Author(s): Liu J, Rong X, Zhong C, Muhong C, Wen Y, et al.
Sediment sources, transport and deposition in the South China Sea (SCS) are addressed based on multiple proxies of 111 surface sediment samples, including clay minerals and rare earth elements. Results reveal that sediment sources in the SCS generally contain volcanic, biogenic and terrigenous materials. Volcanic material is typically distributed west of Luzon Island (including adjacent to Huangyan Island). Carbonate biogenic materials (e.g., coral and foraminifera) develop strongly around the Nansha and Xisha Islands. Terrigenous materials mainly derive from the continent via large rivers (e.g., the Pearl, Red and Mekong Rivers) and from islands via mountainous rivers (e.g. the Gaoping River in Southwest Taiwan and Rajang River in northern Kalimantan).
Author(s): Anderson RF, Lehuray AP, Fleisher MQ, Mur ray JW
Author(s): Saulnier I, Mucci A
Author(s): Dawood YH
Author(s): Chung Y, Chang WC
Author(s): Cuculić V, Neven C, Delko B, Marina M
Author(s): SalahelDin K, Vesterbacka P
Author(s): Och LM, Müller B, Christian M, Adrian W, Vologina EG, et al.
Author(s): Zheng Y, Anderson RF, Alexander VG, Fleisher MQ
Author(s): McManus J, William MB, Klinkhammer GP, Hammond DE, Holm C
Author(s): Sani RK, Peyton BM, Amonette JE, Geesey GG
Author(s): Shumilin E, Griselda R, Guez-Figueroa Sapozhnikov D, Sapozhnikov Y, Choumiline K
Author(s): Mohamed CAR, Mohamed KN, Ahmad Z
Author(s): Srisuksawad K, Porntepkasemsan B, Nouchpramool S, Yamkate P, Carpenter R, et al.
Author(s): Lozano JCP, Blanco R, Vera TF
Author(s): Zulkifli SZ, Ismail A, Yusuff FM, Arai T, Miyazaki N
Author(s): Azman AG
Author(s): Tessier AP, Campbell GC, Bisson M
Author(s): Yamada M, Zhong-liang W, Yoshihisa K
Author(s): Loeff MMR
Author(s): Roy-Barman M, Jeandel C, Souhaut M, Loeff MRVD, Voege I, et al.
Author(s): Carpenter R Peterson ML, Bennett JT, Somayajulu BLK
Author(s): Robinson L, Noble T, Mcmanus J
Author(s): Maity S, Sahu SK, Pandit GG
Author(s): Okubo A, Obata H, Gamo T