ON DEVELOPMENT OF LARGE CITIES IN CHINA

ＯＮＤＥＶＥＬＯＰＭＥＮＴＯＦＬＡＲＧＥＣＩＴＩＥＳＩＮＣＨＩＮＡ￥ＣｕｉＧｏｎｇｈａｏ（崔功豪）（ＮａｎｊｉｎｇＵｎｉｖｅｒｓｉｔｙ，Ｎａｎｊｉｎｇ２１０００８，ＰＲＣ）Ａｂｓｔｒａｃｔ：ＴｈｅｌａｒｇｅｃｉｔｉｅｓｉｎＣｈｉｎａｈａｖｅｇｒｏｗｎ...     

PHYSIOLOGICAL INHIBITORY EFFECT OF OCS IN ARACHIDONIC ACID-RICH PARIETOCHLORIS INCISA (TREBOUXIOPHYCEAE, CHLOROPHYTA)

ＩＮＴＲＯＤＵＣＴＩＯＮＴｈｅｒｏｌｅｏｆａｌｇａｌｅｘｔｒａｃｅｌｌｕｌａｒｍｅｔａｂｏｌｉｔｅａｓａｂｉｏａｃｔｉｖｅｓｕｂｓｔａｎｃｅｔｏｃｏｎｔｒｏｌｓｕｃｃｅｓｓｉｏｎｏｆｍｉ ｃｒｏａｌｇａｌｐｏｐｕｌａｔｉｏｎｓｈａｄｌｏｎｇｂｅｅｎｒｅｃｏｇｎｉｚｅｄ (ＭａｓｔａｎｄＰａｃｅ,1 93 8;ＰｒａｔｔａｎｄＦｏｎｇ,1 940 ) .Ｓｏｍｅｍｉｃｒｏａｌｇａｅ,ｌｉｋｅＣｈｌｏｒｅｌｌａｖｕｌｇａｒｉｓ,Ｃｈｌａｍｙｄｏｍｏｎａｓｒｅｉｎｈａｒｄｔｉｉ,Ｓｋｅｌｅｔｏｎｅｍａｃｏｓｔａｔｕｍ ,ｅｘｃ…     

BASIC FEATURES OF FOREST STEPPE IN THE LOESS PLATEAU OF CHINA

ＢＡＳＩＣＦＥＡＴＵＲＥＳＯＦＦＯＲＥＳＴＳＴＥＰＰＥＩＮＴＨＥＬＯＥＳＳＰＬＡＴＥＡＵＯＦＣＨＩＮＡ￥ＺｈｕＺｈｉｃｈｅｎｇ（朱志诚）（ＤｅｐａｒｔｍｅｎｔｏｆＢｉｏｌｏｇｙ．ＮｏｒｔｈｗｅｓｔＵｎｉｖｅｒｓｉｔｙ，Ｘｉａｎ７１００６９，ＰＲＣ）Ａ...     

ABUNDANCE AND PRODUCTION OF LIMNODRILUS HOFFMEISTERI (OLIGOCHAETA: TUBIFICIDAE) IN ALGAE-DOMINATED LAKE HOUHU (WUHAN, CHINA)

ＩＮＴＲＯＤＵＣＴＩＯＮＬｉｍｎｏｄｒｉｌｕｓｈｏｆｆｍｅｉｓｔｅｒｉ,ａｕｂｉｑｕｉｔｏｕｓｔｕｂｉｆｉｃｉｄ ,ｉｓａｐｒｅｄｏｍｉｎａｎｔｂｅｎｔｈｉｃｉｎｖｅｒｔｅｂｒａｔｅｉｎｍｏｓｔｓｈａｌｌｏｗｅｕｔｒｏｐｈｉｃｌａｋｅｓｉｎＣｈｉｎａ (Ｌｉａｎｇ,1 979) .Ｓｏｆａｒ,ｔｈｅｒｅａｒｅｎｏｄａｔａｏｎｔｈｅｓｅｃｏｎｄａｒｙｐｒｏｄｕｃ ｔｉｏｎｏｆｔｈｉｓｗｏｒｍａｎｄｆｅｗｄａｔａｏｎｔｈａｔｏｆｏｔｈｅｒｚｏｏｂｅｎｔｈｏｓｒｅｐｏｒｔｅｄｉｎＣｈｉｎａ .Ｗｉｔｈｔｈｅｆｉｓｈｅｒ…     

DISTRIBUTION AND POPULATION DYNAMICS OF PARACALANUS PARVUS, PARACALANUS CRASSIROSTRIS, AND ACARTIA BIFILOSA (COPEPODA, CALANOIDA) IN THE BOHAI SEA

ＩＮＴＲＯＤＵＣＴＩＯＮＴｈｅＢｏｈａｉＳｅａｗａｓｃｈｏｓｅｎａｓｔｈｅｓｉｔｅｏｆｔｈｅｆｉｒｓｔｐｈａｓｅｏｆｔｈｅＣｈｉｎａ ＧＬＯＢＥＣ (ＧｌｏｂａｌＯｃｅａｎＥｃｏｓｙｓｔｅｍＤｙｎａｍｉｃｓ)ｐｒｏｇｒａｍｆｒｏｍ 1 997ｔｏ2 0 0 0 ,ｉｎｗｈｉｃｈｔｈｅｄｙｎａｍｉｃｓｏｆｚｏｏｐｌａｎｋｔｏｎｐｏｐｕｌａｔｉｏｎｓｗａｓｏｎｅｏｆｔｈｅｆｏｕｒｐｒｉｎｃｉｐａｌｆｏｃｉ.Ｓｍａｌｌｃｏｐｅｐｏｄｓｃｏｍｐｒｉｓｅａｎｉｍｐｏｒｔａｎｔｃｏｍｐｏｎｅｎｔｏｆｚｏｏｐｌａｎｋｔｏｎｅｓｐ…     

THE CLIMATIC CONDITIONS OF POLAR-TYPE GLACIERS DEVELOPMENT IN CHINA

ＴＨＥＣＬＩＭＡＴＩＣＣＯＮＤＩＴＩＯＮＳＯＦＰＯＬＡＲ－ＴＹＰＥＧＬＡＣＩＥＲＳＤＥＶＥＬＯＰＭＥＮＴＩＮＣＨＩＮＡ￥ＨｕａｎｇＭａｏｈｕａｎ（黄茂桓）（ＬａｎｚｈｏｕＩｎｓｔｉｔｕｔｅｏｆＧｌａｃｉｏｌｏｇｙａｎｄＧｅｏｃｒｙｏｌｏｇｙ，ｔｈｅＣ...     

LANDSCAPE PATTERN CHANGES IN WEST SUBURBS OF SHENYANG

肖笃宁，赵羿，郭林海ＬＡＮＤＳＣＡＰＥＰＡＴＴＥＲＮＣＨＡＮＧＥＳＩＮＷＥＳＴＳＵＢＵＲＢＳＯＦＳＨＥＮＹＡＮＧ￥ＸｉａｏＤｕｎｉｎｇ；ＺｈａｏＹｉ；ＧｕｏＬｉｎｈａｉ（ＩｎｓｔｉｔｕｔｅｏｆＡｐｐｌｉｅｄＥｃｏｌｏｇｙ，ｔｈｅＣｈｉｎｅｓｅＡｃａｄ...     

THE DEVELOPMENT AND PROTECTION OF WETLANDS IN THE FOUR LAKE AREA OF JIANGHAN PLAIN

ＴＨＥＤＥＶＥＬＯＰＭＥＮＴＡＮＤＰＲＯＴＥＣＴＩＯＮＯＦＷＥＴＬＡＮＤＳＩＮＴＨＥＦＯＵＲＬＡＫＥＡＲＥＡＯＦＪＩＡＮＧＨＡＮＰＬＡＩＮＣａｉＳｈｕｍｉｎｇ（蔡述明）（ＩｎｓｔｉｔｕｔｅｏｆＧｅｏｄｅｓｙａｎｄＧｅｏｐｈｙｓｉｃｓ，ｔｈｅＣｈｉｎｅ...     

PHYLOGENETIC RELATIONSHIPS AMONG PUFFERFISH OF GENUS TAKIFUGU BY RAPD ANALYSIS

ＩＮＴＲＯＤＵＣＴＩＯＮＰｕｆｆｅｒｆｉｓｈｅｓｏｆｔｈｅｇｅｎｕｓＴａｋｉｆｕｇｕ (Ｔｅｔｒａｏｄｏｎｔｉｆｏｒｍｅｓ,Ｔｅｔｒａｏｄｏｎｔｉｄａｅ)ａｒｅｍａｉｎｌｙｄｉｓｔｒｉｂｕｔｅｄａｌｏｎｇｔｈｅｃｏａｓｔａｌｒｅｇｉｏｎｓｏｆＣｈｉｎａ ,ＪａｐａｎａｎｄＫｏｒｅａａｎｄａｒｅｃｏｍｍｅｒｃｉａｌｌｙｉｍｐｏｒｔａｎｔｔｏｔｈｅｓｅｃｏｕｎ ｔｒｉｅｓ .Ｏｖｅｒ 2 0ｓｐｅｃｉｅｓｈａｖｅｂｅｅｎｒｅｃｏｒｄｅｄｉｎｔｈｅＹｅｌｌｏｗＳｅａａｎｄｔｈｅＥａｓｔＣｈｉｎａＳｅａ (Ｃｈｅｎｇ…     

THE CHARACTERISTIC， DISTRIBUTION AND CAUSING FACTORC OF THE DISABLED IN HENAN PROVINCE

ＴＨＥＣＨＡＲＡＣＴＥＲＩＳＴＩＣ，ＤＩＳＴＲＩＢＵＴＩＯＮＡＮＤＣＡＵＳＩＮＧＦＡＣＴＯＲＣＯＦＴＨＥＤＩＳＡＢＬＥＤＩＮＨＥＮＡＮＰＲＯＶＩＮＣＥ￥ＬｉｎＦｕｒｕｉ（林富瑞）（ＨｅｎａｎＡｃａｄｅｍｙｏｆＳｃｉｅｎｃｓ，Ｚｈｅｎｇｚｈｏｕ４５００...     

Genesis of underground brine along south coast of Laizhou Bay： hydrochemical characteristics

1 INTRODUCTION Two large-scale concentration mechanisms, evaporation and freezing, have been proposed for marine origin brine production (Bein and Arad, 1992; Bottomley et al., 1999). There are three basic requirements for brine formation by seawater evap…     

The hydrochemical features of salt lakes in Qaidam Basin

There are 37 lakes in the Qaidam Basin: 1 freshwater lake, 6 brackish-water lakes, 2 saline-water lakes and 28 salt lakes. The pH value of salt lake brines is 7.014 on the average, and the average total mineralization is 340.75 g/1. Their water bodies belong mainly to the five-component equilibrium system,: Na, K, Mg//SO₄, Cl-H₂O, which can be further grouped into sodium-magnesium sulfate subtype, magnesium sulfate subtype, chloride transition subtype and chloride type water by their hydrochemical property. The salt lake brines of the first salt forming epoch (N₂−Q₃) were of the sulfate type. In the second salt forming epoch (Q₃−Q₄), some of them were of the chloride type. The pH value of brines decreases with the increase of total mineralization. The pH value is lower when the total mineralization is from 50–310 g/l and higher when the total mineralization is from 310–355 g/l, however, when the total mineralization is higher than 355 g/l, the pH value decreases slowly again. The total mineralization of the chloride type and the chloride transition subtype brine is higher than the sulfate type, being 310–530 g/l, 310–470 g/l, and less than 355 g/l in that order. Of the 40 chemical compositions in the saline lake brines in Qaidam Basin, potassium is mainly concentrated in the chloride type and chloride transition subtype brine, boron and lithium mainly in the sulfate type. Evaporation experiments show that boron and lithium are accumulated in concentrated brine until crystallization of bischofite takes place. Potassium is also accumulated in concentrated brine during the salt forming stage, but its concentration decreases with the increase of total mineralization during the potassium forming stage. This paper was published in Chinese inOcean. et Limn. Sinica;15 (4):341–359, 1984.     

Variation of d δ18O/dT in precipitation in the Qinghai-Xizang Plateau

The relations between δ¹⁸O and temperature on the different time scales were analysed, according to the data from Tuotuohe (34°13′N, 96°25′E; 4533 m a. s. l.), Delingha (37°22′N, 97°22′E; 2981 m a. s. l.) and Xining (36°37′N, 101°46′E; 2261 m a. s. l.) in the Qinghai-Xizang Plateau. The results show that the significance of d δ¹⁸O/dT on different time scales are different. The d δ¹⁸O/dT on the synoptic scale reflects the interdependent relation between δ¹⁸O and temperature in the short-term synoptic scale process; the d δ¹⁸O/d T on the seasonal scale reflects the relation between them whithin a year; and the d δ¹⁸O/d T on the climatic scale reflects the relation between them in the long-term climatic change. The calculated d δ¹⁸O/dT on climatic scale is very close to the theoretical values on the condition of advection transport for Tuotuohe Station. However, there are great differences between the calculated and the theoretical values for Delingha and Xining stations.     

“Tear drop pattern” potash deposits in lacustrine facies

It is well known that there are two patterns of potash deposition in lacustrine facies: “tear drop pattern” (the Dabsan saline lake is a typical example) and “bull's eye pattern”. Potash-forming in tear drop pattern is still continuing. The 2,678 m A. S. L. lake in the middle of the Qarhan playa in the Qaidam Basin covers an area of 210 km², and has an average depth of 0.39 m. Its MgCl₂ type surface brine is 280–340 g/l in salinity and mainly consists of Na, K, Mg and Cl. As a rule, the potash deposits occur as evaporite distributed in tear drop pattern at the northern and northeastern lakeshore zones. They mostly consist of carnallite and halite, occasionally sylvite. The deposition is very unstable and controlled principally by the varying supply of deposit materials from the Golmud River in the south. The potash deposits were formed when concentration of the surface brine reached a certain degree in the main evaporating season. Their forming process followed some crystalization paths in the phase diagram for the Na, K, Mg/Cl H₂O equilibrium system. Such a sedimentary model of potash deposits in the lacustrine facies is relatively common in nature. Under the extremely arid climate, differential concentration of the nonhomogeneous potassium-rich surface brine produced the potash deposits. Qarhan Salt Lake also had the same pattern of potash depositions and so, in a sense, the Dabsan saline lake is the continuation of the Qarhan salt lake in terms of potash formation. Schmalz (1970) put forward two distributive patterns for evaporite: “tear drop pattern” and “bull's eye pattern”. These patterns exist in both marine and continental salt-bearing basins (including recent salt lakes), and are controlled by the conditions of physical geography, hydrogeology, sedimentology and climatology of each basin. In his works (Sun, 1981; 1984; 1986; 1988) on the origins of potash deposits, the author always referred to them as two models of potash formation. The “tear drop pattern” is one of the salt-forming models and also an important potash-forming model. This paper deals with the formative mechanism of the tear drop pattern potash deposition by presenting the Dabsan saline lake as an example and elucidates on the distributive characteristics and formative processes of potash deposits in the lake.     

MODERN CLIMATIC SIGNALS DEDUCED FROM STABLE ISOTOPE IN SHELLS IN XINGCUO LAKE SEDIMENTS,EAST TIBETAN PLATEAU,CHINA

Ｉｔｉｓｏｎｅｏｆｔｈｅｆｒｏｎｔｉｅｒｆｏｃｕｓｅｓｉｎｔｈｅｆｉｅｌｄｏｆｇｌｏｂｌｅｅｎｖｉｒｏｎｍｅｎｔａｌｃｈａｎｇｅｓｔｏｅｘｔｒａｃｔｑｕａｎｔｉｔａｔｉｖｅｌｙｐａｓｔｃｌｉｍａｔｉｃｓｉｇｎａｌｓｆｒｏｍｌａｋｅｓｅｄｉｍｅｎｔｒｅｃｏｒｄｓ．Ｉｎｔｈｅｒｅ-ｃｅｎｔｄｅｃａｄｃｉｏｕｓｙｅａｒｓａｓｅｒｉｅｓｏｆａｃｈｉｅｖｅｍｅｎｔｓｏｎｒｅ-ｂｕｉｌｄｉｎｇｔｈｅｓｅｑｕｅｎｃｅｓｏｆｃｌｉｍａｔｉｃａｎｄｅｎｖｉｒｏｎｍｅｎｔａｌｅｖｏｌｕｔｉｏｎｓａｔｖａｒｉｏｕｓｓ…     

Application of transition metal isotope tracers in global change research

High-precision isotope composition determinations using multicollector, magnetic-sector inductively coupled plasma mass spectrometry (MC-ICPMS) have recently revealed that some transition metal isotopes such as those of Mo, Fe, Cu, Zn etc. can be used as biogeochemical tracers in global change research.The Mo isotope system may be useful in paleoredox investigations indicating that δ^97 ^95Mo in seawater may co-vary with changes in the relative proportions of anoxic and oxic sedimentation in the ocean, and that this variation may be recorded in δ^97 ^95Mo of anoxic sediments. The Mo continental flux into the oceans and the global Mo isotope budget can be estimated from δ^97 ^95M0 values. The Fe isotope composition in seawater is an important issue because Fe plays a controlling role in biological productivity in the oceans and its abundance in seawater may have substantial effect on climate changes. Iron isotope fractionations could result from bio- and abio-processes and have about 0.1% variation ( δ^56 ^54Fe), so Fe isotopes considered alone cannot be used to distinguish the products of abiotic and biotic Fe processing in geological records. Cu and Zn isotopes are also used as biogeochemical tracers, but the researches are relatively less. This review mainly focuses on the methods for preparation, purification and determination of new isotope tracer samples, and on isotope applications in marine environmental changes.     

Stable isotopes in aquatic food web of an artificial lagoon in the Hangzhou Bay, China

Stable isotope values, δ¹³C and δ¹⁵N, were determined for four primary producers and 19 dominant consumers in a small artificial lagoon located in Hangzhou Bay. Based on these results the major pathways for energy flow and trophic structure of the artificial lagoon ecosystem were characterized. The mean δ¹³C values for the 19 consumers ranged from −22.99‰ to −14.24‰. Apart from so-iny mullet Liza haematocheila, the other 18 consumers had intermediate δ¹³C values between those of epibenthic microalgae and particulate organic matter (POM). The results of a multiple source linear mixing model (IsoSource model) indicated that 50% or more of the organic carbon in the tissues of most consumers was derived from epibenthic microalgae. This indicated that these primary producers were the main food source fueling the lagoon food web. The mean δ¹⁵N values for the 19 consumers varied between 4.93‰ and 12.97‰ and indicated four trophic levels in the lagoon. Four macroinvertebrates and zooplankton represented the primary consumers, whilst the other 14 consumers occupied the secondary and tertiary consumer levels. The 19 consumers were divided into three trophic guilds (detritivores/suspension feeders, omnivores and carnivores).     

ORIGIN OF CARBONATE MATERIALS IN THE NORTHERN BASIN OF LAKE BAIKAL AND ITS RELATIONSHIP TO HOLOCENE PALEOCLIMATE

Fine-grained disseminated carbonate was found in Holocene sediments in a core taken from the northern basin of Lake Baikal. The core had two distinct facies. a terrigenous blue-clay overlain by a diatomaceous silt. Oxygen and carbon stable isotope analyses, combined with SEM , X-ray diffraction and .palynology, show that the carbonate in the blue-clay layer is pedogenic in origin, rather than biogenic or authigenic . The S C values in the blue clay suggest that the carbonate is derived from a single source , while the carbonate in the diatom-rich layer might be transported by winds from different sources. On the assumption that the carbonate was formed during the post-glacial age and was transported primarily by river runoff, the 18O isotopic values suggest that the annual temperature in the northern Baikal drainage area was about 3℃ warmer during the middle Holocene (8500-7000 a, B. P.) than during the early Holocene (11 000-8 500a, B.P.) when the blue clay was being deposited . This interpretation is     

高氯酸盐稳定氯、氧同位素测试新技术

高氯酸盐同位素测试技术能够为环境介质中高氯酸盐污染物来源的判识、降解途径与修复效果的监测与评价提供重要的分析工具。在国内建立高氯酸盐稳定氯、氧同位素测试技术,采用真空热解方法组建同位素真空制样系统,并结合GasBenIIIRMS联用技术实现在线高精度测试。实验结果表明,真空制样系统稳定性高,最佳热解反应温度为650℃,样品量约10μmol ClO-₄。δ18O、Δ17O和δ37Cl的方法分析精度分别为0.3‰,0.04‰和0.1‰,达到国际水平,为我国高氯酸盐环境污染的防治研究提供了先进的方法与手段。      

Spatial variation of stable isotopes in different waters during melt season in the Laohugou Glacial Catchment,Shule River basin

To evaluate isotopic tracers at natural abundances by providing basic isotope data of the hydrological investigations and assessing the impacts of different factors on the water cycle, a total of 197 water samples were collected from the Laohugou Glacial catchment in the Shule River basin northwestern China during the 2013 ablation seasons and analyzed their H- and O-isotope composition. The results showed that the isotopic composition of precipitation in the Qilianshan Station in the Laohugou Glacial catchment was remarkable variability. Correspondingly, a higher slope of δ~(18)O-δD diagram, with an average of 8.74, is obtained based on the precipitation samples collected on the Glacier No.12, mainly attributed to the lower temperature on the glacier surface. Because of percolation and elution, the isotopic composition at the bottom of the firn is nearly steady. The δ~(18)O /altitude gradients for precipitation and melt water were -0.37‰/100 m and -0.34‰/100 m, respectively. Exposed to the air and influenced by strong ablation and evaporation, the isotopic values and the δ~(18)O vs δD diagram of the glacial surface ice show no altitudinal effect, indicating that glacier ice has the similar origins with the firn. The variation of isotopic composition in the melt water, varying from -10.7‰ to -16.9‰(δ~(18)O) and from -61.1‰ to -122.1‰(δD) indicates the recharging of snowmelt and glacial ice melt water produced at different altitudes. With a mean value of -13.3‰ for δ~(18)O and -89.7‰ for δD, the isotopic composition of the stream water is much closer to the melt water, indicating that stream water is mainly recharged by the ablation water. Our results of the stable isotopic compositions in natural water in the Laohugou Glacial catchment indicate the fractionations and the smoothing fluctuations of the stable isotopes during evaporation, infiltration and mixture.