

FOLLOWUS
1.CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.Marine Ecology and Environmental Science Laboratory, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
3.University of Chinese Academy of Sciences, Beijing 100049, China
4.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
SONG Jinming, jmsong@qdio.ac.cn
LI Xuegang, lixuegang@qdio.ac.cn
收稿:2019-12-04,
录用:2019-12-9,
网络首发:2020-12-30,
纸质出版:2020-07
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Control factors of DIC in the Y3 seamount waters of the Western Pacific Ocean[J]. 海洋湖沼学报(英文), 2020,38(4):1215-1224.
Jun MA, Jinming SONG, Xuegang LI, et al. Control factors of DIC in the Y3 seamount waters of the Western Pacific Ocean[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1215-1224.
Control factors of DIC in the Y3 seamount waters of the Western Pacific Ocean[J]. 海洋湖沼学报(英文), 2020,38(4):1215-1224. DOI: 10.1007/s00343-020-9314-3.
Jun MA, Jinming SONG, Xuegang LI, et al. Control factors of DIC in the Y3 seamount waters of the Western Pacific Ocean[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1215-1224. DOI: 10.1007/s00343-020-9314-3.
An investigation was carried out in the Y3 seamount area of the Western Pacific Ocean in December 2014
and the distribution of dissolved inorganic carbon (DIC) and its relationship with environmental factors in this area were explored. The results show that DIC concentration was higher in the adjacent waters of the Y3 seamount area
and the uplift of DIC isolines at the stations was close to the seamount. Meanwhile
interaction between the North Equatorial Current (NEC) and the Y3 seamount affected the DIC distribution
i.e.
the upwelling in the same direction of the NEC was obvious
resulting in a decreasing trend of average concentration of DIC in the 200 m water column from the top to the two sides in this direction but in the cross direction. The DIC concentration increased with the water depth increase
and its distribution was affected by various environmental factors. In the surface water
high temperature was a decisive factor for the decrease of the DIC concentration
but the photosynthesis of phytoplankton showing only a weak influence. In the North Pacific Tropic Water (NPTW)
DIC production rate from organic matter decomposition was higher than that of DIC consumption by phytoplankton photosynthesis
leading to a continual increase of DIC. In the North Pacific Intermediate Water (NPIW)
organic matter decomposition played a leading role in the increase of DIC. In the deep water
decomposition of organic matter weakened
and the dissolution of CaCO
3
controlled the carbonate system
and DIC had the smallest variation range.
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