
But the important thing about ice is not how old it is (if you want super-old ice, go mine a comet; mind you that might be quite expensive too...) its how well preserved it is and its stratigraphic sequencing. There are, if you look closely at the Nature report, hints of this: The Kohnen core should also provide more detailed climate evidence than the one from Dome C, at least for more recent times. In the upper parts of the core, ice accumulated more than twice as fast as at Dome C, so it will be easier to distinguish between ice layers laid down in consecutive years. The ice at the bottom of the core, however, seems to be at least as old as that at the bottom of Dome C, so it must be very compressed. Err yes. So we'll get a more detailed *recent* record (which may have some value, e.g. looking again at D-O events in the Antarctic) but that could have been got from a much shallower core. And we'll get a record from a different sector (nice to see how things co-vary). But... a more detailed recent record implies a less detailed deep record; which is probably the greatest interest. The EPICA core goes down reliably to 780 kyr; does the Kohnen core provide useful info for [780,900] kyr? It will be good if it does. OTOH, since Kohnen isn't at a dome, the bottom is probably smeared, and very hard to work out where it came from.
And a postscript, on how rapidly things get sensationalised: Researchers dig up million-year-old ice (bad headline, text not so bad). Ditto from physorg.
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My understanding is that what is most wanted now is the record for the Mid-Pleistocene Transition at 950K bp. It sounds like these cores may be a bit marginal for that purpose.
There was the one also where he told the head of Brazil, "you have black people too?" Condi had to intervene.
It's an urban legend too, but pretty funny.
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