A calendar for tree pollen in London

Data from a pollen monitoring network in Islington, North London, are used to construct tree pollen calendars for the tree seasons 1987 to 1989 inclusive. Annual variations in the pollen abundance and length of flowering season are investigated for individual species in relation to meteorological factors and the inherent biological rhythms of trees. Results indicate clear relationships between seasonal variations in pollen abundance and the weather, both in the prevailing season and also in the preceeding year during the time of pollen formation. Annual variations evident in the pollen records for Betula and Quercus support the theory of inherent biennial cycles for these species. Patterns for other trees do not show clear trends within the period sampled. Insufficient information is available to determine the concentration thresholds of allergic response for most tree pollens, but evidence from Finland is used to identify the timing and duration of periods which exceed the response thresholds for Betula.     

A pollen calendar for Chittagong University Campus,Chittagong (Bangladesh)

Summary This work presents a calendar of pollen types found in the atmosphere of Chittagong University Campus, Chittagong, Bangladesh, recorded over the period of March 1988–February 1990. A total of 9,225 pollen/cm² was encountered and classified in 36 pollen types belonging to 26 families. The pollen concentration showed three peak periods, March, October and November and each period was dominated by a specific pollen type. Low frequency of pollen was probably due to heavy rainfall which washed down the pollen. January and February were also marked by lower abundance of pollen and was probably due to the low rate of flowering. This study clearly showed four airborne pollen seasons from October to November, December to February, March to April and June to September. The dominant pollen types were Poaceae, followed by Amaranthaceae, Arecaceae, Asteraceae and Cyperaceae. The pollen calendar was provided to show the range of flowering with the period of occurrence in air of the area studied.     

A fungal spore calendar for the atmosphere of Melbourne, Australia, for the year 1993

A calendar of fungal spore seasons for Melbourne during 1993was established using a 7-day volumetric Burkard trap. Twenty-ninegenera and five spore groups were identified. The dominant spore typesdetected were Cladosporium (41.7%),Leptosphaeria (14.9%), Coprinus (14.6%),`Ascospore 1' (5.5%), Ganoderma (2.1%) andAlternaria (1.4%). Seasonally, spore levels ofCladosporium and Alternaria peaked in spring andsummer, Leptosphaeria and Ganoderma peaked towardsummer and autumn, `Ascospore 1' peaked in winter, whilst spore levelsof the basidiomycete Coprinus fluctuated year round. Inconclusion, a range of allergenic fungal spores were present in the airof Melbourne throughout the year.     

Palynological differences in the pollen content of Eucalyptus honey from Australia,Portugal and Spain

A melissopalynological study was carried out on 75 samples of Eucalyptus honey from different countries (22 from Australia, 13 from Portugal and 40 from Northwest Spain), in which a total of 145 different pollen types were identified. Of such, only Eucalyptus, Acacia, Brassica, Echium, Ligustrum, Plantago, Rumex, Taraxacum, Trifolium and Vicia pollen are present in the honeys from all three countries.

Among the most abundant pollen types in Australian honeys, those belonging to the following families stand out: Myrtaceae (Angophora and Melaleuca), Fabaceae, Asteraceae, Proteaceae and Euphorbiaceae, along with Raphanus, Echium and Citrus.

In the Portuguese honeys, the presence of Fabaceae, Rosaceae and Cistaceae stands out, with Castanea and Erica as secondary pollen types, while Fabaceae, Asteraceae, Boraginaceae, Cistaceae and Scrophulariaceae are the families with the highest quantity of pollen types in the samples from Spain. In the latter, the most important secondary pollen types are: Castanea, Cytisus, Erica, Lotus, Salix and Rubus.     

Modern pollen rain from the Biligirirangan-Melagiri hills of southern Eastern Ghats, India

A total of 39 soil surface samples collected between 11 degrees 30'N 76 degrees 45'E and 12 degrees 45'N 78 degrees 15'E from the mainly deciduous forests in the Biligirirangan-Melagiri hills of the southern Eastern Ghats were analysed for their pollen content. The samples are distributed among four different deciduous and evergreen vegetation types between 210 and 1700m altitudes and fall within three distinct rainfall regimes. The aims of this paper are to provide new data on the modern pollen rain from the Southern Eastern Ghats, a region characterized by a unique and complex climate and vegetation, and to interpret these data using multivariate statistics and the diagram of pollen percentages. We could distinguish first between the deciduous and the evergreen forests and then also between different types of deciduous forest. The distinction between the evergreen and deciduous forests was based on a humidity gradient and that among the deciduous forests on a physiognomic gradient identified through correspondence analysis. The above analysis also allowed us to identify a set of 14 pollen taxa markers and 11 associated pollen taxa that help differentiate the evergreen from deciduous forests. Similarly, a set of 12 pollen taxa markers and six associated pollen taxa was demarcated to help distinguish woodland formations from scrub and thicket formations, among the deciduous vegetation. We could also differentiate amongst the four distinct vegetation types sampled, on the basis of distinct associations of both tree and herb pollen taxa according to their relative abundance in the pollen diagram as well as on the proportion of total arboreal pollen. The ground cover of grasses and other herbaceous plants in the deciduous forests is effectively demonstrated by percentages of non-arboreal pollen varying between 40 and 70%. The 1000m altitude limit reflecting a gradient of humidity and the physiognomic gradient among deciduous forests seem to be important in this region.     

A pollen diagram from Pitbladdo,Fife

Summary

Pollen analytical data are presented from a site near Cupar, Fife. The stratigraphy and pollen spectra are used to infer the changing patterns of vegetation in the area during the Lateglacial and Postglacial periods. In the Lateglacial Interstadial the local development of Betula-Juniperus scrub was followed by a period of open habitat during the colder Loch Lomond Stadial. The early Postglacial forest was dominated by Corylus and Betula, although Ulmus was also a major woodland component before the arrival of Alnus. Following some initial deforestation due to anthropogenic activity, subsequent woodland clearance was almost total and open habitat communities dominated.     

A massively-constructed iguanodont from Gadoufaoua,lower Cretaceous of Niger

A ponderously constructed ornithischian dinosaur, Lurdusaurus arenatus, nov.g., nov.sp., from the Aptian of Niger resembles extinct giant ground sloths in general body form. Details of its skeletal anatomy indicate a close affinity to European iguanodontids of Early Cretaceous age.     

Cytotoxicity effect of honey,bee pollen,and propolis from seven stingless bees in some cancer cell lines

Our effort to find new material for anti cancer from natural resources leads us to focus on stingless bee products such as honey, bee pollen, and propolis. The products were from seven stingless bees named Homotrigona fimbriata, Heterotrigona itama, Heterotrigona bakeri, Tetragonula sarawakensis, Tetragonula testaceitarsis, Tetragonula fuscobalteata, Tetragonula laeviceps. The stingless bee products were evaluated for their cytotoxicity effect on MCF-7, HeLa and Caco-2 cancer cell lines. This is the first time to be reported that the honey, ethanol extracts of bee pollen and propolis of H. fimbriata displayed more potent cytotoxicity than other stingless bee products. By chromatography and biological activity-guided fractionation, ethanol extract of propolis from H. fimbriata was fractionated and isolated its active compound named mangiferonic acid. Mangiferonic acid showed a cytotoxicity effect with IC₅₀ values 96.76 µM in MCF-7, >110.04 µM in HeLa, and > 110.04 µM in Caco-2, respectively. These results exhibited the potential of ethanol extracts from propolis of H. fimbriata to be further developed for drug and experiments to verify the function are essential.     

北极巴罗地区2种灌木植物及其花粉形态

观察了北极巴罗(Barrow)地区2种灌木植物,全缘叶仙女木(Dryas integrifolia M.Vahl)和圆叶柳(Salix rotundifolia Trautv.)的形态、生境以及它们的花粉形态.这2种植物形态矮小或匍匐蔓生;全缘叶仙女木叶短小似披针状或扁平,全缘;圆叶柳叶圆形,叶脉显著,根、茎、叶均含丰富Vc.它们的花粉形态为球形、近球形或长球形,其萌发孔均为三孔沟或拟三孔沟,花粉均为辐射对称.全缘叶仙女木花粉外壁纹饰在光学显微镜下(LM)为细网状纹饰,在扫描电子显微镜(SEM)下为条纹状纹饰;圆叶柳在LM和SEM下均为细网状纹饰.通过与中国产和日本产相似种的比较研究,显示它们应是温带亚洲高山起源及部分起源于北极本部.     

A comparison of modern and presettlement pollen from southern Michigan (U.S.A.)

Use of samples of modern pollen to interpret assemblages of fossil pollen requires that the effects of man's impact be identified in the modern pollen. A comparison of the modern and presettlement pollen in 23 short cores taken within the lower peninsula of Michigan reveals a varied effect of man's activities on the vegetation. When obvious indicators of human activity (such as ragweed pollen) are removed from the pollen sum, many differences in the composition of the arboreal pollen are still evident between presettlement and modern records. When compared to presettlement data, birch, elm, and willow pollen in the modern data appear in proportionately higher quantities throughout the state, whereas beech, maple, and hemlock are in lower quantities. Within the region of primeaval pine forests, white pine values are much lower and oak values show an increase. Despite these differences in the pollen record, the modern pollen reflect the same basic patterns in the vegetation as the presettlement pollen. Principal component analysis shows the same patterns to exist in the modern data as are in the presettlement pollen.     

A 7 year pollen profile of major Olympic Games venues in Sydney, Australia

The year 2000 Olympic and Paralympic Games heldin Sydney, Australia were unique in the historyof the Games because they were staged in theearly to mid spring. This led to the concernthat pollen-sensitive athletes may havesignificant problems with allergic symptomstriggered by pollen exposure and that this mayhave compromised their ability to attain theirbest performance. Unfortunately, there was nosystematic pollen count data available for thecity of Sydney up until this time so thepurpose of this study was to obtain a profileof the pattern and type of pollens in theregion so that Olympic team managers andmedical staff could be adequately advised andable to prepare allergic athletes for anyexposures encountered while training andcompeting.We performed pollen monitoring of three majorOlympic venues over the six years before theGames to provide a profile of the mostprevalent species appearing over the spring.The pollen counts obtained at the major siteswere extremely high over the periods oftraining and competition. Tree pollens appearedfrom late July, peaking in August andSeptember, whilst grass pollens appeared fromSeptember and peaked in mid October. Arelatively small number of pollen varietiescomprise the majority of the pollen count.     

Holocene forest development along the Setesdal valley, southern Norway, reconstructed from macrofossil and pollen evidence

The Setesdal valley in South Norway runs north to south for 200 km, from alpine vegetation at 1200 m, passing the tree-line at around 1000 m, through Boreal forests, to Nemoral forest at sea level. The Holocene vegetation history and its altitudinal differentiation were reconstructed using pollen percentages and influx and plant macrofossil concentration records from four lakes along an altitudinal transect. During the early Holocene (c. 10500–8000 cal b.p.) Betula pubescens, Pinus sylvestris, Alnus, and Corylus expanded in the lowlands. Only Pinus and B. pubescens reached 1000 m asl (Lille Kjelavatn). Only B. pubescens reached Holebudalen (1144 m asl) at about the same time as it arrived in the lowlands. Between c. 8000–3000 cal b.p. mixed deciduous forest developed around Dalane (40 m asl) and to a lesser extent around Grostjørna (180 m asl), birch woodland with pine surrounded Lille Kjelavatn and birch woodland occurred at Holebudalen. From c. 3000 cal b.p. to present, the vegetation at Dalane hardly changed except for slight human impact and the immigration of Picea abies. At Grostjørna Pinus expanded. At Lille Kjelavatn Pinus disappeared and Betula became sparse as at the tree-line today. Betula retreated from Holebudalen thus leaving it above the tree-line in low-alpine vegetation. The strengths and weaknesses of pollen and plant macrofossil data were assessed for forest reconstructions. Where local pollen production is low, as near the tree-line, percentages of long-distance tree pollen can be misleadingly high. Pollen influxes of Betula and Pinus were much smaller near their altitudinal limits than at lower altitudes, although their macrofossils were equally abundant. The limited dispersal capacity of macrofossils documents the local presence of species and the character of the local vegetation, although macrofossils of some tree taxa are rarely found. Pollen and plant macrofossil evidence complement each other to provide a more complete reconstruction of Holocene tree-limits and tree-lines and hence climate changes, than either form of evidence alone.     

The first find in southern Georgia of fossil honey from the Bronze Age,based on palynological data

The results of a palynological analysis of the organic content of earthenware pots from the Kodiani burial mound (27th–25th centuries b.c.) are reported. The character of the palynological spectrum differs significantly from that of a buried soil within the same burial mound. In the samples taken from the pots, pollen concentration is very high, pollen grains are perfectly preserved and an abundance of pollen from insect-pollinated plants is recorded. It is well known that these features are peculiar to honey palynospectra. In all three pots the pollen of Rosaceae, a family of plants that produce good honey, is dominant. However, the second, third and fourth most dominant pollen types in all three samples are different. For example, Tilia pollen is the second dominant in only one pot. In the second pot, Apiaceae and Poaceae are predominant, and in the third pot, Poaceae, both wild and cultural, is the second dominant. It is clear that the different pots contained different types of honey. The variety of honey types indicates highly developed bee-keeping in the Early Bronze Age. In the same regions of Georgia, agriculture was also highly developed. Wheat cultivation was very important. According to the palynospectra, the landscape and climate of this period were probably quite different to those of today.     

Prevalence of allergenic pollen grains in the aerosol of the city of Calcutta,India: a two year study

The role of pollen grains as a causative agent of respiratory allergic disorders such as asthma and allergic rhinitis is common and very well established. The aim of this study was to assess the frequencies of airborne pollen in the Calcutta metropolis and to identify the taxa which cause significant amounts of sensitization. An aeropalynological survey of the atmosphere of Calcutta was carried out from 2004 to 2006. Skin tests were performed with a panel of the most common pollen types on local patients with clinical features of pollinosis. The meteorological factors responsible for the frequency of the pollen types were analysed. The results of monthly visits to the clinic by these patients were correlated with the monthly pollen counts of three dominant and perennial pollen taxa. The dominant pollen types were Trema (19%), Poaceae (12.98%), Casuarina (5.76%), Cocos (5.7%), Azadirachta (4.65%), Peltophorum (3.71%), Cyperaceae (3.68%), Delonix (3.18%) and Areca (2.56%). Total pollen concentration seems to have a significant positive correlation with temperature and wind speed whereas there was a negative correlation with humidity. Skin tests were most frequently found to be positive with the pollen of Poaceae (49%), Azadirachta (46%), Cocos (47%), Cyperaceae (35%), Peltophorum (33%), Areca (29%), Phoenix (26%), and Borassus (23%). A positive correlation occurred between visits to the clinic and monthly pollen count of Areca, Cocos, and Poaceae. This is the first study to design a pollen calendar for Calcutta city; it will provide useful data for enabling allergologists to achieve accurate diagnosis for patients with pollen hypersensitivity.     

A 200-ka pollen and oxygen-isotopic record from two sediment cores from the eastern Arabian Sea

We present here a pollen record from the northern Indian Ocean that goes back to 200 ka, the boundary between marine isotopic stages (MIS) 7 and 6. Pollen, oxygen-isotopic composition and organic carbon have been examined for two sediment cores from the eastern Arabian Sea (15°02′N and 71°41′E, 13°16′N and 71°00′E), to reconstruct the long-term palaeoclimate and palaeovegetation of the Indian subcontinent. Oxygen-isotope data suggest that glacial periods (MIS 2, 4 and 6) are characterised by low precipitation because of a weak southwest monsoon and a strong northeast monsoon. In contrast, interglacial periods (MIS 1, 3 and 5) are marked by high fresh water input resulting from a strong southwest monsoon. During the last glacial-interglacial cycle, sea-surface temperature and surface salinity changed as a result of variations in the evaporation-precipitation (E-P) balance. Throughout the core, the dominant pollen types are Poaceae and Chenopodiaceae and/or Amaranthaceae (>50%). Their dominance during glacial periods (MIS 2, 4 and 6) suggests that the climate was cold and dry. This dominance is also suggestive of salinity-tolerant vegetation colonizing large areas near seashore due to lower sea level or high E-P conditions. During interglacial periods (MIS 1, 3 and 5) when there was high precipitation, the arid taxa were sparse, whereas Poaceae and Piperaceae were abundant. Hence, Chenopodiaceae and/or Amaranthaceae and Artemisia are suggestive of cold and arid/semi-arid climate, and Poaceae and Piperaceae of warm and wet conditions. Mangrove pollen is not well represented in the cores.     

Azotobacter vinelandii gene clusters for two types of peptidic and catechol siderophores produced in response to molybdenum

Aim: To characterize the complementary production of two types of siderophores in Azotobacter vinelandii. Methods and Results: In an iron‐insufficient environment, nitrogen‐fixing A. vinelandii produces peptidic (azotobactin) and catechol siderophores for iron uptake to be used as a nitrogenase cofactor. Molybdenum, another nitrogenase cofactor, was also found to affect the production level of siderophores. Wild‐type cells excreted azotobactin into molybdenum‐supplemented and iron‐insufficient medium, although catechol siderophores predominate in molybdenum‐free environments. Two gene clusters were identified to be involved in the production of azotobactin and catechol siderophores through gene annotation and disruption. Azotobactin‐deficient mutant cells produced catechol siderophores under the molybdenum‐supplemented and iron‐insufficient conditions, whereas catechol siderophore–deficient mutant cells extracellularly secreted excess azotobactin under iron‐deficient condition independent of the concentration of molybdenum. This evidence suggests that a complementary siderophore production system exists in A. vinelandii. Conclusions: Molybdenum was found to regulate the production level of two types of siderophores. Azotobacter vinelandii cells are equipped with a complementary production system for nitrogen fixation in response to a limited quantity of metals. Significance and Impact of the Study: This is the first study identifying A. vinelandii gene clusters for the biosynthesis of two types of siderophores and clarifying the relationship between them.     

Towards the vegetation and settlement history of the southern Dobrudza coastal region, north-eastern Bulgaria: A pollen diagram from Lake Durankulak

Palynological investigation and radiocarbon dating of a 6-m core from lake Durankulak, north-eastern Bulgaria, enables vegetation development and human occupation from ca. 5500–5300 cal. B.C. onwards to be traced. Steppe vegetation that included with groves of deciduous trees asQuercus, Ulmus, Carpinus belulus andCorylus changed to a forest-steppe after 4000 cal. B.C. The archaeopalynological record indicates three distinct phases of human activity as follows: (1) 5300–4200 cal. B.C. (late Neolithic and Eneolithic) during which farming, that included a substantial arable component, was pursued, (2) 3500–3000 cal. B.C. (transition to early Bronze Age) when stock rearing appears to have dominated, and (3) after 1300 cal. B.C. (late Bronze Age) when arable farming again assumed importance. The palynological data correlate well with the rich archaeological record for human settlement that is available for the region from late Neolithic times onwards.     

Seasonal patterns in biomass burning emissions from southern African vegetation fires for the year 2000

A modeling framework has been developed to examine the spatial and temporal aspects of biomass burning emissions from southern African savanna fires. The complexity of the fire emissions processes is described using a spatially and temporally explicit model that integrates recently published satellite‐driven fuel load amounts, the GBA‐2000 satellite burned area time series and empirically derived parameterizations of combustion completeness and emission factors (EFs). To represent fire behavior characteristics, land cover is classified into grasslands and woodlands using the MODIS percent tree cover product. The combustion completeness is modeled as a function of grass fuel moisture and the EFs as a function of grass fuel moisture in grasslands and fuel mixture in woodlands. Fuel moisture is derived from satellite vegetation index time series. The analysis at the regional scale shows that early burning in grasslands may lead to higher amounts of products of incomplete combustion, despite the lower amounts of fuel consumed, compared with late dry season burning. In contrast, early burning in woodlands results in lower emissions, in both products of complete and incomplete combustion, because less fuel is consumed than in the late dry season when the fuels are drier. Overall, burning in woodlands dominates the regional emission budgets. Emissions estimates for various atmospheric species, many of which are modeled for the first time, are reported. The modeled estimates for 2000 are (in Tg) 296 CO₂, 11.7 CO, 0.350 CH₄, 0.348 NMHC and 1.1 particulates (<2.5 μm). Especially high is the previously undetermined contribution of oxygenated volatile organic compounds (0.915 Tg). A sensitivity analysis of fixed vs. seasonally variable EFs and combustion completeness demonstrates the importance of accounting for the seasonal variations of these two variables in emissions modeling.     

A holocene pollen diagram from El Atrun,northern Sudan

Palynological investigations on a 3.36 m core from El Atrun, Nubia, show vegetation development and climatic change during a period from approximately 9800 to 7000 uncal B.P. From a dry period with a steppe-like vegetation at about 9800-9500 B.P. (zone A), a change to a period with a more favourable climate and a tree covered savanna-like vegetation can be observed in zone B (about 9500-8900 B.P.). In zone C (8900-8400 B.P.), a climatic setback is indicated, with spreading of steppe vegetation and an increase in swamp vegetation as a result of a low lake level. For zone D (about 8400-7000 B.P.), renewed spreading of wooded savanna is inferred.     

A survey of modern pollen and vegetation along an altitudinal transect in southern Georgia, Caucasus region

This paper describes the pollen representation of vegetation patterns along an altitudinal transect in the South Caucasus region. Surface sediments from eight small- to medium-sized lakes and wetlands were analysed for modern pollen, and the results analysed numerically using detrended correspondence analysis (DCA) and dichotomised ordination (TWINSPAN). Pollen spectra from the semidesert region have a clear palynological signal characterised by an abundance of Chenopodiaceae. Differentiation of oak forest, upper tree-line and subalpine communities is more difficult: all are dominated by arboreal pollen (AP) types. The authors propose a number of indicator pollen types and pollen threshold values that may assist in detecting tree-line variations and deforestation events in Holocene pollen diagrams.