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热带森林物种组成的定向变化。

Directional changes in the species composition of a tropical forest.

机构信息

Department of Biological Sciences, Florida International University, Miami, Florida 33199, USA.

出版信息

Ecology. 2011 Apr;92(4):871-82. doi: 10.1890/10-0724.1.

Abstract

Long-term studies have revealed that the structure and dynamics of many tropical forests are changing, but the causes and consequences of these changes remain debated. To learn more about the forces driving changes within tropical forests, we investigated shifts in tree species composition over the past 25 years within the 50-ha Forest Dynamics Plot on Barro Colorado Island (BCI), Panama, and examined how observed patterns relate to predictions of (1) random population fluctuations, (2) carbon fertilization, (3) succession from past disturbance, (4) recovery from an extreme El Niño drought at the start of the study period, and (5) long-term climate change. We found that there have been consistent and directional changes in the tree species composition. These shifts have led to increased relative representations of drought-tolerant species as determined by the species' occurrence both across a gradient of soil moisture within BCI and across a wider precipitation gradient from a dry forest near the Pacific coast of Panama to a wet forest near its Caribbean coast. These nonrandom changes cannot be explained by stochastic fluctuations or carbon fertilization. They may be the legacy of the El Niño drought, or alternatively, potentially reflect increased aridity due to long-term climate change. By investigating compositional changes, we increased not only our understanding of the ecology of tropical forests and their responses to large-scale disturbances, but also our ability to predict how future global change will impact some of the critical services provided by these important ecosystems.

摘要

长期研究表明,许多热带森林的结构和动态正在发生变化,但这些变化的原因和后果仍存在争议。为了更多地了解驱动热带森林变化的力量,我们调查了过去 25 年来巴拿马巴罗科罗拉多岛上 50 公顷森林动态样地内树种组成的变化,并研究了观察到的模式与以下预测之间的关系:(1) 随机种群波动,(2) 碳施肥,(3) 过去干扰后的演替,(4) 研究开始时极端厄尔尼诺干旱后的恢复,以及(5) 长期气候变化。我们发现,树种组成已经发生了一致的和定向的变化。这些转变导致了耐旱物种相对代表度的增加,这是通过物种在巴罗科罗拉多岛土壤湿度梯度上的出现以及更广泛的降水梯度上的出现来确定的,该降水梯度从巴拿马太平洋沿岸的干燥森林到加勒比海沿岸的湿润森林。这些非随机变化不能用随机波动或碳施肥来解释。它们可能是厄尔尼诺干旱的遗留物,或者可能反映了由于长期气候变化导致的干旱加剧。通过研究组成变化,我们不仅提高了对热带森林生态及其对大规模干扰的反应的理解,而且提高了预测未来全球变化将如何影响这些重要生态系统提供的一些关键服务的能力。

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