CARBON POOLS AND FLUX OF GLOBAL FOREST ECOSYSTEMS

被引:2580
|
作者
DIXON, RK
BROWN, S
HOUGHTON, RA
SOLOMON, AM
TREXLER, MC
WISNIEWSKI, J
机构
[1] TREXLER & ASSOCIATES INC, OAK GROVE, OR 97267 USA
[2] WISNIEWSKI & ASSOCIATES INC, FALLS CHURCH, VA 22043 USA
[3] UNIV ILLINOIS, DEPT FORESTRY, URBANA, IL 61801 USA
[4] WOODS HOLE RES CTR, WOODS HOLE, MA 02543 USA
关键词
D O I
10.1126/science.263.5144.185
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Forest systems cover more than 4.1 x 10(9) hectares of the Earth's land area. Globally, forest vegetation and soils contain about 1146 petagrams of carbon, with approximately 37 percent of this carbon in low-latitude forests, 14 percent in mid-latitudes, and 49 percent at high latitudes. Over two-thirds of the carbon in forest ecosystems is contained in soils and associated peat deposits. In 1990, deforestation in the low latitudes emitted 1.6 +/- 0.4 petagrams of carbon per year, whereas forest area expansion and growth in mid- and high-latitude forest sequestered 0.7 +/- 0.2 petagrams of carbon per year, for a net flux to the atmosphere of 0.9 +/- 0.4 petagrams of carbon per year. Slowing deforestation, combined with an increase in forestation and other management measures to improve forest ecosystem productivity, could conserve or sequester significant quantities of carbon. Future forest carbon cycling trends attributable to losses and regrowth associated with global climate and land-use change are uncertain. Model projections and some results suggest that forests could be carbon sinks or sources in the future.
引用
收藏
页码:185 / 190
页数:6
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