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Guillaume de Lafontaine


Collaborating member

Department of biology, chemistry and geography, UQAR

Des Ursulines Building
300 Allée des Ursulines
Quebec, Canada
G5L 3A1

4187231986 extension 1061




Scientific communications

Napier, J.D., de Lafontaine, G., Heath, K.D., Hu, F.S., 2019. Rethinking long‐term vegetation dynamics: multiple glacial refugia and local expansion of a species complex. Ecography(published online 11/01/2019). DOI: 10.1111/ecog.04243.

de Lafontaine, G., Napier, J.D., Petit, R.J., Hu, F.S., 2018. Invoking adaptation to decipher the genetic legacy of past climate change. Ecology, 99(7): 1530-1546. DOI: 10.1002/ecy.2382.

Hao, Q., de Lafontaine, G., Guo, D., Gu, H., Hu, F.S., Han, Y., Song, Z., Liu, H., 2018. The critical role of local refugia in postglacial colonization of Chinese pine: joint inferences from DNA analyses, pollen records, and species distribution modeling. Ecography, 41(4): 592-606. DOI: 10.1111/ecog.03096.

de Lafontaine, G., Payette, S., 2012. Chapter 13: How climate and fire disturbances influence contrasted dynamics of Picea glauca ecotones and alpine tree lines in Atlantic and continental eastern North America. Pages 299-312 in Myster, R.W. (Editor). Ecotones Between Forest and Grassland. Springer. New York, United States.

de Lafontaine, G., Payette, S., 2012. Long-term fire and forest history of subalpine balsam fir (Abies balsamea) and white spruce (Picea glauca) stands in eastern Canada inferred from soil charcoal analysis. The Holocene, 22(2): 1-12. DOI: 10.1177/0959683611414931.

de Lafontaine, G., Asselin, H., 2011. Soil charcoal stability over the Holocene across boreal northeastern North America. Quaternary Research, 76: 196–200. DOI: 10.1016/j.quascirev.2011.01.002.

de Lafontaine, G., Couillard, P.-L., Payette, S., 2011. Permineralization of soil macrofossil charcoal promotes preservation of palaeoecological information. Journal of Quaternary Science, 26(6): 571-575. DOI: 10.1002/jqs.1529.

de Lafontaine, G., Payette, S., 2011. Shifting zonal patterns of the southern boreal forest in eastern Canada associated with changing fire regime during the Holocene. Quaternary Science Reviews, 30: 867-875.

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