A chronology of the PY608E-PC sediment core (Lake Pumoyum Co, southern Tibetan Plateau) based on radiocarbon dating of total organic carbon
被引:5
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作者:
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机构:
Watanabe, Takahiro
[1
,2
]
Nakamura, Toshio
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机构:
Nagoya Univ, Ctr Chronol Res, Chikusa Ku, Nagoya, Aichi 4648601, JapanTohoku Univ, Grad Sch Environm Studies, Aoba Ku, Sendai, Miyagi 9808579, Japan
Nakamura, Toshio
[3
]
Matsunaka, Tetsuya
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Tokai Univ, Sch Marine Sci & Technol, Shimizu, Shizuoka 4240902, JapanTohoku Univ, Grad Sch Environm Studies, Aoba Ku, Sendai, Miyagi 9808579, Japan
Matsunaka, Tetsuya
[4
]
Nara, Fumiko Watanabe
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Tohoku Univ, Grad Sch Sci, Aoba Ku, Sendai, Miyagi 9808578, JapanTohoku Univ, Grad Sch Environm Studies, Aoba Ku, Sendai, Miyagi 9808579, Japan
Nara, Fumiko Watanabe
[2
]
Zhu, Liping
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机构:
Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100085, Peoples R ChinaTohoku Univ, Grad Sch Environm Studies, Aoba Ku, Sendai, Miyagi 9808579, Japan
Zhu, Liping
[5
]
Wang, Junbo
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Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100085, Peoples R ChinaTohoku Univ, Grad Sch Environm Studies, Aoba Ku, Sendai, Miyagi 9808579, Japan
Wang, Junbo
[5
]
Kakegawa, Takeshi
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Tohoku Univ, Grad Sch Sci, Aoba Ku, Sendai, Miyagi 9808578, JapanTohoku Univ, Grad Sch Environm Studies, Aoba Ku, Sendai, Miyagi 9808579, Japan
Kakegawa, Takeshi
[2
]
论文数: 引用数:
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Nishimura, Mitsugu
[4
]
机构:
[1] Tohoku Univ, Grad Sch Environm Studies, Aoba Ku, Sendai, Miyagi 9808579, Japan
[2] Tohoku Univ, Grad Sch Sci, Aoba Ku, Sendai, Miyagi 9808578, Japan
[3] Nagoya Univ, Ctr Chronol Res, Chikusa Ku, Nagoya, Aichi 4648601, Japan
Tibetan Plateau;
Lake Pumoyum Co;
AMS;
C-14;
Lake sediment;
Climate change;
Old carbon effect;
QINGHAI;
GEOCHEMISTRY;
GLACIATION;
D O I:
10.1016/j.nimb.2012.07.015
中图分类号:
TH7 [仪器、仪表];
学科分类号:
0804 ;
080401 ;
081102 ;
摘要:
Paleoclimatic records from the Tibetan Plateau provide important clues for understanding the Asian monsoon and Asian climate systems. To reconstruct climatic and environmental changes in the southern Tibetan Plateau, a 3.77-m-long sediment core (PY608E-PC) was taken from the southeastern part of Lake Pumoyum Co in August 2006. Because terrestrial plant residues are extremely rare in this core, we performed radiocarbon dating on the total organic carbon fraction. We also estimated the old carbon effect and radiocarbon reservoir age of the total organic carbon fraction. Using these estimates, we propose a new radiocarbon chronology for past climatic changes from ca. 12,500 to 700 cal BP. The linear sedimentation rate of the core was founded to be constant at 32.0 cm/kyr, indicating stable sedimentation conditions in Lake Pumoyum Co from the period of the Younger Dryas to the Holocene. (C) 2012 Elsevier B.V. All rights reserved.