Stratigraphic Model Predictions of Geoacoustic Properties

Geoacoustic properties of the seabed have a controlling role in the propagation and reverberation of sound in shallow-water environments. Several techniques are available to quantify the important properties but are usually unable to adequately sample the region of interest. In this paper, we explore the potential for obtaining geotechnical properties from a process-based stratigraphic model. Grain-size predictions from the stratigraphic model are combined with two acoustic models to estimate sound speed with distance across the New Jersey continental shelf and with depth below the seabed. Model predictions are compared to two independent sets of data: 1) Surficial sound speeds obtained through direct measurement using in situ compressional wave probes, and 2) sound speed as a function of depth obtained through inversion of seabed reflection measurements. In water depths less than 100 m, the model predictions produce a trend of decreasing grain-size and sound speed with increasing water depth as similarly observed in the measured surficial data. In water depths between 100 and 130 m, the model predictions exhibit an increase in sound speed that was not observed in the measured surficial data. A closer comparison indicates that the grain-sizes predicted for the surficial sediments are generally too small producing sound speeds that are too slow. The predicted sound speeds also tend to be too slow for sediments 0.5-20 m below the seabed in water depths greater than 100 m. However, in water depths less than 100 m, the sound speeds between 0.5-20-m subbottom depth are generally too fast. There are several reasons for the discrepancies including the stratigraphic model was limited to two dimensions, the model was unable to simulate biologic processes responsible for the high sound-speed shell material common in the model area, and incomplete geological records necessary to accurately predict grain-size

宁康霉素产生菌海洋地衣芽孢杆菌BAC-9912的诱变育种

宁康霉素(Nincomycin)产生菌BAC-9912经紫外线单因子和亚硝基胍化学试剂诱变后,获得两株高产菌株9912-7-2U(UV处理获得)和9912-2U-32N(NTG处理获得),其摇瓶效价分别为176.464×105u·L-1和217.808×105u·L-1。比出发菌株效价分别提高126.9%和180.0%。连续传代摇瓶效价稳定。初步建立了形态观察法和琼脂块大通量法两种初筛模型。

利用比较染色体涂色和BAC定位技术探讨麂属动物染色体的起源和演化

比较细胞遗传学研究发现物种的形成过程往往伴随着核型结构的变化，各种鹿属动物染色体的巨大差异正是很好的例证'赤魔的染色体被证明是由具有端着丝粒的祖先染色体经过多次的串联融合进化而来的。根据祖先染色体的形态和连接方式，可以将染色体串联融合主要分为三类：着丝粒一着丝粒融合，着丝粒一端粒融合和端粒一端粒融合。经典细胞遗传学，比较染色体涂色，卫星DNA序列和部分融合位点序列比较研究都支持串联融合假说。但串联融合的类型和分子机制迄今没有完全弄清楚。本论文旨在对魔属动物的串联融合类型和分子机制进行研究，分为两个部分：一、通过比较染色体涂色的方法，建立小鹿一林察一大额牛的比较染色体图谱，结合以前发表的结果来阐明鹿科（小魔）与牛科（大额牛），寮科（林磨）之间的核型关系；二、建立赤鹿的全基因组BAc文库，通过克隆定位的方法确立在赤魔的染色体进化过程中所发生的串联融合类型，并对其机制进行探讨。主要结果如下：利用小鹿的染色体特异探针与林寮，大额牛的染色体进行杂交，首次建立了小鹿一大额牛，小魔一林察的核型对比关系。结果显示小鹿的1-5、11号染色体均与林集和大额牛的多段染色体同源。结合高分辨的G带比较，发现小魔1-5和11号染色体上的与林爵和大额牛对应的所有同源片断在小鹿染色体上呈着丝粒一端粒连接排列。从而进一步证明小鹿的1-5和11号染色体是由2n=70的祖先核型通过染色体的着丝粒一端粒串联融合方式进化而来的。建立了我国第一个赤魔全基因组BAC文库，该文库由124800个克隆组成。大部分插入片段的大小在100-145kb之间，片段的平均大小为12＜0kb。克隆定位显示克隆的分布与小鹿染色体大小成正比关系，说明整个文库没有染色体的偏倚，文库为整个基因组的6倍，覆盖率几乎为100％。通过赤鹿BAC克隆在小魔和赤鹿染色体上的精确定位，使我们得以准确判断小鹿染色体在赤鹿染色体同源片段上的连接方式，并确定串联融合的类型。结果进一步支持赤鹿的核型是由一个2n=70祖先核型通过着丝粒一端粒的融合方式进化而来的。

Purification and characterization of L-amino acid oxidase from Agkistrodon blomhoffii ussurensis snake venom of Changbai Mountains

The L-a. a, oxidase of Agkistrodon blomhof fii ussurensis of Changbai Mountains in northeast of China has been separated by using ion-exchange and gel filtration techniques, This enzyme is composed of two subunits, the molecular weight of one subunit is about 36 000, the another is about 57 000, determined by sodium dodecyl sulfate-polyacryamide gel electrophoresis and matrix assisted laser desorption ion/time of flight mass spectrometry, The activity of L-a, a. oxidase determined using L-Leu as substrate. The optimal pH of the enzyme is 4. 5 similar to 5. 5 and 8 similar to 9. The UV-Visible absorption spectrum of L-a, a. oxidase shows the characteristics of flavor-proteins.

Construction and characterization of two bacterial artificial chromosome libraries of Zhikong scallop, Chlamys farreri Jones et Preston, and identification of BAC clones containing the genes involved in its innate immune system

Large-insert bacterial artificial chromosome (BAC) libraries are necessary for advanced genetics and genomics research. To facilitate gene cloning and characterization, genome analysis, and physical mapping of scallop, two BAC libraries were constructed from nuclear DNA of Zhikong scallop, Chlamys farreri Jones et Preston. The libraries were constructed in the BamHI and MboI sites of the vector pECBAC1, respectively. The BamHI library consists of 73,728 clones, and approximately 99% of the clones contain scallop nuclear DNA inserts with an average size of 110 kb, covering 8.0x haploid genome equivalents. Similarly, the MboI library consists of 7680 clones, with an average insert of 145 kb and no insert-empty clones, thus providing a genome coverage of 1.1x. The combined libraries collectively contain a total of 81,408 BAC clones arrayed in 212 384-well microtiter plates, representing 9.1x haploid genome equivalents and having a probability of greater than 99% of discovering at least one positive clone with a single-copy sequence. High-density clone filters prepared from a subset of the two libraries were screened with nine pairs of Overgos designed from the cDNA or DNA sequences of six genes involved in the innate immune system of mollusks. Positive clones were identified for every gene, with an average of 5.3 BAC clones per gene probe. These results suggest that the two scallop BAC libraries provide useful tools for gene cloning, genome physical mapping, and large-scale sequencing in the species.

Transformation of accommodation space of the Cretaceous Qingshankou Formation, the Songliao Basin, NE China

Analysis of accommodation space variation during deposition of the Cretaceous Qingshankou Formation in the Songliao Basin, NE China, indicates that accommodation space changed both through time and across the basin as a seesaw movement. The mid-upper Qingshankou Formation is divided into three units. In each unit, changes of accommodation space differ in the southern and northern part of the basin. Increasing accommodation in the southern part is accompanied by a decrease in the northern part, and vice versa. Between the northern and southern basin, there was a neutral belt that is like a fulcrum, called the transformation belt here, where the accommodation did not change to any significant degree. We call this response 'accommodation transformation', whose characteristics are defined by tectonic subsidence analysis, palaeontological and sedimentary analyses. The accommodation increasing belt, decreasing belt, transformation belt and accommodation transformation boundary together constitute the accommodation transformation system. The recognition of accommodation transformation in the Songliao Basin provides a new insight into sequence stratigraphy and might be widely applicable.

Seismic characteristics of a reef carbonate reservoir and implications for hydrocarbon exploration in deepwater of the Qiongdongnan Basin, northern South China Sea

Our analysis of approximately 40,000 km of multichannel 2-D seismic data, reef oil-field seismic data, and data from several boreholes led to the identification of two areas of reef carbonate reservoirs in deepwater areas (water depth >= 500 in) of the Qiongdongnan Basin (QDNB), northern South China Sea. High-resolution sequence stratigraphic analysis revealed that the transgressive and highstand system tracts of the mid-Miocene Meishan Formation in the Beijiao and Ledong-Lingshui Depressions developed reef carbonates. The seismic features of the reef carbonates in these two areas include chaotic bedding, intermittent internal reflections, chaotic or blank reflections, mounded reflections, and apparent amplitude anomalies, similar to the seismic characteristics of the LH11-1 reef reservoir in the Dongsha Uplift and Island Reef of the Salawati Basin, Indonesia, which house large oil fields. The impedance values of reefs in the Beijiao and Ledong-Lingshui Depressions are 8000-9000 g/cc x m/s. Impedance sections reveal that the impedance of the LH11-1 reef reservoir in the northern South China Sea is 800010000 g/cc x m/s, whereas that of pure limestone in BD23-1-1 is > 10000 g/cc x m/s. The mid-Miocene paleogeography of the Beijiao Depression was dominated by offshore and neritic environments, with only part of the southern Beijiao uplift emergent at that time. The input of terrigenous sediments was relatively minor in this area, meaning that terrigenous source areas were insignificant in terms of the Beijiao Depression: reef carbonates were probably widely distributed throughout the depression, as with the Ledong-Lingshui Depression. The combined geological and geophysical data indicate that shelf margin atolls were well developed in the Beijiao Depression, as in the Ledong-Lingshui Depression where small-scale patch or pinnacle reefs developed. These reef carbonates are promising reservoirs, representing important targets for deepwater hydrocarbon exploration. (C) 2008 Elsevier Ltd. All rights reserved.