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Seasonality of Holocene hydroclimate in the Eastern Mediterranean reconstructed using the oxygen isotope composition of carbonates and diatoms from Lake Nar, central Turkey

Dean, Jonathan R.; Jones, Matthew D.; Leng, Melanie J.; Sloane, Hilary J.; Eastwood, Warren J.; Roberts, C. Neil; Dean, Jonathan; Eastwood, Warren; Jones, Matthew; Leng, Melanie; Metcalfe, Sarah E.; Roberts, Neil; Sloane, Hilary

Authors

Jonathan R. Dean

Matthew D. Jones

Melanie J. Leng

Hilary J. Sloane

Warren J. Eastwood

C. Neil Roberts

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

Warren Eastwood

Matthew Jones

Melanie Leng

Sarah E. Metcalfe

Neil Roberts

Hilary Sloane



Abstract

A positive shift in the oxygen isotope composition (δ¹⁸O) of lake carbonates in the Eastern Mediterranean from the early to late Holocene is usually interpreted as a change to drier (reduced precipitation and evaporation (P/E)) conditions. However, it has also been suggested that changes in the seasonality of precipitation could explain these trends. Here, Holocene records of δ¹⁸O from both carbonates and diatom silica, from Lake Nar in central Turkey, provide insights into palaeoseasonality. We show how Δδ18Olakewater (the difference between spring and summer reconstructed δ¹⁸Olakewater) was minimal in the early Holocene and for most of the last millennium, but was greater at other times. For example, between ~4100 and 1600 yr BP, we suggest that increased Δδ¹⁸Olakewater could have been the result of relatively more spring/summer evaporation, amplified by a decline in lake level. In terms of change in annual mean δ¹⁸O, isotope mass balance modelling shows that this can be influenced by changes in seasonal P/E as well as inter-annual P/E, but lake level falls inferred from other proxies confirm that there was a mid-Holocene transition to drier climatic conditions in central Turkey.

Citation

Dean, J. R., Jones, M. D., Leng, M. J., Sloane, H. J., Eastwood, W. J., Roberts, C. N., …Sloane, H. (2018). Seasonality of Holocene hydroclimate in the Eastern Mediterranean reconstructed using the oxygen isotope composition of carbonates and diatoms from Lake Nar, central Turkey. Holocene, 28(2), 267-276. https://doi.org/10.1177/0959683617721326

Journal Article Type Article
Acceptance Date Jun 19, 2017
Online Publication Date Aug 1, 2017
Publication Date Feb 1, 2018
Deposit Date Aug 3, 2017
Publicly Available Date Aug 3, 2017
Journal The Holocene
Print ISSN 0959-6836
Electronic ISSN 1477-0911
Publisher SAGE Publications
Peer Reviewed Peer Reviewed
Volume 28
Issue 2
Pages 267-276
DOI https://doi.org/10.1177/0959683617721326
Keywords Eastern Mediterranean, Lake sediment
Public URL https://hull-repository.worktribe.com/output/453886
Publisher URL http://journals.sagepub.com/doi/10.1177/0959683617721326
Additional Information This is the accepted manuscript of an article published in The Holocene, 2017.

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Copyright Statement
© 2017 The authors. Reprinted by permission of SAGE Publications.





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