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- W3022835125 abstract "Of the existing continents, Asia experienced the most significant deformation during the Cenozoic. From the Cretaceous to early Paleogene, Asia was smaller and “slimmer” compared with the present continent. After the India-Asia collision in the Eocene, Asia significantly enlarged its size and increased its altitude. The west-tilting topography of East Asia was reversed with the uplift of the Tibetan plateau and the opening of marginal seas, resulting in an Asian fluvial system radiating from the uplifted center of the continent. Plateau uplift may have promoted the establishment and growth of the Arctic ice-sheet not only by the alteration of atmospheric circulation and enhancement of weathering, but also by the formation of north-flowing Siberian rivers, which provided the Arctic Ocean with freshwater run-off. The Cenozoic deformation of Asia was also responsible for the initiation of the Asian monsoon system during the early Miocene and its further strengthening at ～8 Ma and ～3 Ma. The formation of a series of seas fringing the East Asian margin has changed the material and energy flux between the Asian continent and Pacific Ocean. The western Pacific boundary currents flowing through the marginal seas are highly sensitive to eustatic and tectonic changes. During low sea-level stands caused by glaciation, the boundary currents flowed outside the marginal seas and reduced the heat and humidity supply from the ocean to the continent. Today, the most active energy and material fluxes in the Earth System occur between Asia and the Pacific, yet the role of Asia in controlling global climatic and environmental history has been underestimated." @default.
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- W3022835125 date "2005-01-01" @default.
- W3022835125 modified "2023-09-26" @default.
- W3022835125 title "Cenozoic Deformation and History of Sea-Land Interactions in Asia" @default.
- W3022835125 hasPublicationYear "2005" @default.
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