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“…In addition, a younger ice advance forming the Cromer Ridge push moraine and depositing thick outwash fan sediments of the Briton's Lane Formation has been correlated with MIS 6 The SAR OSL age estimate of 435 ± 21 ka BP for the glacial sequence is consistent with a previous attribution of Anglian stage glacial deposits to MIS 12 based on ESR dating ( 404 33 42 + − ka BP) suggesting that Hoxnian temperate stage lake sediments overlying Lowestoft Formation till at Hoxne are of MIS 11 age (Grün and Schwarcz, 2000). It is furthermore in keeping with U-series dating of Hoxnian deposits to MIS 11 at Marks Tey (Rowe et al, 1999). At both of these sites, continuity in sedimentation is thought to be well demonstrated because the organic deposits rest in kettle holes or tunnel valleys cut into Anglian Lowestoft Till.…”
Section: Discussion Of Chronological Significancesupporting
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“…In addition, a younger ice advance forming the Cromer Ridge push moraine and depositing thick outwash fan sediments of the Briton's Lane Formation has been correlated with MIS 6 The SAR OSL age estimate of 435 ± 21 ka BP for the glacial sequence is consistent with a previous attribution of Anglian stage glacial deposits to MIS 12 based on ESR dating ( 404 33 42 + − ka BP) suggesting that Hoxnian temperate stage lake sediments overlying Lowestoft Formation till at Hoxne are of MIS 11 age (Grün and Schwarcz, 2000). It is furthermore in keeping with U-series dating of Hoxnian deposits to MIS 11 at Marks Tey (Rowe et al, 1999). At both of these sites, continuity in sedimentation is thought to be well demonstrated because the organic deposits rest in kettle holes or tunnel valleys cut into Anglian Lowestoft Till.…”
Section: Discussion Of Chronological Significancesupporting
“…This event has been be dated to MIS 12 by reference to dated materials (AAR, U-series, ESR) that overlie or underlie the glaciogenic sediments (Bowen et al, 1986; Bowen, 1999, Rowe et al, 1999 Grün and Schwarcz, 2002;Preece et al, 2009;Penkman et al, 2011), and by direct dating of the glaciogenic material using OSL (Pawley et al, , 2010. The MIS 12 age allocation is reinforced by the fact that the glacial deposits at their southern limit can be correlated with terraces of the River Thames that have been dated by a number of geochronometric methods (Bridgland, 1994;Bridgland et al, 2004;Penkman et al, 2011).…”
Section: Terrestrial Evidence 421 Pre Mis 12 Glaciationsmentioning
“…This scheme proposes that in addition to the MIS 12 glaciation described above, extensive glaciation occurred in midland England and East Anglia during MIS 10. This glaciation is dated by a U-series age on overlying peat deposits (Rowe et al, 1999) and correlation of the glacial deposits with the terrace deposits of the Middle Thames near Oxford (Sumbler, 1995(Sumbler, , 2001, although this correlation has since been challenged (Westaway, 2011). The deposits of this glaciation are lithologically distinctive and can be traced above those of the Anglian Glaciation in north East Anglia, where they are sandy tills overlying chalky tills, and the east and west Midlands where they are chalky tills overlying chalk-free tills, but in central and southern east Anglia the tills of both MIS 12 and MIS 10 have a similar lithological composition and a limit for the MIS 10 event has yet to be identified.…”
mentioning
“…3), provides an important basis for supporting the 'longer' of these two chronologies. Added to this, and to the geochronological evidence from Beeches Pit, are results from uranium series dating of the Hoxnian type locality at Hoxne and the paratypesite at Marks Tey, Essex (Grün and Schwarcz, 2000;Rowe et al, 1999), both supporting correlation with MIS 11, and therefore the longer chronology.…”
Section: Synthesis: An Improved Record Of the Mis 9 Interglacial In Tmentioning