The high-frequency sea-level change in the aftermath of the Marinoan snowball Earth: Evidence from the Doushantuo formation in the northern margin of the Yangtze Craton, South China

• Published in: Energy exploration & exploitation 2023-05, Vol.41 (3), p.941-972
• Main Authors: Qi, Kening, Kuang, Hongwei, Liu, Yongqing, Peng, Nan, Wang, Yuchong, Chen, Xiaoshuai, Cui, Mingming, Qiao, Dawei, Li, Shuangying, Chen, Tianhu, Wang, Zhixian, Zhong, Quan, Chen, Jinxin
• Format: Article
• Language: English
• Subjects: Carbonate rocks; Clastics; Deglaciation; Geologists; Glaciation; Glaciology; Lagoons; Sea level
• ISSN: 0144-5987; 2048-4054
• DOI: 10.1177/01445987221149221

The rapid rise of glacioeustatic change is the most extreme paleoenvironment alteration in the aftermath of Snowball Earth. Although geologists conducted a lot of multi-subdiscipline research on this issue previously, there still exists the potential room for further discussions of the process in detail. For decades, the practice proved that the Fischer plot is a simple and robust tool to illustrate the fluctuations of accommodation patterns v.s. cycle sets or strata depth which could be interpreted as relative sea-level changes. This research simulates the Fischer plot to unravel the sea-level change in the aftermath of Marinoan glaciation by measuring the lower Ediacaran Doushantuo Formation in Shennongjia, South China. The result shows that 131 fifth-order cycles and nine third-order cycles help us propose a completed second-order cycle variation of ice melting-forced sea-level change, i.e., (1) early high-frequency and slow to rapid stepwise rising, and (2) followed by a stable decrease in the latter. In addition, the vertical sedimentary facies of the lower Doushantuo Formation display, in ascending order, (1) intertidal carbonate rock, (2) subtidal clastics with turbidite, and (3) intertidal lagoon fine clastics, indicating the process of the relative waxing and waning of sea-level. Such interpretation of the Fischer plot and the sedimentary facies’ vertical evolution is beneficial for studying the high-frequency sea-level change and paleogeographic reconstruction of post-Marinoan deglaciation.