Jonathan R. Dean
Tracking the hydro-climatic signal from lake to sediment: a field study from central Turkey
Dean, Jonathan R.; Eastwood, Warren J.; Roberts, Neil; Jones, Matthew D.; Yi?itba??o?lu, Hakan; Allcock, Samantha L.; Woodbridge, Jessie; Metcalfe, Sarah E.; Leng, Melanie J.
Authors
Warren J. Eastwood
Neil Roberts
MATTHEW JONES MATTHEW.JONES@NOTTINGHAM.AC.UK
Professor of Quaternary Science
Hakan Yi?itba??o?lu
Samantha L. Allcock
Jessie Woodbridge
Professor SARAH METCALFE SARAH.METCALFE@NOTTINGHAM.AC.UK
Deputy Pro-Vice-Chancellor Research Andknowledge Exchange
PROFESSOR MELANIE LENG Melanie.Leng@nottingham.ac.uk
Professor of Isotope Geosciences
Abstract
Palaeo-hydrological interpretations of lake sediment proxies can benefit from a robust understanding of the modern lake environment. In this study, we use Nar Gölü, a non-outlet, monomictic maar lake in central Turkey, as a field site for a natural experiment using observations and measurements over a 17-year monitoring period (1997–2014). We compare lake water and sediment trap data to isotopic, chemical and biotic proxies preserved in its varved sediments. Nar Gölü underwent a 3 m lake-level fall between 2000 and 2010. δ18Olakewater is correlated with this lake-level fall, responding to the change in water balance. Endogenic carbonate is shown to precipitate in isotopic equilibrium with lake water and there is a strong relationship between δ18Olakewater and δ18Ocarbonate, which suggests the water balance signal is accurately recorded in the sediment isotope record. Over the same period, sedimentary diatom assemblages also responded, and conductivity inferred from diatoms showed a rise. Shifts in carbonate mineralogy and elemental chemistry in the sediment record through this decade were also recorded. Intra-annual changes in δ18Olakewater and lake water chemistry are used to demonstrate the seasonal variability of the system and the influence this may have on the interpretation of δ18Ocarbonate. We use these relationships to help interpret the sedimentary record of changing lake hydrology over the last 1725 years. Nar Gölü has provided an opportunity to test critically the chain of connection from present to past, and its sedimentary record offers an archive of decadal- to centennial-scale hydro-climatic change
Citation
Dean, J. R., Eastwood, W. J., Roberts, N., Jones, M. D., Yiğitbaşıoğlu, H., Allcock, S. L., …Leng, M. J. (2015). Tracking the hydro-climatic signal from lake to sediment: a field study from central Turkey. Journal of Hydrology, 529(2), 608-621. https://doi.org/10.1016/j.jhydrol.2014.11.004
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 22, 2014 |
Online Publication Date | Nov 11, 2014 |
Publication Date | Oct 1, 2015 |
Deposit Date | Feb 11, 2016 |
Publicly Available Date | Feb 11, 2016 |
Journal | Journal of Hydrology |
Print ISSN | 0022-1694 |
Electronic ISSN | 1879-2707 |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 529 |
Issue | 2 |
Pages | 608-621 |
DOI | https://doi.org/10.1016/j.jhydrol.2014.11.004 |
Keywords | Oxygen Isotopes, Diatom Analysis, Lake Sediments, Monitoring, Seasonality, Carbonates |
Public URL | https://nottingham-repository.worktribe.com/output/759790 |
Publisher URL | http://www.sciencedirect.com/science/article/pii/S0022169414008890 |
Contract Date | Feb 11, 2016 |
Files
Dean et al. 2015 JoH.pdf
(2.9 Mb)
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Copyright Statement
Copyright information regarding this work can be found at the following address: http://creativecommons.org/licenses/by-nc-nd/4.0
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