姚桥井田构造基本特征研究——兼谈昭阳湖成因

以湖坝为界,将姚桥井田划分为陆上区和湖下区:陆上区煤层断裂构造发育,并具有一定的分区性;而湖下区构造简单。煤系沉积特征由陆上区至湖下区呈现明显的差异性,湖坝附近为过渡区。沿湖坝及陆、湖交界处不发育控制性的地质构造。综合各种地质特征可以得出结论:昭阳湖不是断陷湖。     

A study on environmental changes based upon cladoceran assemblages from the core sediments in Chen Co,southern Tibet

A consecutive sediment core (CC2) was drilled in Chen Co (lake) of southern Tibet using a PISTON sampler in 1998 AD. Cladoceran remains including their species,amount richness and ecological features are analyzed for the top 117 cm sections of the core, upon which 5 cladoceran assemblages are distinguished. CL0 is an assemblage without any cladocera in the depth between 117-105 cm. CL1 assemblage (depths between I01-77 cm, ca.1407-1533 AD) possesses total 9 cladoceran species that appear in the core,and performs the greatest richness in the whole sequence.This assemblage reflected that there was plenty of exotic cold water and organic debrises inputing to the sedimentary site under the warmer conditions. The lake was wide and shallow that satisfied the big hydrophyte living. Cladoceran species and richnesses of CL2 assemblage (depths between 77-29cm, ca. 1533-1831AD) perform much more decreasing than those of CLI. There was only less Chydorus sphaericus which was acclimatized to wide environmental ranges. This implied that the sedimentary environment is so execrable that most of cladoceran lost their living abilities. Compared with CL1 assemblage, CL3 assemblage (depths between 29-10 cm, ca.1831--1941 AD) possesses nearly the same dominant species but lower richnesses. Especially, the cladoceran preferring organic debris also decrease in their amounts. This meant that the surface vegetation in the drainage basin was still poor though the environment turned to be better. Except the 2 zooplankton species, the other 7 species of cladoceran in this core are found in CL4 assemblage (depths between 10-0cm, ca. 1941-1998 AD), in which the eurythermal species had not performed their competition ability comparing withnarrow-temperatures adapted species. It implied that water temperatures were stable and much more influenced by air temperatures under the shallow-water conditions. The environmental features reflected by cladocera assemblages of CC2 core are fully supported by the evidences from ostracoda assemblages, diatom-salinity transfunction, environmental magnetism and relative proxies of the parallel CC1 core. Cladoceran assemblages in the lake sediments of Tibetan Plateau are sensitive to sedimentary environment and very significant to the studies of environmental changes.     

A subfossil chironomid-total phosphorus inference model for lakes in the middle and lower reaches of the Yangtze River

Quantitative environmental reconstruction using subfossil chironomid has attracted much attention in recent years[1]. Consisting of about 400 genera, chi- ronomids (Diptera: Chironomidae) are found in nearly all freshwater bodies[2]. They are holometabolo…     

国内外从盐湖卤水中提锂工艺技术研究进展

金属锂及其化合物在能源和新材料方面具有重大应用前景,盐湖卤水提锂将成为21世纪锂盐生产的主攻方向。本文综合分析了国内外盐湖卤水提锂的工艺技术,提出了盐湖卤水提锂的发展趋势。     

泥河湾古湖湖心区石片的发现

Nihewan basin is famous for its lacustrine deposits, animal fauna and occupied evidence of early humans. All of the discovered Palaeolithic sites are distributed along ancient lakeside or on the terraces of the Sangganhe river and its tributaries. However, the authors discovered a stone flake from the central part of the ancient Nihewan lake in an outcrop section on the right bank of the Sangganhe river. The location is 40°06′33″N and 114°20′15″E, near Jinerwa village, Yangyuan County, Heibei Province. The flake is basaltic and has a size of 4.5 cm×3.2 cm×1.7 cm. Its ventral surface is a fresh plane of fracture with a clear point of percussion,a bulb and a bulbar scar on it. The dorsal surface is composed of a residual part of a rounded pebble surface and a fresh plane formed along a joint. The flake is unearthed at 50.73 m under the lacustrine platform surface in perfectly laminated beds of Mid-Pleistocene. The feafures of the flake do not rule out the possibility of natural origin. But combined with the sedimentary features of the horizon where it is unearthed, the most reasonable explanation is that the flake may be the trace of ancient human activities on the frozen lake of Nihewan.     

洞庭湖区湿地生物资源评价及开发利用

洞庭湖湿地是我国最大的淡水湖泊湿地之一,生物资源十分丰富,其中植物1428种,鸟类216种,鱼类119种,哺乳类22种,两禁爬行类27种,本分析了洞庭湖湿地生物资源的特征,并进行了定性评价,指出了洞庭湖湿地生物资源利用状及存在的主要问题,并就今后本区湿地生物资源的保护和利用提出了一些构想。     

临汾盆地中更新世中晚期以来的演化历史及成因分析

第四纪中晚期以来临汾盆地中发育了五级冲湖积台地或阶地。地貌沉积阶段性发育的特点反映出临汾古湖在这一时期曾经历过多次收缩的变化。根据上覆冲湖积台地或阶地的最老黄土古土壤序列,我们发现在S8的早期（年龄0.75MaBP),S5的早期（年龄0.50MaBP)和S1的早期（年龄0.13MaBP),盆地中发生了三次大幅度的湖退;在L1SS开始发育时（年龄52kaBP),汾河发生了一次强烈下切,形成了T2阶地。从影响湖盆变化的因素分析,构造抬升是导致三次大幅度湖退的根本原因;气候变化是T2阶地的致因。     

Abrupt Holocene changes of the Asian monsoon at millennial- and centennial-scales: Evidence from lake sediment document in Minqin Basin, NW China

Considerable research is now focusing on abrupt Holocene changes at millennial- and centennial-scales all over the world. This study shows that the changes in the Holocene summer monsoon can be divided into two main periods, based on climatic proxy records of lake sediments from the Sanjiaocheng section located at the NW boundary of the summer monsoon, Gansu Province. The early and middle Holocene was humid with stronger summer monsoon, while the late Holocene is dry with weak summer monsoon. Detailed results also show a series of millennial- and centennial-scale changes in the intensity of the summer monsoon, with a periodicity of {dy1600} years during the whole Holocene, and with a periodicity of 800 years during the early Holocene. Ten dry events during the Holocene are associated with the weakening of the summer monsoon. These rapid climatic changes may be representative of a global climatic change pattern during the Holocene.     

探访巴丹吉林沙漠

位于内蒙古自治区西部阿拉善右旗境内的巴丹吉林沙漠,面积4.7万平方公里,是我国境内仅次于新疆塔克拉玛干沙漠与古尔班通古特沙漠的第三大沙漠。自从《中国国家地理》杂志在“选美中国”中将巴丹吉林沙漠评选为中国最美的沙漠之后,我就一直盼望能有机会去那儿看看,去领略它那迷     

Landscape evolution and precipitation changes in the Badain Jaran Desert during the last 30 000 years

On the basis of field expeditions into different parts of the Badain Jaran Desert, new evidence of landscape evolution and precipitation changes during the last 30 000 years has been found from the geomorphological, sedimentological and geochronological studies of the megadune. Different cemented surfaces of palaeo-dunes have been observed in many localities, which are representatives of relatively moister environment. The chronological data show that four periods of more humid environment occurred in the past 30 000 years. The stabilization of dunes in a large scale and the existence of many palaeo-lakes and lacustrine terraces confirm the periodic fluctuations of climate. It implies that the intensity of westerlies and Eastasian monsoons varied in the region of Alashan, and the periods of higher precipitation took place even in the times close to the last glacial maximum.