Lateglacial and Early Holocene palaeoenvironmental change and human activity at Killerby Quarry, North Yorkshire, UK

• Published in: Journal of quaternary science Vol. 38; no. 3; pp. 403 - 422
• Main Authors: Hudson, Samuel M, Waddington, Clive, Pears, Ben, Ellis, Natalie, Parker, Luke, Hamilton, Derek, Alsos, Inger Greve, Hughes, Paul, Brown, Antony
• Format: Journal Article
• Language: English
• Published: Chichester Wiley Subscription Services, Inc 01.04.2023; Wiley
• Subjects: Archaeology; Basins; Changing environments; Deoxyribonucleic acid; DNA; Environmental changes; Flora; Geochemistry; Holocene; hunter‐gatherers; Lakes; Landscape; Late Upper Palaeolithic; Lateglacial; Marshes; Mesolithic; Paleolakes; Pollen; Ponds; Quarries; sedaDNA; Swales; Swamps; Vegetation; Woodlands; United Kingdom > UK
• ISSN: 0267-8179; 1099-1417; 1099-1417
• DOI: 10.1002/jqs.3488

ABSTRACT The hunter‐gatherers that entered the British peninsula after ice‐retreat were exploiting a dynamic, rapidly changing environment. Records of vegetation change and human occupation during the Lateglacial to Early Holocene in northern Britain are more commonly found at upland and cave sites. However, recent research highlights many areas of the Swale–Ure Washlands that preserve extensive environmental sequences in low‐lying ice‐wastage basins, channels and depressions. The Lateglacial–Early Holocene environment of Killerby Quarry, North Yorkshire, is investigated here using a multi‐proxy approach of sedimentary ancient DNA (sedaDNA), pollen, sedimentological (geochemistry and portable optically stimulated luminescence), and rare and well‐preserved archaeology (Lavvu structures and lithics). Results show that the wetland basins and kettleholes were small lakes or ponds in the Lateglacial surrounded by sedge‐fen and birch woodland. A gradual (centennial scale) succession to reed‐swamp and then marsh is seen by the Early Holocene. This environment formed the resource‐scape for hunter‐gatherer transitory settlement in both the Lateglacial (Late Upper Palaeolithic) and Holocene (Early Mesolithic), attracted by the rich communities of pond‐related flora and fauna as well as easy strategic landscape access by way of the River Swale, an arterial route through the landscape connecting the North Sea Basin with the Pennine uplands via the palaeolakes around Killerby.