Abstract

Abstract. High-latitude terrestrial ecosystems are key components in the global carbon cycle. The Northern Circumpolar Soil Carbon Database (NCSCD) was developed to quantify stocks of soil organic carbon (SOC) in the northern circumpolar permafrost region (a total area of 18.7 × 106 km2). The NCSCD is a geographical information system (GIS) data set that has been constructed using harmonized regional soil classification maps together with pedon data from the northern permafrost region. Previously, the NCSCD has been used to calculate SOC storage to the reference depths 0–30 cm and 0–100 cm (based on 1778 pedons). It has been shown that soils of the northern circumpolar permafrost region also contain significant quantities of SOC in the 100–300 cm depth range, but there has been no circumpolar compilation of pedon data to quantify this deeper SOC pool and there are no spatially distributed estimates of SOC storage below 100 cm depth in this region. Here we describe the synthesis of an updated pedon data set for SOC storage (kg C m−2) in deep soils of the northern circumpolar permafrost regions, with separate data sets for the 100–200 cm (524 pedons) and 200–300 cm (356 pedons) depth ranges. These pedons have been grouped into the North American and Eurasian sectors and the mean SOC storage for different soil taxa (subdivided into Gelisols including the sub-orders Histels, Turbels, Orthels, permafrost-free Histosols, and permafrost-free mineral soil orders) has been added to the updated NCSCDv2. The updated version of the data set is freely available online in different file formats and spatial resolutions that enable spatially explicit applications in GIS mapping and terrestrial ecosystem models. While this newly compiled data set adds to our knowledge of SOC in the 100–300 cm depth range, it also reveals that large uncertainties remain. Identified data gaps include spatial coverage of deep (> 100 cm) pedons in many regions as well as the spatial extent of areas with thin soils overlying bedrock and the quantity and distribution of massive ground ice. An open access data-portal for the pedon data set and the GIS-data sets is available online at http://bolin.su.se/data/ncscd/. The NCSCDv2 data set has a digital object identifier (doi:10.5879/ECDS/00000002).

Highlights

  • High latitude terrestrial ecosystems are considered key components in the global carbon (C) cycle (McGuire et al, 2009)

  • This updated pedon data set provides a framework for spatially distributed quantification of soil organic C (SOC) at 100–300 cm depths in soils across the circumpolar permafrost region using the NCSCDv2 (Fig. 2)

  • In the currently assembled data set, we find no significant difference in 0–300 cm SOC storage between Histels from the West Siberian Lowland and Russian Histels outside of the West Siberian Lowland (t test, p > 0.05); West Siberian Lowland Histosols in the permafrost region have significantly less 0–300 cm SOC storage than Russian Histosols in the permafrost region outside of the West Siberian Lowland (t test, p < 0.05)

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Summary

Introduction

High latitude terrestrial ecosystems are considered key components in the global carbon (C) cycle (McGuire et al, 2009). The estimated SOC pool in deeper (> 300 cm) Yedoma deposits (407 Pg) and deltaic deposits (241 Pg) brings the total estimate to 1672 Pg, of which 1466 Pg is stored in perennially frozen ground (Tarnocai et al, 2009) This is about twice as much C as in the atmosphere (Houghton, 2007). The new data set provides separate estimates for the 100–200 cm and 200– 300 cm depth ranges, and represents a significant increase in the amount of available pedons compared to the previous estimate (increase by factors 11 and 8 for the two depth ranges, respectively) This data set has been integrated with the NCSCD (Hugelius et al, 2013) to enable upscaling and calculation of regional and circumpolar SOC stocks. The updated NCSCDv2 is freely available online in several different file formats and spatial resolutions that enable its applications in geographical information system (GIS) mappings and terrestrial ecosystem models

Data set structure
Gap filling with pedo-transfer functions
Extrapolation and estimates based on default values
Calculating SOC storage for soil taxa in different regions
Incorporating data into the updated NCSCDv2
Results and discussion
Permafrost-free mineral soils
Shallow soils and massive ground ice
Organic soils
Issues of data quality
Conclusions and data access
Full Text
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