SONG Shao-hua, ZHOU Wei-jian, PENG Zi-cheng, LIU Wei-guo, CHENG Peng, XIAN Feng. RESPONSE TO ENVIRONMENTAL CONDITIONS OF CORAL δ18O OF PORITES LUTEA FROM SHALAO,HAINAN ISLAND[J]. Marine Geology & Quaternary Geology, 2006, 26(4): 23-28.
Citation: SONG Shao-hua, ZHOU Wei-jian, PENG Zi-cheng, LIU Wei-guo, CHENG Peng, XIAN Feng. RESPONSE TO ENVIRONMENTAL CONDITIONS OF CORAL δ18O OF PORITES LUTEA FROM SHALAO,HAINAN ISLAND[J]. Marine Geology & Quaternary Geology, 2006, 26(4): 23-28.

RESPONSE TO ENVIRONMENTAL CONDITIONS OF CORAL δ18O OF PORITES LUTEA FROM SHALAO,HAINAN ISLAND

More Information
  • Received Date: October 19, 2005
  • Revised Date: February 15, 2006
  • Based on the determination of the oxygen isotopic analysis of the skeleton of living Porites lutea in Shalao fringing reef, Hainan Island, we obtained a coral δ18O record for an 11 year period(1992-2002). We have assessed the characteristics of coral δ18O signals responding to environmental conditions by comparing coral δ18O variation with a local record of sea surface temperature (SST) and sea surface salinity (SSS), respectively. We conclude from our comparison that the annual variation of δ18O is controlled by SST, whereas the seasonal variation of it by SSS.
  • [1]
    梁必骐. 南海热带大气环流系统[M]. 北京:气象出版社, 1991:1-43.[LIANG Bi-qi. System of tropic atmospheric circulation in South China Sea[M]. Beijing:Meteorology Press, 1991:1

    -43.]
    [2]
    Wang P X. Response of Western Pacific marginal seas to glacial cycles:paleoceanographic and sedimentological features[J]. Marine Geology, 1999, 156:5-39.
    [3]
    Gagan M K, Ayliffe L, Beck J W, et al. New views of tropical paleoclimates from corals[J]. Quaternary Science Reviews, 2000, 19:45-64.
    [4]
    Felis T, Pätzold J, Loya Y, et al. A coral oxygen isotope record from the northern Red Sea documenting NAO, and North Pacific teleconnections on Middle East climate variability since the year 1750[J]. Paleoceanography, 2000, 15(6):679-694.
    [5]
    Cole J E, Fairbanks R G, Shen G T. Recent variability in the Southern Oscillation:isotopic results from a Tarawa Atoll coral[J]. Science, 1993, 260:1790-1793.
    [6]
    Dunbar R B, Wellington G M, Colgan M W, et al. Eastern Pacific sea surface temperature since 1600 AD:the δ18O record of climate variability in Galápagos corals[J]. Coral Reefs, 1994, 9:291-315.
    [7]
    Charles C D, Hunter D E, Fairbanks R G. Interaction between the ENSO and the Asian monsoon in a coral record of tropical climate[J]. Science, 1997, 277:925-928.
    [8]
    Quinn T M, Taylor F W, Crowley T J, et al. Evaluation of sampling resolution in coral stable isotope records:a case study using records from New Caledonia and Tarawa[J]. Paleoceanography, 1996, 11(5):529-542.
    [9]
    Kuhnert H, Pätzold J, Hatcher B, et al. A 200-year coral stable oxygen isotope record from a high-latitude reef off Western Australia[J]. Coral Reefs, 1999, 18:1-12.
    [10]
    Cole J E, Dunbar R B, McMlanahan T R,et al. Tropical Pacific forcing of decadal SST variability in the western Indian ocean over the past two centuries[J]. Science, 2000, 287:617-619.
    [11]
    Cobb K M, Charles C D, Cheng H, et al. El Niño/Southern Oscillation and tropical Pacific climate during the last millennium[J]. Nature, 2003, 424:271-276.
    [12]
    Charles C D, Cobb K, Moore M D, et al. Monsoon-tropical ocean interaction in a network of coral records spanning the 20th century[J]. Marine Geology, 2003, 201:207-222.
    [13]
    Le Bec N, Juillet-Leclerc A, Corrège T, et al. A coral δ18O record of ENSO driven sea surface salinity variability in Fiji (south-western tropical Pacific)[J]. Geophysical Research Letters, 2000, 27:3897-3900.
    [14]
    Pfeiffer M, Dullo W-C, Eisenhauer A. Variability of the intertropical convergence zone recorded in coral isotopic records from the central Indian Ocean (Chagos Archipelago)[J]. Quaternary Research, 2004, 61:245-255.
    [15]
    Linsely B K, Dunbar R B, Wellington G M, et al. A coral-based reconstruction of Intertropical Convergence Zone variability over Central America since 1707[J]. Journal of Geophysical Research, 1994, 99:9977-9994.
    [16]
    Dunbar R B, Wellington G M. Stable isotopes in a branching coral monitor seasonal temperature variation[J]. Nature, 1981, 293:453-455.
    [17]
    Watanabe T, Gagan M K, Corrége T, et al. Oxygen isotope systematics in Diploastrea heliopora:new coral archive of tropical paleoclimate[J]. Geochimica et Cosmochimica Acta, 2003, 67(7):1349-1358.
    [18]
    Peng Z C, He J F, Chen T G, et al. Sea surface temperature variability in the north side of the South China Sea over the last 55 years revealed by coral δ18O records[J]. Geochimica et Cosmochimica Acta, 2003, 67(18S):A378.
    [19]
    余克服,陈特固,黄鼎成,等. 中国南沙群岛滨珊瑚δ18O的高分辨率气候记录[J]. 科学通报, 2001, 46(14):1199-1203.

    [YU Ke-fu, CHEN Te-gu, HUANG Ding-cheng, et al. High resolution climate record of coral δ18O from Nansha Island, China[J]. Chinese Science Bulletin, 2001, 46(14):1199-1203.]
    [20]
    Wei G J, Sun M, Li X H, et al. Mg/Ca, Sr/Ca and U/Ca ratios of a Porites coral from Sanya Bay, Hainan Island, South China Sea and their relationships to sea surface temperature[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 162:59-74.
    [21]
    Sun Y L, Sun M, Wei G J, et al. Strontium contents of a Porites coral from Xisha Island, South China Sea:A proxy for sea-surface temperature of the 20th century[J]. Paleoceanography, 2004, 19, doi: 10.1029/2003PA000959.
    [22]
    吕炳全,王红罡,大场忠道,等. 海南岛沙老岸礁区滨珊瑚氧、碳同位素对气候的记录[J]. 地球化学, 2002, 31(4):315-320.

    [LÜ Bing-quan, WANG Hong-gang, TADAMICHI Oba, et al. Monsoon climatic record of oxygen and carbon isotopic data from Porites lutea in Shalao fringing reef, Hainan Island[J]. Geochimica, 2002, 31(4):315-320.]
    [23]
    Quinn T M, Crowley T J, Taylor F W, et al. A multicentury stable isotope record from a New Caledonia coral:interannual and decadal sea surface temperature variability in the southwest Pacific since 1657 AD[J]. Paleoceanography, 1998, 13(4):412-426.
    [24]
    Gagan M K, Ayliffe L K, Hopley D, et al. Temperature and surface-ocean water balance of the mid-Holocene tropical western Pacific[J]. Science, 1998, 279:1014-1018.
    [25]
    Juillet-Leclerc A. A calibration of oxygen isotope paleothermometer of coral aragonite from Porites[J]. Geophysical Research Letters, 2001, 28(21):4135-4138.
    [26]
    McConnaughey T A. 13C and 18O isotopic disequilibrium in biological carbonate, I. Patterns[J]. Geochimca et Cosmochimica Acta, 1998, 53:151-162.
    [27]
    Wellington G M, Dunbar R B, Merlen G. Calibration of stable oxygen isotope signatures in Galápagos corals[J]. Paleoceanography, 1996, 11(4):467-480.
    [28]
    Sun D H, Gagan M K, Cheng H, et al. Seasonal and interannual variability of the Mid-Holocene East Asian monsoon in coral δ18O records from the South China Sea[J]. Earth and Planetary Science Letters, 2005, 237:69-84.
    [29]
    Ren L, Linsley B K, Wellington G M, et al. Deconvolving the δ18O seawater component from subseasonal coral δ18O and Sr/Ca at Rarotonga in the southern subtropical Pacific for the period 1726-1997[J]. Geochimca et Cosmochimica Acta, 2002, 67(9):1609-1621.
  • Related Articles

    [1]XU Hongfei, WU Feng, YE Maosong, ZHU Youhua, WANG Jingwen. Depositional evolution and controlling factors of the middle-late Holocene fringing reef in Hainan Island[J]. Marine Geology & Quaternary Geology, 2025, 45(3): 1-12. DOI: 10.16562/j.cnki.0256-1492.2024111101
    [2]ZHANG Yongwei, TIAN Xu, XU Fangjian, CHEN Bo, YE Youquan, FAN Dejiang. Provenance and environmental response of terrigenous debris in the southeastern continental shelf of Hainan Island since 7.8 kaBP[J]. Marine Geology & Quaternary Geology, 2023, 43(1): 27-36. DOI: 10.16562/j.cnki.0256-1492.2022073101
    [3]XUAN Yutian, ZHAN Wenhuan, YAO Yantao, WANG Pin, LI Jian, FENG Yingci. Testing of quartz ESR dating for the marine strata on the northwestern coast of Hainan Island[J]. Marine Geology & Quaternary Geology, 2022, 42(3): 123-132. DOI: 10.16562/j.cnki.0256-1492.2021122302
    [4]CHEN Hongjun, HUANG Wenkai, QIU Yan. THE INVERSION OF LATE QUATERNARY PALEO-WATER DEPTH IN SOUTHWESTERN OFFSHORE HAINAN ISLAND[J]. Marine Geology & Quaternary Geology, 2017, 37(6): 128-139. DOI: 10.16562/j.cnki.0256-1492.2017.06.014
    [5]LUO Kun, LIU Gang, XUE Yulong, PAN Yanjun, CHEN Wen. PREDICTING SAND-LAYER DISTRIBUTION IN OFFSHORE AREA OF EASTERN HAINAN ISLAND WITH SINGLE-CHANNEL SEISMIC REFLECTION DATA[J]. Marine Geology & Quaternary Geology, 2017, 37(1): 125-130. DOI: 10.16562/j.cnki.0256-1492.2017.01.015
    [6]XU Shendong, CHEN Wenhuang, DENG Wenfeng, JIA Guodong. WINTER SURFACE SEAWATER TEMPERATURE IN THE NORTHERN SOUTH CHINA SEA INDUCED FROM TEMPERATURE INDEX OF SHELL OXYGEN ISOTOPE OF GLOBIGERINOIDES RUBER[J]. Marine Geology & Quaternary Geology, 2016, 36(2): 101-107. DOI: 10.16562/j.cnki.0256-1492.2016.02.012
    [7]DU Yunkong, LIU Hailing, TAN Xiaodong, HAN Yulin, WU Yi, WU Chaohua, ZHAO Meisong. LATE PALEOZOIC TO MESOZOIC PALEOMAGNETIC RESULTS FROM HAINAN ISLAND AND ITS TECTONIC IMPLICATIONS FOR THE NORTHERN MARGIN OF THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2013, 33(6): 93-103. DOI: 10.3724/SP.J.1140.2013.06093
    [8]SHI Xiao-jun, YU Ke-fu, CHEN Te-gu, ZHANG Jiang-yong, ZHAO Jian-xin. MID-TO LATE-HOLOCENE SEA LEVEL HIGHSTANDS: EVIDENCE FROM FRINGING CORAL REEFS AT QIONGHAI, HAINAN ISLAND[J]. Marine Geology & Quaternary Geology, 2008, 28(5): 1-9.
    [9]ZHANG Zhen-ke, MENG Hong-ming, WANG Wan-fang, LI Yan-ming, YOU Kun-yuan, YU Ke-fu. PRELIMINARY STUDY ON THE COASTAL SEDIMENTS RECORDS ABOUT THE HISTORICAL EARTHQUAKE IN THE YEAR OF 1605, HAINAN ISLAND, CHINA[J]. Marine Geology & Quaternary Geology, 2008, 28(3): 9-14.
    [10]MAO Long-jiang, ZHANG Yong-zhan, ZHANG Zhen-ke, WEI Ling, JI Xiao-mei, ZHU Da-kui. CHARACTERISTICS OF SEDIMENTARY ENVIRONMENTS IN SANYA BAY OF HAINAN ISLAND[J]. Marine Geology & Quaternary Geology, 2007, 27(4): 17-22.
  • Cited by

    Periodical cited type(12)

    1. 李林致,郭刚,廖计华,王欣,李婧婧,吴斌,张晓庆. 丽水-椒江凹陷月桂峰组湖相烃源岩的主控因素与分布预测. 海洋地质前沿. 2024(04): 9-17 .
    2. 何雁兵 ,雷永昌 ,邱欣卫 ,肖张波 ,郑仰帝 ,刘冬青 . 珠江口盆地陆丰南地区文昌组沉积古环境恢复及烃源岩有机质富集主控因素研究. 地学前缘. 2024(02): 359-376 .
    3. 郑仰帝,彭光荣,肖张波,黄鑫,何雁兵,杨兴业. 古近系文昌组湖盆古环境及其对烃源岩的控制作用——以珠江口盆地陆丰15洼为例. 华南地震. 2024(01): 11-24 .
    4. 郭奕浩,曾德铭,张芮,王兴志,黄董,张本健,谢圣阳. 川中—川东地区侏罗系大安寨段古环境及油气地质意义. 沉积学报. 2024(03): 1016-1031 .
    5. 阙晓铭,舒誉,汪旭东,雷永昌,王宇辰,吴琼玲. 珠一坳陷古近纪物源特征及其沉积演化:来自碎屑锆石年龄的指示. 地球科学. 2024(07): 2373-2387 .
    6. 耿名扬,刘志峰,吴斌. 渤海海域秦南凹陷沙河街组烃源岩沉积环境及发育模式. 大庆石油地质与开发. 2024(06): 20-28 .
    7. 党昭卿,陈莹,吕成福,白志钊,肖月也,周钱山. 利用三角洲前积层的厚度恢复湖泊最大古水深:以渤海湾盆地秦南凹陷和珠江口盆地惠州凹陷为例. 高校地质学报. 2024(06): 726-736 .
    8. 谢世文,柳保军,庞雄,丁琳,吴宇翔,刘冬青,王宇辰. 珠江口盆地白云凹陷裂陷期沉积环境演化与控烃作用. 天然气地球科学. 2023(02): 296-311 .
    9. 阙晓铭,雷永昌,汪旭东,贾连凯,宋伟. 珠江口盆地陆丰南文五段低矿化度水化学特征及成因分析. 中国海上油气. 2023(02): 23-32 .
    10. 林义华,梁定勇,魏昌欣,吕昭英,吴迪,黄武轩,许国强,杜鹃. 海南岛西北部晚更新世海滩岩地球化学特征及其古环境意义. 科学技术与工程. 2023(10): 4079-4090 .
    11. 贾培蒙,杜家元,陈维涛,杨兴业,熊万林,靳瑶瑶. 断陷盆地边缘洼陷优质烃源岩形成机制——以珠江口盆地惠州26洼东北次洼为例. 海洋地质与第四纪地质. 2022(03): 140-148 . 本站查看
    12. 古榕,王智闻,周华. 准噶尔南缘中段上侏罗统—下白垩统沉积古环境分析. 中国锰业. 2022(05): 11-15 .

    Other cited types(4)

Catalog

    XIAN Feng

    1. On this Site
    2. On Google Scholar
    3. On PubMed
    Article views (2086) PDF downloads (9) Cited by(16)

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return