Department of Geological Sciences, Preston Cloud Research Laboratory, University of California, 93106, Santa Barbara, CA, USA.
Photosynth Res. 1992 Aug;33(2):75-89. doi: 10.1007/BF00039172.
There is diverse, yet controversial fossil evidence for the existence of photosynthesis 3500 million years ago. Among the most persuasive evidence is the stromatolites described from low grade metasedimentary rocks in Western Australia and South Africa. Based on the understanding of the paleobiology of stromatolites and using pertinent fossil and Recent analogs, these Early Archean stromatolites suggest that phototrophs evolved by 3500 million years ago. The evidence allows further interpretation that cyanobacteria were involved. Besides stromatolites, microbial and chemical fossils are also known from the same rock units. Some microfossils morphologically resemble cyanobacteria and thus complement the adduced cyanobacterial involvement in stromatolite construction. If cyanobacteria had evolved by 3500 million years ago, this would indicate that nearly all prokaryotic phyla had already evolved and that prokaryotes diversified rapidly on the early Earth.
35 亿年前就存在光合作用,这方面的化石证据虽然多样,但却颇具争议。其中最有说服力的证据是在澳大利亚西部和南非的低变质沉积岩中描述的叠层石。根据对叠层石古生物学的理解,并利用相关的化石和现代类似物,这些早太古代的叠层石表明,光合生物在 35 亿年前就已经进化了。这些证据进一步表明,蓝细菌也参与其中。除了叠层石,这些岩石单元中还存在微生物和化学化石。一些微观化石在形态上类似于蓝细菌,因此补充了蓝细菌在叠层石建造中的参与。如果蓝细菌在 35 亿年前就已经进化,这将表明几乎所有的原核生物门都已经进化,原核生物在早期地球上迅速多样化。