Wuchiapingian
English
editAlternative forms
editEtymology
editFrom the Wade–Giles romanization of Mandarin 吳家坪/吴家坪 (Wújiāpíng, literally “Wu Family Flatland”) in Shaanxi Province in China: Wu2-chia1-pʻing2.
Proper noun
editWuchiapingian
- (geology, paleontology) A subdivision of the Permian period.
- 2022 January 11, Li Yuan, “Investigating benthic marine redox conditions from late Permian to earliest Triassic”, in Phys.org[1], archived from the original on 11 January 2022, Earth Sciences[2]:
- Anoxic/euxinic benthic marine conditions prevailed throughout the middle Wuchiapingian to the early Changhsingian at Shangsi, which persisted for 3.9 Myr (256.974–253.073 Ma). This long-term middle Wuchiapingian-early Changhsingian anoxia event could be correlated both regionally and globally, and was caused by paleogeographic restrictions, relative high sea levels, high marine productivities, and possible global climate changes.
Translations
editA subdivision of the Permian period.
|