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   dcterms:identifier "fig-11-5";
   gcis:figureNumber "11.5"^^xsd:string;
   dcterms:title "Mechanisms of Soil Carbon Stabilization Associated with Different Soil Orders in the Northern Circumpolar Permafrost Zone"^^xsd:string;
   gcis:hasCaption "Gelisol soils\r\nhave a seasonally frozen active layer at the soil surface\r\nand perennially frozen (permafrost) layer at depth.\r\nHistosol and other soil orders in the permafrost zone\r\nhave seasonally frozen soil at the surface. Of the Gelisol\r\nsoils, freeze-thaw mixing is indicative of the Turbel suborder\r\nand waterlogging of the Histel suborder; Orthels\r\ndo not have characteristics of the first two suborders.\r\nMineral complexation and other mechanisms preserving\r\ncarbon are features of all soils but are labeled here as\r\nsoil orders and suborders not strongly characterized\r\nby freeze-thaw processes or waterlogging. Pie area\r\nrepresents proportional storage of carbon (soil depth of\r\n0 to 3 m) in the permafrost zone. [Data source: Hugelius\r\net al., 2014; see also Table 11.1, p. 439.]"^^xsd:string;
   dcterms:rights [ rdf:value "Figure may be copyright protected and permission may be required. Contact original figure source for information"^^xsd:string; ];
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   a gcis:Figure, doco:Figure .