Phosphate oxygen isotopes constrain Mesoproterozoic marine temperatures and the paucity of phosphorite
文献类型：期刊论文
| 作者 | Ye, Yuntao; Wang, Xiaomei; Wang, Huajian; Fan, Haifeng2,7; Chen, Zhigang6; Guo, Qingjun5,7; Wang, Ziteng5,7; Wu, Chaodong; Canfield, Donald E.; Zhang, Shuichang4 |
| 刊名 | CHEMICAL GEOLOGY
 |
| 出版日期 | 2024-01-20 |
| 卷号 | 644页码:121831 |
| 关键词 | Apatite Phosphate oxygen isotopes Gaoyuzhuang formation Xiamaling formation North China |
| DOI | 10.1016/j.chemgeo.2023.121831 |
| 文献子类 | Article |
| 英文摘要 | Phosphorus (P) is an essential element for life, and the oceanic P cycle is closely coupled with the global carbon and oxygen cycles via the role of P as a limiting nutrient. Since P has only one stable isotope, tracking the P cycle through geological history is challenging. However, phosphate oxygen isotopes (delta 18Op) represent a valuable tool for deciphering various P-related reactions, such as intracellular P turnover and enzymatic P regeneration, and have been successfully applied to modern soils and marine sediments. The marine P cycle prior to the Neoproterozoic Era remains controversial due to the scarcity of phosphorite and large uncertainties in estimating seawater phosphate levels. Here, we present delta 18Op of carbonate fluorapatite (CFA) from the Mesoproterozoic Gaoyuzhuang and Xiamaling Formations in North China. Despite considerable uncertainties, the derived authigenic delta 18Op values are markedly lower than those from modern sites with similar depth and latitude, which imply a warmer climate during the Mesoproterozoic Era compared to the present day. Based on thermodynamic calculations of saturation state with respect to CFA, we suggest that the elevated temperatures could have hindered P authigenesis, partially accounting for the general absence of phosphorite in contemporaneous successions. |
| WOS关键词 | XIAMALING FORMATION ; NORTH ; EVOLUTION ; INSIGHTS ; APATITE ; CARBONATE ; SEDIMENTS ; SEAWATER ; PHOSPHOMONOESTERASES ; FRACTIONATION |
| WOS研究方向 | Geochemistry & Geophysics |
| WOS记录号 | WOS:001127309600001 |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/200931]  |
| 专题 | 资源利用与环境修复重点实验室_外文论文 |
| 作者单位 | 1.Canfield, Donald E.] Univ Southern Denmark, Dept Biol, Nordcee, DK-5230 Odense, Denmark 2.China Natl Petr Corp, Res Inst Petr Explorat & Dev, Key Lab Petr Geochem, Beijing 100083, Peoples R China 3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China 4.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Minist Educ, Beijing 100871, Peoples R China 5.Xiamen Univ, Coll Ocean & Earth Sci, Xiamen 361102, Peoples R China 6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 7.Chinese Acad Sci, State Key Lab Ore Deposit Geochem, Inst Geochem, Guiyang 550081, Peoples R China |
| 推荐引用方式 GB/T 7714 | Ye, Yuntao,Wang, Xiaomei,Wang, Huajian,et al. Phosphate oxygen isotopes constrain Mesoproterozoic marine temperatures and the paucity of phosphorite[J]. CHEMICAL GEOLOGY,2024,644:121831. |
| APA | Ye, Yuntao.,Wang, Xiaomei.,Wang, Huajian.,Fan, Haifeng.,Chen, Zhigang.,...&Zhang, Shuichang.(2024).Phosphate oxygen isotopes constrain Mesoproterozoic marine temperatures and the paucity of phosphorite.CHEMICAL GEOLOGY,644,121831. |
| MLA | Ye, Yuntao,et al."Phosphate oxygen isotopes constrain Mesoproterozoic marine temperatures and the paucity of phosphorite".CHEMICAL GEOLOGY 644(2024):121831. |
入库方式： OAI收割
来源：地理科学与资源研究所
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