共 21 条
[1]
Timing of Holocene sea-level highstands by mass spectro-metric U-series ages of a coral reef from Leizhou Peninsula, South China Sea[J]. ZHAO Jianxin & YU KefuDepartment of Earth Sciences, University of Queensland, Brisbane, Qld 4072, Australia (e-mail: j.zhao@earth.uq.edu.au);South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 501301, China (e-mail: kefuyu@scsi.Chinese Science Bulletin. 2002(04)
[2]
The high-resolution climate recorded in the δ18O of Porites lutea from the Nansha Islands of China[J]. YU Kefu, CHEN Tegu, HUANG Dingcheng, ZHAO Huanting, ZHONG Jinliang & LIU Dongsheng (LIU Tungsheng)South China Sea Institute of Oceanoiogy, Chinese Academy of Sciences. Guangzhou 510301, China:Geology and Geophysics Institute. Chinese Academy of Sciences, Beijing 100029, China.Chinese Science Bulletin. 2001(24)
[3]
A prediction of sea level rising amplitude in 2030 and defensive countermeasures in the Zhujiang delta[J]. 黄镇国 ,张伟强 ,吴厚水 ,陈特固 ,范锦春 ,江沛霖 ,黎子浩 ,黄本胜.Science in China(Series D:Earth Sciences). 2001(05)
[6]
Evidence for solar forcing of climate variation from δ18O of peat cellulose[J]. 洪业汤,刘东生,姜洪波,周立平,洪冰,朱泳煊,李汉鼎,冷雪天,秦小光,王羽,林庆华,曾毅强.Science in China(Series D:Earth Sciences). 2000(02)
[7]
Abrupt climatic changes on the Tibetan Plateau during the Last Ice Age——Comparative study of the Guliya ice core with the Greenland GRIP ice core[J]. 姚檀栋.Science in China(Series D:Earth Sciences). 1999(04)
[8]
Relationship between coral growth rate and sea surface temperature in the northern part of South China Sea during the past 100 a[J]. 聂宝符,陈特固,梁美桃,王有强,钟晋梁,朱袁智.Science in China(Series D:Earth Sciences). 1997(02)
[9]
Late Holocene cooling event in the western Pacific[J]. 翦知湣,李保华,UwePflaumann,汪品先.Science in China,Ser.D. 1996(05)
[10]
The Climatic Fluctuation and Important Events of Holocene Megathermal in China[J]. 施雅风,孔昭宸,王苏民,唐领余,王富葆,姚檀栋,赵希涛,张丕远,施少华.Science in China,Ser.B. 1994(03)