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- W2143536419 abstract "The electron microprobe allows elemental abundances to be mapped at the microm scale, but until now high resolution mapping of light elements has been challenging. Modifications of electron microprobe procedure permit fine-scale mapping of carbon. When applied to permineralized fossils, this technique allows simultaneous mapping of organic material, major matrix-forming elements, and trace elements with microm-scale resolution. The resulting data make it possible to test taphonomic hypotheses for the formation of anatomically preserved silicified fossils, including the role of trace elements in the initiation of silica precipitation and in the prevention of organic degradation. The technique allows one to understand the localization of preserved organic matter before undertaking destructive chemical analyses and, because it is nondestructive, offers a potentially important tool for astrobiological investigations of samples returned from Mars or other solar system bodies." @default.
- W2143536419 created "2016-06-24" @default.
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- W2143536419 date "2001-05-22" @default.
- W2143536419 modified "2023-10-10" @default.
- W2143536419 title "Nondestructive, <i>in situ</i> , cellular-scale mapping of elemental abundances including organic carbon in permineralized fossils" @default.
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- W2143536419 doi "https://doi.org/10.1073/pnas.101130598" @default.
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