Science. 1968 Sep 6;161(3845):1005-8. doi: 10.1126/science.161.3845.1005.
Spheroidal and cupshaped, carbonaceous alga-like bodies, as well as filamentous structures and amorphous carbonaceous matter occur in sedimentary rocks of the Onverwacht Series (Swaziland System) in South Africa. The Onverwacht sediments are older than 3.2 eons, and they are probably the oldest, littlealtered sedimentary rocks on Earth. The basal Onverwacht sediments lie approximately 10,000 meters stratigraphically below the Fig Tree sedimentary rocks, from which similar organic microstructures have been interpreted as alga-like microfossils. The Onverwacht spheroids and filaments are best preserved in black, carbonrich cherts and siliceous argillites interlayered with thick sequences of lavas. These lifelike forms and the associated carbonaceous substances are probably biological in origin. If so, the origins of unicellular life on Earth are buried in older rocks now obliterated by igneous and metamorphic events.
南非翁维瓦特系列(斯威士兰系)沉积岩中存在球粒状和杯状、碳质藻样体、丝状结构和无定形碳质物质。翁维瓦特沉积物的年龄超过 32 亿年,它们可能是地球上最古老、几乎没有变化的沉积岩。底层的翁维瓦特沉积物在大约 10000 米的地层中位于 Fig Tree 沉积岩之下,从这些沉积物中也解读出了类似的有机微观结构,被解释为藻样微化石。翁维瓦特的球粒和丝状体在富含碳的黑色燧石和硅质粘土中保存得最好,这些燧石和硅质粘土与厚层熔岩互层。这些栩栩如生的形态和相关的碳质物质可能具有生物起源。如果是这样,地球上单细胞生命的起源就埋藏在现在已被火成岩和变质作用摧毁的古老岩石中。