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FIGURE 25 in LARGE SCAPHITID AMMONITES (HOPLOSCAPHITES) FROM THE UPPER CRETACEOUS (UPPER CAMPANIAN–LOWER MAASTRICHTIAN) OF NORTH AMERICA: ENDLESS VARIATION ON A SINGLE THEME
FIGURE 25. Hoploscaphites crassus (Coryell and Salmon, 1934), macroconch. A–D. BHI 4292, Baculites baculus Zone, Pierre Shale, Cedar Creek Anticline, east-central Montana. A, Right lateral; B, apertural; C, ventral; D, left lateral. Arrow indicates the base of the body chamber.
Figure 1 in Integrative taxonomy of two morphologically similar species of the subgenus Cryobius Chaudoir, 1838 (Coleoptera: Carabidae: Pterostichus Bonelli, 1810) from northern Eurasia and North America
Figure 1. Males of Pterostichus (Cryobius) kolymensis with genital structures (median lobe of aedeagus in right lateral aspect, right and left parameres): A – holotype (Kolyma Lowland, near Chersky settlement, collected by S. Kolesnikov); B – paratype (Kolyma Lowland, near Krestovka River, collected by S. Kiselev); C – paratype (western Chukotka, near Valkumey settlement, collected by S. Kiselev). The photos are taken by N.A. Zubrii. Scale bars: 5 mm for the body and 1 mm for the structures of genitalia.
Figure 3 in Integrative taxonomy of two morphologically similar species of the subgenus Cryobius Chaudoir, 1838 (Coleoptera: Carabidae: Pterostichus Bonelli, 1810) from northern Eurasia and North America
Figure 3. Scatter plots of principal component (PC) scores of the specimens on the first two axes for the shapes of the pronotum (A), median lobe of the aedeagus (B), and apex of the median lobe of the aedeagus (C) of P. (C.) mandibularoides (red color – population from Chukotka; blue color – population from Yakutia) and P. (C.) kolymensis (grey color) (H – holotype). The reconstructed outlines with the standard deviations (±2 S.D.) for the analysed morphological structures are shown in the individual plots.
Figure 2 in Integrative taxonomy of two morphologically similar species of the subgenus Cryobius Chaudoir, 1838 (Coleoptera: Carabidae: Pterostichus Bonelli, 1810) from northern Eurasia and North America
Figure 2. Median-joining haplotype network of the COI sequences of Pterostichus (Cryobius) mandibularoides dataset (n = 30). The red numbers near the branches indicate the number of nucleotide substitutions between haplotypes. The size of the circles corresponds to the number of available sequences for each haplotype (smallest circle = 1 sequence). See Table 1 for the list of sequences. The photo of a male specimen with genital structures (from left to right: median lobe of aedeagus in right lateral and ventral aspect, right and left parameres) is taken by N.A. Zubrii. Scale bars: 1 mm for the body and 0.5 mm for the structures of genitalia.
Fig. 1 in The biogeography of the caribou lungworm, Varestrongylus eleguneniensis (Nematoda: Protostrongylidae) across northern North America
Fig. 1. Map of Northern North America, including Alaska, USA, Canada and Greenland depicting the geographic distribution of caribou subspecies (Rangifer tarandus sspp.). The distribution of the caribou lungworm, Varestrongylus eleguneniensis, and the muscleworm, Parelaphostrongylus andersoni in caribou is shown based on compiled data from the present study, and all reports in the literature (Lankester and Hauta, 1989; Lankester and Fong, 1998; Kutz et al., 2007, 2012; 2013; Verocai et al., 2013; Kafle et al., 2017a, 2017b; Turgeon et al., 2018). The historic southern range of distribution of caribou is shown as a dotted line to assist in the discussions on the historical biogeography of V. eleguneniensis and Rangifer. (See Fig. S1 and Fig. S2 for the distribution maps for V. eleguneniensis and P. andersoni separately).
Fig. 22.1 in Chapter 22: Rodents from the Chinese Neogene: Biogeographic Relationships with Europe and North America
Fig. 22.1. Distribution of Neogene rodent localities in China. , Early Miocene (Xiejian + Shanwangian): 1, Suosuoquan; 2, Xiejia; 3, Gaolanshan; 4, Zhangjiaping; 5, Gashunyinadege; 6, Wuertu; 7, Shanwang; 8, Sihong (Songlinzhuang, Zhengji, Shuanggou); 9, Fangshan. v, Middle Miocene (Tunggurian): 10, Halamagai; 11, Quantougou; 12, Lierpu (Qijia, Danshuilu); 13, Dingjiaergou; 14, Tunggur; 15, Tairum Nor. M, Late Miocene (Baodean): 16, Songshan; 17, Bulong; 18, Jilong; 19, Qingyang; 20, Baode; 21, Lantian (Bahe); 22, Amuwusu; 23, Shala; 24, Baogedawula; 25, Ertemte (Harr Obo); 26, Shihuiba; 27, Yuanmou. ·, Pliocene (Yushean): 28, Bilike; 29, Jingle; 30, Dingcun; 31, Youhe; 32, Daodi; 33, Zhoukoudian (Cap Travertine); 34, Yinan; 35, Zhaotong; 36, Wushan.., Late Miocene + Pliocene: 37, Yushe (Mahui; Gaozhuang; Mazegou; Haiyan; Jiayucun); 38, Lingtai (Wenwanggou).
Fig. 1 in Catalog Of The Dolichopodidae (Diptera) Of America North Of Mexico
Fig. 1. Cumulative number of species described from America north of Mexico between 1758 and February 2004.
Fig. 52. Discoscaphites jerseyensis, n in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 52. Discoscaphites jerseyensis, n.sp., macroconchs, Pinna Layer, top of the Tinton Formation, Manasquan River Basin, Monmouth County, New Jersey. A–D. AMNH 50393, holotype. A. Right lateral; B. apertural; C. ventral; D. left lateral. E–H. AMNH 50774, paratype. E. Right lateral; F. apertural; G. ventral; H. left lateral. All figures X1.
Fig. 46 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 46. Size frequency histogram of a sample of Discoscaphites iris (Conrad, 1858) from the upper part of the Tinton Formation, mostly the Pinna Layer, Manasquan River Basin, Monmouth County, New Jersey.
Fig. 51 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 51. Discoscaphites gulosus (Morton, 1834), macroconch, MAPS A2025c1, Pinna Layer, top of the Tinton Formation, Manasquan River Basin, Monmouth County, New Jersey. A. Lateral view of part of the shaft; B. ventral view. Both figures X1.
Fig. 50 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 50. Discoscaphites minardi Landman et al., 2004a, macroconchs, or indeterminate (as indicated), Pinna Layer, and underlying part of Tinton Formation (as indicated), Manasquan River Basin, Monmouth County, New Jersey. A–C. AMNH 50760, underlying part of the Tinton Formation. A. Right lateral; B. ventral; C. left lateral. D,E. AMNH 50759. D. Right lateral; E. ventral. F,G. AMNH 50758, dimorph indeterminate, but probably a microconch. F. Ventral; G. left lateral. H,I. AMNH 50761.
Fig. 44 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 44. Discoscaphites iris (Conrad, 1858). A–Q. Pinna Layer, Tinton Formation, and reworked material at the base of the Hornerstown Formation (as indicated), Manasquan River Basin, Monmouth County, New Jersey. A,B. MAPS A2060b34, a microconch. A. Ventral; B. left lateral. C,D. MAPS A2060b33, a microconch. C. Ventral; D. left lateral. E. MAPS A2060b1, part of a cluster of juveniles, with the bottom side down. F–I. AMNH 50711, a microconch. F. Right lateral; G. apertural; H. ventral; I. left
Fig. 38 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 38. Top. Size histogram of a sample of Eubaculites latecarinatus (Brunnschweiler, 1966), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. Most of the specimens are fragments of juvenile body chambers. Bottom. Scatter plot of whorl width versus height in the same sample of E. latecarinatus. Measurements are at the adoral ends of the specimens.
Fig. 37 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 37. Eubaculites latecarinatus (Brunnschweiler, 1966), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A–E. AMNH 51877. A. Right lateral; B. dorsal; C. ventral; D. left lateral; E. whorl section at adoral end. F–I. AMNH 51876. F. Right lateral; G. dorsal; H. ventral; I. left lateral. J–M. AMNH 51862. J. Right lateral; K. dorsal; L. ventral; M. left lateral. N–Q. AMNH 51875. N. Right lateral; O. dorsal; P. ventral; Q. left lateral. All figures X1.
Fig. 43 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 43. Discoscaphites iris (Conrad, 1858), macroconchs. A–E, G–S. Pinna Layer and the underlying part of the Tinton Formation (as indicated), Manasquan River Basin, Monmouth County, New Jersey. A– D. AMNH 50398, slightly crushed, underlying part of the Tinton Formation. A. Right lateral; B. apertural; C. ventral; D. left lateral. E. AMNH 50387, small specimen, partially sideritized, left lateral. G,H. AMNH 50756. G. Right lateral; H. ventral. I,J. AMNH 50389. I. Right lateral; J. ventral. K–M.
Fig. 36 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 36. Eubaculites latecarinatus (Brunnschweiler, 1966), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A,B. AMNH 50419. A. Ventral; B. right lateral. C– G. AMNH 50435. C. Right lateral; D. dorsal; E. ventral; F. left lateral; G. whorl section at adapical end. H–L. AMNH 51888. H. Right lateral; I. dorsal; J. ventral K. left lateral; L. whorl section at adoral end. M–P. AMNH 51874. M. Right lateral; N. dorsal; O. ventral; P. left lateral. Q–U. AMNH 51864. Q. Right lateral; R. dorsal; S. ventral; T. left lateral; U. whorl section at adapical end. V–Y. AMNH 51863. V. Right lateral; W. dorsal; X. ventral; Y. left lateral. All figures X1.
Fig. 35 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 35. Top. Size histogram of a sample of Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County. Nearly all of the specimens are fragments of juvenile body chambers with some exceptions, notably the two largest specimens (AMNH 50766 and MAPS A2058b1), which are presumably mature macroconchs. Bottom. Scatter plot of whorl width versus height in intercostal section in the same sample of E. carinatus. All measurements are at the adoral ends of the specimens. The Xs and Os represent measurements through the ontogeny of AMNH 50766 and MAPS A2058b1, respectively (the open circles indicate the septate portion of MAPS A2058b1; AMNH 50766 is completely septate.) The triangle represents another large body chamber (MAPS A2058b2), presumably a macroconch.
Fig. 34 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 34. Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A. AMNH 50723, composite suture at WH 5 16.7 mm. B. AMNH 50778, suture at WH 5 22.2 mm. C. AMNH 50721, suture at WH 5 9.9 mm.
Fig. 33 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 33. Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A–D. AMNH 50721. A. Right lateral; B. dorsal; C. ventral; D. left lateral. E–H. AMNH 50767. E. Right lateral; F. dorsal; G. ventral; H. left lateral. I–M. AMNH 50768. I. Right lateral; J. dorsal; K. ventral; L. left lateral; M. whorl section at adapical end. N–Q. AMNH 50779. N. Right lateral; O. dorsal; P. ventral; Q. left lateral. All figures X1.
Fig. 31 in CEPHALOPODS FROM THE CRETACEOUS/TERTIARY BOUNDARY INTERVAL ON THE ATLANTIC COASTAL PLAIN, WITH A DESCRIPTION OF THE HIGHEST AMMONITE ZONES IN NORTH AMERICA. PART III. MANASQUAN RIVER BASIN, MONMOUTH COUNTY, NEW JERSEY
Fig. 31. Eubaculites carinatus (Morton, 1834), Pinna Layer, Tinton Formation, Manasquan River Basin, central Monmouth County, New Jersey. A–D. AMNH 50781. A. Right lateral; B. dorsal; C. ventral; D. left lateral. E–H. AMNH 50418. E. Right lateral; F. dorsal; G. ventral; H. left lateral. I. AMNH 50737, mature microconch in matrix, with a possible apertural modification, right lateral. All figures X1.
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