δ18 o and Trace Element Measurements as Proxy for the Reconstruction of Climate Changes at Lake Van (Turkey): Preliminary Results
The sediments of Lake Van, the fourth largest terminal lake on earth, located at the eastern end of the Taurus Mountain Range show an undisturbed continuous record of chemically precipitated carbonate varves, which provide:
a, a yearly carrier for changes in environmental proxy like δ18O, Sr/Caand Mg/Ca of authochthonous precipitated carbonates which allow to detect short term climatic variations,
b, a continuous, non floating varve chronology back to 13,700±356 yrs BP.
Calculations based on an isotopic-hydrologic balance model show that temperature fluctuations are less important for the isotope enrichment in Lake Van than changes of the relative humidity. Thus a paleohumidity curve of Lake Van can be estimated and compared to a Mg/Ca record which is found to be a proxy for lake salinity.
Lake Van sediments indicate a first period of cold and arid climate between 12,600–10,460 yrs BP. During this time humidity decreased by 0.17 or 30% (no temperature shift) or 20%, if temperature is reduced by 5 °C.
A second phase of climatic change also occurred: in a first period (4,190–3,040yrs B.P.), slightly reduction in lake level and humidity mark a regional climate shift toward more continental climate with reduced precipitation. In a second period (3,040– 2,000 yrs B.P.), precipitation increased again, but humidity remained at a level reduced 5% below that encountered today.
- δ18o and Trace Element Measurements as Proxy for the Reconstruction of Climate Changes at Lake Van (Turkey): Preliminary Results
- Book Title
- Third Millennium BC Climate Change and Old World Collapse
- pp 653-678
- Print ISBN
- Online ISBN
- Series Title
- NATO ASI Series
- Series Volume
- Series Subtitle
- Series I: Global Environmental Change
- Springer Berlin Heidelberg
- Copyright Holder
- Springer-Verlag Berlin Heidelberg
- Additional Links
- eBook Packages
- Editor Affiliations
- 1. Department of Geology, Istanbul Technical University
- 2. Lamont Doherty Earth Observatory, Columbia University
- 3. Departments of Anthropology and New Eastern Languages and Civilizations, Yale University
- Author Affiliations
- 4. EAWAG, Swiss Federal Institute for Environmental Science and Technology, Dübendorf, Switzerland
To view the rest of this content please follow the download PDF link above.