4.7 Article

Forest litter constraints on the pathways controlling soil organic matter formation

Journal

SOIL BIOLOGY & BIOCHEMISTRY
Volume 163, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2021.108447

Keywords

C-13-CP/MAS-NMR spectroscopy; Ex vivo pathways; Particulate organic matter; In vivo pathways; Mineral-associated organic matter

Categories

Funding

  1. Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)
  2. Fundacao de Amparo a` Pesquisa de Minas Gerais (FAPEMIG)
  3. Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [88881.189468/2018-01, 88887.356500/2019-00]

Ask authors/readers for more resources

The study found that aboveground litter in tropical forest ecosystems is more efficient in promoting soil organic matter formation and causes less degradation of soil organic matter compared to root litter.
The connection between litter chemistry and the pathways controlling soil organic matter (SOM) formation and decay in forest ecosystems remains poorly understood, particularly in tropical soils. We addressed this question by incubating samples of a Ferralsol for 200 days with typical forest litter (leaves, twigs, bark, and roots) obtained from C-13-enriched Eucalyptus seedlings. Throughout the incubation, we monitored C-13/C-12-CO2 evolved from the soil to quantify the microbial respiration of the C-13-labeled fresh plant litter and of the native SOM. Afterwards, we used density fractionation to obtain particulate organic matter (POM) with density <1.8 g cm(-3), and the soil material remaining was wet-sieved to obtain SOM with particle-size >53 mu m and mineral-associated SOM (MAOM, with particle-size <53 mu m). We used solid-state C-13-CPMAS-NMR spectroscopy to assess the molecular composition of plant material and SOM fractions and quantified microbial amino sugars in bulk soil using gas chromatography. Our C-13/C-12-CO2 results indicate that leaves, twigs, and bark (aboveground litter) were respired at higher rates but led to lower degradation of native SOM as compared to root tissues. On average, aboveground litter promoted net C gains in both POM and MAOM, whereas root litter only led to net C gains in POM. Overall, SOM formation via microbial incorporation of aboveground litter through in vivo pathways appears to be more efficient and causes less degradation of native MAOM than roots. Moreover, a reduction in microbial amino sugars in bulk soils suggests that in vivo pathways also favored the formation of POM, which had more microbial-derived protein than forest litter. Therefore, the connection between litter chemistry and the pathways controlling SOM formation in tropical forest ecosystems must be included in a framework that also considers the mineralization of native SOM and the vertical separation of aboveground and belowground C inputs to soils.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available