Skip to main content

Research Repository

Advanced Search

Re-Os geochronology and coupled Os-Sr isotope constraints on the Sturtian snowball Earth

Rooney, A.D.; Macdonald, F.; Strauss, J.V.; Dudás, F.Ö; Hallmann, C.; Selby, D.

Re-Os geochronology and coupled Os-Sr isotope constraints on the Sturtian snowball Earth Thumbnail


Authors

A.D. Rooney

F. Macdonald

J.V. Strauss

F.Ö Dudás

C. Hallmann



Abstract

After nearly a billion years with no evidence for glaciation, ice advanced to equatorial latitudes at least twice between 717 and 635 Mya. Although the initiation mechanism of these Neoproterozoic Snowball Earth events has remained a mystery, the broad synchronicity of rifting of the supercontinent Rodinia, the emplacement of large igneous provinces at low latitude, and the onset of the Sturtian glaciation has suggested a tectonic forcing. We present unique Re-Os geochronology and high-resolution Os and Sr isotope profiles bracketing Sturtian-age glacial deposits of the Rapitan Group in northwest Canada. Coupled with existing U-Pb dates, the postglacial Re-Os date of 662.4 ± 3.9 Mya represents direct geochronological constraints for both the onset and demise of a Cryogenian glaciation from the same continental margin and suggests a 55-My duration of the Sturtian glacial epoch. The Os and Sr isotope data allow us to assess the relative weathering input of old radiogenic crust and more juvenile, mantle-derived substrate. The preglacial isotopic signals are consistent with an enhanced contribution of juvenile material to the oceans and glacial initiation through enhanced global weatherability. In contrast, postglacial strata feature radiogenic Os and Sr isotope compositions indicative of extensive glacial scouring of the continents and intense silicate weathering in a post–Snowball Earth hothouse.

Citation

Rooney, A., Macdonald, F., Strauss, J., Dudás, F., Hallmann, C., & Selby, D. (2014). Re-Os geochronology and coupled Os-Sr isotope constraints on the Sturtian snowball Earth. Proceedings of the National Academy of Sciences, 111(1), 51-56. https://doi.org/10.1073/pnas.1317266110

Journal Article Type Article
Acceptance Date Nov 8, 2013
Online Publication Date Dec 16, 2013
Publication Date Jan 7, 2014
Deposit Date Dec 20, 2013
Publicly Available Date Feb 19, 2015
Journal Proceedings of the National Academy of Sciences
Print ISSN 0027-8424
Electronic ISSN 1091-6490
Publisher National Academy of Sciences
Peer Reviewed Peer Reviewed
Volume 111
Issue 1
Pages 51-56
DOI https://doi.org/10.1073/pnas.1317266110
Keywords Rhenium-osmium geochronology, Strontium isotopes, Osmium isotopes, Windermere Supergroup Neoproterozoic glaciation.
Public URL https://durham-repository.worktribe.com/output/1473458