The potential for land sparing to offset greenhouse gas emissions from agriculture

Anthony Lamb, Rhys Green, Ian Bateman, Mark Broadmeadow, Toby Bruce, Jennifer Burney, Pete Carey, David Chadwick, Ellie Crane, Rob Field, Keith Goulding, Howard Griffiths, Astley Hastings, Tim Kasoar, Daniel Kindred, Ben Phalan, John Pickett, Pete Smith, Eileen Wall, Erasmus K. H. J. zu Ermgassen Andrew Balmford

Research output: Contribution to journalLetterpeer-review

178 Citations (Scopus)
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Greenhouse gas emissions from global agriculture are increasing at around 1% per annum, yet substantial cuts in emissions are needed across all sectors1. The challenge of reducing agricultural emissions is particularly acute, because the reductions achievable by changing farming practices are limited2, 3 and are hampered by rapidly rising food demand4, 5. Here we assess the technical mitigation potential offered by land sparing—increasing agricultural yields, reducing farmland area and actively restoring natural habitats on the land spared6. Restored habitats can sequester carbon and can offset emissions from agriculture. Using the UK as an example, we estimate net emissions in 2050 under a range of future agricultural scenarios. We find that a land-sparing strategy has the technical potential to achieve significant reductions in net emissions from agriculture and land-use change. Coupling land sparing with demand-side strategies to reduce meat consumption and food waste can further increase the technical mitigation potential—however, economic and implementation considerations might limit the degree to which this technical potential could be realized in practice.
Original languageEnglish
Pages (from-to)488-492
Number of pages5
JournalNature Climate Change
Early online date4 Jan 2016
Publication statusPublished - May 2016

Bibliographical note

This research was funded by the Cambridge Conservation Initiative Collaborative Fund for Conservation, and we thank its major sponsor Arcadia. We thank J. Bruinsma for the provision of demand data, the CEH for the provision of soil data and J. Spencer for invaluable discussions. A.L. was supported by a Gates Cambridge Scholarship. T.B., K.G. and J.P. acknowledge BBSRC funding through grant BBS/E/C/00005198.


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