Evidence for carbon cycling in a large freshwater lake in the Balkans over the last 0.5 million years using the isotopic composition of bulk organic matter.

Abstract In the DEEP core from the Lake Ohrid ICDP drilling project, the carbon isotope composition of bulk organic matter (δ13C TOC) over the last 516 ka shows a negative correlation with total organic carbon (TOC) and total inorganic carbon (TIC). This relationship is marked by periods of lower δ13C TOC values corresponding to higher TIC and TOC. Along with TOC/TN, the correlation between δ13C TOC and δ13C TIC suggests that most of the organic matter in the core is from aquatic primary production within the lake. The combination of TOC, TIC, and δ13C TOC is able to disentangle long-term glacial/interglacial cycles and, to a lesser extent, millennial scale climate variability. Over the longer term, δ13C TOC shows modest variability, indicating that the δ13C of the dissolved inorganic carbon (DIC) pool is stabilised by the supply of karst spring water characterised by δ13C DIC influenced by the bedrock δ13C value, and the long residence time of the lake water and well mixed upper water column promoting equilibration with atmospheric CO 2. However, comparison between arboreal pollen (AP%), TIC and TOC data indicates that the δ13C TOC signal is modulated by the leaching of soil CO 2 through runoff and spring discharge, changes in primary productivity, and recycling of organic matter within the lake, all affecting δ13C DIC. Exceptionally low δ13C TOC during some interglacial periods (e.g. MIS7 and MIS9) possibly indicate rapid intensification of organic matter recycling and/or increasing stratification and enhanced methanogenesis, even if the latter process is not supported by the sedimentological data. Highlights • The organic matter δ13C in Lake Ohrid's DEEP core is most from primary productivity. • DIC from the karst springs and atmospheric CO 2 equilibration dominate Lake Ohrid. • Soil CO 2 drives of the organic matter δ13C over interglacial/glacial periods. [ABSTRACT FROM AUTHOR]