SCSIO OpenIR  > 热带海洋环境国家重点实验室(LTO)
Storm cycles in the last millennium recorded in Yongshu Reef, southern South China Sea
Yu, KF; Zhao, JX; Collerson, KD; Shi, Q; Chen, TG; Wang, PX; Liu, TS; kyu@earth.uq.edu.au; j.zhao@uq.edu.au; k.collerson@uq.edu.au; shiqi@scsio.ac.cn; kefuyu@scsio.ac.cn; pxwang@online.sh.cn; tsliu@public.bta.net.cn
2004
Source PublicationPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
Volume210Issue:1Pages:89-100
AbstractLarge storm-relocated Porites coral blocks are widespread on the reef flats of Nansha area, southern South China Sea. Detailed investigations of coral reef ecology, geomorphology and sedimentation on Yongshu Reef indicate that such storm-relocated blocks originated from large Porites lutea corals growing on the spurs within the reef-front living coral zone. Because the coral reef has experienced sustained subsidence and reef development during the Holocene, dead corals were continuously covered by newly growing coral colonies. For this reason, the coral blocks must have been relocated by storms from the living sites and therefore the ages of these storm-relocated corals should approximate the times when the storms occurred. Rapid emplacement of these blocks is also evidenced by the lack of coral overgrowth, encrustation or subtidal alteration. U-series dating of the storm-relocated blocks as well as of in situ reef flat corals suggests that, during the last 1000 years, at least six strong storms occurred in 1064 +/- 30, 1210 +/- 5-1201 +/- 4, 1336 +/- 9, 1443 +/- 9, 1685 +/- 8-1680 +/- 6, 1872 +/- 15 AD, respectively, with an average 160-year cycle (110-240 years). The last storm, which occurred in 1872 15 AD, also led to mortality of the reef flat corals dated at similar to 130 years ago. Thus, the storm had significant impacts on coral reef ecology and morphology. (C) 2004 Elsevier B.V. All rights reserved.
DepartmentChinese Acad Sci, S China Sea Inst Oceanol, Guangzhou 510301, Peoples R China; Univ Queensland, Adv Ctr Queensland Univ Isotope Res Excellence, Brisbane, Qld 4072, Australia; Tongji Univ, Lab Marine Ecol, Shanghai 200092, Peoples R China; Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
KeywordStorm Coral Reef U-series Dating Late Holocene South China Sea
Subject AreaGeography, Physical ; Geosciences, Multidisciplinary ; Paleontology
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Indexed Bysci
Funding ProjectLED
WOS IDWOS:000222857100004
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Document Type期刊论文
Identifierhttp://ir.scsio.ac.cn/handle/344004/5623
Collection热带海洋环境国家重点实验室(LTO)
Corresponding Authorkyu@earth.uq.edu.au; j.zhao@uq.edu.au; k.collerson@uq.edu.au; shiqi@scsio.ac.cn; kefuyu@scsio.ac.cn; pxwang@online.sh.cn; tsliu@public.bta.net.cn
Recommended Citation
GB/T 7714
Yu, KF,Zhao, JX,Collerson, KD,et al. Storm cycles in the last millennium recorded in Yongshu Reef, southern South China Sea[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2004,210(1):89-100.
APA Yu, KF.,Zhao, JX.,Collerson, KD.,Shi, Q.,Chen, TG.,...&tsliu@public.bta.net.cn.(2004).Storm cycles in the last millennium recorded in Yongshu Reef, southern South China Sea.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,210(1),89-100.
MLA Yu, KF,et al."Storm cycles in the last millennium recorded in Yongshu Reef, southern South China Sea".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 210.1(2004):89-100.
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