首页|大洋中溶解态镉与磷酸盐的相关关系及关键控制过程

大洋中溶解态镉与磷酸盐的相关关系及关键控制过程

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大洋中溶解态锅(Cd)与磷酸盐(PO4)存在相关关系,常被用来反演古海洋生产力的变化.基于国际海洋研究计划"痕量元素及同位素的海洋生物地球化学研究"(GEOTRACES)2023年公布的数据集产品IDP2021v2以及近40年发表的相关文献,综述了大洋Cd-PO4线性相关关系的提出、不同海盆Cd-PO4关系汇总以及影响其相关性因素的最新研究进展.大洋Cd-PO4线性相关关系受多种因素影响,总体呈现双线性相关的特征.不同水深影响其相关关系的关键海洋生物地球化学过程不同:上层水(<200 m)主要为浮游植物的吸收,中层水(500-1 000 m)为颗粒态Cd与磷酸盐的再矿化与水团混合,深层水(>1 500m)则主要为水团混合.其中,起源于南大洋的南极中层水与南极深层水向北的运移对全球大洋中深层水的Cd-PO4值的分布具有重要意义.
Correlation Between Dissolved Cadmium and Phosphate and Its Key Controlling Processes in the Open Ocean
The correlation between dissolved cadmium(Cd)and phosphate(PO4)in the ocean is often used to reconstruct paleoproductivity.Based on the intermediate data product IDP2021v2 released by GEOTRACES(an international study of the marine biogeochemical cycles of trace elements and isotopes)in 2023 and related literature published in the past 40 years,this paper reviews the latest research progress regarding the correlation between Cd and PO4 in the ocean.It summarizes the Cd-PO4 relationship in various ocean basins and identifies their major influencing factors.The controlling factors affecting the oceanic Cd-PO4 relationship differ from surface to deep water and generally exhibit a bilinear correlation.In this study,the key processes controlling the correlation in different water layers are summarized,including the absorption of phytoplankton in the upper water(<200 m),remineralization of particulate Cd and P,mixing of water masses in the intermediate water mass(500~1 000 m),and mixing of different water masses in deep water(>1 500 m).The northward migration of Antarctic intermediate and bottom water from the Southern Ocean is vital in shaping the global ocean Cd-PO4 relationship.

Cd to PO4 ratioBiogeochemical processesWater mass mixingGEOTRACES

张瀚、杨一超、任景玲

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中国海洋大学海洋化学理论与工程技术教育部重点实验室,山东 青岛 266100

镉磷比 生物地球化学过程 水团混合 GEOTRACES

国家自然科学基金项目山东省"泰山学者工程"专项

42176042

2024

地球科学进展
中国科学院资源环境科学信息中心 国家自然科学基金委员会地球科学部 中国科学院资源环境科学与技术局

地球科学进展

CSTPCD北大核心
影响因子:2.045
ISSN:1001-8166
年,卷(期):2024.39(2)
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