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Dual modes of the carbon cycle since the Last Glacial Maximum.
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A 40-million-year history of atmospheric CO(2).
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Palaeoclimatology: the record for marine isotopic stage 11.
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Rates of change in natural and anthropogenic radiative forcing over the past 20,000 years.
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3
The spatial extent of 20th-century warmth in the context of the past 1200 years.
Science. 2006 Feb 10;311(5762):841-4. doi: 10.1126/science.1120514.
5
Rapid atmospheric CO2 changes associated with the 8,200-years-B.P. cooling event.
Proc Natl Acad Sci U S A. 2002 Sep 17;99(19):12011-4. doi: 10.1073/pnas.182420699. Epub 2002 Aug 29.
6
Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability.
Science. 2002 Mar 22;295(5563):2250-3. doi: 10.1126/science.1066208.
8
Stomatal density and stomatal index as indicators of paleoatmospheric CO(2) concentration.
Rev Palaeobot Palynol. 2001 Mar;114(1-2):1-28. doi: 10.1016/s0034-6667(00)00074-9.
9
The HIC signalling pathway links CO2 perception to stomatal development.
Nature. 2000 Dec 7;408(6813):713-6. doi: 10.1038/35047071.
10
Causes of climate change over the past 1000 years.
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