71 / 2025-03-31 09:47:19
Advances in Atom Probe Tomography for Biological Apatite: Techniques and Findings
APT,Apatite,Dental enamel,Conodont
摘要待审
Fan Gao / Institute of Geology and Geophysics, Chinese Academy of Sciences
Qiu-Li Li / Institute of Geology and Geophysics, Chinese Academy of Sciences
Biominerals serve as critical archives for deciphering life-environment interactions throughout geological history (Pérez-Huerta et al., 2018). As exemplary products of biologically controlled mineralization, the structural-compositional signatures of biological apatite preserve key records of metabolic processes. However, geological alteration often obscures these biogenic features, posing significant challenges for identifying the primary biological signals in paleontological and archaeological materials. While nanoscale heterogeneity in mineral structure and composition may retain primary biogenic information, resolving such features requires cutting-edge analytical methodologies. Atom probe tomography (APT), currently the highest-resolution characterization technique, offers unprecedented three-dimensional elemental mapping at sub-nanometer resolution, demonstrating exceptional potential for decoding structural-compositional information within biominerals.

Our APT comparative analysis of modern human enamel and Qin Dynasty ancient enamel (~2200 BP) reveals distinct mineralization patterns. Modern enamel exhibits Mg-Na-F enrichment in hydroxyapatite crystal core with depletion in shell and slight enrichment at intergranular phase, consistent with previous findings (DeRocher et al., 2020). In contrast, Qin specimens retain Mg-rich cores but display inverted Na-F distribution patterns: depletion in core and intergranular phase regions versus significant enrichment in shell, suggesting dietary influences on mechanical property evolution. Further investigation of Early Triassic conodont phosphate fossils reveals residual organic components (C-N co-enrichment) despite extensive biogenic degradation and diagenetic alteration. Most regions show dispersed C-N distribution, documenting dynamic organic degradation processes (Gao et al., 2024).



References

Pérez-Huerta A., Coronado I., Hegna T. A., 2018. Understanding biomineralization in the fossil record. Earth-Science Reviews, 179, 95-122.

DeRocher K.A., Smeets P.J.M., Goodge B.H., Zachman M.J., Balachandran P.V., Stegbauer L., Cohen M.J., Gordon L.M., Rondinelli J.M., Kourkoutis L.F., Joester D., 2020. Chemical gradients in human enamel crystallites. Nature, 583, 66-71.

Gao F., Xue J., Li X-H., Hu R., Li Q-L., 2024. Atom Probe Tomography Reveals Nano-scale Organic Remaining in Conodont. Atomic Spectroscopy, 45, 1-8.



Acknowledgements

This research was funded by the National Natural Science Foundation of China (42225301).
重要日期
  • 会议日期

    06月10日

    2025

    06月13日

    2025

  • 04月15日 2025

    初稿截稿日期

主办单位
National Natural Science Foundation of China
Geobiology Society
National Committee of Stratigraphy of China
Ministry of Science and Technology
Geological Society of China
Paleontological Society of China
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS)
Institute of Vertebrate Paleontology and Paleoanthropology, CAS
International Commission on Stratigraphy
International Paleontological Association
承办单位
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG, Wuhan)
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