Coarse woody debris in sub-boreal spruce forests of west-central British Columbia

An evaluation of how coarse woody debris (CWD) changes in quantity and quality during stand development was conducted using a 426-year chronosequence of 71 stands in sub-boreal forests in British Columbia. Additional characteristics of CWD were determined in 14 of the stands. Most stands are fire initiated and input from the predisturbance stand is critical in controlling the amounts and characteristics of CWD within young stands. Log volume declines from over 100 m(3)/ha in young stands (0-50 years) to just over 60 m(3)/ha in stands from 51 to 200 years old, and then increases to greater than 140 m(3)/ha in the oldest (greater than or equal to 400-year-old) stands. Mean snag basal area is highest (31.6 m(2)ha) in young, postfire stands, decreases to a very low value (2.0 m(2)/ha) in stands 51-100 years old, and then reaches a second maximum (12.1 m(2)/ha) in stands that are 201-250 years old; it declines slightly in very old stands. The high snag basal area in stands 201-250 years old coincides with the successional transition from lodgepole pine (Pinus contorta Dougl, ex Loud. var. latifolia Engelm.) to stands dominated by subalpine fir (Abies lasiocarpa (Hook.) Nutt.) and interior spruce (hybrids of Picea glauca (Moench) Voss and Picea engelmannii Parry). Stand age, characteristics of the predisturbance forest, and the disturbance history of stands subsequent to stand initiation all appear to be very important in determining variation in both the quality and quantity of CWD in these sub-boreal forests.