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Does temperature drive enhanced carbon cycling in Holocene lake sediments?

This project will use annually laminated (varved) lake sediments to reconstruct Holocene sub-decadal summer temperature and carbon cycling. These records can evaluate: (a) different driver-response mechanisms at different timescales; (b) new temperature (including seasonal bias) and carbon cycling proxies; (c) whether past warmer periods enhanced carbon cycling in lakes.

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Imported from UKRI Gateway to Research | Grant 031FB79F-1911-4B17-B82C-014F3A875912.

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Overview

UKRI Gateway to Research record

Grant agreement 031FB79F-1911-4B17-B82C-014F3A875912

Open source

This project will use annually laminated (varved) lake sediments to reconstruct Holocene sub-decadal summer temperature and carbon cycling. These records can evaluate: (a) different driver-response mechanisms at different timescales; (b) new temperature (including seasonal bias) and carbon cycling proxies; (c) whether past warmer periods enhanced carbon cycling in lakes.