AMS C-14 chronology of the world's southernmost woolly mammoth (Mammuthus primigenius Blum.)

IVPP-IR > 中科院古脊椎所（2000年以后）

	AMS C-14 chronology of the world's southernmost woolly mammoth (Mammuthus primigenius Blum.)
	Takahashi, Keiichi ; Wei, Guangbiao ; Uno, Hikaru ; Yoneda, Minoru ; Jin, Changzhu ; Sun, Chengkai ; Zhang, Sheng ; Zhong, Bei ; Takahashi, K (reprint author), Lake Biwa Museum, 1091 Oroshimo, Shiga 5250001, Japan.
	2007-04-01
发表期刊	QUATERNARY SCIENCE REVIEWS
ISSN	0277-3791
卷号	26 期号:7-8 页码:954-957
文章类型	Article
摘要	The world's definite southernmost woolly mammoth record is a molar from Ji'nan (around 36 degrees N), Shandong Province, China. AMS C-14 dating of the specimen, gave a conventional C-14 age of 33,150 +/- 250 BP. The period of 40-30 ka BP corresponds to the later phase of the Marine Oxygen Isotope Stage 3 (MIS 3a), recognized as the global interstadial of the last glacial period. However, it is known that the winter monsoon strengthened in Asia during the period 35-33 ka BP, and the age of the woolly mammoth specimen from Ji'nan corresponds to that age. The specimen suggests that this area became cold and dry in 33 ka BP, and grassland or open forest, suitable habitat for woolly mammoths, developed during this short time span. This age is similar to the age of the southernmost woolly mammoth record in Europe, therefore supporting a hypothesis by Porter and An [1995. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305-308] that an important component of Chinese palaeoclimates may be linked to changes in North Atlantic oceanic conditions. (c) 2007 Elsevier Ltd. All rights reserved.; The world's definite southernmost woolly mammoth record is a molar from Ji'nan (around 36 degrees N), Shandong Province, China. AMS C-14 dating of the specimen, gave a conventional C-14 age of 33,150 +/- 250 BP. The period of 40-30 ka BP corresponds to the later phase of the Marine Oxygen Isotope Stage 3 (MIS 3a), recognized as the global interstadial of the last glacial period. However, it is known that the winter monsoon strengthened in Asia during the period 35-33 ka BP, and the age of the woolly mammoth specimen from Ji'nan corresponds to that age. The specimen suggests that this area became cold and dry in 33 ka BP, and grassland or open forest, suitable habitat for woolly mammoths, developed during this short time span. This age is similar to the age of the southernmost woolly mammoth record in Europe, therefore supporting a hypothesis by Porter and An [1995. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305-308] that an important component of Chinese palaeoclimates may be linked to changes in North Atlantic oceanic conditions. (c) 2007 Elsevier Ltd. All rights reserved.
WOS标题词	Science & Technology ; Physical Sciences
URL	查看原文
关键词[WOS]	NIES-TERRA ; CHINA
收录类别	SCI
语种	英语
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:000248732200009
引用统计
文献类型	期刊论文
条目标识符	http://119.78.100.205/handle/311034/3375
专题	中科院古脊椎所（2000年以后）
通讯作者	Takahashi, K (reprint author), Lake Biwa Museum, 1091 Oroshimo, Shiga 5250001, Japan.
作者单位	1.Lake Biwa Museum, Shiga 5250001, Japan 2.Chongqing Museum Nat Hist, Chongqing 400013, Peoples R China 3.Environm Chem Div, Ecol Chem Sect, Tsukuba, Ibaraki, Japan 4.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
推荐引用方式 GB/T 7714	Takahashi, Keiichi,Wei, Guangbiao,Uno, Hikaru,et al. AMS C-14 chronology of the world's southernmost woolly mammoth (Mammuthus primigenius Blum.)[J]. QUATERNARY SCIENCE REVIEWS,2007,26(7-8):954-957.
APA	Takahashi, Keiichi.,Wei, Guangbiao.,Uno, Hikaru.,Yoneda, Minoru.,Jin, Changzhu.,...&Takahashi, K .(2007).AMS C-14 chronology of the world's southernmost woolly mammoth (Mammuthus primigenius Blum.).QUATERNARY SCIENCE REVIEWS,26(7-8),954-957.
MLA	Takahashi, Keiichi,et al."AMS C-14 chronology of the world's southernmost woolly mammoth (Mammuthus primigenius Blum.)".QUATERNARY SCIENCE REVIEWS 26.7-8(2007):954-957.

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