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Soils in warmer and less developed countries have less micronutrients globally

机译:全球温暖和欠发达国家的土壤微量营养素较少

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摘要

Abstract Soil micronutrients are capital for the delivery of ecosystem functioning and food provision worldwide. Yet, despite their importance, the global biogeography and ecological drivers of soil micronutrients remain virtually unknown, limiting our capacity to anticipate abrupt unexpected changes in soil micronutrients in the face of climate change. Here, we analyzed >1300 topsoil samples to examine the global distribution of six metallic micronutrients (Cu, Fe, Mn, Zn, Co and Ni) across all continents, climates and vegetation types. We found that warmer arid and tropical ecosystems, present in the least developed countries, sustain the lowest contents of multiple soil micronutrients. We further provide evidence that temperature increases may potentially result in abrupt and simultaneous reductions in the content of multiple soil micronutrients when a temperature threshold of 12–14°C is crossed, which may be occurring on 3 of the planet over the next century. Altogether, our findings provide fundamental understanding of the global distribution of soil micronutrients, with direct implications for the maintenance of ecosystem functioning, rangeland management and food production in the warmest and poorest regions of the planet.
机译:摘要 土壤微量营养素是全球生态系统功能和食物供应的资本。然而,尽管土壤微量营养素很重要,但土壤微量营养素的全球生物地理学和生态驱动因素仍然几乎未知,这限制了我们在面对气候变化时预测土壤微量营养素突然发生意外变化的能力。在这里,我们分析了>1300个表土样品,以检查六种金属微量营养素(Cu,Fe,Mn,Zn,Co和Ni)在所有大陆,气候和植被类型的全球分布。我们发现,在最不发达国家存在的温暖干旱和热带生态系统中,多种土壤微量元素的含量最低。我们进一步提供证据表明,当超过12-14°C的温度阈值时,温度升高可能会导致多种土壤微量营养素的含量突然同时降低,这可能在下个世纪发生在地球上的3%上。总而言之,我们的研究结果提供了对土壤微量营养素全球分布的基本理解,对维持地球上最温暖和最贫困地区的生态系统功能、牧场管理和粮食生产有直接影响。

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