海南岛滨珊瑚δ18O对环境条件的响应

宋少华, 周卫健, 彭子成, 刘卫国, 程鹏, 鲜锋

宋少华, 周卫健, 彭子成, 刘卫国, 程鹏, 鲜锋. 海南岛滨珊瑚δ18O对环境条件的响应[J]. 海洋地质与第四纪地质, 2006, 26(4): 23-28.
引用本文: 宋少华, 周卫健, 彭子成, 刘卫国, 程鹏, 鲜锋. 海南岛滨珊瑚δ18O对环境条件的响应[J]. 海洋地质与第四纪地质, 2006, 26(4): 23-28.
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.

海南岛滨珊瑚δ18O对环境条件的响应

基金项目: 

黄土与第四纪地质国家重点实验室开放基金(SKLLQG0319)

国家重点基础研究发展规划项目(2004CB720200)

国家自然科学基金项目(40531003,40121303)

详细信息
    作者简介:

    宋少华(1977-),男,博士生,从事珊瑚古环境研究,E-mail:sshh@ieecas.cn

  • 中图分类号: P736

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

  • 摘要: 利用采自海南岛东岸沙老岸礁的活体橙黄滨珊瑚岩心,测试了其中11 a (1992-2002)的珊瑚骨骼氧同位素组成。通过与同期观测记录的海洋表面温度、海洋表层盐度进行比较分析,提出珊瑚δ18O对环境条件变化的响应特征。该地区珊瑚δ18O的年际变化主要受海洋表面温度的控制,而以夏季为代表的季节性变化则主要受海洋表层盐度的影响。
    Abstract: 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.

计量
  • 文章访问数:  2082
  • HTML全文浏览量:  130
  • PDF下载量:  9
  • 被引次数: 0
出版历程
  • 收稿日期:  2005-10-19
  • 修回日期:  2006-02-15

目录

    /

    返回文章
    返回