fusulinids

Fig. 4. Type of Biwaella and Biwaella poletaevi sp. nov. A–H. Biwaella poletaevi sp. nov. A–G. Kalinovo section, P 2 Limestone, Donets Basin, Ukraine. 2 A. SUI 114238, sample A−3/31a−8, axial section of paratype (A1), box indicates the enlarged part of final volution in A1 showing coarse mural pores (A2). B. SUI 114239, sample A−3/31a−5, axial section of paratype. C. SUI 114240, sample A−3/31a−77; sagital section of paratype. D. SUI 114241, sample A−3/31a−83, axial section of holotype. E. SUI 114242, sample A−3/31a−84, axial section of paratype. F. SUI 114243, sample A−3/31a−96, axial section of paratype. G. SUI 114244, sample A−3/31a−8; sagital section of paratype. H. Biwaella omiensis Morikawa and Isomi, 1960, repository unknown, axial section of holotype, from Morikawa and Isomi (1960: pl. 54: 1);?Artinskian; Minamitoba, near Lake Biwa, Shiga Prefecture, Japan. Scale bars: A1, D–F, H 1 mm, C 0.5 mm, A2 0.1 mm, G 0.1 mm.

Fig. 8 in The castorid Steneofiber from NW Germany and its implications for the taxonomy of Miocene beavers

Fig. 8. Lengths of mandibular tooth rows of Steneofiber depereti from the middle Miocene of Hambach 6C, in comparison to other representatives of the genus from early and middle Miocene localities in France, and in comparison to representatives of Chalicomys. For St. Gérand and Hambach are both given the lengths of occlusal surfaces and the alveole lengths. Data for Steneofiber castorinus and S. depereti from Artenay (marked with *) from Stefen (2005), for subspecies of S. depereti in the Loire Basin from Hugueney (1999), for "Chalicomys" batalleri from Casanovas−Vilar et al. (2008), and for Chalicomys jaegeri from Kaup (1833) and Ünay (1976).

Fig. 7 in The castorid Steneofiber from NW Germany and its implications for the taxonomy of Miocene beavers

Fig. 7. Dimensions of lower cheek teeth of the castorid Steneofiber depereti from the middle Miocene of Hambach 6C, northwestern Germany, in comparison to material from early and middle Miocene localities in France and Germany. Data for Eggingen−Mittelhart (MN 4) (CS unpublished data) and Sach and Heizmann (2001), for Artenay (MN 4) (CS unpublished data), for La Brosse (MN 3) from Ginsburg et al. (2000), for Viehhausen (MN 5) from Seemann (1938), and for Sos (MN 5) from Ginsburg (1967). "Chalicomys" batalleri from Abocador de Can Mata, Spain, MN 7/8 (Casanovas−Vilar et al. 2008) is included. Lower premolars (A) and lower molars (B).

Fig. 3 in Taxonomy, nomenclature, and evolution of the early schubertellid fusulinids

Fig. 3. Biwaella zhikalyaki sp. nov. from Kalinovo section, P 2 Limestone, lower Gzhelian, Donets Basin, Ukraine. A. SUI 114228, sample A−3/31a−2; axial 2 section of paratype (A1), box indicates the enlarged part of final volution in A1, showing coarse mural pores (A2). B. SUI 114229, sample A−3/31a−14; axial section of holotype (B1) arrow pointed into septal pores, box indicates the enlarged part of final volution in B1 showing coarse mural pores (B2). C. SUI 114230, sample A−3/31a−93; axial section of paratype. D. SUI 114231, sample A−3/31a−79; axial section of paratype. E. SUI 114232, sample A−3/31a−97; axial section of paratype. F. SUI 114233, sample A−3/31a−21; axial section of paratype. G. SUI 114234, sample A−3/31a−77; axial section of paratype. H. SUI 114235, sample A−3/31a−84; axial section of paratype. I. SUI 114236, sample A−3/31a−88; axial section of paratype. J. SUI 114237, sample A−3/31a−101; axial section of paratype. Scale bars: A1, B1, C–J 1 mm, B2 0.1 mm.

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Fig. 1. IPS 31102, a left maxillary fragment with the upper incisor and P4–M2 in The Never-Ending Problem of Miocene Beaver Taxonomy

Fig. 1. IPS 31102, a left maxillary fragment with the upper incisor and P4–M2 of the castorid Chalicomys catalaunicus (Bataller, 1838) from Sant Quirze (MN7+8 from the Vallès−Penedès Basin, Catalonia, Spain). Note the abundant cement infilling all synclines.

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Fig. 2 in The Never-Ending Problem of Miocene Beaver Taxonomy

Fig. 2. Scatterplot for the lower cheek teeth of all the Chalicomys species as compared to Steneofiber depereti. Schreuderia adroveri and Euroxenomys minutus rhenanus comb. nov. are also included for discussion (see text for details). A. m 1/2. B. m3 C. p4. The measurements for S. depereti from Hambach were taken from Mörs and Stefen (2010); for Chalicomys jaegeri from Eppelsheim from Stefen (2009) and from MB2B from Van de Weerd (1976); for Chalicomys plassi and E. minutus rhenanus from Dorn−Dürkheim from Franzen and Storch (1975); for S. adroveri from Torrent de Febulines from Aldana Carrasco (1992); for Chalicomys batalleri from ACM/C4–C2 and Chalicomys subpyrenaicus from Simorre from Casanovas−Vilar et al. (2008); and for Chalicomys catalaunicus from Sant Quirze from Crusafont Pairó et al. (1948) and Casanovas−Vilar et al. (2008). Acronyms for locality names are as follows: ACM/C4–C2, Abocador de Can Mata locality C4–C2; MB2B, Masía del Barbo 2B. All the measurements are in millimetres.

Fig. 8 in Lower Tithonian microconchiate simoceratins from eastern Mexico: Taxonomy, biostratigraphy, and palaeobiogeography

Fig. 8. Simoceratin ammonoid Pseudovolanoceras aesinense chiagnahuapense (Cantú−Chapa, 1990), suture lines. A. IGM 9555 [M], last incomplete suture at 70 mm of shell diameter. B. IGM 9544 [m], incomplete suture at 26.19 mm of shell diameter.

Fig. 4 in Lower Tithonian microconchiate simoceratins from eastern Mexico: Taxonomy, biostratigraphy, and palaeobiogeography

Fig. 4. Simoceratin ammonoid Pseudovolanoceras aesinense chignahuapense (Cantú−Chapa, 1990) [microconch]. A–F. From the Apulco section (MT−2). A. Right−side view of IGM 6085−2a showing lappet, bed 21b. B. Right−side view of IGM 9541; eroded and slightly distorted specimen, bed 21b. C. IGM 9543a, close−up view showing incipient longitudinal furrow between tubercles (C1) (see text for allusion to "cordone spirale"); right−side view (C2), bed 25. D, E. IGM 9546a and b, both from the same flattened inner mould. D. Imprint of the left side. E. Left−side view; arrows for lappet and tubercles showing riblets, bed 25. F. Left−side view of IGM 9542a, bed 21b. G. IGM 9544; G1, right−side view, arrow showing the last suture line preserved; G2, close−up view from the body chamber showing tubercles with riblets (arrows); G3, ventral view showing longitudinal furrow between tubercles, arrows indicate the trace of the "cordone spirale" (see text for allusion to "cordone spirale"); G4, close−up view of inner whorls showing tubercles with riblets (arrows); from MTQ section, bed 11.

Fig. 1 in Lower Tithonian microconchiate simoceratins from eastern Mexico: Taxonomy, biostratigraphy, and palaeobiogeography

Fig. 1. Location of the studied sections. A. Regional location for Puebla state. B. Inlet for the precise location of the sections investigated on the banks of the Apulco River in the Mazatepec area.

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Fig. 2 in X-ray Microtomography (XMT) of Fossil Brachiopod Shell Interiors for Taxonomy

Fig. 2. Transverse serial sections of Terebratula terebratula (Linnaeus, 1758), through specimen ZPAL Bp.XLIV/9; Pliocene, Velerín, Spain. Numbers indicate distance in mm from the tip of the ventral umbo.

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Fig. 1 in X-ray Microtomography (XMT) of Fossil Brachiopod Shell Interiors for Taxonomy

Fig. 1. Terebratulide brachiopod Terebratula terebratula (Linnaeus, 1758), Pliocene, Velerín, Spain; complete specimen, ZPAL Bp.XLIV/9. A. Dorsal view. B. Reconstruction of 3−D internal structure with virtually cut out part of the ventral valve.

Fig. 10 in New molecular data help clarify the taxonomy of Central European avian Dicrocoeliidae Looss, 1899 (Trematoda: Plagiorchiida)

Fig. 10. Representative photographs of slides with Lyperosomum turdia. Host species, sampling dates and host identification numbers are indicated. All specimens originated from the Czech Republic.

Fig. 5 in New molecular data help clarify the taxonomy of Central European avian Dicrocoeliidae Looss, 1899 (Trematoda: Plagiorchiida)

Fig. 5. Representative photographs of slides with Brachydistomum olssoni, Brachydistomum salebrosum, and Brachydistomum ventricosum. Host species, sampling dates and host identification numbers are indicated. All specimens originated from the Czech Republic.

Fig. 4 in New molecular data help clarify the taxonomy of Central European avian Dicrocoeliidae Looss, 1899 (Trematoda: Plagiorchiida)

Fig. 4. Maximum likelihood analysis of sequences of the ITS2 DNA locus of Dicrocoeliidae. Bootstrap values (n = 1000) are indicated for nodal support. Black circles indicate new sequences. The scale-bar indicates the number of substitutions per nucleotide site.

Fig. 1 in New molecular data help clarify the taxonomy of Central European avian Dicrocoeliidae Looss, 1899 (Trematoda: Plagiorchiida)

Fig. 1. Maximum likelihood analysis of sequences of the CO1 DNA locus of Dicrocoeliidae. Bootstrap values (n = 1000) are indicated for nodal support. Black circles indicate new sequences. The scale-bar indicates the number of substitutions per nucleotide site.

Fig. 3 in New molecular data help clarify the taxonomy of Central European avian Dicrocoeliidae Looss, 1899 (Trematoda: Plagiorchiida)

Fig. 3. Maximum likelihood analysis of sequences of nuclear DNA loci (28S rDNA (A) and 18S rDNA (B)) of Dicrocoeliidae. Bootstrap values (n = 1000) are indicated for nodal support. Black circles indicate new sequences. The scale-bars indicate the number of substitutions per nucleotide site.

Fig. 2 in New molecular data help clarify the taxonomy of Central European avian Dicrocoeliidae Looss, 1899 (Trematoda: Plagiorchiida)

Fig. 2. Maximum likelihood analysis of sequences of the ND1 DNA locus of Dicrocoeliidae. Bootstrap values (n = 1000) are indicated for nodal support. Black circles indicate new sequences. The scale-bar indicates the number of substitutions per nucleotide site.

Fig. 9 in New molecular data help clarify the taxonomy of Central European avian Dicrocoeliidae Looss, 1899 (Trematoda: Plagiorchiida)

Fig. 9. Representative photographs of slides with Lyperosomum petiolatum. Host species, sampling dates and host identification numbers are indicated. All specimens originated from the Czech Republic.