Background and scope
Land based agricultural production is the source of approximately 95% of human food nutrients (UN FAO). Intensive and often inappropriate practices in agriculture have however resulted in severe soil degradation, thereby reducing the capacity of soils to support food production and other important ecosystem services such as the regulation of water, nutrients, and carbon cycles. Soil degradation is further accelerated by the effects of climate change, with abiotic stresses such as heat, drought, salinity, and waterlogging, often in combination, having negative effects on the world's crop production. The direct impact of a changed climate is also frequently accompanied by indirect impacts due to alterations in the composition and behaviour of weeds, insects, pathogens, and soil microbiome, alongside the impacts of increased amounts of human-generated pollutants.
Plants react to such stresses with what are often conflicting physiological and metabolic responses. These may prioritise one acclimatisation/adaptation strategy over the other, a blend of one or more responses, and/or through developing a completely new strategy, all of which can, in turn, impact final production including nutrient content.
When combined with an increasing human population, likely to increase net demand for food, there is a clear rationale to reinforce existing food and nutrient production
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