Long ago, Earth experienced a series of especially severe glaciations. A new explanation for deposits laid down at the end of these events centres on the large-scale release of methane from solid gas hydrates.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Rent or buy this article
Get just this article for as long as you need it
$39.95
Prices may be subject to local taxes which are calculated during checkout
References
Harland, W. B. Geol. Rundsch. 54, 45–61 (1964).
Kirshvink, J. L. in The Proterozoic Biosphere: A Multidisciplinary Study (eds Schopf, J. W. & Klein, C.) 51–52 (Cambridge Univ. Press, New York, 1992).
Kaufman, A. J., Knoll, G. H. & Narbonne, G. M. Proc. Natl Acad. Sci. USA 94, 6600–6605 (1997).
Jacobsen, S. B. & Kaufman, A. J. Chem. Geol. 161, 37–57 (1999).
Hoffman, P. F. et al. Science 281, 1342–1346 (1998).
Kennedy, M. J., Christie-Blick, N. & Sohl, L. E. Geology 29, 443–446 (2001).
Hyde, W. T., Crowley, T. J., Baum, S. K. & Peltier, W. R. Nature 405, 425–429 (2000).
Crowley, T. J., Hyde, W. T. & Peltier, W. R. Geophys. Res. Lett. 28, 283–286 (2001).
Walker, J. C. G., Hays, P. B. & Kasting, J. F. J. Geophys. Res. 86, 9776–9782 (1981).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Jacobsen, S. Gas hydrates and deglaciations. Nature 412, 691–692 (2001). https://doi.org/10.1038/35089168
Issue Date:
DOI: https://doi.org/10.1038/35089168
This article is cited by
-
Carbon isotope composition and correlation across the Cambrian-Ordovician boundary in Kalpin Region of the Tarim Basin, China
Science in China Series D: Earth Sciences (2008)
-
Carbon isotope composition of the Lower Triassic marine carbonates, Lower Yangtze Region, South China
Science in China Series D (2006)