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Fig. 8 in A new Andean anole species of the Dactyloa clade (Squamata: Iguanidae) from western Ecuador

Fig. 8. Phylogeny of the "western Dactyloa clade" sensu Castañeda and de Queiroz (2011), which is part of the aequatorialis series of Castañeda and de Queiroz (2013), and representatives of the heterodermus series (A. euskalerri- ari), punctatus series (A. transversalis), roquet series (A. lu- ciae), latifrons series (A. agassizi), and a non-Dactyloa Anolis (A. occultus). The tree is a majority rule (50%) consensus tree of 72,000 trees obtained from a Bayesian analysis of the mitochondrial genes COI, ND2, and adjacent tRNAs, and the nuclear gene RAG1. Asterisks correspond to posterior probability values ≥ 0.99. Voucher information is presented in Castañeda and de Queiroz (2011) and Table 1.

Fig. 5 in A new Andean anole species of the Dactyloa clade (Squamata: Iguanidae) from western Ecuador

Fig. 5. Distribution of Anolis gemmosus, A. otongae and A. poei sp. nov. along the first and second principal components axes.

Fig. 4. Part 2. A in A new Andean anole species of the Dactyloa clade (Squamata: Iguanidae) from western Ecuador

Fig. 4. Part 2. A. gemmosus: male (QCAZ 4352, I, J), male (QCAZ 4385, K, L), male (QCAZ 11849, M, N), and female (QCAZ 4393, O, P). All photographs by O. Torres-Carvajal, except A, M, N (S. R. Ron).

Fig. 1 in A new Andean anole species of the Dactyloa clade (Squamata: Iguanidae) from western Ecuador

Fig. 1. Head of the holotype (QCAZ 3449) of Anolis poei sp. nov. in dorsal (top), ventral (middle), and lateral (bottom) views [Scale bar = 10 mm]. Photographs by F. Ayala-Varela.

Fig. 4. Part 1 in A new Andean anole species of the Dactyloa clade (Squamata: Iguanidae) from western Ecuador

Fig. 4. Part 1. Five species of Anolis from western Ecuador. A. aequatorialis: male (QCAZ 11861, A) and female (QCAZ 3443, B); A. binotatus: male (QCAZ 3434, C, D); A. fasciatus: male (QCAZ 3450, E, F); A. otongae: male (QCAZ 11790, G) and female (QCAZ 11791, H).

Fig. 7 in A new Andean anole species of the Dactyloa clade (Squamata: Iguanidae) from western Ecuador

Fig. 7. Anolis poei sp. nov. Adult female (SVL = 46.47 mm, QCAZ 3454, A, B), subadult female (SVL = 47.99 mm, QCAZ 3446, C, D), juvenile male (SVL = 26.85 mm, QCAZ 3453, E, F). Photographs by O. Torres-Carvajal.

Fig. 6 in A new Andean anole species of the Dactyloa clade (Squamata: Iguanidae) from western Ecuador

Fig. 6. Tongue of Anolis poei sp. nov., subadult male (QCAZ 3455, top); A. gemmosus, adult male (QCAZ 4347, middle); A. otongae, adult male (QCAZ 4661, bottom). Photographs by S. R. Ron (top), O. Torres-Carvajal (middle, bottom).

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Figure 1. A in Field surveys in Western Panama indicate populations of Atelopus varius frogs are persisting in regions where Batrachochytrium dendrobatidis is now enzootic

Figure 1. A female Harlequin frog, Atelopus varius. This species, classified as Critically Endangered by IUCN, has been found in small numbers in the mountains of Western Panama.

Figure 8 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 8. (A) maximum likelihood (ML) phylogenetic tree of Pseudodon and (B) haplotype network of P. walpolei inferred from the COI dataset. Values at nodes indicate Bayesian inference (BI) posterior probability percentage/ML ultrafast bootstrap values. Support values>95% for both phylogenetic analyses are indicated by an asterisk. Support values marked with '-' indicate nodes that differ in the BI tree.

Figure 7 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 7. (A) phylogenetic tree of Lens, and (B) haplotype network of the L. contradens–lugens–micropterus clade inferred from the COI dataset.

Figure 6 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 6. (A) maximum likelihood (ML) phylogenetic tree and (B) haplotype network of Rectidens inferred from the COI dataset. Values at nodes indicate Bayesian inference (BI) posterior probability percentage/ML ultrafast bootstrap values. Support values>95% for both phylogenetic analyses are indicated by an asterisk. Support values marked with '-' indicate nodes that differ in the BI tree.

Figure 5 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 5. Images of type localities of (A) Ctenodesma mawonae, i.e. Sungai Sebua Jebung in the Sarawak River basin, Jambusan, Bau, Sarawak, Malaysian Borneo, and (B) Ctenodesma bersinara and Rectidens lauris, i.e. Sungai Rempangi, Pawan River basin, West Kalimantan, Indonesian Borneo.

Figure 4 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 4. Holotypes of Ctenodesma bersinara, Sungai Rempangi, Pawan River basin, West Kalimantan, Indonesian Borneo; Ctenodesma mawonae, Sungai Sebua Jebung, Sarawak River basin, Jambusan, Bau, Sarawak, Malaysian Borneo; and Rectidens lauris, Sungai Rempangi, Pawan River basin, West Kalimantan, Borneo. Abbreviations: FKH, Fahutan Kapuas Hulu Collection, Tanjungpura University, Indonesia; FRST, Faculty of Resource Science and Technology Collection, Universiti Malaysia Sarawak, Malaysia.

Figure 2 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 2. Maximum likelihood (ML) phylogenetic tree inferred from the combined (COI + 16S + ND1 + 18S + 28S) dataset. Values at nodes indicate Bayesian inference (BI) posterior probability percentage/ML ultrafast bootstrap values. Support values>95% for both phylogenetic analyses are indicated by an asterisk. Support values marked with '-' indicate nodes that differ in the BI tree. Species present in Borneo in bold. Species for which DNA sequences are first reported in the present paper in red. Gonideinae clades marked in red; non-Gonideinae clades marked in green.

Figure 1 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 1. Map of western Borneo, showing sites and species of freshwater mussels (Bivalvia: Unionida) found and collected during fieldwork in 2019 and 2022. Protected Areas shapefiles derived from UNEP-WCMC and IUCN (2023). HydroBASINS (Lehner and Grill 2013) shown as solid (level 4) and dashed (level 6) lines.

Figure 3 in High endemic freshwater mussel (Bivalvia: Unionida) diversity in western Borneo, with description of three new species

Figure 3. Types and sequenced specimens of Discomya radulosa, Caudiculatus caudiculatus, Lens lugens, and Pseudodon walpolei. Abbreviations: FKH, Fahutan Kapuas Hulu Collection, Tanjungpura University, Indonesia; MCZ, Museum of Comparative Zoology, Cambridge, USA; MNHN, Muséum National d'Histoire Naturelle, Paris, France; ZMB, Museum für Naturkunde, Berlin, Germany

Fig. 6 in Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau Formation of western Newfoundland

Fig. 6. Problematic taxa from the Lower Cambrian, Forteau Formation (Western Newfoundland). A, B. Chancelloria sp. A. Phosphatic internal mould, NFM−707; B. Phosphatic internal mould viewed from basal facet, NFM−708. C, D. Archiasterella sp. C. NFM−709 from ICS 1421, phosphatic internal mould; C1, lateral view; C2, viewed from basal facet. D. NFM−710, oblique view of phosphatic internal mould. E, F. Hyolithellus sp. E. NFM−711. F. NFM−712. G. Lapworthella shodakensis (Lochman, 1956). NFM−713, dorso−ventrally flattened sclerite; in lateral (G1) and dorsal (G2) views. All specimens from JSP 1982−01 unless otherwise stated. Scale bars 200 ̊m.

Fig. 1 in Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau Formation of western Newfoundland

Fig. 1. Lower Cambrian localities in eastern Laurentia (A), map of Newfoundland indicating the Bonne Bay region (B) and simplified Lower Cambrian stratigraphy in western Newfoundland (C).

Fig. 2 in Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau Formation of western Newfoundland

Fig. 2. Brachiopods from the Lower Cambrian, Forteau Formation (Western Newfoundland). A, B. Eoobolus priscus (Poulsen, 1932). A. NFM−662, exterior view of incomplete ventral valve. B. NFM−663, ventral valve interior with pseudointerarea. C. Ventral valve of Eothele sp., NFM−664 from ICS 1421. D, E. Acrotretid indet. D. NFM−665, ventral valve exterior. E. NFM−666, dorsal valve exterior. F, G. Micromitra bella (Billings, 1872). F. NFM−667, ventral valve interior. G. NFM−668, dorsal valve interior. H, I. Obolella crassa (Hall, 1847). H. NFM−669, fragmentary ventral valve interior. I. NFM−670, fragmentary dorsal valve interior. All specimens from JSP 1982−01 unless otherwise stated. Scale bars 500 ̊m.

Fig. 3 in Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau Formation of western Newfoundland

Fig. 3. Trilobites, echinoderms, and sponges from the Lower Cambrian, Forteau Formation (Western Newfoundland). A. Dorypygidae indet., internal mould of fragmentary cephalon, NFM−671 from ICS 1421; in dorsal (A1) and left lateral (A2) views. B. Calodiscus lobatus (Hall, 1847), NFM−672, dorsal view of silicified cephalon. C. Ptychoparioid indet., NFM−673 from ICS 1421, silicified cephalon. D. Olenellid indet., NFM−674 from ICS 1421, dorsal view of silicified juvenile cephalon. E–J. Phosphatised echinoderm ossicles. E. Morphotype 1, NFM−675, dorsal view. F. Morphotype 1, NFM−676, dorsal view. G. Morphotype 1, NFM−677, ventral view. H. Morphotype 2, NFM−678, ventral view. I. Morphotype 2, NFM−679, dorsal view. J. Morphotype 2, NFM−680, oblique lateral view. K. Hexactinellid spicule, NFM−681, scale bar 100 ̊m. All specimens from JSP 1982−01 unless otherwise stated. All scale bars except K 500 ̊m.