Consequences of depletion of stratospheric ozone for terrestrial Antarcticecosystems: the response of Deschampsia antarctica to enhanced UV-B radiation in a controlled environment
J. Rozema et al., Consequences of depletion of stratospheric ozone for terrestrial Antarcticecosystems: the response of Deschampsia antarctica to enhanced UV-B radiation in a controlled environment, PLANT ECOL, 154(1-2), 2001, pp. 101
Mini UV lamps were installed over antarctic plants at Leonie Island, Antarc
tic peninsula, and shoot length measurements of Deschampsia antarctica were
performed during the austral summer January-February 1999.
We studied the response of the antarctic hairgrass, Deschampsia antarctica
to enhanced UV-B. In a climate room experiment we exposed tillers of Descha
mpsia antarctica, collected at Leonie Island, Antarctic peninsula, to ambie
nt and enhanced levels of UV-B radiation. In this climate room experiment w
ith 0, 2.5 and 5 kJ m(-2) day(-1) UV-B-BE treatments we observed that lengt
h growth of shoots at 2.5 and 5 kJ m(-2) day(-1) UV-B-BE was markedly reduc
ed compared to 0 kJ m(-2) day(-1) UV-B-BE. In addition, there was an increa
sed number of shoots and increased leaf thickness with enhanced UV-B. The R
elative Growth Rate (RGR) was not affected by UV-B, possibly because reduce
d shoot length growth by enhanced UV-B was compensated by increased tilleri
ng. Light response curves of net leaf photosynthesis of plants exposed to 5
kJ m(-2) day(-)1 UV-BBE did not differ from those exposed to 0 kJ m(-)2 da
y(-1) UV-B-BE. The content of UV-B absorbing compounds of plants exposed to
increasing UV-B did not significantly change.
Mini UV-B lamp systems were installed in the field, to expose the terrestri
al antarctic vegetation at Leonie Island to enhanced solar UV-B. In that st
udy, the increment of shoot length of tagged plants of Deschampsia antarcti
ca during the January-February 1999 at Leonie Island, was recorded and comp
ared to shoot length growth under controlled conditions.
The consequences of enhanced UV-B radiation as a result of ozone depletion
for the terrestrial antarctic ecosytems are discussed.