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DOI | 10.1038/s41561-019-0476-6 |
Resupply of mesopelagic dissolved iron controlled by particulate iron composition | |
Bressac, M.1,2; Guieu, C.2,3; Ellwood, M. J.4; Tagliabue, A.5; Wagener, T.6; Laurenceau-Cornec, E. C.1; Whitby, H.7; Sarthou, G.7; Boyd, P. W.1,8 | |
通讯作者 | Bressac, M. |
来源期刊 | NATURE GEOSCIENCE
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ISSN | 1752-0894 |
EISSN | 1752-0908 |
出版年 | 2019 |
卷号 | 12期号:12页码:995-+ |
英文摘要 | The dissolved iron supply controls half of the oceans' primary productivity. Resupply by the remineralization of sinking particles, and subsequent vertical mixing, largely sustains this productivity. However, our understanding of the drivers of dissolved iron resupply, and their influence on its vertical distribution across the oceans, is still limited due to sparse observations. There is a lack of empirical evidence as to what controls the subsurface iron remineralization due to difficulties in studying mesopelagic biogeochemistry. Here we present estimates of particulate transformations to dissolved iron, concurrent oxygen consumption and iron-binding ligand replenishment based on in situ mesopelagic experiments. Dissolved iron regeneration efficiencies (that is, replenishment over oxygen consumption) were 10- to 100-fold higher in low-dust subantarctic waters relative to higher-dust Mediterranean sites. Regeneration efficiencies are heavily influenced by particle composition. Their make-up dictates ligand release, controls scavenging, modulates ballasting and may lead to the differential remineralization of biogenic versus lithogenic iron. At high-dust sites, these processes together increase the iron remineralization length scale. Modelling reveals that in oceanic regions near deserts, enhanced lithogenic fluxes deepen the ferricline, which alter the vertical patterns of dissolved iron replenishment, and set its redistribution at the global scale. Such wide-ranging regeneration efficiencies drive different vertical patterns in dissolved iron replenishment across oceanic provinces. |
类型 | Article |
语种 | 英语 |
国家 | Australia ; France ; U Arab Emirates ; England |
开放获取类型 | Green Submitted |
收录类别 | SCI-E |
WOS记录号 | WOS:000499653700009 |
WOS关键词 | POLAR FRONTAL ZONES ; DUST-DEPOSITION ; SOUTHERN-OCEAN ; MEDITERRANEAN SEA ; SEDIMENT TRAP ; CARBON SEQUESTRATION ; REMINERALIZATION ; BIOGEOCHEMISTRY ; FLUXES ; EXPORT |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
EI主题词 | 2019-12-01 |
来源机构 | French National Research Institute for Sustainable Development |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/311169 |
作者单位 | 1.Univ Tasmania, Inst Marine & Antarct Studies, Hobart, Tas, Australia; 2.Sorbonne Univ, CNRS, LOV, Villefranche Sur Mer, France; 3.New York Univ Abu Dhabi, Ctr Prototype Climate Modeling, Abu Dhabi, U Arab Emirates; 4.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia; 5.Univ Liverpool, Sch Environm Sci, Dept Earth Ocean & Ecol Sci, Liverpool, Merseyside, England; 6.Univ Toulon & Var, Aix Marseille Univ, CNRS, IRD,MIO,UM 110, Marseille, France; 7.IFREMER, CNRS, UMR 6539, LEMAR,IUEM,UBO,IRD, Technopole Brest Iroise, Plouzane, France; 8.Univ Tasmania, Antarctic Climate & Ecosyst Collaborat Res Ctr, Hobart, Tas, Australia |
推荐引用方式 GB/T 7714 | Bressac, M.,Guieu, C.,Ellwood, M. J.,et al. Resupply of mesopelagic dissolved iron controlled by particulate iron composition[J]. French National Research Institute for Sustainable Development,2019,12(12):995-+. |
APA | Bressac, M..,Guieu, C..,Ellwood, M. J..,Tagliabue, A..,Wagener, T..,...&Boyd, P. W..(2019).Resupply of mesopelagic dissolved iron controlled by particulate iron composition.NATURE GEOSCIENCE,12(12),995-+. |
MLA | Bressac, M.,et al."Resupply of mesopelagic dissolved iron controlled by particulate iron composition".NATURE GEOSCIENCE 12.12(2019):995-+. |
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