Evidence for a recent increase in forest growth

被引:285
作者
McMahon, Sean M. [1 ,2 ]
Parker, Geoffrey G. [1 ]
Miller, Dawn R. [1 ]
机构
[1] Smithsonian Environm Res Ctr, Forest Ecol Grp, Edgewater, MD 21307 USA
[2] Smithsonian Trop Res Inst, Ctr Trop Forest Sci, APO, AA 34002 USA
关键词
biomass change; carbon cycle; carbon fertilization; climate change; forest stand dynamics; ABOVEGROUND BIOMASS ACCUMULATION; LONG-TERM; TROPICAL FOREST; CARBON-CYCLE; DYNAMICS; CHRONOSEQUENCE; SEQUESTRATION; ECOSYSTEMS; TEMPERATE; RESPONSES;
D O I
10.1073/pnas.0912376107
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
Forests and their soils contain the majority of the earth's terrestrial carbon stocks. Changes in patterns of tree growth can have a huge impact on atmospheric cycles, biogeochemical cycles, climate change, and biodiversity. Recent studies have shown increases in biomass across many forest types. This increase has been attributed to climate change. However, without knowing the disturbance history of a forest, growth could also be caused by normal recovery from unknown disturbances. Using a unique dataset of tree biomass collected over the past 22 years from 55 temperate forest plots with known land-use histories and stand ages ranging from 5 to 250 years, we found that recent biomass accumulation greatly exceeded the expected growth caused by natural recovery. We have also collected over 100 years of local weather measurements and 17 years of on-site atmospheric CO2 measurements that show consistent increases in line with globally observed climate-change patterns. Combined, these observations show that changes in temperature and CO2 that have been observed worldwide can fundamentally alter the rate of critical natural processes, which is predicted by biogeochemical models. Identifying this rate change is important to research on the current state of carbon stocks and the fluxes that influence how carbon moves between storage and the atmosphere. These results signal a pressing need to better understand the changes in growth rates in forest systems, which influence current and future states of the atmosphere and biosphere.
引用
收藏
页码:3611 / 3615
页数:5
相关论文
共 52 条
[11]  
Clark DA, 2002, ECOL APPL, V12, P3, DOI 10.1890/1051-0761(2002)012[0003:ATFAIC]2.0.CO
[12]  
2
[13]   Application of 1-M and 4-M resolution satellite data to ecological studies of tropical rain forests [J].
Clark, DB ;
Read, JM ;
Clark, ML ;
Cruz, AM ;
Dotti, MF ;
Clark, DA .
ECOLOGICAL APPLICATIONS, 2004, 14 (01) :61-74
[14]  
Clark JS, 2003, ECOLOGY, V84, P17, DOI 10.1890/0012-9658(2003)084[0017:CHTITT]2.0.CO
[15]  
2
[16]   Do temperate rainforest trees have a greater ability to acclimate to changing temperatures than tropical rainforest trees? [J].
Cunningham, SC ;
Read, J .
NEW PHYTOLOGIST, 2003, 157 (01) :55-64
[17]   Nitrogen saturation and net ecosystem production [J].
De Schrijver, An ;
Verheyen, Kris ;
Mertens, Jan ;
Staelens, Jeroen ;
Wuyts, Karen ;
Muys, Bart .
NATURE, 2008, 451 (7180) :E1-E1
[18]   Exceptional carbon uptake in European forests during the warm spring of 2007: a data-model analysis [J].
Delpierre, N. ;
Soudani, K. ;
Francois, C. ;
Koestner, B. ;
Pontailler, J. -Y. ;
Nikinmaa, E. ;
Misson, L. ;
Aubinet, M. ;
Bernhofer, C. ;
Granier, A. ;
Gruenwald, T. ;
Heinesch, B. ;
Longdoz, B. ;
Ourcival, J. -M. ;
Rambal, S. ;
Vesala, T. ;
Dufrene, E. .
GLOBAL CHANGE BIOLOGY, 2009, 15 (06) :1455-1474
[19]   A long-term record of carbon exchange in a boreal black spruce forest: means, responses to interannual variability, and decadal trends [J].
Dunn, Allison L. ;
Barford, Carol C. ;
Wofsy, Steven C. ;
Goulden, Michael L. ;
Daube, Bruce C. .
GLOBAL CHANGE BIOLOGY, 2007, 13 (03) :577-590
[20]  
Eyre F.H., 1980, Forest cover types of the United States and Canada