@article {239,
	title = {From ice age to modern: a record of landscape change in an Andean cloud forest},
	journal = {Journal of Biogeography},
	volume = {37},
	year = {2010},
	note = {id: 869; 639ND Times Cited:5 Cited References Count:63Y},
	pages = {1637-1647},
	abstract = {Aim},
	issn = {0305-0270},
	doi = {10.1111/J.1365-2699.2010.02318.X},
	author = {Valencia, B. G. and Urrego, D. H. and Silman, M. R. and Bush, M. B.}
}
@article {240,
	title = {A long history of cloud and forest migration from Lake Consuelo, Peru},
	journal = {Quaternary Research},
	volume = {73},
	year = {2010},
	note = {id: 1903; 564VS Times Cited:8 Cited References Count:85Y},
	pages = {364-373},
	abstract = {The complete paleoecological history from Lake Consuelo forest yields a record of ground-level cloud formation and changes in its lower altitudinal limit over the last 46,300 cal yr BP. The timing of early lake level fluctuations prior to 37,000 cal yr BP appears sensitive to North Atlantic temperature oscillations, corresponding to Dansgaard-Oeschger interstadials 11, 10 and 8 recorded in GISP2. After the LGM, the first hint of warming is recorded in Lake Consuelo at 22,000 call yr BP and agrees with other estimates for the region. The mid-Holocene (7400-5000 cal yr BP) was the period of highest rates of change and most significant reorganizations in the Consuelo forest. These community changes resulted from a regionally widespread dry period. Results from Lake Consuelo indicate that moisture availability, mediated through cloud cover, played the most significant role in ecological change in this system. Rates of past climate fluctuations never exceeded the forest capacity to accommodate change. Unfortunately, this might not be the case under predicted scenarios for the end of the current century. (C) 2009 University of Washington. Published by Elsevier Inc. All rights reserved.},
	issn = {0033-5894},
	doi = {10.1016/J.Yqres.2009.10.005},
	author = {Urrego, D. H. and Bush, M. B. and Silman, M. R.}
}
@article {1850,
	title = {A 24,900-year paleolimnological history from the Peruvian Andes},
	journal = {Quaternary Research},
	volume = {71},
	year = {2009},
	note = {id: 1902},
	month = {2009},
	pages = {71-82},
	author = {Hillyer, R. and Valencia, B. G. and Bush, M. B. and Silman, M. R. and Steinitz-Kannan, M.}
}
@article {1481,
	title = {Holocene fire and occupation in Amazonia: Records from two lake districts},
	volume = {Ser. B.},
	year = {2007},
	note = {id: 454},
	month = {2007},
	author = {Bush, M. B. and Silman, M. R. and de Toledo, M. B. and Listopad, C. R. S. and Gosling, W. D. and Williams, C. and De Oliveira, P. E. and Krisel, C.}
}
@article {1480,
	title = {A regional study of Holocene climate change and human occupation in Peruvian Amazonia},
	volume = {on-line article},
	year = {2007},
	note = {id: 453},
	month = {2007},
	author = {Bush, M. B. and Listopad, M. C. S. and Silman, M. R.}
}
@article {979,
	title = {A 17,000 year history of Andean climatic and vegetation change from Laguna de Chochos, Peru},
	journal = {Journal of Quaternary Science},
	volume = {20},
	year = {2005},
	note = {id: 1015},
	pages = {703-714},
	abstract = {The manifestation of major climatic events such as the timing of deglaciation and whether, or not, the Younger Dryas affected Andean systems has garnered considerable recent attention. Even the Holocene is rapidly emerging as a time of considerable interest in Neotropical palaeoclimatology and palaeoecology. The Holocene of the Neotropics is now revealed as a time of some temperature change with precipitation:evaporation ratios fluctuating markedly. Major changes in lake level, ice-accumulation, and vegetation are indicative of changes both in precipitation and temperature regimes. Although global-scale forcing mechanisms may underlie some of these changes, e.g. the precessional rhythm, other variability appears to be localised. In a record from near the upper forest limit of the eastern Peruvian Andes, pollen, charcoal, and sedimentary data suggest that the deglaciational period from ca. 17 000 to ca. 11 500 cal. yr BP was a period of rapid climatic oscillations, set against an overall trend of warming. A warm-dry event is evident between ca. 9500 and ca. 7300 cal. yr BP, and comparisons with other regional archives suggest that it was regional in scale. A ca. 1500-yr periodicity in the magnetic susceptibility data is evident between 12 000 and 6000 cal. yr BP, reaching a peak intensity during the dry event. A weaker oscillation with a 500{\textendash}600-yr periodicity is present throughout much of the Holocene. The uppermost sample of the pollen analysis reveals deforestation as modern human land use simplified the landscape.},
	doi = {10.1002/jqs.983},
	author = {Bush, M. B. and Hansen, B. C. S. and Rodbell, D. T. and Seltzer, G. O. and Young, K. R. and Leon, B. and Abbott, M. B. and Silman, M. R. and Gosling, W. D.}
}
@article {1963,
	title = {The last glacial maximum: stability and change in an Andean cloud forest},
	journal = {Journal of Quaternary Science},
	volume = {20},
	year = {2005},
	note = {id: 458},
	month = {2005},
	pages = {693-701},
	author = {Urrego, D. H. and Silman, M. R. and Bush, M. B.}
}
@article {978,
	title = {48,000 years of climate and forest change from a biodiversity hotspot},
	journal = {Science},
	volume = {303},
	year = {2004},
	note = {id: 1016},
	pages = {827-829},
	abstract = {A continuous 48,000-year-long paleoecological record from Neotropical lower montane forest reveals a consistent forest presence and an ice-age cooling of \~{}5{\textdegree} to 9{\textdegree}C. After 30,000 years of compositional stability, a steady turnover of species marks the 8000-year-long transition from ice-age to Holocene conditions. Although the changes were directional, the rates of community change were no different during this transitional period than in the preceding 30,000-year period of community stability. The warming rate of about 1{\textdegree}C per millennium during the Pleistocene-Holocene transition was an order of magnitude less than the projected changes for the 21st century.},
	doi = {10.1126/science.1090795 },
	author = {Bush, M. B. and Silman, M. R. and Urrego, D. H.}
}
