Mesocrystalline Architecture in Hyaline Foraminifer Shells Indicates a Non‐Classical Crystallisation Pathway-Reference-Cited by-同舟云学术

Mesocrystalline Architecture in Hyaline Foraminifer Shells Indicates a Non‐Classical Crystallisation Pathway

Published:2022-06 Issue:6 Volume:23 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Arns A. I.¹^ORCID,Evans D.²^ORCID,Schiebel R.¹^ORCID,Fink L.³^ORCID,Mezger M.⁴^ORCID,Alig E.³,Linckens J.²^ORCID,Jochum K. P.¹^ORCID,Schmidt M. U.³,Jantschke A.⁵^ORCID,Haug G. H.¹⁶

Affiliation:

1. Max Planck Institute for Chemistry Mainz Germany

2. Institute of Geosciences Goethe University Frankfurt Frankfurt Germany

3. Institute of Inorganic and Analytical Chemistry Goethe University Frankfurt Frankfurt Germany

4. Faculty of Physics University of Vienna Vienna Austria

5. Institute of Geosciences Johannes Gutenberg University Mainz Mainz Germany

6. Department of Earth Sciences ETH Zürich Zurich Switzerland

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GC010445

Reference133 articles.

1. Taking Advantage of Disorder: Amorphous Calcium Carbonate and Its Roles in Biomineralization

2. Trace element proxies for surface ocean conditions: A synthesis of culture calibrations with planktic foraminifera

3. Chamber Formation in Planktonic Foraminifera

4. The role of seawater endocytosis in the biomineralization process in calcareous foraminifera

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