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At line 46 added 8 lines
There can also be negative expectations that Mesolithic sites will be disturbed and therefore of little value, or that structural remains such as hearths, pits, and postholes are unlikely to be found: these perceptions can mean that important archaeology is missed or incorrectly assigned to other periods (Spikins 2010).
There are also a number of threats to the resource which in recent years have come to the fore. Growing pressure on previously uncultivated land, which on the one hand presents a new opportunity to identify unrecorded Mesolithic scatters, also results in potential further damage to buried sites which have long been protected by grassland. The severe drying out of peat, at upland sites due to climate change (''ibid''), and on lowland sites due to changing water tables often related to drainage (Boreham et al 2011; Milner et al 2011), is also having a significant damaging effect on the Mesolithic resource.
A number of coastal Mesolithic sites are also under threat from sea-level rise, or are currently eroding into the sea (Milner 2012), such as at Low Hauxley, Northumberland (Waddington 2011; Eadie and Waddington 2013). Rapid assessments of England’s coastal zones,
undertaken to inform asset management in areas affected by coastal erosion and defence, have added significant evidence for nearshore and intertidal peats and forest beds. Many of these organic deposits have dates showing that they formed during the Mesolithic period (eg Eadie
2013, chapter 6). These provide evidence of past environments and relative sea levels. A national database is managed by English Heritage and new discoveries can be added on-line at [http://www.englishheritage.org.uk/professional/research/heritage-science/environmentalarchaeology/Environmental-Studies-Resources/intertidal-peat-database/|http://www.englishheritage.org.uk/professional/research/heritage-science/environmentalarchaeology/Environmental-Studies-Resources/intertidal-peat-database/].