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.

The sedimentation rates in the Okinawa trough during the Late Quaternary

On the basis of accelerator mass spectrometer radiocarbon (AMS C-14) dating, sedimentation rates of 11 cores collected from the northern to southern Okinawa Trough are discussed. The sedimentation rates in the Okinawa Trough roughly range from 11 to 39 cm/ka, and the average is 23.0 cm/ka. China's continental matter is the main sediment source of the middle Okinawa Trough and has important contribution to the northern and southern Okinawa Trough. The sedimentation rates during the marine oxygen isotope (MI5) 2 are uniformly higher than those during MIS 1 in the northern and middle Okinawa Trough while they are on the contrary in the southern Okinawa Trough. Sedimentation rates in the Okinawa Trough can be one of the proxies of sediment source and an indicator of cooling events.

The history of the Yangtze River entering sea since the last glacial maximum: a review and look forward

This review paper provides a brief review on the development of ideas in the fields of the sea level change of the ECS (East China Sea), the history of the Yangtze River entering the sea and paleochannels in the shelf of the ECS since the Last Glacial Maximum (LGM). The paper summarizes two opposite theories about the Yangtze River entering the sea during the LGM. One theory is that the Yangtze River input a lacustrine in the north of Jiangsu province which was defunct in middle Holocene, and the river was once dry. The other was that the Yangtze River still existed and entered into the Okinawa Trough during the LGM, but scholars share different opinions on which course the river ran across and which place the river input the trough. This paper concludes future work is to study the evolution of the Yangtze River and the paleoclimate and the corresponding events as a whole from the view of regional and even global change, and more attention should be paid to the study on mud sediment, the Yangtze River's response to the changes in climate and sea-level, and the channel metamorphosis.

Radiolarian fauna in surface sediments of the northeastern East China Sea

Radiolarian abundance and species composition have been determined in 72 surface: sediment samples from the northeastern East China Sea. The results are compared with chemical and physical properties of the overlying water masses, and with sediment conditions. In the study area, radiolarian abundance and species number increase markedly from northwest to southeast, and their distributions can be divided into three provinces: the low-density zone corresponding to the shelf, the middle-density zone corresponding to the western slope of the Okinawa Trough and the high-density zone corresponding to the central part of the Okinawa Trough. The distribution of radiolarians correlates well with modem sea surface temperature and sea surface salinity, but shows a negative relation with nutrients and primary productivity of the overlying water. This distribution pattern is also strongly affected by the sediment type and terrigenous material input. Also, the Kuroshio Current has an important effect on controlling the distribution and species composition of radiolarian fauna in this area. Based on three Q-mode factors (accounting for 90.2% of the variance), three radiolarian assemblages have been distinguished, and their distributions are clearly correlated with oceanographic current patterns in the region. The mixed water assemblage dominated by Tetrapyle circularis, Tetrapyle quadriloba and Ommatartus tetrathalamus tetrathalamus is restricted to the area of the Mixed Water, but mainly influenced by the Shelf Water. The Kuroshio Water assemblage, which is dominated by Lithelius minor, Dictyocoryne profunda, Stylodictya multispina, Acrosphaera spinosa, Dictyocoryne truncatum, Spongaster tetrars, Stylodictya arachnia and Ommatartus tetrathalamus tetrathalamus, is basically controlled by the Kuroshio Surface Water. And the transition assemblage dominated by Tetrapyle quadriloba and Monozonium pachystylum is associated with the Tsushima Warm Current Water. The boundaries among these assemblages approximately coincide with the oceanographic front. And the changes in the distribution of these assemblages could be,regarded as-not only modifications of the water masses, but also indicators of the possible movements of the oceanic front. (C) 2003 Elsevier Science B.V. All rights reserved.

Paleoceanographic records in the sedimentary cores from the middle Okinawa Trough

Two gravity piston cores (Cores 155 and 18) involved in this study were collected from the middle Okinawa Trough. Stratigraphy of the two cores was divided and classified based on the features of planktonic foraminifera oxygen isotope changes together with depositional sequence, millennium-scale climatic event comparison, carbonate cycles and AMS(14)C dating. Some paleoclimatic information contained in sediments of these cores was extracted to discuss the paleoclimatic change rules and the short-time scale events presented in interglacial period. Analysis on the variation of oxygen isotope values in stage two shows that the middle part of the Okinawa Trough may have been affected by fresh water from the Yellow River and the Yangtze River during the Last Glacial Maximum (LGM). The oxygen isotope value oscillating ranges of the cores have verified that the marginal sea has an amplifying effect on climate changes. The delta(13)C of benthic foraminifera Uvigerina was lighter in the glacial period than that in the interglacial period, which indicates that the Paleo-Kuroshio's main stream moved eastward and its influence area decreased. According to the temperature difference during the "YD" period existing in Core 180 and other data, we can reach the conclusion that the climatic changes in the middle Okinawa Trough area were controlled by global climatic changes, but some regional factors had also considerable influence on the climate changes. Some results in this paper support Fairbanks's point that the "YD" event was a brief stagnation of sea level rising during the global warming up procession. Moreover, the falling of sea level in the glacial period weakened the exchange between the bottom water of the Okinawa Trough and the deep water of the northwestern Pacific Ocean and resulted in low oxygen state of bottom water in this area. These procedures are the reasons for carbonate cycle in the Okinawa Trough area being consistent with the "Atlantic type" carbonate cycle.

Benthic foraminiferal distribution in surface sediments along continental slope of the southern Okinawa Trough: dependance on water masses and food supply

Benthic foraminiferal analysis of 29 samples in surface sediments from the southern Okinawa Trough is carried out. The results indicate that benthic foraminiferal abundance decreases rapidly with increasing water depth. Percentage frequencies of agglutinated foraminifera further confirm the modem shallow carbonate lysocline in the southern Okinawa Trough. From continental shelf edge to the bottom of Okinawa Trough, benthic foraminiferal fauna in the surface sediments can be divided into 5 assemblages: (1) Continental shelf break assemblage, dominated by Cibicides pseudoungerianus, corresponds to subsurface water mass of the Kuroshio Current; (2) upper continental slope assemblage, dominated by Cassidulina carinata, Globocassidulina subglobosa, corresponds to intermediate water mass of the Kuroshio Current; (3) intermediate continental slope assemblage, dominated by Uvigerina hispida, corresponds to the Okinawa Trough deep water mass above the carbonate lysocline; (4), lower continental slope - trough bottom assemblage, dominated by Pullenia bulloides, Epistominella exigua and Cibicidoides hyalinus, corresponds to deep water mass of the Okinawa Trough; and (5) trough bottom agglutinated assemblage, dominated by Rhabdammina spp., Bathysiphon flavidus, corresponds to I strongly dissolved environment of the trough bottom. The benthic foraminiferal fauna in the southern Okinawa Trough are controlled jointly by water masses and food supply. Water temperature, oxygen concentration and carbonate dissolution of the water masses are important controlling factors especially for the continental shelf break and trough bottom assemblages. The food supply also plays an important role in these benthic foraminiferal assemblages along the western slope. of the Okinawa Trough. Both the abundance and the 5 assemblages of benthic foraminifera correspond well to the organic matter supply along the continental slope and a lateral transport of TSM (total suspended matter) and POC (particulate organic carbon) from the shelf break to the deep water is also an important food supply for benthic fauna in this region.

A broad deglacial delta C-13 minimum event in planktonic foraminiferal records in the Okinawa Trough

The equatorial Pacific upwelling zone has been suspected of playing an important role in the global atmospheric CO2 changes associated with glacial-interglacial cycles. In order to assess the influencing scope of the surface water deglacial delta(13)C minimum in the tropical low-latitude Pacific, the core DGKS9603, collected from the middle Okinawa Trough, was examined for 4513 C records of planktonic foraminifera N. dutertrei and G. ruber. The planktonic foraminiferal delta(13)C records show a clear decreasing event from 20 to 6 cal. kaBP., which is characterized by long duration of about 14 ka and amplitude shift of 0.4 x 10(-3). Its minimum value occurred at 15.7 cal kaBP. The event shows fairly synchrony with the surface water deglacial delta(13)C minimum identified in the tropical Pacific and its marginal seas. Because there is no evidence in planktonic foraminiferal fauna and 45180 records for upwelling and river runoff enhancement, the broad deglacial delta(13)C minimum event in planktonic foraminiferal records revealed in core DGKS9603 might have been the direct influencing result of the deglacial surface water of the tropical Pacific. The identification for the event in the Okinawa Trough provides new evidence that the water evolution in the tropical low-latitude Pacific plays a key role in large regional, even global carbon cycle.

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.

Millennial-scale paleoceanography in Okinawa Trough during Late Quaternary period

Based on the analyses of foraminifer and accelerator mass spectrometer radiocarbon dating in DGKS9603 core from mid-Okinawa Trough close to bottom, oscillation curve, which expressed the relation between the surface water temperature and the depth, has been obtained by using foraminifer analysis and calculation of FP-12E transfer function. The whole core indicated seven cold phases and eight warm phases. Obvious expression of low temperature event during Middle and Late Holocene, YD,H1,H2,H3 and H4 events, as well as the short cold phase during the middle last glacial period, implied that short shifts since 50 kaBP would have been global significance. Sedimentation rate during cold phases is usually faster than that in warm stages, with the lowest rate in Holocene, which may be connected with rising sea level and principal axial of Kuroshio Current moving to west. Volcanic activities highly developed in Okinawa Trough during the Quaternary period, thus abundant volcanic glass and pumice were well preserved.

长江口水域富营养化的形成、演变与特点研究

本文以我国长江口水域富营养化为研究对象，对长江水体溶解态无机氮、磷分布特点和通量变化进行了分析，基于长江流域氮“输入-输出”关系模型探索了水体氮的来源；分析了长江口水域富营养化长期演变及特点；探索了长江口海域低氧区的发生机制。结果如下： 长江水体中NO3--N、NH4+-N、DIN和DIP浓度从上游往下游呈增加趋势，但存在季节差异。长江流域从上游往下游的DIN输送通量的变化主要受水流量的影响，但从上游往下游单位面积年产N量逐渐升高；DIP输送通量从上游往下游呈增加趋势，同时也主要受水流量控制，但从季节变化来讲，DIP的月输送通量受其浓度的控制更加明显。自20世纪60年代来，长江水体中NO3--N、NO2--N、DIN和DIP浓度都处于缓慢上升趋势，但到80年代上升速度明显加快；不同历史时期DIN和DIP的季节变化特点也不尽相同，反映出其来源的差异。同时，本研究采用长江流域氮“输入-输出”关系模型（污染负荷统计模型）对长江水体氮来源进行了分析，估算了各种氮源对水体氮的贡献率。结果表明，2006年向长江流域输入氮的总量为17.6 Tg，其中20%的输入氮转移到了水体（3.5 Tg）。本年度长江大通水文站实测氮输送通量为1.8 Tg，表明约50%的氮在水体输送过程中发生了生物、化学、物理损耗。对于长江水体氮的来源来讲，饲养牲畜粪便氮流失和大气干/湿沉降氮的贡献率较大，分别为26%和25%；农业氮肥流失和城市生活污水排放的贡献率相同，都为17%；农村人口粪便氮流失和工业废水排放的贡献率分别为6%和9%。 自20世纪60年代以来，长江口口门内和外海（盐度>30psu）水体中营养盐浓度增加显著。在表层水体盐度大于22psu海域DIN: PO43--P值表现出了明显升高的历史变化趋势。SiO3: PO43--P值从1959年到1985-86年显著下降，然后到2003-06年有所上升。根据SiO3: PO43--P值和DIN: PO43--P值的长期变化趋势，可以推出，SiO3: DIN值从20世纪50-60年代以后呈现下降趋势。在长江口海域，随着营养盐浓度的增加，浮游生物量的大幅度升高在本研究中得到证实。同时，长江口水域浮游植物种群结构对营养盐结构的长期变化产生响应，研究结果表明，硅藻种类比重从1985-86年84.6% 下降到2004-05年69.8%；年均硅藻丰度占浮游植物总丰度比重在1985-86年达到99.5%，但到2004-05年降低为75.5%，而甲藻丰度比重则由0.7%增大到25.4%。 底层水体DO浓度与Delta S（底层水体与表层水体的盐度之差）和Delta T（表层水体与底层水体的温度之差）成显著负相关，这表明了水体层化或者垂直水体交换是控制长江口水域底层水体溶解氧变化的主要因素，但水体温度层化要比盐度层化在控制低氧区形成上起到更大的作用。上升流在该海域低氧的形成和分布上起到很重要的作用，显著影响低氧水团的垂直分布，也显著影响到溶解氧的水平分布。现场生产的浮游植物可能是低氧区的形成的生物基础，日益增加的叶绿素a浓度和大规模的有害藻华可能是长江口低氧区逐渐增大的原因。本研究认为，此海域低氧区的形成主要受长江冲淡水、台湾暖流的入侵、地形、尤其是温跃层的形成和现场生产的有机物质控制。

海湾扇贝微卫星标记的开发及遗传连锁图谱的构建

海湾扇贝（Argopecten irradians）不连续分布于美国大西洋沿岸和墨西哥湾沿岸，自1982年以来北部亚种（A. i. irradians）和南部亚种（A. i. concentricus）被先后引进到中国，由于其生长速度快、繁殖周期短和适宜温度范围广的特点，迅速成为我国海水养殖的重要品种。近年来飞速发展的分子标记技术为优良品种的选育注入了新的活力，相对于传统的表型选择来说，标记辅助选择不易受环境的影响，尤其是对于低遗传力性状和后期表达的性状，能增强选择效率，提高选择的准确度，缩短育种周期。本文通过构建海湾扇贝微卫星富集文库获得大量的微卫星DNA序列，筛选多态的微卫星标记构建了海湾扇贝的遗传连锁图谱，并应用复合区间作图法对生长相关性状进行了QTL定位。 本研究利用富集文库-菌落原位杂交法筛选海湾扇贝微卫星DNA，吸附(AC)15和(AG)15探针的尼龙膜捕捉并富集含有微卫星序列的片段，菌落原位杂交结果显示阳性克隆率达到40%，测序比对后获得521个独立的阳性克隆，其中微卫星506个，小卫星15个。微卫星中，完美型248个，占49.0%，非完美型216个，占42.7%；复合型42个，占8.3%；AG/TC重复占大多数（356个，70.4%），AC/TG重复有150个（29.6%）。设计合成了382对引物，利用38个海湾扇贝个体对其中15个微卫星位点进行了遗传多样性评价，不同位点扩增得到的等位基因数从3到7个不等，期望杂合度和观测杂合度的范围分别为0.198~0.813和0.083~0.833，实验结果表明富集文库-菌落原位杂交法适合大规模筛选微卫星标记。 利用8个微卫星标记对海湾扇贝1个野生种群和3个养殖群体的遗传多样性与分化进行了比较和分析。8个位点共扩增得到35个等位基因，平均每个位点4.38个等位基因，平均有效等位基因数为2.30，平均观测杂合度和期望杂合度分别为0.41和0.46。相比于野生群体（美国），养殖群体（北卡罗来那、浙江和胶南）的等位基因数和杂合度都有所降低，在封闭环境下养殖19代的浙江群体等位基因数丢失最严重，共有9个等位基因丢失（25.7%）。经过多代人工养殖后，海湾扇贝养殖与野生群体之间和养殖群体之间出现了明显的遗传分化，胶南群体与野生群体的遗传距离最大，而胶南群体与浙江群体的遗传距离已经超过了胶南群体（北部亚种）和北卡罗来那（南部亚种）群体的遗传距离，这种分化将有利于海湾扇贝的杂交选育。 利用167个微卫星标记和1个壳色标记，以海湾扇贝2个全同胞F1代为作图群体，构建了海湾扇贝的性别遗传连锁图谱。整合的雌性连锁图谱含有118个标记，覆盖了16个连锁群，每个连锁群含有的标记数目从4到16个不等，平均每个连锁群上有7.4个标记，图谱总长度为761.0 cM，标记间的平均间隔为8.55 cM，图谱的覆盖率为73.5%；整合雄性连锁图谱含有126个标记，覆盖了17个连锁群，每个连锁群含有的标记数目从2到11个不等，平均每个连锁群上有7.4个标记，图谱总长度为729.1 cM，标记间的平均间隔为6.75 cM，图谱的覆盖率为74.7%。雌性亲本的重组率高于雄性，雌雄亲本共享标记间的重组率比值为1.18：1。偏分离标记在性别间呈现不对称分布，雄性亲本的偏分离高于雌性亲本，可能与雄性亲本来源于亚种间杂交的遗传背景相关。 利用海湾扇贝微卫星遗传连锁图谱在两个作图家系中对5个生长性状的QTL进行了定位，5个生长性状的表型相关均达到极显著水平（P < 0.01），Pearson相关系数均超过0.781，总重、壳长、壳宽、壳高和壳重的QTL（LOD > 2.0）的数目分别为8、6、6、7和6个。这些QTL成簇分布于CC5家系的LG1、LG3、LG4、LG8和CC10家系的LG1、LG3、LG6、LG8、LG9连锁群，单个QTL可解释的表型方差为5.5%到29.2%，QTL成簇分布现象说明这些生长相关的性状可能具有共同的遗传基础，家系特异性QTL暗示在不同的遗传背景和环境下存在不同的主效QTL。本研究定位的QTL，尤其在两个家系中共享的QTL为下一步分子标记辅助选择提供了参考区间。

中国明对虾体内凝结作用相关免疫基因的克隆与表达研究

对虾疾病在世界范围内的频频爆发，给地区经济造成了重大损失。然而到目前为止，我们对于对虾免疫系统的分子机制还知之甚少，深入了解其免疫应答过程，包括异物识别，信息传递以及作用方式等是从根本上解决疾病问题的关键之一。本论文从中国明对虾血细胞中分别克隆了一种C型凝集素基因（Fclectin）、参与凝结过程的谷氨酰胺转移酶基因（FcTG）以及参与凝结级联反应和酚氧化酶原激活系统的两种丝氨酸蛋白酶基因（SP-1和SP-2）和两种丝氨酸蛋白酶抑制剂基因（SPI-1和SPI-2），分析了它们的分子结构特征，预测了其可能的作用，并对它们的组织分布及应答不同病原感染的表达变化模式进行了研究。 首次从对虾中克隆了Fclectin基因，比对结果发现该基因属于C型凝集素超家族的成员之一；Northern blot和原位杂交结果显示，Fclectin基因在部分血细胞中呈组成型表达；利用毛细管电泳半定量RT-PCR方法分别研究了细菌和病毒感染后该基因的表达特征，并初步尝试了利用体外培养的原代血细胞系统研究LPS刺激后Fclectin的表达变化。该基因在感染或刺激后表达水平有明显的改变。 利用RACE技术从中国明对虾血细胞中克隆了一个FcTG基因，它与斑节对虾的谷氨酰胺转移酶基因有93%的相似性，可能编码一种具有活性的TG；原位杂交结果FcTG主要在血细胞中表达，在淋巴器官管腔的血细胞中表达尤为丰富，推断该基因可能主要在吞噬细胞中表达；病原的刺激未能使该基因的表达明显改变，但损伤（注射）的刺激会对其表达产生一定影响。 利用本组构建的对虾血液cDNA文库，克隆到了两个不同的丝氨酸蛋白酶基因，命名为SP-1和SP-2。前者为具有假clip结构域的胰蛋白酶样SP类似物（SPH），后者是一个具有完整的clip结构域的SPH，这在对虾中是首次发现。SP-1和SP-2都主要在血细胞中表达，此外SP-1在淋巴器官中的表达水平也很高；细菌的刺激对SP-1的影响不大，但会诱导SP-2表达量的增加，这两个基因的表达模式在病毒刺激后很相似，都出现先上调后下降的过程，可见病毒的感染会导致这两个基因转录的增强。 利用SMART-RACE技术结合对虾血液cDNA文库的利用，从中国明对虾血细胞中克隆到了两种SPI基因，它们分别为kazal-SPI和serpin-SPI，属于两个不同的家族。SPI-1与斑节对虾的SPI有76%的相似性，推断SPI-1可能主要对弹性蛋白酶、枯草杆菌蛋白酶、胰凝乳蛋白酶等有抑制作用；SPI-2为对虾中首次报道的serpin型抑制剂，它与淡水螯虾的serpin有42%的相似性，SPI-2可能主要对胰蛋白酶、酚氧化酶原激活酶、凝血酶和凝结酶有抑制活性。组织分别特征显示这两个抑制剂基因都在鳃、血细胞和淋巴器官中有高水平的表达。细菌的刺激都会导致这两个基因的表达在感染后出现下调，随后又上升至原有水平；病毒感染后，SPI-1和SPI-2的表达变化情况相似，感染后前12h基本没有明显的改变，到了感染的晚期（感染后24h和48h），随着病毒在体内大量复制，这两个基因的表达都急剧下降至接近基因关闭的状态，这可能暗示着与SPI相对应的蛋白酶的活力将很大程度的异常的增加，机体内稳定的免疫系统平衡状态可能已被破坏。

孔石莼多糖及其衍生物的研究

在中国，孔石莼应用于医药方面已有几千年的历史，其煎剂常被当地居民用来治疗中暑和泌尿方面的疾病。实验室以前所做的工作表明，孔石莼的水溶多糖具有很好的抗高血脂活性，本论文在此研究的基础上主要就多糖的长期毒性、一般药理、多糖的衍生化、不同分子量孔石莼多糖的抗氧化活性、衍生物的抗氧化活性和动物调血脂活性进行了研究。 水提醇沉制备多糖，多糖主要由糖醛酸、鼠李糖、木糖、葡萄糖和硫酸根组成，还含有微量的半乳糖、甘露糖和阿拉伯糖。多糖中主要的二糖重复单位为[β-D-Glcp A-(1->4)- α-L-Rhap 3S] 和 [α-L-Idop A-(1->4)- α-L-Rhap 3S]。急性毒性实验表明，KM小鼠对孔石莼多糖的最大耐受量(MTD)大于4000 mg/kg，其腹腔注射雌性小鼠的半致死量(LD50)为408.7 mg/kg，雄性动物为432.7 mg/kg。长期毒性（6个月）实验表明孔石莼多糖无毒反应剂量为1.2 g/kg。一般药理研究表明孔石莼多糖对小鼠中枢神经系统无明显影响，对麻醉犬心血管系统和呼吸系统均无明显影响。 采用过氧化氢降解的方法制备了不同分子量的孔石莼多糖，并且测定了体外抗氧化活性；制备了高硫酸根含量的孔石莼多糖、乙酰化和苯甲酰化孔石莼多糖衍生物，测定了体外抗氧化活性和动物调血脂试验。结果表明，不同分子量的孔石莼多糖其抗氧化活性是不同的，分子量低的孔石莼多糖表现出了较强的抗氧化活性。孔石莼多糖的衍生物其抗氧化活性要优于孔石莼多糖。调血脂动物试验表明，孔石莼多糖以及其衍生物都具有很好的调血脂效果。高硫酸根含量孔石莼多糖的中、低剂量组的调血脂活性要优于高剂量组（低剂量组降低低密度脂蛋白的能力要稍弱于原料），而且，中剂量组与原料组相比，小鼠血清TG明显降低（P＜0.05），LDL－C 明显降低（P＜0.01）。低剂量组乙酰化衍生物降低甘油三酯（TG）和低密度脂蛋白（LDL－C）的能力要优于中高剂量组。对于孔石莼多糖以及衍生物调血脂的机制还需进一步的研究。

Antihyperlipidemic effects of different molecular weight sulfated polysaccharides from Ulva pertusa (Chlorophyta)

Ulvan, a sulfated polysaccharide from Ulva pertusa, was degraded to yield two low molecular weight fractions U1 and U2. The molecular weights of ulvan and its fractions were determined and varied from 151.6 to 28.2 kDa. They were fed to rats on a hypercholesterolemic diet for 21 days to evaluate and compare the antihyperlipidemic actions. Ulvan-based diet significantly lowered the levels of serum total cholesterol (-45.2%, P < 0.05) and low density lipoprotein cholesterol (LDL-cholesterol, -54.1%, P < 0.05). While U1- and U2-based diets significantly elevated the levels of serum high density lipoprotein cholesterol (HDL-cholesterol, +22.0% for U1, not significant; +61.0% for U2; P < 0.05) and reduced triglyceride (TG, -82.4% for U1, -77.7% for U2; P < 0.05) in rats as compared to control diet. In addition, consumptions of various ulvans significantly increased fecal bile acid excrement. The results indicated that ulvans with different molecular weights exhibited diverse effects on lipid metabolism. The high molecular weight ulvan was effective in serum total and LDL-cholesterol, whereas low molecular weight fractions were in TG and HDL-cholesterol. The fractions were considered to be more beneficial to hyperlipidemia associated with diabetes over ulvan. (C) 2003 Elsevier Ltd. All rights reserved.