Biology Reference
In-Depth Information
Cuffy, K. M. 2004. Into an ice age.
Nature
431:133-34. [“Analyses of a new core from Green-
land yield the fi rst high-resolution picture of the start of the last ice age in the Northern
Hemisphere, and of the onset of climate instability as our planet cooled.” Summary of
NGRIP 2004.]
Davies, T. J., A. Purvis, and J. L. Gittleman. 2009. Quaternary climate change and the geo-
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Am. Nat.
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De Batist, M., and E. Chapron, eds. 2008.
Lake systems: Sedimentary archives of climate
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Palaeogeogr. Palaeocl. Palaeoecol.
259:93-356. [Papers on the Salton Basin, California; Laguna Potrok Aike, Argentina;
Mérida Andes, Venezuela; Lago Icalmam, Chile.]
Driese, S. G., K. H. Orvis, S. P. Horn, Z.-H. Li, and D. S. Jennings. 2007. Paleosol evidence for
Quaternary uplift and for climate and ecosystem changes in the Cordillera de Talamanca,
Costa Rica.
Palaeogeogr. Palaeocl. Palaeoecol.
248:1-23.
A dust with climate. 2008. Editors' summary.
Nature
452.
Elliot, M., L. Labeyrie, and J.-C. Duplessy. 2002. Changes in North Atlantic deep-water forma-
tion associated with the Dansgaard-Oeschger temperature oscillations (60-10 ka).
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warming.
Science
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Fall, P. L. 1997. Timberline fl uctuations and late Quaternary paleoclimates in the Southern
Rocky Mountains, Colorado.
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Florindo, F., A. Nelson, and A. M. Haywood, eds. 2008.
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Francis, D. R., A. P. Wolfe, I. R. Walker, and G. H. Miller. 2006. Interglacial and Holocene
temperature reconstructions based on midge remains in sediments of two lakes from
Baffi n Island, Nunavut, Arctic Canada.
Palaeogeogr. Palaeocl. Palaeoecol.
236:107-24.
[“2.22°C for summer water temperatures . . . 1.53°C for mean July air temperatures.
Reconstructions at both sites indicate that summer temperatures during the last
interglacial were higher than at any time in the Holocene, and 5 to 10°C higher than at
present.”]
Fréchette, B., A. P. Wolfe, G. H. Miller, P. J. H. Richard, and A. de Vernal. 2006. Vegetation
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Palaeogeogr. Palaeocl.
Palaeoecol.
236:91-106. [“ July air temperatures of the last interglacial . . . 4 to 5°C
warmer than present on eastern Baffi n Island, which was warmer than any interval within
the Holocene.”]
Giles, J. 2006. How much will it cost to save the world?
Nature
444:6-7. [
Stern Review on the
Economics of Climate Change
estimates that “tackling climate change [now] would cost
20 times less than doing nothing,” or about 1 percent GDP.]
González-Carranza, Z., J. C. Berrío, H. Hooghiemstra, J. F. Duivenvoorden, and H. Behling.
2008. Changes of seasonally dry forest in the Colombian Patía Valley during the early
and middle Holocene and the development of a dry climatic record for the northernmost
Andes.
Rev. Palaeobot. Palynol.
152:1-10. [“The data also show that relatively humid and
wet conditions were present at the Patía Valley from c. 9510 to 8600 cal yr BP, whereas
between c. 8360 to 8260 cal yr BP dry conditions prevailed in the valley. The pollen rec-
