Litter decomposition rates in Canadian forests

被引:167
作者
Moore, TR
Trofymow, JA
Taylor, B
Prescott, C
Camiré, C
Duschene, L
Fyles, J
Kozak, L
Kranabetter, M
Morrison, I
Siltanen, M
Smith, S
Titus, B
Visser, S
Wein, R
Zoltai, S
机构
[1] Canadian Forest Serv, Pacific Forestry Ctr, Victoria, BC V8Z 1M5, Canada
[2] McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada
[3] McGill Univ, Ctr Climate & Global Change Res, Montreal, PQ H3A 2K6, Canada
[4] Taylor Mazier Associates, St Andrews, NS B0H 1X0, Canada
[5] Univ British Columbia, Fac Forestry, Vancouver, BC V6T 1W5, Canada
[6] Univ Laval, Fac Foresterie & Geomat, St Foy, PQ G1K 7P4, Canada
[7] Canadian Forestry Serv, Great Lakes Forestry Res Ctr, Sault St Marie, ON, Canada
[8] McGill Univ, Dept Nat Resource Sci, Montreal, PQ, Canada
[9] BC Minist Forests, Smithers, BC, Canada
[10] Canadian Forestry Serv, No Forestry Ctr, Edmonton, AB, Canada
[11] Govt Yukon, Agr Branch, Whitehorse, YT, Canada
[12] Newfoundland Forestry Ctr, St Johns, NF, Canada
[13] Univ Calgary, Dept Biol, Calgary, AB T2N 1N4, Canada
[14] Univ Alberta, Dept Biol Sci, Edmonton, AB, Canada
关键词
climate change; decomposition; forests; lignin; litter; nitrogen;
D O I
10.1046/j.1365-2486.1998.00224.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
The effect of litter quality and climate on the rate of decomposition of plant tissues was examined by the measurement of mass remaining after 3 years' exposure of 11 litter types placed at 18 forest sites across Canada. Amongst sites, mass remaining was strongly related to mean annual temperature and precipitation and amongst litter types the ratio of Klason lignin to nitrogen in the initial tissue was the most important litter quality variable. When combined into a multiple regression, mean annual temperature, mean annual precipitation and Klason lignin:nitrogen ratio explained 73% of the variance in mass remaining for all sites and tissues. Using three doubled CO2 GCM climate change scenarios for four Canadian regions, these relationships were used to predict increases in decomposition rate of 4-7% of contemporary rates (based on mass remaining after 3 years), because of increased temperature and precipitation. This increase may be partially offset by evidence that plants growing under elevated atmospheric CO2 concentrations produce litter with high lignin:nitrogen ratios which slows the rate of decomposition, but this change will be small compared to the increased rate of decomposition derived from climatic changes.
引用
收藏
页码:75 / 82
页数:8
相关论文
共 43 条
[21]   NUTRIENT-UPTAKE AND GROWTH-RESPONSES OF VIRGINIA PINE TO ELEVATED ATMOSPHERIC CARBON-DIOXIDE [J].
LUXMOORE, RJ ;
ONEILL, EG ;
ELLS, JM ;
ROGERS, HH .
JOURNAL OF ENVIRONMENTAL QUALITY, 1986, 15 (03) :244-251
[22]  
MANABE S, 1991, J CLIMATE, V4, P785, DOI 10.1175/1520-0442(1991)004<0785:TROACO>2.0.CO
[23]  
2
[24]   THE GEOGRAPHY OF ORGANIC DECOMPOSITION RATES [J].
MEENTEMEYER, V .
ANNALS OF THE ASSOCIATION OF AMERICAN GEOGRAPHERS, 1984, 74 (04) :551-560
[25]   MACROCLIMATE AND LIGNIN CONTROL OF LITTER DECOMPOSITION RATES [J].
MEENTEMEYER, V .
ECOLOGY, 1978, 59 (03) :465-472
[26]   Regional Variation in Rate of Mass Loss of Pinus sylvestris Needle Litter in Swedish Pine Forests as Influenced by Climate and Litter Quality [J].
Meentemeyer, Vernon ;
Berg, Bjorn .
SCANDINAVIAN JOURNAL OF FOREST RESEARCH, 1986, 1 (1-4) :167-180
[27]   NITROGEN AND LIGNIN CONTROL OF HARDWOOD LEAF LITTER DECOMPOSITION DYNAMICS [J].
MELILLO, JM ;
ABER, JD ;
Muratore, JF .
ECOLOGY, 1982, 63 (03) :621-626
[28]   GLOBAL CLIMATE-CHANGE AND TERRESTRIAL NET PRIMARY PRODUCTION [J].
MELILLO, JM ;
MCGUIRE, AD ;
KICKLIGHTER, DW ;
MOORE, B ;
VOROSMARTY, CJ ;
SCHLOSS, AL .
NATURE, 1993, 363 (6426) :234-240
[29]  
MELILLO JM, 1996, SCOPE REPORT, V56, P199
[30]   Carbon-nitrogen interactions in CO2-enriched white oak: physiological and long-term perspectives [J].
Norby, Richard J. ;
Pastor, John ;
Melillo, Jerry M. .
TREE PHYSIOLOGY, 1986, 2 (1-3) :233-241