Kulmatiski Andrew, Beard Karen H, Holdrege Martin C, February Edmund C
Department of Wildland Resources and the Ecology Center Utah State University Logan UT USA.
Department of Botany University of Cape Town Cape Town South Africa.
Ecol Evol. 2020 Aug 26;10(18):9776-9787. doi: 10.1002/ece3.6612. eCollection 2020 Sep.
Deep roots have long been thought to allow trees to coexist with shallow-rooted grasses. However, data demonstrating how root distributions affect water uptake and niche partitioning are uncommon.We describe tree and grass root distributions using a depth-specific tracer experiment six times over two years in a subtropical savanna, Kruger National Park, South Africa. These point-in-time measurements were then used in a soil water flow model to simulate continuous water uptake by depth and plant growth form (trees and grasses) across two growing seasons. This allowed estimates of the total amount of water a root distribution could absorb as well as the amount of water a root distribution could absorb in excess of the other rooting distribution (i.e., unique hydrological niche).Most active tree and grass roots were in shallow soils: The mean depth of water uptake was 22 cm for trees and 17 cm for grasses. Slightly deeper rooting distributions provided trees with 5% more soil water than the grasses in a drier season, but 13% less water in a wetter season. Small differences also provided each rooting distribution (tree or grass) with unique hydrological niches of 4 to 13 mm water.The effect of rooting distributions has long been inferred. By quantifying the depth and timing of water uptake, we demonstrated how even small differences in rooting distributions can provide plants with resource niches that can contribute to species coexistence. Differences in total water uptake and unique hydrological niche sizes were small in this system, but they indicated that tradeoffs in rooting strategies can be expected to contribute to tree and grass coexistence because 1) competitive advantages change over time and 2) plant growth forms always have access to a soil resource pool that is not available to the other plant growth form.
长期以来,人们一直认为深根能使树木与浅根草类共存。然而,关于根系分布如何影响水分吸收和生态位划分的数据并不常见。我们在南非克鲁格国家公园的亚热带稀树草原上,在两年内分六次使用深度特异性示踪剂实验来描述树木和草类的根系分布。然后,这些时间点测量数据被用于土壤水流模型,以模拟两个生长季节中不同深度和植物生长形式(树木和草类)的连续水分吸收情况。这使得我们能够估计根系分布能够吸收的总水量,以及一种根系分布相对于另一种根系分布能够额外吸收的水量(即独特的水文生态位)。树木和草类最活跃的根系都在浅层土壤中:树木的水分吸收平均深度为22厘米,草类为17厘米。在较干燥的季节,略深的根系分布使树木比草类多吸收5%的土壤水分,但在较湿润的季节则少吸收13%的水分。微小的差异也为每种根系分布(树木或草类)提供了4至13毫米水分的独特水文生态位。根系分布的影响长期以来一直是推断出来的。通过量化水分吸收的深度和时间,我们证明了即使根系分布的微小差异也能为植物提供有助于物种共存的资源生态位。在这个系统中,总吸水量和独特水文生态位大小的差异很小,但它们表明根系策略的权衡有望促进树木和草类的共存,因为1)竞争优势会随时间变化,2)植物生长形式总能获取另一种植物生长形式无法利用的土壤资源库。