植物对重金属砷和镉胁迫适应的分子机理初探

随着现代工业的发展，重金属污染日趋严重。重金属污染引发的环境和健康问题在许多国家都有报道，我国的重金属污染状况也不容乐观。土壤和水体中的重金属污染可以通过食物链进入人体，对人类健康造成很大的危害，如诱发癌症 和畸胎等。 植物修复是一种利用植物对重金属或有机污染物的超富集能力清除或减低污染的环境生物技术。植物修复的生物学机制的研究为这项技术走向实用化奠定了基础。植物修复近期的进展可能来自于可更有效地富集重金属的植物品种的选择、土壤条件的改善等;但长远看来，植物修复技术的巨大进步将取决于新的可更好地抵抗重金属或降解有机毒物的基因的鉴定和克隆，并通过转基因技术创造一批新的植物品种，如可迅速大量富集重金属的高生物量的用作环境净化的植物，以及可排拒重金属吸收的粮食、蔬菜和水果等作物。 本研究针对砷污染的植物修复机制，以超富集砷的凤尾蕨属植物——蜈蚣草为试材取得了如下进展： 1． 以从砷污染地区采集的蜈蚣草（Pteris vittataL．）为植物材料，利用抑制消减杂交(SSH)分离了经砷诱导处理与其对照间表达有差异的cDNA片段，以期得到与砷富集密切相关的基因。其中筛选到的一个cDNA片段与ABC transporter (ATP-binding cassette transporter)有较高的同源性。通过RACE方法对该基因进行了克隆，并进行了初步的结构和功能分析。结果表明所获得的PvABCTl (Accession No. AY496966)为一全长cDNA，长度为2165 bp，其中开读框架为1791 bp，编码597个氨基酸。该基因所编码的蛋白中含有2个ABC transporter特性结构域，1个ATP-binding cassette和2个ATP/GTP结合位点(P-loop)，没有明显的跨膜区。 2． 对蜈蚣草在砷胁迫下PvABCT1基因的表达模式进行了研究。转录水平分析表明PvABCT1的表达受砷的诱导。进一步通过PvABCTl-GFP融合基因在洋葱细胞中的表达进行亚细胞定位，结果显示该基因可能定位于细胞质中。 3． 为了研究所克隆的PvABCT1基因的功能，本研究构建了PvABCT1的酵母表达载体，把该基因转入因ACR3基因缺失而对砷敏感的酵母突变株。酵母功能互补实验表明PvABCT1不仅不能与ACR3基因功能互补，反而使酵母对砷的敏感性增加，同时酵母细胞中的砷含量较未转化的酵母细胞增加。即在转入PvABCT1后，酵母细胞吸收了更多的砷。这暗示该基因与蜈蚣草中砷的高吸收有关。 针对食品重金属污染问题，本研究探讨了减低蔬菜对重金属吸收的方法及其 作用机理，取得了如下进展： 1．研究了钙离子和镧离子对镉离子胁迫下生菜种子萌发和植株生长的影响，结果表明在种子萌发时外施4 mM CaCI2或0.04 mg/L La(N03)3均可提高生菜对重金属镉的抗性。 2．通过检测0.5 mM CdCl2胁迫下生菜植株中的镉含量以及外施钙离子或镧离子后相应的镉含量，发现4 mM CaCl2可以增加镉胁迫下生菜植株中镉的积累;而0.04 mg/L La(N03)3可以降低镉胁迫下生菜植株中镉的积累。 3．对生菜中植物络合素合酶基因进行了克隆，通过RT-PCR分析以及植物络合素( phytochelatins，PCs)的检测，探讨了外施钙离子或镧离子对镉胁迫下生菜植株中植物络合素合酶基因在转录水平的表达量、植物络合素含量以及镉的积累三者之间的关系。结果表明：4 mM CaCl2可以提高镉胁迫下生菜植株中植物络合素合酶基因在转录水平的表达以及植物络合素的含量，增加镉的积累;而0.04 mg/L La(N03)3虽然同样可以提高植物络合素合酶基因在转录水平的表达以及植物络合素的含量，却能降低镉胁迫下生菜植株中镉的积累。这暗示外施钙离子可以促进用于重金属污染环境修复的植物对重金属的吸收，而外施镧离子可以用于降低叶菜类蔬菜中重金属镉的积累。

苏铁叶绿体的超微结构和功能及对CO2浓度倍增的响应

本研究首次揭示了七种苏铁类植物叶绿体的超微结构。即苏铁科(Cycadaceae)的攀枝花苏铁(C. panzhihuaensis).苏铁(C. revoluta)、叉叶苏铁(C.micholitzii)、 刺叶苏铁(C.rumphii和多歧苏铁(C.multipinnata)，蕨铁科(Stangeriaceae)的蕨铁(Stangeria eriopus)和泽米科(Zamiaceae)的米德尔堡大苏铁(Encephalortos middelburgensis).根据它们叶绿体内膜结构的不同将其大体分为两种类型：1、阴生型叶绿体：多歧苏铁和刺叶苏铁为此类型，它们的叶绿体类囊体垛叠程度高，基粒垛较宽，单个基粒中类囊体的数量很多，有的甚至上百;2、阳生型叶绿体：攀枝花苏铁、米德尔堡大苏铁、苏铁、蕨铁和刺叶苏铁以及外类群的凤尾蕨(Pteris vittata)的叶绿体均有阳生型叶绿体的特征：类囊体膜垛叠程度低，基粒较小。根据它们叶绿体的结构特征，又将其分为两组： ( 1)攀枝花苏铁，米德尔堡大苏铁和叉叶苏铁叶绿体中均有类囊体膜膨大的现象： (2)苏铁和蕨铁在苏铁类中是比较原始的种类，它们的叶绿体与在系统进化上较苏铁类低等的凤尾蕨的叶绿体中都有几个基粒聚集成簇的现象，说明苏铁类在进化的同时一些较原始的性状仍保留了下来。这些苏铁都在温室相同的条件下生长了两年多，但它们的叶绿体结构仍然能够反应原产地生境特点，说明在长期进化中，叶绿体对环境的适应方式已在基因水平上稳定下来，苏铁类植物不同叶绿体结构的形成有其遗传基础。 多歧苏铁，攀枝花苏铁，叉叶苏铁的叶绿体膜垛叠程度依次降低，与此相应，它们的chla/b和F730/F684依次升高，反应了结构与功能的一致性。 选用具有阳生型叶绿体的攀枝花苏铁和有阴生型叶绿体的多歧苏铁用不同的C02浓度（350 umol mol-l和700umol mol-l）处理后观察其叶绿体结构的变化，结果发现C02浓度倍增对它们的叶绿体影响甚微，而作为对照的无论是C3植物小麦(Triticum italica)还是C4植物谷子(Setaria italica)在C02倍增的条件下叶绿体内均有大量淀粉粒积累，并有膜结构改变。这说明苏铁的叶绿体结构有保守性，这有可能是苏铁类能历经亿万年的沧桑而生存下来的结构基础之一。

Arsenic uptake and speciation in the rootless duckweed Wolffia globosa

Duckweeds are a common macrophyte in paddy and aquatic environments. Here, we investigated arsenic (As) accumulation, speciation and tolerance of the rootless duckweed Wolffia globosa and its potential for As phytofiltration.

When grown with 1 mu M arsenate, W. globosa accumulated two to 10 times more As than four other duckweed or Azolla species tested. W. globosa was able to accumulate > 1000 mg As kg(-1) in frond dry weight (DW), and tolerate up to 400 mg As kg-1 DW. At the low concentration range, uptake rate was similar for arsenate and arsenite, but at the high concentration range, arsenite was taken up at a faster rate.

Arsenite was the predominant As species (c. 90% of the total extractable As) in both arsenate-and arsenite-exposed duckweed. W. globosa was more resistant to external arsenate than arsenite, but showed a similar degree of tolerance internally. W. globosa decreased arsenate in solution rapidly, but also effluxed arsenite.

Wolffia globosa is a strong As accumulator and an interesting model plant to study As uptake and metabolism because of the lack of a root-to-frond translocation

Variation in arsenic accumulation - Hyperaccumulation in ferns and their allies

A range of fern species (45) and their allies, Equisetum (5) and Selaginella (2) species and Psilotum nudum were screened for their ability to hyperaccumulate arsenic, to develop a phylogenetic understanding of this phenomenon. A number of varieties (5) of a known arsenic hyperaccumulator Pteris cretica were additionally included in this study. This study is the first to report members of the Pteris genus that do not hyperaccumulate arsenic, Pteris straminea and tremula. A phylogenetic basis for arsenic accumulation in ferns was investigated. Some orders can accumulate more arsenic than others. Although members of the Equisetales and Blechnales did not hyperaccumulate arsenic, they still accumulated relatively high levels in their fronds, approaching 100 mg kg^-1 when grown on a soil dosed with 100 mg kg^-1 arsenic. Arsenic hyperaccumulation was identified as a phenomenon at the extreme range of fern arsenic accumulation. Ferns that exhibit arsenic hyperaccumulation arrived relatively late in terms of fern evolution, as this character is not exhibited by primitive ferns or their allies.

Recognition of two morpho-types in eastern South American brackens (Pteridium-Dennstaedtiaceae-Polypodiopsida)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Assessment of the Removal Capacity, Tolerance, and Anatomical Adaptation of Different Plant Species to Benzene Contamination

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Efeito fitotóxico e potencial remediador de três espécies vegetais contaminadas com benzeno

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Compound specific stable isotopes, BIT, pollen and spores of Miocene to Pliocene sediments of ODP Hole 175-1085A

Pollen and stable carbon (d13C) and hydrogen (dD) isotope ratios of terrestrial plant wax from the South Atlantic sediment core, ODP Site 1085, is used to reconstruct Miocene to Pliocene changes of vegetation and rainfall regime of western southern Africa. Our results reveal changes in the relative amount of precipitation and indicate a shift of the main moisture source from the Atlantic to the Indian Ocean during the onset of a major aridification 8 Ma ago. We emphasise the importance of declining precipitation during the expansion of C4 and CAM (mainly succulent) vegetation in South Africa. We suggest that the C4 plant expansion resulted from an increased equator-pole temperature gradient caused by the initiation of strong Atlantic Meridional Overturning Circulation following the shoaling of the Central American Seaway during the Late Miocene.

Palynological record and radiocarbon dates for sediment core T89-16, Congo River mouth

We present a high-resolution reconstruction of tropical palaeoenvironmental changes for the last deglacial transition (18 to 9 cal. kyr BP) based on integrated oceanic and terrestrial proxies from a Congo fan core. Pollen, grass cuticle, Pediastrum and dinoflagellate cyst fluxes, sedimentation rates and planktonic foraminiferal d18O ratios, uK37 sea-surface temperature and alkane/alkenone ratio data highlight a series of abrupt changes in Congo River palaeodischarge. A major discharge pulse is registered at around 13.0 cal. kyr BP which we attribute to latitudinal migration of the Intertropical Convergence Zone (ITCZ) during deglaciation. The data indicate abrupt and short-lived changes in the equatorial precipitation regime within a system of monsoonal dynamics forced by precessional cycles. The phases of enhanced Congo discharge stimulated river-induced upwelling and enhanced productivity in the adjacent ocean.

AMS radiocarbon dates and pollen analysis of ODP Hole 175-1078C

ODP Site 1078 situated under the coast of Angola provides the first record of the vegetation history for Angola. The upper 11 m of the core covers the past 30 thousand years, which has been analysed palynologically in decadal to centennial resolution. Alkenone sea surface temperature estimates were analysed in centennial resolution. We studied sea surface temperatures and vegetation development during full glacial, deglacial, and interglacial conditions. During the glacial the vegetation in Angola was very open consisting of grass and heath lands, deserts and semi-deserts, which suggests a cool and dry climate. A change to warmer and more humid conditions is indicated by forest expansion starting in step with the earliest temperature rise in Antarctica, 22 thousand years ago. We infer that around the period of Heinrich Event 1, a northward excursion of the Angola Benguela Front and the Congo Air Boundary resulted in cool sea surface temperatures but rain forest remained present in the northern lowlands of Angola. Rain forest and dry forest area increase 15 thousand years ago. During the Holocene, dry forests and Miombo woodlands expanded. Also in Angola globally recognised climate changes at 8 thousand and 4 thousand years ago had an impact on the vegetation. During the past 2 thousand years, savannah vegetation became dominant.

XRF scanning, pollen and spores of ODP Site 108-659

Pliocene vegetation dynamics and climate variability in West Africa have been investigated through pollen and XRF-scanning records obtained from sediment cores of ODP Site 659 (18°N, 21°W). The comparison between total pollen accumulation rates and Ti/Ca ratios, which is strongly correlated with the dust input at the site, showed elevated aeolian transport of pollen during dusty periods. Comparison of the pollen records of ODP Site 659 and the nearby Site 658 resulted in a robust reconstruction of West African vegetation change since the Late Pliocene. Between 3.6 and 3.0 Ma the savannah in West Africa differed in composition from its modern counterpart and was richer in Asteraceae, in particular of the Tribus Cichorieae. Between 3.24 and 3.20 Ma a stable wet period is inferred from the Fe/K ratios, which could stand for a narrower and better specified mid-Pliocene (mid-Piacenzian) warm time slice. The northward extension of woodland and savannah, albeit fluctuating, was generally greater in the Pliocene. NE trade wind vigour increased intermittently around 2.7 and 2.6 Ma, and more or less permanently since 2.5 Ma, as inferred from increased pollen concentrations of trade wind indicators (Ephedra, Artemisia, Pinus). Our findings link the NE trade wind development with the intensification of the Northern Hemisphere glaciations (iNHG). Prior to the iNHG, little or no systematic relation could be found between sea surface temperatures of the North Atlantic with aridity and dust in West Africa.

Palynology on sediment profile Tso Kar in Ladakh

Palynological investigation of a 410 cm long core section from Tso Kar (33°10'N, 78°E, 4527 m a.s.l.), an alpine lake situated in the arid Ladakh area of NW India at the limit of the present-day Indian summer monsoon, was performed in order to reconstruct post-glacial regional vegetation and climate dynamics. The area was covered with alpine desert vegetation from ca. 15.2 to 14 kyr BP (1 kyr=1000 cal. years), reflecting dry and cold conditions. High influx values of long-distance transported Pinus sylvestris type pollen suggest prevailing air flow from the west and northwest. The spread of alpine meadow communities and local aquatic vegetation is a weak sign of climate amelioration after ca. 14 kyr BP. Pollen data (e.g. influx values of Pinus roxburghii type and Quercus) suggest that this was due to a strengthening of the summer monsoon and the reduced activity of westerly winds. The further spread of Artemisia and species-rich meadows occurred in response to improved moisture conditions between ca. 12.9 and 12.5 kyr BP. The subsequent change towards drier desert-steppe vegetation likely indicates more frequent westerly disturbances and associated snowfalls, which favoured the persistence of alpine meadows on edaphically moist sites. The spread of Chenopodiaceae-dominated vegetation associated with an extremely weak monsoon occurred at ca. 12.2-11.8 kyr BP during the Younger Dryas interstadial. A major increase in humidity is inferred from the development of Artemisia-dominated steppe and wet alpine meadows with Gentianaceae after the late glacial/early Holocene transition in response to the strengthening of the summer monsoon. Monsoonal influence reached maximum activity in the Tso Kar region between ca. 10.9 and 9.2 kyr BP. The subsequent development of the alpine meadow, steppe and desert-steppe vegetation points to a moderate reduction in the moisture supply, which can be linked to the weaker summer monsoon and the accompanying enhancement of the winter westerly flow from ca. 9.2 to 4.8 kyr BP. The highest water levels of Tso Kar around 8 kyr BP probably reflect combined effect of both monsoonal and westerly influence in the region. An abrupt shift towards aridity in the Tso Kar region occurred after ca. 4.8 kyr BP, as evidenced by an expansion of Chenopodiaceae-dominated desert-steppe. Low pollen influx values registered ca. 2.8-1.3 kyr BP suggest scarce vegetation cover and unfavourable growing conditions likely associated with a further weakening of the Indian Monsoon.

Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with the coexistence approach to obtain quantitative palaeoclimate data. Visualization of climate results in maps shows a distinct spatial differentiation in Southern China during the Miocene. Higher seasonalities of temperature and precipitation occur in the north and south parts of Southern China, respectively. During the Miocene, most regions of Southern China and Europe were both warm and humid. Central Eurasia was likely to be an arid center, which gradually spread westward and eastward. Our data provide information about Miocene climate patterns in Southern China and about the evolution of these patterns throughout the Miocene, and is also crucial to unravel and understand the climatic signals of global cooling and tectonic uplift.

Distribution of pollen and spores in sediments of ODP Hole 175-1078C

The distribution of pollen in marine sediments is used to record vegetation change on the continent. Generally, a good latitudinal correspondence exists between the distribution patterns of pollen in the marine surface sediments and the occurrence of the source plants on the adjacent continent. To investigate land-sea interactions during deglaciation, we compare proxies for continental (pollen assemblages) and marine conditions (alkenone-derived sea surface temperatures) of two high-resolution, radiocarbon-dated sedimentary records from the tropical southeast Atlantic. The southern site is located West of the Cunene River mouth; the northern site is located West of the Angolan Huambe Mountains. It is inferred that the vegetation in Angola developed from Afroalpine and open savannah during the last Glacial maximum (LGM) via Afromontane Podocarpus forest during Heinrich Event 1 (H1), to an early increase of lowland forest after 14.5 ka. The vegetation record indicates dry and cold conditions during the LGM, cool and wet conditions during H1 and a gradual rise in temperature starting well before the Younger Dryas (YD) period. Terrestrial and oceanic climate developments seem largely running parallel, in contrast to the situation ca. 5° further South, where marine and terrestrial developments diverge during the YD. The cool and wet conditions in tropical West Africa, South of the equator, during H1 suggest that low-latitude insolation variation is more important than the slowdown of the thermohaline circulation for the climate in tropical Africa.

Pollen and non-pollen palynomorph records of the Holocene part of the composite sediment core TMD from lake Tso Moriri (NW India) and of modern surface samples from the Tso Moriri region

The high-altitude lake Tso Moriri (32°55'46'' N, 78°19'24'' E; 4522 m a.s.l.) is situated at the margin of the ISM and westerly influences in the Trans-Himalayan region of Ladakh. Human settlements are rare and domestic and wild animals are concentrating at the alpine meadows. A set of modern surface samples and fossil pollen from deep-water TMD core was evaluated with a focus on indicator types revealing human impact, grazing activities and lake system development during the last ca. 12 cal ka BP. Furthermore, the non-pollen palynomorph (NPP) record, comprising remains of limnic algae and invertebrates as well as fungal spores and charred plant tissue fragments, were examined in order to attest palaeolimnic phases and human impact, respectively. Changes in the early and middle Holocene limnic environment are mainly influenced by regional climatic conditions and glacier-fed meltwater flow in the catchment area. The NPP record indicates low lake productivity with high influx of freshwater between ca. 11.5 and 4.5 cal ka BP which is in agreement with the regional monsoon dynamics and published climate reconstructions. Geomorphologic observations suggest that during this period of enhanced precipitation the lake had a regular outflow and contributed large amounts of water to the Sutlej River, the lower reaches of which were integral part of the Indus Civilization area. The inferred minimum fresh water input and maximum lake productivity between ca. 4.5-1.8 cal ka BP coincides with the reconstruction of greatest aridity and glaciation in the Korzong valley resulting in significantly reduced or even ceased outflow. We suggest that lowered lake levels and river discharge on a larger regional scale may have caused irrigation problems and harvest losses in the Indus valley and lowlands occupied by sedentary agricultural communities. This scenario, in turn, supports the theory that, Mature Harappan urbanism (ca. 4.5-3.9 cal ka BP) emerged in order to facilitate storage, protection, administration, and redistribution of crop yields and secondly, the eventual collapse of the Harappan Culture (ca. 3.5-3 cal ka BP) was promoted by prolonged aridity. There is no clear evidence for human impact around Tso Moriri prior to ca. 3.7 cal ka BP, with a more distinct record since ca. 2.7 cal ka BP. This suggests that the sedimentary record from Tso Moriri primarily archives the regional climate history.