气候变化对豆科赤藓属(Erythrina crista-galli L.)自然界限外潜在全球分布的影响

Luciano Moura de Mello
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引用次数: 0

摘要

外来物种对本地生物群的保护具有潜在的危险,因为它们逃避了捕食者、竞争者和病原体,而这些通常不会随着外来物种迁移到它们开始定居的地区。对本地物种的潜在分布进行建模是识别外来物种、引进物种和归化物种所占环境的重要工具。赤藓属(Erythrina crista-galli L.)是一种先锋植物,原产于巴西、乌拉圭、阿根廷、玻利维亚和巴拉圭。由于其生态特性,它有能力扩大其分布到新的可利用。本研究旨在确定南美以外的赤藓属植物的潜在分布区域,并对距今22000年的有利区域进行评估,以验证这些区域在其自然界限之外的扩张或缩小趋势。结果表明,该算法能够有效地指出该物种可能发生归化的区域,从而增加其在新的洲际边界的分布。在这些地区,由于其生态特性,红加利可能会影响当地的生态系统。该研究还指出,这些潜在地区的动态趋势与末次盛冰期以来发生的气候变化有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Influence of climate change on the potential global distribution of Erythrina crista-galli L. (Fabaceae) outside its natural limits
Exotic species are potentially dangerous for the conservation of native biota because they escapepredators, competitors and pathogens that usually are not displaced with the species to the areas inwhich they begin to colonize. The modeling of the potential distribution of occurrence of a nativespecies can be an important tool for the recognition of environments colonized by an exotic, introducedand naturalized species. Erythrina crista-galli L. (Fabaceae) is a pioneer species, native of Brazil,Uruguay, Argentina, Bolivia and Paraguay. Due to its ecological characteristics, it has the capacity toexpand its distribution to new available. This work aimed to identify the potential areas of distributionof Erythrina crista-galli L. outside South America, evaluating the favorable areas of 22,000 years BPuntil today as a way to verify the tendency of expansion or reduction of these territorial spaces outsideits natural limits. The results indicate that the algorithm used in modeling the distribution for the speciesis highly efficient in pointing out areas in which the naturalization of the species could occur, increasingits distribution to new intercontinental frontiers. In these areas E. crista-galli could, due to its ecologicalcharacteristics, impact these local ecosystems. The study also indicates what would be the trend ofdynamics of these potential areas in relation to the climatic changes that have occurred since the lastglacial maximum.
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