首页> 外文OA文献 >Vegetation Dynamics at the Upper Reaches of a Tropical Montane Forest are Driven by Disturbance Over the Past 7300 Years
【2h】

Vegetation Dynamics at the Upper Reaches of a Tropical Montane Forest are Driven by Disturbance Over the Past 7300 Years

机译:热带山地森林上游的植被动态在过去7300年受到干扰的驱动

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

We assessed tropical montane cloud forest (TMCF) sensitivity to natural disturbance by drought, fire, and dieback with a 7300-year-long paleorecord. We analyzed pollen assemblages, charcoal accumulation rates, and higher plant biomarker compounds (average chain length [ACL] of n-alkanes) in sediments from Wai'ānapanapa, a small lake near the upper forest limit and the mean trade wind inversion (TWI) in Hawai‘i. The paleorecord of ACL suggests increased drought frequency and a lower TWI elevation from 2555–1323 cal yr B.P. and 606–334 cal yr B.P. Charcoal began to accumulate and a novel fire regime was initiated ca. 880 cal yr B.P., followed by a decreased fire return interval at ca. 550 cal yr B.P. Diebacks occurred at 2931, 2161, 1162, and 306 cal yr B.P., and two of these were independent of drought or fire. Pollen assemblages indicate that on average species composition changed only 2.8% per decade. These dynamics, though slight, were significantly associated with disturbance. The direction of species composition change varied with disturbance type. Drought was associated with significantly more vines and lianas; fire was associated with an increase in the tree fern Sadleria and indicators of open, disturbed landscapes at the expense of epiphytic ferns; whereas stand-scale dieback was associated with an increase in the tree fern Cibotium. Though this cloud forest was dynamic in response to past disturbance, it has recovered, suggesting a resilient TMCF with no evidence of state change in vegetation type (e.g., grassland or shrubland).
机译:我们以长达7300年的古记录评估了热带山地云雾森林(TMCF)对自然干旱,干旱,大火和枯萎的敏感性。我们分析了威阿纳帕纳帕(Wa'ānapanapa)沉积物中的花粉组合,木炭积累速率和较高的植物生物标记化合物(正构烷烃的平均链长[ACL]),靠近森林上限的小湖和平均贸易风反转(TWI)在夏威夷。 ACL的古记录表明,从公元前2555年至1323年,干旱频率增加且TWI升高较低。公元前606和334年木炭开始积累,并开始了新的燃烧方案。 B.P. 880 yr yr。,随后回火间隔减小,大约为公元550年死亡发生在公元前2931年,2161、1162和306 cal年,其中两个与干旱或火灾无关。花粉组合表明,平均物种组成每十年仅改变2.8%。这些动态,尽管轻微,但与干扰显着相关。物种组成变化的方向随干扰类型而变化。干旱与更多的葡萄藤和藤本植物有关。大火与树木蕨类植物萨德勒菌病的增加以及开阔,受干扰的景观指标有关,但以附生蕨类植物为代价。而林分规模的枯萎与树蕨Cibotium的增加有关。尽管此云雾森林是对过去干扰的动态响应,但已经恢复,表明TMCF具有弹性,没有证据表明植被类型(例如草地或灌木丛)的状态发生变化。

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