000K  utf8
1100  $c2022
1500  eng
2050  urn:nbn:de:gbv:8:3-2022-00598-3
2051  10.3390/coasts2030011
3000  Le, Thuyen Xuan
3010  Bui, Luan Thi
3010  Nguyen, Thanh Cong
3010  Schwarzer, Klaus
3010  Unverricht, Daniel
4000  Late Holocene Morphodynamic Feedback in Can Gio Mangrove Tide-Dominated River Mouth Systems, Vietnam  [Le, Thuyen Xuan]
4209  Can Gio (CG), a mangrove forest with a dense network of tidal creeks, gradually grew and spread seaward on a coastal platform, which was built since about 8 ka before present (BP). Along with this development, a sand ridge began to form and moved back with the shoreline withdrawal landward in the Late Holocene. This mangrove environment is likely abandoned from the mainland but was, however, the place for settlement of ancient Vietnamese a few centuries BC. The CG mangrove forest was severely destroyed during the American War and was restored since 1980. However, the historical change of the landscape along the Saigon-Dong Nai River (SG-DNR) since the Late Holocene is not completely unraveled. By analyzing sediment cores with a multiproxy approach, we investigated the recent geological development with regard to the variation of the intensity of the East Asian palaeomonsoon and regarding the accommodation space, as both regulate the development of this coastal environment. A recently significant shift in the coastline, mainly due to a change of hydroclimatic factors, was observed. A continuous coastline retreat occurred over the last millennium, changing the depositional environment and reshaping the CG mangrove landscape. Along the present coast and tidal channels, partially strong erosion and bank failures occur, alternating with accretion at other coastal sections. This development tends to increase progressively
4950  https://doi.org/10.3390/coasts2030011$xR$3Volltext$534
4950  https://nbn-resolving.org/urn:nbn:de:gbv:8:3-2022-00598-3$xR$3Volltext$534
4961  https://macau.uni-kiel.de/receive/macau_mods_00003027
5051  550
5550  back barrier development
5550  Can Gio mangroves
5550  coastal morphodynamics
5550  mangrove coast evolution
5550  pre-Oc Eo culture
5550  sand ridge