High-frequency climatic oscillations recorded in a Holocene coral reef at Leizhou Peninsula,South China Sea

被引:9
作者
余克服
沈承德
钟晋梁
宋朝景
赵焕庭
赵建新
刘东生
陈特固
机构
关键词
coral reef; Holocene Hypsithermal; abrupt climate change; sea level; Leizhou events; South China Sea;
D O I
暂无
中图分类号
P732 [海洋气象学];
学科分类号
0706 ; 070601 ;
摘要
<正> A detailed study of the Goniopora reef profile at Dengloujiao, Xuwen County, Leizhou Peninsula, the northern coast of the South China Sea suggests that a series of high-frequency, large-amplitude and abrupt cold events occurred during the Holocene Hypsithermal, an unusual phenomenon termed "Leizhou Events" in this paper. This period (corresponding to 14C age of 6.2 -6.7 kaBP or calendar age of 6.7-7.2 kaBP), when the climatic conditions were ideal for coral reefs to develop, can be divided into at least nine stages. Each stage (or called a "climate optimum"), lasting about 20 to 50 a, was terminated by an abrupt cold nap and (or) a sea-level lowering event in winter, leading to widespread emergence and death of the Goniopora corals, and growth discontinuities on the coral surface. Such a cyclic process resulted in the creation of a >4m thick Goniopora reef flat. During this period, the crust subsided periodically but the sea level was rising.The reef profile provides valuable archives for the study of d
引用
收藏
页码:1057 / 1067
页数:11
相关论文
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)
[4]   华南沿海地区验潮站资料反映的海平面变化与海岸升降 [J].
徐起浩 ;
丁丽青 ;
酆晓 .
华南地震, 2000, (03) :52-56
[5]   雷琼海区近40年海温变化趋势 [J].
余克服 .
热带地理, 2000, (02) :111-115
[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)