叠层石
元古代
无氧光合作用
微生物垫
前寒武纪
地质学
古生物学
地质记录
太古宙
雪球土
早期地球
沉积构造
岩相学
地球科学
生态学
相
生物
碳酸盐
化学
冰期
构造盆地
蓝藻
细菌
光养
有机化学
构造学
作者
Tanja Bosak,Andrew H. Knoll,Alexander P. Petroff
标识
DOI:10.1146/annurev-earth-042711-105327
摘要
Stromatolites document microbial interactions with sediments and flowing water throughout recorded Earth history and have the potential to illuminate the long-term history of life and environments. Modern stromatolites, however, provide analogs to only a small subset of the structures preserved in Archean and Proterozoic carbonates. Thus, interpretations of secular trends in the shapes and textures of ancient columnar stromatolites require nonuniformitarian, scale-dependent models of microbial responses to nutrient availability, seawater chemistry, influx of sediment grains, shear, and burial. Models that integrate stromatolite scales, macroscopic organization, and shapes could also help test the biogenicity of the oldest stromatolites and other structures whose petrographic fabrics do not preserve direct evidence of microbial activity. An improved understanding of stromatolite morphogenesis in the presence of oxygenic and anoxygenic microbial mats may illuminate the diversity of microbial metabolisms that contributed to stromatolite growth in early oceans.
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