Forest succession along a productivity gradient following fire exclusion
Introduction
Recurrent fire truncates succession, resulting in marked discrepancies between edaphic and climatic potential and typical biotic expression (Bond et al., 2005, Pyne, 1982). Accumulation of biomass and shifts in species composition associated with disruption of historical fire patterns following Euro-American settlement have been documented across boreal, eastern deciduous, Rocky Mountain evergreen, Pacific coastal, southeastern mixed evergreen, and Mexican montane forest biomes of North America (e.g., Brown et al., 2015, Stephens et al., 2015, Boucher et al., 2009, Nowacki and Abrams, 2008, Friedman and Reich, 2005, Moore et al., 2004, Heyerdahl and Alvarado, 2003, Gilliam and Platt, 1999, Fulé and Covington, 1994). The effects of fire exclusion on successional dynamics are often compounded by land use practices, climate change, pollution, and introduction of invasive species (Wimberly and Liu, 2014, King et al., 2013, Littell et al., 2010, Brooks et al., 2004, Fenn et al., 2003, Hemstrom, 2001).
In the inland Pacific Northwest (IPN), extensive logging, livestock grazing, and fire suppression has resulted in a decline in large and old trees, an increase in the relative abundance of fire intolerant tree species, and an increase in overall forest density (Spies et al., 2006, Hessburg and Agee, 2003). Dendroecological reconstructions (Merschel et al., 2014, Everett et al., 2008, Perry et al., 2004, Wright and Agee, 2004, Camp, 1999), analyses of historical timber inventories (Hagmann et al., 2014, Hagmann et al., 2013), and interpretation of historical photography (Hessburg et al., 2007, Hessburg et al., 1999) have documented significant changes to IPN forest structure and composition relative to historical conditions. Successional dynamics in the absence of fire have been reported for a variety of different regions throughout the American West (O’Connor et al., 2016, Margolis and Malevich, 2016, Abella et al., 2015, Taylor, 2010, Taylor, 2000, Fulé et al., 2009), but to date only a few studies have carefully examined how the magnitude and direction of forest change varies among different forest types in the IPN (Merschel et al., 2014, Heyerdahl et al., 2001, Camp, 1999).
Historical forest dynamics in the IPN and appropriate management strategies to restore historical conditions are almost always inferred from existing forest structure and composition (Stine et al., 2014, Franklin and Johnson, 2012, Hessburg et al., 2007, Franklin et al., 2002). But there is little empirical data that links contemporary conditions to past successional and disturbance dynamics, especially in moister and more productive forest types (Stine et al., 2014). Examining the characteristics of succession in the absence of fire in different IPN forest types will help inform management decisions and predict the potential for forests to return to stable structural and compositional configurations (Halpern, 1988), or experience uncharacteristically severe disturbance or state changes (Miller et al., 2009, Savage and Mast, 2005, Beisner et al., 2003).
This study uses detailed dendroecological reconstructions of forest structure and composition across a broad productivity gradient in the southern Blue Mountains of eastern Oregon to better understand the variability in forest response to disturbance regime shifts. Objectives of this study include: (1) Quantifying historical structure and composition in diverse forest types; and, (2) describing the magnitude and direction of succession in different forest types in the absence of fire.
Section snippets
Study area
Data were collected within the Malheur National Forest (MNF), which encompasses 688,000 ha of federal lands that make up the southern Blue Mountains of eastern Oregon, a northeast to southwest trending axis of rolling hills, plateaus, river canyons, and occasional high ridges and peaks. Elevations on the MNF range from 998 to 2756 m. Approximately 90% of the total land area of the MNF is found between 1300 and 2000 m, where precipitation ranges from 420 to 775 mm annually. 71% of precipitation
Forest groups
Cluster analysis of live basal area in reconstruction plots identified a total of four statistically significant (AU p ≤ 0.01) groups within two broad biophysical settings (Fig. 3). Two groups (a total of 12 reconstruction plots) were found in biophysical settings characterized by low water availability, high summer vapor pressure deficits, and low tree biomass. Forest stands belong to these groups were dominated by ponderosa pine. Two groups (a total of eight reconstruction plots) were found in
Limitations and uncertainties of historical reconstructions
Dendroecological reconstructions underestimate the extent of historical structure when wood evidence has been removed by fire or decomposition prior to sampling (Fritts and Swetnam, 1989). Although this study almost certainly does not reconstruct all tree structure present in the 19th century, the reconstruction methods utilized here likely reconstructed most larger tree structure that form the majority of stand basal area even in contemporary southern Blue Mountains stands and are a reasonable
Acknowledgements
Chris Dunn, John Bailey, Emily Comfort, Tom Spies, David Peterson, Keala Hagmann, Garrett Meigs, and three anonymous reviewers provided helpful comments on draft manuscripts. Harold Zald, Alan Tepley, Steve Voelker, and faculty at the Laboratory of Tree Ring Research at the University of Arizona provided dendroecological methods training. Mike Vernon provided laboratory assistance. Tim Lillebo provided important insights into the terrain and ecology of the southern Blue Mountains. Conversations
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