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Skáholt 2002 - Nabo

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ensuring local wealth; this may be further tested, by consideration of church<br />

cartularies. The alternative hypothesis is that Skálholt did not intensively manage<br />

land, preferring to rely on tithing (i.e. external income) to maintain wealth.<br />

If the first hypothesis is validated and intensity of land management at Skálholt is<br />

consistently high throughout the early ‘Christian’ period, then a second<br />

hypothesis is that crop productivity was high throughout this period, even during<br />

periods of climatic deterioration. This will, in part, reflect the significance of<br />

year-on-year improvement to land quality through manuring strategies.<br />

Soils survey will be undertaken by systematic ha nd augering and by exposure of selected<br />

profiles for sampling. Analyses of soils will be undertake using thin section<br />

micromorphology (Davidson and Simpson, 2001) and element analyses used in<br />

CENTURY soil organic carbon and productivity modelling (total carbon, total nitrogen<br />

and total phosphorus – Simpson et al., <strong>2002</strong>). The temporal and spatial framework of the<br />

study will allow statistical models and comparisons of soil properties and productivities<br />

to be made.<br />

Preliminary soil assessment<br />

A preliminary soil assessment has begun to indicate the validity of a soils-based approach<br />

to understanding early land management practices associated with the Skálholt<br />

ecclesiastical settlement. One exposure in a ditch section has demonstrated accumulating<br />

silt loam and sandy silt loam soils with colours ranging from 2.5YR 3/6 (dark red) to 10<br />

YR 3/1 (dark grey brown) (Figure 4). Prior to the landnám tephra of AD 871±2 there is<br />

no disturbance or amendment of soils. Post landnám there is evidence of cultivation<br />

ridges, with an earlier phase overlain by a later phase, that have a distance of<br />

approximately 120cm between the high points of the ridges. Based on colour<br />

characteristics, these cultivation ridges were created by overturning turves and exposing<br />

the soil. The occurrence of occasional fine charcoals and rare small bone fragments<br />

indicate that these soils were amended with a view to maintaining and enhancing soil<br />

15

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