In both valleys there exists a clear lithostratigraphic boundary between basal gravels with organic channel fills and a thick capping sandy silt unit (up to 5 m thick). In both valleys this sedimentary Dinaciclib discontinuity or bounding surface can be traced throughout the valley fill. In terms of sedimentary architecture it is therefore clear that it is higher than a 5th order bounding surface (sensu Miall, 1996) and so must be a 6th order surface comparable to the discontinuity which exists between the bedrock and valley fill or between Pleistocene glacial sediments and the Holocene fill ( Table 3; Murton and Belshaw, 2011). Such surfaces often form boundaries for geological

Stages and also Epochs. However, in the Frome this bounding surface is dated at 3600–4400 cal BP but in the Culm it is dated to 1300–220 cal BP. From palaeoecological and archaeological data we can see that this abrupt change in sedimentation is primarily a function of intensive arable agriculture. Even over as short a distance as 100 km this

boundary is time-transgressive by at least 2300 years and could not be associated with any one climatic episode in the Holocene. This presents significant problems for the recognition of this sedimentary boundary as the start of the Anthropocene. This agriculturally created sedimentary boundary is also common across North West Europe. find more Excellent examples have been documented in Northern France (Lespez et al., 2008), Saxony in northern Germany (Bork, 1989 and Bork and Lang, 2003), mid-Germany (Houben, 2012), south Germany (Dotterweich, 2008) and further east in Poland (Starkel et al., 2006 and Dotterweich et al., 2012) and Slovakia (Dotterweich et al., 2013). Indeed wherever lowland Holocene sedimentary sequences are investigated such a discontinuity is discovered. Moving south the picture is complicated by the greater sensitivity of Mediterranean catchments to climatic influences (cf. Maas and Macklin, 2002, Butzer, 2005 and Fuchs, 2007). However, it has been identified in northern and central Italy ( Brown and Ellis, 1996) and Greece Tyrosine-protein kinase BLK ( van Andel et al., 1990,

Lespez, 2003 and Fuchs, 2007) and Spain ( Schulte, 2002 and Thorndycraft and Benito, 2006). It is clear that in Europe there is significant diachrony in the late Holocene increase in valley sedimentation but it most frequently occurs over the last 1000 to 2000 years ( Notebaert and Verstraeten, 2010). Recent studies have also shown similar alluvial chronologies in northern Africa, which appear primarily driven by rapid climate change events but with sedimentation response being intensified by anthropogenic impact ( Faust et al., 2004 and Schuldenrein, 2007). Studies to the east from the Levant to India have largely been part of archaeological investigations and have focussed on climatic influences on early agricultural societies.