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• W2892345308 abstract "Research Article| September 18, 2018 High-Paleolatitude Environmental Change During the Early To Middle Devonian: Insights from Emsian–Eifelian (Lower–Middle Devonian) Siliciclastic Depositional Systems of the Ceres Subgroup (Bokkeveld Group) of South Africa Cameron R. Penn-Clarke; Cameron R. Penn-Clarke 1Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, South Africa 2School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa Search for other works by this author on: GSW Google Scholar Bruce S. Rubidge; Bruce S. Rubidge 1Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, South Africa 2School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa Search for other works by this author on: GSW Google Scholar Zubair A. Jinnah Zubair A. Jinnah 2School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa Search for other works by this author on: GSW Google Scholar Author and Article Information Cameron R. Penn-Clarke 1Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, South Africa 2School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa Bruce S. Rubidge 1Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, South Africa 2School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa Zubair A. Jinnah 2School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa e-mail: cpennclarke@gmail.com Publisher: SEPM Society for Sedimentary Geology First Online: 18 Sep 2018 Online Issn: 1938-3681 Print Issn: 1527-1404 Copyright © 2018, SEPM (Society for Sedimentary Geology) Journal of Sedimentary Research (2018) 88 (9): 1040–1075. https://doi.org/10.2110/jsr.2018.53 Article history First Online: 18 Sep 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Cameron R. Penn-Clarke, Bruce S. Rubidge, Zubair A. Jinnah; High-Paleolatitude Environmental Change During the Early To Middle Devonian: Insights from Emsian–Eifelian (Lower–Middle Devonian) Siliciclastic Depositional Systems of the Ceres Subgroup (Bokkeveld Group) of South Africa. Journal of Sedimentary Research 2018;; 88 (9): 1040–1075. doi: https://doi.org/10.2110/jsr.2018.53 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Sedimentary Research Search Advanced Search Abstract Re-evaluation of the sedimentology of the Emsian–Eifelian part of the Bokkeveld Group, the Ceres Subgroup, in the Clanwilliam Sub-basin of South Africa indicates that sedimentation occurred in an array of paleoenvironments that are related to three broad siliciclastic depositional systems in a marginal- to shallow-marine setting. These are: storm- and wave-dominated shallow marine depositional systems; transgressive barrier-island–lagoon depositional systems; and wave-influenced deltaic depositional systems. Storm- and wave-dominated shallow marine depositional systems comprise offshore, offshore transition zone to distal lower shoreface, proximal lower shoreface, and upper shoreface–beach complex paleoenvironments. This depositional system is present in the Gydo–Gamka and Voorstehoek–Hex River Formation intervals. A transgressive barrier-island–lagoon depositional system is present in the lower to middle Tra-Tra Formation and comprises back-barrier tidal-flat and lagoon and transgressive beach-barrier paleoenvironments. The wave-influenced deltaic depositional system is restricted to the top Tra-Tra–Boplaas Formation interval and comprises prodelta to distal delta-front and proximal delta-front paleoenvironments. The presence of these depositional systems and their constituent paleoenvironments provides an alternative explanation to existing storm- and wave-dominated delta and mixed wave- and tide-dominated delta models. High levels of variability in depositional environments along this coastal system constrain the effects of major changes in Devonian terrestrial environments on marginal and shallow marine sedimentation at high paleolatitudes. Application of sequence stratigraphy to the Ceres Subgroup has enabled recognition of environmental and relative sea-level change at high paleolatitudes during the Emsian–Eifelian. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2892345308 created "2018-09-27" @default.
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• W2892345308 date "2018-09-18" @default.
• W2892345308 modified "2023-10-18" @default.
• W2892345308 title "High-Paleolatitude Environmental Change During the Early To Middle Devonian: Insights from Emsian–Eifelian (Lower–Middle Devonian) Siliciclastic Depositional Systems of the Ceres Subgroup (Bokkeveld Group) of South Africa" @default.
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• W2892345308 doi "https://doi.org/10.2110/jsr.2018.53" @default.
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