Oxygen isotope variations in Chinese cave deposits have been interpreted as proxies for the East Asian summer monsoon. Numerical simulations suggest the deposits may instead record remote climate changes over India and the Indian Ocean.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Wang, Y. J. et al. Nature 451, 1090–1093 (2008).
Cheng, H. et al. Science 236, 248–252 (2009).
Pausata, F. S. R., Battisti, D. S., Nisancioglu, K. H. & Bitz, C. M. Nature Geosci. 4, 474–480 (2011).
Dayem, K. E., Molnar, P., Battisti, D. S. & Roe, G. H. Earth Planet. Sci. Lett. 295, 219–230 (2010).
LeGrande, A. N. & Schmidt, G. A. Clim. Past 5, 441–455 (2009).
Wang, Y. J. et al. Science 294, 2345–2348 (2001).
Ding, Y., Li, C. & Liu, Y. Adv. Atmos. Sci. 21, 343–360 (2004).
Clemens, S. C., Prell, W. L. & Sun, Y. Paleoceanography 25, PA4207 (2010).
Maher, B. A. The Holocene 18, 861–866 (2008).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Johnson, K. Long-distance relationship. Nature Geosci 4, 426–427 (2011). https://doi.org/10.1038/ngeo1190
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo1190
This article is cited by
-
Is Chinese stalagmite δ18O solely controlled by the Indian summer monsoon?
Climate Dynamics (2019)