Seasonal distribution of pollen in the atmosphere of melbourne: an airborne pollen calendar

Environmental monitoring of pollen grains in the atmosphere of Melbourne has been achieved using Burkard volumetric traps. Twenty-two families of flowering plants and confiers were identified in the pollen counts. About 62% of these pollen grains belonged to trees, 20% to grasses and 9% to herbs and weedy plants. During spring and summer, the atmosphere contained about 70% of the total annual pollen count. Tree pollen, predominantly elm and cypress, occurred abundantly in late winter and spring, with grass pollen predominantly in spring and early summer. These three types of pollen grains occurred in significant amounts, together accounting for more than 60% of the total annual catch. A seasonal incidence chart (pollen calendar) for Melbourne based on 2 years observation has been constructed. This pollen calendar is useful in identifying sources of allergies against particular seasonal airborne pollen types. Comparison of the time of occurrence of a particular pollen type using the pollen calendar and the time of allergic symptoms, can lead to accurate diagnosis and preventive measures being taken. This study has confirmed that grass pollen is the major source of allergenic pollen in the external environment triggering hay fever and allergic asthma in spring and early summer in Melbourne, Australia.     

武昌地区豚草花粉症研究

豚草原产北美洲,为一年生草本,高达200cm,属风媒植物,是北美地区引起花粉症的主要致敏植物\"'。自40年代进入我国后,迅速蔓延。为探明武昌地区豚草的分布及其花粉在空气中的污染情况,我们于19g4年5月1日～1995年4月30日对本地区豚草花粉及其致敏性进行了调查、研究。1材料     

Pinus pollen in the atmosphere of Vigo and its relationship to meteorological factors

The Pinus genus has an elevated pollen production and an anemophilous nature. Although considered to be hypoallergenic, numerous cases of allergies caused by Pinus pollen have been cited and different authors believe that its allergenicity should be studied in more depth. In the city of Vigo several patients have tested positive for Pinus pollen extracts in skin tests, some of them being mono-sensitive to such pollens. In order to ascertain the behaviour of Pinus pollen and its correlation to the main meteorological factors, we carried out an aerobiological study in the city of Vigo from 1995 to 1998 by using a Hirst active-impact volumetric sporetrap, model Lanzoni VPPS 2000, placed on the left bank of the Vigo estuary (42°14’15’’N, 8°43’30’’W). Pinus has high quantitative importance in the airborne pollen spectrum of the city. It is one of the best represented taxa constituting 13%–20% of the total annual pollen levels. The quantity of Pinus pollen present in the atmosphere of the city of Vigo throughout a year is 5751 grains (as the average for the sampled years), with a very long pollination period, from the middle of January until May. The maximum concentration was recorded in 1998 with 1105 grains/m³ on 3 March, a much greater value than those for the previous years. At the end of its pollination period there is usually a final increase in Pinus pollen concentrations coinciding with the pollination of Pinus silvestris, which are more abundant in mountainous areas far from the city. Received: 17 March 1999 / Revised: 20 December 1999 / Accepted: 20 December 1999     

花粉—气候因子转换函数建立及其对古气候因子定量重建

以中国北方215块表土孢粉样品分析结果中的13种花粉类型与4种气候参数为基础资料建立花粉-气候因子转换函数。同时选取内蒙中部调角海子DJ钻孔岩芯高分辨率孢粉分析结果为材料,定量重建该地区10000～2100 a BP古气候因子数值特征。研究结果表明:内蒙古调角海子地区进入全新世后温湿状况较前全新世有了明显好转,在中全新世形成最为良好的气候要素组合。最高年平均温度比现在高4℃左右,最低年平均温度比现在低2℃左右。7月份和1月份平均温度的分析结果表明,1月份平均温度变化趋势较7月份的更接近年平均温度的变化趋势,说明该地区冬季温度占主导地位。在气候转折时期,气温和降水随时间的变化梯度明显加强,波动幅度为4～5℃。     

The effect of varying the number of pollen grains used in fertilization

Summary The number of pollen grains placed upon a stigma influence both the development of pollen tubes and subsequently the progeny which result from fertilizations by gametes from these pollen tubes. The first influence is demonstrated by reduced pollen tube growth rates when pollen grains are few in number. This may indicate direct effects of pollen tubes upon the stylar tissues or perhaps more complex interactions between pollen and style. The second and potentially more important influence of limited pollination is upon the progeny. This was demonstrated with studies on three species. In each case, variation among the resultant plants was greater when pollen was limited than when normal, that is excessive, pollen was used. The mechanism of this phenomenon is not certain, but our data indicate that it is not simply an artefact of variation in seed size.     

Aerobiology of Vigo, North-Western Spain: atmospheric pollen spectrum and annual dynamics of the most important taxa, and their clinical importance for allergy

Vigo is a city located in the northwest of the Iberian Peninsula. Influenced by the Atlantic climate, it is surrounded by a Eurosiberian-type vegetation, modified by the introduction of forestry and ornamental species. Different ruderal vegetation types, resulting from human influence, grow in the area. The study of the pollen content of the air of Vigo started in 1989, with a Cour trap. Average results for the period 1989–1995 are presented in this paper, together with the lowest and highest values found. The representativeness of the mean values is analysed by calculating the coefficient of variation of the data series. Most pollen types in the atmosphere of Vigo are from tree species (54.2%); an important proportion comes from herb species (43.9%) and very few (1.8%) correspond to shrub species. A total of 73 different pollen types have been identified. The most abundant, listed in decreasing order of mean annual values for the period, are:Pinus (25.1%), Poaceae (21.1%), Urticaceae (14.6%),Quercus (8.5%),Castanea (3.7%),Betula (3.6%),Eucalyptus (3.4%),Plantago (3.2%),Alnus (2.1%), Cupressaceae (2.1%), Oleaceae (1.6%;Olea 1.3%),Platanus (1.3%),Rumex (1.3%), Chenopodiaceae/Amaranthaceae (1.0%), Ericaceae (0.8%), Asteraceae (0.6%;Artemisia 0.1% andTaraxacum type 0.2%) andMercurialis (0.5%). A pollen calendar showing the annual dynamics of all these pollen types is presented in this paper. A parallel study of the clinical importance of respiratory allergies in Vigo was also conducted. From a sample of 2750 patients, 87.2% suffered from rhinoconjunctivitis, 26.0% of these due to pollen, and 78.3% from asthma, 17.2% due to pollen. The pollen types responsible for these allergies, listed in decreasing order, are: Poaceae (78%),Parietaria (12%),Chenopodium (11%),Plantago (9%), Oak (4%),Artemisia (3%),Pinus (3%),Eucalyptus (3%),Olea (2%),Platanus (2%),Castanea (2%),Taraxacum (2%),Rumex (2%),Betula (1%),Cupressus (1%) andMercurialis (1%).     

Specific IgE and IgG4 antibodies to Japanese cedar pollen and total IgE antibody in lumbermen

Serum levels of specific IgE and IgG4 antibodies to Japanese cedar (Cryptomeria japonica) pollen and total IgE antibody in 75 lumbermen and in 53 male office workers at an urban establishment were measured by means of an enzyme linked immunosorbent assay (ELISA) and compared. No significant differences of specific IgE and IgG4 to cedar pollen and total IgE were found between the lumbermen and the office workers. There were no significant differences of incidence of cedar pollinosis and positive (greater than 100 FU/ml) rate of serum specific IgE between the two groups, though the lumbermen were exposed to dense concentrations of cedar pollen in their working area. In the lumbermen who showed positive values of specific IgE, the mean value of the specific antibody in Japanese cedar pollinosis lumbermen was significantly higher than that in symptom-free lumbermen, while no significant differences of serum level of specific IgG4 were found between the two groups.     

武汉市武昌地区气传致敏花粉调查研究

应用曝片法连续３６５ｄ收集武昌地区３个调查点的气传花粉,全年共检同花粉４８６４３粒,分属２８个科,属。一年中出现２次花粉高峰,即３～４月份,８～９月份,其中优势花粉为悬铃木属（Ｐｌａｔａｎｕｓ）柏科（Ｃｕｐｒｅｓｓａｃｅａｅ）,松属（Ｐｉｎｕｓ）蒿属（Ａｒｔｅｍｉｓｉａ）等;最主要的致敏花粉为蒿属,豚草属（Ａｍｂｒｏｓｉａ）对影响本地区空气中花粉飘散的因素,几种优势花粉的致敏特点及其临床意义作了初     

武汉市武昌地区气传致敏花粉调查研究

应用曝片法连续365d收集武昌地区3个调查点的气传花粉,全年共检出花粉48643粒,分属28个科、属。一年中出现2次花粉高峰,即3～4月份,8～9月份。其中优势花粉为悬铃木属（Platanus）、柏科（Cupressaceae）、松属（Pinus）、蒿属（Artemisia）等;最主要的致敏花粉为蒿属、豚草属（Ambrosia）。对影响本地区空气中花粉飘散的因素,几种优势花粉的致敏特点及其临床意义作了初步探讨。     

Are modern savannas degraded forests?-A Holocene pollen record from the Sudanian vagetation zone of NE Nigeria

A pollen record from a crater lake (Lake Tilla, 10°23N, 12°08E, c. 700 m asl) in the Sudanian zone of northeast Nigeria provides evidence for the persistence of woodland savanna throughout the Holocene. Wetter conditions from c. 10,000 B.P. to c. 6800 B.P. enabled the establishment of a dense Guinean savanna, though the occurrence and rapid spread of the montane elementOlea hochstetteri indicates cool climatic conditions prior to c. 8800 B.P. Patches of closed dry forest may have existed, but never completely displaced the savanna vegetation. Grass fires were frequent throughout the Holocene and were probably important in promoting the open character of the vegetation. From c. 6800 B.P. onwards a gradual floristic change from a Guinean to a Sudano-Guinean savanna and a lowering of lake levels point to drier environmental conditions, which intensified around 3700 B.P. Human impact might have caused increasing sedimentation rates from c. 2500 B.P. onwards. The pollen diagram of Lake Tilla reflects a history of the savanna which appears to have been primarily controlled by climatic changes. The lack of unambiguous pollen indicators might be the reason why human activities remain palynologically hidden even for the late Holocene.     

武汉地区空气中花粉调查研究

空气中花粉粒的调查研究属气传孢粉应用学科,它正愈来愈受到临床医学界的重视。掌握本地区空气中花粉播散规律,对预防、诊断、治疗呼吸道过敏性疾病具有十分重要而现实的意义。本文着重报道了从1985年4月1日至1986年3月31日在武汉地区空气中孢粉散布的基本规律,并讨论分析了空气中花粉含量与气候的关系。根据花粉在空气中出现时期的长短及数量的多少,笔者把武汉地区空气中常遇到的一些植物花粉分为3种类型,这对考虑湖北武汉地区哪些植物花粉可能导致过敏性疾病是有意义的。     

Predicting the intensity of the birch pollen season

We present a model for the prediction of the magnitude ofBetula flowering and pollen dispersal which may be used in the management of birch pollinosis and in the planning of clinical trials. The pollen sum during the flowering season is regressed on the temperature sum from May 1st to July 20th during the initiation year, the pollen sum of the initiation year, and the temperature sum during the main pollen season in the flowering year. We suggest that the fluctuating flowering pattern inBetula alba-species is primarily determined by the availability of assimilation products during inflorescence initiation and development during the spring one year before anthesis. When inflorescences, which are initiated during the previous year, elongate in the beginning of anthesis, they act as strong sinks to stored carbohydrates, and thus compete with developing leaves and shoots. The result is an initially reduced photosynthetic capacity in years with intense flowering, and a limited potential for the initiation of new inflorescences for the following year. The ambient temperature during catkin initiation affects assimilation efficiency and is a determinant of about equal importance to flowering intensity as is the magnitude of the flowering in the initiation year. The amount of pollen dispersed is also dependent on the weather during anthesis, which is not possible to predict until about one month in advance. The two other independent variables are available during the previous summer, making it possible to give a sufficiently valid prediction to allergologists about the magnitude of the next birch pollen season, according to its botanical determinants. We suggest that the varying reproductive output inBetula alba should not be described as true masting. A more parsimonious explanation to the flowering pattern is that an individual continually maximizes reproductive effort, according to what is possible, but that reproduction is often constrained by the environment.     

Vegetation history of Lago Battaglia (eastern Gargano coast,Apulia, Italy) during the middle-late Holocene

A pollen and charcoal record from Gargano (southern Italy) provides new information on the vegetation history and environmental change in southern Italy during the middle to late Holocene. The chronological framework is provided by six AMS radiocarbon dates carried out on plant macroremains. Pollen diagrams record a Mediterranean vegetation along the coastland and a stable mixed oak forest at higher elevations between ca. 5900 and 4200 cal b.p. A sharp and dramatic fall of tree pollen concentrations and a change in fire frequencies occurred from approximately 4200 cal b.p. suggesting a climate change towards drier conditions. This event is coherent with regional and extra-regional palaeoclimatic records that suggest that a mid-Holocene dry period was experienced in southern Italy, southern Spain, and perhaps further afield. Human impact on vegetation seems to have occurred since about 2700 cal b.p.     

Influence of climatic factors on the development of pneumonia in lambs

Pneumonia is responsible for important economical losses in the sheep industry in Spain and many other sheep-rearing countries, being the main cause of lamb death, and of losses due to condemnations in abattoirs and of drug costs. This respiratory syndrome is a complex disease involving the relationship between host and environment. The present study analyses the influence of environmental factors on the development of pneumonia in lambs. Statistically significant correlations were found between pneumonia as a cause of lamb death and climatic factors such as rainfall, humidity and intensity and direction of wind. The type of farm building was also an important factor to take into account in order to improve the prevention of pneumonia in lambs. Moreover, the age of the lambs was seen to be a significant item in the study of pneumonia. Respiratory pathology increased from 23 days of age. This fact permits the implementation of measures from birth to 23 days with a view to reducing pneumonia and its negative influence on lamb production. The paper discusses the practical implications of these findings for sheep production.     

Predicting the intensity of the birch pollen season

We present a model for the prediction of the magnitude ofBetula flowering and pollen dispersal which may be used in the management of birch pollinosis and in the planning of clinical trials. The pollen sum during the flowering season is regressed on the temperature sum from May 1st to July 20th during the initiation year, the pollen sum of the initiation year, and the temperature sum during the main pollen season in the flowering year. We suggest that the fluctuating flowering pattern inBetula alba-species is primarily determined by the availability of assimilation products during inflorescence initiation and development during the spring one year before anthesis. When inflorescences, which are initiated during the previous year, elongate in the beginning of anthesis, they act as strong sinks to stored carbohydrates, and thus compete with developing leaves and shoots. The result is an initially reduced photosynthetic capacity in years with intense flowering, and a limited potential for the initiation of new inflorescences for the following year. The ambient temperature during catkin initiation affects assimilation efficiency and is a determinant of about equal importance to flowering intensity as is the magnitude of the flowering in the initiation year. The amount of pollen dispersed is also dependent on the weather during anthesis, which is not possible to predict until about one month in advance. The two other independent variables are available during the previous summer, making it possible to give a sufficiently valid prediction to allergologists about the magnitude of the next birch pollen season, according to its botanical determinants. We suggest that the varying reproductive output inBetula alba should not be described as true masting. A more parsimonious explanation to the flowering pattern is that an individual continually maximizes reproductive effort, according to what is possible, but that reproduction is often constrained by the environment.     

Short-term climate changes in the southern Aegean Sea over the last 48,000 years

High-resolution palaeoenvironmental changes, corresponding to a mean time interval of 450 years covering the last 48,000 years, were examined in a core from the Cretan Basin in the southern Aegean Sea. The intensity and duration of the climatic and oceanographic events were determined by examining the compositional changes in the planktonic foraminifera and pollen assemblages, along with the δ¹⁸O signal of Globigerinoides ruber. A reconstruction of sea-surface temperatures was attempted using the Modern Analogue Technique (MAT). In total, 10 stadials and 6 interstadials occurred over the last 48,000 years. These fluctuations in climatic conditions coincide with fluctuations documented in the western and central Mediterranean and seem to be associated with Dansgaard–Oeschger events. Some of these climatic fluctuations are correlated with changes in the vegetation in the surrounding land.

Between 48 and 10 cal kyr BP the most pronounced stadials occurred at 41 cal kyr BP (C69-ST10) and at 13 cal kyr BP (C69-ST4). These events are characterized by: (i) high positive δ¹⁸O values of Globigerinoides ruber, (ii) drops in SST and (iii) increases in aridity. These events may be correlated with the Heinrich H4 event and the Younger Dryas event, respectively. Two other stadials at 23 cal kyr BP (C69-ST6) and at 16 cal kyr BP (C69-ST5) which are characterized by increases in the abundance of the cold plaktonic foraminifera species and increases in aridity may be correlated with the H2 and H1 events, respectively. The dominant planktonic foraminiferal species during the stadials witch are correlated with the Heinrich events were Turborotalita quinqueloba and Globorotalia scitula. The most pronounced interstadials occurred between 39.5 and 38.5 cal kyr BP (C69-IST6) and between 25 and 24 cal kyr BP (C69-IST3) and are characterized by depletion in δ¹⁸O values, increases in SST and increases in humidity. The former event coincides with the formation of the sapropelitic layer S2.

In the Holocene the most pronounced stadial occurred between 8 and 6.5 cal kyr BP (C69-ST2), during the interruption of S1 and is characterized by a reduction in SST and an increase in aridity. The most pronounced interstadials of Holocene occurred during the formation of S1a and S1b between 9 and 8 cal kyr BP (C69-IST1) and between 6.5 and 5.5 cal kyr BP (C69-IST2), respectively. These events are characterized by depletion in δ¹⁸O values, increased SST and an increase in humidity as is indicated by the expansion of temperate evergreen and Mediterranean taxa in the pollen record.