气候变化领域集成服务门户(CCPortal): Trace-Elemental and Petrographic Constraints on the Severity Of Hydrographic Restriction in the Silled Midland Basin During the Late Paleozoic Ice Age

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DOI	10.1130/B35336.1
	Trace-Elemental and Petrographic Constraints on the Severity Of Hydrographic Restriction in the Silled Midland Basin During the Late Paleozoic Ice Age
	Peng J.; Fu Q.; Larson T.E.; Janson X.
发表日期	2020
ISSN	167606
起始页码	57
结束页码	73
卷号	133
英文摘要	Enrichment of redox-sensitive trace elements in ancient marine shales is conventionally believed to be controlled by marine benthic redox conditions, whereas the influence of hydrographic conditions on trace element enrichment pattern has been rarely considered. Here, we present newly obtained data sets from the Upper Pennsylvanian organicrich Cline Shale in the Midland Basin, Texas, to illustrate the influence of hydrographic circulation on the trace-element enrichment pattern and the stratigraphic record of mudrocks. Various lithofacies, including siliceous mudrocks, argillaceous mudrocks, skeletal-bearing argillaceous mudrocks, calcareous mudrocks, and wackestone, are identified in the Cline Shale. Significant changes in the trace-element enrichment pattern, mineral composition, texture of framboidal pyrite, and other bulk geochemical parameters in different lithofacies are interpreted to have been caused by high-amplitude and high-frequency glacio-eustatic sea-level oscillations in the silled Midland Basin during the late Paleozoic ice age. Specifically, glacio-eustatic sea-level falls generally resulted in the severe isolation of the Midland Basin from the Panthalassic Ocean, highly restricted hydrographic circulation, long deep-water renewal time, euxinic bottom-water conditions, depleted seawater Mo (molybdenum) in the silled basin, and low sediment Mo/TOC (total organic carbon), coupled with significant extrabasinal detrital quartz input, forming siliceous mudrocks. Enhanced phosphorus cycling and excellent preservation conditions are considered to be responsible for the high TOC observed in siliceous mudrocks. In contrast, glacio-eustatic sea-level rises substantially enhanced water exchange between the basin and the Panthalassic Ocean, created overall suboxic to anoxic bottom-water conditions, resupplied seawater Mo, elevated sediment Mo/TOC, and increased platform carbonate production in the basin, forming calcareous mudrocks and wackestone. © 2020 Geological Society of America
语种	英语
来源期刊	Bulletin of the Geological Society of America
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/184855
作者单位	Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas 78713, United States
推荐引用方式 GB/T 7714	Peng J.,Fu Q.,Larson T.E.,et al. Trace-Elemental and Petrographic Constraints on the Severity Of Hydrographic Restriction in the Silled Midland Basin During the Late Paleozoic Ice Age[J],2020,133.
APA	Peng J.,Fu Q.,Larson T.E.,&Janson X..(2020).Trace-Elemental and Petrographic Constraints on the Severity Of Hydrographic Restriction in the Silled Midland Basin During the Late Paleozoic Ice Age.Bulletin of the Geological Society of America,133.
MLA	Peng J.,et al."Trace-Elemental and Petrographic Constraints on the Severity Of Hydrographic Restriction in the Silled Midland Basin During the Late Paleozoic Ice Age".Bulletin of the Geological Society of America 133(2020).