CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; University of Chinese Academy of Sciences, Beijing 100049, China; Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China.
CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; Function Laboratory of Marine Ecology and Environmental Sciences, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China; University of Chinese Academy of Sciences, Beijing 100049, China; Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China.
Mar Pollut Bull. 2019 Jun;143:163-174. doi: 10.1016/j.marpolbul.2019.04.045. Epub 2019 Apr 28.
Nutrients distribution and influencing factors in three seamount areas named Y3, M2 and C4 of the Tropical Western Pacific Ocean (TWPO) were investigated. Nutrients showed obvious uplifts around the three seamounts, consistent with the uplifts of isotherms and isohalines, indicating the existence of a bottom-up process of nutrients. Meanwhile, compared with the stations away from seamount and the reference stations in the TWPO, nutrients concentrations around seamount were much higher. Among the three seamounts, the average nutrients concentrations were highest in Y3, while they were lowest in C4. Moreover, compared with the obvious nitrogen limitation in Y3 and M2, the N:P (13.5:1) and Si:N (6.1:1) were closed to the Redfield ratio. The current-seamount interaction was the determining influencing factor on nutrients distribution, causing the hydrology dynamic changes such as uplifts and Taylor column. Meanwhile, T and S also affected nutrients distribution, especially nutrients and T showed significant negative correlations.
调查了热带西太平洋(TWPO)Y3、M2 和 C4 三个海山区的营养物质分布及其影响因素。营养物质在三个海山周围明显上升,与等温线和等盐线的上升一致,表明存在营养物质的自下而上的过程。同时,与远离海山的站位和 TWPO 参考站位相比,海山周围站位的营养物质浓度要高得多。在这三个海山中,Y3 的平均营养物质浓度最高,而 C4 的最低。此外,与 Y3 和 M2 中明显的氮限制相比,N:P(13.5:1)和 Si:N(6.1:1)接近赤潮比。海流与海山的相互作用是决定营养物质分布的决定性影响因素,导致水动力变化,如上升和泰勒柱。同时,T 和 S 也影响营养物质的分布,特别是营养物质和 T 之间呈显著负相关。