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Sophie Opfergelt
Soils are known to be an enormous reservoir of carbon and represent an important and dynamic part of the global carbon cycle. However, this reservoir is under constant threat due to a combination of issues, including mismanagement, climate change and intensive agricultural production which has led to depletion of soil organic carbon. Understanding and fostering soil carbon sequestration reviews the wealth of research on important aspects of soil carbon sequestration, including its potential in mitigating and adapting to climate change and improving global food security. The collection explores our understanding of carbon sequestration in soils, detailing the mechanisms and abiotic factors that can affect the process, as well as the socioeconomic, legal and policy issues that can arise as a result of this use. In its extensive exploration of soil carbon cycling and capture, the book highlights how an informed understanding of carbon sequestration in a variety of soil types can contribute to achieving a more su
Climate change affects the Arctic and sub-Arctic regions by exposing previously frozen permafrost to thaw, unlocking soil nutrients, changing hydrological processes, and boosting plant growth. As a result, sub-Arctic tundra is subject to a shrub expansion, called “shrubification”, at the expense of sedge species. Depending on the intrinsic foliar properties of these plant species, changes in foliar mineral element fluxes with shrubification in the context of permafrost degradation may influence topsoil mineral element composition. Despite the potential implications of changes in topsoil mineral element concentrations for the fate of organic carbon, this remains poorly quantified. Here, we investigate vegetation foliar and topsoil mineral element composition (Si, K, Ca, P, Mn, Zn, Cu, Mo, V) across a natural gradient of permafrost degradation at a typical sub-Arctic tundra at Eight Mile Lake (Alaska, USA). Results show that foliar mineral element concentrations are higher (up to 9 times; Si, K, Mo for all spec
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