Ra. Monserud et al., CHANGE IN PHYTOMASS AND NET PRIMARY PRODUCTIVITY FOR SIBERIA FROM THEMIDHOLOCENE TO THE PRESENT, Global biogeochemical cycles, 9(2), 1995, pp. 213-226
Phytomass (live plant mass) and net primary productivity are major com
ponents of the terrestrial carbon balance. A major location for phytom
ass storage is the subcontinent of Siberia, which is dominated by exte
nsive reaches of taiga (boreal forest). The responsiveness of the phyt
omass component of the carbon pool is examined by comparing vegetation
in the mid-Holocene (4600-6000 years before present) to modern potent
ial vegetation. The mid-Holocene was warmer and moister in middle and
northern Siberia than today, producing conditions ideal for boreal for
est growth. As a result, both northern and middle taiga were dominated
by shade-tolerant dark-needled species that thrive in moist climates.
Today, shade-tolerant dark-needled taiga is restricted to western Sib
eria and the highlands of central Siberia, with its central and easter
n components in the mid-Holocene replaced today by light-demanding lig
ht-needled species with lower productivity and phytomass. Total phytom
ass in Siberia in the mid-Holocene was 105.0 +/- 3.1 Pg, compared to 8
5.9 +/- 3.2 Pg in modern times, a loss of 19.1 +/- 3.1 Pg of phytomass
. The reduction in dark-needled northern and middle taiga classes resu
lts in a loss of 28.8 Pg, while the expansion of the corresponding lig
ht-needled taiga results in a gain of 13.5 Pg, a net loss of 15.3 Pg.
The loss is actually greater, because the modern figures are for poten
tial vegetation and not adjusted for agriculture and other anthropogen
ic disturbances. Given long periods for vegetation to approach equilib
rium with climate, the phytomass component of the carbon pool is respo
nsive to climate change. Changes in net primary productivity (NPP) for
Siberia between the mid-Holocene and the present were not as large as
changes in phytomass. A minor decrease in NPP (0.6 Pg yr(-1), 10%) ha
s occurred under our cooler modern climate, primarily due to the shift
from dark-needled taiga in the mid-Holocene to light-needled taiga to
day.