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33 results for “Tectonic history”
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.
Data from: Diversity dynamics of mammals in relation to tectonic and climatic history: comparison of three Neogene records from North America
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Data from: Detecting diversification rates in relation to preservation and tectonic history from simulated fossil records
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Data from: Tectonic evolution of the Tethyan region created the Eurasian extratropical biodiversity hotspots: tracing Pireneitega spiders' diversification history
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Fig. 5 in Tectonic history and the biogeography of the freshwater fishes from the coastal drainages of eastern Brazil: an example of faunal evolution associated with a divergent continental margin
Fig. 5. Schematic diagram of origin and erosional SE-NW retreat of Serra do Mar coastal range in region between inland Paraná basin, and the Santos basin, coast of SE Brazil. 1- Eroded Senonian uplift, allowing deposition in both Santos and Paraná basins. Alkaline volcanism (A); Santos Fault (F). 2- Development of the Japi Erosional Surface at the end of Senonian. 3- Paleocene deformation of the Japi Surface (isostatic adjustment). Serra do Mar (SM) is generated at Santos Fault (F), system of continental rifts originated and continental platform formed in coast (P). 4- Erosional retreat (R) of Serra do Mar toward present position. The approximate position of Depressão Periférica is indicated (DP). Alkaline intrusions represent islands. Conventions: 1. Santos formation deposits, 2. Phanerozoic cover beneath the Serra Geral basalt, 3. Serra Geral Formation, 4. Alkaline bodies, 5. Bauru Group, 6. Faults (fromAlmeida & Carneiro, 1998).
Fig. 1 in Tectonic history and the biogeography of the freshwater fishes from the coastal drainages of eastern Brazil: an example of faunal evolution associated with a divergent continental margin
Fig. 1. Crustal provinces of South America. I – South American Platform; II – Patagonian massif; III – Andean orogenic belt; IV – foreland basins; AM = Amazon craton; SL = São Luis craton; SF = São Francisco craton; LA = Luiz Alves craton; RP = Rio de la Plata craton; B = Borborema province; T = Tocantins province; M = Mantiqueira province; DF = Dom Feliciano belt. (Modified from Cordani et al., 2000 and Cordani & Sato, 1999).
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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International Brain Laboratory public data
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OpenNeuro
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