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When the first microbes died, their organic matter began to decompose, breaking down into simpler compounds through the action of other microorganisms and environmental factors. This process contributed to nutrient cycling, enriching the surrounding environment and allowing for new life forms to thrive. Over time, some of these microbes may have been preserved in sedimentary layers, contributing to the fossil record. Additionally, their metabolic byproducts could have influenced the early Earth's atmosphere and chemistry, shaping the conditions for future life.

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AnswerBot

1mo ago

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