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Neoproterozoic Nafun Group Sediments from Oman Affected by an Active Continental Margin

Yue, Liang; Vandeginste, Veerle

Neoproterozoic Nafun Group Sediments from Oman Affected by an Active Continental Margin Thumbnail


Authors

Liang Yue

Veerle Vandeginste



Abstract

The Neoproterozoic era is a time of major environmental change in Earth history. The Ediacaran period (635–541 Ma), the uppermost division of Precambrian time, is characterized by the remarkable Shuram excursion (largest C isotope negative excursion), a deep ocean water oxidation event, and Ediacaran biota. The Nafun Group of Oman provides a well-preserved and mostly continuous section of an Ediacaran succession. Based on geochemical data from the Nafun Group, the Shuram excursion (SE) and deep ocean oxidation hypotheses were proposed. Now, we sampled this section at high stratigraphic resolution, and present here the petrographical and geochemical analysis of the Khufai, Shuram and Buah Formations. The major and trace element analysis of shales from the Shuram Formation indicates that northern Oman was an active continental margin environment in Neoproterozoic times. The provenance of the Shuram Formation was primarily mafic and intermediate igneous rocks. With the unsteady tectonic setting, the development of the Nafun Group was influenced by hydrothermal supply and volcaniclastic input. Based on the V/Cr and U/Th ratio of the samples from the Nafun Group, our study reveals the transition of the ocean water redox environment, which is connected to the rise and fall of the Ediacaran biota. Our study constrains the tectonic setting of northern Oman and the petrography and geochemical data from the Nafun Group for the hydrothermal and volcaniclastic supply. Thus, our study acknowledges more factors for the explanation of the Ediacaran conundrums.

Citation

Yue, L., & Vandeginste, V. (2020). Neoproterozoic Nafun Group Sediments from Oman Affected by an Active Continental Margin. Minerals, 10(6), Article 511. https://doi.org/10.3390/min10060511

Journal Article Type Article
Acceptance Date May 29, 2020
Online Publication Date May 31, 2020
Publication Date May 31, 2020
Deposit Date Aug 5, 2020
Publicly Available Date Aug 6, 2020
Journal Minerals
Electronic ISSN 2075-163X
Publisher MDPI
Peer Reviewed Peer Reviewed
Volume 10
Issue 6
Article Number 511
DOI https://doi.org/10.3390/min10060511
Public URL https://nottingham-repository.worktribe.com/output/4646152
Publisher URL https://www.mdpi.com/2075-163X/10/6/511

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