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.

HPLC-APCI-MS determination of free fatty acids in Tibet folk medicine Lomatogonium rotatum with fluorescence detection and mass spectrometric identification

A simple and sensitive method for the determination of free fatty acids (FFAs) using acridone-9-ethyl-p-toluenesulfonate (AETS) as a fluorescence derivatization reagent by high performance liquid chromatography (HPLC) has been developed. Free fatty acid derivatives were separated on an Eclipse XDB-C-8 column with a good baseline resolution and detected with the fluorescence of which excitation and emission wavelengths of derivatives were set at lambda(ex) 404 and lambda(em) 440 nm, respectively. Identification of 19 fatty acid derivatives was carried out by online post-column mass spectrometry with an atmospheric pressure chemical ionization (APCI) source under positive-ion detection mode. Nineteen FFAs from the extract of Lomatogonium rotatum are sensitively determined. The results indicate that the plant Lomatogonium rotatum is enriched with an abundance of FFAs and FFAs of higher contents, which mainly focus on even carbon atoms, C-14, C-16, and C-18. The validation of the method including linearity, repeatability, and detection limits was examined. Most linear correlation coefficients for fatty acid derivatives are > 0.9989, and detection limits (at signal-to-noise of 3: 1) are 12.3-43.7 fmol. The relative standard deviations (RSDs) of the peak areas and retention times for 19 FFAs standards are < 2.24% and 0.45%, respectively. The established method is rapid and reproducible for the separation determination of FFAs from the extract of Lomatogonium rotatum with satisfactory results.

渤海湾地区末次冰期古环境

The loess-paleosol sequence in China is one of the best archives for studying paleoenvironmental and paleoclimatic processes. The loess deposits in the coast of the Bohai Sea are suitable for the study of aridification in the northern China during glacial periods (fig.2-1). In this paper, stratigraphy was correlated by using magnetic susceptibility, grain size, and thermoluminence (TL) and accelerater mass spectrometer (AMS) ~(14)C ages. Based on the loess records, an interpretation has been made for paleoenvironmental changes on the coast of the Bohai Sea during the last glacials. The results of magnetic susceptibility, grain size, biostratigraphy, TL and ~(14)C dating, suggest that the loess-paleosol sequence in the coast of the Bohai Sea is discontinuous. The loess deposits correlated with the marine δ~(18)O stage 2 are usually absent in some profiles. Also, the thickness of the loess deposits in the same period varied significantly in different sections. In the coast of the Bohai Sea, the higher magnetic susceptibility corresponds to the finer grain size, consistent with the results of the Loess Plateau. It is indicated that the changes in magnetic susceptibility and grain size may record the paleoclimatic fluctuations of the last glacial. Although the loess deposits during the last glacial have been slightly altered by slope runoff, they have still remained main characters as the representative loess deposits of the Loess Plateau. During the last glacial, the less accumulation rate in the coast of the Bohai Sea is similar to that of the desert-loess transition zone in the northwestern Loess Plateau, and the all section contain high concentrations of sand (>60μm), indicate that the aridification in the Bohai Sea occurred during the glacial. But the changes in sand content of loess deposits along a north-south transect of the Bohai Sea and the changes of magnetic susceptibility implicate that desertification might not occur in the shelf of the Bohai Sea during the last glacial. The frequent fluctuations of summer monsoon during the marine δ~(18)O stage 4 are demonstrated by magnetic susceptibility, frequency-dependent susceptibility and the abundance of foraminifera. 46 genera, 71 species of foraminifera were identified from 138 loess samples. Almost all of the foraminifera are present in the last glacial loess, but the distribution patterns of foraminifera show significant temporal changes. The results of magnetic susceptibility, grain size and XRD indicate that not only sea-level changes had influences on foraminifera abundance, but also variations in sediment flux by rivers when sea-level drops might control the abundance of foraminifera. In addition, the diversity and exquitability of the foraminifera suggest that the frequent fluctuations of foraminifera fossil abundance during the marine δ~(18)O stages could be partly attributed to leaching. In summary, the changes in foraminifera of abundance related to the paleoclimatic variations, and the aridification extends to the coast of the eastern China during the last glacial.

释光测年实验室的建立与沉积物释光测年技术研究

The main research projects reported in this paper are the establishment of a luminescence (OSL/TL) dating laboratory in The Institute of Geology and Geophysics, CAS, and studies on OSL dating technique and protocol of sediments from North China. These projects have been suggested in order to fit in with the needs of research developments in environmental changes, in particular the aridity and desertification in North China. A new luminescence dating laboratory in which there are a Rise TL/OSL-DA-15B/C reader with Sr-90 beta source, a set of Little More Tape 9022 alpha and beta irradiators, three set of Daybreak 583 intelligent alpha counters and sample preparation system has been set up in the Institute in June 2001. The courses of the establishment of a new laboratory involved a series of technical works, besides making a suitable choice of the equipment, as follows: installing and testing TL/OSL reader, calibrating the dose rate of the beta and alpha sources in the irradiators with the standard sources, testing and calibrating the count rates of the thick source alpha counting in the alpha counters with a standard sample, and then dating of the know age samples to check and examine the OSL/TL dating system. All data obtained from above calibrations and tests show that the established OSL/TL system, including the used equipment in it, can be used to determine age of the geological and archaeological samples with an error of equivalent dose (De) of less than 5%. The OSL dates of several sediment samples obtained from the system are good agreement with those from the OSL dating laboratory in Hong Kong University and ~(14)C dates within 1 - 2 standard deviations. The studies on OSL dating technique and protocol of sediment samples being in progress involve the De determinations with single aliquot regeneration (SAR) (Murray and Wintle, 2000) of the coarse grain quartz from sand dune samples and comparison of the De determinations obtained from SAR with those measured by using multiple aliquot regeneration of loess fine grains. The preliminary results from these research works are shown as follows. The very low natural equivalent dose (De) of about 0.012 - 0.03 Gy, corresponding age of less than 10 years, for BLSL (blue light stimulated luminescence) of the coarse grain quartz from modern sand dune samples in Horqin sand fields has been determined with both the SAR and multiple aliquot regeneration (MAR) techniques. This imply that the BLSL signal zeroing of the quartz could be reached before burying of the sand in Horqin sand fields. The De values and ages of the coarse grain quartz measured with SAR protocol are in good agreement with those obtained from multiple aliquot technique for the modern sand dune samples, but the errors of De from the MAR is greater than those from the SAR. This may imply that the higher precision of age determination for younger sand dune samples could be achieved with the SAR of coarse grain quartz. The MAR combining with "Australian Slide method" may be a perfect choice for De measurements of loess fine grain samples on the basis of analysis of De values obtained from the SAR and from the MAR. The former can be employed to obtain a reliable age estimate of loess sample as older as approximately SO ka BR There is a great difference between De determinations from the (post-IR) OSL of the SAR (Roberts and Wintle, 2001) and those from independent or expected estimates for the older samples. However, the age estimates obtained from the (post-IR) OSL of the SAR are mostly closed to the independent age determinations for the younger (age less than 10 ka) fine grain samples. It may be suggested that the (post-IR) OSL of the SAR protocol of the fine grain fraction would be a suitable choice to dating of the younger samples, but may be unsuitable for the older samples.

黄东海及朝鲜海峡冰后期陆架沉积物的环境磁学研究

There are four chapters in this dissertation. The first chapter briefly synthesizes the basic theories, methods and present-day applying situation of environmental magnetism. The second chapter probes into the magnetic mineral diagenesis in the post-glacial muddy sediments from the southeastern South Yellow Sea and its response to marine environmental changes, using the muddy sediment of Core YSDP103 formed in the shelf since about 13 ka BP. The third chapter illustrates the high-resolution early diagenetic processes by investigating the rapidly deposited muddy sediments during the last 6 ka in Cores SSDP-102 and SSDP-103 from the near-shore shelf of Korea Strait. The fourth chapter presents the results of detailed rock magnetic investigation of the surface sediments from the fine-grained depositional area on the outer shelf of the East China Sea in an attempt to provide environmental magnetic evidence for the provenance of the fine-grained deposit. Core YSDP103 was retrieved in the muddy deposit under the cold eddy of the southeastern South Yellow Sea, and the uppermost 29.79 m core represents the muddy sediments formed in the shelf since about 13 ka BP. The lower part from 29.79 to 13.35 m, called Unit A2, was deposited during the period from the post-glacial transgression to the middle Holocene (at about 6 ~(14)C ka BP) when the rising sea level reached its maximum, while the upper part above 13.35 m (called Unit Al) was deposited in a cold eddy associated with the formation of the Yellow Sea Warm Current just after the peak of post-glacial sea level rise. For the the uppermost 29.79 m core, detailed investigation of rock-magnetic properties and analyses of grain sizes and geochemistry were made. The experimental results indicate that the magnetic mineralogy of the core is dominated by magnetite, maghemite and hematite and that, except for the uppermost 2.35 m, the magnetic minerals were subject to reductive diagenesis leading to significant decline of magnetic mineral content and the proportion of low-coercivity component. More importantly, ferrimagnetic iron sulphide (greigite) is found in Unit A2 but absent in Unit Al, suggesting the control of marine environmental conditions on the magnetic mineral diagenesis. Magnetic parameters show abrupt changes across the boundary between the Unit Al and A2, which reflects a co-effect of environmental conditions and primary magnetic components of the sediments on the diagenesis. Alternating zones of high and low magnetic parameters are observed in Unit A2 of Core YSDP103, which is presumably due to periodic changes of the concentration and/or grain size of magnetic minerals carried into the study area. Cores SSDP-102 and SSDP-103, two studied sediment cores from the Korea Strait contain mud sequences (14 m and 32.62 m in thickness) that were deposited during the last 6,000 years. Analyses of grain sizes and geochemistry of the cores have demonstrated that the sediments have uniform lithology and geochemical properties, however, marked down-core changes in magnetic properties suggest that diagenesis has significantly impacted the magnetic properties. An expanded view of early diagenetic reactions that affect magnetic mineral assemblages is evident in these rapidly deposited continental shelf sediments compared to deep-sea sediments. The studied sediments can be divided into four descending intervals, based on magnetic property variations. Interval 1 is least affected by diagenesis and has the highest concentrations of detrital magnetite and hematite, and the lowest solid-phase sulfur contents. Interval 2 is characterized by the presence of paramagnetic pyrite and sharply decreasing magnetite and hematite concentrations, which suggest active reductive dissolution of detrital magnetic minerals, the absolute minimum abundance of magnetite is reached at the end of this interval. Interval 3 is marked by a progressive loss of hematite with depth, and at the base of this interval, 82% to 88% of the hematite component was depleted and the bulk magnetic mineral concentration was reduced to the lowest value in the entire studied mud section. Interval 4 has an increasing down-core enhancement of authigenic greigite, which is interpreted to have formed due to arrested pyritization resulting from consumption of pore water sulfate with depth. This is the first clear demonstration from an active depositional environment for a delay of thousands of years for acquisition of a magnetization carried by greigite. This detailed view of diagenetic processes in continental shelf sediments suggests that studies of geomagnetic field behavior from such sediments should be conducted with care. Paleoceanographic and paleoclimatic studies based on the magnetic properties of shelf sediments with high sedimentation rates like those in the Korea Strait are also unlikely to provide a meaningful signature associated with syn-depositional environmental processes. The rock magnetic properties of the surface sediments from the fine-grained depositional area on the outer shelf of the East China Sea, an area surrounded by sands, are investigated with a view to providing information on the sediment provenance. Multiple magnetic parameters such as magnetic susceptibility (%), anhysteretic remanent magnetization (ARM), saturation rernanent magnetization (SIRM), coercivities of SIRM (Her), and S ratios (relative abundance of low-coercivity magnetic minerals) are measured for all 179 surface samples, and partial representative samples are examined for their magnetic hysteresis parameters, temperature-dependence of magnetic susceptibility and x-ray diffraction spectra. Our research indicates that the magnetic mineralogy is dominated by magnetite with a small amount of hematite and is primarily of pseudo-single domain (PSD) to multidomain (MD) nature with a detrital origin. In the surface sediments, the granulometry of magnetic fractions is basically independent of grain sizes of the sediment containing the magnetic grains, and the composition of magnetic minerals remains almost homogeneous, that is, with a relatively constant ratio of low to high coercivity fraction throughout the area. The magnetic concentration in the study area generally decreases to the east or southeast accompanied by magnetic-particle fining to the east or to the northeast. The geographic pattern of magnetic properties is most reasonably explained by a major source of sediment jointly from the erosion of the old Huanghe River deposit and the discharge of the Changjiang River. The rock magnetic data facilitate understanding of the transport mechanism of fine-grained sediments in the outer shelf of the East China Sea.

外源草酸对采后果实的保鲜效应及其生理机理研究

本文以桃(Prunus persica L. cv. Bayuecui.)栽培种‘八月脆’和芒果（Mangifera indica L.）栽培种‘圣心’为材料，研究外源草酸对采后果实的生理生化效应及其作用机理，为果实贮藏保鲜提供新方法。采后桃果实用1、5 mM的草酸溶液浸果10 min，以浸水10 min为对照，然后在常温下贮藏，测定果实在贮藏期间对草酸处理的一些生理生化反应。芒果经采后杀菌剂（post- P）、采后草酸（post-OA）、采前＋采后草酸（pre-OA + post-OA）、采前Ca ＋ 采后草酸处理（pre-Ca + post-OA）处理，以采后浸水为对照，然后分别将果实在常温(25 C)、低温（14 C）和控制性气调（3% CO2 + 2% O2 ，14 ± 1 C）下贮藏，测定草酸处理对芒果的成熟进程、病情发展及其相关生理指标的影响。研究结果表明如下： 1．与对照相比，草酸处理的桃果实在贮藏期间果实的电解质渗漏量和呼吸速率降低、果实硬度高、果实的抗氧化酶（超氧化物岐化酶、SOD;过氧化物酶，POD;过氧化氢酶、CAT;抗坏血酸过氧化物酶、APX）和多酚氧化酶（PPO）活性提高、脂氧合酶（LOX）活性降低。同时，在贮藏后期，果实的活性氧自由基（ROS）产量（超氧阴离子、O2.;过氧化氢、H2O2)和丙二醛（MDA）含量降低。草酸的这些生理效应有利于保持膜的完整性和延缓桃果实的成熟;草酸诱导POD、SOD、PPO活性可能有助于提高采后果实的抗病性。 2．外源5、10 mM浓度的草酸（pH值中和或不中和）对芒果炭疽病原菌（Colletotrichum gloeosporioides）孢子萌发和菌丝生长均表现出显著的抑制作用。这种作用不仅与草酸降低培养基（PDA）的pH值相关，而且与草酸独特的化学特性相关。 3．在常温、低温和控制性气调贮藏下，采后草酸、采前 + 采后草酸、采前Ca + 采后草酸处理均能有效减缓芒果果实的软化速率，延缓芒果的成熟进程，降低芒果的病情指数，同时改善芒果成熟时的表皮着色，对果实完全后熟时的可溶性固形物（SSC）、可滴定酸（TA）含量、果肉口感均没有产生负面的影响。 4．草酸处理增强芒果细胞膜的稳定性，诱导提高芒果抗氧化酶活性，特别是提高果皮SOD、APX活性，降低LOX活性，以及降低果皮O2.、H2O2 和果肉H2O2含量，抑制采后果实的乙烯生物合成。这些生理生化效应与延缓芒果的成熟衰老和提高果实的抗病性相关。 5． 采后草酸、采前 + 采后草酸和采前Ca + 采后草酸处理表现出高效低廉、无毒无副作用、易操作等优点，是芒果采后贮藏保鲜的可供选、具有实际应用前景的新方法。

三种萝藦科植物中C21甾类成分的研究

　　本实验对三种萝藦科植物通光散(Marsdenia tenacissima)、黑水藤（Biondia insignis Tsiang）和徐长卿（Cynanchum Paniculatum）中的C21甾体化合物进行了研究。从通光散藤茎乙酸乙酯提取物的水解产物中，分离得到两类八个C21甾类甙元。经光谱鉴定，它们的结构分别为11α-O-(2-甲基)-丁酰基-12β-O-顺芷酰通光藤甙元乙（1），11α-O-乙酰基-12β-O-乙酰基通光藤甙元乙（2），11α-O-（2-甲基）-丁酰基-12β-O-乙酰基通光藤甙元乙(3), 11α-O-苯甲酰基-12β-O-乙酰基通光藤甙元乙(4)， 11α-O-顺芷酰基-12β-O-乙酰基通光藤甙元乙（5）11α-O-顺芷酰基-12β-O-顺芷酰基通光藤甙元乙（6），12β-O-乙酰基通光藤甙元甲（7）和12β-O-顺芷酰基通光藤甙元甲（8）。其中，化合物2和8为新化合物。从黑水藤乙醇提取物的水解产物中，分离得到了两个C21甾体化合物。经1D、2D NMR技术鉴定，分别为（3β，14β，15β，17β）-3, 14-二羟基-15，16-裂-孕甾-5-烯-15-醛-16-半缩醛-20-酮（1）和白前甙元C（2）。其中1为15，16-裂环的新骨架类型的C21甾体化合物，命名为黑水藤甙元甲。从采购于昆明、浙江、湖南三地药材市场的徐长卿的根及根茎中，分离得到了18个化合物（其中昆明徐长卿6个，浙江徐长卿9个，湖南徐长卿3个）。经光谱数据分析，这些化合物被鉴定为：cynapanoside-C (1), cynapanoside-A (2), 白前甙元B 3-O-β-D-磁嘛吡喃糖甙(3)，白前甙元C 3-O-β-D-葡萄吡喃糖基-(1 → 4)-α-L-2-脱氧洋地黄吡喃糖基-（1 → 4）-β-D-洋地黄吡喃糖基-（1 → 4）-β-D-夹竹吡喃糖甙（4），白前甙元C3-O-β-D-葡萄吡喃糖基-(1 → 4)-α-D-夹竹桃吡喃糖基-(1 → 4)-β-D-洋地黄吡喃糖基-(1 → 4)-β-D-夹竹桃吡喃糖甙（5），白前甙元C 3-O-β-D-葡萄吡喃糖基-（1 → 4）-β-D-葡萄吡喃糖基-（1 → 4）-α-D-夹竹桃吡喃糖基-（1 → 4）-β-D-洋地黄吡喃糖基-（1 → 4）-β-D-夹竹桃吡喃糖甙（6），cynatratoside-B (7)，cynatratoside-C (8);glaucoside A(9)，新白薇甙元B 3-O-β-L-磁嘛吡喃糖基-（1 → 4）-β-D-洋黄吡喃糖基-（1 → 4）-β-D-夹竹桃吡喃糖甙（10），白前甙元 A 3-O-α-L-磁嘛吡喃糖基-（1 → 4）-β-D-洋地黄吡喃糖基-（1 → 4）-β-D-磁嘛吡喃糖甙（11），白前甙元 B 3-O-α-L-磁糖基吡喃糖基-(1 → 4)-β-D-磁嘛吡喃糖基-(1 → 4)-β-D-磁嘛吡喃糖甙(12)，白前甙元D 3-O-α-L-磁嘛吡喃糖基（1 → 4）-β-D-洋地黄吡喃糖基-（1 → 4）-β-D-磁嘛吡喃糖甙（13），白前甙元 C 3-O-β-D-葡萄吡喃糖基-（1 → 4）-β-D-葡萄吡喃糖基-（1 → 4）-α-L-2-脱氧洋地黄吡喃糖基-（1 → 4）-β-D-磁嘛吡喃糖基-（1 → 4）-β-D-夹竹桃吡喃糖甙（14），白前甙元 C 3-O-β-D-葡萄吡喃糖基-（1 → 4）-β-D-葡萄吡喃糖基-（1 → 4）-α-L-磁嘛吡喃糖基-（1 → 4）-β-D-洋地黄吡喃糖基-（1 → 4）-β-D-夹竹桃吡喃糖甙（15），白前甙元 B 3-O-α-D-夹竹桃吡喃糖基-(1 → 4)-β-D-洋地黄吡喃糖基-（1 → 4）-β-D-磁嘛吡喃糖甙（16），白前甙元 D 3-O-α-D-夹竹桃吡喃糖基-(1 → 4)-β-D-洋地黄吡喃糖基-(1 → 4)-β-D-磁嘛吡喃糖甙(17)，白前甙元月B 3-O-α-L-磁嘛吡喃糖基-(1 → 4)-β-D-洋地黄吡喃糖基-(1 → 4)-β-D-磁嘛吡喃糖甙（18）。其中，化合物3-6，10-18为新化合物，10的甙元为一个新甙元，命名为新白薇甙无B。

青鼬(Martes flavigula)的核型研究

用G带,C带和银染技术对青鼬的核型观察分析结果:2n=40,双臂染色体16对,单臂染色体3对。X染色体为中着丝粒染色体。No.14同源染色体着丝点C带,一条呈阳性,另一条呈阴性。其余全部着丝点C带均显示强阳性。No.8染色体长臂显示C带阳性,No.11和No.13染色体的短臂具端位异染色质。仅有1对Ag-NORs,分布于No.15染色体的次缢痕部位,其短臂显示C带阳性,No.19染色体整个呈C带阳性。并同貂属其他种作了比较,初步探讨了青鼬的分类地位和亲缘关系。图版1表1参17

直链烷基苯磺酸盐在模拟水生态系统中转化和归宿的研究

用~(14)C标记直链烷基苯磺酸盐,(~(14)C-LAS),研究了在由塘泥、水草、鱼、螺蛳和溞构成的室内模拟水生态系统中,LAS的降解规律、在水生生物体内的积累分布及其与在水中降解之间的相互关系.

An evidence of defect gettering in GaN

The effect of Neon ion implantation on the structural and optical properties of MOCVD grown GaN was studied. X-ray diffraction and low temperature photoluminescence measurements were carried out on the implanted samples annealed at 900 degrees C. The peak at 3.41 eV exhibited an interesting behavior in as-grown and the implanted samples. Annealing has enhanced the intensity of this peak in as-grown samples, but suppressed in all the implanted samples. Capturing of defects by cavities during gettering process is interpreted as the reason for the observed behavior of this luminescence peak. Implantation dose of 5 x 10(15) ions/cm(2) caused the complete quenching of yellow band luminescence. (C) 2008 Elsevier B.V. All rights reserved.

二萜类生物碱和环糊精复合物的“软电离”质谱研究

随着基质辅助激光解吸／离(MALDI)和电喷雾电离(ESI)技术的发展，“软电离”质谱在一些新领域正在发挥着越来越大的作用。本论文运用这些新技术对二萜类生物碱、环糊精与氨基酸复合物和环糊精与肽复合物进行了系统地研究。具体研究结果如下：一、附子中二萜类生物碱的质谱研究使用基质辅助激光解吸飞行时间质谱仪(MALDI-TOF/MS)研究了附子提取物中C-19二萜类生物碱。实验结果表明：MALDI适合同时检测粗提物中多种生物碱，并且在分析速度和灵敏度方面明显优于其它方法。在附子甲醇提取物中检测到三类14种已知生物碱（单双酯型生物碱、阿替生型生物碱和脂类生物碱）和三种未知生物碱。同时还进行了生物碱萃取方法优化实验研究，并探讨了复方煎煮过程中成分-成分之间的相互作用。研究发现：生物碱的极性、碱性和毒性与生物碱C-8取代基相关，而且该基团在电离过程中容易形成中性碎片；在煎煮过程中甘草促进附子中剧毒的双酯型生物碱水解为低毒性的单酯型生物碱，从而证实了复方解毒机理。把电喷雾质谱(ESI-MS)和多级串联质谱（MS~n，n = 2-10）结合用以分析附子中脂类生物碱的成分。ESI-MS能够依据分子量的不同实现脂类生物碱的有效分离，并且Ms~n可以提供有关分子结构的信息。这样，就在附子乙醚提取物中确认出了12种已知脂类生物碱，并发现四种新的脂类生物碱。二、环糊精／氨基酸和环糊精／肽两种复合物的气相行为在10mM醋酸铵缓冲的环糊精(CD)／氨基酸(AAs)溶液的ESI-MS谱中，分别观察到α、β-CD与9种氨基酸复合物的正负离子；结合碰撞诱导解离(CID)技术确定了气相复合物的价键性质和结构。溶液中CD和AAs之间的疏才斜目互作用由于ESI过程中溶剂化作用的减弱而减弱，甚至完全消失，而分子之间的静电作用和氢键可能因此被加强。去质子化复合物的CID实验显示：当CD复合物从溶液相转入气相时，分子之间的主要作用力发生变化，静电相互作用成为主要作用力。研究还发现：β-CD／芳香氨基酸复合物的稳定性与氨基酸侧链和cD空腔之间的尺寸适合有关。因为CD／芳香氨基酸复合物与CD／其它氨基酸复合物的解离途径是不同的。由于芳香侧链被包结在CD空腔内，当CD／芳香氨 基酸复合物解离时，CD发生“爆裂”。为了进一步解释气相中CD和氨基酸的复合形式，引入氨基酸侧链极性表面积以评价氨基酸侧链对复合物稳定性的贡献。结果显示：氨基酸侧链羟基对复合物稳定性没有明显影响，这更加证明了在气-液两相中CD／芳香氨基酸复合物的结构是一致的。用ESI-MS和MS~n对α、β-CD与谷胱甘肽(GSH)及其修饰物进行研究，实验结果表明：两种环糊精均能催化GSH氧化反应。1:1和1:2CD/GSH复合物的CID揭示了分子之间具有较强的氢键作用。与GSH二聚体相比，1:2复合物作为催化氧化反应的中间体能够提供双分子GSH氧化反应的空间条件。此外，在1:1CD/GSH复合物的CID谱中观察到了GSH的氧化产物，说明在cID的离子富集和活化过程中会发生复合物离子-复合物离子之间的相互作用。这一结果不仅解释了CD催化反应的机理，同时揭示了气相复合物的化学性质。

Production cross section of neutron cluster from the reaction of light neutron rich nuclei

Within the Boltzmann-Langevin equation, the neutron cluster production cross sections in the reactions induced by Be-14, He-8, He-6, Li-11, B-17, Be-11, C-19 on C-12 at 35MeV/u were studied. The experimental data for (4)n production cross section from Be-14+C-12 at 35MeV/u can be reproduced. It is found that the production cross section of neutron cluster is large in the reaction that the projectile has more halo nucleons. And the projectiles with big mass number are easy to produce the neutron cluster, when they have the same number of halo nucleons. The neutron cluster is probably mainly from the halo nucleons of projectile.

Evidence for perimeter sites over SmOx-modified Rh(100) surface by CO chemisorption

SmOx modified Rh(l 0 0) surfaces have been in-situ prepared by depositing metallic Sin and subsequently oxidizing under controlled conditions, and the interaction between the lanthanide oxide and transition metal has been characterized by means of X-ray photoelectron spectroscopy (XPS) and high-resolution electron-energy-loss spectroscopy (HREELS) as well as thermal desorption spectroscopy (TDS). As evidenced, the adsorption of CO on the modified surfaces shows some different features to the original surface of Rh(l 00). The covering of SmOx blocks some sites on the surface and consequently suppresses adsorption of the typical CO species with an uptake at about 500 K, while a novel desorption peak centered at 260 K emerges in the CO TDS. Correspondingly, the XP spectrum exhibits a new C Is peak at 287.9 eV and 0 Is peak at 532.6 eV. The intensity of the low temperature peak varies with the coverage of SmOx, which shows an actual correlation to the perimeter sites of SmOx particles on the surface. (C) 2004 Elsevier B.V. All rights reserved.