Soil in the Anthropocene
Soil in the Anthropocene
复制标题
人类世的土壤
DOI：
10.1088/1755-1315/25/1/012010
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发表时间：
2015
期刊：
影响因子：
--
通讯作者：
M. L. Mobley
中科院分区：
文献类型：
--
作者：
D. Richter;A. Bacon;Zachary S Brecheisen;M. L. Mobley
随着学者们为我们的地质时代，即人类世，考虑一个新的名称，无论是生物学家、化学家还是物理学家，土壤科学家都在记录地球上大多数土壤正在发生的重大变化。这种全球土壤变化与大气、生物圈、水圈和岩石圈(即地球的临界区)相互作用，这些发展也对地球的地层记录产生了重大影响。实际上，土壤科学家在人类学中研究这种全球土壤变化，这直接导致了将土壤地层转变为土壤地层学的需要，这是一门探索全球土壤变化如何改变地球岩石、生物和化学地层的科学。这些发展强化了地球确实正在进入人类世的观点。
With scholars deliberating a new name for our geologic epoch, i.e., the Anthropocene, soil scientists whether biologists, chemists, or physicists are documenting significant changes accruing in a majority of Earth's soils. Such global soil changes interact with the atmosphere, biosphere, hydrosphere, and lithosphere (i.e., Earth's Critical Zone), and these developments are significantly impacting the Earth's stratigraphic record as well. In effect, soil scientists study such global soil changes in a science of anthropedology, which leads directly to the need to transform pedostratigraphyinto an anthro-pedostratigraphy, a science that explores how global soil change alters Earth's litho-, bio-, and chemostratigraphy. These developments reinforce perspectives that the planet is indeed crossing into the Anthropocene.