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| Funder | Natural Environment Research Council |
|---|---|
| Recipient Organization | University of Cambridge |
| Country | United Kingdom |
| Start Date | Sep 30, 2023 |
| End Date | Mar 30, 2027 |
| Duration | 1,277 days |
| Number of Grantees | 2 |
| Roles | Student; Supervisor |
| Data Source | UKRI Gateway to Research |
| Grant ID | 2887807 |
Pleistocene volcanism associated with the MER produced colossal pyroclastic deposits found widely as tephra layers within sedimentary archives such as lake sediments and fluvial terraces. Due to the prevalence of tephra in archaeological sequences, their correlation and dating has become fundamental to the chronology of the hominin record
in Ethiopia (and in eastern Africa more generally). However, the record of past MER volcanism is far from complete and recent work combining volcanic outcrop, archaeological, fluvial and lake sediment sequences, has shown that many correlations require testing with new samples and state-of-the-art analytical protocols. In addition, there is now
demonstrated potential to use cryptotephra methods to fill critical gaps in the volcanological record and increase the detection and correlation of tephra isochrons within sedimentary sequences.
University of Cambridge
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