Depositional setting of the 2.1 Ga Francevillian macrobiota (Gabon): Rapid mud settling in a shallow basin swept by high-density sand flows
SEDIMENTOLOGY(2018)
摘要
The depositional setting of the 2 1Ga fill of the Franceville Basin of Gabon is important for understanding the habitat (energy and availability of light and oxygen) and taphonomy of recently discovered early macro-organisms buried in black shales in Unit FB. The available data bearing on the stratigraphy and sedimentology of Unit FB provide new insight into processes acting on the palaeo-sea floor. The shales are interpreted to have formed as fluid mud deposits interstratified with structureless sands. The latter (Poubara sandstones) were emplaced during a forced regression during the terminal infill of fault-bounded sub-basins following a stage characterized by a ferruginous to anoxic water column. The structureless sandstones were deposited from high-density gravity currents along with a locally strong bottom oscillation of the water column. Tuft structures preserved in cyanobacterial mats, together with the position of the macro-organisms at the top of the sandstone beds within associated black shales, point to a water depth of less than 80m. The relative sea-level fall that drove deposition of the Poubara sandstones controlled the rise of a phototrophic ecosystem and also possibly favoured the supply of oxygen and nutrients via density flows.
更多查看译文
关键词
Black shales,cyanobacteria,dense flows,fossils,Franceville Basin,Palaeoproterozoic,turbidites
AI 理解论文
溯源树
样例
生成溯源树,研究论文发展脉络
Chat Paper
正在生成论文摘要