A genetic linkage map of Pacific white shrimp (Litopenaeus vannamei): sex-linked microsatellite markers and high recombination rates

Pacific white shrimp (Litopenaeus vannamei) is the leading species farmed in the Western Hemisphere and an economically important aquaculture species in China. In this project, a genetic linkage map was constructed using amplified fragment length polymorphism (AFLP) and microsatellite markers. One hundred and eight select AFLP primer combinations and 30 polymorphic microsatellite markers produced 2071 markers that were polymorphic in either of the parents and segregated in the progeny. Of these segregating markers, 319 were mapped to 45 linkage groups of the female framework map, covering a total of 4134.4 cM; and 267 markers were assigned to 45 linkage groups of the male map, covering a total of 3220.9 cM. High recombination rates were found in both parental maps. A sex-linked microsatellite marker was mapped on the female map with 6.6 cM to sex and a LOD of 17.8, two other microsatellite markers were also linked with both 8.6 cM to sex and LOD score of 14.3 and 16.4. The genetic maps presented here will serve as a basis for the construction of a high-resolution genetic map, quantitative trait loci (QTLs) detection, marker-assisted selection (MAS) and comparative genome mapping.

cDNA cloning, characterization and expression analysis of the antioxidant enzyme gene, catalase, of Chinese shrimp Fenneropenaeus chinensis

Catalase is an important antioxidant protein that protects organisms against various oxidative stresses by eliminating hydrogen peroxide. The full-length catalase cDNA of Chinese shrimp Fenneropenaeus chinensis was cloned from the hepatopancreas using degenerate primers by the method of 3' and 5' rapid amplification of cDNA ends PCR. The cDNA sequence consists of 1892 bp with a 1560 bp open reading frame, encoding 520 amino acids with high identity to invertebrate, vertebrate and even bacterial catalases. The sequence includes the catalytic residues His71, Asn144, and Tyr354. The molecular mass of the predicted protein is 58824.04 Da with an estimated pl of 6.63. Sequence comparison showed that the deduced amino acid sequence of F. chinensis catalase shares 96%, 73%, 71% and 70% identity with that of Pacific white shrimp Litopenaeus vannamei, Abalone Haliotis discus hannai, Zhikong scallop Chlamys farreri and Human Homo sapiens, respectively. Catalase transcripts were detected in hepatopancreas, hemocytes, lymphoid organ, intestine, ovary, muscle and gill. by real-time PCR. The variation of catalase mRNA transcripts in hemocytes and hepatopancreas was also quantified by real-time PCR and the result indicated that the catalase showed up-regulated expression trends in hemocytes at 14 h and in hepatopancreas at 37 h after injection with white spot syndrome virus (WSSV). (c) 2008 Elsevier Ltd. All rights reserved.

Molecular cloning and characterization of a thioester-containing protein from Zhikong scallop Chlamys farreri

Thioester-containing proteins are a family of proteins characterized by the unique intrachain beta-cysteinyl-gamma-glutamyl thioester, which play important roles in innate immune responses. The cDNA of Zhikong scallop Chlamys farreri thioester-containing protein (designated as CfTEP) was cloned by expressed sequence tag (EST) and rapid amplification of cDNA ends (RACE) approaches. The full-length cDNA of CfTEP was of 4616 bp, consisting of a 5 '-terminal untranslated region (UTR) of 30 bp and a 3 ' UTR of 140 bp with a polyadenylation signal sequence AATAAA and a poly(A) tail. The CfTEP cDNA encoded a polypeptide of 1481 amino acids with the theoretical isoelectric point of 5.98 and the predicted molecular weight of 161.4 kDa. The deduced amino acid sequence of CfTEP contained the canonical thioester motif GCGEQ, nine potential N-glycosylation sites and a C-terminal distinctive cysteine signature. It also contained a presumed catalytic histidine and proteolytic cleavage sites that were similar to C3 molecules. The high similarity of CfTEP with the thioester-containing proteins in other organisms, such as the TEPs from insects, the complement component C3, C4, C5 and the protease inhibitor alpha(2)-macroglobulin indicated that CfTEP should be a member of TEP family. The phylogenetic analysis revealed that CfTEP was closely related to TEPs from mollusc, nematodes and insects, and they formed a separate branch apart from the branches of complements factors and alpha(2)-macroglobulins. The spatial expression of CfTEP transcripts in healthy and bacterial challenged scallops was examined by semi-quantitative RT-PCR. The CfTEP transcripts were mainly detected in the tissues of hepatopancreas and gonad, and remarkably up-regulated by Microbial challenge, which suggested that CfTEP was a constitutive and inducible acute-phase protein involved in immune defense. These results provided new insights into the role of CfTEP in scallop immune responses, as well as the evolutionary origin of this important, widespread and functionally diversified family of proteins. (c) 2007 Published by Elsevier Ltd.

Molecular cloning, expression of a peroxiredoxin gene in Chinese shrimp Fenneropenaeus chinensis and the antioxidant activity of its recombinant protein

Peroxiredoxin (Prx) is known to be an antioxidant protein that protects the organisms against various oxidative stresses and functions in intracellular signal transduction. A Prx gene was firstly isolated in the crustacean, Chinese shrimp Fenneropenaeus chinensis. The full-length cDNA consists of 942 bp with a 594 bp open reading frame, encoding 198 amino acids. The molecular mass of the deduced amino acid is 22041.17 Da with an estimated pI of 5.17. Sequence comparison showed that Prx of F. chinensis shares 76%, 73% and 72% identity with that of Aedes aegypti, Branchiostoma belcheri tsingtaunese and Drosophila melanogaster, respectively. Northern blot analysis revealed the presence of Prx transcripts of F chinensis in all tissues examined. Real-time PCR analysis indicated that the Prx showed different expression profiles in shrimp hemocytes and hepatopancreas after artificial infection with Vibrio anguillarum. In addition, a fusion protein containing Prx was produced in vitro. LC-ESI-MS analysis showed that four peptide fragments of the recombinant protein were identical to the corresponding sequence of F. chinensis Prx. And the purified recombinant proteins were shown to reduce H2O2 in the presence of dithiothreitol. (c) 2007 Elsevier Ltd. All rights reserved.

Species identification in salted products of red snappers by semi-nested PCR-RFLP based on the mitochondria 12S rRNA gene sequence

A molecular approach was developed to distinguish species of red snappers among commercial salted fish products. The specific fragments of the mitocliondrial 12S rRNA gene, which were about 450 bp, were obtained using the semi-nested polymerase chain reaction (semi-nested PCR). Subsequently, PCR amplicons were sequenced, aiming to select restriction endonucleases that generated species-specific restriction fragment length polymorphism (RFLP) profiles. Discrimination of red snappers Lutjanus sanguineus, L. erythopterus from L. argentintaculatus, L. malabarius and other morphologically similar fishes such as Lethrinus leutjanus and Pinjalo pinjalo was feasible by one restriction digestion reaction with three endonucleases Hae III, Sca I and SnaB I, however, for differentiation of L. sattguineus and L. erythopterus, another restriction digestion reaction with single restriction endonuclease Mae II was needed. The seminested PCR-RFLP was demonstrated to be reliable in species identification of salted fish products in this study. (c) 2005 Published by Elsevier Ltd.

Isolation and mapping of telomeric pentanucleotide (TAACC)(n) repeats of the pacific whiteleg shrimp, Penaeus vannamei, using fluorescence in situ hybridization

To develop genetic and physical maps for shrimp, accurate information on the actual number of chromosomes and a large number of genetic markers is needed. Previous reports have shown two different chromosome numbers for the Pacific whiteleg shrimp, Penaeus vannamei, the most important penaeid shrimp species cultured in the Western hemisphere. Preliminary results obtained by direct sequencing of clones from a Sau3A-digested genomic library of P. vannamei ovary identified a large number of (TAACC/GGTTA)-containing SSRs. The objectives of this study were to (1) examine the frequency of (TAACC)(n) repeats in 662 P. vannamei genomic clones that were directly sequenced, and perform homology searches of these clones, (2) confirm the number of chromosomes in testis of P. vannamei, and (3) localize the TAACC repeats in P. vannamei chromosome spreads using fluorescence in situ hybridization (FISH). Results for objective I showed that 395 out of the 662 clones sequenced contained single or multiple SSRs with three or more repeat motifs, 199 of which contained variable tandem repeats of the pentanucleotide (TAACC/GGTTA),, with 3 to 14 copies per sequence. The frequency of (TAACC)n repeats in P. vannamei is 4.68 kb for SSRs with five or more repeat motifs. Sequence comparisons using the BLASTN nonredundant and expressed sequence tag (EST) databases indicated that most of the TAACC-containing clones were similar to either the core pentanucleotide repeat in PVPENTREP locus (GenBank accession no. X82619) or portions of 28S rRNA. Transposable elements (transposase for Tn1000 and reverse transcriptase family members), hypothetical or unnamed protein products, and genes of known function such as 18S and 28S rRNAs, heat shock protein 70, and thrombospondin were identified in non-TAACC-containing clones. For objective 2, the meiotic chromosome number of P. vannamei was confirmed as N = 44. For objective 3, four FISH probes (P1 to P4) containing different numbers of TAACC repeats produced positive signals on telomeres of P. vannamei chromosomes. A few chromosomes had positive signals interstitially. Probe signal strength and chromosome coverage differed in the general order of P1 > P2 > P3 > P4, which correlated with the length of TAACC repeats within the probes: 83, 66, 35, and 30 bp, respectively, suggesting that the TAACC repeats, and not the flanking sequences, produced the TAACC signals at chromosome ends and TAACC is likely the telomere sequence for P. vannamei.

Benthic foraminifera and bottom water evolution in the middle-southern Okinawa Trough during the last 18 ka

A piston sediment core E017 from the middle-southern Okinawa Trough was investigated. A preliminary study of the deep-water evolution since 18 cal. ka BP was performed based on the quantitative census data of benthic foraminiferal fauna, together with planktonic foraminiferal oxygen and carbon isotope, AMS(14)C dating, and the previous results achieved in the southern Okinawa Trough. The result shows that the benthic fauna was dominated by Bulimina aculeata (d'Orbigny), Uvigerina peregrina (Cushman), Hispid Uvigerina and Uvigerina dirupta (Todd) during the glaciation-deglaciation before 9.2 cal. ka BP, while Epistominella exigua (Brady), Pullenia bulloides (d'Orbigny), Cibicidoides hyalina (Hofker), Sphaeroidina bulloides (d'Orbigny) and Globocassidulina subglobosa (Brady) predominated the fauna in the post-glacial period after 9.2 cal. ka BP. The benthic foraminifera accumulation rate (BFAR), paleoproductivity estimates and benthic foraminiferal assemblage conformably indicate that surface water paleoproductivity and organic matter flux during the glaciation-deglaciation were higher than those of the post-glacial period in the middle-southern Okinawa Trough, and gradually enhanced from the southern to the central Okinawa Trough during the glaciation-deglaciation, which could be caused by the discrepancy of the terrigenous nutrients supply. High abundances of E exigua, an indicator of pulsed organic matter input, after 9.2 cal. ka. BP may indicate that the intensity of seasonally riverine pulsed flux during the post-glacial period was stronger than that of the glaciation-deglaciation period, and the seasonal influx in the central trough might be stronger than in the south. The temporal distributions of the typical species indicating bottom water oxygen content and ventilation condition show that the ventilation of the bottom water during the post-glacial period is more active than the glaciation-deglaciation, which reflects that the evolution of the intermediate and deep waters of the northwestern Pacific during the last glaciation has no evident influence on the deep-water of the middle-southern Okinawa Trough. Additionally, the variations in agglutinated benthic foraminiferal abundance and other carbonate dissolution proxies indicate that carbonate dissolution gradually increased since the last 18 ka in the Okinawa Trough and rapidly enhanced at 9.2 cal. ka BP. The modern shallow carbonate lysocline could form at 3 cal. ka BP.

Recent 2000-year geological records of mud in the inner shelf of the East China Sea and their climatic implications

AXIS(14)C dating and grain-size analysis for Core DD2, located at the north of the Yangtze River-derived mud off the Zhejiang-Fujian coasts in the inner shelf of the East China Sea, provide us a high-resolution grain-size distribution curve varying with depth and time. Data in the upper mud layer of Core DD2 indicate that there are at least 9 abrupt grain-size increasing in recent 2000 years, with each corresponding very well with the low-temperature events in Chinese history, which might result from the periodical strengthening of the East Asian Winter Monsoon (EAWM), including the first-revealed maximum temperature lowering event at around 990 a BP. At the same time, the finer grain size section in Core DD2 agrees well with the Sui-Tang Warming Period (600-1000 a AD) defined previously by Zhu Kezhen, during which the climate had a warm, cold and warm fluctuation, with a dominated cooling period of 750-850 a AD. The Little Ice Age (LIA) can also be identified in the core. It starts around 1450 a AD and was followed by a subsequent cooling events at 1510, 1670 and 1840 a AD. Timing of these cold events revealed here still needs to be further verified owing to some current uncertainty of dating we used in this study.

Sedimentary changes during the Holocene in the Bohai Sea and its paleoenvironmental implication

Samples of two cores, Cores M5-5 and M7-4 in the Bohai Sea were analyzed in isotopes, grain size, heavy minerals, chemical compositions, and 14 C dating to reconstruct the sedimentation during the Holocene. Abrupt change in carbon and oxygen stable isotopes was recognized at Core M5-5 at about 6400 a BP, which was likely due to the intrusion of the Yellow Sea Warm Current (YSWC) extension into the Bohai Sea. At Core M7-4, sediments between 5900 and 6600 a BP (150-260 cm depth) became coarse-grained, containing rich garnet, high manganese content, and nil autogenic pyrite, indicating a very dynamic sedimentary event during which the ambience was transformed from reductive to oxidative, and sedimentation boosted. Meanwhile, the YSWC had invaded into the Bohai Sea indicated by rich planktonic foraminifera in this event. (c) 2008 Elsevier Ltd. All rights reserved.

Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene

AMS(14)C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed. These three proxies, mean grain size (>9.71 mu m), chemical index of alteration (CIA) and ratio of smectite to kaolinite in particular, show similar fluctuation patterns. Furthermore, 10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene; these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon. The cooling events correlated well with the results of the delta O-18 curves of the Dunde ice core and GISP2, which therefore revealed a regional response to global climate change. Four stages of the East Asia winter monsoon were identified, i.e. 8300-6300 a BP, strong and unstable; 6300-3800 a BP, strong but stable; 3800-1400 a BP, weak and unstable; after 1400 a BP, weak but stable.

Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea

AMS(14)C dating and grain-size analysis for Core PC-6, located in the middle of a mud area on the inner shelf of the East China Sea (ECS), were used to rebuild the Holocene history of the East Asian winter monsoon (EAWM). The 7.5-m core recorded the history of environmental changes during the postglacial transgression. The core's mud section (the upper 450 cm) has been formed mainly by suspended sediment delivered from the Yangtze River mouth by the ECS Winter Coastal Current (ECSWCC) since 7.6 kyr BP. Using a mathematical method called "grain size vs. standard deviatioW', we can divide the Core PC-6's grain-size distribution into two populations at about 28 mu m. The fine population (< 28 mu m) is considered to be transported by the ECSWCC as suspended loads. Content of the fine population changes little and represents a stable sedimentary environment in accord with the present situation. Thus, variation of mean grain-size from the fine population would reflect the strength of ECSWCC, which is mainly controlled by the East Asian winter monsoon. Abrupt increasing mean grain size in the mud section is inferred to be transported by sudden strengthened ECSWCC, which was caused by the strengthened EAWM. Thus, the high resolution mean grain-size variation might serve as a proxy for reconstruction of the EAWM. A good correlation between sunspot change and the mean grain-size of suspended fine population suggests that one of the primary controls on centennial- to decadal-scale changes of the EAWM in the past 8 ka is the variations of sun irradiance, i.e., the EAWM will increase in intensity when the number of sunspots decreases. Spectral analyses of the mean grain-size time series of Core PC-6 show statistically significant periodicities centering on 2463, 1368, 128, 106, 100, 88-91, 7678, and 70-72 years. The EAWM and the East Asian summer monsoon (EASM) agree with each other well on these cycles, and the East Asian Monsoon (EAM) and the Indian Monsoon also share in concurrent cycles in Holocene, which are in accord with the changes of the sun irradiance. (c) 2005 Elsevier B.V. All rights reserved.

中华绒螯蟹（Eriocheir sinensis）Peroxiredoxin 6和Thioredoxin1基因的克隆及表达

中华绒螯蟹是我国重要的水产经济动物，近年来养殖规模不断扩大，产量持续增加。但是，伴随着养殖规模的扩大，养殖环境也日益恶化并导致了大量疾病的发生，严重制约了中华绒螯蟹养殖业的健康发展。因此，疾病预防和控制对中华绒螯蟹养殖业的可持续发展具有举足轻重的作用。与其他无脊椎动物一样，中华绒螯蟹的免疫系统没有免疫球蛋白和淋巴细胞，而是依靠由细胞免疫和体液免疫构成的固有免疫系统来对病原进行识别和清除。中华绒螯蟹的固有免疫机制的研究有助于推动中华绒螯蟹病害防治工作的开展。 本研究采用大规模EST测序方法，结合末端快速扩增（rapid amplification of cDNA ends，RACE）技术从中华绒螯蟹血淋巴中克隆到了过氧化物还原酶（peroxiredoxin，EsPrx6）和硫氧还蛋白（thioredoxin，EsTrx1）基因的cDNA 全长序列；采用实时荧光定量PCR 技术检测了这两个基因在健康个体中表达的组织分布情况以及鳗弧菌刺激后血淋巴细胞中的时序表达规律；同时，将这两个基因的编码区克隆到pET 系列载体，并在大肠杆菌中实现了重组表达，并进行了体外活性检测。 过氧化物还原酶是一个抗氧化蛋白超家族，在保护机体免受活性氧（reactive oxygen species，ROS）的伤害中发挥着重要作用。中华绒螯蟹Prx6（EsPrx6） 基因的cDNA 全长为1076 bp，5` UTR（untranslated region，UTR） 为69 bp，3` UTR 为347 bp，开放阅读框（open reading frame，ORF）为660 bp，编码219 个氨基酸的蛋白。mRNA 3`-端具有多聚腺苷酸加尾信号（polyadenylation signal）AATAAA 和polyA 尾巴。EsPrx6 的预测分子量为 24 kDa，理论等电点为6.21，具有一个保守的Prx 结构域、一个AhpC 结构域和过氧化物酶催化活性中心PVCTTE，表明EsPrx6 属于1-Cys 型Prx。在所检测的组织中均有EsPrx6 的表达，其中以肝胰腺表达量最高，为血淋巴细胞中表达量的17.4 倍。鳗弧菌刺激后，血淋巴细胞中EsPrx6 的表达下降，到12 h 时，实验组显著低于对照组（P<0.05）；随时间推移，表达水平逐渐回升，但在整个实验期间，都没有恢复到起始水平。将EsPrx6 进行体外重组并在大肠杆菌E. coli BL21（DE3）中实现表达，重组EsPrx6 具有预期的抗氧化活性和过氧化物酶活性，其中抗氧化活力为14.69 U/mg 蛋白，高于相同条件下GSH 的抗氧化力（P<0.05），过氧化物酶活力为23.46 U/mg 蛋白。结果表明，EsPrx6 作为一种重要的抗氧化剂，在中华绒螯蟹抵御ROS 可能引起的氧化损伤方面具有重要作用。 硫氧还蛋白是广泛存在于生物体内的一种具有硫醇依赖性的具有还原活性的蛋白。中华绒螯蟹Trx1（EsTrx1）基因的cDNA 全长为641 bp，5` UTR 为17 bp，3` UTR 为306 bp，开放阅读框为318 bp，编码105 个氨基酸。EsTrx1 的预测分子量为12.2 kDa，理论等电点为4.8。EsTrx1 不含信号肽，其氨基酸序列与其他动物的Trx1s 具有高度相似性，如与地中海黄蝎的Trx1 相似度达到73%；而与其他物种Trx2 的同源性很低，相似度仅为14.3-22.8%，表明EsTrx1 属于Trx1 亚族。实时荧光定量PCR 检测发现，EsTrx1 在鳃、性腺、肝胰腺、肌肉、心脏和血淋巴细胞中都有表达。血淋巴细胞中EsTrx1 mRNA 的表达量在菌刺激后上升，刺激后6 h，实验组表达量显著高于对照组和空白组（P<0.05），然后逐渐恢复到刺激前水平。为进一步探讨其生物学功能，将EsTrx1 进行体外重组并在大肠杆菌E. coli BL21（DE3）得到表达，重组EsTrx1 具有预期的氧化还原调节活性，抗氧化活力为3.06 U/mg，且抗氧化活力高于GSH（P<0.05）。rEsTrx1 的二硫键还原活力为5.03，低于凡纳滨对虾的二硫键还原活力（10.44），接近于大肠杆菌（4.93），小牛胸腺（6.50）和小牛肝脏（5.09），而高于鲍鱼Trx2（1.83）活力。结果表明，EsTrx1 在生理条件下能够作为一种重要的抗氧化剂，参与对细菌感染的免疫应答反应。

苔藓动物线粒体基因组的测定及系统发生分析

苔藓动物为一类底栖、滤食性、营附着生活的小型水生群体动物。苔藓动物作为重要的海洋无脊椎动物，在生态上具有重要意义，同时在生物活性物质分离等方面也有重要的应用价值。然而目前对于苔藓动物门的分子系统发生研究还相对较少，对于本门的进化地位尚存在许多争议。本门在后生动物中的进化地位尚未得到确定，它同腕足动物门、帚虫动物门、内肛动物门间的进化关系仍然悬而未决，门内部的系统发生关系也未达成一致。 本研究采用Long-PCR技术扩增了管孔目苔虫扇形管孔苔虫（Tubulipora flabellaris）和唇口目苔虫颈链血苔虫（Watersipora subtorquata）的线粒体基因组，然后利用DNA文库构建结合引物步移的策略获得了它们的线粒体基因组序列。结果显示它们的线粒体基因组具有一些显著的特点：1. T. flabellaris与W. subtorquata线粒体基因组全长分别为13,763 bp和14,144 bp，与其它后生动物相比较小；2. 两个基因组的最大的非编码区都较小，分别为230 bp和100 bp；3. 两个基因组都编码36个基因，包括12个蛋白质编码基因、2个核糖体RNA基因和22个转运RNA基因。与典型的动物线粒体基因组相比，它们都缺失了atp8基因；4. 通过对基因排列顺序的比较分析发现，T. flabellaris与W. subtorquata的线粒体基因组基因排列顺序与其它后生动物显著不同，相同的基因块（不包括转运RNA基因）最长分别为4个和3个基因。目前已知的四个苔藓动物线粒体基因组的基因排列顺序也非常不同，说明苔藓动物的线粒体基因组经历了大规模的基因重排过程。 为了探讨苔藓动物门的进化地位，基于26个后生动物线粒体基因组的11个蛋白质编码基因（不包括atp6和atp8）的氨基酸序列，分别采用最大似然法与贝叶斯法构建分子系统发生树。本研究的结果支持冠轮动物为单系群，触手冠动物位于冠轮动物内部。结果显示毛颚动物与苔藓动物亲缘关系接近，然而这需要更多的证据的支持。最大似然法与贝叶斯分析的结果都支持触手冠动物为多系群，却不支持腕足动物门与帚虫动物门亲缘关系接近构成一个单系群的观点。

海洋聚磷菌Halomonas YSR-3的除磷特性研究

本论文报道从海洋中分离到的一株聚磷菌的分离、鉴定、在系统发育中的地位、除磷特性、菌体内多磷酸盐颗粒的研究、D-海因酶和核苷二磷酸激酶基因的克隆及序列分析，为海水系统的生物除磷提供部分基础资料。 从黄海海域分离到聚磷菌Halomonas sp. YSR-3，菌体呈杆状，大小为3.5 μm×1 μm，革兰氏阴性，好氧生长，能运动。透射电镜观察发现，菌体内有致密颗粒。经DAPI染色确定该致密颗粒是多磷酸盐，亦可称为异染粒、迂回体。16S rDNA鉴定结果表明，YSR-3与Halomonas属中的marine bacterium B5-7有较高的同源性，相似值99%。YSR-3的生理生化特性：对氯霉素和卡那霉素敏感；淀粉水解呈阳性；反硝化和几丁质降解呈阴性；能将葡萄糖作为唯一碳源和能源。 对YSR-3的培养条件进行优化。以海水2216培养基、24 ℃、180 rpm、pH 6.5的条件培养，更利于菌体生长和菌体内多磷酸盐的形成。 对YSR-3的除磷特性进行研究。无磷培养时，菌体不能生长；用磷酸钾盐作为磷源时，菌体生长较好，形成多磷酸盐的菌体比例较高；较适合YSR-3菌体生长和多磷酸盐形成的磷源是KH2PO4，较适磷浓度为1.5 mmol/L。pH的变化影响菌株的生长、多磷酸盐形成和除磷效果。pH值为5时，菌体的数量几乎不增加，体内多磷酸盐和培养基中磷含量变化不大；pH值为6、7和8时，菌体生长良好，95%以上的菌体内形成多磷酸盐，培养基中磷含量明显下降。YSR-3在不同培养基中除磷量和除磷率不同。在高磷培养基中除磷量为0.7 mmol/L(磷含量由1.84 mmol/L降到1.14 mmol/L)，除磷率为37.5%；在低磷培养基中除磷量为0.02 mmol/L(磷含量由0.028 mmol/L降到0.008 mmol/L)，除磷率为72.2%。 以海洋聚磷菌Halomonas sp. YSR-3的总DNA为模板，用PCR法扩增D-海因酶基因和核苷二磷酸激酶基因，将扩增片段克隆到pGM-T载体，转化E.coli TOP10菌株，经蓝白斑筛选、菌落PCR得到阳性克隆，测序后对序列进行Blast比对分析。得到的D-海因酶基因序列长度为1510 bp，与Pseudomonas entomophila L48的海因酶基因序列的相似性为77%。翻译后的序列与Pseudomonas fluorescens Pf-5，Marinomonas sp. MED121，Burkholderia vietnamiensis G4的海因酶蛋白序列相似性分别为75%，73%，70%。得到的核苷二磷酸激酶基因序列长度为420bp，翻译后的序列与Loktanella vestfoldensis SKA53，Jannaschia sp. CCS1，Roseobacter sp. CCS2的核苷二磷酸激酶蛋白序列相似性分别为89%，86%，85%。 聚磷菌能将外界环境中的磷吸收到体内，并以多磷酸盐的形式储存。多磷酸盐对于细胞的生存和生长有很重要的作用，但目前对于多磷酸盐的形成过程以及过程调控还不是很清楚。在今后可以通过构建高效表达的重组菌，提高与除磷相关的酶的纯度及活性。同时可以将相关酶的基因进行突变，对基因表达的调控以及酶的代谢以及功能结构等多方面进行基础研究，使聚磷菌在生物除磷中得到广泛应用。

冲绳海槽黑潮流域近4万年以来的古海洋环境演化

本文采用取自冲绳海槽的91个站位的表层样品和2个柱状岩芯，通过微体古生物有孔虫分析、氧碳同位素测试、AMS~(14)C测年、沉积物粒度和地球化学分析，探讨了现代生物群落、表层沉积物氧同位素与现代海洋环境之间的关系，进而对冲绳海槽区域近4万年来的古海洋环境和古黑潮演化进行了详细的研究。表层沉积物中的浮游有孔虫氧同位素与现代海洋环境之间的关系密切，浮游有孔虫从G.ruber到G.sacculifer到N.dutertrei其δ~(18)O值由轻变重，表明三种有孔虫其生活水层依次由浅到深。在横穿海槽的剖面上浮游有孔虫δ~(18)O在近陆端因受冲淡小影响较强而变轻，而在东侧站位，受黑潮暖流或其支流的影响氧同位素同样有变轻的趋势。N. dutertrei和G.ruber的氧同位素差值表明了冲绳海槽北部区域黑潮支流对表层水体的影响要大于次表层水体，而在冲绳海槽南部区域，黑潮暖流对次表层水体有相对较强的影响。冲绳海槽南部表层沉积物中的浮游有孔虫整体上属于赤道区组合，溶解作用对该区的浮游有孔虫群落有显的影响，冲绳海槽北部区浮游有孔虫组合对具有温带群落的特征。浮游有孔虫分布与海洋环境密切相关，南北区的浮游有孔虫分布都明显受暖流的影响，在暖流的主流轴处浮游有孔虫丰度通常较高。冲绳海槽具有相对较浅的碳酸盐溶跃面，浮游有孔虫丰度和底栖有孔虫深水胶结壳的含量都进一步表明了该区碳酸钙溶跃面大约在1700 m水深左右，比开放大洋明显要浅得多。表层沉积物中的底栖有孔虫主要受水深和水团等因素的制约。水深制约着有孔虫属种的分带，也影响底栖有孔虫的组合。根据Q型因子分析，冲绳海槽南部表层沉积物中的底栖有孔虫从陆架连缘到海槽底部可以划分为5个特定的组合，分别对应黑潮表层水和次层水影响环境、黑潮中层水影响环境、溶跃面以上的黑潮深层水影响环境、黑潮底层水团影响环境和溶解作用较强的槽底环境；北部区的底栖有孔虫群落反映了四个组合，分别代表了陆架混合水团影响环境、黑潮暖流中层水影响环境、冷涡沉积和上升流区影响环境以及对马暖流水团影响下的环境。以氧同位素曲线为基础，结合AMS~(14)C测年和生物地层学对柱状岩芯进行了地层划分和对比，E107孔记录了冰消期以来大约15,000 a来的古环境演化记录，具有较高的沉积速率，DOC－42孔保存在主要是末冰期中40－10ka BP期间的古环境沉积记录，沉积物记录的分辨率相对较低。浮游有孔虫有碎壳比和底栖有孔虫深海胶结壳含量表明了现代冲绳海槽的浅溶跃面是大约最近2000 a BP才开始突然变浅形成的，碳酸盐的溶解作用从冰消期到现在逐增强。冲绳海槽南部E107孔的底栖有孔虫组合把映了15,000 a来的底层水团具有两种完全不同的营养状况，约6500 a BP以前有机质通量较高，6500 a BP以后有机质通量则明显降低。DOC－42孔的底栖有孔虫组合反映该区约4万年以来的底部水团演化主要受有机质通量和氧含量的共同制约，氧同位素3期主要为高有机质通量的沉积环境，伴随有氧含量水平的较大波动；氧同位素2期有机质通量有所降低，氧含量整体为中等水平；氧同位素1期早期义部水体则较高氧含量为主。浮游有孔虫温跃层转换函数反映了冲绳海槽中部的温跃层在约13100 a BP有一个明显的变化，在这之前产温跃层深度较浅，平均89 m，而在该时间以后，温跃层平均深度变为166 m。此外在160 cm处和100 cm的温跃层深度的两次明显的降低，分别对应于新仙女木事件和黑潮暖流的重新入侵，表明这两个事件导致了海洋上层水体结构的突然变化。冲绳海槽北部浮游有孔虫转换函数古温度和浮游有孔虫的低温、低盐特征种反映了在氧同位素3期早期约40000a BP和氧同位素2期间存在两个明显的低温、低盐阶段，可能与沿岸水在该期间加强有关。其中氧同位素3期早期的表层海水古水温比末次冰期还要低，反映了区域海洋环境的重大变化。冲绳海槽南部E107孔的沉积物粒度、地球化学特征、黑潮特征指示种、表层古水温以及底层水团的性质在6500 a BP左右发生了重大的改变，与冲绳海槽南部的其他岩芯反映的古环境化基本一致，表明了南部海槽在6500 a BP前后古黑潮流径发生了重大变化。而冲绳海槽北部区域2万年以来的古环境则与南部有明显差异，总结前人对冲绳海槽古黑潮流径的研究，笔者对未次冰盛期古黑潮流径提出了新的推测。