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68 results for “myriapods”
Figure 1 in Terrestrial isopods and myriapods in a forested scree slope: subterranean biodiversity, depth gradient and annual dynamics
Figure 1. Distribution of Isopoda, Diplopoda and Chilopoda along the depth gradient of the scree slope expressed as the total number of individuals trapped in two sampling periods (November 2008–November 2009; November 2009–July 2010).
Predators of Japanese myriapods — survey using literature, social media, Web, and mobile application —
<p>I provide a database reviewing information on predators of Japanese myriapods. The information within this database was compiled from published accounts in Japan along with visual media accumulated on the Internet.</p>
Linked collectors and determiners for: Field Museum of Natural History (Zoology) Insect, Arachnid and Myriapod Collection.
Natural history specimen data linked to collectors and determiners held within, "Field Museum of Natural History (Zoology) Insect, Arachnid and Myriapod Collection". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/7931dcab-94f1-46ce-8092-56e4335423de">https://bionomia.net/dataset/7931dcab-94f1-46ce-8092-56e4335423de</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/7931dcab-94f1-46ce-8092-56e4335423de">https://gbif.org/dataset/7931dcab-94f1-46ce-8092-56e4335423de</a>. Formatted as a Frictionless Data package.
FIG. 2 in Les myriapodes chilopodes (Chilopoda) du Parc national du Mercantour, du département des Alpes-Maritimes et de leurs environs: description d'une nouvelle espèce du genre Lithobius Leach, 1814 s.s., synthèse des connaissances et espèces menacées
FIG. 2. — Lithobius (Lithobius) lemairei n. sp. (holotype femelle, 8 mm de long, d'Entrevaux). A, tête, vue latérale; B, bord rostral du coxosternum forcipulaire, vue ventrale; C, moitié postérieure du corps, vue dorsale; D, patte 15 droite, vue ventrale (pores glandulaires non représentés); E, gonopodes, vue ventrale. Échelles: A, D: 0,2 mm; B, E: 0,1 mm; C: 0,5 mm.
FIG. 1 in Les myriapodes chilopodes (Chilopoda) du Parc national du Mercantour, du département des Alpes-Maritimes et de leurs environs: description d'une nouvelle espèce du genre Lithobius Leach, 1814 s.s., synthèse des connaissances et espèces menacées
FIG. 1. — Lithobius (Lithobius) lemairei n. sp. (holotype femelle, 8 mm de long, d'Entrevaux): A, habitus, vue dorsale; B, tête et premiers segments pédifères, vue ventrale; C, derniers segments pédifères et segments gonopodiaux, vue ventrale; D, patte 14 gauche, vue ventrale. Échelles: A-C, 0,5 mm; D, 0,2 mm.
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).
Figure 53 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 53. Land areas in the Mid-Cambrian Period, Paleozoic Era, adapted from the website of Ron Blakey, Geology Dept., Northern Arizona University, Flagstaff, Arizona, USA (http://jan.ucc.nau.edu/~ rcb7/RCB.html), symbols as in Fig. 52. The bold arrow represents emergence of the original ancestor from the Iapetus Ocean onto the Avalonia terrane that is still attached to Gondwana I around 524 ma, and the short, lighter arrows show initial dispersions through Avalonia and onto Gondwana I proper; at this time, other land masses and the rest of Gondwana I were devoid of diplopods. A, Avalonia terrane; Af, "proto-Africa" region of Gondwana I; B, Baltica; GI, Gondwana I; K, Kazakhstania; L, Laurentia; S, Siberia; SA, "proto-South America" region of Gondwana I.
Figure 30 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 30. Distribution of the Suborder Cambalidea. Asterisk, location of Protosilvestria sculpta, the Oligocene fossil from Quercy, France (Mauriès 1992).
Figure 23-25. Distributions. 23 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 23-25. Distributions. 23) Distribution of the "minor" orders. Star/Circled Areas, Siphonocryptida (Colobognatha); Dots, Siphoniulida (Helminthomorpha incertae sedis). 24) Known (solid lines) and projected (dashed lines) distributions of the Subterclass Eugnatha showing the locations of significant fossils. The arrow points to the Kodiak Island, Alaska, USA, record of Chordeumatida (Tingupidae). Inverted triangle, approximate location of Gobiulus sabulosus Dzik, 1975, the Cretaceous spirobolidan fossil from Mongolia; Asterisk, location of Protosilvestria sculpta, the Oligocene cambalidean fossil in Quercy, France (Mauriès 1992). 25) Known (solid lines) and projected (dashed lines) distributions of the Superorder Juliformia showing the locations of significant fossils. Parameters as in Fig. 1 except no records or samples are available from the dotted area in North America, the Great Basin Physiographic Province, western USA. Inverted triangle, approximate location of Gobiulus sabulosus Dzik, 1975, the Cretaceous spirobolidan fossil from Mongolia; Asterisk, location of Protosilvestria sculpta, the Oligocene cambalidean fossil in Quercy, France (Mauriès 1992). The question mark indicates the generalized record of Epinannolenidea from Northern Territory, Australia (Black 1997).
Figure 14-15. Distributions. 14 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 14-15. Distributions. 14) Known (solid lines) and projected (dashed lines) distributions of the Infraclass Helminthomorpha showing the locations of significant fossils, parameters as in Fig. 1. It differs from that of the Subclass Chilognatha (Fig. 5) in the imperceptibly shorter length along the southern coast of Western Australia, the only place where Pentazonia have been taken without helminthomorphs. Upright triangle, site of Archidesmus macnioli Peach, 1887, the oldest fossil, from Silurian deposits in Scotland; Inverted triangle, approximate location of Gobiulus sabulosus Dzik, 1975, the Cretaceous spirobolidan fossil from Mongolia; Asterisk, location of Protosilvestria sculpta, the Oligocene cambalidean fossil in Quercy, France (Mauriès 1992). 15) Known (solid lines) and projected (dashed lines) distribution of the Subterclass Colobognatha. The question marks in Australia represent generalized records from Northern Territory, South Australia, and "Upper Western Australia" by Black (1997). Some point localities probably represent the ubiquitous, introduced polyzoniidan (Siphonotidae), Rhinotus purpureus (Pocock, 1894).
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