Jonathan R. Dean
Palaeo-seasonality of the last two millennia reconstructed from the oxygen isotope composition of carbonates and diatom silica from Nar Gölü, central Turkey
Dean, Jonathan R.; Jones, Matthew D.; Leng, Melanie J.; Sloane, Hilary J.; Neil Roberts, C. Neil; Woodbridge, Jessie; Swann, George E.A.; Metcalfe, Sarah E.; Eastwood, Warren J.; Yiǧitbaşioǧlu, Hakan
Authors
Professor MATTHEW JONES MATTHEW.JONES@NOTTINGHAM.AC.UK
Head of School (Professor of Quaternary Science)
Professor MELANIE LENG Melanie.Leng@nottingham.ac.uk
PROFESSOR OF ISOTOPE GEOSCIENCES
Hilary J. Sloane
C. Neil Neil Roberts
Jessie Woodbridge
Professor GEORGE SWANN GEORGE.SWANN@NOTTINGHAM.AC.UK
PROFESSOR OF PALAEOCLIMATOLOGY
Professor SARAH METCALFE SARAH.METCALFE@NOTTINGHAM.AC.UK
Deputy Pro-Vice-Chancellor Research Andknowledge Exchange
Warren J. Eastwood
Hakan Yiǧitbaşioǧlu
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
Dean, J. R., Jones, M. D., Leng, M. J., Sloane, H. J., Neil Roberts, C. N., Woodbridge, J., Swann, G. E., Metcalfe, S. E., Eastwood, W. J., & Yiǧitbaşioǧlu, 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 |
Publication Date | Apr 15, 2013 |
Deposit Date | Feb 13, 2025 |
Publicly Available Date | Feb 28, 2025 |
Journal | Quaternary Science Reviews |
Print ISSN | 0277-3791 |
Electronic ISSN | 1873-457X |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 66 |
Pages | 35-44 |
DOI | https://doi.org/10.1016/j.quascirev.2012.07.014 |
Public URL | https://nottingham-repository.worktribe.com/output/3178529 |
Publisher URL | https://www.sciencedirect.com/science/article/pii/S0277379112002818?via%3Dihub |
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Publisher Licence URL
https://creativecommons.org/licenses/by/3.0/
Copyright Statement
0277-3791 Ó 2012 Elsevier Ltd.
http://dx.doi.org/10.1016/j.quascirev.2012.07.014
Quaternary Science Reviews 66 (2013) 35e44
Open access under CC BY license.
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