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Plant and Soil

, Volume 424, Issue 1–2, pp 319–334 | Cite as

Linkages between root traits, soil fungi and aggregate stability in tropical plant communities along a successional vegetation gradient

  • Julien Demenois
  • Freddy Rey
  • Thomas Ibanez
  • Alexia Stokes
  • Fabian Carriconde
Regular Article

Abstract

Aims

Determining which abiotic and biotic factors influence soil aggregate stability (MWD) in tropical climates is often confounded by soil type. We aimed to better understand the influence of soil physical and chemical components, vegetation and fungal abundance on MWD of a Ferralsol along a successional gradient of vegetation in New Caledonia.

Methods

Five plant communities (sedge dominated, open sclerophyllous shrubland, Arillastrum forest, Nothofagus forest and mixed rainforest) were studied. For each community, MWD, soil texture, soil organic carbon (SOC), iron (Fe) and aluminium (Al) sesquioxides, root length density (RLD), specific root length (SRL), root mass density (RMD) and fungal abundance were measured. Generalized linear models were used to predict MWD from soil and plant trait data.

Results

The best prediction of MWD combined abiotic and biotic factors. Along the gradient, Fe increased MWD, while root traits, fungal abundance and SOC modified MWD. From the sedge-dominated community to Arillastrum forest, RMD and SOC increased MWD, while between Nothofagus and mixed rainforest, it was likely that floristic composition and fungal communities influenced MWD.

Conclusions

Plant community, the intrinsic nature of Ferralsol and fungal abundance all modified MWD. However, the specific effect of microbial communities should be addressed through a metagenomics approach to elucidate microbial interactions with plant communities.

Keywords

Ferralsol Erosion Abiotic factors Biotic factors Soil aggregation Ultramafic substrates New Caledonia 

Abbreviations

AM

Arbuscular mycorrhiza

ECM

Ectomycorrhizal fungi

MWD

Mean weight diameter

PCA

Principal Component Analysis

qPCR

Quantitative PCR

rDNA

Ribosomal DNA

RLD

Root length density

RMD

Root mass density

SRL

Specific root length

SLA

Specific leaf area

SOC

Soil organic carbon

Notes

Acknowledgements

We gratefully acknowledge the field staff of IAC (‘Unité SARA’): A. Bouarat, R. Guiglion, J.P. Lataï and A. Pain for their substantial assistance. We are thankful to our colleagues at IAC who gave substantial help for qPCR analyses: M. Lelièvre, K. Letellier, N. Robert, J. Soewarto and S. Gigante. We thank the US191 LAMA at IRD Nouméa who carried out the sesquioxides measurements. Fieldwork and laboratory analyses were funded by INRA, IAC and through a collaboration agreement between IAC and Société Le Nickel (agreement IAC-SLN n°DE2013-041). We thank the French Ministry of Agriculture for funding a PhD bursary (J. Demenois). Finally, we thank the anonymous reviewers for their helpful comments on the manuscript. In memoriam: we dedicate this paper to Christian Papineau who spent a large part of his life studying Arillastrum forests.

Supplementary material

11104_2017_3529_Fig5_ESM.gif (89 kb)
Supplementary Fig. 1

Types of plant communities along the successional vegetation gradient from shrubland to forest. Retrocessions due to disturbances are not shown. (GIF 89 kb)

11104_2017_3529_MOESM1_ESM.tif (9.3 mb)
High resolution image (TIFF 9522 kb)
11104_2017_3529_Fig6_ESM.gif (17 kb)
Supplementary Fig. 2

Non-metric dimensional scaling (NMDS) performed on Bray-Curtis dissimilarity indices for the five plant communities. S is Sedge-dominated formation; Mq is shrubland with Tristaniopsis glauca; Ag is Arillastrum forest; Na is Nothofagus forest and M is mixed rainforest. (GIF 17 kb)

11104_2017_3529_MOESM2_ESM.tif (6 mb)
High resolution image (TIFF 6181 kb)
11104_2017_3529_Fig7_ESM.gif (63 kb)
Supplementary Fig. 3

Spearman correlations between soil characteristics, root traits and fungal biomass. *** indicates correlations with P < 0.001 for ρ > 0.7. The size of the circle is proportional to ρ. Abbreviations are: Fe2O3: Fe sesquioxides; Al2O3: Al sesquioxides; SOC: soil organic carbon; RLD: root length density; RMD: root mass density; SRL: specific root length; FR: % of fine roots, VFR: % of very fine roots. (GIF 63 kb)

11104_2017_3529_MOESM3_ESM.tif (11.1 mb)
High resolution image (TIFF 11360 kb)

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Copyright information

© Springer International Publishing AG, part of Springer Nature 2018

Authors and Affiliations

  • Julien Demenois
    • 1
    • 2
  • Freddy Rey
    • 3
  • Thomas Ibanez
    • 2
  • Alexia Stokes
    • 4
  • Fabian Carriconde
    • 2
  1. 1.Institut Agronomique néo-Calédonien (IAC), « Equipe Sol & Végétation » (SolVeg)ParisFrance
  2. 2.Institut Agronomique néo-Calédonien (IAC), « Equipe Sol & Végétation » (SolVeg)NouméaNew Caledonia
  3. 3.University of Grenoble Alpes, Irstea, UR EMGRSaint Martin-d’Hères cedexFrance
  4. 4.Inra, Amap, Ird, Cnrs, CiradUniversity of MontpellierMontpellierFrance

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