Stratigraphic formation of the Mekong River Delta and its recent shore change

Tên bài báo Stratigraphic formation of the Mekong River Delta and its recent shore change
Tác giả Liu, J.P., DeMaster, D.J, Nitrouer C.A., Eidam E.F., Thanh T. Nguyen, Saito, Y., Van Lap Nguyen, Thi Kim Oanh Ta, Li, X.,
Đơn vị thực hiện Phòng Địa lý tổng hợp
Phân loại Công bố ngoài nước
Tạp chí Oceanography
Mã tạp chí ISSN: 1042-8275


Where the Mekong River discharges into the East Sea (also known as the South China Sea), it has formed the world’s third largest delta plain with an area of ~50,000 km2. Numerous cores recovered from the subaerial delta reveal that it has prograded ~220 km southeastward within the past 7,500 years. Recent extensive seismic and geochemical surveys of the adjacent subaqueous delta indicate that the Mekong River forms a classic sigmoidal, cross-shelf clinoform immediately off its distributaries that is up to 15 m thick, with topset, foreset, and bottomset facies. These deposits are constrained within water depths of 20 m. Mekong-derived sediment packages extend ~300 km along shelf in the southwestward direction to the tip of the Ca Mau Peninsula, where they form a distal mud depocenter up to 22 m thick. These sediment packages can also be traced into the Gulf of Thailand to water depths of 25 m. The proximal and distal deposits cover ~11,000 kmof the shelf.

Historically, the Mekong Delta has prograded seaward at a mean rate of >30 m yr–1, or 7 km2 yr–1; however, study of the past 43 years of Landsat images indicates that the mode of sedimentation in the delta shifted starting in 2005. From 1973 to 2005, the Mekong Delta’s seaward shoreline growth decreased gradually from a mean of 7.8 m yr–1 to 2.8 m yr–1, and after 2005 it became negative, with a retreat rate of −1.4 m yr–1. The net deltaic land area gain has also been slowing, with the mean rate decreasing from 4.3 km2 yr–1 (1973–1979) to 1.0 km2 yr–1 (1995–2005), and then to −0.05 km2 yr–1 (2005–2015). Thus, in about 2005, the subaerial Mekong Delta transitioned from a constructive mode to an erosional (or destructive) mode. Furthermore, not only is the subaerial Mekong Delta land area gradually diminishing, but high-resolution CHIRP sonar profiling surveys off the east-central Ca Mau Peninsula reveal that this portion of the subaqueous delta is also eroding. With the construction of more dams, sand mining, delta subsidence, increasing storms, and sea level rise, the Mekong Delta will likely face more destructive changes, with erosion both of coastlines and underwater deposits.