Orlando Acevedo-Charry, Scott K. Robinson, Bette A. Loiselle, Miguel A. Acevedo
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引用次数: 0
Abstract
Poor-soil Amazonian ecosystems, such as white-sand ecosystems (WSE, sensu lato), were widespread in the past, reflecting a diverse origin, and have a history of repeated expansion and contraction in response to climate fluctuations and landscape reconfiguration. Although modern climate change outpaces natural processes, we hypothesize that soil nutrient degradation will trigger a cascade of ecosystem reconfigurations, favoring the eventual expansion of WSE-like habitats long into the future. This expansion may be a nuanced aspect of the broader process of Amazon degradation. Long-term monitoring and field experiments remain necessary to test these predictions regarding the “once and future” Amazon Forest.
贫瘠土壤的亚马逊生态系统,如白沙生态系统(WSE, sensu lato),在过去广泛分布,反映了多样化的起源,并具有响应气候波动和景观重构的反复扩张和收缩的历史。尽管现代气候变化超过了自然过程,但我们假设土壤养分退化将引发一系列生态系统重新配置,有利于在未来很长一段时间内最终扩大类似wse的栖息地。这种扩张可能是亚马逊退化过程中一个微妙的方面。为了验证这些关于“曾经和未来”亚马逊森林的预测,长期监测和实地实验仍然是必要的。
期刊介绍:
Ranked by the ISI index, Biotropica is a highly regarded source of original research on the ecology, conservation and management of all tropical ecosystems, and on the evolution, behavior, and population biology of tropical organisms. Published on behalf of the Association of Tropical Biology and Conservation, the journal''s Special Issues and Special Sections quickly become indispensable references for researchers in the field. Biotropica publishes timely Papers, Reviews, Commentaries, and Insights. Commentaries generate thought-provoking ideas that frequently initiate fruitful debate and discussion, while Reviews provide authoritative and analytical overviews of topics of current conservation or ecological importance. The newly instituted category Insights replaces Short Communications.