Oxygen isotopes from Chinese caves: records not of monsoon rainfall but of circulation regime
Article first published online: 29 MAY 2012
Copyright © 2012 John Wiley & Sons, Ltd.
Journal of Quaternary Science
Volume 27, Issue 6, pages 615–624, August 2012
How to Cite
Maher, B. A. and Thompson, R. (2012), Oxygen isotopes from Chinese caves: records not of monsoon rainfall but of circulation regime. J. Quaternary Sci., 27: 615–624. doi: 10.1002/jqs.2553
- Issue published online: 10 AUG 2012
- Article first published online: 29 MAY 2012
- Manuscript Accepted: 30 MAR 2012
- Manuscript Revised: 15 MAR 2012
- Manuscript Received: 16 JAN 2012
Additional Supporting Information may be found in the online version of this article.
|jqs_2553_sm_SupplAppS1.doc||27K||Supporting Appendix S1: Further discussion|
|jqs_2553_sm_SupplFigS1.doc||474K||Supporting Fig. S1: Maps of magnetic susceptibility and reconstructed rainfall (mm a−1) values for past interglacial stages (Maher, 2011). Contours of magnetic susceptibility run from 50 to 240 × 10−8 m3 kg−1, rainfall contours run between 420 and 705 mm a−1; XA marks the location of Xi'an.|
|jqs_2553_sm_SupplFigS2.doc||768K||Supporting Fig. S2: Maps of magnetic susceptibility and reconstructed rainfall (mm a−1) values for past glacial stages. Contours and symbols as in Fig. S2.|
|jqs_2553_sm_SupplTabS1.doc||47K||Supporting Table S1: GNIP station data, location and altitude.|
|jqs_2553_sm_SupplTabS2.doc||28K||Supporting Table S2: Annual range and monsoonal (June–September) anomaly statistics.|
Please note: Wiley Blackwell is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.