Volume 41 Issue 1
Jan.  2022
Turn off MathJax
Article Contents
Baohong Chen, Kaiwen Zhou, Kang Wang, Jigang Wang, Sumin Wang, Xiuwu Sun, Jinmin Chen, Cai Lin, Hui Lin. Temporal and spatial distribution characteristics of nutrients in Clarion-Clipperton Fracture Zone in the Pacific in 2017[J]. Acta Oceanologica Sinica, 2022, 41(1): 1-10. doi: 10.1007/s13131-021-1931-y
Citation: Baohong Chen, Kaiwen Zhou, Kang Wang, Jigang Wang, Sumin Wang, Xiuwu Sun, Jinmin Chen, Cai Lin, Hui Lin. Temporal and spatial distribution characteristics of nutrients in Clarion-Clipperton Fracture Zone in the Pacific in 2017[J]. Acta Oceanologica Sinica, 2022, 41(1): 1-10. doi: 10.1007/s13131-021-1931-y

Temporal and spatial distribution characteristics of nutrients in Clarion-Clipperton Fracture Zone in the Pacific in 2017

doi: 10.1007/s13131-021-1931-y
Funds:  The Eastern Pacific Ecoenvironment Monitoring and Protection Project under contract No. DY135-E2-5-02; the Global Change and Air-sea Interaction II under contract No. GASI-01-NPAC-STsum; the Scientific Research Foundation of the Third Institute of Oceanography, Ministry of Natural Resources of China under contract No. 2019017.
More Information
  • Corresponding author: E-mail: lincai@tio.org.cnlinhui@tio.org.cn
  • Received Date: 2021-01-05
  • Accepted Date: 2021-02-19
  • Available Online: 2021-12-02
  • Publish Date: 2022-01-10
  • This research investigated eight stations in Clarion-Clipperton Fracture Zone (CCFZ) in the eastern tropical Pacific in 2017 to study the spatial distribution characteristics of nutrients and chlorophyll a (Chl a) concentration, and compared nutrient concentrations and molar ratios with those of other investigations 20 years ago in the same area. The study found that dissolved inorganic nutrient (N, P and Si) concentrations were lowest in the upper layer, and increased from surface to some depths, then they decreased a little to the bottom. N was the limited nutrient factor for the growth of phytoplankton community. Although nutrient concentrations and molar ratios have no obvious changes in 2017 comparing those in 1998−2003, supplemented from the equatorial Pacific, nutrient concentrations in the study area were higher than those in seamounts in the North Pacific and Station ALOHA. Furthermore, this study used Generalized Additive Models (GAMs) to infer the underlying bottom-up factors controlling phytoplankton abundance (Chl a concentration), showing that depth, salinity and ${\rm{PO}}_4^{3 - }{\text -}{\rm{ P}} $ concentration were major factors controlling the growth of phytoplankton community. Furthermore, this study can provide basic data and theoretical support for the development of polymetallic nodule area and its long-term impact assessment on the environment.
  • loading
  • [1]
    Bahamón N, Velásquez Z, Cruzado A. 2003. Chlorophyll a and nitrogen flux in the tropical North Atlantic Ocean. Deep-Sea Research Part I: Oceanographic Research Papers, 50(10–11): 1189–1203
    [2]
    Bange H W, Rixen T, Johansen A M, et al. 2000. A revised nitrogen budget for the Arabian Sea. Global Biogeochemical Cycles, 14(4): 1283–1297. doi: 10.1029/1999GB001228
    [3]
    Cavender-Bares K K, Karl D M, Chisholm S W. 2001. Nutrient gradients in the western North Atlantic Ocean: Relationship to microbial community structure and comparison to patterns in the Pacific Ocean. Deep-Sea Research Part I: Oceanographic Research Papers, 48(11): 2373–2395. doi: 10.1016/S0967-0637(01)00027-9
    [4]
    Chang B X, Devol A H, Emerson S R. 2010. Denitrification and the nitrogen gas excess in the eastern tropical South Pacific oxygen deficient zone. Deep-Sea Research Part I: Oceanographic Research Papers, 57(9): 1092–1101. doi: 10.1016/j.dsr.2010.05.009
    [5]
    Chen Baohong, Ji Weidong, Zhou Kaiwen, et al. 2014. Nutrient and eutrophication characteristics of the Dongshan Bay, South China. Chinese Journal of Oceanology and Limnology, 32(4): 886–898. doi: 10.1007/s00343-014-3214-3
    [6]
    Chen Bingzhang, Liu Hongbin, Huang Bangqin. 2012. Environmental controlling mechanisms on bacterial abundance in the South China Sea inferred from generalized additive models (GAMs). Journal of Sea Research, 72: 69–76. doi: 10.1016/j.seares.2012.05.012
    [7]
    Codispoti L A, Brandes J A, Christensen J P, et al. 2001. The oceanic fixed nitrogen and nitrous oxide budgets: moving targets as we enter the anthropocene?. Scientia Marina, 65(S2): 85–105.
    [8]
    Codispoti L A, Christensen J P. 1985. Nitrification, denitrification and nitrous oxide cycling in the eastern tropical South Pacific Ocean. Marine Chemistry, 16(4): 277–300. doi: 10.1016/0304-4203(85)90051-9
    [9]
    Deng Jianming, Qin Boqiang, Wang Bowen. 2015. Quick implementing of generalized additive models using R and its application in blue-green algal bloom forecasting. Chinese Journal of Ecology, 34(3): 835–842
    [10]
    Feely R A, Gammon R H, Taft B A, et al. 1987. Distribution of chemical tracers in the eastern equatorial Pacific during and after the 1982–1983 El Niño/Southern Oscillation event. Journal of Geophysical Research: Oceans, 92(C6): 6545–6558. doi: 10.1029/JC092iC06p06545
    [11]
    Fiedler P C, Lavin M F. 2006. Introduction: a review of eastern tropical Pacific oceanography. Progress in Oceanography, 69(2–4): 94–100
    [12]
    Fiedler P C, Talley L D. 2006. Hydrography of the eastern tropical Pacific: a review. Progress in Oceanography, 69(2–4): 143–180
    [13]
    General Administration of Quality Supervision, Inspection and Quarantine of the People’s Republic of China, Standardization Administration. 2008. GB/T 12763.4-2007 Specifications for oceanographic survey—Part 4: Survey of Chemical Parameters in Sea Water. Beijing: Standards Press of China (in Chinese)
    [14]
    Glover A G, Smith C R, Paterson G L J, et al. 2002. Polychaete species diversity in the central Pacific abyss: local and regional patterns, and relationships with productivity. Marine Ecology Progress Series, 240: 157–170. doi: 10.3354/meps240157
    [15]
    Hastie T J, Tibshirani R J. 1990. Generalized Additive Models. New York, USA: Chapman & Hall/CRC
    [16]
    Jia Bin, Wang Tong, Wang Linna, et al. 2005. Concurvity in generalized additive models in study of air pollution. Journal of the Fourth Military Medical University, 26(3): 280–283
    [17]
    Jones D O B, Kaiser S, Sweetman A K, et al. 2017. Biological responses to disturbance from simulated deep-sea polymetallic nodule mining. PLoS ONE, 12(2): e0171750. doi: 10.1371/journal.pone.0171750
    [18]
    Kalvelage T, Lavik G, Jensen M M, et al. 2015. Aerobic microbial respiration in oceanic oxygen minimum zones. PLoS ONE, 10(7): e0133526. doi: 10.1371/journal.pone.0133526
    [19]
    Kamykowski D, Zentara S J. 1990. Hypoxia in the world ocean as recorded in the historical data set. Deep-Sea Research Part A: Oceanographic Research Papers, 37(12): 1861–1874
    [20]
    Karl D M, Björkman K M, Dore J E, et al. 2001. Ecological nitrogen-to-phosphorus stoichiometry at Station ALOHA. Deep-Sea Research Part II: Topical Studies in Oceanography, 48(8–9): 1529–1566
    [21]
    Kessler W S. 2006. The circulation of the eastern tropical Pacific: a review. Progress in Oceanography, 69(2–4): 181–217
    [22]
    Kim J H, Lee H, Kang J H. 2019. Associating the spatial properties of a watershed with downstream Chl a concentration using spatial analysis and generalized additive models. Water Research, 154: 387–401. doi: 10.1016/j.watres.2019.02.010
    [23]
    Libby P S, Wheeler P A. 1997. Particulate and dissolved organic nitrogen in the central and eastern equatorial Pacific. Deep-Sea Research Part I: Oceanographic Research Papers, 44(2): 345–361. doi: 10.1016/S0967-0637(96)00089-1
    [24]
    Loubere P. 2001. Nutrient and oceanographic changes in the eastern equatorial Pacific from the last full Glacial to the Present. Global and Planetary Change, 29(1–2): 77–98
    [25]
    Menendez A, James R H, Lichtschlag A, et al. 2019. Controls on the chemical composition of ferromanganese nodules in the Clarion-Clipperton Fracture Zone, eastern equatorial Pacific. Marine Geology, 409: 1–14. doi: 10.1016/j.margeo.2018.12.004
    [26]
    Ni Jianyu, Liu Xiaoqi, Zhao Hongqiao, et al. 2011. Nutrients distribution in the middle-to-low latitude zone of North Pacific. Marine Geology & Quaternary Geology, 31(2): 11–19
    [27]
    Qiao Yinhuan, Feng Jianfeng, Cui Shangfa, et al. 2017. Long-term changes in nutrients, chlorophyll a and their relationships in a semi-enclosed eutrophic ecosystem, Bohai Bay, China. Marine Pollution Bulletin, 117(1–2): 222–228
    [28]
    Raimbault P, Slawyk G, Boudjellal B, et al. 1999. Carbon and nitrogen uptake and export in the equatorial Pacific at 150°W: evidence of an efficient regenerated production cycle. Journal of Geophysical Research: Oceans, 104(C2): 3341–3356. doi: 10.1029/1998JC900004
    [29]
    Raitsos D E, Korres G, Triantafyllou G, et al. 2012. Assessing chlorophyll variability in relation to the environmental regime in Pagasitikos Gulf, Greece. Journal of Marine Systems, 94 (S1): S16–S22
    [30]
    Smith C R, De Leo F C, Bernardino A F, et al. 2008. Abyssal food limitation, ecosystem structure and climate change. Trends in Ecology & Evolution, 23(9): 518–528
    [31]
    Song Hongjun, Zhang Xuelei, Wang Baodong, et al. 2014. Bottom-up and top-down controls of the phytoplankton standing stock off the Changjiang Estuary. Haiyang Xuebao (in Chinese), 36(8): 91–100
    [32]
    Toggweiler J, Carson S. 1995. What are upwelling systems contributing to the ocean’s carbon and nutrient budgets?. In: Summerhays C, ed. Upwelling in the Ocean: Modern Processes and Ancient Records. New York, USA: John Wiley, 337–360
    [33]
    Tu Xiaoxia. 2006. The research of nutrient dynamic in the China Pioneer Area of the Northeast Pacific Ocean (in Chinese) [dissertation]. Guangzhou: Guangzhou Institute of Geochemistry, Chinese Academy of Sciences
    [34]
    Volz J B, Mogollón J M, Geibert W, et al. 2018. Natural spatial variability of depositional conditions, biogeochemical processes and element fluxes in sediments of the eastern Clarion-Clipperton Zone, Pacific Ocean. Deep-Sea Research Part I: Oceanographic Research Papers, 140: 159–172. doi: 10.1016/j.dsr.2018.08.006
    [35]
    Wang Chunzai, Enfield D B. 2001. The tropical Western Hemisphere warm pool. Geophysical Research Letters, 28(8): 1635–1638. doi: 10.1029/2000GL011763
    [36]
    Wood S N. 2006. Generalized Additive Models: An introduction with R. Boca Raton, FL, USA: Chapman & Hall/CRC, 7–15
    [37]
    Wu Jingfeng, Chung Shi-wei, Liang Sawwen, et al. 2003. Dissolved inorganic phosphorus, dissolved iron, and Trichodesmium in the oligotrophic South China Sea. Global Biogeochemical Cycles, 17(1): 1008
    [38]
    Wu Yuehong, Liao Li, Wang Chunsheng, et al. 2013. A comparison of microbial communities in deep-sea polymetallic nodules and the surrounding sediments in the Pacific Ocean. Deep-Sea Research Part I: Oceanographic Research Papers, 79: 40–49. doi: 10.1016/j.dsr.2013.05.004
    [39]
    Zhang Hanxiao, Huo Shouliang, Yeager K M, et al. 2019. Phytoplankton response to climate changes and anthropogenic activities recorded by sedimentary pigments in a shallow eutrophied lake. Science of the Total Environment, 647: 1398–1409. doi: 10.1016/j.scitotenv.2018.08.081
    [40]
    Zhou Huimin, Feng Jianfeng, Zhu Lin. 2014. Effects of environmental factors on the chlorophyll a in central Bohai Sea with GAM. Marine Environmental Science, 33(4): 531–536
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(7)  / Tables(8)

    Article Metrics

    Article views (273) PDF downloads(7) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return