Peak detection in sediment-charcoal records: impacts of alternative data analysis methods on fire-history interpretations

被引:263
作者
Higuera, Philip E. [1 ]
Gavin, Daniel G. [2 ]
Bartlein, Patrick J. [2 ]
Hallett, Douglas J. [3 ,4 ]
机构
[1] Univ Idaho, Dept Forest Ecol & Biogeosci, Moscow, ID 83844 USA
[2] Univ Oregon, Dept Geog, Eugene, OR 97493 USA
[3] Univ Calgary, Biogeosci Inst, Calgary, AB T2N 1N4, Canada
[4] Queens Univ, Sch Environm Studies, Kingston, ON K7L 3N6, Canada
基金
美国国家科学基金会;
关键词
bias; paleoecology; sensitivity; YELLOWSTONE-NATIONAL-PARK; OREGON COAST RANGE; TREE-RING RECORDS; CLIMATE-CHANGE; POSTGLACIAL VEGETATION; NORTHWESTERN MINNESOTA; BRITISH-COLUMBIA; BOREAL FORESTS; NORTH-AMERICA; LATE-HOLOCENE;
D O I
10.1071/WF09134
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Over the past several decades, high-resolution sediment-charcoal records have been increasingly used to reconstruct local fire history. Data analysis methods usually involve a decomposition that detrends a charcoal series and then applies a threshold value to isolate individual peaks, which are interpreted as fire episodes. Despite the proliferation of these studies, methods have evolved largely in the absence of a thorough statistical framework. We describe eight alternative decomposition models (four detrending methods used with two threshold-determination methods) and evaluate their sensitivity to a set of known parameters integrated into simulated charcoal records. Results indicate that the combination of a globally defined threshold with specific detrending methods can produce strongly biased results, depending on whether or not variance in a charcoal record is stationary through time. These biases are largely eliminated by using a locally defined threshold, which adapts to changes in variability throughout a charcoal record. Applying the alternative decomposition methods on three previously published charcoal records largely supports our conclusions from simulated records. We also present a minimum-count test for empirical records, which reduces the likelihood of false positives when charcoal counts are low. We conclude by discussing how to evaluate when peak detection methods are warranted with a given sediment-charcoal record.
引用
收藏
页码:996 / 1014
页数:19
相关论文
共 75 条
[1]   Changes in fire regime explain the Holocene rise and fall of Abies balsamea in the coniferous forests of western Quebec, Canada [J].
Ali, Adam A. ;
Asselin, Hugo ;
Larouche, Alayn C. ;
Bergeron, Yves ;
Carcaillet, Christopher ;
Richard, Pierre J. H. .
HOLOCENE, 2008, 18 (05) :693-703
[2]   Comparing fire-history interpretations based on area, number and estimated volume of macroscopic charcoal in lake sediments [J].
Ali, Adam A. ;
Higuera, Philip E. ;
Bergeron, Yves ;
Carcaillet, Christopher .
QUATERNARY RESEARCH, 2009, 72 (03) :462-468
[3]   Long-term fire frequency variability in the eastern Canadian boreal forest: the influences of climate vs. local factors [J].
Ali, Adam A. ;
Carcaillet, Christopher ;
Bergeron, Yves .
GLOBAL CHANGE BIOLOGY, 2009, 15 (05) :1230-1241
[4]   Paired charcoal and tree-ring records of high-frequency Holocene fire from two New Mexico bog sites [J].
Allen, Craig D. ;
Anderson, R. Scott ;
Jass, Renata B. ;
Toney, Jaime L. ;
Baisan, Christopher H. .
INTERNATIONAL JOURNAL OF WILDLAND FIRE, 2008, 17 (01) :115-130
[5]   Holocene vegetation and fire regimes in subalpine and mixed conifer forests, southern Rocky Mountains, USA [J].
Anderson, R. S. ;
Allen, C. D. ;
Toney, J. L. ;
Jass, R. B. ;
Bair, A. N. .
INTERNATIONAL JOURNAL OF WILDLAND FIRE, 2008, 17 (01) :96-114
[6]   Holocene development of Boreal forests and fire regimes on the Kenai Lowlands of Alaska [J].
Anderson, R. S. ;
Hallett, D. J. ;
Berg, E. ;
Jass, R. B. ;
Toney, J. L. ;
de Fontaine, C. S. ;
DeVolder, A. .
HOLOCENE, 2006, 16 (06) :791-803
[7]   A 14 000 year sedimentary charcoal record of fire from the northern Sierra Nevada, Lake Tahoe Basin, California, USA [J].
Beaty, R. Matthew ;
Taylor, Alan H. .
HOLOCENE, 2009, 19 (03) :347-358
[8]  
Birks H.J.B., 2001, TRACKING ENV CHANGE
[9]  
Bretherton CS, 1999, J CLIMATE, V12, P1990, DOI 10.1175/1520-0442(1999)012<1990:TENOSD>2.0.CO
[10]  
2