Holocene climate evolution: information from the Lacustrine–Fluvial sediment in North China

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Han-tao Ni ◽  
Yong Wang ◽  
Fei Tian ◽  
Pei-yi Yao ◽  
Lu-peng Yuan ◽  
...  
2018 ◽  
Vol 30 (4) ◽  
pp. 1161-1176
Author(s):  
WU Yaling ◽  
◽  
WANG Yongbo ◽  
LIU Xingqi ◽  
YU Zhitong ◽  
...  

Terra Nova ◽  
1997 ◽  
Vol 9 (5) ◽  
pp. 246-250
Author(s):  
M. Bernasconi ◽  
J. Dobson ◽  
J.A. McKenzie ◽  
D. Ariztegui ◽  
F. Niessen ◽  
...  

2008 ◽  
Vol 25 (6) ◽  
pp. 986-998 ◽  
Author(s):  
Wolfgang Schwanghart ◽  
Brigitta Schütt ◽  
Michael Walther

Terra Nova ◽  
1997 ◽  
Vol 9 (5-6) ◽  
pp. 246-250 ◽  
Author(s):  
S. M. Bernasconi ◽  
J. Dobson ◽  
J. A. McKenzie ◽  
D. Ariztegui ◽  
F. Niessen ◽  
...  

2017 ◽  
Vol 473 ◽  
pp. 16-25 ◽  
Author(s):  
Kasun Gayantha ◽  
Joyanto Routh ◽  
Rohana Chandrajith

2015 ◽  
Vol 129 ◽  
pp. 111-127 ◽  
Author(s):  
Heiko Moossen ◽  
James Bendle ◽  
Osamu Seki ◽  
Ursula Quillmann ◽  
Kimitaka Kawamura

The Holocene ◽  
2021 ◽  
pp. 095968362110332
Author(s):  
Wuhui Duan ◽  
Zhibang Ma ◽  
Ming Tan ◽  
Hai Cheng ◽  
R. Lawrence Edwards ◽  
...  

In this paper, a new decadal resolution stalagmite δ18O record covering 10.4–6.5 ka BP from Kulishu cave in Beijing, north China is presented in combination with the published stalagmite δ18O record covering 10.4–14.0 ka BP in the same cave. Five significant monsoon collapses were identified around 11.5, 11.0, 10.0, 9.4, and 8.2 ka BP as well as three smaller ones around 10.3, 9.0, and 8.6 ka BP. The weak monsoon episodes around 8.6 and 8.2 ka BP form the two-step structure of the 8.2 ka event. All monsoon collapses, coeval with the cooling in northern high-latitude records, are correlated with Lakes Agassiz-Ojibway outbursts. Thus, our data support the idea of freshwater forcing of abrupt climate anomalies during the early Holocene. Nevertheless, the decreased irradiance together with freshwater outburst may account for the 9.2/9.3 ka event, which is expressed more significantly in low-latitude records.


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