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Fig. 3 in Trichomonas stableri n. sp., an agent of trichomonosis in Pacific Coast band-tailed pigeons (Patagioenas fasciata monilis)

Fig. 3. Consensus phylogenetic tree of partial Fe-hydrogenase gene sequences (750 bp alignment) made by Bayesian inference. Legend denotes substitutions per site. All node posterior probabilities are>90% unless otherwise noted.

opencc-by-4.0Jul 2021View details →

Figure 3 in Ant (Hymenoptera: Formicidae) species diversity in secondary forest and three agricultural land uses of the Colombian Pacific Coast

Figure 3. Number of shared ant species and total number of specimens caught (pitfall and Winkler sack) between four areas of different land use. Two oil palm plots of three and seven years of age were pooled. El Mira Research Center, Tumaco, Pacific Coast of Colombia. / Número de especies de hormigas compartidas y número total de individuos capturados (Pitfall y sacos Winkler) entre cuatro áreas con diferente uso de tierra. Las dos parcelas de palma de aceite de tres y siete años fueron agrupadas. Centro de Investigación El Mira, Tumaco, Nariño, costa pacÍfica de Colombia.

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Figure 1 in Ant (Hymenoptera: Formicidae) species diversity in secondary forest and three agricultural land uses of the Colombian Pacific Coast

Figure 1. Map of El Mira Research Center of the Corporación Colombiana de Investigación Agropecuaria, Tumaco, Nariño, Pacific Coast of Colombia, with the location (arrows) of the pitfall trap transects. Yellow hybrid oil palm 7 years old; red hybrid oil palm 3 years old; black peach palm; white secondary forest. / Mapa del Centro de Investigación El Mira de la Corporación Colombiana de Investigación Agropecuaria, Tumaco, Nariño, costa pacÍfica de Colombia con la ubicación (flechas) de las trampas pitfall en los transectos. Amarillo palma de aceite hÍbrido 7 años; rojo palma de aceite hÍbrido 3 años; negro palma de chontaduro; blanco bosque secundario.

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Figure 2 in Ant (Hymenoptera: Formicidae) species diversity in secondary forest and three agricultural land uses of the Colombian Pacific Coast

Figure 2. Variation in 0D diversity (species number) of Formicidae between four areas of different land use: El Mira Research Center, Tumaco, Pacific Coast of Colombia. SF: secondary forest, PP: Peach palm, OP7: Oil palm 7 years old, OP3: Oil palm 3 years old. / Variación en la diversidad 0D (número de especies) de Formicidae entre cuatro áreas con diferente uso de tierra. Centro de Investigación El Mira de la Corporación Colombiana de Investigación Agropecuaria, Tumaco, Nariño, costa pacÍfica de Colombia.

Fig. 7. The relationship between antenna 1 in The Distinctive Species Characteristics Of Metaprotella Sandalensis Mayer, 1898 (Crustacea: Amphipoda), Commonly Distributed Throughout The Tropical West Pacific Coasts

Fig. 7. The relationship between antenna 1 length and body length of Metaprotella sandalensis collected from coastal areas of Lifou Island.

Fig. 4 in The Distinctive Species Characteristics Of Metaprotella Sandalensis Mayer, 1898 (Crustacea: Amphipoda), Commonly Distributed Throughout The Tropical West Pacific Coasts

Fig. 4. Metaprotella sandalensis, female, 5.03 mm, AM P.87576, Pointe de Easo (= Easho), Baie de Sandal, Lifou Island. Scales for G1 and G2 represent 0.1 mm; A1, A2, and whole body represent 0.2 mm.

Fig. 3 in The Distinctive Species Characteristics Of Metaprotella Sandalensis Mayer, 1898 (Crustacea: Amphipoda), Commonly Distributed Throughout The Tropical West Pacific Coasts

Fig. 3. Metaprotella sandalensis, male, 8.87 mm, AM P.87572, Pointe de Easo (= Easho), Baie de Sandal, Lifou Island. Scales for ABD (L) and ABD (V) represent 0.05 mm; P3 and P4 represent 0.1 mm; P5 and P7 represent 0.2 mm.

Fig. 5 in The Distinctive Species Characteristics Of Metaprotella Sandalensis Mayer, 1898 (Crustacea: Amphipoda), Commonly Distributed Throughout The Tropical West Pacific Coasts

Fig. 5. Metaprotella sandalensis, female, 5.03 mm, AM P.87576, Pointe de Easo (= Easho), Baie de Sandal, Lifou Island. All scales represent 0.05 mm.

Fig. 6 in The Distinctive Species Characteristics Of Metaprotella Sandalensis Mayer, 1898 (Crustacea: Amphipoda), Commonly Distributed Throughout The Tropical West Pacific Coasts

Fig. 6. Metaprotella sandalensis, female, 5.03 mm, AM P.87576, Pointe de Easo (= Easho), Baie de Sandal, Lifou Island. Scales for ABD (L) and ABD (V) represent 0.05 mm; P3, P4, P5, P6, and P7 represent 0.1 mm.

Fig. 2 in The Distinctive Species Characteristics Of Metaprotella Sandalensis Mayer, 1898 (Crustacea: Amphipoda), Commonly Distributed Throughout The Tropical West Pacific Coasts

Fig. 2. Metaprotella sandalensis, male, 8.87 mm, AM P.87572, Pointe de Easo (= Easho), Baie de Sandal, Lifou Island. All scales represent 0.05 mm.

Fig. 1 in The Distinctive Species Characteristics Of Metaprotella Sandalensis Mayer, 1898 (Crustacea: Amphipoda), Commonly Distributed Throughout The Tropical West Pacific Coasts

Fig. 1. Metaprotella sandalensis, male, 8.87 mm, AM P.87572, Pointe de Easo (= Easho), Baie de Sandal, Lifou Island. Scales for A1, G1, and HD represent 0.1 mm; A2 and G2 represent 0.2 mm; whole body represents 0.5 mm.

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Fig. 3 in Ammonite faunal dynamics across bio-events during the mid- and Late Cretaceous along the Russian Pacific coast

Fig. 3. Changes in the number of Cretaceous ammonite species from Far East Russia, arranged in the ten most speciose families: non−heteromorphs (Phylloceratidae, Tetragonitidae, Gaudryceratidae, Pachydiscidae, Kossmaticeratidae) and heteromorphs (Scaphitidae, Baculitidae, Turrilitidae, Nostoceratidae, Diplomoceratidae). Abbreviations: low., lower; mid., middle; up., upper.

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Fig. 4 in Ammonite faunal dynamics across bio-events during the mid- and Late Cretaceous along the Russian Pacific coast

Fig. 4. Regional bio−events recorded in ammonite assemblages from Far East Russian regions (present paper); regional palaeotemperature curves modified after Zakharov et al. (1998, 1999, 2005); generalised scheme of records of transgression and regression from Sakhalin and northeast Russia; global bio−events (Kauffmann and Hart 1995); global sea level curves by Haq et al. (1987); global palaeotemperature curves by Skelton (2003). Stages are shown without calibration to absolute time. Abbreviations: C–T, Cenomanian–Turonian boundary; Cr–Pg, Cretaceous Paleogene boundary; OAE, Oxygen Anoxic Event.

Fig. 8 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 8. Single most parsimonious tree derived from maximum parsimony analysis of 49 hadrosauroid species, highlighting the position of Saurolophus morrisi sp. nov. within saurolophine hadrosaurids. Numbers above the branches indicate decay indices (Bremer support), whereas those below indicate bootstrap frequencies. Lambeeosaurinae is collapsed into a single branch for clarity; lambeosaurine interrelationships recovered were identical to those in Fig. 7.

Fig. 1 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 1. Partial right postorbital of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2852), lower Maastrichtian Moreno Formation of San Benito County, California, USA, showing the autapomorphic ornamentation of its jugal process. Posterior (A) and right lateral (B) views.

Fig. 5 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 5. Appendicular elements of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2760, a subadult), lower Maastrichtian Moreno Formation of Panoche Hills, Fresno County, California, USA. A. Partial left scapula and coracoid in lateral view. B. Partially articulated forelimb elements. C. Proximal segment of right tibia in lateral view. D. Distal fragments of femora. E. Right metatarsal III in dorsal view.

Fig. 3 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 3. Right posterolateral view of the frontal of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2760, a subadult), lower Maastrichtian Moreno Formation of Panoche Hills, Fresno County, California, USA, showing the eroded remnant of the buttressing base of the posterodorsal frontal ramus.

Fig. 7 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 7. Strict consensus tree of the three most parsimonious trees derived from maximum parsimony analysis of 49 hadrosauroid species. LACM/CIT 2760 and 2852 were coded as separate OTUs and their position within Saurolophinae in highlighted in the cladogram. Numbers above the branches indicate decay indices (Bremer support), whereas those below indicate bootstrap frequencies.

Fig. 9 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 9. Comparison of the general skull and premaxillary morphology of two hadrosaurid dinosaurs Saurolophus osborni Brown, 1912, holotype AMNH 5220 (A) and Saurolophus morrisi sp. nov., holotype LACM/CIT 2852 (B), highlighting characters shared by these two taxa. Skull in right lateral view (A1, B1), right premaxilla in lateral view (A2, B2).The white inscription on the premaxilla denote the abbreviation for that bone, painted by the curatorial staff back in the early twentieth century.

Fig. 6 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 6. Appendicular elements of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2852), lower Maastrichtian Moreno Formation of San Benito County, California, USA. A. Partial right scapula in lateral view. B. Right ulna in lateral view and possible manual phalanx II−1 in dorsal view. C. Right metatarsal III in dorsal (C1) and lateral (C2) views.