The Open UniversitySkip to content

Potential of Chromium Isotopes as a Tracer of Past Ocean Oxygenation

Bonnand, Pierre (2011). Potential of Chromium Isotopes as a Tracer of Past Ocean Oxygenation. PhD thesis The Open University.

Full text available as:
PDF (Version of Record) - Requires a PDF viewer such as GSview, Xpdf or Adobe Acrobat Reader
Download (37MB) | Preview
Google Scholar: Look up in Google Scholar


Levels of atmospheric oxygen (O2) have increased from <2% of the present atmospheric level (PAL) to values similar to the PAL during the Neoproterozoic. This is likely to have resulted in significant changes in redox conditions in the oceans. The aim of this study is to provide new constraints on redox conditions in shallow seawater during the Neoproterozoic by analysis of the rare earth element (REE) concentration and chromium (Cr) isotopic composition of marine carbonates. To this end, a new method for δ53Cr analysis in low concentration samples has been developed. In addition, the Cr isotopic composition of modern and Phanerozoic carbonates, and seawater, have been determined to provide new constraints of the environmental behaviour of Cr isotopes.

Modern seawater is characterised by heavy δ53Cr values (+0.55-1.55%) relative to the continental crust (-0.12%), which indicates that Cr isotopes are fractionated during oxidative weathering. Importantly, the Cr isotopic composition of modern carbonates, precipitated in shallow water, is within the range of seawater. This suggests that fractionation of Cr isotopes during carbonate precipitation is minimal, and carbonates should provide a record of seawater δ53Cr. Carbonate samples of Phanerozoic age also have high δ53Cr values (0.737-1.994%), consistent with oxidative weathering on the continents at this time.

Most of the Neoproterozoic carbonates have significantly lower δ53Cr values than the modern and Phanerozoic carbonates. However, oolitic limestones deposited just prior to the first Cryogenian glaciations, have higher δ53Cr (+0.571-1.004%). Together, the δ53Cr and REE data suggest that the operation of the Cr cycle was significantly different in the Neoproterozoic. Changes in δ53Cr reflect either a shift in the relative importance of riverine and hydrothermal sources, and/or changes in levels of atmospheric O2 . Modelling indicates that shallow waters were either dysoxic or suboxic during the Cryogenian, and levels of atmospheric O2 must have been less than 30-40% PAL.

Item Type: Thesis (PhD)
Copyright Holders: 2011 The Author
Academic Unit/School: Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Item ID: 60959
Depositing User: ORO Import
Date Deposited: 07 May 2019 10:13
Last Modified: 30 Jun 2019 01:44
Share this page:

Download history for this item

These details should be considered as only a guide to the number of downloads performed manually. Algorithmic methods have been applied in an attempt to remove automated downloads from the displayed statistics but no guarantee can be made as to the accuracy of the figures.

Actions (login may be required)

Policies | Disclaimer

© The Open University   contact the OU