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台湾海峡南部海域好氧不产氧光合异养细菌对上升流的响应

陈瑶 张瑶 焦念志

陈瑶,张瑶,焦念志. 台湾海峡南部海域好氧不产氧光合异养细菌对上升流的响应[J]. 海洋学报,2021,43(6):98–107 doi: 10.12284/hyxb2021068
引用本文: 陈瑶,张瑶,焦念志. 台湾海峡南部海域好氧不产氧光合异养细菌对上升流的响应[J]. 海洋学报,2021,43(6):98–107 doi: 10.12284/hyxb2021068
Chen Yao,Zhang Yao,Jiao Nianzhi. Response of aerobic anoxygenic phototrophic bacteria to upwelling in the southern Taiwan Strait of China[J]. Haiyang Xuebao,2021, 43(6):98–107 doi: 10.12284/hyxb2021068
Citation: Chen Yao,Zhang Yao,Jiao Nianzhi. Response of aerobic anoxygenic phototrophic bacteria to upwelling in the southern Taiwan Strait of China[J]. Haiyang Xuebao,2021, 43(6):98–107 doi: 10.12284/hyxb2021068

台湾海峡南部海域好氧不产氧光合异养细菌对上升流的响应

doi: 10.12284/hyxb2021068
基金项目: 科技部重点研发计划(2016YFA0601400)
详细信息
    作者简介:

    陈瑶(1980-),女,浙江省永康市人,博士,主要研究方向为海洋生态学。E-mail:baby_680@126.com

    通讯作者:

    张瑶,教授,博士生导师,主要研究方向为微生物海洋学。E-mail: yaozhang@xmu.edu.cn

    焦念志,中国科学院院士,主要研究海洋微型生物碳泵、海洋微型生物生理生态、分子生态学以及相关的资源环境效应。E-mail: jiao@xmu.edu.cn

  • 中图分类号: P714+.5

Response of aerobic anoxygenic phototrophic bacteria to upwelling in the southern Taiwan Strait of China

  • 摘要: 国内外关于好氧不产氧光合异养细菌(AAPB)和上升流之间关系的研究甚少。本文采用“基于蓝细菌校正的时序红外显微技术”研究了台湾海峡南部近岸上升流中心区AAPB对上升流变化的响应。研究结果发现,在上升流涌升的初始阶段,AAPB和总异养细菌丰度较低;随着上升流的发展,两者丰度均增加并在上升流的成熟期达到最高值;而当上升流衰退时,AAPB和总异养细菌丰度开始下降。在上升流发展过程中,AAPB丰度与叶绿素a浓度在一定范围内呈显著正相关,但同时受环境低磷浓度的限制,总异养细菌丰度与氮、磷、硅营养盐均有显著正相关,表明叶绿素a指示的浮游植物所释放的溶解有机碳和环境中的磷限制可能对AAPB起着更为直接和重要的作用,而营养盐则可能在总异养细菌对上升流的响应中起着重要作用。本研究有助于我们理解AAPB在碳及其他生源要素循环中的作用及其调控机制。
  • 图  1  台湾海峡站位

    Fig.  1  Location of the stations in the Taiwan Strait

    图  2  台湾海峡南部海域大面站温度(单位:°C)和盐度的垂直分布

    Fig.  2  Vertical distribution of temperature (unit: °C) and salinity in the southern Taiwan Strait

    图  3  B1站位温度(a)和盐度(b)剖面动态变化

    Fig.  3  Variation of temperature (a) and salinity (b) at Station B1

    图  4  台湾海峡南部海域大面站营养盐浓度(单位:μmol/L)的垂直分布

    Fig.  4  Vertical distribution of nutrients concentration (uint: μmol/L) in the southern Taiwan Strait

    图  5  B1站位营养盐浓度(单位:μmol/L)的剖面动态变化

    a. 硝酸盐; b. 亚硝酸盐; c. 铵盐; d. 磷酸盐; e. 硅酸盐

    Fig.  5  Variation of nutrients concentration (unit: μmol/L) at Station B1

    a. $ {{\rm {NO}}_3^-} $-N; b. $ {{\rm {NO}}_2^-} $-N; c. $ {{\rm {NH}}_4^+} $-N; d. $ {{\rm {PO}}_4^{3-}} $-P; e. $ {{\rm {SiO}}_3^{2-}} $-Si

    图  6  B1站位叶绿素a浓度(单位:μg/L)(a)、AAPB丰度(单位:cell/mL)(b)、总异养细菌丰度(单位:cell/mL)(c)和AAPB%(d)的剖面动态变化

    Fig.  6  Variation of chlorophyll a concentration (unit: μg/L) (a), AAPB abundance (unit: cell/mL) (b), total bacterial abundance (unit: cell/mL) (c) and AAPB% (d) at Station B1

    图  7  台湾海峡南部海域上升流事件中AAPB丰度(a)、总异养细菌丰度(b)和叶绿素a浓度的相关关系

    实心圆代表叶绿素a浓度较低的站位,AAPB丰度与叶绿素a浓度显著正相关;空心圆代表叶绿素a浓度较高的站位,AAPB和总异养细菌丰度与叶绿素a浓度无相关性

    Fig.  7  Plots of AAPB abundance (a) and total bacterial abundance (b) vs chlorophyll a concentration in the development of upwelling in the southern Taiwan Strait

    The solid circles represent the stations with low chlorophyll a concentration where AAPB abundance is positively correlate with chlorophyll a concentration; the open circles represent the stations with high chlorophyll a concentration where AAPB abundance and total bacterial abundance display little correlation with chlorophyll a concentration

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  • 收稿日期:  2020-12-14
  • 修回日期:  2021-02-18
  • 网络出版日期:  2021-05-24
  • 刊出日期:  2021-06-30

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