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Episodes of aeolian sand movement, Skagen Odde, Denmark Reimann et al. 2011) report extensive aeolian sand movement and transgressive dune formation along north-western European shores during the Little Ice Age (LIA) between approximately AD 1350 and AD 1900 (Hass 1996). This phase of large-scale aeolian sand movement has been related to increased North Atlantic storminess (e.g. Clarke & Rendell 2009; Clemmensen et al. 2009). Aeolian sand invasion was particular severe along the Danish west coast of Jutland where transgressive dunes formed by persistent westerly storm winds migrated up to 10 km inland during this period (Clemmensen et al. 2007; Clemmensen et al. 2009). Also the Skagen Odde spit system in northCoastal dunefields in north-western Europe have experienced episodic activation throughout the later part of the Holocene (e.g. Clarke & Rendell 2009, 2011; Clemmensen et al. 2009). If dated sufficiently precisely and placed correctly in a cultural framework, periods of aeolian sand movement within the dunefields may act as proxy records of past wind climate and North Atlantic storminess variation (e.g. Clemmensen et al. 2001a; Clemmensen et al. 2007; Madsen et al. 2007; Clarke & Rendell 2009; Clemmensen et al. 2009). Numerous studies (e.g. Pye & Neal 1993; Knight et al. 1998; Wilson et al.2001, 2004; Clarke et al. 2002; Clarke & Rendell 2009; Clemmensen et al. 2009; Episodes of aeolian sand movement on a large spit system (Skagen Odde, Denmark) and North Atlantic storminess during the Little Ice Age