Oxygen Isotopes in Authigenic Clay Minerals: Toward Building a Reliable Salinity Proxy

Abstract Most clay minerals in sedimentary environments have traditionally been considered to be of detrital origin, but under certain conditions, authigenic clay minerals can form at low temperature through the transformation of precursor clays or as direct precipitates from lake water. Such clay m...

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Bibliographic Details
Main Authors: D. Gebregiorgis, D. M. Deocampo, F. J. Longstaffe, A. Simpson, G. M. Ashley, E. J. Beverly, J. S. Delaney, J. Cuadros
Format: Article
Language:English
Published: Wiley 2020-02-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2019GL085576
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