The distribution and economic losses of alien species invasion to China

Invasive alien species have become one of the most serious environmental issues in the world. Data of taxon, origin, pathway, and environmental impacts of invasive alien microorganisms, invertebrates, amphibians and reptiles, fish, birds, mammals, herbs, trees, and, marine organisms in terrestrial, aquatic, and marine ecosystems of China were analyzed during 2001 and 2003, based on literature retrieval and field survey. There were 283 invasive alien species in China, and the number of species of invasive alien microorganisms, aquatic plants, terrestrial plants, aquatic invertebrates, terrestrial invertebrates, amphibians and reptiles, fish, and mammals were 19, 18, 170, 25, 33, 3, 10, and 5, respectively. The proportion of invasive alien species originated from America, Europe, Asia, Africa, and Oceania were 55.1, 21.7, 9.9, 8.1, and 0.6%, respectively. Methods for estimation of direct economic losses to agriculture, forestry, stockbreeding, fishery, road and water transportation, storage, water conservancy, environment and public facilities, and human health were established. Methods for estimation of indirect economic losses caused by invasive alien species to service functions of forest ecosystems, agricultural ecosystems, grassland ecosystems, and wetland ecosystems were also established. The total economic losses caused by invasive alien species to China were to the time of USD 14.45 billion, with direct and indirect economic losses accounting for 16.59% and 83.41% of total economic losses, respectively.

The status and causes of alien species invasion in China

Data of classification, origin, pathway and environmental impacts of invasive alien micro-organisms, invertebrates, amphibians and reptiles, fish, birds, mammals, weeds, trees, and marine organisms in terrestrial, aquatic and marine ecosystems of China, were analyzed, based on literature retrieval, field survey and consultation. Some 283 invasive alien species were recorded in China, including 19 invasive alien micro-organisms, 18 aquatic plants, 170 terrestrial plants, 25 aquatic invertebrates, 33 terrestrial invertebrates, 3 amphibians and reptiles, 10 fish, and 5 mammals. Of the invasive alien species, 55.1% originated from North and South America, 21.7% from Europe, 9.9% from Asia, 8.1% from Africa and 0.6% from Oceania. Many institutions and individuals in China lack adequate knowledge of ecological and environmental consequences caused by invasive alien species, with some ignorance of the dangerous invasion in the introduction of alien species. For instance, 50.0% of invasive alien plants were intentionally introduced as pasture, feedingstuff, ornamental plants, textile plants, medicinal plants, vegetables, or lawn plants, 25% of alien invasive animals were intentionally introduced for cultivation, ornament, or biological control, In addition, more efforts are being made in the introduction of alien species, and little attention is paid on the management of introduced alien species, which may cause their escape into natural environment and potential threats to the environment. There were also gaps in quarantine system in China. All microorganisms were unintentionally introduced, through timber, seedling, flowerpot, or soil; 76.3% of alien invasive animals invaded through commodity or transportation facility because of the failure of quarantine. Therefore, quarantine measures should be strictly implemented; and meanwhile the intentional introduction of alien species should be strictly managed and a system of risk assessment should be implemented.

Cytological and Molecular Identification of Alien Chromatin in Giant Spike Wheat Germplasm

Alien chromosomes of twelve giant spike wheat germplasm lines were identified by C-banding, genomic in situ hybridization (GISH), sequence characterized amplified region (SCAR), and random amplified polymorphic DNA (RAPD). All lines showed a chromosome number of 2n = 42, five of them carried both a pair of wheat-rye (Triticum aestivum-Secale cereal) 1BL/1RS translocation chromosomes and a pair of Agropyron intermedium (Ai) chromosomes, three carried a pair of Ai chromosomes only, three others carried a pair of 1BL/1RS chromosomes only, and one carried neither 1BL/1BS nor Ai chromosome. Further identification revealed that the identical Ai chromosome in these germplasm lines substituted the chromosome 2D of common wheat (Triticum aestivum L.), designated as 2Ai. The genetic implication and further utilization of 2Ai in wheat improvement were also discussed.

我国严重威胁性外来入侵植物入侵与扩散历史过程重建及其潜在分布区的预测

外来生物入侵已经在世界范围内造成严重的危害，它不仅导致生物多样性的减少和丧失而且威胁着全球的生态环境和经济发展。入侵种在入侵区域的种群扩散是入侵种带来风险的最根本问题，也是其造成危害的重要原因。研究入侵物种的扩散规律可以了解其在入侵地的入侵状况和扩散趋势，这对制定合理的控制措施具有重要意义。本研究选取14种在我国具有较强威胁性的外来入侵植物，通过对其入侵历史动态的分析，判断其在我国的入侵与扩散阶段，进而预测其在我国的潜在分布区。这14种外来植物为紫茎泽兰（Ageratina adenophora）、土荆芥 （Chenopodium ambrosioides.）、喜旱莲子草（Alternanthera philoxeroides）、反枝苋（Amaranthus retroflexus）、刺苋（Amaranthus spinosus）、皱果苋（Amaranthus viridis）、北美独行菜（Lepidium virginicum）、藿香蓟（Ageratum conyzoides）、钻形紫菀（Aster subulatus）、小蓬草（Conyza canadensis）、一年蓬（Erigeron annuus）、牛膝菊（Galinsoga paviflora）、飞机草（Eupatorium odorata）和北美商陆（Phytolacca americana）。 　　紫茎泽兰最早于20世纪40年代入侵我国，经过1940—1960年长达20年的时滞期，紫茎泽兰开始在云南及其临近的省份如四川、贵州和广西迅速扩散。其中，紫茎泽兰在南亚热带和中亚热带气候条件下的扩散速度为20公里/年，而在垂直地带性北亚热带地区的扩散速度为6.8公里/年。紫茎泽兰仍没有入侵到垂直地带性暖温带地区。尽管1990年后，紫茎泽兰在云南基本停止扩散，但其在邻近省（市）的快速传播表明紫茎泽兰在我国仍处在扩散阶段，还没有达到饱和阶段。生态位模型预测结果和紫茎泽兰在已经入侵地区扩散的地理生态式样基本相符。我国南部及中南部地区的气候条件十分适合紫茎泽兰生长。而在华中地区，由于环境条件不太适宜，其扩散速度会相对较慢。我国北部和西北部的气候条件完全不适合紫茎泽兰生存。因此，我国南部和中南部广大未入侵地区将会受到紫茎泽兰入侵和快速扩散的严重威胁，对此应该立即采取紧急措施。 　　自从紫茎泽兰于1978年首次入侵四川省以来，已经在四川、重庆和湖北大面积扩散。紫茎泽兰在此新近入侵区域主要沿河流、公路、铁路扩散。其中沿安宁河、108国道和成昆铁路向北扩散的平均速度为19公里/年，而沿金沙江－长江向东北扩散的平均速度为33公里/年。特别是2000年以后，紫茎泽兰沿金沙江－长江的扩散速度达到了88公里/年。紫茎泽兰得以如此迅速扩散是其本身生物学特性和当地地理生态特点多种因素之间一系列耦合关系共同作用的结果。人类活动和1998年金沙江－长江特大洪水也促进了紫茎泽兰在该地区的扩散。另一方面，紫茎泽兰在新近入侵地区的垂直分布范围说明随海拔高度上升所引起的垂直地带性气候变冷是紫茎泽兰入侵和扩散的自然限制条件。 　　此外，通过对其余13种外来入侵植物入侵历史过程重建发现，除了牛膝菊、反枝苋和皱果苋最早入侵地位于内陆地区以外，其余10种外来入侵植物的最早入侵地都位于我国的东部、南部沿海和西南边境地区。这13种外来植物通常不是通过单一途径传入，而是通过两种或多种途径传入不同的地点。相应地，入侵后也呈现不同的扩散模式。这13种外来植物在我国大体上包括5种入侵和扩散式样即1）从南部沿海和西南边境分别向内陆扩散，如霍香蓟、飞机草，北美商陆;2）从东部沿海向内陆扩散，例如钻形紫菀，小蓬草、北美独行菜和喜旱莲子草;3）从东部沿海、南部沿海和西南边境分别向内陆扩散，如刺苋;4）从南部沿海向内陆扩散，如土荆芥;5）从最早入侵的内陆地区向周边地区扩散，如反枝苋、牛膝菊和皱果苋。分布区动态分析显示当前这13种外来入侵植物在我国都还处在扩散阶段，而且有些外来植物还处在快速扩散阶段，如飞机草。 　　在上述研究基础上，我们对这13种外来入侵植物开展了生态位模型适生区预测和比较分析。并且结合其扩散动态和当前分布现状，我们对其潜在的分布区及扩散趋势进行了系统分析和预测。飞机草、土荆芥、霍香蓟、牛膝菊和北美商陆，这5种外来植物的现有分布区明显小于其在我国的适生区，因此它们在我国的潜在分布区很广，应给予足够的重视。喜旱莲子草、反枝苋、皱果苋、北美独行菜、一年蓬、钻行紫菀和北美商陆在我国的入侵范围与其适生区域之间基本重合，但在其入侵范围内仍存在大面积的未入侵区域。这些未入侵地区通常被已入侵区域所包围，因此也应当给予足够的重视。刺苋和小蓬草在我国的潜在的分布区相对较小，这些植物已经基本上完全入侵了其适生区。因此，这些植物在我国向临近区域继续扩散的可能性不大。 　　

寄生植物在入侵植物防治中的作用——以两种菟丝子为例

生物入侵在全世界广泛发生，目前已经受到全球关注。入侵生物对群落生物多样性和生态系统功能造成严重威胁，导致严重的环境问题和惨重的经济损失。薇甘菊(Mikania micrantha)、五爪金龙(Ipomoea cairica)和南美蟛蜞菊(Wedelia trilobata)是我国华南地区危害最严重的三种外来入侵种，其中以薇甘菊危害最严重，是世界十大有害杂草之一。从20世纪80年代发生以来，薇甘菊已在我国广东农林区域造成严重危害。 机械防治、化学防治和传统的生物防治等治理措施，未能有效治理外来入侵种的危害，直到使用本地种菟丝子(Cuscuta spp)的防治策略。与从原产地引进有害生物天敌的传统生物防治方法不同，本地种由于适应当地气候且与其他物种协同进化，因此，对生态环境潜在的负作用小。从2000年，被发现寄生和抑制薇甘菊之后，菟丝子被认为是防治薇甘菊的有效措施。 为了探讨菟丝子寄生对外来入侵种的治理，及对入侵群落的恢复，本研究在内伶仃岛的林地(入侵种群落被引入菟丝子寄生1-4年)，以及东莞、深圳和海丰的干扰样地(入侵种群落被菟丝子自然寄生5年以上)开展野外调查。在每个样地分别设立外来种入侵亚群和菟丝子治理亚群，通过测定群落结构与组成、土壤性质与养分含量，以及外来种和菟丝子的生长与养分含量等参数之后，本研究得出以下主要结论。 (1) 虽然，被寄生的外来入侵种薇甘菊、五爪金龙和南美蟛蜞菊通过调节资源分配以抵御南方菟丝子(Cuscuta australis)的寄生影响，但是，菟丝子寄生导致外来入侵种生物量降低、繁殖能力下降、养分含量降低。虽然，很多寄生植物都是广谱寄生，能同时寄生多种寄主植物，但是，在本研究的被入侵的群落中，菟丝子主要寄生外来入侵植物。尤其是寄生于南美蟛蜞菊和薇甘菊的菟丝子，生长旺盛、繁殖能力强，表现出高度的适应性。因此，菟丝子对外来入侵种(南美蟛蜞菊和薇甘菊)有寄生偏好性，并对本地种的负面影响小。 (2) 通过吸收寄主的养分，田野菟丝子(Cuscuta campestris)有效地抑制了薇甘菊的危害。由于入侵种的凋落物养分含量高且分解效率高，而且，菟丝子能够促进其它凋落物的分解，并使难以被植物吸收的养分转化成易于被吸收利用的状态。因此，菟丝子与薇甘菊的寄生作用导致土壤养分含量的升高。在薇甘菊被抑制之后，本地种利用丰富的土壤养分资源，提高生长适应性，增强抵抗入侵的能力，甚至抵制薇甘菊的再生。 (3) 菟丝子的寄生作用改变了外来寄主与本地非寄主的竞争平衡，促进本地植物的生长与重建。在外来种被抑制之后，本地种的丰度和群落的物种多样性逐渐增加。本地种如：野葛(Pueraria lobata)和芦苇(Phragmites australis)，取代了入侵群落中的入侵种，成了群落的优势种。而其它原先被薇甘菊抑制的本地草本、藤本和灌木，在引入菟丝子防治之后长势较好。群落稳定性与物种多样性密切相关，被治理群落本地种的增加有利于群落的演替与稳定。 (4) 被干扰的生态系统往往更容易被外来种入侵，而外来入侵种又常导致人工干扰生境的严重退化。在人工干扰样地的菟丝子对薇甘菊的抑制效果与在林地的效果一致，导致被寄生的薇甘菊生长衰退、养分竞争能力下降、入侵危害能力降低。而在薇甘菊被菟丝子治理之后，土壤养分资源增加，入侵群落的物种丰度和生物多样性提高。本 地种的重建与本地群落的恢复密切相关，利于本地被治理群落的稳定，促进被干扰植被的恢复。 菟丝子是一种治理外来入侵种危害的有效措施，适用于破碎的生境和被干扰的生态系统，尤其是在采用目前防治措施难以治理的情况下。本研究为本地种防治外来入侵种提供科学依据，且表明以入侵地的本地种治理外来入侵种有可能成为有效且可持续发展的生物防治策略。

Threat and management strategies of potentially invasive insects in China

The Global Invasive Species Database, GISD, comprises 27 species of the most significant invasive alien insects in the world (through November, 2005), 6 of which are originally native to China, 11 are established in China, and 10 have a potential invasion

Zoospores of Undaria pinnatifida: their efficiency to attach under different water velocities and conjugation behavior during attachment

In the invading course of Undaria pinnatifida, zoospore attachment in a dynamically changed subtidal water environment is crucial for the establishment of a potential population in alien waters. Among many abiotic factors that may interfere with the attachment process, water velocity is the most important one. In this investigation, the effect of water velocity on zoospore attachment of U. pinnatifida was investigated in an artificially designed system. It was found that freshly released zoospores that were transported by water flowing at 0 similar to 16 cm/s showed no difficulty in attaching the smooth surface. Zoospore attachment decreased at elevated water flowing rates. At 70 cm/s no spore attachment occurred. Spores that have settled on glass slide for up to I h could not be stripped away by flowing water at a rate of 129 cm/s, the same was true of the 20 d old filamentous gametophytes. It was found that more than 70% of free-swimming zoospores tended to settle down adjacent to the settled spores and formed conjugated clusters from two up to a few hundred cells in still culture.

Pollinator shift and reproductive performance of the qinghai-tibetan plateau endemic and endangered Swertia przewalskii (Gentianaceae)

Reproductive failure results in many plant species becoming endangered. However, little is known of how and to what extent pollinator shifts affect reproductive performance of endangered species as a result of the artificial introduction of alien insects. In this study we examined breeding systems, visitor species, visiting frequency and seed set coefficients of Swertia przewalskii in two years that had different dominant pollinator species (native vs. alien). Flowers of this species were protandrous and herkogamous and insects were needed for the production of seeds. The stigmatic receptivity of this species was shorter than for other gentians. No significant difference in seed set coefficient was found for hand-pollinated plants between the two years, indicating that pollinator shift only had a minor effect on this plant's breeding system. The commonest pollinators in 2002 were native bumblebees, alien honeybees and occasional solitary bees, however, only alien honeybees were observed in 2004. The flower visitation rate in both years was relatively high, although the total visit frequency decreased significantly in 2004. The control flowers without any treatment produced significantly fewer seed sets in 2004 than in 2002. In the past decade the seed production of this species may have partly decreased due to pollination by alien honeybees, however, we suggest that they might have acted as alternative pollinators ensuring seed production of S. przewalskii when native pollinators were unavailable. The main reason that this plant is endangered is probably the result of habitat destruction, but changes in land use, namely intensified agricultural practice and unfavorable animal husbandry have also contributed to its decline. We recommend that in-situ conservation, including the establishment of a protected area, is the best way to preserve this species effectively.

Pg震相走时的各向异性影响及各向异性结构成像

As the first arrival of seismic phase in deep seismic sounding, Pg is the important data for studying the attributes of the sedimentary layers and the shape of crystalline basement because of its high intensity and reliable detection. Conventionally, the sedimentary cover is expressed as isotropic, linear increasing model in the interpretation of Pg event. Actually, the sedimentary medium should be anisotropic as preferred cracks or fractures and thin layers are common features in the upper crust, so the interpretation of Pg event needs to be taken account of seismic velocity anisotropy. Traveltime calculation is the base of data processing and interpretation. Here, we only study the type of elliptical anisotropy for the poor quality and insufficiency of DSS data. In this thesis, we first investigate the meaning of elliptical anisotropy in the study of crustal structure and attribute, then derive Pg event’s traveltime-offset relationship by assuming a linear increasing velocity model with elliptical anisotropy and present the invert scheme from Pg traveltime-offset dataset to seismic velocity and its anisotropy of shallow crustal structure. We compare the Pg traveltime calculated by our analytic formula with numerical calculating method to test the accuracy. To get the lateral variation of elliptical anisotropy along the profiling, a tomography inversion method with the derived formula is presented, where the profile is divided into rectangles. Anisotropic imaging of crustal structure and attribute is efficient method for crust study. The imaging result can help us interprete the seismic data and discover the attribute of the rock to analyze the interaction between layers. Traveltime calculation is the base of image. Base on the ray tracing equations, the paper present a realization of three dimension of layer model with arbitrary anisotropic type and an example of Pg traveltime calculation in arbitrary anisotropic type is presented. The traveltime calculation method is complex and it only adapts to nonlinear inversion. Perturbation method of travel-time calculation in anisotropy is the linearization approach. It establishes the direct relation between seismic parameters and travetime and it is fit for inversion in anisotropic structural imaging. The thesis presents a P-wave imaging method of layer media for TTI. Southeastern China is an important part of the tectonic framework concerning the continental margin of eastern China and is commonly assumed to comprise the Yangtze block and the Cathaysia block, the two major tectonic units in the region. It’s a typical geological and geophysical zone. In this part, we fit the traveltime of Pg phase by the raytracing numerical method. But the method is not suitable here because the inefficiency of numerical method and the method itself. By the analytic method, we fit the Pg and Sg and get the lateral variation of elliptical anisotropy and then discuss its implication. The northeastern margin of Qinghai-Tibetan plateau is typical because it is the joint area of Eurasian plate and Indian plate and many strong earthquakes have occurred there in recent years．We use the Pg data to get elliptical anisotropic variation and discuss the possible meaning.

青藏高原东部长周期大地电磁测深研究

As a complement to conventional MT, Long-period Magnetotellurics (LMT) has been developed at low frequency for soundings of deep electric structures. Eastern Himalayan Syntaxis (EHS) and surrounding area is a key place for the study of dynamics of the uplift of Tibetan plateau. Experiments in the pioneer studies for EHS3D project showed that the study area shares an unusual low resistive crust and upper mantle. Conventional MT could not provide sufficient information about the deep structures of the study area that requested long period MT measurement to be complemented. This thesis presents the LMT studies in eastern Tibet along the EHS3D-3 Profile from Xiachayu to Yushu including data acquisition, processing, inversion and interpretation. The effective period of the measured LMT signals extend from 10s up to 30000s for the duration more than one week measurement. The resulting model shows that the LMT sounding coincides with the MT data in overlapped periods. Especially the induction arrows and tippers derived from LMT data provide more information about the base of the conductors beneath the plateau with higher resolution. Anomalous induction coefficients and 2-D model suggest extensive conductive bodies beneath Lhasa block and Qiangtang terrain which would be a possible evidence for partial melt and fluids at depth.