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Atomic force microscopy of Precambrian microscopic fossils
André Kempe1, J William Schopf, Wladyslaw Altermann
1Institut für Kristallographie und Angewandte Mineralogie, Center for NanoScience, Ludwig-Maximilians-Universität München, Theresienstrasse 41, D-80333 Münich, Germany.
Summary
Atomic force microscopy revealed Precambrian microfossils are made of stacked organic platelets. This technique helps study ancient organic matter and fossil preservation.
Area of Science:
- Paleontology
- Geochemistry
- Materials Science
Background:
- Organic-walled microfossils, such as sphaeromorph acritarchs, offer insights into Precambrian life.
- Understanding their fine structure is crucial for paleobiological and geochemical interpretations.
- Previous studies lacked high-resolution nanoscale imaging of these ancient organic structures.
Purpose of the Study:
- To analyze the submicron-scale structure of 650-million-year-old acritarch fossils.
- To determine the composition and arrangement of organic material within fossil walls.
- To explore the utility of advanced microscopy and spectroscopy for fossil analysis.
Main Methods:
- Application of Atomic Force Microscopy (AFM) for high-resolution imaging of fossil surfaces.
- Utilizing laser-Raman spectroscopy for in-situ chemical analysis of individual microfossil specimens.
- Correlating AFM topographical data with spectroscopic chemical signatures.
Main Results:
- AFM imaging revealed fossil walls composed of stacked, angular platelets approximately 200 nm in size.
- Laser-Raman spectroscopy confirmed these platelets are made of polycyclic aromatic kerogen.
- The study successfully elucidated the nanoscale architecture of the acritarchs' organic walls.
Conclusions:
- AFM and laser-Raman spectroscopy are effective tools for detailed microfossil analysis.
- The findings provide insights into the geochemical maturation and preservation mechanisms of ancient organic matter.
- This methodology can aid in distinguishing genuine microfossils from pseudofossils.