Oniscomorpha
publication ID |
https://doi.org/ 10.5281/zenodo.5164069 |
persistent identifier |
https://treatment.plazi.org/id/350B6716-0D2D-FFD3-FF71-FC57FD09F9D8 |
treatment provided by |
Felipe |
scientific name |
Oniscomorpha |
status |
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Superorder Oniscomorpha View in CoL ( Fig. 8 View Figure 7-9 )
Oniscomorpha occupy ten areas on all continents except South America, with a questionable sphaerotheriidan record from the Bismarck Archipelago, Papua New Guinea (Attens 1943). They traverse the Equator and both Tropics, and terminate in southern Scandinavia well south of the Arctic Circle. The detached Libyan site is near Benghazi, east of the Gulf of Sidra.
Areas in the New World, Europe/north Africa, and central Asia attribute solely to Glomerida as may the Paleozoic/Carboniferous fossil from Illinois, USA ( Fig. 8-9 View Figure 7-9 , star); those in southern Africa/ Madagascar /Indian Ocean, Australia / New Zealand, and India / Sri Lanka represent Sphaerotheriida ; and that in east/southeastern Asia represents both orders, which are sympatric and highly congruent here (compare Fig. 9 View Figure 7-9 and 13). Both encompass the Indochina and Malay peninsulas, Thailand, Myanmar, Indonesia from Sulawesi westward, and the Philippines. Both also exhibit a narrow dactyliform extension that runs westward through eastern India, Bhutan, and the eastern half of Nepal. Sphaerotheriida ranges farther eastward in Indonesia, around Halmahera, and Glomerida spread substantially farther north, encircling Taiwan, coastal China to the Shangdong Peninsula, most of the Korean Peninsula, and the Ryukyu Islands and “mainland” Japan northward to central Honshu. The northernmost sphaerotheriidan locality is Fuzhou, Fujian Prov., China, ~ 1,080 km (675 mi) south of the northernmost glomeridan, but Sphaerotheriida extend farther inland.
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