A review: iron and nutrient supply in the subarctic Pacific and its impact on phytoplankton production

被引:0
作者
Jun Nishioka
Hajime Obata
Toru Hirawake
Yoshiko Kondo
Youhei Yamashita
Kazuhiro Misumi
Ichiro Yasuda
机构
[1] Hokkaido University,Pan
[2] Hokkaido University,Okhotsk Research Center, Institute of Low Temperature Science
[3] The University of Tokyo,Arctic Research Center
[4] Hokkaido University,Atmosphere and Ocean Research Institute
[5] Nagasaki University,Faculty of Fisheries Sciences
[6] Hokkaido University,Graduate School of Fisheries and Environmental Sciences
[7] Central Research Institute of Electric Power Industry,Faculty of Environmental Earth Science
来源
Journal of Oceanography | 2021年 / 77卷
关键词
Iron supply processes; Nutrient dynamics; Subarctic Pacific; Marginal seas; Phytoplankton production;
D O I
暂无
中图分类号
学科分类号
摘要
One of the most important breakthroughs in oceanography in the last 30 years was the discovery that iron (Fe) controls biological production as a micronutrient, and our understanding of Fe and nutrient biogeochemical dynamics in the ocean has significantly advanced. In this review, we looked back both previous and updated knowledge of the natural Fe supply processes and nutrient dynamics in the subarctic Pacific and its impact on biological production. Although atmospheric dust has been considered to be the most important source of Fe affecting biological production in the subarctic Pacific, other oceanic sources of Fe have been discovered. We propose a coherent explanation for the biological response in subarctic Pacific high nutrient low chlorophyll (HNLC) waters that incorporates knowledge of both the atmospheric Fe supplies and the oceanic Fe supplies. Finally, we extract future directions for Fe oceanographic research in the subarctic Pacific and summarize the uncertain issues identified thus far.
引用
收藏
页码:561 / 587
页数:26
相关论文
共 1092 条
[1]  
Aguilar-Islas A(2007)Micro- and macronutrients in the southeastern Bering Sea: insight into iron-replete and iron-depleted regime Prog Oceanogr 73 99-126
[2]  
Hurst MP(1987)Satellite passive microwave studies of the Sea of Okhotsk ice cover and its relation to oceanic processes 1978–1982 J Geophys Res Oceans 92 13013-13028
[3]  
Buck KN(2020)GEOTRACES: accelerating research on the marine biogeochemical cycles of trace elements and their isotopes Annu Rev Mar Sci 12 49-85
[4]  
Sohst B(1994)Redfield ratios of remineralization determined by nutrient data analysis Global Biogeochem Cycles 8 65-80
[5]  
Smith GJ(2002)Robotic observations of dust storm enhancement of carbon biomass in the North Pacific Science 298 817-821
[6]  
Lohan MC(1999)Near-surface circulation of the northeast Pacific Ocean derived from WOCE-SUP satellite-tracked drifters Deep Sea Res II 46 2371-2403
[7]  
Bruland KW(1998)Determination of sub-nanomolar levels of iron in seawater using flow injection with chemiluminescence detection Anal Chim Acta 361 189-200
[8]  
Alfultis MA(2010)The biogeochemical cycle of iron in the ocean Nature Geo 3 675-682
[9]  
Martin S(1998)Atmospheric iron supply and enhanced vertical carbon flux in the NE subarctic Pacific: is there a connection? Global Biogeochem Cycles 12 429-441
[10]  
Anderson RF(2004)The decline and fate of an iron-induced subarctic phytoplankton bloom Nature 428 549-553