globalchange  > 过去全球变化的重建
DOI: 10.1186/s42408-019-0033-0
WOS记录号: WOS:000466437800001
论文题名:
Late Holocene fire history and charcoal decay in subtropical dry forests of Puerto Rico
作者: Huang, Wei1; Liu, Xianbin1; Gonzalez, Grizelle2; Zou, Xiaoming1,3
通讯作者: Zou, Xiaoming
刊名: FIRE ECOLOGY
ISSN: 1933-9747
出版年: 2019
卷: 15
语种: 英语
英文关键词: anthropology ; charcoal decay ; paleoclimate ; paleofire ; Puerto Rico forest ; soil charcoal
WOS关键词: SOIL CHARCOAL ; TROPICAL FORESTS ; STABLE-ISOTOPES ; CLIMATE-CHANGE ; BOREAL FOREST ; VEGETATION ; DISTURBANCE ; TEMPERATE ; DYNAMICS ; RECORDS
WOS学科分类: Ecology ; Forestry
WOS研究方向: Environmental Sciences & Ecology ; Forestry
英文摘要:

Background: Fire is an important disturbance that influences species composition, community structure, and ecosystem function in forests. Disturbances such as hurricanes and landslides are critical determinants of community structure to Caribbean forests, but few studies have addressed the effect of paleofire disturbance on forests in Puerto Rico, USA. Soil charcoal is widely used to reconstruct fire history. However, the occurrence and frequency of paleofire can be underestimated due to charcoal decay.


Results: We reconstructed the fire history of subtropical dry forests of Puerto Rico based on the analysis of soil macrocharcoal numbers adjusted by the negative exponential decay function of charcoal. Twenty-one fire events occurred over the last 1300 yr in the subtropical dry forest of northeastern Puerto Rico, and 10 fire events occurred over the last 4900 yr in the subtropical dry forest of southeastern Puerto Rico. The average turnover time of charcoal in these subtropical dry forest soils of Puerto Rico was 1000 to 1250 yr. Soil charcoal decay leads to an underestimation of one to two undetected fire events during the Late Holocene in the subtropical dry forests of Puerto Rico. The peak of paleofire events for subtropical dry forests in northeastern and southeastern Puerto Rico was broadly similar, occurring between 500 to 1300 calibrated years before present (cal yr BP; before present is understood to mean before 1950 AD). Fire frequency of the subtropical dry forests in Puerto Rico decreased after the immigration of Europeans in the past 500 yr. The fire that occurred between 4822 and 4854 cal yr BP can be interpreted as either a natural fire or a new record of a native peoples settlement in southeastern Puerto Rico. Fire became a frequent disturbance in the subtropical dry forest of Puerto Rico after the development of cultigens by native peoples.


Conclusions: Our data suggested that fire was a frequent disturbance and human activity was likely a dominant cause of these paleofires in the subtropical dry forests of Puerto Rico.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/136803
Appears in Collections:过去全球变化的重建

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作者单位: 1.Univ Puerto Rico, Coll Nat Sci, Dept Environm Sci, POB 70377, San Juan, PR 00936 USA
2.US Forest Serv, Int Inst Trop Forestry, USDA, 1201 Calle Ceiba, Rio Piedras, PR 00926 USA
3.Nanjing Forestry Univ, Coll Biol & Environm, 159 Longpan Rd, Nanjing 210037, Jiangsu, Peoples R China

Recommended Citation:
Huang, Wei,Liu, Xianbin,Gonzalez, Grizelle,et al. Late Holocene fire history and charcoal decay in subtropical dry forests of Puerto Rico[J]. FIRE ECOLOGY,2019-01-01,15
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