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17 results for “Palaeosetidae”
FIGURE 6 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 6. Fragmentation of the northern Melanesian Arc over the last 13 Ma; dark shading, present day islands, intermediate shading, former Samoan islands (now as seamounts), pale shading, <2000 m depth. Modified from Schellart (2002a, b).
FIGURE 1 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 1. Exoporia: (a) Mnesarchaea acuta (photo by George Gibbs©); (b) Aenetus cohici (photo by Thierry Salesne©); (c) Abantiades labyrinthicus (photo by Kees Green©); (d) Oxycanus gelidus (photo by Ethan Beaver©); (e) Cladoxycanus minos (photo by Steve Kerr©); (f) Aoraia rufivena (photo by Rod Morris/rodmorris.co.nz©); (g) Elhamma australasiae (photo by John Nielsen©); (h) Wiseana signata (photo by Phil Bendle©); (i) Phassodes vitiensis (photo by Kirk Williams©); (j) Fraus crocea (photo by David Fischer©).
FIGURE 56 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 56. Northern North America: (a) Gazoryctra species (each color coded), (b) Sthenopis species (each color coded), (c) Phymatopus, (d) Korscheltellus gracilis (see http://mothphotographersgroup.msstate.edu/ for identification of individual species). Regions of high topographic relief shaded, predominantly marine regions unshaded.
FIGURES 40–51 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURES 40–51. Tectonic correlations of Australian Exoporia. Fig. 40: Zelotypia stacyi; Fig. 41: Aenetus ramsayi; Fig. 42: Oncopera filiform antenna group comprising O. parva, O. mitocera, O. brachyphylla (solid line), O. brunneata/alboguttata (shaded), O. epargyra (solid star), and O. tindalei (open square); Fig. 43: Aenetus thermistis; Fig. 44: Aenetus mirabilis; Fig. 45: Palaeoses scolastica (shaded area) and Anomoses hylecoetes (pale circle at MMO); Fig. 46: Aenetus scotti (pale shading) and sister species A. edwardsi (dark shading); Fig. 47: Abantiades leucochiton (dark shading) and sister species Abantiades n.sp (pale shading); Fig. 48: Abantiades marcidus; Fig. 49: Elhamma australasiae (pale shading) and disjunct sister group in New Guinea (dark shading); Fig. 50: Fraus polyspila clade comprising F. polyspila (pale shading), F. griseomaculata (intermediate shading), F. pelagia (dark shading); Fig. 51: Fraus crocea (pale circles) and partially sympatric sister species F. fusca (dark circles). McPherson-Macleay Overlap (MMO, arrowed); Otway-Bass-Gippsland Basin system (OBGB); Whitsunday Volcanic Province (WVP). Distribution data from Common (1990) and Simonsen (2015, 2018).
FIGURES 9–10. Fig. 9 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURES 9–10. Fig. 9. Distribution of oxycanine groups: Neohepialiscus (North Africa), Hepialiscus (Himalaya-southern Asia), Napialus (China), Oxycanus (New Guinea-Australia), and New Zealand oxycanine genera. Fig. 10. Known and potential distribution of Phassodes.
FIGURE 3 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 3. Global distribution range of Exoporia families: Hepialidae (dotted outline), Mnesarchaeidae (solid outline), Palaeosetidae (stars), Neotheoridae (circles), Prototheoridae (shaded), and Anomosetidae (open star in northeastern Australia).
FIGURE 5 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 5. Southwest Pacific tectonics: Sequence of four principal time periods: large arrows, direction of expansion; pointed lines, subduction zones (dark lines active, pale lines deactivated); LHR, Lord Howe Ridge; NC, New Caledonia Ridge; dark shaded areas, magmatic plateaus; unshaded areas, oceanic seafloor (modified from Heads 2017: fig. 3.15). EMF, Emerald Fracture Zone; APF, Alpine Fault.
FIGURE 8 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 8. Distribution of Aenetus: (a) distribution range (not including Sumatra outlier); (b) northwestern distribution boundary of Aenetus (yellow circles) and southeastern boundary of Endoclita (purple circles); allopatry of Endoclita and Aenetus (not including Sumatra outlier for Aenetus),? denotes region without any records of Hepialidae.
FIGURE 7 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 7. Hypothetical vicariance origin of Mnesarchaeidae: (a) widespread ancestor over East Gondwana in heavy stippling; vicariance mediated by tectonic disruption (such as the large silicic province in red) resulting in isolation and differentiation of Mnesarchaeidae (horizontal wavy lines) with a small distribution range to the east, and Hepialoidea (light stipple) with a large, almost global, distribution range to the west; (c) subsequent range expansion by Hepialoidea resulting in sympatry with Mnesarchaeidae. Tectonic outline from Strogen et al. (2017).
FIGURES 52–53 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURES 52–53. Tectonic correlations of Australian Exoporia. Fig. 52. Oncopera clavate group species: O. intricata (Tasmania), O. fasciculatus/intracatoides (dark circles), O. alpina (dark squares), O. commoni (pale square); Fig. 53. Fraus nanus (pale shading) and sister species F. furcata (dark shading). Tectonic structures: McPherson-Macleay Overlap (MMO, arrowed); Otway-Bass-Gippsland Basin system (OBGB); Whitsunday Volcanic Province (WVP). Distribution data from Simonsen (2018).
FIGURES 28–39 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURES 28–39. Tectonic correlations of New Zealand and Australian Exoporia. Fig. 28. Aoraia aspina; Fig. 29. Fraus pteromela; Fig. 30. Fraus simulans; Fig. 31: Abantiades hyalinatus; Fig. 32: Oncopera rufrobrunnea; Fig. 33: Abantiades magnificus; Fig. 34: Abantiades barcas; Fig. 35: Aenetus ligniveren clade (pale shading) including undescribed species (star) and A. astathes (dark shading); Fig. 36: Aenetus eximia; Fig. 37: Abantiades aphenges (pale shading) and sister species A. fulvomaculatus (dark shading); Fig. 38: Fraus linogyna; Fig. 39: Aenetus montanus and sister species A. ombraloma. Tectonic structures: McPherson-Macleay Overlap (MMO, arrowed); Otway-Bass-Gippsland Basin system (OBGB); Whitsunday Volcanic Province (WVP). Distribution data from Kristensen & Nielsen (1989), Kallies et al. (2015) and Simonsen (2018).
FIGURE 54 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 54. Cartoon illustrating the concept of distributional stability over time: (a) Distribution boundary of ghost moths at a Mesozoic rift valley; (b) Cenozoic distribution boundary of ghost moth species at the fault zone remnants of failed rift valley. Half arrows – direction of uplift or subsidence, whole arrows – direction of expansion or compression.
FIGURES 20–27 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURES 20–27.Tectonic correlations of New Zealand Exoporia. Fig. 20: Dumbletonius (a) D. characterifer (dark shading) west of fault except at Torlesse Node (star) and sister species D. unimaculatus (pale shading) sympatric in south-central North Island, (b) hypothesized ancestral allopatry; Fig. 21: Wiseana signata with possibly disjunct coastal Kaikoura population east of the fault (cf. Mnesarchaea acuta, Fig. 12); Fig. 22. Aoraia aurimaculata; Fig. 23. Aoraia dinodes (pale shading), Aoraia hespera (solid square), Aoraia insularis (dark shading); Fig. 24. Wiseana mimica (intermediate shading) and sister species Wiseana fuliginea (pale shading) with area of sympatry (dark shading); Fig. 25 Heloxycanus patricki; Fig. 26. Aoraia rufivena (pale shading) and A. lenis (dark shading); Fig. 27: Aoraia orientalis (dark shading), Aoraia senex (pale shading), and Aoraia oreobolae (solid square). WEP, West-East Province boundary; WFZ, Waitaki Fault Zone; ETWS, Earnslaw-Taieri-Wakatipu synform; MTZ, Moonlight Tectonic Zone. Distribution data from Dugdale (1994).
FIGURES 11–19 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURES 11–19. Tectonic correlations of New Zealand Exoporia. Fig. 11: Mnesarchaea fallax clade (species in cladogram) and Fiordland endemic Mnesarchaea species "g"; Fig. 12: Mnesarchaea acuta (circles) and undescribed sister species "c" (squares); Fig. 13: Mnesarchaea loxoscia; Fig. 14: Wiseana copularis; Fig. 15: Aoraia enysii; Fig. 16: Dioxycanus fusca (dark shading) and sister species D. oreas (light shading); Fig. 17: Cladoxycanus minos; Fig.18: Wiseana jocosa; Fig. 19: Wiseana cervinata. Alpine Fault, thick solid line; arrows indicate direction of movement; WEP, West-East Province boundary; WFZ, Waitaki Fault Zone; WHFZ Waihemo Fault Zone. Distribution data from Dugdale (1994) for Hepialidae, and Gibbs (1990) and G.W. Gibbs (pers. comm.) for Mnesarchaea.
FIGURE 4 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 4. Tectonic and geological structure of East Gondwana prior to Late Cretaceous formation of the Tasman basin that separated New Zealand and New Caledonia from Australia. Outline of New Zealand shown in position prior to Alpine Fault movement. Large silicic province, red shaded band (dotted outline as probable position on the seafloor); dark shading, regions of present day land; pale shading, continental area; blue lines, zones of Late Cretaceous rifting.
FIGURE 2 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 2. Phylogeny of the exoporian families (from Simonsen 2017).
FIGURE 55 in Evolutionary biogeography and tectonic history of the ghost moth families Hepialidae, Mnesarchaeidae, and Palaeosetidae in the Southwest Pacific (Lepidoptera: Exoporia)
FIGURE 55. Correlated Cretaceous geography and exoporian distribution. Southern Africa: (a) present day range of Exoporia; (b) present day range mapped onto Cretaceous geography (adapted from de Witt (2007). Distribution data from Janse (1942), Nielsen & Scoble (1986), Davis (1996, 2001), Landry & Davis (2018).
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