دورية أكاديمية
Lithium isotopic constraints on the evolution of continental clay mineral factory and marine oxygenation in the earliest Paleozoic Era.
| العنوان: | Lithium isotopic constraints on the evolution of continental clay mineral factory and marine oxygenation in the earliest Paleozoic Era. |
|---|---|
| المؤلفون: | Wei GY; School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China.; Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA., Zhao M; Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA.; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China., Sperling EA; Department of Earth and Planetary Sciences, Stanford University, Stanford, CA 94305, USA., Gaines RR; Geology Department, Pomona College, Claremont, CA 91711, USA., Kalderon-Asael B; Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA., Shen J; State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China., Li C; State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China.; Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications of Ministry of Natural Resources, Chengdu University of Technology, Chengdu 610059, China.; International Center for Sedimentary Geochemistry and Biogeochemistry Research, Chengdu University of Technology, Chengdu 610059, China., Zhang F; School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China., Li G; School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China., Zhou C; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing 210008, China., Cai C; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China., Chen D; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China., Xiao KQ; State Key Lab of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Shuangqing Rd. 18, 10085, Beijing, China.; University of Chinese Academy of Sciences, Beijing, 100049, China., Jiang L; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China., Ling HF; School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China., Planavsky NJ; Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA., Tarhan LG; Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA. |
| المصدر: | Science advances [Sci Adv] 2024 Mar 29; Vol. 10 (13), pp. eadk2152. Date of Electronic Publication: 2024 Mar 29. |
| نوع المنشور: | Journal Article |
| اللغة: | English |
| بيانات الدورية: | Publisher: American Association for the Advancement of Science Country of Publication: United States NLM ID: 101653440 Publication Model: Print-Electronic Cited Medium: Internet ISSN: 2375-2548 (Electronic) Linking ISSN: 23752548 NLM ISO Abbreviation: Sci Adv Subsets: PubMed not MEDLINE; MEDLINE |
| أسماء مطبوعة: | Original Publication: Washington, DC : American Association for the Advancement of Science, [2015]- |
| مستخلص: | The evolution of oxygen cycles on Earth's surface has been regulated by the balance between molecular oxygen production and consumption. The Neoproterozoic-Paleozoic transition likely marks the second rise in atmospheric and oceanic oxygen levels, widely attributed to enhanced burial of organic carbon. However, it remains disputed how marine organic carbon production and burial respond to global environmental changes and whether these feedbacks trigger global oxygenation during this interval. Here, we report a large lithium isotopic and elemental dataset from marine mudstones spanning the upper Neoproterozoic to middle Cambrian [~660 million years ago (Ma) to 500 Ma]. These data indicate a dramatic increase in continental clay formation after ~525 Ma, likely linked to secular changes in global climate and compositions of the continental crust. Using a global biogeochemical model, we suggest that intensified continental weathering and clay delivery to the oceans could have notably increased the burial efficiency of organic carbon and facilitated greater oxygen accumulation in the earliest Paleozoic oceans. |
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| تواريخ الأحداث: | Date Created: 20240329 Latest Revision: 20240426 |
| رمز التحديث: | 20240426 |
| مُعرف محوري في PubMed: | PMC10980266 |
| DOI: | 10.1126/sciadv.adk2152 |
| PMID: | 38552018 |
| قاعدة البيانات: | MEDLINE |
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