辽河三角洲植被结构、功能及其驱动机制

辽河三角洲优越的植被生态系统维系着多种生态功能，使该地区成为全国著名的商品粮基地、造纸原料基地和旅游基地。但是，气候变化和人为干扰使得辽河三角洲的植被结构发生了显著变化，影响到植被功能的发挥。 为了应对气候变化和人为干扰对辽河三角洲植被造成的不利影响，本论文围绕植被结构和生产功能，从空间和时间方面，重点阐述了辽河三角洲植被的结构及其驱动机制；辽河三角洲植被生产功能及其驱动机制。 采用的研究方法包括遥感解译、样带调查和全面调查。通过遥感解译方法获取各植被类型的面积、分布及其变化信息，以研究植被的空间分布格局及其变化。通过样带调查方法，获取植被类型、土壤和水文等信息，并结合规范对应分析和偏相关分析等，研究植被空间分布格局的驱动机制。通过全面调查方法，获取植被净第一性生产力、粮食产量、土壤和水文等信息，并结合地理信息系统(GIS)的插值分析和相关分析等，研究植被生产功能的空间分布格局及其驱动机制。主要结论如下： 1. 植被组成和空间格局：辽河三角洲植被主要由自然湿地植被、人工湿地植被、自然旱地植被、人工旱地植被四大植被类型组成。其中，面积最大的3种植被是玉米、水稻和芦苇。四大植被类型以双台子河口为中心，基本上呈现半环状分布格局。 2. 植被空间格局变化：1988～2006年辽河三角洲植被空间格局发生了显著变化，主要植被类型分布趋于集中，形成了一些较大的斑块，而不是离散和破碎。从面积上看，水稻是面积增加最多的植被类型；玉米是面积减少最多的植被类型。从变化速率看，水稻、玉米和芦苇的变化幅度都较大，分别为33.2%、-16.1%和-23.2% 。 3. 植被空间格局形成机制：辽河三角洲植被分布格局不是由气候因子决定的，而是由土壤因子决定。土壤可溶性盐是决定植被分布格局最重要的环境因子，其次是土壤含水量。 4. 植被生产功能：辽河三角洲植被具有极高的生产力。其中，玉米、水稻和芦苇3种主要植被的地上净第一性生产力分别为30,485、18,248和17,440 kg/(ha•a)。玉米和水稻单位面积粮食产量也非常高，分别为14,813和10,365 kg/(ha•a)。 5. 植被生产功能年际变化：辽河三角洲植被生产力存在明显的年际波动。1992～2005 年间玉米和水稻粮食产量呈现显著的年际波动；1949～1990 年间芦苇产量不仅存在较明显的年际波动，而且呈现非常显著的增加趋势。 6. 植被生产功能年际变化的驱动机制：气候因子是玉米和水稻粮食产量年际变化的主要驱动因子，气候因子对玉米和水稻粮食产量的影响远远大于人为因子（农业人口、施肥量、灌溉面积）的影响。气候因子和人为因子对芦苇产量年际变化的影响都非常显著。在气候因子中，年日照数是驱动玉米产量年际波动的主导气候因子；年降水量是驱动水稻产量年际波动的主导气候因子；年蒸发量是驱动芦苇产量年际波动的主导气候因子。 7. 植被生产功能空间格局：植被地上净第一性生产力存在显著的空间差异，表现为一种环形空间分布格局，三角洲中部较低，四周地区较高。这种空间分布格局表明，在辽河三角洲，植被地上净第一性生产力最高的不是湿地植被，而是周围旱地植被。 8. 植被生产功能空间格局的形成机制：土壤含水量和海拔是驱动辽河三角洲植被生产力空间格局的主要因子；土壤盐度、土壤pH和土壤容重对植被生产力的空间格局影响不大。土壤营养元素(氮、磷、钾) 对植被生产力的空间格局几乎没有影响。

Investigations into the perplexing interrelationship of the Genus Takifugu Abe, 1949 (Tetraodontiformes, Tetraodontidae)

The phylogenetic relationships within the genus Takifugu Abe, 1949 (Tetraodontiformes, Tetraodontidae) remain unresolved. Because of the use of Takifugu as model organisms, the resolution of these relationships is crucial for the interpretation of evolutionary trends in biology. Pufferfishes of this genus are comprised of a comparatively small number of species and are mainly distributed along the coastal region of the western part of the Sea of Japan and the coastline of China. Mitochondrial gene sequences were employed to test the phylogenetic hypotheses within the genus. Seventeen species of the genus were examined. Molecular phylogenetic trees were constructed using the maximum parsimony, neighbor-joining, maximum likelihood and Bayesian methods. Our hypothesis of internal relationships within the genus differs from previous hypotheses. Our results indicate that (1) the genus Takifugu is a monophyletic assemblage; (2) the genus is divided into 6 subgroups based on the molecular data; and (3) there is low genetic diversity among the species within this genus. In addition, speciation within Takifugu appears to be driven by hybridization and isolation by distribution. Our results also suggested that the taxonomy in the genus should be clarified based on both molecular and morphological data.

Phylogeny of diplozoids in five genera of the subfamily diplozoinae palombi, 1949 as inferred from ITS-2 rDNA sequences

The phylogenetic relationship of 5 genera, i.e. Diplozoon Nordmann, 1832, Paradiplozoon Achmerov, 1974, Inustiatus Khotenovsky, 1978, Sindiplozoon Khotenovsky, 1981, and Eudiplozoon Khotenovsky, 1985 in the subfamily Diplozoinae Palombi, 1949 (Monogenea, Polyopisthocotylea) was inferred from rDNA ITS-2 region using neighbour-joining (NJ), maximum likelihood (ML) and Bayesian methods. The phylogenetic trees produced by using NJ, ML and Bayesian methods exhibit essentially the same topology. Surprisingly, freshwater species of Paradiplozoon from Europe clustered together with species of Diplozoon, but separated from Chinese Paradiplozoon species. The results of molecular phylogeny and lower level of divergence (4(.)1-15(.)7%) in ITS-2 rDNA among Paradiplozoon from Europe and Diplozoon and, on the other hand, high level of divergence (45(.)3-53(.)7%) among Paradiplozoon species from Europe and China might indicate the non-monophyletic origin of the genus Paradiplozoon. Also, the generic status of European Paradiplozoon needs to be revised. The species of Paradiplozoon in China is a basal group in Diplozoinae as revealed by NJ and Bayesian methods, and Sindiplozoon appears to be closely related to European Paradiplozoon and Diplozoon. with their relationship to Eudiplozoon and Inustiatus being unresolved.

Analytical intercomparison results from the 1990 Intergovernmental Oceanographic Commission open-ocean baseline survey for trace metals: Atlantic Ocean

“Dissolved” (< 0.4 μm filtered) and “total dissolvable” (unfiltered) trace element samples were collected using “clean” sampling techniques from four vertical profiles in the eastern Atlantic Ocean on the first IOC Trace Metals Baseline expedition. The analytical results obtained by 9 participating laboratories for Mn, Fe, Co, Ni, Cu, Zn, Cd, Pb, and Se on samples from station 4 in the northeast Atlantic have been evaluated with respect to accuracy and precision (intercomparability). The data variability among the reporting laboratories was expressed as 2 × SD for a given element and depth, and was comparable to the 95% confidence interval reported for the NASS seawater reference standards (representing analytical variability only). The discrepancies between reporting laboratories appear to be due to inaccuracies in standardization (analytical calibration), blank correction, and/or extraction efficiency corrections.Several of the sampling bottles used at this station were not adequately pre-cleaned (anomalous Pb results). The sample filtration process did not appear to have been a source of contamination for either dissolved or particulate trace elements. The trace metal profiles agree in general with previously reported profiles from the Atlantic Ocean. We conclude that the sampling and analytical methods we have employed for this effort, while still in need of improvement, are sufficient for obtaining accurate concentration data on most trace metals in the major water masses of the oceans, and to enable some evaluation of the biogeochemical cycling of the metals.

1990～2000年中国土壤碳氮蓄积量与土地利用变化

基于2473个土壤剖面资料和1980年代末~1990年代末陆地卫星TM影像分析中国1990~2000年林地、草地、耕地之间的土地利用变化对土壤碳氮蓄积量的影响。IPCC建议的国家温室气体清单方法计算表明从1990~2000年中国林地、草地、耕地土壤(30cm)有机碳氮库分别损失了77.6±35.2TgC(1Tg=106t)和5.6±2.6TgN,年均损失约7.76TgC/yr和0.56TgN/yr,其中耕地土壤碳库分别增加了79.0±7.7TgC和9.0±0.7TgN,草地土壤碳氮蓄积量分别损失了100.7±25.9TgC和9.8±2.2TgN,林地土壤碳氮蓄积量分别损失了55.9±17.0TgC和4.9±1.1TgN。同时根据中国6大行政区林地、耕地和草地之间的相互转换面积、土壤有机碳氮密度的变化率进行估算,表明土壤(30cm和100cm)有机碳氮蓄积量分别损失了53.7TgC、5.1TgN和99.5TgC、9.4TgN。由于中国不同地区土地利用变化的空间格局差异显著,从而导致东北地区土壤碳氮蓄积量变化较大,而华东地区变化较小。

STUDY ON THE SPATIAL PATTERNS OF LAND-USE CHANGE AND ANALYSES OF DRIVING FORCES IN NORTHEASTERN CHINA DURING 1990-2000

Land-use change is an important aspect of global environment change. It is, in a sense, the direct result of human activities influencing our physical environment. Supported by the dynamic serving system of national resources, including both the environment database and GIS technology, this paper analyzed the land-use change in northeastern China in the past ten years (1990 - 2000). It divides northeastern China into five land-use zones based on the dynamic degree (DD) of land-use: woodland/grassland - arable land conversion zone, dry land - paddy field conversion zone, urban expansion zone, interlocked zone of farming and pasturing, and reclamation and abandoned zone. In the past ten years, land-use change of northeastern China can be generalized as follows: increase of cropland area was obvious, paddy field and dry land increased by 74. 9 and 276. 0 thousand ha respectively; urban area expanded rapidly, area of town and rural residence increased by 76. 8 thousand ha; area of forest and grassland decreased sharply with the amount of 1399. 0 and 1521. 3 thousand ha respectively; area of water body and unused land increased by 148. 4 and 513. 9 thousand ha respectively. Besides a comprehensive analysis of the spatial patterns of land use, this paper also discusses the driving forces in each land-use dynamic zones. The study shows that some key biophysical factors affect conspicuously the conversion of different land- use types. In this paper, the relationships between land- use conversion and DEM, accnmlated temperature(>= 10 degrees C) and precipitation were analysed and represented. We conclude that the land- use changes in northeast China resulted from the change of macro social and economic factors and local physical elements. Rapid population growth and management changes, in some sense, can explain the shaping of woodland/grassland - cropland conversion zone. The conversion from dry land to paddy field in the dry land - paddy field conversion zone, apart from the physical elements change promoting the expansion of paddy field, results from two reasons: one is that the implementation of market-economy in China has given farmers the right to decide what they plant and how they plant their crops, the other factor is originated partially from the change of dietary habit with the social and economic development. The conversion from paddy field to dry land is caused primarily by the shortfall of irrigation water, which in turn is caused by poor water allocation managed by local governments. The shaping of the reclamation and abandoned zone is partially due to the lack of environment protection consciousness among pioneer settlers. The reason for the conversion from grassland to cropland is the relatively higher profits of fanning than that of pasturing in the interlocked zone of farming and pasturing. In northeastern China, the rapid expansion of built-up areas results from two factors: the first is its small number of towns; the second comes from the huge potential for expansion of existing towns and cities. It is noticeable that urban expansion in the northeastern China is characterized by gentle topographic relief and low population density. Physiognomy, transportation and economy exert great influences on the urban expansion.