共 27 条
Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey
被引:357
作者:
Fleitmann, D.
[1
,3
]
Cheng, H.
[2
]
Badertscher, S.
[1
,3
]
Edwards, R. L.
[2
]
Mudelsee, M.
[4
]
Goektuerk, O. M.
[1
,3
]
Fankhauser, A.
[1
]
Pickering, R.
[1
]
Raible, C. C.
[3
,5
]
Matter, A.
[1
]
Kramers, J.
[1
]
Tuysuz, O.
[6
]
机构:
[1] Univ Bern, Inst Geol Sci, CH-3012 Bern, Switzerland
[2] Univ Minnesota Twin Cities, Dept Geol & Geophys, Minneapolis, MN 55455 USA
[3] Univ Bern, Oeschger Ctr Climate Change Res, CH-3012 Bern, Switzerland
[4] Climate Risk Anal, D-30167 Hannover, Germany
[5] Univ Bern, Inst Phys, CH-3012 Bern, Switzerland
[6] Istanbul Tech Univ, Eurasia Inst Earth Sci, TR-80626 Istanbul, Turkey
基金:
瑞士国家科学基金会;
美国国家科学基金会;
关键词:
LAST GLACIAL PERIOD;
LATE PLEISTOCENE;
HIGH-RESOLUTION;
MONSOON RECORD;
ICE;
SPELEOTHEMS;
MARINE;
CALIBRATION;
CHRONOLOGY;
EUROPE;
D O I:
10.1029/2009GL040050
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
A 50 kyr-long exceptionally well-dated and highly resolved stalagmite oxygen (delta(18)O) and carbon (delta(13)C) isotope record from Sofular Cave in northwestern Turkey helps to further improve the dating of Greenland Interstadials (GI) 1, and 3-12. Timing of most GI in the Sofular record is consistent within +/- 10 to 300 years with the "iconic'' Hulu Cave record. Larger divergences (>500 years) between Sofular and Hulu are only observed for GI 4 and 7. The Sofular record differs from the most recent NGRIP chronology by up to several centuries, whereas age offsets do not increase systematically with depth. The Sofular record also reveals a rapid and sensitive climate and ecosystem response in the eastern Mediterranean to GI, whereas a phase lag of similar to 100 years between climate and full ecosystem response is evident. Finally, results of spectral analyses of the Sofular isotope records do not support a 1,470-year pacing of GI. Citation: Fleitmann, D., et al. (2009), Timing and climatic impact of Greenland interstadials recorded in stalagmites from northern Turkey, Geophys. Res. Lett., 36, L19707, doi: 10.1029/2009GL040050.
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