Speleothem isotopic evidence of winter rainfall variability in northeast Turkey between 77 and 6 ka

An oxygen isotope record from a stalagmite that grew between 77 ka and 6 ka in northeast Turkey contains both a strong precessional signal, and sub-orbital oscillations similar to those in Greenland ice cores and Chinese speleothem records of monsoon intensity. Fluid inclusion evidence of a negative...

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Veröffentlicht in:	Quaternary science reviews 2012-06, Vol.45, p.60-72
Hauptverfasser:	Rowe, P.J., Mason, J.E., Andrews, J.E., Marca, A.D., Thomas, L., van Calsteren, P., Jex, C.N., Vonhof, H.B., Al-Omari, S.
Format:	Artikel
Sprache:	eng
Schlagworte:	Asian monsoons Carbon isotopes Fluid inclusions Last glacial maximum Mediterranean Oxygen isotopes Palaeoclimate Precession Speleothem U–Th dating
Online-Zugang:	Volltext
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