For crops, modelling shows that drought often becomes constraining despite elevated CO2 levels acting as a ‘fertilizer’ (Parry et al., 2004). In cold climates, it is not unusual for natural tree populations to be located under sub-optimal conditions, with the discrepancy between the
inhabited and the optimal climate increasing with the severity of climate (Rehfeldt DNA Damage inhibitor et al., 2004). In such locations, an increase in temperature, coupled with at least stable precipitation, may result in increased wood yields in the short- to medium-term. Projected examples of such increases include: Pinus banksiana in the North American Great Lakes region ( Mátyás and Yeatman, 1992 and Mátyás, 1994); Pinus contorta, Pinus sylvestris and Larix sibirica in Siberia ( Rehfeldt et al., 1999, Rehfeldt et al., 2001 and Rehfeldt et al., 2004); Picea glauca in southern Quebec ( Beaulieu and Rainville, 2005); and Pseudostsuga menziesii in western North America ( Leites et al., 2012a and Leites et al., 2012b). In the longer-term, however, declines are expected as adaptive and plastic capacities to respond to change are exhausted
( Mátyás et al., selleckchem 2010). Here, we address the role that forest genetic resources (FGR, the genetic variation in trees of present or potential benefit to humans; FAO, 1989) can play in responding to anthropogenic climate change. The present distribution of FGR globally is the result of natural geological, ecological and genetic processes, which, Y-27632 molecular weight over
thousands of years, and along with the influence of man, have resulted in adaptation to local environments (Alberto et al., 2013). Included in this is adaptation to local disturbances, such as fire, insects and diseases. We review the pressures on FGR imposed directly by changing climate, as well as the indirect impacts on forests induced by changes in the biotic (e.g., insect and disease) and abiotic (e.g., fire, flood) disturbances that affect them. In particular, we consider climate-related responses in the context of linkages to disturbances and associated feedback loops, an issue not widely addressed in previous reviews on climate change and tree genetic resources. We conclude by discussing the feasibility of various management options to utilize the genetic variation in trees to respond to climate change and present options for policy-makers. Impacts are experienced through several demographic and genetic processes (Kremer et al., 2012 and Savolainen et al., 2011). Some are directional and gradual, such as trends in increasing temperature and reducing rainfall, while others involve abrupt change, including drought, flood, fire and sudden pest invasions (in this paper we refer to these as catastrophic events; Scheffer et al., 2001 and Scheffer and Carpenter, 2003).