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Regeneration patterns reveal contraction of ponderosa forests and little upward migration of pinyon juniper woodlands

机译:再生模式揭示了Ponderosa森林的收缩,拼豆杜松林地的起伏较小

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摘要

A recent severe drought caused widespread mortality of ponderosa pine (Pinus ponderosa) and pinyon pine (Pinus edulis) in forests and woodlands in the southwestern United States. The sustainability of these tree species in the region depends on adequate regeneration and perhaps movement to more climatologically favorable locations. We investigated tree regeneration and species migration along elevation gradients in three community types (pinyon juniper woodlands, woodland-forest ecotones, and ponderosa pine forests) and three soil parent materials (sedimentary, flow basalt, and volcanic cinder) at 27 sites in northern Arizona. We measured stand characteristics, historic cone production, and density of tree regeneration and small trees. All species produced cones at sites with cinder soil parent material but had little regeneration. Woodlands and woodland-forest ecotones had regeneration of pinyon pine and juniper despite earlier mortality of some mature pinyon trees. Regeneration of ponderosa pine was nearly absent in woodland-forest ecotones, suggesting eventual loss of ponderosa pine and transition to pinyon-juniper woodland. Forests had little regeneration and few small trees of any tree species, indicating little upward migration of pinyon pine and juniper. Occurrence of pinyon pine and juniper regeneration was associated with a suite of biotic and abiotic factors, including a negative relationship with temperature and a positive relationship with precipitation. Regeneration failure of ponderosa pine at woodland-forest ecotone and low-elevation forest sites coupled with limited upward migration of pinyon pine and juniper portends future losses of tree cover as climate continues to warm.
机译:最近在美国西南部的森林和林地中的柚子松(Pinus Pine)和拼音松(Pinus Edulis)引起了巨大的暴干。该地区中这些树种的可持续性取决于足够的再生,也许是移动到更加活跃的有利位置。我们调查了沿着三个社区类型(Pinyon Juniper Woodlands,Woodland-Forest Ecotones和Ponderososa Pine Forest)的梯度沿着海拔梯度迁移的树木再生和物种迁移,以及亚利桑那州北部的27个地点的三种土壤母材(沉积,流动玄武岩和火山煤渣) 。我们测量了实体特征,历史锥形生产和树木再生和小树的密度。所有物种在含有煤渣母体材料的地点产生锥体,但重新组成几乎没有。林地和林地林过渡带有pinyon松树和Juniper的再生尽管一些成熟的pinyon树木的早期死亡率。在林地 - 森林杂物中几乎不存在Ponderosa Pine的再生,这表明最终失去了Ponderosa Pine的损失和到拼豆杜松林地的过渡。森林几乎没有再生和少数任何树种的小树,表明拼音松树和杜松略微迁移。拼音松树和杜松再生的发生与一套生物和非生物因子有关,包括与温度的负面关系和与沉淀的阳性关系。在加上pinyon松树和杜松的限制向上迁移林地林过渡带和低海拔森林网站黄松有再生的失败预示着树木覆盖的未来损失,气候持续变暖。

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