榆科榉属的植物地理学

榉属是东亚—地中海间断分布局,分属于东亚植物区、地中海植物区及伊朗—土兰植物区。根据现存榉属植物的形态演化趋势、细胞学、孢粉学证据及其化石资料和古地质历史事件相结合分析,该属植物是第三纪温带森林的孑遗成分而且第三纪末期的喜马拉雅造山运动及第四纪的冰川作用是样属植物演化的主要动力。在欧洲,由于喜马拉雅造山运动及第四纪冰川作用的较强烈,使分布于此的榉属植物受到严厉的生存竞争,未能适应环境的物种遭受灭绝,少数进行适应性变异的物种在极端环境条件下生存了下来。而东亚地区由于自然环境相对较稳定,便成了榉属植物的避难所,因此也保留了榉属植物种较为古老的种类。     

豆科黄华族植物地理学的初步研究

在系统学业伦和地理分布及古植物学资源的基础上,利用形态－地理学的原理和方法,对豆科Papilionaceae黄华族和Tribe Thermopsideae进行了植物地理学的初步研究。结果表明,（１）黄华族可能是古地中海起源的,它的起源地在古北大陆的南岸,大约相当于现在的中纬度地区;（２）起源时间能早于第三纪,大约处白垩纪末和始新世之间。当时有一个所谓的“北热带植物群”Ｂoreotropical Flora发生;（３）本族６个属基本上构成一个比较自然的单元。它们是由原始槐族类祖先演化而来的;（４）木本类是本族原始的,早出的类群,它们基本上处于遗状态;草本类是本族进化的、晚出的类群,们种类多,分布区有扩大的趋势;（５）Ｔhermopsis间断分布于亚洲（包括中亚和东亚）、北美（包括北美东部和北美西部。东亚太平洋沿岸和北美大西洋沿岩最有可能是它的原始保存地,而不是起源地,它们主要是通过古地中海海道而发生联系的,造成原始类群星散分布的格局不是由一次,而是多次地史和气候变化的结果;（６）晚第三纪亚洲腹地造山运动引起的喜马拉雅山的降起和青藏高原的抬升,以及北美落基山山体抬升引起的水温条件的急剧变化是某些类群（包括Piptanthus和Thermopsis)物种局部分化的主要动力。     

Oleaceae in Trieste (NE Italy): aerobiological and clinical data

Oleaceae pollen concentrations in the Trieste area are low (<10%) compared to the total number of airborne pollen grains, with only one pollination peak at the beginning of June when the Oleaceae concentration reached 62% of the total pollen count in 1992. This peak was due to an exceptionally high pollination of olive trees in 1992, when airborne pollen concentration rose to 1357 pollen grains/m³ on June 3. Sensitization toOlea increased from 1989 to 1993, when it was present in 23.4% of symptomatic patients, but the role ofOlea in inducing allergic respiratory symptoms is difficult to evaluate because almost all patients were sensitized to other pollens, and in particular to Gramineae: only four subjects were sensitized toOlea alone (1.4%). Despite the low Oleaceae pollen counts, this pollinosis is increasing, probably because of increased cultivation ofOlea in recent years. However, although skin prick test positivity is common in polysensitized patients, its role in inducing sensitization and symptoms is presently less important than that of other pollens.     

Phytogeographical analysis of a treeline community in northern Yukon (NW-Canada)

The phytogeography of a treeline Salix pulchra community from the northern Yukon is studied by means of classification and ordination on a matrix of species and Operational Geographic Units. The basic data were obtained from the global distributions of the species. Results suggest that this community is an example of pre-glacial treeline vegetation which survived in ice-free areas within ancient Beringia.Abbreviations OGV = Operational Geographical Unit     

Late Quaternary vegetation history at Stracciacappa (Rome, central Italy)

The pollen diagram from Stracciacappa (Sabatini volcanic complex, Rome) provides a record of vegetational and climatic change spanning the last 60000 years, which is the time since when volcanic activity in the crater came to an end. The chronological framework of the sediment core is set by five AMS and three conventional radiocarbon dates; the mean sedimentation rate obtained by radiocarbon measurements was used to extrapolate the age of the record beyond the reach of ¹⁴C dating. The sequence from Stracciacappa provides results of fundamental importance for the understanding of the vegetational changes which occurred during the last pleniglacial period in central Italy, and it can be considered as a reference pollen record for the regional biostratigraphic characterization of this period. The site shows a high climatic sensitivity, particularly highlighted by the development of some pleniglacial oscillations with woodland, which interrupted the succession of steppe and grassland vegetational formations typical of the glacial periods. Unfortunately, due to sedimentation problems and alteration of the top level sediments, the Holocene is only recorded in part. Only for one millennium, from ca. 8300 to 7200 uncalb.p., was a real forest expansion characterized by over 90% arboreal pollen found.     

Vegetation mapping in Italy

A brief history of the vegetation mapping in Italy is described. The principal types of maps are physiognomical, of vegetation belts, of vegetation series, phytosociological, of dynamical tendencies in vegetation, ecological, of potential vegetation and environmental. The first botanical map of whole Italy was made by Fiori in 1908 and it is of physiognomical type. The last one was realized by Pedrotti in 1989 and represents the natural potential vegetation (in 1:1 500 000 scale).This report was oral presented at the V^th International Congress of Ecology (August 23–30, 1990 - Yokohama, Japan).     

Mediterranean hay meadow communities: diversity and dynamics in mountain areas throughout the Iberian Central Range (Spain)

This paper reports a phytosociological study on managed hay meadow communities in the main mountains of the Spanish Central Range. Multivariate techniques (Cluster analysis and CA-ordination) were applied in the classification of the relevés and ordination of vegetation units and species. Clusters were related to the following associations: Agrostio castellanae–Arrhenatheretum bulbosi, Festuco amplae–Cynosuretum cristati, and F. amplae–Agrostietum castellanae. The scattergram suggested that the dynamic patterns between communities are associated with soil nutrient content and moisture. We propose a new subassociation: F. amplae–A. castellanae gaudinietosum fragilis that includes Salmantincensean Agrostis castellana communities growing in regions with lower supramediterranean thermotype.     

Human impact during the Bronze Age on the vegetation at Lago Lucone (northern Italy)

Lake-sediment records were used to reconstruct human impact on the landscape around Lago Lucone (45°33′N, 10°29′E, 249 m a.s.l.), a former lake in the western amphitheatre system of the Lago di Garda. Presence of prehistoric human populations is attested by pile-dwelling settlements from the Early-Middle Bronze Age, with one settlement at a distance of only 100 m from the coring site. Pollen, plant-macrofossil and microscopic charcoal analyses were applied to a 250 cm sediment core with four dates providing the time control. A mixed oak forest that was important during the Early-Middle Holocene was cleared and replaced by open vegetation during the Bronze Age (∼2000–1100 b.c.) when open lands were estimated to have covered more than 60% of the total relevant pollen-source area. During a phase of high human impact, independent climatic proxies suggest warm and dry climatic conditions. Later, ca. 1100 b.c., palaeobotanical evidence indicates a sharp decrease in human pressure in the Lago Lucone area. The comparison with other sedimentary palaeocultural records shows that the period 1300–1100 b.c. was characterised by general declines of agricultural activities both south and north of the Alps. These declines have been previously attributed to a change towards wetter and colder climatic conditions in and around the Alps. However, the decline in human impact around Lago Lucone cannot be exclusively attributed to climatic variation. Therefore other forcing factors independent of climatic changes, such as cultural crises or changes in spatial organisation of the habitats, cannot be ruled out under the present state of knowledge.     

The warmth index of Kira for the interpretation of vegetation belts in Italy and SW. Australia two regions with Mediterranean type bioclimates

The Warmth Index of Kira was calculated for 36 meteorological stations in Italy and 18 stations in SW. Australia, both countries with mediterranean type climate. On the basis of a correlation with rainfall it appears possible to indicate distinct ecological spaces for most climatogenous vegetation types. A remarkable ecological parallelism between the natural vegetation in Italy and SW. Australia can be evidentiated; some particular features are discussed.     

Mire vegetation in the Apuanian Alps (Italy)

Mire vegetation in the Apuanian Alps (N Italy) is analyzed from the phytosociological and the synecological points of view. Three vegetation types are delimited by numerical methods and compared with mire communities of the Alps and the Apennines. Furthermore, a chorological evaluation of this vegetation is attempted on a floristical basis.     

Aerobiology of Fagaceae pollen in Trieste (NE Italy)

The aerobiological behaviour of Fagaceae in Trieste and the correlations with the meteorological parameters were examined. Airborne pollen grains of Castanea, Fagus and Quercus were collected from 1990 to 2003 using a Hirst type spore trap. The main pollen season (MPS) takes place in April and May for Quercus and Fagus, in June and July for Castanea. The highest values occur in year 1993 for Quercus, in 1998 for Castanea and in 1992 for Fagus. The Fagaceae content of the air is mainly due to Quercus and Castanea pollen, Fagus usually having a scarce pollen shedding in Trieste. The highest counts of Fagaceae pollen grains are found from late April to mid May and are mainly due to the pollen shedding of oaks. The cumulative counts vary over the years, with a mean value of 2.719 pollen grains, a lowest total of 1.341 in 2002 and a highest total of 4.704 in 1993. No positive nor negative long-term trends in pollen shedding are found. No cyclic variations were observed. Spearman’s correlation was used to establish the relationship between the daily pollen counts and the daily meteorological data. Daily pollen concentrations present sometimes positive correlation with temperature, negative with rainfall and wind speed, and no correlation with humidity. Fagus and Quercus start dates result positively correlated between themselves. Significant correlations are found between the start of MPS and the mean and maximum temperature in March for Fagus and Quercus, and May for Castanea.     

Mitochondrial DNA polymorphisms in the Albanian population of Calabria (Southern Italy)

RFLPs of mtDNA for HpaI, BamHI, HaeII, MspI, AvaII and HincII were analyzed in 100 individuals from 15 Albanian villages of the Cosenza province (Calabria, Southern Italy). Thirteen mtDNA types were identified, one of which is new and is due to an AvaII morph (AvaII 27^Alb) never described before. Other two types (15-2 and 40-2) previously unfound in Italians were detected in one and two individuals respectively. The intra-group homogeneity (F=.49) resulted to be the highest found among the Italian groups examined so far. It is however very similar to that of a control sample of the Calabria population (F=.46). On the whole no important differences have emerged in the comparison between Albanians and not Albanians from Calabria. These results can indicate either that the markers we examined are not discriminative or that genetic admixture has occurred at least by immigration of Calabrian women into the Albanian group.     

Aerobiology of Urticaceae pollen in Trieste (NE Italy)

The aerobiological behaviour of Urticaceae in Trieste and the correlations with the meteorological parameters were examined. Airborne pollen was collected from 1990 to 1999 using a Hirst type spore trap (Burkard) and the data interpretation was performed according to the standard method adopted by the Italian Aeroallergen Network. The main pollen season of Urticaceae in Trieste goes from mid-April to mid-September. The highest values occur in May and June. Although different seasonal patterns are found every year, the main peak occurs on average at the beginning of May, followed by other decreasing peaks until September. Thecumulative counts vary greatly over the years, with a mean value of 18.315 p/m³. The maximum annual total pollen grains was registered in 1996 and the minimum in 1991. Spearman's correlation was used to establish the relationship between the daily pollen counts and the daily meteorological data both considering their original quantitative values and transformed values according to their day by day changes. Daily pollen concentrations present usually positive correlation with temperature, negative with rainfall and wind speed and no correlation with humidity. Better results were obtained with transformed values.     

The Massaciuccoli Holocene pollen sequence and the vegetation history of the coastal plains by the Mar Ligure (Tuscany and Liguria,Italy)

A 90 m deep core from the Massaciuccoli lake basin (Tuscany, Italy) offers new material for improving the knowledge of the Holocene vegetation history in the coastal plains in Tuscany and Liguria bordering the Mar Ligure (Ligurian sea). In this paper, an assessment of the upper part of the core is presented. During the Holocene, the area was covered by woodlands whose composition changed in time. Numerous oscillations of the tree taxa were recorded which can probably be connected to sea level variations that had a strong influence on the depth of the water table. Human impact is evident particularly at ca. 4200–2500 b.p. when traces of opening of the woodland accompanied by noticeable pollen percentages of Vitis could suggest an early agricultural practice favouring this native plant. The new data have been integrated with previous palaeobotanical and archaeobotanical research. The occurrence of coastal wetlands has been shown. Throughout the Holocene, Mediterranean evergreen vegetation is generally poorly represented; it becomes widespread only in the late Holocene, suggesting that its establishment was probably favoured by the management practices in the coastal plains, particularly land reclamations, starting from the Roman period.     

Pollen concentrations in central Italy (Ascoli Piceno and Perugia)

Summary Air-borne pollen grains were collected using Hirst volumetric spore traps in both Ascoli Piceno and Perugia during the March–November 1983 period. Similar types of pollens were recorded in both towns. In Perugia, higher total amounts of Cupressaceae/Taxaceae pollens were recorded in March and of Quercus, Gramineae, Urticaceae and Oleaceae in May–June. However, the pollen concentration in the Ascoli Piceno atmosphere was higher in the August–October period owing to the pollen of the ?summer weeds?.

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Riassunto I granuli di polline aerodiffusi sono stati campionati con trappole volumetriche tipo Hirst sia in Ascoli Piceno che in Perugia durante il periodo marzo–novembre 1983. In entrambe le città sono stati rilevati tipi di polline simili. In Perugia sono state registrate concentrazioni di polline in atmosfera più elevate rispetto ad Ascoli Piceno in marzo per la pollinazione di Cupressaceae/Taxaceae e in maggio–giugno per la pollinazione di Quercus, Gramineae, Urticaceae e Oleaceae. In Ascoli Piceno, invece, la concentrazione di polline in atmosfera è state più elevata di Perugia nel periodo agosto–ottobre per la pollinazione delle ?erbe estive?.

     

Phenological surveys of allergenic species in the neighbourhood of Bologna (Italy)

The results of phenological observations in ageomorphologically differentiated area are shown.Phenological surveys were conducted on flowering andpollen emission of some common and widely diffusedGraminaceae species, using a 7-step key. By means ofmultiple regression analysis altitude,latitude, slope and exposure were identified as significantenvironmental factors in giving rise to thepollination: in particular with respect to altitude thephenological pattern showed a negative gradient below100 m of altitude and a positive one above.     

Pollution of soil and vegetation in the Thriasian Plain,Greece

Summary The Thriasian Plain near Athens in Greece is a site of concentrated industrial development. Total concentrations of Pb, Cd and extractable SO₄ ^2– in surface soil samples collected from this area, were found to be, respectively, 2–7, 6–34 and 2–20 times higher than those in similar soil samples from parts of the country remote from industrial activity.Total concentrations of Pb, Cd, Zn, Cr and S in samples of olive leaves from the same area were found to be, respectively, 4–40, 3–10, 3–9, 2–6 and 17–21 times higher than those found in samples of olive leaves from rural sites. Leaves of cabbages growing in the area contained between 0.82 and 40 g/g (wet weight) of Pb.Addition of Cd, Ni and Cu to a calcareous potted soil at concentrations of 100, 200 and 200 ppm increased the concentrations of the metals in the needles of Aleppo pine (Pinus halepensis) seedlings to 4.5, 3.5 and 10 ppm, respectively, after 7 months growth in the nursey.     

The halophilous vegetation of the Po Delta (northern Italy)

The halophilous vegetation in the Po Delta region (north Adriatic) has been studied with the Braun-Blanquet method. Vegetation types have been defined by numerical classification of vegetation data. Their ecology has been studied by indirect gradient analysis. The following three main groups of phytocoena have been recognized. (1) Perennial halophytic vegetation (class Puccinellio-Salicornietea) including 7 associations: Spartinetum maritimae, Puccinellietum palustris, Salicornietum radicantis, Salicornietum fruticosae, Agropyro-Inuletum crithmoidis, Halimionetum portulacoidis, are quoted according to an approximate gradient of decreasing soil moisture. The Juncetum maritimi is conditioned by soil erosion. (2) Therophytic vegetation settled on soils subject to natural or artificial disturbance (class Thero-Salicornietea), including 3 associations: Suaedo-Kochietum hirsutae, Salicornietum herbaceae s.1. and the Aster tripolium-Suaeda maritima community. (3) Halotolerant vegetation (class Artemisietea vulgaris), including only the Atripliceto-Elytrigietum pungentis settled on soils with a low salt content.Nomenclature of species follows Pignatti (1982).The research was supported by a grant of the Istituto per i Beni Artistici, Culturali e Naturali, Regione Emilia-Romagna (Italy) and by a grant of the Italian C.N.R. (Research Group for Naturalistic Biology).     

Changes in the flora and vegetation of the coastal dunes of Voorne (The Netherlands) in relation to environmental changes

Ecologically the former isle of Voorne is very varied. This is reflected by an exceptionally high number of plant species and vegetation types. Many data regarding flora and vegetation have been collected during more than 25 years. A comparison of the early and the later data show that in this period many changes have taken place in flora and vegetation. The changes are partly the result of a natural development of the vegetation, but to a considerable extent they are due to human activities in the coastal area itself and in its surroundings. Examples of changes produced by natural developments and by human activities are given. The effects on flora and vegetation of the area are illustrated by comparing flora inventories, vegetation maps and permanent plot studies. In addition, the future development in the region which will strongly affect its natural value, is discussed.I would like to thank Michiel Boeken, Joke van der Linden and Elly van Oosterhoud who carried out the second flora inventory and Jeanette van Beuzekom and Inge Boelens who mapped parts of the Voorne dune area. I am particularly indebted to Wiecher Smant who offered assistance in many ways.