首页> 外文OA文献 >Effects of Quaternary Climatic Fluctuations on the Distribution of Neotropical Savanna Tree Species
【2h】

Effects of Quaternary Climatic Fluctuations on the Distribution of Neotropical Savanna Tree Species

机译:第四纪气候波动对新热带稀树草原树种分布的影响

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

In order to develop niche models for tree species characteristic of thecerrado vegetation (woody savannas) of central South America, and tohindcast their distributions during the Last Glacial Maximum and Last Inter-Glacial, we compiled a dataset of tree species checklists for typical cerradovegetation (n=282) and other geographically co-occurring vegetationtypes, e.g. seasonally dry tropical forest (n=355). We then performed anIndicator Species Analysis to select ten species that best characterizetypical cerrado vegetation and developed niche models for them using theMaxent algorithm. We used these models to assess the probability ofoccurrence of each species across South America at the following timeslices: Current (0 ka pre-industrial), Holocene (6 ka BP), Last GlacialMaximum (LGM - 21 ka BP), and Last Interglacial (LIG - 130 ka BP). Theniche models were robust for all species and showed the highest probabilityof occurrence in the core area of the Cerrado Domain. The palaeomodelssuggested changes in the distributions of cerrado tree species throughoutthe Quaternary, with expansion during the LIG into the adjacentAmazonian and Atlantic moist forests, as well as connections with otherSouth American savannas. The LGM models suggested a retraction ofcerrado vegetation to inter-tableland depressions and slopes of the CentralBrazilian Highlands. Contrary to previous hypotheses, such as thePleistocene Refuge Theory, we found that the widest expansion of cerradotree species seems to have occurred during the LIG, most probably due toits warmer climate. On the other hand, the postulated retractions duringthe LGM were likely related to both decreased precipitation andtemperature. These results are congruent with palynological andphylogeographic studies in the Cerrado Domain.
机译:为了开发南美中部cererado植被(木本稀树草原)的树种特征的利基模型,并在最后一次冰期最大值和最后一次冰期之间对它们的分布进行后推,我们为典型的植被植被(n = 282)和其他地理上同时出现的植被类型,例如季节性干燥的热带森林(n = 355)。然后,我们进行了指标物种分析,以选择十种最能代表典型塞拉多植被的物种,并使用Maxent算法为其开发了生态位模型。我们使用这些模型在以下时间片上评估了南美各个物种的发生概率:当前(工业前0 ka),全新世(6 ka BP),最大冰川最大(LGM-21 ka BP)和最后冰川间( LIG-130 ka BP)。 Theniche模型对所有物种都具有鲁棒性,并且在塞拉多地区的核心区域显示出最高的发生概率。古模型建议整个第四纪塞拉多树种的分布发生变化,在LIG期间扩展到邻近的亚马逊和大西洋湿润森林,以及与其他南美大草原的联系。 LGM模型建议将cerrado植被退回至巴西中部高地的高原间洼地和山坡。与以前的假设(例如更新世避难所理论)相反,我们发现在LIG期间,塞拉多树种的扩展最为广泛,这很可能是由于其气候变暖所致。另一方面,LGM期间假定的收缩可能与降水减少和温度降低有关。这些结果与塞拉多地区的古生物学和植物学研究一致。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号