Microfossils with tail-like structures in the 3.4 Gyr old Strelley Pool Formation

نویسندگان

چکیده

Some of the oldest traces for planktonic lifestyle have been reported in ca. 3.4 billion years old silicified sediments from Strelley Pool Formation Western Australia. Observation flange appendages suggests that Archean life motility was passive and driven by drifting microorganisms their surrounding environment. Until now, active are 2.1 old. Whether or not already existed during eon remains an open question. In this study, we report discovery new microfossils exhibiting a tail-like structure isolated Formation. Exhibiting Raman spectra typically observed organic-walled Formation, these syngenetic with host rock. Composed carbon, nitrogen, and, one specimen, phosphorus, some also exhibit significant level aliphatic amide moieties supporting biogenicity. addition, appendage sharing similar morphological features locomotory organelles modern such as archaella, flagella, cilia. This likely provided them movement capabilities. If correct, ability to move, were capable escaping harsh environments and/or colonizing ecological niches early ago.

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ژورنال

عنوان ژورنال: Precambrian Research

سال: 2021

ISSN: ['1872-7433', '0301-9268']

DOI: https://doi.org/10.1016/j.precamres.2021.106187