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土壤特性解释了磷亏缺热带森林中树木的生长和死亡,但不能解释生物量。

Soil properties explain tree growth and mortality, but not biomass, across phosphorus-depleted tropical forests.

机构信息

Climate and Ecosystem Science Division, Lawrence Berkeley National Laboratory, Berkeley, 94720, California, USA.

PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Wilrijk, 2610, Belgium.

出版信息

Sci Rep. 2020 Feb 10;10(1):2302. doi: 10.1038/s41598-020-58913-8.

Abstract

We observed strong positive relationships between soil properties and forest dynamics of growth and mortality across twelve primary lowland tropical forests in a phosphorus-poor region of the Guiana Shield. Average tree growth (diameter at breast height) increased from 0.81 to 2.1 mm yr along a soil texture gradient from 0 to 67% clay, and increasing metal-oxide content. Soil organic carbon stocks in the top 30 cm ranged from 30 to 118 tons C ha, phosphorus content ranged from 7 to 600 mg kg soil, and the relative abundance of arbuscular mycorrhizal fungi ranged from 0 to 50%, all positively correlating with soil clay, and iron and aluminum oxide and hydroxide content. In contrast, already low extractable phosphorus (Bray P) content decreased from 4.4 to <0.02 mg kg in soil with increasing clay content. A greater prevalence of arbuscular mycorrhizal fungi in more clayey forests that had higher tree growth and mortality, but not biomass, indicates that despite the greater investment in nutrient uptake required, soils with higher clay content may actually serve to sustain high tree growth in tropical forests by avoiding phosphorus losses from the ecosystem. Our study demonstrates how variation in soil properties that retain carbon and nutrients can help to explain variation in tropical forest growth and mortality, but not biomass, by requiring niche specialization and contributing to biogeochemical diversification across this region.

摘要

我们在圭亚那盾磷贫乏地区的 12 个主要低地热带森林中观察到,土壤特性与森林生长和死亡率之间存在强烈的正相关关系。平均树木生长(胸径)从 0 到 67%的粘土地段从 0.81 毫米/年增加到 2.1 毫米/年,而金属氧化物含量也在增加。在 30 厘米的表层土壤中,有机碳储量从 30 吨 C/公顷到 118 吨 C/公顷不等,磷含量从 7 毫克/千克土壤到 600 毫克/千克土壤不等,丛枝菌根真菌的相对丰度从 0 到 50%不等,所有这些都与土壤粘粒以及铁和铝的氧化物和氢氧化物含量呈正相关。相比之下,在粘粒含量增加的土壤中,原本就较低的可提取磷(Bray P)含量从 4.4 毫克/千克降低到<0.02 毫克/千克。在粘粒含量较高的森林中,丛枝菌根真菌的丰度更高,树木生长和死亡率更高,但生物量没有增加,这表明尽管需要更大的养分吸收投资,但高粘粒含量的土壤实际上可能通过避免生态系统中磷的损失,有助于维持热带森林的高生长。我们的研究表明,保留碳和养分的土壤特性的变化可以帮助解释热带森林生长和死亡率的变化,但不能解释生物量的变化,因为这需要生态位特化,并有助于该地区的生物地球化学多样化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/36f3/7010742/78fca2b07d46/41598_2020_58913_Fig1_HTML.jpg

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