# **************************************************************** # ** Please acknowledge the contributors and the International ** # ** Multiproxy Paleofire Database when using these data. ** # **************************************************************** # # Site name: Archuleta Mesa Plot C6 # Investigators: Peter M. Brown and Rosalind Wu # # Dating Method : Crossdated # Collectors : Peter M. Brown, Rosalind Wu # Species name : Pinus ponderosa, Juniperus scopulorum, Pseudotsuga menziesii # Common name : ponderosa pine, Rocky Mountain juniper, Douglas-fir # Country : United States # State : Colorado # National Forest: San Juan National Forest # Ranger district: Pagosa # UTM easting : 0301356 (NAD83, 13) # UTM northing : 4115479 (NAD83, 13) # Elevation : 2441 m # Slope : 8 deg # Aspect : 280 deg # Sample Storage Location: Rocky Mountain Tree-Ring Research, Inc., # Ft. Collins, CO # # Fire scar data from this site are available in FHX2 format at: # ftp://ftp.ncdc.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/usach021.fhx # along with associated metadata at: # ftp://ftp.ncdc.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/usach021.txt # # Methods: See Brown and Wu 2005. Increment cores were removed from 10 cm # height above ground level on living trees and cross sections were cut # from logs and snags such that one surface was 10 cm above the estimated # root-shoot boundary. Sampled cores were no more than a field estimated # 10 yr from pith to minimize pith offset when assessing pith date. On # increment cores and cross sections that did not include pith but inside # ring curvature was visible, pith dates were estimated using overlaid # concentric circles of varying diameters that take into account both # average inside ring widths and an estimated distance to pith. Pith dates # at 10 cm height were corrected to germination dates by subtracting # 5 yr, the average time we estimated for seedlings to grow from germination # to 10 cm height (P. M. Brown, unpublished data). # # Reference: P.M. Brown & R. Wu. 2005. Climate and disturbance forcing of # episodic tree recruitment in a southwestern ponderosa pine landscape. # Ecology 86:3030-3038. # # Abstract: Strong but relatively short (annual to decadal length) climate # change can have broad-scale and long-lasting effects on forest communities. # Climate impacts forests through direct effects on tree demography (mortality # and overstory recruitment) and indirect effects on disturbance regimes. # Here, we compare multicentury chronologies of tree recruitment from a # 307-ha ponderosa pine forest in southwestern Colorado to reconstructions # of fire years, hydroclimate, and the El Nino-Southern Oscillation (ENSO). # Few trees predate a regional multiyear megadrought centered in the 1580s. A # prolonged pluvial in the early 1600s resulted in a pulse of tree recruitment # that corresponds to recruitment seen over much of the Southwest. Other cohorts # in the early 1700s and mid-1800s established during multidecadal fire- # quiescent periods. These periods correspond to shifts in ENSO that apparently # resulted in dampening of interannual wet/dry oscillations responsible for # fuel buildup and drying. Fires, mediated by stochastic climate variation, # acted as a density independent regulation on tree populations since # establishment was not limited by overstory tree density, but rather by # fire-caused mortality of seedlings and saplings during periods of more # frequent fires. Even-aged cohorts in ponderosa pine forests likely have # little if anything to do with episodic mortality caused by more severe # fires, but rather relate mainly to episodic recruitment opportunities. # Fire cessation after Euro-American settlement in the late 1800s resulted # in an increase in tree density and changes in forest composition, which # are major factors that have contributed to recent severe wildfires in other # Southwestern forests. Our results document clear linkages between synoptic # climate forcing, fires, and recruitment episodes, and highlight the # importance of regional historical processes on contemporary forest # composition and structure. # # Comments: The first 2 letters of the tree ID represents the species: PP=Pinus # ponderosa, JS=Juniperus scopulorum, PM=Pseudotsuga menziesii. # 1 Tree ID 2 Year 3 Feature PPC63,1880,pith PPC63,2002,bark PMC64,1733,earliest ring PMC64,2002,bark PMC65,1747,pith PMC65,2002,bark PMC66,1782,earliest ring PMC66,2002,bark PPC67,1675,pith PPC67,2002,bark PPC69,1676,pith PPC69,2002,bark PMC610,1920,pith PMC610,2002,bark PPC611,1577,pith PPC611,1801,fire scar undetermined PPC611,1802,last ring PPC612,1579,pith PPC612,1852,last ring JSC614,1902,earliest ring JSC614,2002,bark PMC615,1885,pith PMC615,2002,bark PPC616,1882,pith PPC616,2002,bark PPC617,1869,pith PPC617,2002,bark PPC618,1816,pith PPC618,2002,bark PMC620,1889,pith PMC620,2002,bark PMC622,1880,pith PMC622,2002,bark PMC624,1882,pith PMC624,2002,bark PMC627,1882,pith PMC627,2002,bark PPC629,1900,pith PPC629,2002,bark