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使用示踪技术测量草本植物、幼树和树木的根生态位分隔。

Root niche partitioning among grasses, saplings, and trees measured using a tracer technique.

机构信息

Department of Biological Sciences, University of Alaska, Anchorage, AK 99508, USA.

出版信息

Oecologia. 2013 Jan;171(1):25-37. doi: 10.1007/s00442-012-2390-0. Epub 2012 Jul 3.

Abstract

Niche partitioning of resources by plants is believed to be a fundamental aspect of plant coexistence and biogeochemical cycles; however, measurements of the timing and location of resource use are often lacking because of the difficulties of belowground research. To measure niche partitioning of soil water by grasses, planted saplings, and trees in a mesic savanna (Kruger National Park, South Africa), we injected deuterium oxide into 102,000 points in 15, 154-m(2) plots randomly assigned to one of five depths (0-120 cm) and one of three time periods during the 2008/2009 growing season. Grasses, saplings and trees all demonstrated an exponential decline in water uptake early in the season when resources were abundant. Later in the season, when resources were scarce, grasses continued to extract the most water from the shallowest soil depths (5 cm), but saplings and trees shifted water uptake to deeper depths (30-60 cm). Saplings, in particular, rapidly established roots to at least 1 m and used these deep roots to a greater extent than grasses or trees. Helping to resolve contradictory observations of the relative importance of deep and shallow roots, our results showed that grasses, saplings and trees all extract the most water from shallow soils when it is available but that woody plants can rapidly shift water uptake to deeper soils when resources are scarce. Results highlight the importance of temporal changes in water uptake and the problems with inferring spatial and temporal partitioning of soil water uptake from root biomass measurements alone.

摘要

植物对资源的生态位分割被认为是植物共存和生物地球化学循环的一个基本方面;然而,由于地下研究的困难,往往缺乏对资源利用的时间和位置的测量。为了测量中湿稀树草原(南非克鲁格国家公园)中草、种植的树苗和树木对土壤水分的生态位分割,我们在 2008/2009 生长季的三个时间阶段之一和五个深度之一的 154 平方米(15 米 x 10 米)的 152 个随机分配的 102000 个点中注入了重水。草、树苗和树木在资源丰富的季节早期都表现出了对水分吸收的指数下降。在季节后期,当资源稀缺时,草继续从最浅的土壤层(5 厘米)中提取最多的水分,但树苗和树木将水分吸收转移到更深的深度(30-60 厘米)。特别是树苗,迅速将根扎入至少 1 米的深度,并比草或树更广泛地利用这些深根。我们的研究结果有助于解决深根和浅根相对重要性的矛盾观察,表明当资源可用时,草、树苗和树木都从浅层土壤中提取最多的水分,但当资源稀缺时,木本植物可以迅速将水分吸收转移到更深的土壤中。研究结果强调了水分吸收的时间变化的重要性,以及仅从根生物量测量推断土壤水分吸收的时空分割所存在的问题。

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