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FIGURE 7 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 7. Canonical variate plot for analysis of cranial data with Castor californicus treated as a distinct taxon a priori. Axes depict shape variation, associated with landmark deformations, indicated by thin plate splines deformation grids.

FIGURE 1 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 1. Late Miocene through Late Pleistocene fossil localities of Castor across North America. Locality points obtained from NOW database of Fossil Mammals.

FIGURE 5 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 5. Relative warp plot for the dentary. Axes depict shape variation, associated with landmark deformations indicated by thin plate splines deformation grids.

FIGURE 6 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 6. Histogram of canonical variate scores for analysis of cranial data with Castor californicus treated as an unknown. The x axis depicts shape variation, associated with landmark deformations, indicated by thin plate splines deformation grids. The y axis indicates the frequency of canonical variate scores among studied taxa.

FIGURE 4 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 4. Relative warp plot for the lateral view of the cranium. Axes depict shape variation, associated with landmark deformations, indicated by thin plate splines deformation grids.

FIGURE 3 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 3. Relative warp plot for the dorsal view of the cranium. Axes depict shape variation, associated with landmark deformations, indicated by thin plate splines deformation grids.

FIGURE 2 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 2. Landmark placement for craniums in dorsal (A), lateral (B), and ventral (C) views and dentaries (D) in lateral view on Castor canadensis MVZ 80744. Definitions of landmarks are outlined in Table 1 for the cranium and Table 2 for the dentary.

FIGURE 10 in Comparison of Miocene to early Pleistocene-aged Castor californicus (Rodentia: Castoridae) to extant beavers and implications for the evolution of Castor in North America

FIGURE 10. Dendrogram of cranial hierarchical cluster analysis. Specimens used in analysis are labeled by species and catalog number.

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Figure 5. Bayesian phylogeny, with species divergence age estimates reconstructed with BEAST using all the 26 in Complete mitochondrial genomes from museum specimens clarify millipede evolution in the Eastern Arc Mountains

Figure 5. Bayesian phylogeny, with species divergence age estimates reconstructed with BEAST using all the 26 mitochondrial genomes generated in this study. The dataset was supplemented with Thyropygus sp. and Abacion magnum as outgroups, derived from GenBank. GenBank accession numbers are provided in parentheses. Blue bars indicate the 95% highest probability density intervals for node ages. Age estimation for lineage divergence was based on a general arthropod mitochondrial DNA substitution rate and should be considered with caution. *Thyropygus sp. (red font) is very likely to be a misidentification; for more information, see the Discussion.

Figure 37 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 37. Known (solid lines) and projected (dashed line) distributions of the Order Callipodida. The question mark denotes the record from Budapest, Hungary, whose origin is uncertain.

Figure 29 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 29. Known (solid lines) and projected (dashed lines) distributions of the Order Spirostreptida s. l. (sensu Hoffman 1980a, Shelley 2003a), parameters as in Fig. 1. Asterisk, location of Protosilvestria sculpta, the Oligocene fossil from Quercy, France (Mauriès 1992).

Figure 49-50. Distributions. 49 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 49-50. Distributions. 49) Distributions of Merocheta/Polydesmida in Europe, North Africa, the Middle East, and western Asia; the dotted line circumscribes an area lacking both records and samples. 50) Distributions of Merocheta/Polydesmida in Central Asia; the dotted line circumscribes an area lacking both records and samples.

Figure 28 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 28. Distribution of the Order Spirobolida, parameters as in Fig. 1. Inverted triangle, location of Gobiulus sabulosus Dzik, 1975, the Cretaceous fossil from Mongolia.

Figure 41 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 41. Known (solid lines) and projected (dashed lines) distributions of the Order Chordeumatida, parameters as in Fig. 1; a few records are available from the dotted area in North America. The upper arrow denotes the Tingupidae record from Kodiak Island, Alaska, USA, and the lower one indicates the known and projected ranges of Eudigonidae in Chile.

Figure 45-46. Distributions. 45 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 45-46. Distributions. 45) Distribution of the Order Stemmiulida. 46) Known (solid lines) and projected (dashed lines) distributions of the Superorder Merocheta and the Order Polydesmida, parameters as in Fig. 1. No records or samples are available from the dotted areas.

Figure 39 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 39. Distribution of Callipodida in Europe and the Middle East. The question mark denotes the record from Budapest, Hungary, whose origin is uncertain.

Figure 34-35. Distributions. 34 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 34-35. Distributions. 34) Known (solid lines) and projected (dashed lines) distributions of the Suborder Spirostreptidea, parameters as in Fig. 1. 35) Known (solid lines) and projected (dashed lines) distributions of the Superorder Nematophora, parameters as in Fig. 1; a few records are available from the dotted area in North America. The upper arrow denotes the Chordeumatida (Tingupidae) record from Kodiak Island, Alaska, USA, and the lower one denotes the known and projected distribution of Chordeumatida (Eudigonidae) in Chile.

Figure 22 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 22. Distribution of the Order Siphonophorida; the dot in North America/USA (California) signifies the type and only known locality of Illacme plenipes Cook and Loomis, 1928 (Siphonorhinidae), the world's "leggiest" animal (Cook and Loomis 1928; Shelley 1996c, d; Marek and Bond 2006). The question mark represents the generalized record from Northern Territory, Australia (Black 1997), and the arrow denotes the locality of Siphonophoridae on Auckland Island, New Zealand (Johns 1964).

Figure 19-20. Distributions. 19 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 19-20. Distributions. 19) Distribution of Platydesmida in Europe, the Middle East, and North Africa. 20) Known (solid lines) and projected (dashed lines) distribution of the Order Polyzoniida, parameters as in Fig. 15.

Figure 32 in Atlas of Myriapod Biogeography. I. Indigenous Ordinal and Supra-Ordinal Distributions in the Diplopoda: Perspectives on Taxon Origins and Ages, and a Hypothesis on the Origin and Early Evolution of the Class

Figure 32. Known (solid lines) and projected (dashed lines) distributions of the Suborder Epinannolenidea. Parameters are as in Fig. 1, except the question marks in Australia represent general records from Northern Territory, South Australia, and northern Western Australia (Black 1997).