Soil networks become more connected and take up more carbon as nature restoration progresses

Elly Morriën(Institute for Biodiversity), S. Emilia Hannula(Netherlands Institute of Ecology), Basten L. Snoek(Netherlands Institute of Ecology), Nico R. Helmsing(Netherlands Institute of Ecology), Hans Zweers(Netherlands Institute of Ecology), Mattias de Hollander(Netherlands Institute of Ecology), Raquel Luján Soto(Netherlands Institute of Ecology), Marie‐Lara Bouffaud(Agroécologie), Marc Buée(Interactions Arbres-Microorganismes), W.J. Dimmers(Wageningen University & Research), Henk Duyts(Netherlands Institute of Ecology), Stefan Geisen(University of Cologne), Mariangela Girlanda(Institute for Sustainable Plant Protection), Robert I. Griffiths(UK Centre for Ecology & Hydrology), Helene-Bracht Jørgensen(Lund University), John Jensen(Aarhus University), Pierre Plassart(Agroécologie), Dirk Redecker(Agroécologie), Rüdiger M. Schmelz(Universidade da Coruña), Olaf Schmidt(University College Dublin), Bruce C. Thomson(UK Centre for Ecology & Hydrology), Émilie Tisserant(Interactions Arbres-Microorganismes), Stéphane Uroz(Interactions Arbres-Microorganismes), Anne Winding(Aarhus University), Mark Bailey(UK Centre for Ecology & Hydrology), Michael Bonkowski(University of Cologne), J.H. Faber(Wageningen University & Research), Francis Martin(Interactions Arbres-Microorganismes), Philippe Lemanceau(Agroécologie), Wietse de Boer(Netherlands Institute of Ecology), Johannes A. van Veen(Leiden University), Wim H. van der Putten(Netherlands Institute of Ecology)
Nature Communications
February 8, 2017
Cited by 922Open Access
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Abstract

Soil organisms have an important role in aboveground community dynamics and ecosystem functioning in terrestrial ecosystems. However, most studies have considered soil biota as a black box or focussed on specific groups, whereas little is known about entire soil networks. Here we show that during the course of nature restoration on abandoned arable land a compositional shift in soil biota, preceded by tightening of the belowground networks, corresponds with enhanced efficiency of carbon uptake. In mid- and long-term abandoned field soil, carbon uptake by fungi increases without an increase in fungal biomass or shift in bacterial-to-fungal ratio. The implication of our findings is that during nature restoration the efficiency of nutrient cycling and carbon uptake can increase by a shift in fungal composition and/or fungal activity. Therefore, we propose that relationships between soil food web structure and carbon cycling in soils need to be reconsidered.


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