几种非营养无公害添加剂对大菱鲆的效应和机理研究

在基础饲料中分别添加0.04％低聚木糖、0.13％酵母细胞壁、0.08％胆汁酸和同量组合添加，形成5个处理组。采用随机区组试验设计，将体重151.3±15.2 g 的健康大菱鲆鱼165尾平均分配到5个处理组(A～E)中（每组3重复），经72天试验，进行了生长、水质、消化、免疫等试验和测定，结果如下： 组合组的生长效果和饲料利用率最好，酵母细胞壁或低聚木糖单独添加，表现出优良的促生长和饲料利用率；单独添加胆汁酸也有良好效果。4试验组（组合组、酵母细胞壁组、低聚木糖组、胆汁酸组）与对照组比较，增重率分别提高15.4％、13.9％、12.4％（p<0.05）和7.4％(P>0.05)，饲料系数分别降低6.9％、6.2％、5.4％（p<0.05）和3.8％(P>0.05)。 不同添加剂及组合对试验鱼所处水环境因子变化仅有小幅影响，统计差异不显著（p>0.05）。4试验组比对照组的水体氨氮含量分别提高4.0％、3.2％、3.0％和0.8％(P>0.05)，COD含量分别提高2.8％、-2.2％、-3.4％和0.8％(P>0.05)。根据试验结果，建议水环境因子（氨氮、磷酸盐、COD等）作为水产动物营养与饲料研究的主要衡量指标之一。 3种添加剂组合后达到提高生长大菱鲆非特异性免疫功能的最优效果，对补体C3和C4、细胞吞噬活力和SOD的提高作用尤为显著；酵母细胞壁单独添加对补体C3和细胞吞噬活力的作用更加显著；低聚木糖单独添加对补体C4和细胞吞噬活力的作用显著；单独添加胆汁酸提高免疫力的作用相对较弱。 4试验组比对照组的蛋白质消化酶活力在胃和前肠，分别提高20％和24％、17％和19％、16％和15％（p<0.05）、11％和3％(P>0.05)；脂肪消化酶活力在前肠和中肠，分别提高22％和19％、19％和17％（p<0.05）、7％和12％（p>0.05）、19％和18％（p<0.05）。 4试验组比对照组的蛋白质消化率分别提高了3.6％、2.9％、3.7％（p<0.05）和1.5％（p>0.05）；粪蛋白质排出量减少12.7％、7.1％、13.4％和2.4％（p>0.05）。说明，3种添加剂显著提高了生长大菱鲆蛋白质消化率，使粪蛋白质排出量不同程度降低，显示了试验使用添加剂的无公害效应。 权衡不同添加剂及其组合对大菱鲆生长期生长性能、饲料利用率、水生态因子、消化酶活力、非特异性免疫、蛋白质消化与粪蛋白质排出的综合影响，本研究从生态与环保角度得出：3种添加剂组合的效果最好，酵母细胞壁或低聚木糖单独添加表现出优良效果；单独添加胆汁酸也有良好作用。

紫菜壳孢子萌发过程及其世代差异研究

紫菜是一类海洋藻类研究的模式系统，具有重要的经济价值和理论研究意义。本研究基于紫菜的世代交替生活史，对其壳孢子萌发过程进行了研究，并对丝状孢子体与叶状配子体的世代差异进行了分析，主要包括以下三部分： 1） 对紫菜丝状孢子体与叶状配子体的连接枢纽——壳孢子的发育过程及其光影响进行了研究与讨论，发现壳孢子只有在附着后才能形成细胞壁并发育，说明壳孢子的附着是触发了壳孢子细胞壁的形成以及后期发育的开关，亦即附着是触发紫菜世代交替过程中配子体转录组表达的开关；纤维素酶和果胶酶均能抑制壳孢子附着，但影响机制各不相同，推测果胶质主要介导壳孢子的初始附着，而纤维素则与永久附着相关；波长≥580 nm的高强度（200 μmol•m-2•s-1）可见光有利于壳孢子早期发育。 2） 结合现有藻类数据，对坛紫菜丝状孢子体阶段11000 EST数据进行了大规模的生物信息学分析，结果首次发现坛紫菜丝状孢子体中可能存在PCK型C4光合固碳途径，并筛选出44条在紫菜孢子体中表达上调的代表基因。 3） 结合坛紫菜、条斑紫菜、海带和红毛菜，对红藻和褐藻等大型海藻孢子体与配子体阶段代表基因Rubisco的表达与羧化酶活性差异进行了研究分析，结果表明Rubisco的表达量和初始羧化酶活在其配子体中均显著高于其孢子体世代，即与藻体不同世代的相对复杂度无关，而与染色体倍性相关，说明Rubisco的世代差异极有可能与染色体倍性相连锁，因而可能是海藻世代交替过程中的重要功能基因。

双刺纺锤水蚤（Acartia bifilosa）基础生物学与生态学研究

20世纪90年代以来，为了确保日益增长的人口对蛋白质的需求，海洋鱼类养殖在全球范围内日趋发展。然而，许多养殖鱼类的品质如抗病力、口味等与野生种类相比大为降低。饵料对于鱼类品质的好坏起着至关重要的作用。在海洋的自然环境中，浮游动物，特别是数量庞大、种类繁多的桡足类是野生鱼类的天然活饵料。哪些桡足类适于作养殖饵料，如何获得、从何处获得桡足类，人工培养是否可行，能否通过加入桡足类来改善养殖鱼类的品质是长期以来业内人士一直关注的问题，需要大量的基础性探索研究工作。 开展有潜在开发价值种的生物学特性及室内培养的基础研究，进而开展大量生产技术的研究与应用，不仅是开发利用桡足类的一个重要途径，而且可以获得一些重要的生态学参数。 本论文自2003年10月－2004年9月之间，在胶州湾采集不同的桡足类种类，通过室内比较培养实验，选定双刺纺锤水蚤作为具有开发潜力的研究培养对象，对其展开一系列培养条件及生物学特性研究，在此基础上进行了小水体增殖培养，结合现场调查资料对与其生活策略相关的生态学问题进行了初步研究探索。结果如下： 筛选：2003年10月－2004年9月全年不同季节共采集11 种桡足类，在室内自然温度、自然海水（盐度30－32）下长时间培养，粗略筛选出能够经受实验室人工养殖水体生活的种类有：强额拟哲水蚤（Paracalanus. crassirostris）、汤氏长足水蚤（Calanopia thompson）、太平洋真宽水蚤（Eurytemora pacifica）、双刺纺锤水蚤（Acartia bifilosa）。对上述种类的成体和子代幼体分别测定其对不同盐度、温度的耐受能力。培养结果表明：18℃室温下，强额拟哲水蚤幼体在盐度20以上的环境中，存活时间不超过11天；汤氏长足水蚤雌体在培养温度低于20℃时，只能存活10天；25℃室温下，当盐度低于20时，汤氏长足水蚤雌体存活时间不超过9天，子代的存活时间不超过7天；太平洋真宽水蚤不适宜在温度较高的夏秋季培养，幼体在不同盐度的实验条件下存活时间不超过5天，不适宜长期培养；双刺纺锤水蚤在全年8－24℃的室内培养温度范围内保持了24－85％的存活率，雌体和子代在盐度10－35的范围内都能存活，最终结果表明双刺纺锤水蚤是其中最适宜进行人工培养的种类。 繁殖：对双刺纺锤水蚤雌体的培养条件和繁殖生物学的研究结果表明：在本实验所使用的6种微藻饵料：微绿球藻（Nannochloropsis oculata）、小球藻（Chlorella.sp）、等鞭金藻（Isochrysis galbana）、三角褐指藻(Phaeodactylum tricornutum)、亚心型扁藻(Platymonas subordiformis)、中肋骨条藻(Skeletonema costatum)中，亚心型扁藻和中肋骨条藻适宜成体培养，亚心型扁藻对雌体存活有利，排粪率也要比中肋骨条藻低得多，亚心型扁藻在高温条件下的饵料利用效率要高于中肋骨条藻，中肋骨条藻对产卵有利，二者混合优势互补；预饥饿处理的双刺纺锤水蚤恢复到最高产卵率需要较长的时间，并且一直保持较低的产卵率；该种繁殖的最适温度范围15－20℃；在10－25℃温度范围内的平均产卵率差异并不显著。 生长及发育：对双刺纺锤水蚤幼体培养条件及发育生物学研究结果表明：在本实验所使用的6种微藻饵料中，微绿球藻是比较理想的开口饵料；粒径小（ 4 m）的微藻——微绿球藻和小球藻不能保证双刺纺锤水蚤后期无节幼体发育至桡足阶段，22℃以下采用微绿球藻 + 亚心型扁藻 + 中肋骨条藻的食物搭配，22℃以上需加入粒径在4m左右的等鞭金藻。 世代时间：通过一系列的温度梯度实验，证明在相同饵料的情况下，温度对双刺纺锤水蚤的发育具有显著的影响，在15－25℃的范围内，随着温度的升高，生长速度加快、世代周期缩短；在温度条件为15、18、20、22、25℃下的世代时间分别为25.5, 18.5, 13, 11.5, 9.5天。 群体培养：研究了适宜的微藻饵料种类搭配比例以及总饵料浓度对种群日均增值率的影响。结果表明：20℃下培养宜采用亚心型扁藻：中肋骨条藻：微绿球藻按含碳量2:1:1的比例组成混合饵料，达到最高增殖率的混合饵料浓度范围在1.0－4.0 μg C ml-1之间；25℃下培养宜采用亚心型扁藻：中肋骨条藻：微绿球藻：等鞭金藻按含碳量2:1:1:2的比例组成混合饵料，日均增殖率在混合饵料总浓度为1.0 μg C ml-1 时最高，低于和高于此浓度都会降低日增值率。 度夏机制：针对野外大面调查发现双刺纺锤水蚤在高温季节的胶州湾内仍然存在的事实（传统观点认为该种在夏季从水体中消失，通过休眠卵度夏），本论文从基础生态学研究出发，根据胶州湾夏季的温度和叶绿素浓度资料，设计实验研究了高温和饵料浓度对成体繁殖和幼体生长发育的影响。实验发现，饵料浓度对高温下雌体的繁殖有着明显的影响，15g Chla l-1浓度下的雌体在28℃都可以保持产卵状态，而且卵的孵化率也在50％以上；各处理中的卵都很快孵化，并保持了60％以上的孵化率；高浓度组15 g Chla l-1和10 g Chla l-1，无节幼体都能发育至成体，低浓度5 g Chla l-1处理组中，28℃下，不能发育至桡足阶段，而25℃下也只能发育至C4期。在本实验中没有发现双刺纺锤水蚤产生休眠卵。在胶州湾自然环境中发现该种全年存在。胶州湾中的双刺纺锤水蚤在夏季能够在不产生休眠卵的情况下安全度夏。

胶州湾和东太平洋海隆(~13°N)沉积物微生物多样性研究

海洋是一个巨大的生态系统，多样的微生物是构成海洋生态系统的基本元素。海洋微生物的群落结构及演变深刻的反映着海洋生态系统的变迁。本文采用分子生物学技术，研究了近海沉积物生态系统——胶州湾沉积物中细菌的多样性、群落结构的时空演替规律以及远洋深海沉积物生态系统——东太平洋海隆北纬13o附近深海沉积物中细菌和古细菌群落结构沿沉积物断层的分布情况，结果表明在两处沉积物中，微生物群落的结构都与环境因子有显著的相关性，是反映海洋沉积物环境特征的重要（分子）标志物，并且可能在这些环境中参与生物地球化学循环等重要过程。 1.从胶州湾不同区域的8个代表性站点采集4个季度的沉积物样品。提取总基因组DNA，利用16S rDNA作为分子标记，采用克隆文库对胶州湾沉积物中细菌群落的组成、空间分布和季节演替规律进行了研究。结果显示沉积物中的细菌具有高度多样性，来自于13个细菌门，同时还有28%的未鉴定克隆，表明胶州湾沉积物中蕴藏着巨大的微生物资源。其中已鉴定的优势种群是α-、β-、γ-、δ-变形细菌、绿弯菌、厚壁菌、蓝细菌和放线菌。同时还包括酸杆菌、拟杆菌、浮霉菌、疣微菌、芽单胞菌、绿菌、梭杆菌、异常球菌-栖热菌等类群的存在。将各克隆库的组成与温度、总碳、总氮等环境因子结合分析，结果显示细菌群落结构更替的主要驱动力是季节变化所带来的温度等环境因子的演变。对数据库中与本研究所获得序列具有最近亲缘关系序列的来源环境进行分析表明，胶州湾中细菌群落受航运活动、水产养殖、重金属污染等人类活动的明显影响，同时这些活动表现出显著的空间特异性，比如C4和D6等站点明显受到航运活动的影响，而A3和Y1等站点则容易受到沿岸径流所带来的淡水和油污染的影响。 2.分别利用PCR-DGGE和克隆文库技术对东太平洋海隆北纬13o附近深海柱状沉积物样品中细菌和古菌群体进行研究，结果显示这些微生物群落沿四个分别代表不同沉积年代断层明显的成层分布，与环境因子结合分析表明这种成层分布与氧化还原性质等地球化学特征的成层分布相吻合，提示我们该生态系统中的微生物受到环境因子的巨大作用，同时也表明这些微生物可能参与该生态系统中硫、金属元素代谢等过程。通过系统发育分析，四个断层中的微生物群落中呈现出很多与热液活动相关的个体（其中34.7%的细菌序列和31%的古菌序列与来源于各种热液环境的序列具有最近的亲缘关系）。但总体群落结构分析表明该区域可能属于热液活动影响区域的边缘，处于从热液活动环境到普通的低温沉积物环境的过渡区域。 3.将在胶州湾和东太平洋海隆北纬13o附近海洋沉积物生态系统中都存在的优势细菌类群（α-、β-、γ-、δ-变形细菌和放线菌、绿弯菌、厚壁菌、酸杆菌、浮霉菌）进行系统发育分析和背景比较分析，结果显示两处沉积物中的细菌优势种群虽然在大类群上很多是相同的，但是可能由于两处沉积物中不同物理化学等环境因子的选择作用（如胶州湾的近海特征和人为活动，东太平洋深海特点和热液活动），而导致优势种群在系统发育关系上距离比较远。这表明独特的微生物群落结构，特别是优势种群的群落结构信息是描述特定环境生态系统的重要方面。本研究表明在全球环境变迁中,自然环境因子和人类活动都在深刻改变着微生物群落的结构和功能。本文阐述了在环境变迁特定时期两处沉积物生态系统中的微生物群落结构及时空差异，为研究大范围生态系统的演变提供了依据，同时也为在两处沉积物环境中进行微生物参与的生物地球化学研究奠定了基础。

Sources and preservation of organic matter in Plum Island salt marsh sediments (MA, USA): long-chain n-alkanes and stable carbon isotope compositions

Elemental (TOC, TN, C/N) and stable carbon isotopic (delta(13)C) compositions and n-alkane (nC(16-38)) concentrations were measured for Spartina alterniflora, a C-4 marsh grass, Typha latifolia, a C-3 marsh grass, and three sediment cores collected from middle and upper estuarine sites from the Plum Island salt marshes. Our results indicated that the organic matter preserved in the sediments was highly affected by the marsh plants that dominated the sampling sites. delta(13)C values of organic matter preserved in the upper fresh water site sediment were more negative (-23.0+/-0.3) as affected by the C-3 plants than the values of organic matter preserved in the sediments of middle (-18.9+/-0.8) and mud flat sites (-19.4+/-0.1) as influenced mainly by the C4 marsh plants. The distribution of n-alkanes measured in all sediments showed similar patterns as those determined in the marsh grasses S. alterniflora and T. latifolia, and nC(21) to nC(33) long-chain n-alkanes were the major compounds determined in all sediment samples. The strong odd-to-even carbon numbered n-alkane predominance was found in all three sediments and nC(29) was the most abundant homologue in all samples measured. Both delta(13)C compositions of organic matter and n-alkane distributions in these sediments indicate that the marsh plants could contribute significant amount of organic matter preserved in Plum Island salt marsh sediments. This suggests that salt marshes play an important role in the cycling of nutrients and organic carbon in the estuary and adjacent coastal waters. (C) 2003 Elsevier Ltd. All rights reserved.

The Yellow Sea cold bottom water - an oversummering site for Calanus sinicus (Copepoda, Crustacea)

The vertical distribution and stage-specific abundance of Calanus sinicus were investigated on three key transects in the southern Yellow Sea and the northern East China Sea in August 1999. The results showed that in summer C. sinicus shrank its distribution area to the central cold (less than or equal to10degreesC) bottom water in the Yellow Sea, i.e. the Yellow Sea Cold Bottom Water, remaining in high abundance (345.7 ind m(-3)). In the northern East China Sea on a transect from the mouth of the Yangtze River to the Okinawa trench, only a few individuals appeared in the inner side and none had been found either in the upper layer or in the deep layer of the outer shelf area. The population of C. sinicus in YSCBW consisted of mainly adults (46.83%) and C5 (37.41%). C1-C4 only accounted for 15.76%. The low proportion of the earlier copepodite stages and the high female:male ratio (11.39) indicated that the reproduction of C. sinicus in YSCBW was at a very low level due to the low temperature and low food concentration. It is concluded that the dramatic decrease of C. sinicus population in the shelf area of China seas in summer is caused by the shrinkage of its distribution area and the YSCBW served as an oversummering site.

青藏高原3种植被类型净生态系统CO2交换量的比较

采用涡度相关观测技术系统, 于2003年7月1日～2004年6月30日对青藏高原高寒草甸3种植被类型(矮嵩草草甸、金露梅灌丛草甸和藏嵩草沼泽化草甸)生态系统CO2通量进行观测和分析. 结果表明, 嵩草草甸、灌丛草甸和沼泽化草甸CO2最大吸收率分别为16.78, 10.42和16.57 mmol/m2•s; 最大CO2排放率分别为8.22, 7.73和18.67 mmol/m2•s; 嵩草草甸和灌丛草甸一年从大气中分别吸收CO2 282和53 g/m2, 而沼泽草甸一年向大气排放CO2 478 g/m2. 证明青藏高原嵩草草甸和灌丛草甸比C4草原和一些低海拔草原和森林具有一个较低CO2吸收和排放量潜能, 而沼泽化草甸具有一个较高的排放潜能, 揭示了青藏高原高寒草甸生态系统不同植被类型的碳源/汇的明显差异, 主要是由植物光合能力不同和土壤呼吸差异引起的.

基于稳定碳同位素技术研究青藏高原东部高寒区植被的光合型

通过对青藏高原东部玛多县境内高寒地区20个科、38个属、62种植物叶片的稳定性碳同位素的测定,来确定植物群落的光合型.结果表明,所测定的62种植物的稳定性碳同位素比值(δ13C)介于-28.6‰和-25.2‰之间,说明这62种植物均属于C3植物,没有C4植物或CAM植物.植物这种光合型的分布与该研究区的环境因素有密切关系,低温是该区没有C4植物分布的关键因素,同时光合型的分布也反映了植物对独特地理环境的适应.

Stable carbon isotope analyses show dominance of C3 grasses in the feed selected by small herbivores at the alpine meadow at the Tibetan Plateau

Muscle samples were collected from small herbivorous mammals (Ochotona curzoniae, Microtus oecnomus, Myospalax fontanierii and Lepus oiostolus) at the alpine meadow ecosystem at the Tibetan Plateau in order to address variability in stable carbon isotope composition. Stable carbon isotope values of muscles remain steady and show no significant variations (-25.72 to -27.04 parts per thousand) among the four small mammal species. Based on the mass balance theory of stable isotopes, it is proposed that small herbivorous mammals mainly (or totally) rely on C3 grasses as food supply, and there is few or no distribution of C4 grasses at the ecosystem. The results reflect our previous study on the isotope patterns of plant species. Thus, stable carbon isotope analysis of muscles provides a method to address dietary selection and dietary variability in herbivores. In addition, stable carbon isotopic analyses can be used to address changes in vegetation distributions in ecosystem and paleovegetaion and paleoclimate.

黄土高原中部60万年来黄土—古土壤序列有机碳同位素研究

Vegetation is very sensitive to climate change. Carbon isotopes in paleosol have been widely used to contruct the propotion of plants using C3 and C4 photosynthetic pathways. δ13C of Loess organic matter were analyzed on the loess- paleosols samples from Jingchuan sections and Luochuan S4—S5 sequence. This paper presents a long carbon isotope time series, covering the last 600kyr. δ13C record of Loess organic matter in Jingchuan is correlated with marine oxygen isotope records. Basing on former research work, this paper discusses temperature, rainfall and P CO2 effect on δ13Corg value. In the interglacial periods, carbon isotope is more sensitive than other proxies and indicates several climate fluctuations. The main conclusions are as follows: 1. Obtained δ13C composition from paleosols and loess sediments in Jingchuan range of -20.0‰ to -24.6‰, the maximum biomass of C4 is 35%, indicating a C3 and C4 mixed steppe with C3 dominated. C4 plant is not always expansion during paleosols periods. The minimum values of Jingchuan section appeared in S4 soil, and the vegetation was almost pure C3 plant at that time. δ13Corg value in S5-2 is also lower than loess in S5, reaching the minimum valus of S5 soil. 2. PCO2 variation has little impact on δ13Corg value in interglacial periods for the last 600kyr. The correlation between δ13Corg value curve and magnetic susceptibility curve as proxy of summer monsoon in general, means summer monsoon drive C4 plant expansion during glacial and interglacial. 3. The lowerδ13Corg values in S4 and S5-2 appear at Jingchuan and Luochuan, suggest origin from woodland or C3 grassland. Whatever vegetation it is, indicate strengthened East Asian summer monsoon and increase of precipitation. C4 plant percentage is lower in S5-1 and S1 which have stronger summer monsoon, than S0 and S2. And it also indicates increase of precipitation.δ13Corg values has not always non-linearity correlation with summer monsoon. 4. The maximum entroy spectral analysis of δ13C values of the last 600kyr indicates there is 21 kyr cycles in Loess sequence. It means that summer monsoon in the Chinese Loess Plateau also has the precession cycles like its origin low latitude.

北天山新生代构造演化与古环境演变

The Tianshan Mountains is located about 1000-2000 km north of the India-Asia suture and is the most outstanding topography in central Asia, with transmeridional length of nearly 2500 km, north-southern wideness of ~ 300-500 km, peaks exceeding 7000 m above sea level (asl.), and average altitude of over 4000 m asl. Much of the modern relief of the Tianshan Range is a result of contraction driven by the collision of the India subcontinent with the southern margin of Asia, which began in early Tertiary and continues today. Understanding where, when and how the deformation of the Tianshan Mountains occurred is essential to decipher the mechanism of intracontinental tectonics, the process of foreland basin evolution and mountain building, and the history of climate change in central Asia. In order to better constrain the Cenozoic building history of the Tianshan Mountains and the climate change in the southern margin of the Junggar Basin, we carried out multiple studies of magnetostratigraphy, sedimentology, and stable isotopes of paleosol carbonate at the Jingou River section, which is located at the Huoerguosi anticline, the westernest one of the second folds and thrust faults zone in the northern piedmont of the Tianshan Mountains. The Jingou River section with a thickness of about 4160 m is continuous in deposits according to the observed gradual change in sedimentary environments and can be divided into five formations: Anjihaihe, Shawan, Taxihe, Dushanzi and Xiyu in upward sequence. Characteristic remamences were isolated by progressive thermal demagnetization, generally between 300 and 680℃. A total of 1133 out of 1607 samples yielded well-defined ChRMs and were used to establish the magnetostratigraphic column of a 3270-m-thick section from the exposed base of the Anjihaihe Formation to the middle of the Xiyu Formation. Two vertebrate fossil sites and a good correlation with the CK95 geomagnetic polarity time scale suggest that the section was deposited from ~30.5 to ~4.6 Ma and the age of the top of the Xiyu formation is ~2.6 Ma based on an extrapolation of the sedimentation rates. A plot of magnetostratigraphic age vs. height at the Jingou River section shows that significant increases in sedimentation rates as well as notable changes in depositional environments occurred at ~26-22.5 Ma, ~13-11 Ma and ~7 Ma, which represent the initial uplift of the Tianshan Mountains and two subsequent rapid uplift events. In addition, changes in sedimentation rates display characteristic alternations between increases and decreases, which probably indicate that the uplift of the Tianshan Mountains was episodic. We discussed the history of C4 biomass and climatic conditions in the southern margin of the Junggur Basin using the stable carbon and oxygen isotope composition of paleosol carbonates from the Jingou River section during ~17.5-6.5 Ma. The δ13C values indicate that the proportion of C4 biomass was uniform and moderate (15-20 %) during the interval of ~17.5-6.5 Ma. We proposed three hypotheses for this pattern of C4 biomass: (1) counteraction of two opposed factors (global cooling since ~15 Ma and thereafter increased dry and seasonality in central Asia) controlling the growth of C4 grasses, (2) variability in abundance of C3 grasses relative to C3 trees and shrubs if vegetation had ever changed in ecosystems, and (3) the higher latitude of the studied region. The δ18O values show a stepwise negative trend since ~13 Ma which may be attributed to three factors: (1) the temperature decreasing gradually after the middle Miocene (~15 Ma), (2) the increasing contribution of the moistures carried by the polar air masses from the Arctic Ocean to precipitation, and (3) the gradual retreat westward and disappearance of the Paratethys Ocean. Among them, which one played a more important role will need further study of the paleoclimate in central Asia.

陆生蜗牛壳体同位素组成及其对生长季节的响应

Stable isotope compositions of land snail shells have a great potential as an indicator of paleoclimatic and paleoenvironmental changes. However, some key issues, such as the relationship of carbon isotope between snail food and local vegetation, and the uncertainty of the dominant factors about snail body fluid changes in oxygen isotope composition, remain less well known, strongly limiting shell isotopic application. In this study, we measure the stable isotope compositions on the shells of both live snails and fossils collected from the Chinese Loess Plateau and a loess sequence at Mangshan, Xingyang, respectively. Based on the analyses, the association of the stable isotope compositions of land snail shells with their growing seasons is investigated. In addition, the climatic and environmental significances of isotopic differences among several snail species are discussed. The main results and conclusions are presented as follows: 1. δ18O values for the shell lip samples of Bradybaena ravida redfieldi range from -6.79‰ to -1.92‰, and parallels to the monthly changes of local rain water δ18O, temperature and humidity. The compatibility of shell lip δ18O with monthly modeled shell δ18O indicates that the shell lip δ18O changes are mainly resulted from the 18O variations of rain-water. The shells of a land snail growing in spring could be enriched in 18O, and those growing in summer depleted in 18O. 2. Carbon isotope compositions of snail shells are controlled by their diet, which is affected by the relative proportion of C3 to C4. There are some differences in carbon isotopic compositions among different snail species, especially between P. orphana and V. tenera or P. aeoli. Shell δ13C for P. orphana is the most positive with an average of -5.88 ± 2.54 ‰. The C4 plant fraction of the food for “cold-aridiphilous” taxa, P. aeoli and V. tenera, is distinctly lower than that for “thermo-humidiphilous” taxa, P. orphana, indicating that summer is likely to be the main active season of P. orphana and spring of P. aeoli and V. tenera. Therefore, some discrepancy of carbon isotopic compositions among different species may be related to snail active season. 3. δ13C values among different species have a certain degree of positive correlation, which may be influenced by local vegetation ecosystem. δ13C value of the snail shells (especially P. orphana) shows an eastward increasing trend and consists with the variations of C4 plants biomass in Loess Plateau. The result shows that the carbon isotope in local vegetation ecosystem is one of the main factors influencing δ13C values of snail food. Therefore, both carbon isotopes of local vegetation ecosystem and snail active season contribute to the carbon isotopic differences among different snail species and in different areas. 4. δ13C values of living snail shells and soil organic matter have a positive correlation with each other, which further supports the view that carbon isotope in local vegetation ecosystem is one of the main factors influencing δ13C values of snail food. However, the range of δ13C values of snail food for various species in response to carbon isotope in local vegetation ecosystem is different. It is suggested that 13C enrichment of snail shells relative to local vegetation ecosystem has a potential to indicate snail active season and the degree of climate temperature and humidity. 5. There is a significant negative correlation between carbon and oxygen isotopic compositions of living snail shells in Loess Plateau. This result further supports that snail active season can be inferred based on the shell carbon and oxygen isotopic compositions. Moreover, there are some positive correlations between mean annual temperature and differences of shell δ13C values ( 13CV. tenera-P. orphana) and that of δ18O values ( 18OV. tenera-P. orphana) for P. orphana, a typical “thermo-humidiphilous” taxa, and V. tenera, a typical “cold-aridiphilous” taxa, respectively. It shows that  13CV. tenera-P. orphana and  18OV. tenera-P. orphana may have a potential to indicate mean annual temperature or the length of biological growing season. 6. Stable isotopes of land snail shell in the Mangshan loess sequence show that the shell δ18O value of “cold-aridiphilous” taxa V. tenera is more positive than “thermo-humidiphilous” taxa P. orphana and δ13C value of the former is more negative than the latter. In addition, the shell δ18O value of V. tenera varies significantly in different period. During the last glacial maximum, its δ18O value with an average of -7.89 ‰ is more negative than that (-5.88 ‰) from the last deglaciation to the early Holocene. This phenomenon indicates that its growing season during different period is significantly different. It tends to grow in summer in last glacial maximum. With climate warming, it prefers growing in spring with relatively low temperature. While the shell δ18O value of P. orphana varies in a little range, which shows that its activity season is shorter and mainly in summer. These results further support that the change of the snail growing season is one of the main factors of differences of carbon isotopic compositions among different snail species and varies with time. Furthermore, it is consistent that changes in magnetic susceptibility and trend of differences of shell δ18O values and δ13C values respectively between the two snail fossils. It is further testified that 13CV. tenera-P. orphana and  18OV. tenera-P. orphana may have a potential to indicate mean annual temperature or the length of biological growing season.

碳、氧稳定同位素分析在古环境研究中的应用

A number of proxy records of paleoenvironment using stable isotopes could show the history of past environmental changes. These archives include peat and lake sediments, loess-paleosot sequence, fossil mammals and stalagmite, and so on. The stable isotopic composition of carbonate and organic matter and frequency magnetic susceptibility from Tianshuigou and Yuanlei loess-palesol sequence can be used to give estimates of the paleoenvironmental history of Dali, and even of the whole Chinese Loess Plateau during the last 250ka. Features of the High Temperature and Large Precipitation Event in the Tibet Plateau and its adjacent area during 40~30kaBP had been studied by Professor Shi Y. In this dissertation, its impact on Chinese Loess Plateau has been discussed again. Carbon and oxygen isotopic ratios, magnetic susceptibility and frequency magnetic susceptibility in Tianshuigou and Yuanlei profiles show that the Event in this area is not so stronger as the Tibet Plateau. The carbon isotopic composition of organic matter in Tianshuigou, Yuanlei, dingcun and Jingcun loess-palesol sequences are indicative of major changes in the paleovagetation between terrace and plain of the Chinese Loess Plateau. Water is one of the most important factors adjusting the relative biomass of C4 plant in terrestrial ecosystems. Stable carbon isotope ratio of vertebrate tooth enamel is used increasingly to reconstruct environmental and ecological information modern and ancient ecosystems. The SI3C value of tooth enamel bioapatites can distinguish between browsers and grazers. Data from typical grassland of Inter Mongolia, the Alpine meadow of Qinghai-Tibet Plateau and the Yaluzangbu Great Canyon indicate that diets of mammals could record the relative biomass of C4 plant only in the C4 dominated ecosystem. In a C3 dominated ecosystem, diet of mammals would include more C3 plants than vegetation. According to Professor Cerling, proxy records from North and South America, Africa and Pakistan show that at the end of the Miocene (between 8Ma to 6 Ma) there was a global expansion of CA biomass, probably when atmospheric CO2 levels declined. Thus, "C4 world" and "CO2 starvation" are put forward. In this dissertation, carbon isotopes of fossil tooth such as Equus sanmeniensis and Hipparion chiai from Linxia, China reveal that there is a C3 dominated ecosystem in the late Miocene. Diets of ancient mammals in Linxia are not evidence of global expansion of C4 biomass.

湛江湖光岩玛珥湖55ka以来植硅体化石记录及古环境变迁

The study of biogenic proxy of tropical and subtropical regions provides important evidence about the process and history of vegetation and environmental changes, and is of globally importance for understanding the dynamic mechanism of paleoclimatic and paleoenvironmental changes. The sediments from the Huguangyan Maar lake in Guangdong Province offer a continuous high-resolution record of the past 55 ka about environmental and vegetational changes. The studies of chronology, and physical, chemical environmental proxies have provided much important information about the paleoenvironmental and paleoclimatic histories. The phytolith, a new biogenicl proxy, has been used to determine the nature and types of plants in this area since the last 55 ka. This study presents a preliminary result about the characteristics of phytolith shapes, the variations of the fossils assemblages, and their significance for environmental changes. Moreover, the author probes the process of special specie evolution and their relationship to climatic parameters. The history of fire has been reconstructed based on the variations in charcoals. The main results and conclusions include: 28 types of phytoliths from 233 samples have been identified. Their environmental meanings are investigated in detail. Based on the variations in phytolith associations, the history and process of climatic and environmental changes in the last 55 kaBP have been established for this region. Climatic changes experienced eight intervals during this period, showing the variations of hot-humid to cool-try climate in the ten thousands years scale, and a shorter dry-hot climate condition in millennial scale. The history of palm plant has been established in this region. Two peaks appeared from 55-39 ka and since the Holocene. Plants in Bambusoideae have been growing in this area all the period, representing the impact of the East Asian summer monsoon. Bamboo plants have similar tendency in their abundance to palm plants, but with a lag of 1-2 ka BP. Panicoideae plants, the representative of C4 plants, have 6 flourishing periods occurred at 54.5, 44, 41.5, 32.5, 14, and 10 kaBP, respectively, reflecting 6 times short-term arid events. Charcoal record from the Huguang Marr lake reveals the history of nature fire, that mostly happened in dry period of last glacial from 55-10 kaBP, centered at 50-45, 40-35, 30-25, and 20-15kaBP, showing about a cycle of 10,000 years.

稳定碳同位素示踪农林生态转换系统中土壤有机制裁的迁移和赋存规律

为了探讨土壤有机质在降解过程中的迁移、赋存规律，利用C3、C4植物的δ13C值差异，通过分析土壤的不同粒径组分和比重组分中土壤有机质的δ13C值，表明，粗砂中的土壤有机质年代最新，细粉中的土壤有机质年代最老，有机质在降解过程中，在土壤各粒径组分中的迁移次序是：粗砂→细砂→粗粉→粘土→细粉；土壤重组分中的有机质年代较老，以降解充分、稳定的有机无机复合体为主，轻组分中的有机质含有更多的降解尚不充分、活性较大的有机质.