On the distribution of broad-winged moths (Lepidoptera, Oecophoridae) of the Palaearctic fauna

The Palaearctic fauna of broad-winged moths (Oecophoridae with the subfamilies Oecophorinae, Pleurotinae, and Deuterogoniinae) comprises 47 genera and 329 species. The number of species rapidly increases from north to south, from 19 species in the Euro-Siberian taiga Region to 149 in the Mediterranean Region, but the Scythian steppe Region (30 species) and Sethian desert Region (49 species) have relatively poor faunas because the majority of oecophorid species are trophically associated with arboreal plants. The proper desert species are very rare among Oecophoridae moths, and the majority of species in the Sethian desert Region occur in the mountains. The number of endemic species is also greater in southern regions; it amounts for more than half of the total number of species in the Hesperian and Orthrian evergreen forest regions and in the Sethian desert Region. The faunas of European (62 species) and Far Eastern (67 species) deciduous forests comprise close numbers of species but are very different, having only 5 species in common. This fact indicates their long isolation. The Oecophoridae are represented in the Palaearctic mainly by the genera with a small number of species, except for 2 genera, Pleurota (100 species) and Promalactis (85 species). The distribution patterns of these genera are opposite: the species of Pleurota are numerous in the south of West Europe and in North Africa, their number quickly decreasing from west to east and only 2 species being present in China (Wang, 2006). The species of Promalactis are numerous in Southeast Asia, their number quickly decreasing from east to west: 3 species occur in Tibet and only 1, P. splendidella (Amsel, 1935), in Israel and Turkey.     

Mammal distributions in the western Mediterranean: the role of human intervention

The natural distribution of the 17 non-flying mammal species occurring wild in both the Maghreb (north-west Africa) and Iberia (south-west Europe) is considered. It is concluded that only four species – Red Fox Vulpes vulpes, Wild Boar Sus scrofa, Wild Cat Felis silvestris and Otter Lutra lutra – are native to both regions, while another three – Red Deer Cervus elaphus, Brown Bear Ursus arctos and Aurochs Bos primigenius – were native to North Africa until the mid-Holocene but have probably died out naturally. Algerian Hedgehog Atelerix algirus, Barbary Ape Macaca sylvanus, Genet Genetta genetta and Egyptian Mongoose Herpestes ichneumon are widely accepted as introductions to Europe from North Africa. The remaining six species, and Red Deer now found in Africa, were also probably introduced – Rabbit Oryctolagus cuniculus, Weasel Mustela nivalis, Wood Mouse Apodemus sylvaticus and Lesser White-toothed Shrew Crocidura russula from Europe to Africa; Algerian Mouse Mus spretus from Africa to Europe; Savi’s Pygmy Shrew Suncus etruscus perhaps from the eastern Mediterranean to both Iberia and the Maghreb. There are two Maghrebi species which, although not found in Europe, are more closely related to Palaearctic than to Afrotropical species: Garden Dormouse Eliomys melanurus, probably native to north-west Africa, although possible augmentation of the natural population cannot be ruled out, and Whitaker’s Shrew Crocidura whitakeri, a North African endemic. Removal of so many species of European provenance from the list of mammals native to north-west Africa should not be considered to weaken its position as part of the Palaearctic zoogeographical region. Bats and other, non-mammalian, taxa illustrate the clear faunal relationship between the Maghreb and south-west Europe, whilst emphasizing its distinction from subsaharan Africa.     

Basic features of the nemoral curculionid-beetle fauna (Coleoptera,Curculionoidea) from eastern Europe and western Siberia

There are 132 curculionids associated with deciduous trees in eastern Europe and western Siberia. The weevils and bark beetles make up the basis of the fauna, forming almost 80%. The fauna of oak is the richest (64 species). The species composition on the ash-tree (50% are monophages) is highly original. Impoverishment of the species composition from the west to the east is revealed. The fauna declines by 18% from 45 to 55° E. The species composition reduces two times beyond the Urals. The faunal boundaries are revealed from west to east and from east to west. The most significant boundary (47% of the fauna do not pass it) for distribution of species to the east is situated between 40 and 45° E. Two significant faunal boundaries are revealed from south to north. The fauna of curculionids of deciduous trees is formed by four groups of species. The southern European species (54%) and western palaearctic species (40%) dominate. The species composition of the studied territory is similar to the fauna of Middle Europe. Formation of the modern fauna of curculionids of deciduous trees in eastern Europe probably occurred in the Holocene. The western Palaearctic and Transpalaearctic species could have occupied the considered territory since the Late Pleistocene. Southern European species appeared in the considered territory after the Valdai glaciation during the warming in the Atlantic period of the Holocene. Penetration of East Palaearctic species began rather recently (last few decades), probably due to climate warming and economic activities.     

Patterns of formation of the flea (Siphonaptera) fauna in the Caucasus

Fleas of the Caucasus belong to 155 species of 40 genera, constituting 17% and 43% of the species and generic composition of the Palaearctic fauna, respectively. The Caucasian fauna includes 23 endemic species but no endemic genera or subgenera. In the number of species, the Caucasian fauna is similar to that of the Mediterranean Subregion and is significantly poorer than the faunas of the Euro-Siberian (by 2.2 times) and Irano-Turanian (by 1.7 times) Subregions. Based on taxonomic diversity, we can propose a hypothesis on the West and East Palaearctic sources of the Caucasian fauna. The West Palaearctic source has determined the distribution of pulicomorph fleas of the families Pulicidae and Coptopsyllidae from Africa, on the one hand, and of fleas of the genera Ctenopthalmus and Palaeopsylla from Europe, on the other hand. Fleas of the Holarctic genera, such as Ceratophyllus and Megabothris, entered the Caucasus by the north Asian route; fleas of the genera Neopsylla, Rhadinopsylla, and Hystrichopsylla migrated to the Caucasus from east and central Asia by the south Asian route, through Middle and Western Asia.     

Living in a tilted world: climate change and geography limit speciation in Old World anchovies (Engraulis; Engraulidae)

Historical changes in the distributions of temperate species in response to Milankovitch climate cycles have been well documented in palaeontological studies and recently evaluated with phylogeographical methods. How these cycles influence biological diversity remains a matter of debate. Molecular surveys of terrestrial and freshwater fauna demonstrate glacial refugia in low latitudes and range expansions into high latitudes, but few genetic studies have assessed the corresponding impact on marine fauna. In the present study, mtDNA sequences (N = 84) are surveyed to understand the impact of long‐term climate oscillations on ‘Old World’ anchovies (genus Engraulis), a monophyletic group occurring in north and south temperate zones of the eastern Atlantic and the western Pacific. The analysis of a 521‐bp sequence of mtDNA cytochrome b indicates a late Miocene or Pliocene dispersal from the north‐eastern Pacific (California–Mexico) to the north‐western Pacific (Japan), followed by Pleistocene dispersal from the north‐western Pacific to Europe. Geography mandates that populations in southern Africa and Australia were stepping‐stones for this dispersal. However, neither population occupies an intermediate position in the mtDNA genealogy; both populations are more recently derived from their northern neighbours. Haplotype diversity is high (h = 0.93–0.97) in European, Australian, and Japanese anchovies, but low (h = 0.22) in the southern African population, where all haplotypes are more closely related to European specimens than to each other. These southern populations occupy a precarious position, lacking north–south coastlines that allow range shifts during climatic extremes. Recurring extinctions and episodic recolonizations from northern hemisphere populations are the likely results. In this case, ocean‐climatic changes retard rather than enhance opportunities for evolutionary radiations. © 2006 The Linnean Society of London, Biological Journal of the Linnean Society, 2006, 88 , 673–689.     

叶蜂总科昆虫生物地理研究II叶蜂总科广布属的地理分布特性(膜翅目)

本文系统分析了叶蜂总科广布属的地理分布特性。叶蜂总科广布属被分为１２个主要的分布类型,其中全北界分布型６９属,可再分为６种次类型。在各分布型下列举了全部具有该类分布特征的叶蜂总科属名,并提出了一些有关起源与扩散的设想和推论。在广布型属的地理分布研究基础上,对各大生物地理界之间的关系也提出了一些看法。     

Does vicariance shape biotas? Biogeographical tests of the vicariance model in the north‐west European land snail fauna

Aim To investigate the importance of vicariance in shaping the north‐west European land snail fauna. Location North‐west Europe. Methods We tested whether there is a non‐random congruence, i.e. a clustering of species ranges, using a Monte Carlo procedure with a null model that generates range data sets such that their range size distribution, the species richness distribution of the geographic cells and the spatial autocorrelation of the occurrences of a taxon approach the parameters in the real data set. Biotic elements, groups of species with similar ranges, were delimited with Model based Gaussian clustering. The prediction that closely related species belong to different biotic elements, has been tested with a chi‐square test. Results The distribution areas of the north‐west European land snail species are significantly clustered as predicted by the vicariance model. One widespread and seven regional biotic elements were identified. Contrary to the predictions of the vicariance model, closely related north‐west European land snail species belong significantly more often to the same biotic element than should be expected by chance. Main conclusions The clustering of closely related north‐west European land snail species within the same biotic element indicates that speciation modes other than vicariance were frequent or that the imprint of vicariance on the ranges was obscured by extensive post‐speciational dispersal. Extensive dispersal may have been caused by Pleistocene climatic fluctuations. The core areas of the regionally restricted biotic elements might indicate the positions of glacial refugia of land snails.     

Studies of ancient crania from northern Africa

Historical sources and archaeological data predict significant population variability in mid-Holocene northern Africa. Multivariate analyses of crania demonstrate wide variation but also suggest an indigenous craniometric pattern common to both late dynastic northern Egypt and the coastal Maghreb region. Both tropical African and European metric phenotypes, as well intermediate patterns, are found in mid-Holocene Maghreb sites. Early southern predynastic Egyptian crania show tropical African affinities, displaying craniometric trends that differ notably from the coastal northern African pattern. The various craniofacial patterns discernible in northern Africa are attributable to the agents of microevolution and migration.     

Chronologie des sites du Pléistocène inférieur et moyen du nord de l’Afrique

North Africa, and in particular the Maghreb, is a key region for African prehistory in that it contains sites whose chronology covers the entire Pleistocene period from 2.5 Ma to the Holocene. In terms of culture, it fits into the general pattern of the Stone Age, but it has particularities that make it a region apart with its own cultures. Due to its climate and geographical position, between the desert regions of the south and the Mediterranean Sea to the north, it has offered mankind a diversity of landscapes and environments that are quite unique and favorable to the development of human evolution. Finally, this region gives access to Europe through several maritime passages (Gibraltar, Sicily), which were probably used during the Pleistocene, thus reinforcing the interest in studying this northern part of Africa. The recent development of numerous dating methods has made it possible to reinforce and consolidate the chronostratigraphic framework, which for many years had been based solely on radiocarbon dating. These methods have sometimes even contributed to the confirmation of ‘new’ ideas that have dusted off the existing framework of prehistory. This article presents a chronology of the main ancient sites of the Maghreb dated by different methods whose ages compared to the results obtained by other disciplines participate and contribute to a better understanding of the environmental and cultural framework of prehistoric Man.     

利用HPA-1～3,5和15系统多态性估算中外不同人群遗传距离

依据血小板同种抗原5个系统的遗传多态性, 采用聚合酶链反应序列特异性引物技术, 对1 000名中国汉族无关献血者HPA-1~3, 5和15系统进行基因分型, 计算基因频率。使用DISPAN软件及PHYLIP软件计算不同群体间遗传距离并绘制系统树。系统树显示, 亚洲人群先与欧洲人群相聚, 之后再与非洲人群相聚, 非洲人群位于系统发生树的最顶部; 印度人群处于亚洲人群与欧洲人群之间; 南美洲巴西白人与欧洲人群聚在一起; 大洋洲的波利尼西亚人与亚洲人群聚在一起。此研究从一个侧面证明了人类“非洲起源说”, 印证亚洲人群由南亚向东南亚再向东亚迁徙的路线, 并推断出欧洲人群由南欧向北欧、西欧迁徙的线路。HPA能有效估算不同人群间遗传距离, 分析人类迁徙过程, HPA可作为遗传标记应用于人类进化的研究。     

Skipping‐type migration in a small Arctic wader,the Temminck's stint Calidris temminckii

By using morphometric data and geolocator tracking we investigated fuel loads and spatio‐temporal patterns of migration and non‐breeding in Temminck's stints Calidris temminckii. Body masses in stints captured at autumn stopover sites from Scandinavia to northern Africa were generally not much higher than during breeding and did not vary geographically. Thus, we expected migrating stints to make several stopovers and either circumventing the Sahara desert with low fuel loads or fuelling at north African stopover sites before desert crossing. Geolocation revealed that birds (n = 6) departed their Norwegian breeding site in the last part of July and all but one migrated south‐west over continental western Europe. A single bird headed south‐east to the Balkan Peninsula where the geolocator died. As predicted, southbound migration proceeded in a typical skipping manner with 1–4 relatively short stopovers (median 4 d) during 10–27 d of migration before reaching north‐west Africa. Here birds spent 11–20 d before crossing the Sahara. The non‐breeding sites were located at or near the Niger River in Mali and were occupied continuously for more than 215 d with no indications of itinerancy. Spring migration commenced in late April/early May when birds crossed the desert and used stopover sites in the western Mediterranean basin in a similar manner as during autumn. The lowest body masses were recorded in spring at islands in the central Mediterranean basin, indicating that crossing the Sahara and Mediterranean barriers is exhausting to these birds. Hence, the skipping‐type pattern of migration revealed by geolocators is likely to be natural in this species and not an effect of instrumentation.     

Two Mitochondrial Barcodes for one Biological Species: The Case of European Kuhl's Pipistrelles (Chiroptera)

The Kuhl’s pipistrelle (Pipistrellus kuhlii) is a Western Palaearctic species of bat that exhibits several deeply divergent mitochondrial lineages across its range. These lineages could represent cryptic species or merely ancient polymorphism, but no nuclear markers have been studied so far to properly assess the taxonomic status of these lineages. We examined here two lineages occurring in Western Europe, and used both mitochondrial and nuclear markers to measure degrees of genetic isolation between bats carrying them. The sampling focused on an area of strict lineage sympatry in Switzerland but also included bats from further south, in North Africa. All individuals were barcoded for the COI gene to identify their mitochondrial lineages and five highly polymorphic microsatellite loci were used to cluster them according to their nuclear genotypes. Despite this low number of nuclear markers, all North African nuclear genotypes were grouped in a highly distinct subpopulation when compared with European samples sharing the same mitochondrial barcodes. The reverse situation prevailed in Switzerland where bats carrying distinct barcodes had similar nuclear genotypes. There was a weak east/west nuclear structure of populations, but this was independent of mitochondrial lineages as bats carrying either variant were completely admixed. Thus, the divergent mitochondrial barcodes present in Western Europe do not represent cryptic species, but are part of a single biological species. We argue that these distinct barcodes evolved in allopatry and came recently into secondary contact in an area of admixture north of the Alps. Historical records from this area and molecular dating support such a recent bipolar spatial expansion. These results also highlight the need for using appropriate markers before claiming the existence of cryptic species based on highly divergent barcodes.     

Population genomic analysis uncovers African and European admixture in Drosophila melanogaster populations from the south‐eastern United States and Caribbean Islands

Drosophila melanogaster is postulated to have colonized North America in the past several 100 years in two waves. Flies from Europe colonized the east coast United States while flies from Africa inhabited the Caribbean, which if true, make the south‐east US and Caribbean Islands a secondary contact zone for African and European D. melanogaster. This scenario has been proposed based on phenotypes and limited genetic data. In our study, we have sequenced individual whole genomes of flies from populations in the south‐east US and Caribbean Islands and examined these populations in conjunction with population sequences from the west coast US, Africa, and Europe. We find that west coast US populations are closely related to the European population, likely reflecting a rapid westward expansion upon first settlements into North America. We also find genomic evidence of African and European admixture in south‐east US and Caribbean populations, with a clinal pattern of decreasing proportions of African ancestry with higher latitude. Our genomic analysis of D. melanogaster populations from the south‐east US and Caribbean Islands provides more evidence for the Caribbean Islands as the source of previously reported novel African alleles found in other east coast US populations. We also find the border between the south‐east US and the Caribbean island to be the admixture hot zone where distinctly African‐like Caribbean flies become genomically more similar to European‐like south‐east US flies. Our findings have important implications for previous studies examining the generation of east coast US clines via selection.     

横断山区昆虫区系初探

1981—1984年,中国科学院青藏高原科学考察队在我国西南部的横断山区进行了大规模的多学科综合考察,收集昆虫标本17万多号.横断山区特殊的自然地理条件孕育着独特的昆虫区系.种类繁庶、成分复杂,特有种,尤其高山特有种相当丰富,物种分化显著,并具有地域上的狭布性,构成本区昆虫区系特征.作者根据古北、东洋、高山特有三种主要成分的分布,试提出古北、东洋两大区系在本区的分异界线.典型东洋区系成分一般限于海拔2,800—3,000m以下地区,约与亚热带常绿阔叶林分布上线一致.     

Mitochondrial phylogeography,contact zones and taxonomy of grass snakes (Natrix natrix,N. megalocephala)

Grass snakes (Natrix natrix) represent one of the most widely distributed snake species of the Palaearctic region, ranging from the North African Maghreb region and the Iberian Peninsula through most of Europe and western Asia eastward to the region of Lake Baikal in Central Asia. Within N. natrix, up to 14 distinct subspecies are regarded as valid. In addition, some authors recognize big‐headed grass snakes from western Transcaucasia as a distinct species, N. megalocephala. Based on phylogenetic analyses of a 1984‐bp‐long alignment of mtDNA sequences (ND4+tRNAs, cyt b) of 410 grass snakes, a nearly range‐wide phylogeography is presented for both species. Within N. natrix, 16 terminal mitochondrial clades were identified, most of which conflict with morphologically defined subspecies. These 16 clades correspond to three more inclusive clades from (i) the Iberian Peninsula plus North Africa, (ii) East Europe and Asia and (iii) West Europe including Corso‐Sardinia, the Apennine Peninsula and Sicily. Hypotheses regarding glacial refugia and postglacial range expansions are presented. Refugia were most likely located in each of the southern European peninsulas, Corso‐Sardinia, North Africa, Anatolia and the neighbouring Near and Middle East, where the greatest extant genetic diversity occurs. Multiple distinct microrefugia are inferred for continental Italy plus Sicily, the Balkan Peninsula, Anatolia and the Near and Middle East. Holocene range expansions led to the colonization of more northerly regions and the formation of secondary contact zones. Western Europe was invaded from a refuge within southern France, while Central Europe was reached by two distinct range expansions from the Balkan Peninsula. In Central Europe, there are two contact zones of three distinct mitochondrial clades, and one of these contact zones was theretofore completely unknown. Another contact zone is hypothesized for Eastern Europe, which was colonized, like north‐western Asia, from the Caucasus region. Further contact zones were identified for southern Italy, the Balkans and Transcaucasia. In agreement with previous studies using morphological characters and allozymes, there is no evidence for the distinctiveness of N. megalocephala. Therefore, N. megalocephala is synonymized with N. natrix.     

Niche dynamics in the European ranges of two African carnivores reflect their dispersal and demographic histories

According to recent phylogeographical evidence, the common genet (Genetta genetta) and the Egyptian mongoose (Herpestes ichneumon) have dissimilar dispersal histories from Maghreb to south‐western Europe. Through comparative ecological niche modelling based on >1100 occurrences, we assessed whether the niche dynamics (i.e. niche shift versus conservatism) of the two species in their European ranges reflected DNA‐based demographic scenarios. Sensitivity analyses and projections of climatic niche models from the species' native ranges (Africa and Middle East) to Europe yielded support for (1) partial climatic niche shift in the northern European range of the common genet and (2) climatic niche conservatism in the Egyptian mongoose. Our results were consistent with demographic scenarios that predicted multiple introductions and demographic expansion in the common genet and long‐term, stable historical demography in the Egyptian mongoose. Our models further predicted a range expansion of the common genet in north‐western France and Italy, and progression of the Egyptian mongoose into Europe from the Near East. Overall, our study suggested a scenario of different niche dynamics in Europe for these two species of African carnivores, supporting the view that historical factors such as dispersal and demographic history may shape niche dynamics and thus distribution potential in colonized ranges. © 2015 The Linnean Society of London, Biological Journal of the Linnean Society, 2015, 114 , 737–751.     

WATER-BIRDS OVER THE SAHARA

An investigation is made of the extent to which Palaearctic birds belonging to typically water-bird families occur south of the Sahara in areas remote from both the sea and the Nile, namely, Darfur, Northern Nigeria and the Inundation Zone of the Niger, and hence may be presumed to cross the Sahara. Fifty-seven species fall to be considered and for these occurrences within the Sahara are also collated. The results owe a great deal to work done in the last few years, especially ringing. Most of the 57 species dealt with occur regularly in appreciable numbers in one or more of the areas under consideration and some of the species are enormously common. In general there is evidence to show that many birds winter in Africa far to the west of their Palaearctic breeding grounds, from which much diagonal passage of the Sahara is to be inferred. The results are considered in relation to the ecological conditions on the northern and southern edges of the desert and in relation to the meteorological conditions over it. A remarkable circumstance is that few water-birds indeed of any species have been observed in the oases of the Sahara, so that their crossing of the desert is clearly very efficient, although so much of it is by lengthy diagonal and although many birds entering Africa in the middle longitudes meet with no suitable habitat between Europe and the tropics. Except perhaps for storks, which soar, and certainly for herons, which proceed by heavy flapping, the air speed of water-birds is much greater than that of the small passerine migrants, the necessary potentiality of which has been calculated as 50–60 hours of flight without refuelling; but too little is known of the aerodynamics and physiology involved for it to be calculated whether water-birds need to start with the comparable accumulations of fat and no definite information exists except for the Wood Sandpiper, which has been shown to put on up to 32% of fat. By comparison with passerines, more individual water-bird species winter partly north and partly south of the Sahara; the factors affecting each bird's behaviour in this respect are unknown.     

Phylogeny and evolution of the genus Barbus in the Iberian Peninsula as revealed by allozyme electrophoresis

Variation of 14 enzyme systems encoded by 31 presumptive loci in different barbel species was studied using starch gel electrophoresis. Eighteen samples representing 11 Barbus tetraploid taxa were taken, including 10 populations from the Iberian Peninsula, six from other parts of western and southern Europe, one from northern Africa and one diploid species as outgroup from Asia Minor. The genetic analysis reassessed of the taxonomic status of the Iberian barbels into two distinct species groups. The first group included B. bocagei, B. comiza, B. graellsii, B. gulraonis, B. microcephalus , and B. sclateri , that aligned with B. callensis from northern Africa and with B. apoensis from Asia Minor; the other group included B. haasi and B. merldlonahs that was related to the European species, B. barbus, B. plebejus and B. peloponnesius . These groups are probably not monophyletic. It is suggested that the isolation of the Iberian Peninsula from Europe since the Oligocene-Miocene may explain the genetic affinities of the Iberian barbels with those of North African rather than with the European group.     

The ancient Britons: groundwater fauna survived extreme climate change over tens of millions of years across NW Europe

Global climate changes during the Cenozoic (65.5–0 Ma) caused major biological range shifts and extinctions. In northern Europe, for example, a pattern of few endemics and the dominance of wide‐ranging species is thought to have been determined by the Pleistocene (2.59–0.01 Ma) glaciations. This study, in contrast, reveals an ancient subsurface fauna endemic to Britain and Ireland. Using a Bayesian phylogenetic approach, we found that two species of stygobitic invertebrates (genus Niphargus) have not only survived the entire Pleistocene in refugia but have persisted for at least 19.5 million years. Other Niphargus species form distinct cryptic taxa that diverged from their nearest continental relative between 5.6 and 1.0 Ma. The study also reveals an unusual biogeographical pattern in the Niphargus genus. It originated in north‐west Europe approximately 87 Ma and underwent a gradual range expansion. Phylogenetic diversity and species age are highest in north‐west Europe, suggesting resilience to extreme climate change and strongly contrasting the patterns seen in surface fauna. However, species diversity is highest in south‐east Europe, indicating that once the genus spread to these areas (approximately 25 Ma), geomorphological and climatic conditions enabled much higher diversification. Our study highlights that groundwater ecosystems provide an important contribution to biodiversity and offers insight into the interactions between biological and climatic processes.     

First records of Microptila Ris (Trichoptera: Hydroptilidae) from Japan, with description of a new species

Microptila orienthula , sp. n. from Japan is described and illustrated based on adults of both sexes. The new species represents the first finding of Microptila in the Eastern Palaearctic Region, and it appears to be more closely related to Oriental species of Microptila than to the two Western Palaearctic species. The finding of a new species with affinities to the Oriental species as far northeast as Japan is noteworthy but fits well with general zoogeographical affinities of the Japanese fauna to the Oriental Region. The type locality indicates a hygropetric habitat for the larva, in agreement with the known larval habitat of the European type species Microptila minutissima Ris, 1897.