Higher sea surface temperature in the northern South China Sea during the natural warm periods of late Holocene than recent decades
文献类型：期刊论文
| 作者 | Shao, D (Shao, Da)[ 1 ]; Wei, GJ (Wei, Gangjian)[ 4 ]; Wang, YH (Wang, Yuhong)[ 3 ]; Sun, LG (Sun, Liguang)[ 1 ]; Yan, H (Yan, Hong)[ 2,1 ] |
| 刊名 | CHINESE SCIENCE BULLETIN
 |
| 出版日期 | 2014-11-01 |
| 卷号 | 59期号:31页码:4115-4122 |
| 关键词 | Tridacna South China Sea Lateholocene Natural Warm Periods Sea Surfacetemperature |
| DOI | 10.1007/s11434-014-0317-3 |
| 文献子类 | 期刊论文 |
| 英文摘要 | The large-scale syntheses of global mean temperatures in IPCC fourth report suggested that the Northern Hemisphere temperature in the second half of the 20th century was likely the highest in at least the past 1,300 years and the 1990s was likely the warmest decade. However, this remains debated and the controversy is centered on whether temperatures during the recent half century were higher than those during the Medieval Climate Anomaly (MCA, AD 800-1300) and the Roman Warm Period (RWP, BC 200-AD 400), the most recent two natural warm periods of the late Holocene. Here the high resolution sea surface temperatures (SSTs) of two time windows around AD 990 (+/- 40) and AD 50 (+/- 40), which located in the MCA and RWP respectively, were reconstructed by the Sr/Ca ratio and delta O-18 of Tradacna gigas shells from the northern South China Sea. The results suggested that the mean SSTs around AD 990 (+/- 40) and AD 50 (+/- 40) were 28.1 A degrees C and 28.7 A degrees C, 0.8 A degrees C and 1.4 A degrees C higher than that during AD 1994-2005, respectively. These records, together with the tree ring, lake sediment and literature records from the eastern China and northwest China, imply that the temperatures in recent decades do not seem to exceed the natural changes in MCA, at least in eastern Asia from northwest China to northern SCS. |
| 语种 | 英语 |
| 源URL | [http://ir.ieecas.cn/handle/361006/9828]  |
| 专题 | 地球环境研究所_古环境研究室 |
| 通讯作者 | Sun, LG (Sun, Liguang)[ 1 ] |
| 作者单位 | 1.State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment, Chinese Academy of Sciences,Xi’an 710075, China; 2.Institute of Polar Environment, School of Earth and SpaceSciences, University of Science and Technology of China,Hefei 230026, China; 3.Guangzhou Institute of Geochemistry, Chinese Academy ofSciences, Guangzhou 510640, China 4.Advanced Management Research Center, Ningbo University,Ningbo 315211, China; |
| 推荐引用方式 GB/T 7714 | Shao, D ,Wei, GJ ,Wang, YH ,et al. Higher sea surface temperature in the northern South China Sea during the natural warm periods of late Holocene than recent decades[J]. CHINESE SCIENCE BULLETIN,2014,59(31):4115-4122. |
| APA | Shao, D ,Wei, GJ ,Wang, YH ,Sun, LG ,&Yan, H .(2014).Higher sea surface temperature in the northern South China Sea during the natural warm periods of late Holocene than recent decades.CHINESE SCIENCE BULLETIN,59(31),4115-4122. |
| MLA | Shao, D ,et al."Higher sea surface temperature in the northern South China Sea during the natural warm periods of late Holocene than recent decades".CHINESE SCIENCE BULLETIN 59.31(2014):4115-4122. |
入库方式： OAI收割
来源：地球环境研究所
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