Effects of ammonium on growth, nitrogen and carbohydrate metabolism of Potamogeton maackianus A. Benn

Growth, nitrogen and carbohydrate metabolism in relation to eutrophication were studied for a submerged plant Potamogeton maackianus, a species common in East Asian shallow lakes. The plants were grown in six NH4+-N concentrations (0.05, 0.50, 1.00, 3.50, 5.00 and 10.00 mg/L) for six days. NH4+-N levels in excess of 0.50 mg/L inhibited the plant growth. The relationships between external NH4+-N availability and total nitrogen (TN), protein-N, free amino acid-N (FAA-N) and NH4+-N in plant tissues, respectively, conformed to a logarithmic model suggesting that a feedback inhibition mechanism may exist for ammonium uptake. The response of starch to NH4+-N was fitted with a negative, logarithmic curve. Detailed analysis revealed that the influx NH4+-N had been efficiently incorporated into organic-N and eventually stored as protein at the expense of starch accumulation. These data suggest that this species may be able to tolerate high levels of ammonium when dissolved oxygen is sufficient.

Phylogenetic relationships of Cyprinidae (Teleostei : Cypriniformes) inferred from the partial S6K1 gene sequences and implication of indel sites in intron 1

The family Cyprinidae is widely distributed in East Asia, and has the important phylogenetic significance in the fish evolution. In this study, the 5' end partial sequences (containing exon 1, exon 2 and indel 1) of S6K1 gene were obtained from 30 representative species in Cyprinidae and outgroup using PCR amplification and sequencing. The phylogenetic relationships of Cyprinidae were reconstructed with neighbor joining (NJ), maximum parsimony (MP), maximum likelihood (ML), and Bayesian methods. Myxocyprinus asiaticus (Catostomidae) was assigned to the outgroup taxon. Similar phylogenetic relationships within the family Cyprinidae were achieved with the four analyses. Leuciscini and Barbini were monophyletic lineages respectively with the high nodal supports. Leuciscini comprises Hypophthalmichthyinae, Xenocyprinae, Cultrinae, Gobioninae, Acheilognathinae and East Asian species of Leuciscinae and Danioninae. Monophyly of East Asian clade was supported with high nodal support. Barbini comprises Schizothoracinae, Barbinae, Cyprininae and Labeoninae. The monophyletic lineage consisting of Danio rerio, D. myersi, and Rasbora trilineata was basal in the tree. In addition, the large fragment indels in intron 1 were analyzed to improve the understanding of Cyprinidae relationships. The results showed that the large fragment indels were correlated with the relations among species. Some conserved regions in intron 1 were thought to be involved in the functional regulation. However, no correlation was found between sequence variations and species characteristic size.

Loess magnetic properties in the Ili Basin and their correlation with the Chinese Loess Plateau

     Over the past two decades, magnetoclimatological studies of loess-paleosol sequences in the Chinese Loess Plateau (CLP) have made outstanding achievements, which greatly promote the understanding of East Asian paleomonsoon evolution, inland aridification of Asia, and past global climate changes. Loess magnetic properties of the CLP have been well studied. In contrast, loess magnetic properties from outside the CLP in China have not been fully understood. We have little knowledge about the magnetic properties of loess in the Ili Basin, an intermontane depression of the Tianshan (or Tien Shan) Mountains. Here, we present the results of rock magnetic measurements of the Ili loess including mass magnetic susceptibility (χ) and anhysteretic remanent magnetization (ARM), high/low temperature dependence of susceptibility (TDS) and hysteresis, as well as X-ray diffraction (XRD) for mineral analysis. Based on the comparison with loess-paleosol sequences in the CLP (hereafter referred to as the Chinese loess), we discuss the possible magnetic susceptibility enhancement mechanism of the Ili loess. The results show that 1) the total magnetic mineral concentration of the Ili loess is far lower than that of the Chinese loess, though they have similar magnetic mineral compositions. The ferrimagnetic minerals in the Ili loess are magnetite and maghemite, and the antiferromagnetic mineral is hematite; XRD analysis also identifies the presence of ilmenite. The ratio of maghemite is lower in the Ili loess than in the Chinese loess, but the ratios of magnetite and hematite are higher in the Ili loess than in the Chinese loess. 2) The granularity of magnetic minerals in the Ili loess, dominated by pseudo-single domain (PSD) and multi-domain (MD) grains, is generally much coarser than that of the Chinese loess. Ultrafine pedogenically-produced magnetic grains have a very limited contribution to the susceptibility enhancement. Rather, PSD and MD particles of magnetite and maghemite are the main contributors to the enhancement of susceptibility in the Ili loess. 3) The susceptibility enhancement mechanism for the Ili loess is complicated and superimposes both a wind velocity/vigor model (Alaskan or Siberian model) and the in situ ultrafine grain pedogenic model; the former might play an important role in the Ili loess. 4) Magnetic susceptibility enhancements of the Ili loess are related not only to the eolian input of the source area, but also to the local climate, landform, and geological background. Therefore, great care should be taken when reconstructing paleoclimate using magnetic susceptibility data from the Ili loess.

Molecular determination of oxytetracycline-resistant bacteria and their resistance genes from mariculture environments of China

Aims: To assess the diversity of antibiotic-resistant bacteria and their resistance genes in typical maricultural environments. Methods nand Results: Multidrug-resistant bacteria and resistance genes from a mariculture farm of China were analysed via cultivation and polymerase chain reaction (PCR) methods. Oxytetracycline (OTC)-resistant bacteria were abundant in both abalone and turbot rearing waters, accounting for 3.7% and 9.9% of the culturable microbes. Multidrug resistance was common, with simultaneous resistance to OTC, chloramphenicol and ampicillin the most common resistance phenotype. 16S rDNA sequence analyses indicate that the typical resistant isolates belonged to marine Vibrio, Pseudoalteromonas or Alteromonas species, with resistance most common in Vibrio splendidus isolates. For OTC resistance, tet(A), tet(B) and tet(M) genes were detected in some multidrug-resistant isolates, with tet(D) being the most common molecular determinant. For chloramphenicol resistance, cat II was common, and floR was also detected, especially in marine Pseudoalteromonas strains. Conclusions: There is the risk of multidrug-resistant bacteria contamination in mariculture environments and marine Vibrio and Pseudoalteromonas species serve as reservoirs of specific antibiotic resistance determinants. Significance and Impact of the Study: This paper and similar findings from Korea and Japan indicate the potential for widespread distribution of antibiotic resistance genes in mariculture environments from the East Asian region of the world.

Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea

A 700-year record (1.0-1.5 a resolution) of the East Asian winter monsoon (EAWM), based on grain-size analysis and AMS(14)C dating of Core EC2005 from the inner-shelf mud wedge of the East China Sea (ECS), was compared with the Dongge stalagmite delta O-18 record during the mid-Holocene. The upper muddy section of Core EC2005 has been formed mainly by suspended sediments derived from the Changjiang (Yangtze) River mouth since 7.3 ka BP. High precipitation and a strengthened EAWM might have played key roles in the high sedimentation rate (1 324-1 986 cm/ka) between 5.9-5.2 ka BP. The EAWM strengthened when the Asian summer monsoon weakened, especially around 5 500 a BP, which corresponded to a worldwide cold event. The EAWM during the mid-Holocene shows statistically significant solar periodicities at 62 and 11 a. The 5 500 a BP cold event might be resulted from orbital forcing and changes in solar activity.

Heinrich event imprints in the Okinawa Trough: evidence from oxygen isotope and planktonic foraminifera

Planktonic foraminiferal faunas, oxygen isotope and modern analog technique sea surface temperature records were obtained in piston core DGKS9603 (28degrees08.869'N, 127degrees16.238'E, water depth 1100 in) collected from the middle Okinawa Trough. During the last glaciation, four cold events were identified and correlate Heinrich events (HE) H2-5 of the last 45 ka. During the last deglaciation, core DGKS9603 has begun to be influenced by the Kuroshio since about 16 cal ka BP. Three weakenings of this warm current occurred at about 2.8-5.3, 11.4 and 15.5 cal ka BP respectively. Among the three fluctuations, the oldest one is synchronous with HE1 and could be a response to the strong cooling observed in the North Atlantic Ocean. The fluctuation occurring at about 11.4 cal ka ago corresponds to the Younger Dryas within the age error bars. Our observations provide new evidence that the HEs documented from Greenland and the northern North Atlantic had a global climatic impact. Changes in the intensity of the East Asian monsoon could be the main mechanism responsible for the paleoccanographic variations observed in the Okinawa Trough. (C) 2001 Elsevier Science B.V. All rights reserved.

The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP

Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling factor.

Responses of summertime extreme wave heights to local climate variations in the East China Sea

We detected the responses of summertime extreme wave heights (H-top10, average of the highest 10% of significant wave heights in June, July and August) to local climate variations in the East China Sea by applying an empirical orthogonal function analysis to Htop10 derived from the WAVEWATCH- III wave model driven by 6 hourly sea surface wind fields from ERA-40 reanalysis over the period 1958-2002. Decreases in H-top10 in the northern East China Sea ( Yellow Sea) correspond to attenuation of the East Asian Summer Monsoon, while increases in the south are primarily due to enhancement of tropical cyclone activities in the western North Pacific.

Equatorial pacific SSTA-related decadal variations of potential predictability of ENSO and interannual climate

Based on analysis of NCEP reanalysis data and SST indices of the recent 50 years, decadal changes of the potential predictability of ENSO and interannual climate anomalies were investigated. Autocorrelation of Nino3 SST anomalies (SSTA) and correlation between atmospheric anomalies fields and Nino3 SSTA exhibit obvious variation in different decades, which indicates that Nino3 SSTA-related potential predictability of ENSO and interannual climate anomalies has significant decadal changes. Time around 1977 is not only a shift point of climate on the interdecadal time scale but also a catastrophe point of potential predictability of ENSO and interannual climate. As a whole, ENSO and the PNA pattern in boreal winter are more predictable in 1980s than in 1960s and 1970s, while the Nino3 SSTA-related potential predictability of the Indian monsoon and the East Asian Monsoon is lower in 1980s than in 1960s and 1970s.

东亚—北美间断分布类群的分子生物地理学研究—以莲科和菖蒲科为例

在洲际间断生物地理学研究中，东亚—北美间断分布类群的分子生物地理学研究一直是关注和研究的热点。在本论文中我们选取了水生和半水生的植物代表类群，莲科（Nelumbonaceae）和菖蒲科（Acoraceae）作为研究对象，通过来自叶绿体、线粒体和核基因组的DNA 序列分析和微卫星分析，一方面探讨莲科的系统位置、揭示其间断地理格局的形成过程、重建菖蒲科的系统发育及其地理格局的形成过程的同时，另一方面，在总结前人研究成果的基础上，总结东亚—北美间断分布的基本特点。主要成果总结如下。 1. 菖蒲科的系统发育和分子生物地理学 菖蒲科仅含一属，菖蒲属（Acorus），共5 种。其中北美菖蒲（A. americanus） 分布于北美，其余4 种（A. calamus, A. gramineus, A. tatarinowii and A. rumphianus） 分布于亚洲的东部和南部。北美菖蒲和菖蒲（A. calamus）叶片中间具有明显的中肋；其余3 种不具有明显的中肋。本论文的19 份材料包含了4 个种，（不含较狭域分布的长苞菖蒲A. rumphianus），利用4 个叶绿体基因片段（trnL-F, psbA-trnH, rps16-trnK, rbcL）和1 个核基因片段（ITS）的序列重建菖蒲属的系统发育。结果表明（1）具有中肋和不具中肋的物种各自聚为一支；（2）具有中肋的菖蒲和北美菖蒲亲缘关系最近，构成东亚—北美间断种对关系；（3）在不具有中肋的一支内部，来自台湾的材料与其它材料差异最大，其余的材料也明显的分为了两类。基于rbcL 序列，使用松散分子钟模型、贝叶斯算法估算菖蒲属起源时间约为135.17 百万年（mya），菖蒲和北美菖蒲的间断分歧时间约为3.72mya。该结果支持菖蒲属为古老的单子叶植物，但东亚—北美间断物种分化时间较年轻。我们推测间断的种对可能通过白令陆桥，从东亚扩散到了北美。 2. 莲科的系统位置和分子生物地理学 莲科仅含一属，莲属（Nelumbo），两个种莲（N. nucifera）和美洲黄莲（N. lutea），间断分布于东亚、澳大利亚北部和北美东部。莲科的系统位置在形态和分子证据不一致。本论文使用了核基因18S rDNA、26S rDNA，叶绿体基因atpB、rbcL，线粒体基因NAD1 的序列重新构建莲科的系统位置并进行了分化时间推算。结果为：（1）叶绿体和核基因构建的严格一致树的拓扑结构不一致，叶绿体数据支持莲科和山龙眼科、悬铃木科具有较近的亲缘关系，核基因数据显示莲科位于真双子叶植物的基部；（2）5 个基因片段的合并分析结果显示，莲科与山龙眼科、悬铃木科聚为一支但支持率不高；（3）基于核基因、叶绿体和5 个基因的分别合并数据，使用松散分子钟模型、贝叶斯算法估算莲科起源时间分别为，113.13 、109.38 和110.35mya ，两个间断物种的分化时间为，3.77、4.34、5.85mya；（4）根据间断的时间和两个物种的遗传差异程度，现存的两个物种应是来自于东亚或北美的冰期残遗，而不是来自于两个大陆祖先种的独立进化后裔。 3. 莲的分子谱系地理学研究 我们采集了37 份莲的材料，10 份美洲黄莲的材料，代表了两者的主要分布区。我们选取了叶绿体基因（trnL-trnF, trnS-trnG, petB-petD 和psbA-trnH），线粒体基因COX1，以及11 个微卫星位点进行莲的分子谱系地理研究。DNA 序列显示莲和美洲黄莲均具有很低的遗传多样性；微卫星数据揭示了稍高于DNA 序列的遗传多样性。两物种相比，美洲黄莲的多样性较高。基于微卫星数据的遗传结构分析表明，莲存在明显的3 个地理分化区域，这三个区域的遗传分化显著（FST=0.542），说明莲远距离群体间基因交流有限。基于DNA 序列和微卫星数据的单倍型地理分布关系，我们推测东南亚地区是莲的避难所或冰期残遗区，冰期后群体分别向西和向北扩张。 4. 东亚—北美间断分布的一般特点 （1）东亚—北美东部间断分歧时间范围较长，从始新世中期甚至更早一直持续到1mya 左右；东亚—北美西部间断类群分化时间跨度相对小，集中在中新世时期；东亚—整个北美间断分化时间与东亚—北美东部间断类群一样经历较长时间；草本类群晚于木本类群形成间断分布式样，洲际间断分化时间与类群的起源时间并无相关性。（2）东亚与北美间断分布类群的起源地因类群而异。（3） 东亚与北美间断分布类群扩散方向呈不确定性。（4）东亚与北美间断类群扩散有三条可能的路径，即大西洋陆桥、白令陆桥和南半球跨洋长距离传播。