Arid
DOI10.1016/j.marpetgeo.2021.105179
Geochemical characteristics and geological significance of humid climate events in the Middle-Late Triassic (Ladinian-Carnian) of the Ordos Basin, central China
Zhang, Kun; Liu, Rong; Liu, Zhaojun; Li, Li
通讯作者Liu, R (corresponding author), Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China.
来源期刊MARINE AND PETROLEUM GEOLOGY
ISSN0264-8172
EISSN1873-4073
出版年2021
卷号131
英文摘要Many Middle-Late Triassic (Ladinian-Carnian) global and local humid climate events that impacted on global palaeontological evolution and mineral distribution have been recorded in the rocks. The lacustrine sedimentary sequence of the Yanchang Formation in the Ordos Basin in the northeastern Tethys region may be an important example of control by global humid climate events. As revealed by an established chronostratigraphic framework and the study of organic carbon isotopes, elemental geochemistry and clay minerals, the Chang 7 Member of the Yanchang Formation was deposited in the Ladinian-Carnian, and the high total organic carbon (TOC) and total nitrogen (TN) contents indicate the high productivity of the ancient lake. The observed elemental ratios (Sr/Cu, Rb/Sr and Al2O3/MgO) and high contents of mixed-layer smectite indicate humid climate events in the Chang 73 and Chang 71 members. The increases in weathering degree, surface temperature and terrigenous clastic material input indicate enhancement of the hydrological cycle driven by a warm-humid climate. The arid-wet transitions, the negative excursions of the studied organic carbon isotope and the temperature fluctuations during the deposition of the Chang 73 and Chang 71 members of the Yanchang Formation are consistent with the Carnian humid event (CHE) and Ladinian-Carnian humid interval (L-CHI). The palaeontological diversity and the development of organic shales, turbidity currents and sandy debris flows in the Chang 7 Member may represent the continental sedimentary responses to coeval global humid climate events. The isochronous eruptions of volcanoes around the Ordos Basin may have intensified the global greenhouse effect and become an important factor driving the multi-stage humid climate events in the Ordos Basin.
英文关键词Organic carbon isotopes Elemental geochemistry Climate humid event Continental response Ladinian-carnian Ordos basin
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000671183700001
WOS关键词SEDIMENTARY ORGANIC-MATTER ; BLACK SHALE DEPOSITION ; CHANG 7 MEMBER ; YANCHANG FORMATION ; CARBON-ISOTOPE ; PLUVIAL EPISODE ; LAKE-SEDIMENTS ; YANGTZE BLOCK ; SOUTHERN ALPS ; APPALACHIAN BASIN
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/368501
作者单位[Zhang, Kun; Liu, Rong; Liu, Zhaojun] Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China; [Zhang, Kun; Liu, Rong; Liu, Zhaojun] Key Lab Oil Shale & Coexistent Energy Minerals Ji, Changchun 130061, Peoples R China; [Liu, Rong; Liu, Zhaojun] Jilin Univ, Minist Educ, Key Lab Evolut Life & Environm Northeast Asia, Changchun 130026, Peoples R China; [Li, Li] Macquarie Univ, MQ Marine Res Ctr, Dept Earth & Planetary Sci, Sydney, NSW 2109, Australia
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Zhang, Kun,Liu, Rong,Liu, Zhaojun,et al. Geochemical characteristics and geological significance of humid climate events in the Middle-Late Triassic (Ladinian-Carnian) of the Ordos Basin, central China[J],2021,131.
APA Zhang, Kun,Liu, Rong,Liu, Zhaojun,&Li, Li.(2021).Geochemical characteristics and geological significance of humid climate events in the Middle-Late Triassic (Ladinian-Carnian) of the Ordos Basin, central China.MARINE AND PETROLEUM GEOLOGY,131.
MLA Zhang, Kun,et al."Geochemical characteristics and geological significance of humid climate events in the Middle-Late Triassic (Ladinian-Carnian) of the Ordos Basin, central China".MARINE AND PETROLEUM GEOLOGY 131(2021).
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