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南美洲南部生长在源自年轻火山物质的基质上的山龙眼科物种的生态生理表现。

Ecophysiological Performance of Proteaceae Species From Southern South America Growing on Substrates Derived From Young Volcanic Materials.

作者信息

Delgado M, Zúñiga-Feest A, Reyes-Díaz M, Barra P J, Ruiz S, Bertin-Benavides A, Valle S, Pereira M, Lambers H

机构信息

Center of Plant, Soil Interaction and Natural Resources Biotechnology, Scientific and Technological Bioresource Nucleus (BIOREN), Universidad de La Frontera, Temuco, Chile.

Laboratorio de Biología Vegetal, Instituto de Ciencias Ambientales y Evolutivas, Facultad de Ciencias, Universidad Austral de Chile, Valdivia, Chile.

出版信息

Front Plant Sci. 2021 Feb 19;12:636056. doi: 10.3389/fpls.2021.636056. eCollection 2021.

DOI:10.3389/fpls.2021.636056
PMID:33679850
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7933449/
Abstract

Southern South American Proteaceae thrive on young volcanic substrates, which are extremely low in plant-available phosphorus (P). Most Proteaceae exhibit a nutrient-acquisition strategy based on the release of carboxylates from specialized roots, named cluster roots (CR). Some Proteaceae colonize young volcanic substrates which has been related to CR functioning. However, physiological functioning of other Proteaceae on recent volcanic substrates is unknown. We conducted an experiment with seedlings of five Proteaceae (, , , , and ) grown in three volcanic materials. Two of them are substrates with very low nutrient concentrations, collected from the most recent deposits of the volcanoes Choshuenco and Calbuco (Chile). The other volcanic material corresponds to a developed soil that exhibits a high nutrient availability. We assessed morphological responses (i.e., height, biomass, and CR formation), seed and leaf macronutrient and micronutrient concentrations and carboxylates exuded by roots. The results show that was less affected by nutrient availability of the volcanic substrate, probably because it had a greater nutrient content in its seeds and produced large CR exuding carboxylates that supported their initial growth. exhibited greater total plant height and leaf P concentration than species. In general, in all species leaf macronutrient concentrations were reduced on nutrient-poor volcanic substrates, while leaf micronutrient concentrations were highly variable depending on species and volcanic material. We conclude that Proteaceae from temperate rainforests differ in their capacity to grow and acquire nutrients from young and nutrient-poor volcanic substrates. The greater seed nutrient content, low nutrient requirements (only for ) and ability to mobilize nutrients help explain why and are better colonizers of recent volcanic substrates than species.

摘要

南美洲南部的山龙眼科植物在年轻的火山基质上生长旺盛,这些基质中植物可利用的磷(P)含量极低。大多数山龙眼科植物表现出一种基于从特殊根(称为簇生根,CR)释放羧酸盐的养分获取策略。一些山龙眼科植物在年轻的火山基质上定殖,这与簇生根的功能有关。然而,其他山龙眼科植物在近期火山基质上的生理功能尚不清楚。我们用五种山龙眼科植物(、、、和)的幼苗在三种火山材料中进行了一项实验。其中两种是养分浓度极低的基质,取自智利乔舒恩科火山和卡尔布科火山最近的沉积物。另一种火山材料是一种养分有效性高的发育土壤。我们评估了形态学反应(即高度、生物量和簇生根形成)、种子和叶片的大量营养素和微量营养素浓度以及根系分泌的羧酸盐。结果表明,受火山基质养分有效性的影响较小,可能是因为其种子中的养分含量较高,并产生了大量分泌羧酸盐的簇生根,支持其初期生长。与其他物种相比,其总株高和叶片磷浓度更高。一般来说,在所有物种中,在养分贫瘠的火山基质上,叶片大量营养素浓度降低,而叶片微量营养素浓度则因物种和火山材料而异。我们得出结论,来自温带雨林的山龙眼科植物从年轻且养分贫瘠的火山基质中生长和获取养分的能力不同。种子中更高的养分含量、较低的养分需求(仅针对)以及调动养分的能力有助于解释为什么和比其他物种更能在近期火山基质上定殖。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/fb364903ae87/fpls-12-636056-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/17be632f0bdc/fpls-12-636056-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/ab5ebd1236f6/fpls-12-636056-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/07678600c4ae/fpls-12-636056-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/4f6fd721905a/fpls-12-636056-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/7eac1d826a6f/fpls-12-636056-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/fb364903ae87/fpls-12-636056-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/17be632f0bdc/fpls-12-636056-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/ab5ebd1236f6/fpls-12-636056-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/07678600c4ae/fpls-12-636056-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/4f6fd721905a/fpls-12-636056-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/7eac1d826a6f/fpls-12-636056-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/87be/7933449/fb364903ae87/fpls-12-636056-g006.jpg

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