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Preparation of Functional Silica Using a Bioinspired Method
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Potassic, high-silica Hadean crust.

Patrick Boehnke1,2, Elizabeth A Bell3, Thomas Stephan4,2

  • 1Department of the Geophysical Sciences, The University of Chicago, Chicago, IL 60637; pboehnke@gmail.com tmark.harrison@gmail.com.

Proceedings of the National Academy of Sciences of the United States of America
|June 6, 2018
PubMed
Summary

Early Earth's crustal composition is revealed by analyzing strontium isotopes in ancient zircons. This research indicates a diverse range of igneous rocks existed by 4.2 billion years ago, impacting early planetary conditions.

Keywords:
Nuvvuagittuqearly Earthhabitabilityhadeanzircons

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Area of Science:

  • Geoscience
  • Early Earth studies
  • Isotope geochemistry

Background:

  • Understanding the Hadean (>4 Ga) Earth's crust is crucial for reconstructing early planetary conditions.
  • The composition of the early crust and its associated volatiles influenced the atmosphere, oceans, and nutrient cycles.
  • Limited data and consensus exist regarding the nature of the Hadean crust.

Purpose of the Study:

  • To investigate the composition of the Hadean crust.
  • To provide insights into the petrogenesis of early Earth's crustal rocks.
  • To constrain the timing of crustal differentiation processes.

Main Methods:

  • Analysis of the 87Sr/86Sr ratio in apatite inclusions within Archean zircons.
  • Utilizing samples from the Nuvvuagittuq Supracrustal Belt, Canada.
  • Radiometric dating techniques to establish temporal constraints.

Main Results:

  • Evidence for a high rubidium/strontium (Rb/Sr) ratio reservoir (>1) by at least 4.2 Ga.
  • The protolith of the analyzed zircons indicates early crustal differentiation.
  • The findings suggest the presence of a wide spectrum of igneous rock compositions.

Conclusions:

  • The Hadean crust was not uniform and encompassed a broad range of igneous compositions, from mafic to highly silicic.
  • Early-formed crustal reservoirs influenced the subsequent evolution of Earth's surface environment.
  • This study provides critical geochemical evidence for early crustal heterogeneity.