Nepstad Daniel C, Tohver Ingrid Marisa, Ray David, Moutinho Paulo, Cardinot Georgina
Woods Hole Research Center, 149 Woods Hole Road, Falmouth, Massachusetts 02540-1644, USA.
Ecology. 2007 Sep;88(9):2259-69. doi: 10.1890/06-1046.1.
Severe drought episodes such as those associated with El Niño Southern Oscillation (ENSO) events influence large areas of tropical forest and may become more frequent in the future. One of the most important forest responses to severe drought is tree mortality, which alters forest structure, composition, carbon content, and flammability, and which varies widely. This study tests the hypothesis that tree mortality increases abruptly during drought episodes when plant-available soil water (PAW) declines below a critical minimum threshold. It also examines the effect of tree size, plant life form (palm, liana, tree) and potential canopy position (understory, midcanopy, overstory) on drought-induced plant mortality. A severe, four-year drought episode was simulated by excluding 60% of incoming throughfall during each wet season using plastic panels installed in the understory of a 1-ha forest treatment plot, while a 1-ha control plot received normal rainfall. After 3.2 years, the treatment resulted in a 38% increase in mortality rates across all stems >2 cm dbh. Mortality rates increased 4.5-fold among large trees (>30 cm dbh) and twofold among medium trees (10-30 cm dbh) in response to the treatment, whereas the smallest stems were less responsive. Recruitment rates did not compensate for the elevated mortality of larger-diameter stems in the treatment plot. Overall, lianas proved more susceptible to drought-induced mortality than trees or palms, and potential overstory tree species were more vulnerable than midcanopy and understory species. Large stems contributed to 90% of the pretreatment live aboveground biomass in both plots. Large-tree mortality resulting from the treatment generated 3.4 times more dead biomass than the control plot. The dramatic mortality response suggests significant, adverse impacts on the global carbon cycle if climatic changes follow current trends.
诸如与厄尔尼诺南方涛动(ENSO)事件相关的严重干旱期会影响大片热带森林,且未来可能会更加频繁。森林对严重干旱最重要的反应之一是树木死亡,这会改变森林结构、组成、碳含量和易燃性,而且差异很大。本研究检验了这样一个假设:当植物可利用土壤水分(PAW)降至临界最低阈值以下时,干旱期树木死亡率会突然增加。研究还考察了树木大小、植物生活型(棕榈、藤本植物、树木)和潜在冠层位置(林下、中层冠层、上层冠层)对干旱诱导的植物死亡的影响。通过在1公顷森林处理样地的林下安装塑料板,在每个雨季排除60%的林冠穿透水,模拟了一场持续四年的严重干旱期,而1公顷的对照样地则接受正常降雨。3.2年后,处理导致所有胸径>2厘米的茎干死亡率增加了38%。作为对处理的响应,大树(胸径>30厘米)的死亡率增加了4.5倍,中等树木(胸径10 - 30厘米)的死亡率增加了两倍,而最小的茎干反应较小。补充率无法弥补处理样地中较大直径茎干死亡率的升高。总体而言,藤本植物比树木或棕榈更容易受到干旱诱导的死亡影响,潜在的上层树种比中层冠层和林下树种更脆弱。两个样地中,大树干贡献了预处理地上生物量的90%。处理导致的大树死亡产生的死亡生物量是对照样地的3.4倍。这种显著的死亡反应表明,如果气候变化遵循当前趋势,将对全球碳循环产生重大的不利影响。