Afforestation with tropical N-fixing species in the Brazilian Atlantic rainforest: carbon and nitrogen in the soil profile

IF 1.8 4区 环境科学与生态学 Q3 ECOLOGY
David Pessanha Siqueira , Emanuela Forestieri Gama-Rodrigues , Marcos Vinicius Winckler Caldeira , Carlos Eduardo Rezende , Claudio Roberto Marciano , Deborah Guerra Barroso
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引用次数: 0

Abstract

The Atlantic Rainforest biome is one of the most threatened in the world by deforestation where afforestation programs are urgently needed. N-fixing species should be prioritized in re-establishing forest covers as they can enhance soil C and N and stimulate cycling of other nutrients. Yet, tropical ecosystems play a key role in global warming and remain underrepresented in global biogeochemical assessments. To better understand the effects of tropical N-fixing species on soil C and N pools after pasture conversion we selected three 27-year-old monospecific stands comprising Plathymenia reticulata, Hymenaea courbaril, and Centrolobium tomentosum. We evaluated soil organic carbon (SOC), nitrogen (STN), and the natural abundance of 13C and 15N in the soil profile up to 100 cm depth. SOC was higher for P. reticulata, but that was not true when considering soil layers up to 30 cm soil depth. Meanwhile, STN was similar across species and δ15N values showed enrichment at intermediate soil layers indicating 14N gaseous loss. Most of the SOC originated from the planted trees rather than the former pasture, except beneath C. tomentosum where C4 derived C is decreasing at a slower rate. This study presents novel insights in understanding how tropical N-fixing tree species may be impacting soil C and N pools where specific-species leaf traits appear to be mediating SOC retention to the mineral soil.
巴西大西洋雨林中热带固氮物种造林:土壤剖面中的碳和氮
大西洋雨林是世界上受森林砍伐威胁最严重的生物群落之一,迫切需要植树造林计划。在重建森林覆盖时应优先选择固氮物种,因为它们能提高土壤C和N,并促进其他养分的循环。然而,热带生态系统在全球变暖中发挥着关键作用,在全球生物地球化学评估中仍未得到充分体现。为了更好地了解热带固氮物种对草地转换后土壤C和N库的影响,我们选择了3个27年的单种林分,分别是网状白桫椤(Plathymenia reticulata)、库巴勒膜属(Hymenaea courbaril)和毛毡心(Centrolobium tomentosum)。我们评估了土壤有机碳(SOC)、氮(STN)以及13C和15N在100 cm深度土壤剖面中的自然丰度。土壤有机碳含量较高的是绿桫椤,但在30 cm以下的土层中并非如此。同时,不同物种间的STN相似,δ15N值在中间土层呈富集,表明14N气态损失。土壤有机碳主要来源于人工种植的树木,而非原牧场,但在毛毛草下,C4衍生的碳减少的速度较慢。该研究为理解热带固氮树种如何影响土壤C和N库提供了新的见解,其中特定物种的叶片特征似乎可以调节矿物土壤的SOC保留。
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来源期刊
CiteScore
3.60
自引率
0.00%
发文量
57
审稿时长
>0 weeks
期刊介绍: Acta Oecologica is venue for the publication of original research articles in ecology. We encourage studies in all areas of ecology, including ecosystem ecology, community ecology, population ecology, conservation ecology and evolutionary ecology. There is no bias with respect to taxon, biome or geographic area. Both theoretical and empirical papers are welcome, but combinations are particularly sought. Priority is given to papers based on explicitly stated hypotheses. Acta Oecologica also accepts review papers.
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