Classification and Phytogeography of Larch Forests of Northeast Asia

This study focuses on a phytosociological system of the extensive Larix gmelinii and Larix cajanderi dominated forests and woodlands that span the nemoral, boreal and subarctic zones in northeast Asia in the Russian Far East, Eastern Siberia and northern China, an area that covers more than 5 million km². A total of 299 relevés representing different parts of the larch forest range were used to classify communities in this area into the boreal Rhytidio rugosi-Laricetea sibiricae and Vaccinio-Piceetea and to the nemoral Querco mongolicae-Betuletea davuricae. The hierarchical system of lower syntaxa of larch forests and woodlands of northeast Asia includes 24 associations and nine subassociations. Nineteen associations and two alliances – Rhododendro aurei-Laricion cajanderi and Rhododendro daurici-Laricion gmelinii – are described for the first time. Two associations were classified into Dictamno dasycarpi-Quercion mongolicae of Lespedezo bicoloris-Quercetalia mongolicae representing the nemoral class Querco mongolicae-Betuletea davuricae. All larch communities in the nemoral zone represent different post-fire-event stages. Eleven associations occurring in humid conditions of the boreal zone and in the areas influenced by the Pacific Ocean are classified into Abieti nephrolepidis-Piceion jezoensis, Piceion jezoensis and Pino pumilae-Piceion jezoensis representing boreal forests of humid maritime regions belonging to the order Abieti veitchii-Piceetalia jezoensis. In this area seral larch communities occupy zonal sites, and primeval larch forests may occur only in edaphic conditions restricting the distribution of zonal dominants, Picea jezoensis and the species of Abies. The area of continuous permafrost within the boreal zone having continental and ultracontinental climate conditions is occupied by primeval larch forests united in Ledo palustris-Laricion cajanderi and Rhododendro aurei-Laricion cajanderi of Ledo palustris-Laricetalia cajanderi, and on sites with dry soils with a deeper frozen horizon in Lathyro humilis-Laricion cajanderi of Lathyro humilis-Laricetalia cajanderi.     

Vegetation surveys in the circumboreal coniferous forests: A review

As an introduction to the special issue “Vegetation of Circumboreal Coniferous Forests”, a brief history is provided of the development and present state of floristic vegetation surveys of the boreal and mountain coniferous forests of Europe, northern Asia and North America. The focus is on forests assigned to the phytosociological classVaccinio-Piceetea and closely related vegetation types.     

A comparative phytosociological study of the subalpine coniferous forests in northeastern Asia

Previous classification systems of the subalpine coniferous forests, belonging to the class Vaccinio-Piceetea Br.-Bl. 1939, in northeastern Asia were reviewed based on phytosociological data of Korea and Japan. A new order, the Abieti nephrolepidis-Piceetalia jezoensis was proposed for the subalpine coniferous forests in the continental part of northeastern Asia. Its distribution range and subordinate vegetation units are as follows:Order Abieti nephrolepidis-Piceetalia jezoensis ordo nov.In Korea:Alliance Abieti nephrolepidis-Piceion jezoensis Song 1991Association Taxo-Pinetum pumilae Song et Nakanishi 1985Association Thujo-Abietetum nephrolepidis Song 1991Association Abieti koreanae-Piceetum jezoensis Song 1991Alliance Abietion koreanae Song 1991Association Saso-Abietetum koreanae Song et Nakanishi 1985Association Betulo saitoanae-Abietetum koreanae (Song et Nakanishi 1985) em. Song 1991In northeast China and Maritime Province of Siberia, U.S.S.R.: (one separate alliance level or the same alliance as Abieti nephrolepidis-Piceion jezoensis)Formation Abies nephrolepis form. (Wu 1980)Formation Picea jezoensis-Abies nephrolepis form. (Wu 1980)Generally the Abieti nephrolepidis-Piceetalia jezoensis develops under the dry and cool continental climate and on the monophylogenic Dark Brown Conifer Soil Group derived mostly from granite and granitic gneiss. The subalpine or subarctic coniferous forests in Hokkaido, Sakhalin and Southern Kuriles may also belong to the Abieti nephrolepidis-Piceetalia jezoensis because of their floristic composition and the historical relevance of plant geography. The subordinate vegetation units are as follows:Alliance Piceion jezoensis Suz.-Tok. ex Jinno et Suzuki 1973Association Piceo-Abietetum sachalinensis Ohba 1967Association Piceetum glehnii Suz.-Tok. ex Miyawaki 1988The Abieti veitchii-Piceetalia jezoensis hondoensis Miyawaki et al. 1968 seems to fit only to the subalpine coniferous forests of Honshu and Shikoku of the Japanese Archipelago.     

Epiphytic lichen diversity and its dependence on bark chemistry in the northern Mongolian dark taiga

Epiphytic lichen diversity was studied in a dark taiga forest of Pinus sibirica, Abies sibirica and Picea obovata in the western Khentey Mountains, northern Mongolia. Though most lichen species occurred on all three tree species, lichen diversity was higher on Abies and Picea than on Pinus. On branches, lichen vegetation differed less between tree species than on the trunk. The occurrence of many Parmeliaceae species with a hydrophilic surface and of many species producing the dibenzofuran usnic acid gives evidence of the low deposition of acidic pollutants in the study area. The Mn content of bark, which is known to limit at high values the abundance of epiphytic lichens in coniferous forests of Europe and North America, is apparently not controlling the spatial distribution of epiphytic lichens in the dark taiga of Mongolia. This is attributed to the dry and cold winters in Mongolia, as high Mn is especially leached from the surface of trees under moist conditions at temperatures around the freezing point, when the contact between water droplets and the tree surface is particularly intensive. Such moist and cold weather conditions are frequent in most parts of the northern coniferous forests of Europe and North America, but are rare events in the most continental parts of Asia, i.e. in Mongolia and eastern Siberia.     

Climatic change in the Russian Altai, southern Siberia, based on palynological and geomorphological results, with implications for climatic teleconnections and human history since the middle Holocene

Two pollen diagrams from near the Chuya Basin, Russian Altai, are presented together with results from geomorphological archives. The Kuray Range profile (2330 m a.s.l.) is situated just above the forest line and starts with the weak cooling of the middle Atlantic period (ca. 6500–5900 b.p.) that bisects the Holocene optimum, as in other parts of Siberia. Taiga (boreal coniferous forest) with Picea obovata established afterwards but was displaced at ca. 5300 b.p. by the pronounced cooling of the early Sub-boreal. A gradual recovery of taiga stopped and it disappeared around 3400 b.p. at the end of the middle Sub-boreal. Since then the climatic and vegetational conditions much resemble those of the Sub-atlantic. In the last two millennia, three climatic declines are documented in the second diagram from the Tarkhata Valley (2210 m a.s.l.) from the dry limit of Larix sibirica: a cold and wet one around the 5th century a.d., a cold and dry one around a.d. 1200 and the Little Ice Age which started around a.d. 1600. In addition, several of the climatic periods and especially local human influence can be proved by the geomorphological findings. Most of the climatic changes seem to be connected with socio-ecological changes in Asia and even Europe, with movements of the Huns and Mongols, which show the possible dimensions of global climatic change. Hints of teleconnections between Siberia, the Mediterranean and the Himalayas via the North Atlantic and the Arctic Oscillation are discussed.     

Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia

Pollen and plant macrofossil data from northern Eurasia were used to reconstruct the vegetation of the last glacial maximum (LGM: 18,000 ± 2000 ¹⁴C yr bp ) using an objective quantitative method for interpreting pollen data in terms of the biomes they represent ( Prentice et al., 1996 ). The results confirm previous qualitative vegetation reconstructions at the LGM but provide a more comprehensive analysis of the data. Tundra dominated a large area of northern Eurasia (north of 57°N) to the west, south and east of the Scandinavian ice sheet at the LGM. Steppe‐like vegetation was reconstructed in the latitudinal band from western Ukraine, where temperate deciduous forests grow today, to western Siberia, where taiga and cold deciduous forests grow today. The reconstruction shows that steppe graded into tundra in Siberia, which is not the case today. Taiga grew on the northern coast of the Sea of Azov, about 1500 km south of its present limit in European Russia. In contrast, taiga was reconstructed only slightly south of its southern limit today in south‐western Siberia. Broadleaved trees were confined to small refuges, e.g. on the eastern coast of the Black Sea, where cool mixed forest was reconstructed from the LGM data. Cool conifer forests in western Georgia were reconstructed as growing more than 1000 m lower than they grow today. The few scattered sites with LGM data from the Tien‐Shan Mountains and from northern Mongolia yielded biome reconstructions of steppe and taiga, which are the biomes growing there today.     

Three new species ofMarasmius sectionSicci from eastern Honshu, Japan

Three new species belonging toMarasmius sectionSicci (Agaricales) are described and illustrated from eastern Honshu, Japan:Marasmius nocturnus sp. nov., forming a dark brown pileus and marginate lamellae, was found on leaf litter inPasania—Quercus forests;Marasmius occultatus sp. nov., producing brownish orange or light brown basidiomata and long, cylindrical-fusoid basidiospores, was found on dead fallen twigs ofAphananthe aspera andQuercus myrsinaefolia;Marasmius opulentus sp. nov., having a reddish orange pileus and a pubescent stipe, was found on leaf litter in laurel-leaved forest.     

A latitudinal gradient in tree growth response to climate warming in the Siberian taiga

We investigated the climate response of three Siberian taiga species, Larix cajanderi, Picea obovata, and Pinus sylvestris, across a latitudinal gradient in central Siberia. We hypothesized that warming is more frequently associated with increased growth for evergreen conifers (P. obovata and P. sylvestris) than for L. cajanderi, and for northern than for southern sites; we also hypothesized that increased growth is associated with a positive trend in normalized difference vegetation index (NDVI). In mixed stands, growth of L. cajanderi and P. obovata increased over time, but the larger growth increases in P. obovata may presage a shift in competitive balance between these species. Climate response varied among and within populations of all species, and positive responses to temperature prevailed at northern sites, where trees grew faster in years with warm early summers. Negative responses to warming declined along the south to north latitudinal gradient. We observed considerable variability in climate response within populations which even exceeded that among species or sites. Tree response to climate was correlated with NDVI trends, indicating that patterns of tree‐growth response to climate were indicative of a coherent landscape‐scale response to warming. Our findings suggest that increased productivity with warming is likely only in the northern reaches of the Siberian taiga. An increased prevalence of evergreen conifers in areas currently dominated by deciduous Larix species also seems likely.     

A review of gamasid mites (Parasitiformes,Mesostigmata) dwelling in the taiga of the Pechoro-Ilychskii Nature Reserve (northern Cis-Ural Region) with analysis of their assemblages in spruce forests

In the plain taiga of the Pechoro-Ilychskii Nature Reserve, 91 species of gamasid mites have been revealed. Cheiroseius (7 species), Veigaia (6), Arctoseius (5), Dendrolaelaps (5), and Dinychus (4) are the most diverse genera. European (29%), Palaearctic (27%), and Holarctic species (30%) are represented in the fauna by somewhat equal fractions, whereas cosmopolitan and semicosmopolitan species constitute about 14%. Comparison of gamasid assemblages populating certain habitats allowed revealing two distinct groupings, namely, forest and floodplain ones. Forest assemblages are characterized by high population density (220–760 ind./dm²) and by predominance of Parazercon radiatus, Zercon forsslundi, Veigaia nemorensis, Gamasellus montanus, and Trachytes spp. Floodplain assemblages are less abundant (80–130 ind./dm²) and comprise mainly meadow and hydrophilic species (A. cetratus, Cheiroseius spp. Gaeolaelaps spp., and Gamasellodes bicolor). Low diversity of the family Parasitidae (4 species) and structural peculiarities of assemblages dwelling in coniferous forests (namely, the absence of Pergamasinae and significant fractions of Veigaia, Gamesellus, Trachytes, and also of representatives of the family Zerconidae) demonstrate similarities between the mesostigmatan population of this northern European region and that of the Siberian taiga. Solitary records of such Arctic species as Arctoseius ornatus and Zerconopsis labradorensis, and of the hypoarcto-montane species Iphidinychus gaieri within the taiga belt, seem to reflect the instability of range margin. Taking into account the literary data, we recognize a complex of boreal and borealmountain species (Trachytes edleri, Dinychus septentrionalis. D. crassus, Caurozercon duplex, Neozercon smirnovi, Zercon forsslundi, and Z. zelawaiensis) in the Palaearctic fauna. Their habitats, however, are not restricted only to dark coniferous forest along. The structure of gamasid mite assemblages in mesophytic spruce forests of the Palaearctic varies strongly. By contrast to vascular plants, where many species accompany the dark coniferous taiga everywhere, there is not a single mesostigmatic mite species common to all the spruce forests analyzed, ranging from Romania in the west to Sakhalin Island in the east. On the whole, changes in gamasid mite assemblages across the spruce forest belt seem to follow a succession of meridional changes in gamasid faunas regardless of an edificatory spruce species.     

Epigeic lichen communities of taiga and tundra regions

The major physiognomic and ecological categories of the lichen-rich, epigeic communities in the boreal (taiga) and arctic (tundra) zones are defined and their syntaxonomy and ecology in Europe, Asia and North America is reviewed. In the boreal and hemiarctic areas open, dry, acidophytic lichen woodlands are widespread, especially on sandy habitats. Their epigeic lichen synusiae are usually dominated by four fruticoseCladina species, being extremely homogeneous in species composition and structure throughout the boreal zone, while the dominant trees and the other vascular plant flora of the woodlands are geographically more variable. No phytosociological classification system exists that would cover most of these communities over the circumpolar regions. Very similar communities, though much more poorly known, are found on thin soils over Precambrian rock outcrops. Other sites to produce epigeic lichen communities include open sand dunes, treeless heathlands, drier bogs and many seral stages, like those on road banks. Boreal lichen-rich communities on eutrophic soils may be developed in semiarid regions, in particular. In the Arctic, lichens are common in most communities, and the driest ones are regularly lichen-dominated, whether acidophytic or eutrophytic, chionophytic or achionophytic. Detailed syntaxonomic systems for their classification have been developed, especially in Greenland and Scandinavian mountains (in oroarctic zones in the latter regions). The richest fruticose lichen areas are in continental, hemiarctic timberline regions in northern Siberia and Canada. The southern and middle arctic subzones are also characterized by many macrolichens, such asCetraria cucullata, C. nivalis, Alectoria ochroleuca, andThamnolia vermicularis, but everywhere also small, crustose lichens are common on soil, such asRinodina turfacea andLopadium pezizoideum, which are often overlooked in vegetation analyses. The presence of microlichens and the formation of mosaic micropatterns of soil lichen communities is particularly typical of the northern arctic subzone. The conservation problems of the boreal and arctic lichen communities include overgrazing by reindeer or caribou, which has caused delichenization in some regions, extensive forest and tundra fires, use of heavy transport vehicles in forestry and tundra operations, and, locally, heavy industrial air pollution.     

Contribution à l’étude des groupements Végétaux du vercors méridional: Les groupements fontinaux et des bas-marais de l’étage subalpin

Conclusions L’important mémoire deJ. Braun-Blanquet (1971) sur les Associations des basmarais suisses ainsi que d’autres travaux (E. Oberdorfer, 1970;H. Ellenberg, 1963), permettent d’affirmer que les groupements de l’Eriophorion latifoliae (Br.-Bl. et Tx. 43) et des Caricetalia Davallianae (Br.-Bl. 49) sont représentés dans l’ensemble de la cha?ne alpine sur substrat riche en calcium et, en général, à partir de l’étage montagnard supérieur. Dans les Alpes et Préalpes fran?aises, plusieurs auteurs ont décrit des groupements du Caricion Davallianae (M. Guinochet en Tinée et en Haute-Savoie, 1938 et 1939;G. Aubert, L. Borel, A. Lavagne etP. Moutte dans l’étage subalpin de la feuille d’Embrun-Est, 1965). Dans le Vercors, seuleCh. Faure (1968) signale simplement l’existence du Caricion Davallianae (Klika 34) dans la partie septentrionale du massif (feuille de Vif). Enfin, dans les Préalpes du sud où les étages montagnard et, a fortiori, subalpin sont peu ou pas représentés.A. Archiloque, L. Borel etA. Lavagne (1970) constatent l’absence du Cratoneurion commutati (W. Koch. 28) et du Caricion Davallianae (Klika 34) sur la feuille de Javie (préalpes de Digne). Bien que la nature de la roche-mère soit déterminante pour l’existence des groupements de source et bas-marais alcalins, c’est en définitive la relative permanence de l’alimentation en eau courante et fra?che qui représente le facteur décisif pour ces associations. Dans la région étudiée, celles-ci sont à leur limite méridionale, ce qui confirme—s'il en était besoin—l’originalité et la richesse de ce secteur des Préalpes. Laboratoire de Taxonomie Expérimentale et de Phytosociologie de la Faculté des Sciences de BESAN?ON (25)—FRANCE.     

Zur taxonomischen Stellung und Nomenklatur vonMicropus longifolius (Compositae-Inuleae)

Zusammenfassung Die unter den NamenMicropus longifolius Boiss. etReut. bzw.Cymbolaena longifolia (Boiss. etReut.)Smoljan. gut bekannte Art wurde zuerst alsStylocline griffithii A.Gray beschrieben. Ihre taxonomische Stellung in bezug auf die GattungenMicropus undStylocline wird diskutiert. Es erscheint am richtigsten, die Art in eine eigene monotypische Gattung zu stellen, ihr korrekter Name ist dannCymbolaena griffithii (A.Gray)Wagenitz, comb. nov.

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Summary The species usually known asMicropus longifolius Boiss. etReut. orCymbolaena longifolia (Boiss. etReut.)Smoljan. was described for the first time in 1873 asStylocline griffithii A.Gray. The taxonomic position in relation to the generaMicropus andStylocline is discussed. It seems most appropriate to regard this species as belonging to a monotypic genus. In this case its correct name isCymbolaena griffithii (A.Gray)Wagenitz, comb. nov.

     

The callovian (Middle Jurassic) crinoids from northern Lithuania

Callovian strata in northern Lithuania (Papilė area) have yielded some crinoid taxa[Chariocrinus andreae (Desor),Balanocrinus berchteni Hess —Pugin,B. subteres (Münster inGoldfuss) andIsocrinus nicoleti (Desor)], which have not been described from this area. The only form known previously wasBalanocrinus pentagonalis (Goldfuss).Palaeocomaster jaegeri n. sp. is the first free-living crinoid recorded from the Callovian of eastern Europe. It is characterized by possessing a very low, strongly flattened and narrow radial cavity. A very similar crinoid assemblage is known from the Callovian glacially-derived clays exposed in the Łuków region (eastern Poland), which were originally located near the Baltic Sea during the Middle Jurassic. It is considered that the allochthonous Callovian deposits from Poland are facies equivalents of the deposits known from Lithuania. The sole significant exception is the domination of free-moving comatulids (Comatulida) in the sediments known from the Papilė region, which may suggest that the Lithuanian sea basin was a little shallower than that located farther west in the Baltic area.      

Diversity of forest vegetation across a strong gradient of climatic continentality: Western Sayan Mountains, southern Siberia

Southern Siberian mountain ranges encompass strong climatic contrasts from the relatively oceanic northern foothills to strongly continental intermountain basins in the south. Landscape-scale climatic differences create vegetation patterns, which are analogous to the broad-scale vegetation zonation over large areas of northern Eurasia. In their southern, continental areas, these mountains harbour forest types which potentially resemble the full-glacial forests recently reconstructed for Central Europe. To identify forest vegetation–environment relationships in the southern Siberian mountain ranges, forest vegetation of the Western Sayan Mountains was sampled on a 280 km transect running from the northern foothills with oceanic climatic features to the continental Central Tuvinian Basin in the south. Based on the species composition, vegetation was classified into hemiboreal forests, occurring at drier and summer-warm sites with high-pH soil, and taiga, occurring at wetter, summer-cool sites with acidic soil. Hemiboreal forests included Betula pendula-Pinus sylvestris mesic forest, Larix sibirica dry forest and Pinus sylvestris dry forest. Taiga included Abies sibirica-Betula pendula wet forest, Abies sibirica-Pinus sibirica mesic forest and Pinus sibirica-Picea obovata continental forest. Hemiboreal forests were richer in vascular plant species, while taiga was richer in ground-dwelling cryptogams. Vegetation–environment relationships were analysed by indirect and direct ordination. Winter and summer temperatures and precipitation exerted a dominant influence on species composition. Soil pH was also an important correlate of species composition, but this factor itself was probably controlled by precipitation. At a more local scale, the main source of variation in species composition was topography, producing landscape patterns of contrasting plant communities on slopes of different aspects and valley bottoms. The response of tree species to major environmental factors was expressed with Huisman–Olff–Fresco models. Larix sibirica appeared to be most resistant to drought and winter frosts, Pinus sibirica was adapted to low temperatures both in winter and summer, and Picea obovata had an intermediate response to climate. Betula pendula, Pinus sylvestris and Populus tremula were associated with the warmest sites with intermediate precipitation, while Abies sibirica was the most moisture-demanding species, sensitive to deep winter frosts.     

Succession after stand replacing disturbances by fire,wind throw,and insects in the dark Taiga of Central Siberia

The dark taiga of Siberia is a boreal vegetation dominated by Picea obovata, Abies sibirica, and Pinus sibirica during the late succession. This paper investigates the population and age structure of 18 stands representing different stages after fire, wind throw, and insect damage. To our knowledge, this is the first time that the forest dynamics of the Siberian dark taiga is described quantitatively in terms of succession, and age after disturbance, stand density, and basal area. The basis for the curve–linear age/diameter relation of trees is being analyzed. (1) After a stand-replacing fire Betula dominates (4,000 trees) for about 70 years. Although tree density of Betula decreases rapidly, basal area (BA) reached >30 m²/ha after 40 years. (2) After fire, Abies, Picea, and Pinus establish at the same time as Betula, but grow slower, continue to gain height and eventually replace Betula. Abies has the highest seedling number (about 1,000 trees/ha) and the highest mortality. Picea establishes with 100–400 trees/ha, it has less mortality, but reached the highest age (>350 years, DBH 51 cm). Picea is the most important indicator for successional age after disturbance. Pinus sibirica is an accompanying species. The widely distributed “mixed boreal forest” is a stage about 120 years after fire reaching a BA of >40 m²/ha. (3) Wind throw and insect damage occur in old conifer stands. Betula does not establish. Abies initially dominates (2,000–6,000 trees/ha), but Picea becomes dominant after 150–200 years since Abies is shorter lived. (4) Without disturbance the forest develops into a pure coniferous canopy (BA 40–50 m²/ha) with a self-regenerating density of 1,000 coniferous canopy trees/ha. There is no collapse of old-growth stands. The dark taiga may serve as an example in which a limited set to tree species may gain dominance under certain disturbance conditions without ever getting monotypic.     

Taxonomic notes on<Emphasis Type="Italic">Linaria</Emphasis> mill. (<Emphasis Type="Italic">Scrophulariaceae</Emphasis>) for Flora Iberica

Taxonomic considerations and nomenclatural adjustments as a part of a revision ofLinaria Mill. undertaken within the “Flora iberica” project are presented. Data on morphology, seed coat surface, chorology, ecology, synonymy and variability of 11 accepted taxa are reported. The following new combinations are proposed:Linaria aeruginea subsp. cardonica (Font Quer)L. Sáez etM. Sainz,Linaria depauperata subsp.ilergabona (M.B. Crespo etV.J. Arán)L. Sáez, andLinaria saturejoides subsp.angustealata (Willmott)L. Sáez etM.B. Crespo.     

Bemerkungen zu einigenStipagrostis-Arten (Gramineae) aus Afrika und Arabien

Summary A new species from Egypt (Sinai) and Arabia is described asStipagrostis multinerva H.Scholz. Stipagrostis arabiaefelicis Bor 1967 is a synonym ofSt. drarii (V.Täckholm)de Winter 1963 (Aristida drarii V.Täckholm 1941). The taxonomic status ofStipagrostis foexiana (Maire etWilczek)de Winter (Aristida obtusa subsp.pubescens Andreánszky) in North and South Africa is discussed. Furthermore some new data on taxonomy and distribution of the following species are recorded:Stipagrostis acutiflora subsp.algeriensis (Henrard) comb, nov. et stat. nov.,St. ciliata (Desf.)de Winter,St. lanata (Forsk.)de Winter,St. libyca (H.Scholz) comb, nov.,St. papposa (Trin. etRupr.)de Winter,St. raddiana (Savi)de Winter,St. shawii (H.Soholz) comb, nov., andSt. sokotrana (Vierhapper)de Winter.      

拟爪绵蚜新属及三新种记述 (同翅目:蚜总科:瘿绵蚜科)

该文记述了瘿绵蚜科一新属拟爪绵蚜属ＳｉｃｉｕｎｇｕｉｓＺｈａｎｇｅｔＱｉａｏｇｅｎ．ｎｏｖ．和这个属的二个新种,即十绵蚜Ｓ．ｄｅｃｉｍａＺｈａｎｇｅｔＱｉａｏ,ｓｐ．ｎｏｖ．,九绵蚜Ｓ．ｎｏｖｅｎａＺｈａｎｇｅｔＨｕ,ｓｐ．ｎｏｖ．,另外还记述了爪绵蚜属ＡｐｈｉｄｏｕｎｇｕｉｓＴａｋａｈａｓｈｉ,１９６３一个新种,苹果根爪绵蚜Ａ．ｐｏｍｉｒａｄｉｃｏｌａＺｈａｎｇｅｔＨｕ,ｓｐ．ｎｏｖ．,模式标本存放在中国科学院动物研究所．拟爪绵蚜新属ＳｉｃｉｕｎｇｕｉｓＺｈａｎｇｅｔＱｉａｏｇｅｎ．ｎｏｖ．模式种：十绵蚜ＳｉｃｉｕｎｇｕｉｓｄｅｃｉｍａＺｈａｎｇｅｔＱｉａｏ,ｓｐ．ｎｏｖ．本新属与爪绵蚜属ＡｐｈｉｄｏｕｎｇｕｉｓＴａｋａｈａｓｈｉ,１９６３和绵蚜属ＥｒｉｏｓｏｍａＬｅａｃｈ,１８１８有较近的亲缘关系,不同在于：有翅孤雌蚜腹管位于腹部背片Ⅵ,隆起,周围有毛环绕（前者：位于背片Ⅵ,不隆起,无毛环绕;后者：位于背片Ⅴ,隆起,有毛环绕）;触角稍长,至少为体长０．３５,具有线形次生感觉圈;后者：稍长,至少为体长０．４０,具有环形次生感觉圈）。十绵蚜ＳｉｃｉｕｎｇｕｉｓｄｅｃｉｍａＺｈａｎｇｅｔＱｉａｏ,ｓｐ．ｎｏｖ     

Intorno ad un lievito osmofilo sistematicamente prossimo a Sacch. Elegans Lodder et Kreger-van Rij

Riassunto Viene descritto un lievito osmofilo, isolato da mosto d'uva naturale, tassonomicamente vicino aSacch. elegans Lodder etKreger-van Rij.Questo lievito viene riguardato comeSacch. elegans var.intermedia nov. var. (pro tempore).

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Summary Here is described an osmophilic yeast isolated from natural grape must which is taxonomically similar toSacch. elegans Lodder etKreger-van Rij.This yeast is regarded asSacch. elegans var.intermedia nov. var. (pro tempore).

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Resumo Nêste trabalho descrive-se uma levedura osmofila isolada de môsto de uva natural taxonomicamente proxima aSacch. elegans Lodder etKreger-van Rij.Esta levedura è considerada então, comoSacch. elegans, var.intermedia nov. var. (pro tempore).

     

Phytosociological study of thePicea jezoensis forests of the far east

Forest communities dominated byPicea jezoensis (Yezo spruce) are described from across their entire distributional range in eastern Asia, including the territories of the Russian Far East and Japan. A total of 476 relevés are used representing the following dominant types of spruce forests: pureP. jezoensis, mixedP. jezoensis andAbies sachalinensis, mixedP. jezoensis andAbies nephrolepis, and purePicea glehnii communities. The vegetation is classified into 11 associations, 2 community types, 6 subassociations, 25 variants and 8 subvariants. Nine associations, including theAsaro heterotropoidis-Abietetum sachalinensis, Weigelo middendorffianae-Piceetum jezoensis, Lysichito-Piceetum glehnii, Swido albae-Piceetum obovatae, Oplopanaco elati-Piceetum jezoensis, Philadelpho tenuifolii-Piceetum jezoensis, Vaccinio-Piceetum jezoensis, Rhododendro aurei-Piceetum jezoensis, andMoneseto uniflorae-Piceetum jezoensis, are described for the first time. The ecology and structure of all communities are described and their syntaxonomy discussed. The communities are placed in three alliances,Piceion jezoensis, Abieti nephrolepidis-Piceion jezoensis andPino pumilae-Piceion jezoensis, all. nov. All of the communities described are considered to belong to the orderAbieti-Piceetalia of the classVaccinio-Piceetea.