Identification of the interstellar cyanomethyl radical (CH2CN) in the molecular clouds TMC-1 and Sagittarius B2

We report the astronomical identification of the cyanomethyl radical, CH2CN, the heaviest nonlinear molecular radical to be identified in interstellar clouds. The complex fine and hyperfine structures of the lowest rotational transitions at about 20.12 and 40.24 GHz are resolved in TMC-1, where the abundance appears to be about 5 x 10(-9) relative to that of H2. This is significantly greater than the observed abundance of CH3CN (methyl cyanide) in TMC-1. In Sgr B2 the hyperfine structure is blended in the higher frequency transitions at 40, 80, and 100 GHz, although the spin-rotation doubling is clearly evident. Preliminary searches in other sources indicate that the distribution of CH2CN is similar to that for such carbon chain species as HC3N or C4H.     

Development of two novel CYP-antibodies and their use in a PCB exposure experiment with Mytilus edulis

In an attempt to learn more about the cytochrome P450 (CYP) system of mussels, we used protein databases and alignment software to extract highly conserved CYP sequences. From these alignments synthetic peptides were produced and used for rabbit immunisation, which yielded polyclonal antibodies against the CYP families 2 and 4. The antibodies were evaluated with Western Blot and ELISA assays, using digestive gland microsomal samples from the mussel Mytilus edulis. Western Blots revealed immunoreactions for both antibodies. The anti-CYP2 sequence rendered one major immunopositive protein of approximately 49 kDa size, and weak signals for proteins of approximately 41 and 56 kDa size. The anti-CYP4 sequence rendered two major bands of approximately 56 and 59 kDa size, and also a weak immunoreaction with a protein of approximately 43 kDa size. ELISA rendered only weak signals even with a 1:50 dilution of IgG-purified serum. A 10-day exposure to Aroclor 1254 did not appear to affect any of the immunopositive proteins, while total PCBs in soft bodies increased from 14-40 ng/g DW in controls to 373-638 ng/g DW in exposed mussels.     

用于评价吸湿性播撒云和降水演变的短波偏振雷达技术

引言近年来,借助于有显著改进的遥感及模拟的方法,天气研究和应用已经取得了很大进展。然而,人工影响天气的研究和应用已经到了需要抉择的重要关头。由于在流域范围内重要区域缺少使人信服的降水增加一致性的证据,这个领域或是将变成不再存在,并且当世界淡水危机是如此的严重以致不能不管时,只能等待未来几代人的努力才能解决,或是将实施战略研究,通过采用新技术进入现代主流来寻找保障继续发展的技术。为了更好地证明作为基础的假设并在应用中提供可能的产品,实施战略研究是很有必要的。然而,直到现在,除了孤立的研究计划以外,还没有涉及到…     

Survey of estrogenic and androgenic disruption in Swedish coastal waters by the analysis of bile fluid from perch and biomarkers in the three-spined stickleback

The potential for endocrine disruption close to sewage treatment plant and pulp mill effluent discharge points along the Swedish Baltic Sea coast was explored using a dual survey strategy employing two stationary fish species. The levels of vitellogenin and spiggin as biomarkers of endocrine disruption were determined in juvenile three-spined sticklebacks (Gasterosteus aculeatus L.) together with the sex ratios and the presence of intersex. As an indication of exposure, estrogenic and androgenic substances were analysed by GC–MS in bile from perch (Perca fluviatilis L.). Spiggin and vitellogenin levels in juvenile three-spined sticklebacks were generally low, and, for most sampling sites no deviation in gonad type ratios were observed. No remarkable levels of natural or synthetic estrogens or androgens were observed in bile fluid from perch, while bisphenol A and 4-nonylphenol were detected in perch from both reference sites and exposed sites. Taken together, the results did not indicate estrogenic or androgenic disruption in the investigated waters.     

内蒙古敖汉旗早三叠世正长花岗岩锆石U-Pb年代学、地球化学特征

正近些年研究显示华北地台北缘存在一条近东西向展布的早三叠世后造山的花岗岩带,在吉林东部,内蒙古中部及西部地区具有发现,但在赤峰敖汉旗地区还未见报道。本次工作在敖汉旗区域地质调查过程中,从原来侏罗纪岩体中重新厘定出一套正长花岗岩,本文对其年代学及地球化学进行介绍,以探讨华北地台北缘中段-东段过渡带的古亚洲洋闭合时限。     

金银矿床中流体包裹体研究现状

<正> 70年代以来,“黄金热”促使地质工作者对金银矿床进行了大量的流体包裹体研究,并取得了丰富的成果。本文将尽量详细地介绍这方面的研究现状。在此之前,让我们首先回顾一下包裹体的研究史,以加深我们对包裹体研究趋势的认识。1 历史回顾 最早的流体包裹体研究可以追溯到19世纪初期。1818年,Breislak等第一次对包裹体进行了成分分析,目的是证明矿物和岩石是从水中形成的。在以后的数十年中,Sorby和Zirkel等在流体包裹体研究方面获得了具有实质性的成果。Sorby(1858年)认为包裹体     

大兴安岭地区三叠系划分与对比

厘定后的大兴安岭中南部地区老龙头组以红杂色沉积岩为主,夹或不夹中酸性火山岩层,含早三叠世Calamospora-Lundbladispora-Alisporites和Verrucosisporites-Lundbladispora-Chordasporites孢粉组合,Huanghestheria-Cornia-Palaeolimnadia叶肢介组合以及Darwinula triassiana-D. rotundata介形类组合.大兴安岭中北部地区以安山岩为主的哈达陶勒盖组整合在老龙头组之上,据此将该区下三叠统自下而上分为老龙头组和哈达陶勒盖组.原下侏罗统或上三叠统-下侏罗统东宫组自下而上分为一段和二段,根据一段同位素平均年龄为208.97 Ma（K-Ar法）,并被二段（相当于下侏罗统查伊河组）平行不整合覆盖,将第一段单独划为东宫组,时代属于晚三叠世.