Effects of tree density and stand age on carbon allocation patterns in postfire lodgepole pine

被引:121
作者
Litton, CM
Ryan, MG
Knight, DH
机构
[1] Univ Wyoming, Dept Bot, Laramie, WY 82071 USA
[2] US Forest Serv, USDA, Rocky Mt Res Stn, Ft Collins, CO 80526 USA
[3] Colorado State Univ, Dept Forest Sci, Ft Collins, CO 80523 USA
[4] Colorado State Univ, Grad Degreee Program Ecol, Ft Collins, CO 80523 USA
关键词
aboveground net primary productivity (ANPP); carbon pools; fluxes; and allocation patterns; fire; lodgepole pine; Pinus contorta; total belowground carbon allocation (TBCA); Yellowstone National Park; Wyoming;
D O I
10.1890/02-5291
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Validating the components of the carbon (C) budget in forest ecosystems is essential for developing allocation rules that allow accurate predictions of C pools and fluxes. In addition, a better understanding of the effects of natural disturbances on C cycling is critical, particularly in light of alterations to disturbance regimes that may occur with global climate change. However, quantitative data about how postfire differences in ecosystem structure affect C allocation patterns are lacking. For this study, we examined how above- and belowground C pools, fluxes, and allocation patterns varied with fire-initiated differences in tree density and stand age in lodgepole pine stands in Yellowstone National Park of four forest types: low (< 1000 trees/ha), moderate (7000-40 000 trees/ha), and high tree densities (>50 000 trees/ha) in 13-year-old stands, and in similar to110-year-old mature stands. C pools in live biomass and detritus were estimated with allometric equations and direct sampling. Aboveground net primary productivity (ANPP) was estimated as aboveground biomass increment plus fine litterfall, and total belowground carbon allocation (TBCA) was estimated using a C balance approach. Our results indicate that the magnitude of C pools and fluxes varies greatly with fire-initiated differences in tree density and stand age. Coarse woody debris and mineral soil carbon accounted for the majority of total ecosystem C in young stands (91-99%), in contrast to mature stands where the largest amount of C was found in live biomass (64%). ANPP and TBCA increased with tree density (mean ANPP was 59, 122, and 156 g C.m(-2)-yr(-1), and TBCA was 68, 237, and 306 g C.m(-2).yr(-1) for low-, moderate-, and high-density young stands, respectively), and with stand age (ANPP was 218 g C.m(-2).yr(-1) and TBCA was 382 g C.m(-2).yr(-1) for 110-year-old stands). ANPP and TBCA were positively correlated, and both variables were well correlated with leaf area index. Notably, the ratio of TBCA to (TBCA + ANPP) remained remarkably constant (0.63-0.66) across extreme gradients of tree density and stand age, differing only slightly for the low-density young stands (0.54). These results suggest that C allocation patterns in a postfire lodgepole pine ecosystem are independent of tree density and stand age.
引用
收藏
页码:460 / 475
页数:16
相关论文
共 66 条
[1]   Paired-tower measurements of carbon and energy fluxes following disturbance in the boreal forest [J].
Amiro, BD .
GLOBAL CHANGE BIOLOGY, 2001, 7 (03) :253-268
[2]   FOREST WILDFIRES AS A RECENT SOURCE OF CO2 AT NORTHERN LATITUDES [J].
AUCLAIR, AND ;
CARTER, TB .
CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE, 1993, 23 (08) :1528-1536
[3]  
Bashkin MA, 1998, ECOLOGY, V79, P828, DOI 10.1890/0012-9658(1998)079[0828:CISCFA]2.0.CO
[4]  
2
[5]   ION-EXCHANGE RESIN BAG METHOD FOR ASSESSING FOREST SOIL-NITROGEN AVAILABILITY [J].
BINKLEY, D ;
MATSON, P .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1983, 47 (05) :1050-1052
[6]   Effect of fire on soil-atmosphere exchange of methane and carbon dioxide in Canadian boreal forest sites [J].
Burke, RA ;
Zepp, RG ;
Tarr, MA ;
Miller, WL ;
Stocks, BJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D24) :29289-29300
[7]  
Chen WJ, 2002, CAN J FOREST RES, V32, P833, DOI [10.1139/x01-165, 10.1139/X01-165]
[8]  
Clark DA, 2001, ECOL APPL, V11, P356, DOI 10.1890/1051-0761(2001)011[0356:MNPPIF]2.0.CO
[9]  
2
[10]   ABOVE-GROUND AND BELOW-GROUND BIOMASS AND PRODUCTION OF LODGEPOLE PINE ON SITES WITH DIFFERING SOIL-MOISTURE REGIMES [J].
COMEAU, PG ;
KIMMINS, JP .
CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE, 1989, 19 (04) :447-454