Chronostratigraphy of the 600,000 year old continental record of Lake Van (Turkey)

Lake Van sediment cores from the Ahlat Ridge and Northern Basin drill sites of the ICDP project PALEOVAN contain a wealth of information about past environmental processes. The sedimentary sequence was dated using climatostratigraphic alignment, varve chronology, tephrostratigraphy, argon-argon sing...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Stockhecke, Mona, Kwiecien, Ola, Vigliotti, Luigi, Anselmetti, Flavio S., Beer, Jürg, Çağatay, M. Namik, Channell, James E.T., Kipfer, Rolf, Lachner, Johannes, Litt, Thomas, Pickarski, Nadine, Sturm, Michael
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2014
Subjects:
ICDP project PALEOVAN
long terrestrial paleoenvironmental records
climatostratigraphic alignment
radiometric dating
tephrostratigraphy
magnetostratigraphy
Greenland
Hulu
EPICA
Greenland ice core
ice core
NGRIP
Online Access:https://doi.org/10.1016/j.quascirev.2014.04.008
Description
Summary:Lake Van sediment cores from the Ahlat Ridge and Northern Basin drill sites of the ICDP project PALEOVAN contain a wealth of information about past environmental processes. The sedimentary sequence was dated using climatostratigraphic alignment, varve chronology, tephrostratigraphy, argon-argon single-crystal dating, radiocarbon dating, magnetostratigraphy, and cosmogenic nuclides. Based on the lithostratigraphic framework, the different age constraints are compiled and a robust and precise chronology of the 600,000 year-old Lake Van record is constructed. Proxy records of total organic carbon content and sediment color, together with the calcium/potassium-ratios and arboreal pollen percentages of the 166-m-long event-corrected Ahlat Ridge record, mimic the Greenland isotope stratotype (NGRIP). Therefore, the proxy records are systematically aligned to the onsets of interstadials reflected in the NGRIP and synthesized Greenland ice-core stratigraphy. The chronology is constructed using 49 age control points derived from visual synchronization with the Greenland ice-core stratigraphy using the GICC05 timescale, an absolutely-dated speleothem timescale (e.g., Hulu, Sanbao, Linzhu cave) and the Epica Dome C timescale. In addition, the uppermost part of the sequence is complemented with four ages from Holocene varve chronology and three calibrated radiocarbon ages. Furthermore, nine argon-argon ages and a comparison of the relative paleointensity record of the magnetic field with reference curve PISO-1500 confirm the accuracy of the age model. Also the identification of the Laschamp event via measurements of 10 Be in the sediment confirms the presented age model. The chronology of the Ahlat Ridge record is transferred to the 79-m-long event-corrected composite record from the Northern Basin and supplemented by additional radiocarbon dating on organic marco-remains. The basal age of the Northern Basin record is estimated at ∼90 ka. The variations of the time series of total organic carbon content, the Ca/K ratio, and ...

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