The root system of individual layerings excavated in an 8 m diameter,
approximately 500-year-old clonal island of white spruce (Picea glauca
[Moench] Voss) on the forest-tundra near Churchill, Manitoba, consist
ed of roots in accumulating litter and peat within the island and one
or two main roots up to 12.25 m long extending into the surrounding li
chen-heath. One of the latter, recently dead, was 280 Fears old with a
n initial extension rate similar to roots of the early 1900s. Needle m
ass, wood surface area, sapwood volume and current annual mass of wood
were measured as estimates of carbon allocation in one layering. Belo
w ground, wood surface area and sapwood volume constituted 74% and 84%
respectively of the totals for woody material, substantially more tha
n the 47% of current wood production. Based on the size and distributi
on of roots, the island may be composed of 30-40 individual layerings,
most of which developed in the last 100 years.