The last deglaciation was punctuated by several millennial-scale climate changes. In the Gulf of California, the cold stages were marked by decreased upwelling, opposite to the changes expected if these shifts were analogous to modern seasonal variability.
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References
Dansgaard, W. et al. Nature 364, 218–220 (1993).
Bond, G. et al. Nature 365, 143–147 (1993).
Hendy, I. L. & Kennett, J. P. Paleoceanography 25, 30–42 (2000).
Peterson, L. C. et al. Science 290, 1947–1951 (2000).
McClymont, E. L. et al. Paleoceanography 27, PA2202 (2012).
Leduc, G. et al. Quat. Res. 72, 123–131 (2009).
Prange, M. et al. Quat. Sci. Rev. 29, 1317–1321 (2010).
Pak, D. K., Lea, D. W. & Kennett, J. P. Paleoceanography 27, PA1212 (2012).
Hendy, I. L. et al. Paleoceanography 19, PA3007 (2004).
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Pak, D. Analogue complexity. Nature Geosci 5, 450–451 (2012). https://doi.org/10.1038/ngeo1510
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DOI: https://doi.org/10.1038/ngeo1510