Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

A carbon- and oxygen-isotope record of recent environ- mental change from Qinghai Lake, NE Tibetan Plateau

An understanding of natural climatic variability is essential for evaluating anthropogenic impacts on recent and future climate[1—3]. Due to the lack of lengthy instrumental records, such an understanding must be gained from natural archives of climate change. Palaeolimnological indicators of past lake levels may provide a sensitive record of changes in effective precipitation in closed basins. This approach is particularly relevant on the Tibetan Plateau, where instrumental records are very…     

南澳岛及其附近岛屿夏季鸟类的初步调查

作者一行于 2 0 0 1年夏季对南澳及其附近岛屿的鸟类资源状况进行了调查研究 .结果发现 ,南澳及其附近岛屿有鸟类 51种 ,隶属 1 3目 2 8科 ,其中雀形目 2 3种 ,占所发现种类的 45% ,非雀形目 2 8种 ,占 55% ;国家一、二级保护动物各一种 ,分别为 :白腹军舰鸟 (F regataandrewsi)和岩鹭 (Egretta sacra) .按鸟类的栖息和迁徙习惯划分 ,有海鸟 8种 ,湿地候鸟 2种 ,湿地留鸟 9种 ,陆地候鸟 4种 ,陆地留鸟 2 8种 .在所有鸟类中以褐翅燕鸥 (Sterna anae-thetus)为优势种 ,数量最大 ,分布最广 .     

生物医学研究热点及意义

生物医学研究是目前发展最快、令人振奋的科技领域。本文概述了生物医学的发展趋势，并对生物医学前沿领域的研究热点，如基因组、蛋白质组、细胞信号转导机制、干细胞研究、神经科学研究、生物信息学等进行了分析。对生物技术领域的研究热点，如生物芯片技术、高效基因转移系统技术、组织工程技术和干细胞定向分化技术、基因敲除和敲入技术、克隆技术等进行了综述。提出研究中应该注意针对研究热点选题，注意多学科交叉和集团作战，同时注意知识产权保护。     

五台山滹沱群SHRIMP锆石U-Pb年龄: 华北克拉通早元古代拼合新证据

采自五台山台怀镇南8 km处滹沱群变质火山-沉积岩层中的长英质凝灰岩样品含有两组锆石, 所记录的SHRIMP锆石方法²⁰⁷Pb/²⁰⁶Pb年龄分别为2180±5 Ma和2087±9 Ma. 在误差范围内, 较老的一组年龄与五台山大洼梁花岗岩年龄相当, 表明它们来自相似的地壳岩浆源; 而较年轻的一组锆石年龄与相邻地区阜平杂岩湾子表壳岩中变沉积岩和变火山岩及南营花岗片麻岩年龄相当, 因而被解释为滹沱群火山作用年龄. 这两组年龄的存在表明: (1) 滹沱群形成于早元古代而非太古宙; (2) 早元古代火山-沉积作用在五台和阜平地区同时间发生. 这样, 早元古代沉积作用在该区是广泛的, 它们代表了华北克拉通东部陆块西侧大陆边缘相沉积. 滹沱群火山作用年龄的确定也表明该群所经历的变质-变形事件发生在2087±9 Ma 之后, 这进一步佐证我们最近根据其他方面研究结果所得出的吕梁造山事件(约1.8 Ga)是该区主要构造事件的结论: 该事件导致华北克拉通东部陆块和西部陆块的最终拼合, 并成为全球早-中元古代超级大陆组成部分之一.     

一类带有奇异项的临界椭圆方程正解的存在性

研究了一类带有负指数项和Sobolev-Hardy临界项的半线性椭圆方程，运用变分法证明了正解的存在性。     

Effect of hydrogen peroxide on the binding of Merocyanine 540 to human erythrocytes

The fluorescent dye Merocyanine 540 (MC540) is often used as a probe to monitor the molecular packing of phospholipids in the outer leaflet of biomembranes. In a previous study we showed that the increased staining of erythrocytes with a perturbed membrane structure was mainly due to an increase in the fluorescence yield of cell-bound MC540, rather than to an increase of the number of bound molecules. Erythrocytes and ghosts exposed to continuous fluxes of H₂O₂ exhibited pronounced lipid peroxidation. Further, red blood cells subjected to this form of oxidative stress also showed increased staining with MC540. It appeared that this was caused by a strong increase in binding of MC540, together with a slight red shift of the fluorescence emission maximum and a small increase in the fluorescence yield of bound MC540. The changed MC540 binding characteristics were not observed when lipid peroxidation was suppressed by the presence of the antioxidant BHT in the incubation medium. However, open ghosts exposed to H₂O₂ showed no increase of MC540 binding, excluding a direct involvement of lipid peroxidation. Measurement of fluorescence emission spectra and gel filtration studies showed that MC540 can bind to H₂O₂-exposed hemoglobin. Experiments with erythrocytes lysed in hypotonic medium after exposure to H₂O₂ revealed that peroxidation of lipids with H₂O₂ induced a non-specific permeabilization of the plasma membrane to MC540, thereby allowing MC540 to bind to the oxidatively denatured, more hydrophobic hemoglobin. These results indicate that conclusions about packing of phospholipids in the outer leaflet of the membrane based on increased MC540-staining should be drawn with care. Received 27 September 1996; received after revision 5 November 1996; accepted 27 November 1996