Ice core temperatures are local so these paleorecords aren't directly
comparable to global means.

http://en.wikipedia.org/wiki/Proxy_%28climate%29#Water_isotopes_and_temperature_reconstruction

"since ocean temperatures are relatively stable the δ value mostly
reflects the temperature where precipitation occurs"

===

Also, temperatures atop the Antarctic ice sheet have been falling of late.

http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17257
http://www.pewclimate.org/global-warming-basics/antarcticfactsheet

" surface warming from the greenhouse effect is weaker in the southern
hemisphere than in the northern hemisphere, whereas cooling from
stratospheric ozone depletion is stronger in the south than in the
north. Consequently, the Arctic has warmed dramatically, even as the
Antarctic has experienced a small cooling trend. Climate models
reproduce this pattern when they are driven by both greenhouse gas
increases and stratospheric ozone depletion (Gillett and Thompson
2003; Shindell and Schmidt 2004). Hence, the present cooling of
Antarctica is consistent with the rest of the Earth's surface warming
in response to rising greenhouse gas concentrations."

===

Maybe you would do better to look at Greenland core data vs Greenland
surface data? There are paleo proxies of global temperature from
benthic foraminifera deposits but they don't have decadal resolution.

mt

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