scispace - formally typeset
Open AccessJournal ArticleDOI

Soil organic carbon pools in the northern circumpolar permafrost region

Reads0
Chats0
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.

read more

Content maybe subject to copyright    Report

Citations
More filters
Journal ArticleDOI

A simplified, data-constrained approach to estimate the permafrost carbon-climate feedback

TL;DR: An approach to estimate the feedback from large-scale thawing of permafrost soils using a simplified, data-constrained model that combines three elements: soil carbon maps and profiles to identify the distribution and type of C in permaf frost soils; incubation experiments to quantify the rates of C lost after thaw; and models of soil thermal dynamics in response to climate warming.
Journal ArticleDOI

Experimental drought in a tropical rain forest increases soil carbon dioxide losses to the atmosphere

TL;DR: Together, the data suggest that declines in precipitation in tropical rain forests could drive higher CO2 fluxes to the atmosphere both via increased soil 02 availability and through responses to elevated DOM concentrations.
Journal ArticleDOI

Temperature and peat type control CO2 and CH4 production in Alaskan permafrost peats

TL;DR: Temperature, moisture, organic matter, and microbial controls on soil organic carbon (SOC) losses following permafrost thaw in peat soils across Alaska, and carbon dioxide and methane emissions varied depending on the peat type and peat decomposition stage rather than thermal state.

Methane seeps along boundaries of arctic permafrost thaw and melting glaciers

TL;DR: In this paper, the authors document the release of geologic methane to the atmosphere from abundant gas seeps concentrated along boundaries of permafrost thaw and receding glaciers in Alaska.
Journal ArticleDOI

Patterns and persistence of hydrologic carbon and nutrient export from collapsing upland permafrost

TL;DR: In this paper, the authors studied the effect of permafrost collapse on aquatic biogeochemical cycles and found that thermokarst caused substantial increases in dissolved organic carbon and other solute concentrations with a particularly large impact on inorganic nitrogen.
References
More filters
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.
Journal ArticleDOI

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.
Journal ArticleDOI

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.
Related Papers (5)