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DOI | 10.1038/s41561-020-0558-5 |
Palaeoproterozoic oxygenated oceans following the Lomagundi-Jatuli Event | |
Mand, Kaarel1,2; Lalonde, Stefan V.3; Robbins, Leslie J.4; Thoby, Marie3; Paiste, Kart2,5; Kreitsmann, Timmu2; Paiste, Paarn2; Reinhard, Christopher T.6,7; Romashkin, Alexandr E.8; Planavsky, Noah J.4,7; Kirsimae, Kalle2; Lepland, Aivo2,5,9,10; Konhauser, Kurt O.1 | |
2020-03-16 | |
发表期刊 | NATURE GEOSCIENCE |
ISSN | 1752-0894 |
EISSN | 1752-0908 |
出版年 | 2020 |
卷号 | 13期号:4页码:302-+ |
文章类型 | Article |
语种 | 英语 |
国家 | Canada; Estonia; France; USA; Norway; Russia |
英文摘要 | The oceans probably remained well-oxygenated for millions of years after the Palaeoproterozoic Lomagundi-Jatuli Event, according to high concentrations and isotope signatures of redox-sensitive metals in the 2-billion-year-old Zaonega Formation, Russia. The approximately 2,220-2,060 million years old Lomagundi-Jatuli Event was the longest positive carbon isotope excursion in Earth history and is traditionally interpreted to reflect an increased organic carbon burial and a transient rise in atmospheric O-2. However, it is widely held that O-2 levels collapsed for more than a billion years after this. Here we show that black shales postdating the Lomagundi-Jatuli Event from the approximately 2,000 million years old Zaonega Formation contain the highest redox-sensitive trace metal concentrations reported in sediments deposited before the Neoproterozoic (maximum concentrations of Mo = 1,009 mu g g(-1), U = 238 mu g g(-1) and Re = 516 ng g(-1)). This unit also contains the most positive Precambrian shale U isotope values measured to date (maximum U-238/U-235 ratio of 0.79 parts per thousand), which provides novel evidence that there was a transition to modern-like biogeochemical cycling during the Palaeoproterozoic. Although these records do not preclude a return to anoxia during the Palaeoproterozoic, they uniquely suggest that the oceans remained well-oxygenated millions of years after the termination of the Lomagundi-Jatuli Event. |
领域 | 地球科学 ; 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000519843400001 |
WOS关键词 | GREAT OXIDATION ; ZAONEGA FORMATION ; MOLYBDENUM ; URANIUM ; RECORD ; GEOCHEMISTRY ; ISOTOPES ; RISE ; GA ; PRESERVATION |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/249298 |
专题 | 地球科学 气候变化 |
作者单位 | 1.Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB, Canada; 2.Univ Tartu, Dept Geol, Tartu, Estonia; 3.European Inst Marine Studies, CNRS, UMR6538, Lab Geosci Ocean, Plouzane, France; 4.Yale Univ, Dept Geol & Geophys, New Haven, CT USA; 5.UiT Arctic Univ Norway, Dept Geosci, CAGE Ctr Arctic Gas Hydrate Environm & Climate, Tromso, Norway; 6.Georgia Tech, Sch Earth & Atmospher Sci, Atlanta, GA USA; 7.Univ Calif Riverside, NASA, Astrobiol Inst, Alternat Earths Team, Riverside, CA 92521 USA; 8.Karelian Sci Ctr, Inst Geol, Petrozavodsk, Russia; 9.Geol Survey Norway NGU, Trondheim, Norway; 10.Tallinn Univ Technol, Dept Geol, Tallinn, Estonia |
推荐引用方式 GB/T 7714 | Mand, Kaarel,Lalonde, Stefan V.,Robbins, Leslie J.,et al. Palaeoproterozoic oxygenated oceans following the Lomagundi-Jatuli Event[J]. NATURE GEOSCIENCE,2020,13(4):302-+. |
APA | Mand, Kaarel.,Lalonde, Stefan V..,Robbins, Leslie J..,Thoby, Marie.,Paiste, Kart.,...&Konhauser, Kurt O..(2020).Palaeoproterozoic oxygenated oceans following the Lomagundi-Jatuli Event.NATURE GEOSCIENCE,13(4),302-+. |
MLA | Mand, Kaarel,et al."Palaeoproterozoic oxygenated oceans following the Lomagundi-Jatuli Event".NATURE GEOSCIENCE 13.4(2020):302-+. |
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