@article{HerreroThorntonMasonD'Crozetal.2020,
  author    = {Herrero, Mario and Thornton, Philip K. and Mason-D'Croz, Daniel and Palmer, Jeda and Bodirsky, Benjamin Leon and Pradhan, Prajal and Barrett, Christopher B. and Benton, Tim G. and Hall, Andrew and Pikaar, Ilje and Bogard, Jessica R. and Bonnett, Graham D. and Bryan, Brett A. and Campbell, Bruce M. and Christensen, Svend and Clark, Michael and Fanzo, Jessica and Godde, Cecile M. and Jarvis, Andy and Loboguerrero, Ana Maria and Mathys, Alexander and McIntyre, C. Lynne and Naylor, Rosamond L. and Nelson, Rebecca and Obersteiner, Michael and Parodi, Alejandro and Popp, Alexander and Ricketts, Katie and Smith, Pete and Valin, Hugo and Vermeulen, Sonja J. and Vervoort, Joost and van Wijk, Mark and van Zanten, Hannah H. E. and West, Paul C. and Wood, Stephen A. and Rockstr{\"o}m, Johan},
  title     = {Articulating the effect of food systems innovation on the Sustainable Development Goals},
  series = {The lancet Planetary health},
  volume    = {5},
  journal   = {The lancet Planetary health},
  number    = {1},
  publisher = {Elsevier},
  address   = {Oxford},
  issn      = {2542-5196},
  doi       = {10.1016/S2542-5196(20)30277-1},
  pages     = {E50 -- E62},
  year      = {2020},
  abstract  = {Food system innovations will be instrumental to achieving multiple Sustainable Development Goals (SDGs). However, major innovation breakthroughs can trigger profound and disruptive changes, leading to simultaneous and interlinked reconfigurations of multiple parts of the global food system. The emergence of new technologies or social solutions, therefore, have very different impact profiles, with favourable consequences for some SDGs and unintended adverse side-effects for others. Stand-alone innovations seldom achieve positive outcomes over multiple sustainability dimensions. Instead, they should be embedded as part of systemic changes that facilitate the implementation of the SDGs. Emerging trade-offs need to be intentionally addressed to achieve true sustainability, particularly those involving social aspects like inequality in its many forms, social justice, and strong institutions, which remain challenging. Trade-offs with undesirable consequences are manageable through the development of well planned transition pathways, careful monitoring of key indicators, and through the implementation of transparent science targets at the local level.},
  language  = {en}
}
@article{TokeArrowsmithRymeretal.2011,
  author    = {Toke, Nathan A. and Arrowsmith, J. Ramon and Rymer, Michael J. and Landgraf, Angela and Haddad, David E. and Busch, Melanie and Coyan, Joshua and Hannah, Alexander},
  title     = {Late Holocene slip rate of the San Andreas fault and its accommodation by creep and moderate-magnitude earthquakes at Parkfield, California},
  series = {Geology},
  volume    = {39},
  journal   = {Geology},
  number    = {3},
  publisher = {American Institute of Physics},
  address   = {Boulder},
  issn      = {0091-7613},
  doi       = {10.1130/G31498.1},
  pages     = {243 -- 246},
  year      = {2011},
  abstract  = {Investigation of a right-laterally offset channel at the Miller's Field paleoseismic site yields a late Holocene slip rate of 26.2 +6.4/-4.3 mm/yr (1 sigma) for the main trace of the San Andreas fault at Parkfield, California. This is the first well-documented geologic slip rate between the Carrizo and creeping sections of the San Andreas fault. This rate is lower than Holocene measurements along the Carrizo Plain and rates implied by far-field geodetic measurements (similar to 35 mm/yr). However, the rate is consistent with historical slip rates, measured to the northwest, along the creeping section of the San Andreas fault (<30 mm/yr). The paleoseismic exposures at the Miller's Field site reveal a pervasive fabric of clay shear bands, oriented clockwise oblique to the San Andreas fault strike and extending into the uppermost stratigraphy. This fabric is consistent with dextral aseismic creep and observations of surface slip from the 28 September 2004 M6 Parkfield earthquake. Together, this slip rate and deformation fabric suggest that the historically observed San Andreas fault slip behavior along the Parkfield section has persisted for at least a millennium, and that significant slip is accommodated by structures in a zone beyond the main San Andreas fault trace.},
  language  = {en}
}