Ecosphere Resilience Research Center, Faculty of Applied Sciences, University of Sri Jayewardenepura, Nugegoda 10250, Sri Lanka; School of Civil Engineering and Surveying, Faculty of Health, Engineering and Sciences, University of Southern Queensland, West Street, Toowoomba, Queensland 4350, Australia.
School of Civil Engineering and Surveying, Faculty of Health, Engineering and Sciences, University of Southern Queensland, West Street, Toowoomba, Queensland 4350, Australia.
Environ Int. 2019 Oct;131:104974. doi: 10.1016/j.envint.2019.104974. Epub 2019 Jul 31.
The transformation of trace metals (TMs) in natural environmental systems has created significant concerns in recent decades. Ultramafic environments lead to potential risks to the agricultural products and, subsequently, to human health. This unique review presents geochemistry of ultramafic soils, TM fractionation (i.e. sequential and single extraction techniques), TM uptake and accumulation mechanisms of ultramafic flora, and ultramafic-associated health risks to human and agricultural crops. Ultramafic soils contain high levels of TMs (i.e. Cr, Ni, Mn, and Co) and have a low Ca:Mg ratio together with deficiencies in essential macronutrients required for the growth of crops. Even though a higher portion of TMs bind with the residual fraction of ultramafic soils, environmental changes (i.e. natural or anthropogenic) may increase the levels of TMs in the bioavailable or extractable fractions of ultramafic soils. Extremophile plants that have evolved to thrive in ultramafic soils present clear examples of evolutionary adaptations to TM resistance. The release of TMs into water sources and accumulation in food crops in and around ultramafic localities increases health risks for humans. Therefore, more focused investigations need to be implemented to understand the mechanisms related to the mobility and bioavailability of TMs in different ultramafic environments. Research gaps and directions for future studies are also discussed in this review. Lastly, we consider the importance of characterizing terrestrial ultramafic soil and its effect on crop plants in the context of multi-decadal plans by NASA and other space agencies to establish human colonies on Mars.
在过去几十年中,痕量金属(TMs)在自然环境系统中的转化引起了人们的极大关注。超镁铁质环境对农产品造成了潜在风险,进而对人类健康造成影响。本文独特地综述了超镁铁质土壤的地球化学、TM 分馏(即顺序和单一提取技术)、超镁铁质植物的 TM 吸收和积累机制,以及与超镁铁质相关的人类和农业作物的健康风险。超镁铁质土壤中含有高水平的 TMs(如 Cr、Ni、Mn 和 Co),且 Ca:Mg 比值低,缺乏作物生长所需的必需大量营养素。尽管较高比例的 TMs 与超镁铁质土壤的残余部分结合,但环境变化(如自然或人为)可能会增加超镁铁质土壤中生物可利用或可提取部分的 TMs 水平。在超镁铁质土壤中进化而来的极端微生物是对 TM 抗性进化适应的明显例证。TMs 释放到水源中,并在超镁铁质地区及其周围的粮食作物中积累,增加了人类的健康风险。因此,需要进行更有针对性的研究,以了解不同超镁铁质环境中 TMs 的迁移和生物可利用性相关机制。本文还讨论了未来研究的差距和方向。最后,我们考虑了在 NASA 和其他太空机构制定在火星上建立人类殖民地的数十年计划的背景下,对陆地超镁铁质土壤及其对作物的影响进行特征描述的重要性。