Jm. Welker et al., RESPONSES OF DRYAS-OCTOPETALA TO ITEX ENVIRONMENTAL MANIPULATIONS - ASYNTHESIS WITH CIRCUMPOLAR COMPARISONS, Global change biology, 3, 1997, pp. 61-73
We have examined organismic responses of Dryas octopetala to simulated
changes in the summer climate at four tundra sites as part of the Int
ernational Tundra Experiment (ITEX). Our study sites are located in th
e High Arctic, on Svalbard, Norway in the Low Arctic at Abisko, Sweden
, and at Toolik Lake, Alaska, USA and our temperate alpine site is at
Niwot Ridge, Colorado, USA. These sites represent a range of tundra te
mperature and precipitation regimes, being generally cold and dry in t
he High Arctic and warmer and wetter at Toolik Lake and Niwot Ridge. R
esults from our studies indicate organismic attributes such as floweri
ng shoot length varies by 30% between low and high arctic populations
and that experimental warming results in significant increases in shoo
t height at three of four sites. We find that phenological development
of Dryas is accelerated under experimentally warmed conditions which
corresponds with a lengthening of the growing season in autumn, greate
r degrees of seed set and a higher likelihood of colonization of bare
ground. We also observe that Dryas dominated ecosystems which are expo
sed to experimental manipulations are capable of exhibiting net carbon
sequestration in late autumn, and that Dryas photosynthesis and green
leaf biomass is significantly greater under warmer as opposed to ambi
ent temperature conditions. Dryas leaf nitrogen is also significantly
lowered under warmer conditions resulting in senescent leaves having a
higher C:N ratio than those under ambient conditions. Together these
findings indicate that Dryas phenology and carbon flux may be altered
to the greatest degree in spring and again in autumn by higher summer
temperatures and that simultaneously both positive and negative feedba
ck effects may result from changes in plant and ecosystem performance.