Three-dimensional structure, crystallography, and magnetism of giant magnetofossils
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Abstract
Biomineralization has existed on Earth for billions of years, documenting life evolution history and major geological events. However, determining the origins of putative biogenic minerals remains a persistent challenge. A prime example is the micrometer-sized fossil magnetite crystals (giant magnetofossils) discovered in global marine sediments, dating from the present to 97 Ma ago. Their origin remains unclear because their shape and size are different from any known nanometer-sized magnetite produced by magnetotactic bacteria. Here, we present three-dimensional (3D) reconstructions of giant magnetofossils with nanometer resolution, and report two new morphologies of giant magnetofossils. By identifying diagnostic 3D morphological, crystallographic, and micromagnetic features, our results provide key identification criteria for giant magnetofossils and suggest a potential biologically controlled mineralization origin. This study provides a comprehensive 3D characterisation of giant magnetofossils, aiding the search for ancient microbial activities on Earth and extraterrestrial bodies.
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Acknowledgements: This study utilized samples from the International Ocean Discovery Program (IODP). We acknowledge Thermo Fisher Scientific for providing access to and supporting the cryo-EM facilities at the Cambridge Pharmaceutical Consortium. We acknowledge Simon M. Fairclough for assistance in cryogenic electron tomography, Xu Tang for assistance in electron diffraction analysis using TEM at the IGGCAS, Hassan A. Sheikh, George R. Lewis, and Bassel Arnaout for assistance in tomography data processing, and Sergio Valencia for discussions on micromagnetic simulation results. L.C. acknowledges support from the National Natural Science Foundation of China grant 42330204. L.C. and R.J.H. also thank the funding from the Royal Society Newton Advanced Fellowship (NAF\R1\201096). W.W. acknowledge Natural Environment Research Council (NERC) for their financial support (NE/Z000068/1, NE/W006707/1 and NE/V001388/1). We thank Jinhua Li and an anonymous reviewer for their valuable suggestions and the editors for their efficient handling of our manuscript.
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2662-4435
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Royal Society (NAF\R1\201096)

