The tenebrionid beetles on 25 circum-Sicilian islands were studied to determine the influence of island geographical and landscape features on three main intercorrelated biogeographical patterns: (1) species richness, studied using species-area and species environment relationships, (2) species assemblage composition, investigated using Canonical Correspondence Analysis (CCA), and (3) inter-site faunal similarity, investigated using Canonical Correlation Analysis (CANCOR) applied to multidimensional scaling of inter-island faunal dissimilarities. Species richness was mostly influenced by island area and landscape heterogeneity (expressed using various indices of diversity based on land cover categories). When species identities were considered in the CCA, no substantial effect of landscape was detected. Current island isolation did not have a strong influence on species richness, but has a distinct effect in determining species assortments on the remotest islands. Historical influences of Pleistocene landbridge connections were not detectable in species richness relationships using geographical variables in species richness analyses or in assemblage gradients in the CCA, but emerged distinctly from inter-island similarities in the CANCOR. and Simone Fattorini.
Large-scale phylogeographical patterns and the underlying factors driving species divergence in Mesoamerica are poorly understood, but it is widely documented that tectonic events and Pleistocene climate changes play an important role in determining species diversification. As glaciations in Mesoamerica developed only around high mountains, one hypothesis is that the known effects of the Last Glacial Maximum on the geographical distribution and genetic diversity of bird populations, producing the contraction/ expansion latitudinal pattern observed in temperate bird species, should be largely undetected in resident bird populations inhabiting environmentally more stable habitats. To gain insight into the effects of Quaternary habitat and climate stability on the genetic diversity, we use ecological niche modelling and generalised linear modelling to determine the role of changes in habitat stability on the genetic diversity in eight widespread or range restricted hummingbird species. We found lesser changes in suitable habitat from past to present in most of the species than those predicted by palaeodistribution models at northern temperate regions. Contemporary seasonal precipitation, Quaternary habitat and climate stability had superior explanatory power, but the magnitude and directionality of their effects on genetic diversity varied between range-restricted and widely distributed species. We observed that the species studied have not responded equally to changes in climate stability in this complex region, suggesting that habitat differences and/or the altitudinal range of the hummingbird species influenced genetic diversity, and that the species-specific responses are not only linked to habitat stability in the region but also to contemporary seasonality associated with the availability of floral resources.
This paper reviews the data on quaternary palynological sequences collected in the Czech Republic, attempts to store them in the Czech Quaternary Palynological Database (PALYCZ) and outlines a possible use for regional syntheses. Work on pollen stratigraphies done over the last hundred years has yielded a very large amount of data for this region. These data can be used globally for various types of environmental reconstructions and are of local importance, especially when combined with local databases. For data to be included in PALYCZ it has to meet certain criteria, the determination of the pollen of herbaceous plants must be well resolved and radiocarbon dated. As of 31 December 2008, we had reviewed 177 pollen profiles. Data from 152 sequences are already stored in PostgreSQL® in relational tables, which allow a broad range of queries to be addressed using the html protocol. The data collected since 1959 by 15 authors contain raw pollen counts together with 14C dates and various metadata on locality. All the pollen samples were ordered using non-metric multidimensional scaling. Display of the ordination diagram incorporating the appropriate millennial time slices revealed a common pattern in all data. The quality of data is also discussed in the context of the history of the research and methods used. Database access can be found at http://botany.natur.cuni.cz/palycz.
This paper presents an overview of the latest information about the beginnings of the technology of pottery making in the area of the forest-steppe belt in Siberia and the Russian part of Eastern Europe all the way to the Ural Mountains. From a continental point of view, a brief spatiotemporal diagram presents a completely different background of the beginnings of pottery in our lands and also in corresponding parts of Southeast Europe, where the origin of pottery has traditionally been linked to the Neolithisation of Europe. The earliest pottery technology in China dates back to 20 000 BP, followed by all the subsequent data from the Far East area to Lake Baikal. The earliest pottery culture, Jomon, which had been developing in Japan for more than ten thousand years, is not included here. In the Russian part of Eastern Europe, pottery technology starts developing only after 8 000 BP. Typologically uniform and mostly unchangeable development of beaker-shaped pottery, mostly with a pointed bottom, is common for both these areas. This development continues in Scandinavia and adjacent areas of the Baltic and in Atlantic Europe. In the central parts of Europe, similar shapes only occur sporadically in the earliest period. However, the earliest Eurasian pottery had influenced the development of later prehistoric periods. Numerous settlement groups on the Eurasian continents were characterised by two traditions that are archaeologically recognisable. In simple terms, one of the traditions was agricultural, the other conservative. and Práce předkládá přehled nejnovějších informací o počátcích technologie výroby keramiky v oblastech lesostepního pásma Sibiře a ruské východní Evropy až k Uralu. Data nejstarší keramické technologie v Číně přesahují číslo 20 tis. BC. Na území ruské východní Evropy začíná vývoj keramické technologie většinou až po roce 8000 BC. Obě oblasti spojuje typologicky jednotný a málo proměnlivý vývoj kotlovitých tvarů převážně se špičatým dnem. Na tento vývoj navazuje srovnatelně kulturní posloupnost ve Skandinávii a v přilehlých oblastech Baltu i Evropského pobřeží Atlantiku. V centrálních oblastech Evropy se podobné tvary vyskytnou v nejstarším období zcela ojediněle. Eurasijská nejstarší keramika však nepochybně ovlivnila vývoj i v pozdějších pravěkých obdobích. Početné skupiny osídlení na evropském i eurasijském kontinentu se vyznačovaly dvojí tradicí hmatatelnou archeologicky nejen v keramice. Zjednodušeně řečeno, jedna byla zemědělská, druhá konzervativní.
We present an overview of the emerging field of species-level distributional ecology, particularly as it relates to phylogeographic studies of birds in Eurasia. This field centers around distributional inferences and predictions deriving from the use of ecological niche modeling. We provide a brief historical review, and then proceed to outline a number of crucial methodological considerations, if models are to have biological meaning and reality. We then proceed to provide a worked example, as well as some thinking about directions in which the field should be moving in terms of questions and approaches.
The tenebrionid fauna of the Tuscan Islands (Central Italy) is well known and is an ideal system for studying the role of current and historical factors in determining the biogeographical patterns in a complex archipelago. Cluster analyses, species-area relationships and Mantel tests were used to investigate the influence of current geography and Pleistocene connections with the mainland on the structure of insular communities. Current biogeographical similarity patterns fit both Pleistocene and Recent geography, but marked effects of Pleistocene geography appeared when the influence of Recent geography was removed. Thus, in contrast to more mobile insects, such as butterflies and chrysidids, tenebrionid colonization is likely to have occurred via land-bridges when the islands were connected to the mainland in the Pleistocene. The relict distributions of organisms with poor mobility should be of great concern to conservationists, because depletion of island populations cannot be balanced by new immigrations from mainland populations. The continued influence of man on the Tuscan Islands has adversely affected the natural environment, however, man made habitats may also be colonized and exploited by tenebrionids.
The aim of this paper is to examine whether current and/or Pleistocene geography affect the species richness and composition of Tuscan archipelago butterflies. This archipelago is located between Tuscany (Italy) and Corsica (France). Faunistic data was obtained from the literature and surveys. Our data revealed that contemporary geography is the most important factor determining the species richness and faunal composition of Tuscan archipelago butterflies. Indeed, current area and isolation of the islands are the only predictors significantly correlated with species richness. Paleogeographic features of the archipelago are not significantly correlated with species richness. Multidimensional scaling revealed patterns similar to those reported for other living groups. Specifically, Capraia and Montecristo group together with Corsica, while Elba, Giglio, Pianosa, Gorgona, Giannutri and the fossil island of Monte Argentario group with the Tuscan mainland. Recent geography seems to affect the faunal composition. Indeed Mantel test indicates that the similarity in the faunal composition of the Tuscan Archipelago islands is mainly related to present-day island characteristics and their relative distance from Tuscany and Corsica. Our results are similar to those recently obtained for Aegean archipelago butterflies.
The genetic differentiation of Oxynoemacheilus bureschi (Drensky, 1928) from all three drainages (Struma=Strymon, Mesta=Nestos, Vardar=Axios) where this species occurs, as well as its phylogenetic relationships with other European stone loaches, was assessed using the mitochondrial cytochrome b gene. The phylogenetic reconstruction revealed two distinct clades within the European stone loaches with high bootstrap values. Very low genetic variability with no internal haplotypic structure has been found between and within all examined O. bureschi populations, indicated by low polymorphism and similar haplotypes. According to the nesting design and demographic patterns, the range of O. bureschi was not constant, but underwent expansion in the recent past. Lack of variation, a rather unusual phenomenon for fishes from the southern Balkans, is ascribed to facilitation of dispersal due to seashore regression, confluence events and river capture during the Pleistocene.
Host-parasite cospeciation, in which parasite divergence occurs in response to host divergence, is commonly proposed as a driver of parasite diversification, yet few empirical examples of strict cospeciation exist. Host-parasite co-evolutionary histories commonly reflect complex mosaics of cospeciation, dispersal, lineage extinction and other phenomena. The episodic host-switching model of parasite diversification accounts for complexity by suggesting that diversification and faunal assembly is a consequence of fluctuation between environmental disruption and environmental stability. The phylogeographic predictions of the strict cospeciation and episodic host-switching models were tested using the North American pika/parasite assemblage, with a primary focus on the American pika, Ochotona princeps (Richardson, 1828), and a suite of its endoparasitic cestodes and nematodes. This approach integrating phylogeographic and demographic methods with inferences drawn from species distribution modelling revealed that the parasite community of pikas has been shaped by climate-driven range fluctuation of hosts and bouts of geographic and host colonization by parasites associated with transitions between glacial and interglacial phases.
Cold-season beetles, Catops nigricans Spence, Choleva agilis Illiger and Choleva elongata Payk., i.e. beetles which start to lay eggs in autumn, which are active during the winter in the adult stage and develop from the egg stage to the adult stage mainly during the winter months, were collected from various locations in north-western Europe and reared in the laboratory at varying temperatures and photoperiods.
Reproduction of all species started in autumn and continued during the winter months. Highest reproductive and survival rates occurred at low temperatures and within a small thermal window ranging from 5° to 10°C: The fitness of individuals decreased at higher and lower temperatures. The lower thermal threshold for all developmental stages was in the range from -5°C to +2°C. The metabolisms of the species were independent of temperature in both dormant and non-dormant stages and were elevated in the low temperature range in comparison to other species which show a temperature-dependent reaction pattern.
Optimal dates for reproduction were determined by the duration of an obligatory adult summer diapause. In C. nigricans, which favours the litter layer of deciduous forests, this duration was fine-tuned by exogenic factors, such as photoperiod and temperature. In contrast, the soil-inhabiting species Ch. elongata showed a homeostatic response pattern, independent of temperature and photoperiod. Heritability (h2) of the duration of diapause was approximately 0.26 in C. nigricans, less pronounced in Ch. agilis (ca. 0.12) and not evident in the subterranean species Ch. elongata.
All three species compensated for the vagaries of climate through bet-hedging tactics. Bet-hedging is so pervasive that a recent substantial increase in temperature seems to have a negligible effect on the distribution pattern of all three species. Based on life-history data it is conceivable that both soil-inhabiting Choleva species, which require a relatively low thermal sum for their development, were already present in western Europe during the sub-arctic conditions when ice shields reached their maximum extension during glacial periods by shifting their activity from the cold to the warm season. The Atlantic fringe north of the Pyrenees, where the climate was not cold enough for permafrost during glacial stages, was probably the only refuge where Ch. elongata might have survived. In contrast, the Mediterranean region should have been the northernmost refuge for C. nigricans during glacial periods. This species has relatively high day-degree requirements (= 1150 d°) for individual development when compared to both Choleva species (= 700 d°).