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Palaeo-seasonality of the last two millennia reconstructed from the oxygen isotope composition of carbonates and diatom silica from Nar Gölü, central Turkey

Yi?itba?io?lu, Hakan; Dean, Jonathan R.; Jones, Matthew D.; Leng, Melanie J.; Sloane, Hilary J.; Neil Roberts, C.; Woodbridge, Jessie; Swann, George E.A.; Metcalfe, Sarah E.; Eastwood, Warren J.; Yi?itba??o?lu, Hakan

Authors

Hakan Yi?itba?io?lu

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Dr Jonathan Dean J.Dean2@hull.ac.uk
Lecturer in Quaternary Science, Director of Education, Co-Deputy Head of School

Matthew D. Jones

Melanie J. Leng

Hilary J. Sloane

C. Neil Roberts

Jessie Woodbridge

George E.A. Swann

Sarah E. Metcalfe

Warren J. Eastwood

Hakan Yi?itba??o?lu



Contributors

Abstract

Carbonates and diatoms are rarely deposited together in lake sediments in sufficient quantities for the oxygen isotope composition (δ18O) to be investigated simultaneously from both hosts. Here, d18Ocarbonate are compared to δ18Odiatom data from the varved sediments of Nar Gölü, a closed lake in central Turkey, over the last 1710 years. Lake monitoring suggests carbonate is probably precipitated during MayeJune and δ18Ocarbonate is a proxy for regional water balance. Diatom activity is mainly weighted towards the spring. At times between ~301 and 561 AD, while δ18Ocarbonate values are the highest for the entire 1710 year period, suggesting summer drought, δ18Ocorrected-diatom values are among the lowest. δ18Olakewater values estimated for the times of diatom growth and carbonate precipitation show large differences. We suggest this could be explained by increased snowmelt that formed a freshwater lid on the lake at the time of peak diatom growth. Increased snowmelt is also inferred ~561-801 AD. From 801 AD to the present, precipitation is less winter-dominated, although increased snowmelt is inferred 921-1071 AD and in the latter part of the Little Ice Age (i.e. the mid to late 1800s AD). By combining oxygen isotope data from hosts that form in lakes at different times of the year, we show that such analyses can provide insights into palaeo-seasonality. © 2012 Elsevier Ltd. All rights reserved.

Citation

Yiǧitbaşioǧlu, H., Dean, J. R., Jones, M. D., Leng, M. J., Sloane, H. J., Neil Roberts, C., …Yiğitbaşıoğlu, H. (2013). Palaeo-seasonality of the last two millennia reconstructed from the oxygen isotope composition of carbonates and diatom silica from Nar Gölü, central Turkey. Quaternary science reviews, 66, 35-44. https://doi.org/10.1016/j.quascirev.2012.07.014

Journal Article Type Article
Acceptance Date Jul 11, 2012
Online Publication Date Aug 10, 2012
Publication Date Apr 15, 2013
Deposit Date Feb 22, 2020
Publicly Available Date Mar 31, 2020
Journal Quaternary Science Reviews
Print ISSN 0277-3791
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 66
Pages 35-44
DOI https://doi.org/10.1016/j.quascirev.2012.07.014
Keywords δ18O; Seasonality; Near East; Mass balance; Energy-Dispersive X-ray Spectroscopy; Lake sediments
Public URL https://hull-repository.worktribe.com/output/3444419
Publisher URL https://www.sciencedirect.com/science/article/pii/S0277379112002818?via%3Dihub
Related Public URLs http://nora.nerc.ac.uk/id/eprint/503475/

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