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10th November 2016 - Lucy Farr, University of Cambridge:. Archaeological insights into the 8.2 ka event. ... 9th November 2012 - Dr Aline Govin (MARUM, Bremen):. Precipitation changes in the Amazon Basin during the last 240 ka.

Palaeoenvironmental records from the West Antarctic Peninsula drift sediments over the last 75 ka.

Palaeoenvironmental records from the West Antarctic Peninsula drift sediments over the last 75 ka.

10th November 2016 - Lucy Farr, University of Cambridge:. Archaeological insights into the 8.2 ka event. ... 9th November 2012 - Dr Aline Govin (MARUM, Bremen):. Precipitation changes in the Amazon Basin during the last 240 ka.

and Büntgen, U., 2024. Sudden disappearance of yew (Taxus baccata) woodlands from eastern England coincides with a possible climate event around 4.2 ka ago.

There is clear evidences that centennial droughts occurred is the past, especially between 4.5 and 3 kyr BP, which is sometimes reported as the 4.2 ka event.

478-424 ka), whilst glaciation during the subsequent Devensian Stage (MIS 2; c. ... 29-18 ka) resulted in blockage of The Wash, causing further river diversions.

In addition, Masaya is one of the few known volcanoes responsible for basaltic plinian activity (20 and 6.5 ka BP), and its subdued topography (about 600 m above sea-level)

In the Chew Bahir cores we are focussing on creating a high-resolution age model for the 135 ka – 125 ka interval, around the transition from MIS 6 to MIS 5, ... which will allow a test of the hypothesis that human population increase and range

Venue: Scott Polar Research Institute, main lecture theatre. The Scandinavian Ice Sheet (SIS) reached its maximum extent over Fennoscandia and Northern Europe 21–20 ka.