Lopuchin A S
Orig Life. 1975 Jan-Apr;6(1-2):45-57.
Spheroidal microfossils mainly 20 to 100 mug in diameter and exhibiting granular surface textures have been recovered from Early Precambrian rocks by applying a new method of water separation in combination with thin chemical preparation. In contrast to the Acritarcha, these microfossils are characterized by a relatively low specific weight (close to one) and considerable fragility due to impregnation by mineral matter. They occur in Archean sediments of Hindustan, in rocks of the Baltic and Aldan Shields with ages of 3.0 to 3.5 billion (10-9) years, and in Proterozoic deposits in many regions of Euro-Asia. They commonly occur in great number in Precambrian sediments of West Africa, Australia and North America. These forms are here regarded as Menneria Lopuchin and are considered to be blue-green algae. Menneria resembles alga-like forms reported by Engel, Nagy and their co-workers from the Onverwacht Series and microfossils reported by Schopf and Barghoorn from the Fig Tree Series, both of the Swaziland System of southern Africa. In addition to spheroidal microfossils, ribbon-like and filiform microstructures are here reported from Archean deposits. The biogenic structures here described from the Early Precambrian of Euro-Asia are considered to have been photosynthetic and planktonic. Their progressive evolution, intensive production of organic matter, and biogeochemical role in concentration of rare elements is discussed.
通过采用一种新的水分离方法并结合精细的化学制备,已从早前寒武纪岩石中发现了主要直径为20至100微克且表面呈现颗粒纹理的球状微化石。与疑源类不同,这些微化石的特点是比重相对较低(接近1),且由于矿物质的浸染而相当脆弱。它们出现在印度斯坦的太古代沉积物中、波罗的海和阿尔丹地盾年龄为30亿至35亿(10 - 9)年的岩石中,以及欧亚大陆许多地区的元古代沉积物中。它们通常大量出现在西非、澳大利亚和北美的前寒武纪沉积物中。这些形态在这里被视为门氏藻属(Menneria Lopuchin),并被认为是蓝藻。门氏藻类似于恩格尔、纳吉及其同事从南非斯威士兰系翁弗瓦赫特统中报道的藻状形态,以及肖普夫和巴格霍恩从同一统的无花果统中报道的微化石。除了球状微化石外,这里还报道了来自太古代沉积物的带状和丝状微观结构。这里描述的欧亚大陆早元古代的生物成因结构被认为具有光合和浮游特性。文中还讨论了它们的渐进演化、有机质的大量生产以及在稀有元素富集方面的生物地球化学作用。