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Soil organic carbon pools in the northern circumpolar permafrost region

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TLDR
In this article, the authors reported a new estimate of the carbon pools in soils of the northern permafrost region, including deeper layers and pools not accounted for in previous analyses.
Abstract
of all soils in the northern permafrost region is approximately 18,782 � 10 3 km 2 ,o r approximately 16% of the global soil area. In the northern permafrost region, organic soils (peatlands) and cryoturbated permafrost-affected mineral soils have the highest mean soil organic carbon contents (32.2–69.6 kg m �2 ). Here we report a new estimate of the carbon pools in soils of the northern permafrost region, including deeper layers and pools not accounted for in previous analyses. Carbon pools were estimated to be 191.29 Pg for the 0–30 cm depth, 495.80 Pg for the 0–100 cm depth, and 1024.00 Pg for the 0–300 cm depth. Our estimate for the first meter of soil alone is about double that reported for this region in previous analyses. Carbon pools in layers deeper than 300 cm were estimated to be 407 Pg in yedoma deposits and 241 Pg in deltaic deposits. In total, the northern permafrost region contains approximately 1672 Pg of organic carbon, of which approximately 1466 Pg, or 88%, occurs in perennially frozen soils and deposits. This 1672 Pg of organic carbon would account for approximately 50% of the estimated global belowground organic carbon pool.

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Spatial distribution of soil organic carbon in northwest Greenland and underestimates of high Arctic carbon stores

TL;DR: In this paper, a detailed study of soil organic carbon (SOC) content by depth in 55 soil pits in a high Arctic ecosystem of northwest Greenland was performed, and the amount of SOC in the various ecosystems was mapped using a correlation of SOC with high-resolution ASTER satellite imagery and the normalized difference vegetation index (NDVI) classes from the Circumpolar Arctic Vegetation Map.
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Effect of climate change on delivery and degradation of lipid biomarkers in a Holocene peat sequence in the Eastern European Russian Arctic

TL;DR: In this article, a peat plateau profile from the Northeast European Russian Arctic was analyzed and the peat originated as a wet fen ca. 9.9 ka BP and developed into peat bog after the onset of...
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High arctic heath soil respiration and biogeochemical dynamics during summer and autumn freeze-in – effects of long-term enhanced water and nutrient supply

TL;DR: Autumn soil microbial activity seems tightly linked to growing season plant production through plant-associated carbon pools, and no change in soil organic matter content after 14 years of environmental manipulations is observed, suggesting high ecosystem resistance to environmental changes.
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Effects of warming and clipping on ecosystem carbon fluxes across two hydrologically contrasting years in an alpine meadow of the Qinghai-Tibet Plateau

TL;DR: The results suggest the response of C fluxes to warming and clipping depends on hydrological variations, and highlight the importance of changes in soil moisture in mediating the responses of ecosystem C fluxe to climate warming in an alpine meadow ecosystem.
References
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Journal ArticleDOI

Temperature sensitivity of soil carbon decomposition and feedbacks to climate change

TL;DR: This work has suggested that several environmental constraints obscure the intrinsic temperature sensitivity of substrate decomposition, causing lower observed ‘apparent’ temperature sensitivity, and these constraints may, themselves, be sensitive to climate.
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The vertical distribution of soil organic carbon and its relation to climate and vegetation

TL;DR: In this paper, the authors examined the association of soil organic carbon (SOC) content with climate and soil texture at different soil depths, and tested the hypothesis that vegetation type, through patterns of allocation, is a dominant control on the vertical distribution of SOC.
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Northern Peatlands: Role in the Carbon Cycle and Probable Responses to Climatic Warming.

TL;DR: Satellite-monitoring of the abundance of open water in the peatlands of the West Siberian Plain and the Hudson/James Bay Lowland is suggested as a likely method of detecting early effects of climatic warming upon boreal and subarctic peatland environments.
Journal ArticleDOI

Total carbon and nitrogen in the soils of the world

TL;DR: In this article, a discrepancy of approximately 350 × 1015 g (or Pg) of C in two recent estimates of soil carbon reserves worldwide is evaluated using the geo-referenced database developed for the World Inventory of Soil Emission Potentials (WISE) project.
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