Distribution and evolution of Carboniferous reefs in South China

Reefs are sensitive proxies for palaeontological, palaeoenvironmental, and palaeogeographical changes during geological history. In South China, after the collapse of the reef ecosystem during the Frasnian-Famennian and Hangenberg mass extinction events, Carboniferous reefs underwent evolutionary episodes of recovery, decline, and turnover, which were controlled by changes of reef-builders abundance, sedimentary facies, relative sea level, and even global climate. In Tournaisian times, only a few Waulsortian-like banks have been found in Liuzhou, Guangxi without metazoan reefs, which were caused by the lack of reef-builders, such as colonial rugose corals and bryozoans, and the dominant non-carbonate facies (shale, mud stone and sandstone) driven by low relative sea level. The absence of mud mounds in the early Viséan was attributed to the regression event during the Tournaisian-Viséan boundary. During Viséan times, bryozoan-coral reefs in Huishui, Guizhou and Tianlin, Guangxi occurred during a time of increasing biodiversity and carbonate facies resulting from relative sea-level rise. The number of potential reef-builders as colonial rugose coral and bryozoan genera significantly increased in Viséan times in South China. The reef abundance declined during Serpukhovian times in South China and the controlling factors were decreasing abundance of potential reef-builders and developing non-carbonate facies due to a relative sea-level fall. The sedimentary facies were characterized by shale, mud stone, sandstone, and dolostone during this time. A distinct change in reef types occurred after the Mississippian-Pennsylvanian boundary, when phylloid algae and red algae reefs (distributed in Ziyun, Guizhou and Beibuwan, Guangxi) replaced metazoan reefs and became the dominant role in reef ecosystem. This reef turnover event may be triggered by the dramatic relative sea-level fall during the mid-Carboniferous, and continued low relative sea level in South China and global flourish of phylloid and red algae during Pennsylvanian times. Grainstone and dolomitic limestone were the main composition of the platform sedimentary facies in South China during Pennsylvanian times. In addition, global climate cooling and warming, resulted from the waxing and waning of Gondwana glaciation, may also influence the reef evolution in South China, as evidenced from the consistent transgression and regression events and reef evolutionary pattern between South China and globe during the Carboniferous.     

Bam HI DNA甲基化酶酶学性质的研究

以Lineweave-Burk plot双倒数作图法测得该酶对底物S-腺苷酰甲硫氨酸(SAM)的K_m=7.69×10~(-6)mol/L,在1mmol/LS-腺苷酰高半胱氨酸(SAH)存在下,Ki=7.33×10~(-4)mol/L,两条直线相交于纵轴,证明SAH是该酶的竞争性抑制剂。该酶最适pH为7.8,对热不稳定。同时还测定了该酶对不同DNA底物的专一性及盐浓度、代谢相关物’两价阳离子、某些酸根等对该酶调节性质的影响。以碘代乙酰胺修饰该酶的SH基’及用二硫苏糖醇(DTT)和巯基乙醇(MSH)保护该酶SH基所作的实验表明SH基是该酶活性中心所必需的,用高效液相色谱(HPLC)法证明该酶所甲基化的碱基为刘氏小球菌(M·L、DNA)分子中的胞嘧啶,且求得甲基化30min后所得甲基化水平为2.39％。同时也证明当用该酶将λDNA甲基化后,可使BamHI限制性核酸内切酶对甲基化后的λDNA丧失切割作用。     

ESTs library from embryonic stages reveals tubulin and reflectin diversity in Sepia officinalis (Mollusca — Cephalopoda)

New molecular resources regarding the so-called “non-standard models” in biology extend the present knowledge and are essential for molecular evolution and diversity studies (especially during the development) and evolutionary inferences about these zoological groups, or more practically for their fruitful management. Sepia officinalis, an economically important cephalopod species, is emerging as a new lophotrochozoan developmental model. We developed a large set of expressed sequence tags (ESTs) from embryonic stages of S. officinalis, yielding 19,780 non-redundant sequences (NRS). Around 75% of these sequences have no homologs in existing available databases. This set is the first developmental ESTs library in cephalopods. By exploring these NRS for tubulin, a generic protein family, and reflectin, a cephalopod specific protein family,we point out for both families a striking molecular diversity in S. officinalis.     

Neutral Amino Acid Transport in Astrocytes: Characterization of Na+-Dependent and Na+-Independent Components of α-Aminoisobutyric Acid Uptake

Neutral amino acid transport is largely unexplored in astrocytes, although a role for these cells in blood-brain barrier function is suggested by their close apposition to cerebrovascular endothelium. This study examined the uptake into mouse astrocyte cultures of alpha-aminoisobutyric acid (AIB), a synthetic model substrate for Na+-dependent system A transport. Na+-dependent uptake of AIB was characteristic of system A in its pH sensitivity, kinetic properties, regulatory control, and pattern of analog inhibition. The rate of system A transport declined markedly with increasing age of the astrocyte cultures. There was an unexpectedly active Na+-independent component of AIB uptake that declined less markedly than system A transport as culture age increased. Although the saturability of the Na+-independent component and its pattern of analog inhibition were consistent with system L transport, the following properties deviated: (1) virtually complete inhibition of Na+-independent AIB uptake by characteristic L system substrates, suggesting unusually high affinity of the transporter; (2) apparent absence of trans-stimulation of AIB influx; (3) unusually concentrative uptake at steady state (the estimated distribution ratio for 0.2 mM AIB was 55); and (4) susceptibility to inhibition by N-ethylmaleimide. Direct study of the uptake of system L substrates in astrocytes is needed to confirm the present indications of high affinity and concentrative Na+-independent transport.     

Cardiac Stress Test Induced by Dobutamine and Monitored by Cardiac Catheterization in Mice

Dobutamine is a β-adrenergic agonist with an affinity higher for receptor expressed in the heart (β₁) than for receptors expressed in the arteries (β₂). When systemically administered, it increases cardiac demand. Thus, dobutamine unmasks abnormal rhythm or ischemic areas potentially at risk of infarction. Monitoring of heart function during a cardiac stress test can be performed by either ecocardiography or cardiac catheterization. The latter is an invasive but more accurate and informative technique that the former.Cardiac stress test induced by dobutamine and monitored by cardiac catheterization accomplished as described here allows, in a single experiment, the measurement of the following hemodynamic parameters: heart rate (HR), systolic pressure, diastolic pressure, end-diastolic pressure, maximal positive pressure development (dP/dtmax) and maximal negative pressure development (dP/dt_min), at baseline conditions and under increasing doses of dobutamine.As expected, in normal mice we observed a dobutamine dose-related increase in HR, dP/dt_max and dP/dt_min. Moreover, at the highest dose tested (12 ng/g/min) the cardiac decompensation of high fat diet-induced obese mice was unmasked.     

Technical Aspects of the Mouse Aortocaval Fistula

Technical aspects of creating an arteriovenous fistula in the mouse are discussed. Under general anesthesia, an abdominal incision is made, and the aorta and inferior vena cava (IVC) are exposed. The proximal infrarenal aorta and the distal aorta are dissected for clamp placement and needle puncture, respectively. Special attention is paid to avoid dissection between the aorta and the IVC. After clamping the aorta, a 25 G needle is used to puncture both walls of the aorta into the IVC. The surrounding connective tissue is used for hemostatic compression. Successful creation of the AVF will show pulsatile arterial blood flow in the IVC. Further confirmation of successful AVF can be achieved by post-operative Doppler ultrasound.     

Melatonin in the multi‐oscillatory mammalian circadian world

In mammals, the complex interaction of neural, hormonal, and behavioral outputs from the suprachiasmatic nucleus (SCN) drives circadian expression of events, either directly or through coordination of the timing of peripheral oscillators. Melatonin, one of the endocrine output signals of the clock, provides the organism with circadian information and can be considered as an endogenous synchronizer, able to stabilize and reinforce circadian rhythms and to maintain their mutual phase‐relationship at the different levels of the circadian network. Moreover, exogenous melatonin, through an action on the circadian clock, affects all levels of the circadian network. The molecular mechanisms underlying this chronobiotic effect have also been investigated in rats. REV‐ERB α seems to be the initial molecular target.     

城镇污水诱发青蛙蝌蚪红细胞微核及其在环境监测中的应用

本文利用青蛙(Rana nigromaculata Hallowell)蝌蚪红细胞微核试验,作为检测城镇污水诱变活性的一种新的监测技术。在16d生活污水处理的实验中,青蛙蝌蚪红细胞微核细胞率2d后就呈现统计上的显著增加,并随处理时间的延长而增高,第12d达到最大值。在不同浓度混合污水处理实验中,蝌蚪红细胞微核细胞率呈现明显的剂量依赖性增加。上述实验证明城镇生活污水和混合污水都具有较强的诱变活性。作者从遗传毒理学的角度评价了湖北黄州综合生物塘系统对污水诱变活性的净化效能。城镇混合污水经综合生物塘各级塘处理,蝌蚪微核细胞率逐级下降,由进水的7.54‰下降到最后出水的1.52‰,接近对照(1.07‰)水平。其中综合生物塘的藻菌单元比水生植物单元对污水诱变活性具有更强的净化效力。本文提出污水“诱变指数”可作为综合生物塘一项功能评价指标。     

Mass-transfer-limited nitrate uptake on a coral reef flat,Warraber Island,Torres Strait,Australia

Previous research has identified a relationship between the rate of dissipation of turbulent kinetic energy, , and the mass-transfer-limited rate of uptake by a surface, herein called the ^1/4 law, and suggests this law may be applicable to nutrient uptake on coral reefs. To test this suggestion, nitrate uptake rate and gravitational potential energy loss have been measured for a section of Warraber Island reef flat, Torres Strait, northern Australia. The reef flat section is 3 km long, with a 3 m tidal range, and on the days measured, subject to 6 m s^–1 tradewinds. The measured nitrate uptake coefficient, S , on two consecutive days during the rising tide was 1.23±0.28 and 1.42±0.52×10^–4 m s^–1. The measured loss of gravitational potential energy across the reef flat, GPE , on the same rising tides over a 178 m section was 208±24 and 161±20 kg m^–1 s^–2. Assuming the GPE is dissipated as turbulent kinetic energy in the water column, and using the ^1/4 law, the mass-transfer-limited nitrate uptake coefficient, S_MTL , on the two days was 1.57±0.03 and 1.45±0.04×10^–4 m s^–1. Nitrate uptake on Warraber Island reef flat is close to the mass-transfer limit, and is determined by oceanographic nitrate concentrations and energy climate.Communicated by B.C. Hatcher