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adding to our understanding of the variety of life on the early Earth. While transmission electron microscopy of FIB sections is also relatively new, the research by Wacey et al. 61 illustrates that the ultrastructure of organic structures is drastically affected by silicification.Traditionally, efforts to assess biogenicity and syngeneity of natural residues in sedimentary rocks have targeted on geochemical signatures in kerogen and soluble extracts and/or morphological and chemical signatures of natural materials observable in thin section utilizing optical microscopy and techniques akin to Raman spectroscopy. This dissimilarity provides proof that the extracted

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