A two-year report of pollen influx into Tauber traps in Mar Chiquita coastal lagoon,Buenos Aires,Argentina

Modern pollen deposition and its relationship to the surrounding vegetation were studied at a coastal lagoon from the southeast of Buenos Aires Province (Argentina). Tauber traps were monitored monthly over a 2-year period in a coastal dune barrier, salt marsh and continental freshwater lake. Pollen deposition exhibited seasonal patterns with maximum values during summer and a spatial variability of increasing deposition from the coast to inland sites. The pollen spectra suggest that airborne pollen originates mainly from local vegetation with scarce representation of extraregional sources. Herbaceous pollen predominates, comprising up to 90% of the total amount with Poaceae, Chenopodiineae and Asteroideae as the main types. Hydrophytic, psammophytic and extraregional types had little influence on the pollen spectra, generally comprising <5% of the total pollen. Pollen influx–vegetation abundance discrepancies were explained considering pollination syndrome, spatial distribution and structure of vegetation.     

Vegetation history and sea level variations during the last 13,500 years inferred from a pollen record at Chilika Lake,Orissa, India

Chilika Lake is the largest lagoon in Asia, situated in the state of Orissa in India. In the year 2000, many surface samples and cores were taken. Here the lithological results and especially those of the pollen analysis are shown. The oldest sediments of core CHI 9 were dated at about 13,500 cal years b.p. At this time the area of Chilika Lake was a river or a river delta with fresh water vegetation. With the increase in the sea level after about 9,500 cal years b.p. the area became an estuary with mangrove vegetation. Small variations in the sea level between about 5,000 and 2,500 cal years b.p. are not visible in our pollen profile. However the regression after about 2,000 cal years b.p. caused the formation of a barrier spit and sand ridges with the consequence that a big lagoon was formed, Chilika Lake. Marine influence diminished and the fresh water impact from the rivers increased. Mangrove vegetation disappeared and was replaced by fresh water vegetation. This paper is dedicated to Prof. Dr. Hans-Jürgen Beug on his 75th birthday.     

K-77(2)雄性不育小麦花粉壁结构特征

K-77(2)不育花粉内壁比保持系厚将近一倍。在保持系花粉内壁中,有径向排列的、断断续续的、着色深的管状结构。而不育花粉内壁中则没有管状结构,且在不育花粉内壁中形成许多小泡。在花粉粒后期,往往在Z层与内壁连接处断开。推测,由于花粉内壁结构被破坏,影响了正常的营养运输和萌发所需酶的合成而抑制花粉发育。     

A late Holocene pollen diagram from the Megaris,Greece, giving possible evidence for cultivation of<Emphasis Type="Italic"> Ceratonia siliqua</Emphasis> L. during the last 2000 years

A late Holocene pollen profile from the Megaris on the eastern Gulf of Corinth shows a vegetation which was strongly influenced by human impact throughout. A Pistacia-Phillyrea maquis, which is reflected in the older parts of the profile, changed later to a more degraded vegetation type. In the uppermost part Pinus dominates the pollen spectrum. A continuous record of Ceratonia siliqua pollen older than cal a.d. 100 is of special interest.     

History of vegetation and land use from 3200 B.P. to the present in the north-west Burren,a karstic region of western Ireland

A radiocarbon-dated pollen profile provides the first evidence for the vegetation history of the north-west Burren, a karstic region in Co. Clare, western Ireland. The profile, which spans the period ca. 3200-0 B.P., shows that Corylus was the main woody species and that, apart from the later eighteenth and nineteenth centuries, when woody species were almost totally cleared, it constituted a more important element in the landscape than at present. The data indicate that small populations of Quercus, Fraxinus, Betula, Alnus and possibly Ulmus were also present until at least the mid seventeenth century. Exceptionally high values of Plantago lanceolata (mostly in excess of 20% total terrestrial pollen) suggest intensive pastoral farming over most of the period. Between A.D. 200–580, a lull in activity is recorded during which woody species and, in particular, hazel scrub regenerated. The separation of pollen of cereal origin from large cereal-type pollen produced by non-cultivated grasses proved particularly problematic. Reliance has therefore been placed on the weed pollen flora as a guide to arable activity. This flora indicates that arable farming was of some importance in the Burren from A.D. 1000 onwards. The implications of the various findings for the longer term history of the rarer elements of the Burren flora and the relationship between the pollen record and the archaeological and historical evidence for settlement and land use are discussed.     

Holocene palaeoenvironment in a former coastal lagoon of the arid south eastern Iberian Peninsula: salinization effects on δ<Superscript>15</Superscript>N

The palaeoenvironment of a former coastal lagoon in the south eastern Iberian Peninsula (San Rafael, Almeria, Spain) were inferred from one core analyzed for particulate organic matter content (POM) together with its C/N, δ¹³C, δ¹⁵N to depict the biogeochemical record from the Late Glacial to the Holocene. The results, complemented by previously reported pollen assemblages, indicate the appearance of a freshwater lagoon at 7300 b.p. (uncalibrated ¹⁴C age), its salinization at 6200 b.p. and its disappearance at 4400 b.p. The period of existence of the lagoon coincided with a period of wetter conditions as inferred from terrestrial vegetation. The lagoon’s salinization was not related to a decrease in precipitation but to a stronger maritime influence since there were no parallel changes in terrestrial vegetation. Salinization caused an increase in δ¹³C, associated with a higher relative presence of C₄ plants, and an increase in δ¹⁵N, due to a decrease in plant N demand. The late period of the lagoon, from about 5100 to 4400 b.p., shows a progressive drying and salinization not detected in isotopes but reflected in a decrease in POM, and in the pollen records. Increases in δ¹⁵N were related to increases in salinity within the lagoon, and are indicative of a more open N cycle, because the absence of changes in terrestrial vegetation rules out changes in the catchment area as the cause for changes in δ¹⁵N.     

Mangrove dynamics in the Cispata lagoon system (Colombian Caribbean) during last 900 years

The lagoon complex of Cispatá (old Sinú river delta) located at the Northwestern coast of the Colombian Caribbean, encloses one of the biggest mangrove areas in this region. This area has changed during the last 330 years because of several environmental and climatic causes, mainly changes in the position of the delta (Sinú River), which is the main freshwater source in this area, and sea level rise. We hypothesized that the climatic and geomorphologic dynamics has caused changes in the extension and composition of mangrove vegetation, especially during last 150 years. The dynamics of mangroves during the last 900 years was reconstructed based on the changes in the stratigraphy, pollen record, calcite concentrations (CaCO3) and C/N ratio, along two sediment cores from La Flotante and Navio lagoons, located in Cispatá complex. The age model was built based on lineal interpolation of 210Pb ages and changes in granulometry. Establishment and expansion of mangrove forests during the last 900 years were related to fluviomarine dynamics in the area and the lagoon formation. During the period encompassed between 1064 and 1762 A.D., the Mestizos spit was formed when marine conditions predominated in the surroundings of La Flotante Lagoon. At the site of Navío, a river dominated lagoon, terrigenous conditions dominated since 1830. Although the colonization of herbaceous pioneer vegetation started between 1142 and 1331 A.D., mangrove colonization only took place since 1717 A.D. Mangrove colonization was a result of the delta progradation. In 1849 A.D. the Sinú river delta migrated to the Cispatá bay. The eustatic sea level rise, the increase in river discharges and sedimentation rates produced the establishment of mangrove forests dominated by Rhizophora since 1849. Since 1900 a marine intrusion was recorded in both lagoons. In 1938, the migration of the delta toward its actual location in Tinajones gave place to the formation of the present lagoon system and to the expansion of mangrove forests, which reflects the balance between the high alluvial sediment input and the current sea level rise as has been recorded in similar ecosystems.     

Characterization and functional analysis of a novel PCP gene BcMF5 from Chinese cabbage (Brassica campestris L. ssp. chinensis Makino)

Brassica campestris Male Fertile 5 (BcMF5), a novel member of the pollen coat protein class A (PCP-A) gene family, was identified from Brassica campestris L. ssp. chinensis Makino (Chinese cabbage-pak-choi). Temporal and spatial expression analysis showed that BcMF5 is a late-expressed PCP gene related to the process of determining pollen fertility. Functional analysis by hairpin RNA (hpRNA)-mediated RNA interference also showed that the expression of BcMF5 is inhibited, which resulted in the low germination ability of the pollen and also in an abnormality of the pollen exemplified by a collapsed germination furrow. This demonstrates that the expression of BcMF5 is closely related to the tapetum. Further, the expression profile of the BcMF5 promoter in Arabidopsis was also analyzed. This analysis indicated that the BcMF5 promoter began expression in the early stage of anther development and drove high levels of glucuronidase (GUS) expression in anthers, pollen, and the pollen tube in the late stage of pollen development, but did not drive any expression in petals, sepals, or pistils. Together with the functional analysis, the hypothesis that BcMF5 may have a sporophytic or gametophytic expression pattern is presented.     

Late-glacial and Holocene woodland dynamics and land-use history of the Lower Oder valley, north-eastern Germany, based on two, AMS14C-dated, pollen profiles

High-resolution Holocene pollen profiles from lakes Großer Krebssee and Felchowsee, in the Lower Oder valley, north-eastern Germany, are presented. The Großer Krebssee profile includes a Late-glacial sequence. These investigations have been carried out in the context of a programme of archaeological excavation. AMS radiocarbon dates (26 in all) based on pollen concentrates have been used to provide a chronology for the pollen records. Holocene forest history and human impact are reconstructed for contrasting landscapes, namely, the Neuenhagener Oderinsel in the Lower Oderbruch (Großer Krebssee profile) and the more fertile Uckermärker Hügelland (Felchowsee profile) that lies immediately to the north. Both landscapes were glaciated during the Pomeranian stage of the Weichselian. New information on the spread of trees, includingTilia, Fagus and Carpinus, at both regional and local level, is presented. Five major phases of intensive human activity are recognised, the most intensive activity of the prehistoric period occurring in the Neolithic (Großer Krebssee profile). Differences between the records is explained in terms of local habitat, especially edaphic conditions, settlement history and also the pollen source area, the profile from the much larger Felchowsee lake providing a record of environmental change that is more regional in character.     

Sporo-Pollen Dissemination and Quantitative Character of Surface Sample of Manzhouli-Dayangshu Region

According to the profile of modern vegetation and pollen analysis of surface samples, the character of sporo-pollen assemblages from the steppe of Huluengbar to forest of Daxinganling mountain being investigated, indicated that, there existed a sylvosteppe zone in between the steppe and forest zones, in which the percentage of A. P. is a little more than that of N. A. P. (about 30%～70%). At the same time a nonlinear correlation was found between the percentage of pollen and the abundance of maternal plant. There were three states in the of plant/pollen system: (1)inferior position with abundance of pollen or the maternal plant both less than 30% or 20% .(2) dominant position with both over 70% and (3) mixed pisition with both between 30%～70%. In the first state, there existed a value of Po (pollen from another place) or Vo (short of pollen, or if none at all) in the second state, the linear correlation of pollen and plant became nonlinear and only in the third state, did the correction factor (value of R) approach constant.     

Environmental factors controlling the spring immigration of two estuarine fishes Atherina boyeri and Pomatoschistus spp. into a Mediterranean lagoon

Atherina boyeri , a pelagic species, mainly entered a Mediterranean lagoon in the Rhone River Delta, during the day, whatever the flow direction. Flow velocity did not appear to be a significant factor and its swimming abilities seemed to be sufficient to cope with the observed velocity. The combined responses of Pomatoschistus spp., benthic species, to the different environmental factors clearly demonstrated a change in behavioural response during their ontogenic development, i.e. a shift from passive to active or active-passive migration. Young Pomatoschistus spp. (<20 mm L _T) exhibited a behaviour that correspond to the classical selective tidal stream transport of young fishes towards estuarine areas (passive drifting). Large Pomatoschistus spp. were also able to enter the lagoon with the flow, but they remained negatively affected by the flow velocity. The diel cycle appeared to be the main factor controlling the immigration of A. boyeri into the lagoon whereas Pomatoschistus spp. seemed more sensitive to hydrographic conditions prevailing at the connection.     

新疆天山北坡地区中晚全新世古生物多样性特征

选择新疆天山北坡不同海拔高度、不同植被带和不同沉积年代的大西沟、桦树窝子、小西沟、东道海子和四厂湖剖面计算孢粉复合分异度指数,并根据已发表的有关文献中关于粒度、磁化率、烧失量等多项分析的数值整合结果探讨了本区中晚全新世以来生物多样性的时空变化和环境特征。森林草原过渡带的古生物多样性远高于高山、亚高山草甸带和荒漠带,孢粉复合分异度较高,鉴定的孢粉科属数较多。3600~3200 aB.P.、1700~1400 aB.P.、1000~600 aB.P.和450 aB.P.以来4个时段的生物多样性偏高。大西沟地区3600~3200 aB.P.期间和四厂湖地区中世纪期间气候均较湿润,其古生物多样性也较高,可见古环境演变和古生物多样性的动态变化具有相对一致性,孢粉复合分异度指数在一定程度上可以反映气候与环境的变化。但由于孢粉鉴定的精确度较差、受外来花粉的干扰等多种因素影响,使得孢粉多样性指数在反映生物多样性和古环境方面存在一定的偏差。     

Modern pollen/land-use relationships as an aid in the reconstruction of past land-uses and cultural landscapes: an example from south Sweden

An on-going, integrated project concerning modern pollen/vegetation/land-use relationships in south Sweden is outlined. Some preliminary results and their potential uses in palaeoecological reconstructions are discussed. Moss polsters were collected from 92 examples of vegetation/land-use areas of south Sweden (e.g. nonfertilized grazed areas, burned and grazed heaths, traditionally managed fodder-producing meadows, etc.). A total of 23 land-use (e.g. management type) and environment variables (e.g. soil chemistry) is available for 84 sites. The 84 sample data-set was analysed by canonical correspondence analysis and associated statistical testing using Monte Carlo permutation tests to explore and test patterns of modern pollen variation in relation to the environment, and by weighted averaging regression and calibration to derive local-scale environmental and land-use reconstructions from fossil pollen assemblages preserved in a soil profile.     

Involvement of Enterobacter cloacae in the mortality of the fish, Mugil cephalus

Aims:  To identify the causative agent of the mortality in the fish, Mugil cephalus , in Muttukadu lagoon.
Methods and Results:  An enteric bacterium from the kidneys of moribund fish M. cephalus , was isolated and identified as Enterobacter cloacae (MK). Mugil cephalus was experimentally infected by this isolate and was re-isolated from the kidneys of the moribund fish. Enterobacter cloacae isolates from the lagoon water (MW1, MW2 and reference strain ATCC 13047) and the reference strain were not able to induce similar pathogenesis. The putative factor imparting pathogenicity to the MK isolate was identified as a cationic molecule, which migrated towards the cathode on agarose gel electrophoresis.
Conclusions:  The Ent. cloacae (MK) isolate harbouring a cationic factor was the causative agent for the mortality of M. cephalus , found in Muttukadu lagoon.
Significance and Impact of the Study:  This study reveals that human enteric bacteria MK which is considered as nonpathogenic to fish, may become pathogenic to fish when it harbours this cationic factor. This cationic factor is found to be pathogenic to the fish M. cephalus leading to mortality. It was also found to be pathogenic to mice. Therefore, the shuttling of Ent. cloacae , harbouring cationic factor, between human and fish may be of human health importance.     

Characterization of a pollen-specific cDNA clone from Zea mays and its expression.

A pollen-specific cDNA clone, Zmc13, has been isolated from a cDNA library constructed to poly(A) RNA from mature maize pollen. The cDNA as shown by primer extension analysis is a full-length copy of the mRNA. The cDNA has been sequenced and is 929 nucleotides in length plus a 47-nucleotide poly(A) tail. Putative polyadenylation signals are identifiable in the 3'-nontranslated region. The mRNA codes for a predicted polypeptide containing 170 amino acid residues and with a molecular mass of 18.3 kilodaltons. The hydropathy profile suggests a possible signal sequence on the amino terminus. A comparison of the nucleotide and deduced amino acid sequence with sequences in data banks has not shown homology to known molecules. In situ hybridizations using RNA probes show that the mRNA is located in the cytoplasm of the vegetative cell of the pollen grain and after germination is distributed throughout the pollen tube cytoplasm.     

From forest to open pastures and fields: cultural landscape development in western Norway inferred from two pollen records representing different spatial scales of vegetation

The cultural landscape development of a farming community in western Norway was investigated through pollen analyses from a lake and a peat/soil profile. The pollen record from the lake indicates that there was a decrease in arboreal pollen (AP) by the end of the Mesolithic period (ca. 4200 cal b.c.), and that a substantial forest clearance occurred during the Bronze Age (ca. 1500 cal b.c.). The latter, together with grazing indicators and cereals, suggests a widespread establishment of farming. At the beginning of the Roman Iron Age there is an increase in heath communities. The pollen diagram from the peat/soil profile shows the forest clearance in the Bronze Age more clearly than the lake profile. This local pollen diagram is compared with modern pollen samples from mown and grazed localities in western Norway. Both analogue matching and ordination (PCA) indicate that the site was characterised by pastures and cereal fields from the Late Bronze Age to the Late Iron Age. An expansion of cereal cultivation took place during the Pre-Roman Iron Age, and an arable field was established at the site after ca. a.d. 800. This investigation illustrates the potential of selecting pollen sites reflecting different spatial scales, and complements the cultural history of the area as inferred from archaeological and historical records.     

云南亚热带南部孢粉空间组合特征及其与环境分异的关系

以云南亚热带南部野外调研孢粉资料为基础,分析了7个样地的35个表土样品以及28个剖面样品孢粉组合的空间分异特征.结果发现:(1)表土孢粉无论是在科属种类、数量及优势科属还是在科属植物区系上,哀牢山山脉东西两侧的样地均具有较大的差异.孢粉科属种类和数量方面,哀牢山西侧样地要较东部丰富;优势科属方面,哀牢山山脉西侧植物群落的优势科属不明显,且较东部要复杂,而东部地区植物群落的优势科属则较为集中和突出;植物区系分布方面,世界广布、泛热带、热带亚洲至热带非洲以及北温带分布等4个植物区系,其数量和所占比例东西差异都很大.(2)剖面孢粉的分析结果显示,其空间变化趋势与表土孢粉基本一致,同样反映了孢粉组合的东西空间差异.(3)孢粉组合的空间组合与区域的地形、气候分异特征有关.纵向排列的山系对大气环流的"阻隔"作用,以及哀牢山东西侧不同的季风环流系统导致的水热组合条件的差异是造成孢粉组合空间分异格局的主要原因.云南亚热带南部孢粉空间组合反映了区内自然环境的区域差异.     

Simplicissin,a New Pollen Growth Inhibitor Produced by the Fungus,Penicillium cf. simplidssimum (Oudemans) Thorn No. 410

A new pollen growth inhibitor, named simplicissin, was isolated from Penicillium cf. simplicissimum (Oudemans) Thorn No. 410, and its structure was established by spectroscopic methods including 2D NMR. The biological activities of the compound were examined by the bioassay methods involving tea pollen together with lettuce seedlings. The compound inhibited the growth of the tea pollen tube by 45% at a concentration of 3 mg/liter and showed complete inhibition at 10mg/liter.     

太子参花药发育及精细胞分离

太子参花药壁发育为基本型,腺质绒毡层。小孢子母细胞减数分裂为同时型,小孢子四分体为四面体型,成熟花粉具两个精细胞,为3胞花粉。在花粉表面具散孔,孔数22—30个,均匀分布于花粉粒表面上。花粉在10％甘露醇或15％蔗糖溶液中可直接爆破,精细胞易被释放并散开,通过显微操作仪可收集到一定数目的精细胞。FDA染色荧光显示释放出来的精细胞活力可维持25—50min。花粉在舍O．03％CaCl2、0．01％H3803、0．01％KH2P04和20％PEG、pH5．8的培养液中2—5min即萌发花粉管．花粉管生长2h可达815μm。一般花粉管伸长500—600μm时,一对精细胞才进入花粉管。DAPI染色后荧光观察．可观察到精细胞和营养细胞核在花粉管中的移动状况。爆破花粉管后可释放出一对精细胞。