PGR Forum Session 1 11:10-11:30 Does vegetation respond to centennial-scale climatic oscillations? Evidence from Tirinie, a Last Glacial-Interglacial Transition site in the Scottish Highlands


Abrupt climatic change, during the Late Quaternary in northern Europe, can be identified using different proxy data sources from sedimentary archives. The Last Glacial-Interglacial Transition (LGIT) (16-8 ka BP) is one such period that provides evidence of well-defined millennial scale climatic oscillations and associated reorganisation of ecosystems… (More)