The effect of progressive dissolution on the oxygen and silicon isotope composition of opal-A phytoliths: Implications for palaeoenvironmental reconstruction-Reference-Cited by-同舟云学术

The effect of progressive dissolution on the oxygen and silicon isotope composition of opal-A phytoliths: Implications for palaeoenvironmental reconstruction

Published:2016-07 Issue: Volume:453 Page:42-51
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Prentice Andrea J.,Webb Elizabeth A.

Funder

Canadian Foundation for Innovation

Ontario Research Fund

UWO Academic Development Fund

UWO Faculty of Science and Research Western

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference68 articles.

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2. The oxygen isotopic composition of phytolith assemblages from tropical rainforest soil tops (Queensland, Australia): validation of a new palaeoenvironmental tool;Alexandre;Clim. Past,2012

3. Effect of climate and vegetation on oxygen-18 and deuterium profiles in soils;Allison,1984

4. Fossil opal-phytoliths;Baker;Micropaleontology,1960

5. Experimental dissolution of diatom silica in concentrated salt solutions and implications for paleoenvironmental reconstruction;Barker;Limnol. Oceanogr.,1994

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