Zanchetta, Giovanni, Baneschi, Ilaria, Francke, Alexander ORCID: 0000-0002-0370-5802, Boschi, Chiara, Regattieri, Eleonora ORCID: 0000-0003-0089-4027, Wagner, Bernd ORCID: 0000-0002-1369-7893, Lacey, Jack H. ORCID: 0000-0002-6329-2149, Leng, Melanie J., Vogel, Hendrik ORCID: 0000-0002-9902-8120 and Sadori, Laura ORCID: 0000-0002-2774-6705 (2018). 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. Quat. Sci. Rev., 202. S. 154 - 166. OXFORD: PERGAMON-ELSEVIER SCIENCE LTD. ISSN 0277-3791
Full text not available from this repository.Abstract
In the DEEP core from the Lake Ohrid ICDP drilling project, the carbon isotope composition of bulk organic matter (delta C-13(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 delta C-13(TOC) values corresponding to higher TIC and TOC. Along with TOC/TN, the correlation between delta C-13(TOC) and delta C-13(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 delta C-13(TOC) is able to disentangle long-term glacial/interglacial cycles and, to a lesser extent, millennial scale climate variability. Over the longer term, delta C-13(TOC) shows modest variability, indicating that the delta C-13 of the dissolved inorganic carbon (DIC) pool is stabilised by the supply of karst spring water characterised by delta C-13(DIC) influenced by the bedrock delta C-13 value, and the long residence time of the lake water and well mixed upper water column promoting equilibration with atmospheric CO2. However, comparison between arboreal pollen (AP%), TIC and TOC data indicates that the delta C-13(TOC) signal is modulated by the leaching of soil CO2 through runoff and spring discharge, changes in primary productivity, and recycling of organic matter within the lake, all affecting delta C-13(DIC). Exceptionally low delta C-13(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. (C) 2018 Elsevier Ltd. All rights reserved.
Item Type: | Journal Article | ||||||||||||||||||||||||||||||||||||||||||||
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URN: | urn:nbn:de:hbz:38-161959 | ||||||||||||||||||||||||||||||||||||||||||||
DOI: | 10.1016/j.quascirev.2018.10.022 | ||||||||||||||||||||||||||||||||||||||||||||
Journal or Publication Title: | Quat. Sci. Rev. | ||||||||||||||||||||||||||||||||||||||||||||
Volume: | 202 | ||||||||||||||||||||||||||||||||||||||||||||
Page Range: | S. 154 - 166 | ||||||||||||||||||||||||||||||||||||||||||||
Date: | 2018 | ||||||||||||||||||||||||||||||||||||||||||||
Publisher: | PERGAMON-ELSEVIER SCIENCE LTD | ||||||||||||||||||||||||||||||||||||||||||||
Place of Publication: | OXFORD | ||||||||||||||||||||||||||||||||||||||||||||
ISSN: | 0277-3791 | ||||||||||||||||||||||||||||||||||||||||||||
Language: | English | ||||||||||||||||||||||||||||||||||||||||||||
Faculty: | Unspecified | ||||||||||||||||||||||||||||||||||||||||||||
Divisions: | Unspecified | ||||||||||||||||||||||||||||||||||||||||||||
Subjects: | no entry | ||||||||||||||||||||||||||||||||||||||||||||
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Refereed: | Yes | ||||||||||||||||||||||||||||||||||||||||||||
URI: | http://kups.ub.uni-koeln.de/id/eprint/16195 |
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