7. Layer After Layer
Finely layered geological deposits called stromatolites were common deposits on Early Earth. Many stromatolites have been interpreted to be of microbiological origin (biotic), while others may have been produced by non-biological (abiotic) processes. Can you hypothesize about the types of abiotic processes that may be capable of forming a stromatolite? How might you distinguish them from fine layers created by biotic processes?
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