Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India.
J Biosci. 2009 Nov;34(5):765-76. doi: 10.1007/s12038-009-0065-8.
The discovery of Precambrian microfossils in 1954 opened a new vista of investigations in the field of evolution of life. Although the Precambrian encompasses 87% of the earth's history, the pace of organismal evolution was quite slow. The life forms as categorised today in the three principal domains viz. the Bacteria, the Archaea and the Eucarya evolved during this period. In this paper, we review the advancements made in the Precambrian palaeontology and its contribution in understanding the evolution of life forms on earth. These studies have enriched the data base on the Precambrian life. Most of the direct evidence includes fossil prokaryotes, protists, advanced algal fossils, acritarchs, and the indirect evidence is represented by the stromatolites, trace fossils and geochemical fossils signatures. The Precambrian fossils are preserved in the form of compressions, impressions, and permineralized and biomineralized remains.
1954 年,前寒武纪微生物化石的发现为生命进化领域的研究开辟了新的视野。尽管前寒武纪涵盖了地球历史的 87%,但生物进化的速度相当缓慢。今天被归类为细菌、古菌和真核生物的生命形式就是在这一时期进化而来的。本文综述了前寒武纪古生物学的进展及其对理解地球上生命形式进化的贡献。这些研究丰富了前寒武纪生命的数据基础。大多数直接证据包括化石原核生物、原生生物、高级藻类化石、疑源类和间接证据则由叠层石、痕迹化石和地球化学化石特征代表。前寒武纪化石以压缩、印痕、矿化和生物矿化的形式保存下来。