Patterns of boreal permafrost peatland vegetation across environmental gradients sensitive to climate warming

被引:3
作者
Camill, P [1 ]
机构
[1] Duke Univ, Dept Bot, Durham, NC 27708 USA
来源
CANADIAN JOURNAL OF BOTANY-REVUE CANADIENNE DE BOTANIQUE | 1999年 / 77卷 / 05期
关键词
bogs; fens; boreal; permafrost; vegetation; ordination;
D O I
10.1139/b99-008
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
This study documents changes in community and functional group across environmental gradients sensitive to climate warming in boreal permafrost peatlands and describes how future changes in temperature and precipitation may lead to changes in species composition and ecosystem properties. At the landscape scale, the presence of permafrost strongly influenced species composition. The position of permafrost thaw affected surface water pH and species composition. At local scales, a combination of water table depth and vegetation structure strongly controlled community composition. Permafrost plateau plots with high Picea mariana basal area were characterized by darker and drier understorey conditions, low cover of Sphagnum fuscum, Ledum groenlandicum, and lichen, and high cover of feather mosses. Aquatic collapse scar plots were dominated by aquaticSphagnum and Carex, whereas more xeric plots were dominated by hummock Sphagnum and ericaceous shrubs. Functional group responses indicated that changing environmental conditions with climate warming may have significant impacts on community composition and ecosystem processes. A decomposition example is presented to show how changes in species and functional group composition could have important implications for ecosystem-level processes like peat accumulation during climate warming.
引用
收藏
页码:721 / 733
页数:13
相关论文
共 66 条
[1]   A CHECKLIST OF SPHAGNUM IN NORTH-AMERICA NORTH OF MEXICO [J].
ANDERSON, LE .
BRYOLOGIST, 1990, 93 (04) :500-501
[2]   LIST OF THE MOSSES OF NORTH-AMERICA NORTH OF MEXICO [J].
ANDERSON, LE ;
CRUM, HA ;
BUCK, WR .
BRYOLOGIST, 1990, 93 (04) :448-499
[3]  
[Anonymous], 1994, Modern applied statistics with S-Plus
[4]   ARCTIC TUNDRA - A SOURCE OR SINK FOR ATMOSPHERIC CARBON-DIOXIDE IN A CHANGING ENVIRONMENT [J].
BILLINGS, WD ;
LUKEN, JO ;
MORTENSEN, DA ;
PETERSON, KM .
OECOLOGIA, 1982, 53 (01) :7-11
[5]  
BOER GJ, 1992, J CLIMATE, V5, P1045, DOI 10.1175/1520-0442(1992)005<1045:GGCCSW>2.0.CO
[6]  
2
[7]   Multiple limiting gradients in peatlands: A call for a new paradigm [J].
Bridgham, SD ;
Pastor, J ;
Janssens, JA ;
Chapin, C ;
Malterer, TJ .
WETLANDS, 1996, 16 (01) :45-65
[8]  
Brown R. J. E., 1973, PERMAFROST, P71
[9]   A LATE WISCONSIN AND HOLOCENE VEGETATION HISTORY FROM THE CENTRAL BROOKS RANGE - IMPLICATIONS FOR ALASKAN PALEOCOLOGY [J].
BRUBAKER, LB ;
GARFINKEL, HL ;
EDWARDS, ME .
QUATERNARY RESEARCH, 1983, 20 (02) :194-214
[10]   Climate change disequilibrium of boreal permafrost peatlands caused by local processes [J].
Camill, P ;
Clark, JS .
AMERICAN NATURALIST, 1998, 151 (03) :207-222