Abstract

Tree planting is increasingly being proposed as a strategy to combat climate change through carbon (C) sequestration in tree biomass. However, total ecosystem C storage that includes soil organic C (SOC) must be considered to determine whether planting trees for climate change mitigation results in increased C storage. We show that planting two native tree species (Betula pubescens and Pinus sylvestris), of widespread Eurasian distribution, onto heather (Calluna vulgaris) moorland with podzolic and peaty podzolic soils in Scotland, did not lead to an increase in net ecosystem C stock 12 or 39years after planting. Plots with trees had greater soil respiration and lower SOC in organic soil horizons than heather control plots. The decline in SOC cancelled out the increment in C stocks in tree biomass on decadal timescales. At all four experimental sites sampled, there was no net gain in ecosystem C stocks 12-39years after afforestation-indeed we found a net ecosystem C loss in one of four sites with deciduous B. pubescens stands; no net gain in ecosystem C at three sites planted with B. pubescens; and no net gain at additional stands of P. sylvestris. We hypothesize that altered mycorrhizal communities and autotrophic C inputs have led to positive 'priming' of soil organic matter, resulting in SOC loss, constraining the benefits of tree planting for ecosystem C sequestration. The results are of direct relevance to current policies, which promote tree planting on the assumption that this will increase net ecosystem C storage and contribute to climate change mitigation. Ecosystem-level biogeochemistry and C fluxes must be better quantified and understood before we can be assured that large-scale tree planting in regions with considerable pre-existing SOC stocks will have the intended policy and climate change mitigation outcomes.

Highlights

  • Anthropogenic climate change has been described as the greatest current threat to ecosystems and all that depends on them (Nolan et al, 2018)

  • World-wide strategies to mitigate climate change have been proposed (Paris Agreement, 2015). Notable among these is the growing international momentum behind tree planting, and the extensive afforestation of areas with future climates potentially suitable for forest cover (Bastin et al, 2019; Lewis, Wheeler, Mitchard, & Koch, 2019; New York Declaration of Forests, 2014; UNEP, 2011). These proposed mitigation steps rely on sequestration of carbon dioxide (CO2) by the production of tree biomass, but rarely consider the fate and storage of C in soils

  • Soil C storage is critically important, as more C is stored in soil globally than in vegetation and the atmosphere combined (Tarnocai et al, 2009)

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Summary

| INTRODUCTION

Anthropogenic climate change has been described as the greatest current threat to ecosystems and all that depends on them (Nolan et al, 2018). World-wide strategies to mitigate climate change have been proposed (Paris Agreement, 2015) Notable among these is the growing international momentum behind tree planting, and the extensive afforestation of areas with future climates potentially suitable for forest cover (Bastin et al, 2019; Lewis, Wheeler, Mitchard, & Koch, 2019; New York Declaration of Forests, 2014; UNEP, 2011). Planting trees in previously un-forested areas (or areas which have been deforested for centuries) creates profound changes to plant communities This affects below-ground microbial communities, resulting in a reshaping of the ecosystem with consequences for stored soil C (Kyaschenko, Clemmensen, Hagenbo, Karltun, & Lindahl, 2017; Wardle et al, 2004; Wurzburger, Brookshire, McCormack, & Lankau, 2017).

| MATERIALS AND METHODS
Findings
| DISCUSSION
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