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Soil is the best testifier of the diachronous dawn of the Anthropocene
Journal of Plant Nutrition and Soil Science ( IF 2.5 ) Pub Date : 2021-01-27 , DOI: 10.1002/jpln.202000481
Giacomo Certini 1 , Riccardo Scalenghe 2
Affiliation  

Humans act at worldwide scale as a growing geomorphic agent since mid‐Holocene (8,200–4,200 y BP) through the pervasive impacts of domestication, deforestation, agriculture, urbanization, and mining. The concept of Anthropocene has been introduced exactly to indicate the timespan in which humans have joined with other natural forces in impacting the outermost shell of the planet and the biosphere. Soils, which are the Earth's skin, are sensitive archives of any major human‐induced local to global change. Especially when buried, soils can permanently preserve the primordial traces of a significant impact of man on the environment, which occurred at different times and rates in different areas. As a result, we assert that the oldest “anthropogenic” soils from all around the world collectively are an appropriate marker for the diachronous dawn of an early Anthropocene.

中文翻译:

土壤是人类世历时曙光的最好证明

自全新世以来(8,200–4,200 y BP)以来,人类通过驯化,森林砍伐,农业,城市化和采矿的普遍影响,在全球范围内充当着不断增长的地貌代理。引入人类世的概念正是为了指出人类与其他自然力量共同影响地球和生物圈最外层外壳的时间跨度。土壤是地球的皮肤,是任何由人类引起的局部到全球变化的敏感档案。尤其是在埋葬后,土壤可以永久保存人类对环境的重大影响的原始痕迹,这种痕迹发生在不同时间,不同地区的发生率不同。因此,
更新日期:2021-04-06
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