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哥伦比亚安第斯山脉北部的高海拔泥炭地。

The High-Elevation Peatlands of the Northern Andes, Colombia.

作者信息

Benavides Juan C, Vitt Dale H, Cooper David J

机构信息

Departamento de Ecología y Territorio, Pontificia Universidad Javeriana, Bogotá 110231, Colombia.

School of Biological Sciences, Plant Biology, Southern Illinois University, Carbondale, IL 62901-6509, USA.

出版信息

Plants (Basel). 2023 Feb 20;12(4):955. doi: 10.3390/plants12040955.

Abstract

Andean peatlands are important carbon reservoirs for countries in the northern Andes and have a unique diversity. Peatland plant diversity is generally related to hydrology and water chemistry, and the response of the vegetation in tropical high-elevation peatlands to changes in elevation, climate, and disturbance is poorly understood. Here, we address the questions of what the main vegetation types of peat-forming vegetation in the northern Andes are, and how the different vegetation types are related to water chemistry and pH. We measured plant diversity in 121 peatlands. We identified a total of 264 species, including 124 bryophytes and 140 vascular plants. We differentiated five main vegetation types: cushion plants, , true mosses, sedges, and grasses. Cushion-dominated peatlands are restricted to elevations above 4000 m. Variation in peatland vegetation is mostly driven be elevation and water chemistry. Encroachment of sedges and in disturbed sites was associated with a reduction in soil carbon. We conclude that peatland variation is driven first by elevation and climate followed by water chemistry and human disturbances. Sites with higher human disturbances had lower carbon content. Peat-forming vegetation in the northern Andes was unique to each site bringing challenges on how to better conserve them and the ecosystem services they offer.

摘要

安第斯泥炭地是安第斯山脉北部国家重要的碳库,具有独特的多样性。泥炭地植物多样性通常与水文和水化学有关,而热带高海拔泥炭地植被对海拔、气候和干扰变化的响应尚不清楚。在这里,我们探讨了安第斯山脉北部形成泥炭的植被的主要植被类型是什么,以及不同的植被类型如何与水化学和pH值相关。我们测量了121个泥炭地的植物多样性。我们共鉴定出264种植物,其中包括124种苔藓植物和140种维管植物。我们区分了五种主要植被类型:垫状植物、 、真藓、莎草和禾本科植物。以垫状植物为主的泥炭地仅限于海拔4000米以上。泥炭地植被的变化主要受海拔和水化学的驱动。在受干扰的地点,莎草和 的入侵与土壤碳的减少有关。我们得出结论,泥炭地变化首先由海拔和气候驱动,其次是水化学和人类干扰。人类干扰较大的地点碳含量较低。安第斯山脉北部形成泥炭的植被在每个地点都很独特,这给如何更好地保护它们以及它们提供的生态系统服务带来了挑战。

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