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Changes varied by wetland class and the presence or absence of surface water outlets.
Fig. 2 Map overlay results showing a distribution of pre-settlement wetlands colour coded by wetland class, b current wetlands colour coded by wetland class, and c current land cover classification for converted wetlands, coloured by land use type.
With coarse (250 m–1 km resolution) data, peatlands typically are grouped with a more general wetland class.
In the pre-settlement reconstruction, the marsh wetland class is overwhelmingly dominant and swamp wetlands are proportionately much smaller; both observations contrast to modern-day (Fig. 2).
Each pre-settlement polygon had spatial proximity with type-classified polygons from the 2011 wetland map, and the spatially closest one was allocated to the same wetland class.
Tree swamp is now the most frequent wetland class (Fig. 2b) and occupies 75.6% of the total current wetlands by areal extent, compared to 40.5% of the total historical wetland extent in Table 1.
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However, wetland classes vary in terms of carbon storage potential.
The greatest densities of SOC were documented in wetland classes.
Different land uses were summarized by each ecodistrict and by our five wetland classes.
The wetland classes were categorised by employing the Ramsar classification system for wetland types.
Thus, a critical step in obtaining accurate estimates of potential wetland carbon storage is the assignment to correct wetland classes, as each class has different carbon storage potential.
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