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台湾近海热液体系独特的生物及地球化学特征

陈雪刚 吴斌 郑豪 樊炜 叶瑛 陈镇东

陈雪刚,吴斌,郑豪,等. 台湾近海热液体系独特的生物及地球化学特征[J]. 海洋学报,2019,41(10):161–168,doi:10.3969/j.issn.0253−4193.2019.10.010
引用本文: 陈雪刚,吴斌,郑豪,等. 台湾近海热液体系独特的生物及地球化学特征[J]. 海洋学报,2019,41(10):161–168,doi:10.3969/j.issn.0253−4193. 2019.10.010
Chen Xuegang,Wu Bin,Zheng Hao, et al. Hydrothermal systems at offshore Taiwan: Unique biological and geochemical characteristics[J]. Haiyang Xuebao,2019, 41(10):161–168,doi:10.3969/j.issn.0253−4193.2019.10.010
Citation: Chen Xuegang,Wu Bin,Zheng Hao, et al. Hydrothermal systems at offshore Taiwan: Unique biological and geochemical characteristics[J]. Haiyang Xuebao,2019, 41(10):161–168,doi:10.3969/j.issn.0253−4193. 2019.10.010

台湾近海热液体系独特的生物及地球化学特征

doi: 10.3969/j.issn.0253-4193.2019.10.010
详细信息
    作者简介:

    陈雪刚(1983—),男,浙江省衢州市人,从事海底热液地球化学研究。E-mail: chenxg83@zju.edu.cn

    通讯作者:

    陈镇东,男,讲座教授,主要研究海底热液活动以及海洋碳循环。E-mail: ctchen@mail.nsysu.edu.tw

  • Lebrato M, Garbe-Schönberg D, Tseng L C, et al. Earthquake and typhoon trigger shifts in shallow vents biogeochemistry analogous to human-made ocean disturbances[J]. Submitted to Scientific Reports, 2019.
  • 中图分类号: P722.6; P738.6

Hydrothermal systems at offshore Taiwan: Unique biological and geochemical characteristics

  • 摘要: 台湾地处西太平洋构造活动带,近海发育了多处热液活动,其中最典型的为龟山岛和绿岛热液体系。本文对海峡两岸在龟山岛和绿岛热液的地球化学特征以及周边生物体的响应的研究进展进行了综述。龟山岛热液喷出流体具有全球最低的pH(1.52),富含重金属元素和CO2等酸性气体,是周围海水中有色溶解有机质的来源;绿岛具有全球热液中最低的溶解有机碳浓度(14 μmol /L),且具有特殊的动力学特性。喷口周边分布了较为罕见的自然硫烟囱体和硫磺球。喷口的高毒性、高酸性热液改变了热液区生物体如螃蟹的生活习性和解毒机制。热液区的主要活跃菌群为参与碳、硫和氮代谢途径的γ-和ε-变形菌。主要生物质合成以硫还原和硫氧化的化能无机自养型生物为主,微生物硫代谢促进了热液系统中的微生物能量流动和元素循环作用。某些热液生物采用繁殖期迁徙的机制应对高毒性、高酸性热液环境。在热液活动的胁迫下,这些微生物产生了新颖独特的代谢产物。此外,龟山岛和绿岛热液体系还受到了潮汐、台风和地震等灾害性事件的影响。台湾近海热液体系的研究对认识热液地球化学循环、探讨热液的生态环境效应等具有重要的意义。
    1)  Lebrato M, Garbe-Schönberg D, Tseng L C, et al. Earthquake and typhoon trigger shifts in shallow vents biogeochemistry analogous to human-made ocean disturbances[J]. Submitted to Scientific Reports, 2019.
  • 图  1  台湾近海构造地质背景(a);龟山岛热液系统的远景和俯瞰图(b, c);绿岛热液体系的典型喷口(d)

    Fig.  1  Geological setting of offshore Taiwan (a); outlook of the Kueishantao hydrothermal system (b, c); and a typical vent of the Lutao geothermal field (d)

    图  2  自主研制的热液保真采样器在龟山岛热液喷口进行采样 (a);原位化学传感器链获得的龟山岛海域pH分布[6] (b)

    Fig.  2  Fluid sampling at the Kueishantao vents using self-made samplers (a); spatial distribution pattern of pH in the Kueishantao field that collected using in-situ chemical sensors[6] (b)

    图  3  龟山岛热液独特的自然硫烟囱体(a)、硫磺丘(b)、硫磺球(c)和热液喷口周围生活的特有物种乌龟怪方蟹(d)

    Fig.  3  the unique native sulfur chimney (a), sulfur mound (b), sulfur balls (c), and Xenograpsus testudinatus of the Kueishantao hydrothermal system (d)

    图  4  龟山岛热液流体温度受到全日潮的影响,2000年台风“碧利斯”摧毁了所监测的喷口使其不再活动[4] (a);潮汐对绿岛热液“户外池”水深的影响(b)

    Fig.  4  The Kueishantao vent fluids were affected by diurnal tides, and the Typhoon “Bilis” at 2000 destroyed the monitored vent (a); semi-diurnal oscillation of water depth induced by tide of the Lutao hydrothermal system (b)

    图  5  热液口微生物介导的生物地球化学过程,以及这些独特生态系统中碳、硫和氮循环的可能耦合机制(根据文献[23]重新绘制)

    rTCA/CCB表示还原性三羧酸循环/卡尔文循环

    Fig.  5  Microbial involved biogeochemical process, and the carbon, sulfur and nitrogen cycles and possible coupling mechanisms of this unique hydrothermal ecological system (modified from referance [23])

    rTCA/CCB represents reductive tricarboxylic acid cycle/Calvin-Benson-Bassham cycle

    图  6  从龟山岛热口微生物中分离鉴定的首次从自然界发现的物质

    Fig.  6  The new compounds extracted from the micro-organisms living near the Kueishantao hydrothermal vents

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出版历程
  • 收稿日期:  2019-06-27
  • 修回日期:  2019-08-19
  • 网络出版日期:  2021-04-21
  • 刊出日期:  2019-10-25

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