Abstract:Old‐growth forests are biologically and ecologically valuable systems that are disappearing worldwide at a rapid rate. México still holds large areas covered by temperate forests in the mountains of the Sierra Madre Occidental, but few of these retain old‐growth characteristics. We studied four sites with remnant old‐growth forests in Mesa de las Guacamayas, a site in the Sierra Madre Occidental in northwestern Chihuahua, to assess their composition, structure, and age characteristics. Overstory tree densities… Show more
“…This has increased the risk and susceptibility of these forests to maintain forest dynamics, hydrological functions, forest productivity, and other ecosystem services. This change in fire frequency is not exclusive to the study area; studies in other locations of the Sierra Madre Occidental, in the states of Durango and Chihuahua, have reported similar changes in fire frequency since the 1950s Covington 1997, 1999;Heyerdahl and Alvarado 2003;Cortes-Montaño et al 2012). In other sites, the greater amplitude in fire frequency intervals has resulted in an increase in quantity and continuity of fuel loads (White and Vankat 1993;Skinner et al 2008).…”
Background: Fire scars are the primary source of physical evidence used to date past fires around the world, and to estimate parameters of historical fire regimes and fire-climate relationships. Despite an increase in studies about historical fire regimes and the relationship between fire and climate, these studies are still limited for Mexican forests. Our goal was to characterize the historical fire regime in two sites with different elevations, to assess changes in fire frequency, and to determine the relationship between fire regimes and climate patterns in a conifer-dominated forest in the Upper Nazas watershed of the Sierra Madre Occidental, Mexico. We were able to cross-date 50 fire-scarred samples of Pinus arizonica Engelm., P. strobiformis Engelm., P. teocote Schlecht. & Cham., P. durangensis Martínez, and Pseudotsuga menziesii (Mirb.) Franco and identify a total of 596 fire scars. Results: Evidences are compelling evidences on forest fires occurred frequently in the study area, starting in the mid eighteenth century and through the mid twentieth century. The season of fire occurrence was determined for 560 (94%) fire scars. Most fire scars at both of our sampling locations, found at low and high elevation sites, occurred in the spring (525, 93.8%) and only 6.2% occurred in the summer. The mean fire interval and Weibull median fire interval values were < 10 years for all fire-scar filter (all samples, ≥10% and ≥ 25%), and the average per-sample fire interval was < 25 years. Conclusions: Our results suggest fire frequency has changed over time at our study site, becoming less common and less extensive since the 1950s. In addition, extensive fires occurred in dry years as indicated by low precipitation, negative NIÑO 3 Sea Surface Temperature (SST) values, and negative Palmer Drought Severity Index (PDSI) values. Fire frequencies must be maintained within the amplitude of their historical regime, with the objective of reducing the risk of severe fires and preserving ecological and hydrological benefits in the watershed.
“…This has increased the risk and susceptibility of these forests to maintain forest dynamics, hydrological functions, forest productivity, and other ecosystem services. This change in fire frequency is not exclusive to the study area; studies in other locations of the Sierra Madre Occidental, in the states of Durango and Chihuahua, have reported similar changes in fire frequency since the 1950s Covington 1997, 1999;Heyerdahl and Alvarado 2003;Cortes-Montaño et al 2012). In other sites, the greater amplitude in fire frequency intervals has resulted in an increase in quantity and continuity of fuel loads (White and Vankat 1993;Skinner et al 2008).…”
Background: Fire scars are the primary source of physical evidence used to date past fires around the world, and to estimate parameters of historical fire regimes and fire-climate relationships. Despite an increase in studies about historical fire regimes and the relationship between fire and climate, these studies are still limited for Mexican forests. Our goal was to characterize the historical fire regime in two sites with different elevations, to assess changes in fire frequency, and to determine the relationship between fire regimes and climate patterns in a conifer-dominated forest in the Upper Nazas watershed of the Sierra Madre Occidental, Mexico. We were able to cross-date 50 fire-scarred samples of Pinus arizonica Engelm., P. strobiformis Engelm., P. teocote Schlecht. & Cham., P. durangensis Martínez, and Pseudotsuga menziesii (Mirb.) Franco and identify a total of 596 fire scars. Results: Evidences are compelling evidences on forest fires occurred frequently in the study area, starting in the mid eighteenth century and through the mid twentieth century. The season of fire occurrence was determined for 560 (94%) fire scars. Most fire scars at both of our sampling locations, found at low and high elevation sites, occurred in the spring (525, 93.8%) and only 6.2% occurred in the summer. The mean fire interval and Weibull median fire interval values were < 10 years for all fire-scar filter (all samples, ≥10% and ≥ 25%), and the average per-sample fire interval was < 25 years. Conclusions: Our results suggest fire frequency has changed over time at our study site, becoming less common and less extensive since the 1950s. In addition, extensive fires occurred in dry years as indicated by low precipitation, negative NIÑO 3 Sea Surface Temperature (SST) values, and negative Palmer Drought Severity Index (PDSI) values. Fire frequencies must be maintained within the amplitude of their historical regime, with the objective of reducing the risk of severe fires and preserving ecological and hydrological benefits in the watershed.
“…This highlights the significance of fire as a thinning agent and the important relationship between fire‐free periods and age peaks. Similar increases in pine establishment during periods of decreased fire activity have also been reported in Mexican pine forests with frequent fire regimes (Fulé & Covington, ; Cortez‐Montaño et al ., ).…”
Aim The purpose of this study was to examine the influence of moisture and fire on historical ponderosa pine (Pinus ponderosa Dougl. ex Laws.) age structure patterns.Location We used a natural experiment created over time by the unique desert island geography of southern Arizona.
MethodsWe sampled tree establishment dates in two sites on Rincon Peak and another site in the Santa Catalina Mountains. The influence of regional moisture patterns was investigated by examining synchrony among tree age peaks and periods of favourable moisture. The influence of fire was investigated by examining the relationship between local fire histories and age peaks.Results Tree age peaks (recruitment events) were synchronized with periods of reduced fire frequencies, suggesting that periods of reduced fire activity allowed time for young trees to develop fire-resistant characteristics. For example, two age peaks (1670s-1680s and 1770s-1780s) in the Rincon Peak-north site coincided with a period of reduced fire frequency. These age peaks were absent in the Rincon Peak-south site where fires were more frequent during that time. All three sites had age peaks in the early 19th century, coinciding with regional climate variability (i.e. El Niño Southern Oscillation patterns) that reduced fire activity.Main conclusions Historically prior to fire suppression, the survivorship, and thus cohort establishment, of ponderosa pine was ultimately determined by local fire history patterns. The importance of fire as a tree establishment regulator highlights the need to use fire at appropriate intervals not just to restore but to maintain healthy forests.
“…Additionally, surveys of old growth forest structure [88] and species requiring specialized habitats protected from severe fire (e.g., Jemez Mountain salamander [89]) can also be taken as indicators of refugia on disturbed or undisturbed landscapes. We concur with recommended conservation measures considering the potential impacts of climate change that include maintenance of the greatest possible number of local refugia as habitat networks [25].…”
Abstract:The spatial patterns resulting from large fires include refugial habitats that support surviving legacies and promote ecosystem recovery. To better understand the diverse ecological functions of refugia on burn mosaics, we used remotely sensed data to quantify neighborhood patterns of areas relatively unchanged following the 2011 Las Conchas fire. Spatial patterns of refugia measured within 10-ha moving windows varied across a gradient from areas of high density, clustered in space, to sparsely populated neighborhoods that occurred in the background matrix. The scaling of these patterns was related to the underlying structure of topography measured by slope, aspect and potential soil wetness, and spatially varying climate. Using a nonmetric multidimensional scaling analysis of species cover data collected post-Las Conchas, we found that trees and forest associates were present across the refugial gradient, but communities also exhibited a range of species compositions and potential functions. Spatial patterns of refugia quantified for three previous burns (La Mesa 1977, Dome 1996, Cerro Grande 2000 were dynamic between fire events, but most refugia persisted through at least two fires. Efforts to maintain burn heterogeneity and its ecological functions can begin with identifying where refugia are likely to occur, using terrain-based microclimate models, burn severity models and available field data.
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