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DOI | 10.1016/j.palaeo.2019.109367 |
Long-term evolution of terrestrial inputs from the Ediacaran to early Cambrian: Clues from Nd isotopes in shallow-marine carbonates; South China | |
Wei G.-Y.; Ling H.-F.; Shields G.A.; Chen T.; Lechte M.; Chen X.; Qiu C.; Lei H.; Zhu M. | |
发表日期 | 2019 |
ISSN | 0031-0182 |
卷号 | 535 |
英文摘要 | The emergence and radiation of metazoans have been widely attributed to a progressively more oxidizing surface environment through the Ediacaran–Cambrian transition interval. However, the root causes for atmospheric and oceanic oxygenation are still disputed. Long-term tectonic changes could possibly have led to atmospheric oxygenation but geochemical evidence for this linkage remains elusive. In this study, we analyzed the radiogenic Nd isotopic compositions (εNd) of shallow-marine carbonates from South China in order to track secular variations in terrestrial inputs from Ediacaran to early Cambrian time. Compared with most other geochemical indices, the Nd isotope system in carbonates is less susceptible to early diagenetic exchange and can thus act as a robust proxy for continental materials undergoing weathering. We interpret an abrupt excursion to lower εNd values during the middle Ediacaran as due to rapid exchange of different water masses. However, the more gradual trend towards lower Nd isotope values from the Ediacaran to early Cambrian, accompanied by increasing 87Sr/86Sr ratios of the studied carbonates, likely indicates the enhanced weathering of old continental rock following the assembly of Gondwana. Increased net accumulation of atmospheric oxygen as a result of enhanced organic carbon burial may have benefited from intense continental denudation. © 2019 Elsevier B.V. |
英文关键词 | Animal radiation; Continental denudation; Neodymium isotope record; Neoproterozoic oxygenation event; Tectonic activity |
语种 | 英语 |
scopus关键词 | adaptive radiation; biostratigraphy; Cambrian; carbonate; denudation; Ediacaran; emergence; Gondwana; metazoan; neodymium isotope; organic carbon; oxygenation; shallow water; tectonic setting; Animalia; Metazoa |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/150770 |
作者单位 | State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, School of Earth Sciences and Engineering, Nanjing University, 163 Xianlin Avenue, Nanjing, 210023, China; Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, United Kingdom; Department of Earth and Planetary Sciences, McGill University, 3450 University St., Montreal, QC H3A 0E8, Canada; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Nanjing, 210008, China |
推荐引用方式 GB/T 7714 | Wei G.-Y.,Ling H.-F.,Shields G.A.,et al. Long-term evolution of terrestrial inputs from the Ediacaran to early Cambrian: Clues from Nd isotopes in shallow-marine carbonates; South China[J],2019,535. |
APA | Wei G.-Y..,Ling H.-F..,Shields G.A..,Chen T..,Lechte M..,...&Zhu M..(2019).Long-term evolution of terrestrial inputs from the Ediacaran to early Cambrian: Clues from Nd isotopes in shallow-marine carbonates; South China.Palaeogeography, Palaeoclimatology, Palaeoecology,535. |
MLA | Wei G.-Y.,et al."Long-term evolution of terrestrial inputs from the Ediacaran to early Cambrian: Clues from Nd isotopes in shallow-marine carbonates; South China".Palaeogeography, Palaeoclimatology, Palaeoecology 535(2019). |
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