Research on acidification in forest soil driven by atmospheric nitrogen deposition

Soil acidification is defined as the process in which exchangeable cations are leaching and soil H⁺ concentration is raising thereby increases soil acidity. Changes in soil pH value and acid neutralizing capacity are mainly indicators of soil acidification. Soil acidification is considered to be a serious ecological and environmental issue, which not only reduces soil quality, but also decreases biodiversity of forest ecosystem and induces forest decline. With nitrogen (N) deposition rapidly increasing, its contribution to soil acidification becomes a major concern in the world. However, the impact of increased N deposition on soil acidification is not well addressed highlighting the need for further attention to the issue. In this paper, the studies on forest soil acidification induced by N deposition were reviewed. The factors related to soil acidification driven by N deposition were classified and discussed, which included soil acidic buffering capacity, N components in atmospheric N deposition, climate, plant species in forests, and N status in ecosystem. Iron (Fe) buffering phase and the consequent Fe toxicity occurring to the acidified soil caused by high N deposition were concerned. The scarcity of phosphorus (P) element induced by soil acidification was particularly emphasized. The research methods used to study soil acidification driven by N deposition were also evaluated. In the end we stressed the importance of the study on soil acidification especially in tropical and subtropical regions driven by N deposition and its mechanisms. This paper can serve for maintaining sustainable forest and agricultural ecosystems.     

Ammonite and inoceramid radiations after the Santonian-Campanian bioevent in Sakhalin, Far East Russia

Study of several marine Santonian-Campanian successions from Sakhalin Island, Far East Russia, has revealed that evolution of the ammonites and inoceramid bivalves proceeded at different rates after the major faunal turnover at the (locally defined) Santonian-Campanian boundary. Sometimes changes in the inoceramid assemblages were more frequent and rapid than changes in the ammonite assemblages, and sometimes vice versa. Significant levels of inoceramid turnover and radiation events have been identified at the (locally defined) Santonian-Campanian and lower-upper Campanian boundaries. Changes in ammonite and inoceramid diversity, and in the proportions of endemic and cosmopolitan species, were investigated in the context of the local relative sea-level curve and inferred environmental changes. In Far East Russia, the main ammonite and inoceramid radiation after the local Santonian-Campanian faunal turnover occurred in the early Late Campanian Pachydiscus (P.) aff. egertoni ammonite Zone and the coeval Schmidticeramus schmidti inoceramid Zone. This condensed interval of ammonite and inoceramid maximum diversity provides a perfect stratigraphic marker that is recognizable in Sakhalin, North-East Russia and Japan. The succession of Santonian-Campanian assemblages identified in Sakhalin enabled the establishment of seven ammonite and six inoceramid zones, which correlate relatively well with those of North-East Russia and Japan. The problems of placing the Santonian-Campanian boundary in Sakhalin and in the adjacent Japanese island of Hokkaido are reviewed.     

俄罗斯远东及黑龙江省春小麦种质资源的遗传多样性

利用31个SSR引物分析56份俄罗斯远东地区春小麦(Triticum aestivum)及56份黑龙江省2010生(区)试品系的遗传变异和群体结构。结果表明,黑龙江省春小麦和俄罗斯远东春小麦明显分化为两大类群,聚类结果同地理来源的划分基本一致;居群间和个体间都存在显著性差异;群体的遗传分化程度较高,但群体间的基因交流有限,血缘相对比较单一。鉴于部分黑龙江省同一育种单位的品种(系)间的遗传距离非常相近,目前亟需拓宽和创制新的小麦种质资源。实验结果证明种质资源遗传多样性与地理来源和人为选择压力密切相关。     

Interaction between hatchery and wild Pacific salmon in the Far East of Russia: A review

We review studies of interactions between hatchery and wild Pacific salmon in the Russian Far East. This includes the role of hatchery practices that result in premature migration to the sea and increased mortality, and data on feeding and territorial competition between juveniles of hatchery and wild origin. In the course of downstream migration many juvenile hatchery salmon are eliminated by wild salmon predation. During the marine period, Japanese hatchery chum salmon (Oncorhynchus keta) distribution overlaps the distribution of Russian wild salmon. Consequently, replacement of wild populations by hatchery fishes, as a result of abundant juvenile hatchery releases combined with extensive poaching in spawning grounds, is apparent in some Russian rivers. Interactions between the populations occur in all habitats. The importance of conservation of wild salmon populations requires a more detailed study of the consequences of interactions between natural and artificially reared fishes.     

Neogene Deep-sea Smelts (Argentiniformes: Microstomatidae) from the Far East Russia

Deep-sea smelts (Argentiniformes: Microstomatidae, Bathylaginae) from the Miocene of Far East Russia (Sakhalin and Urup islands) are described. The specimens described belong to four taxa, one of which is assigned to a new species of the genus Leuroglossus. Like Recent smoothtongues, the new species has thickened medial rays in the caudal fin. The small number of abdominal vertebrae makes the new species similar to the extant southern smoothtongue L. stilbius, which occurs along the eastern coasts of the Pacific Ocean. The new species differs from extant smoothtongues in the short snout, which is not longer than the orbit. Phylogenetic analysis of morphological features of the new species, using a matrix of characters of living deepsea smelts, shows that it occupies a basal position in the genus Leuroglossus. Three other extinct taxa cannot be reliably classified below the level of the subfamily Bathylaginae or tribe Bathylagini because of insufficient preservation of available specimens. The new records of deep-sea smelts in Far East Russia show that this fish subfamily was widespread and highly morphologically differentiated in the Neogene.     

俄罗斯远东地区勺嘴鹬繁殖地夏季水鸟调查

俄罗斯远东地区是全球鸟类重要的繁殖地之一,特别是楚科奇半岛的阿纳德尔地区是全球极危鸟种勺嘴鹬(Calidris pygmeus)已知的重要繁殖地。为了履行中俄候鸟及其栖息地保护双边协定,掌握俄罗斯远东的阿纳德尔地区夏季水鸟的资源状况,2017年6月25日至7月20日,中俄双方对阿纳德尔南部地区进行了夏季水鸟资源调查。调查区域主要包括阿纳德尔、从阿纳德尔至白令戈夫斯基的海域、白令戈夫斯基、梅内皮尔吉诺周边苔原区域以及附近海域四个部分。共记录35种水鸟,隶属于6目10科,其中14种有繁殖活动。分析中俄环志回收数据表明,在我国长江流域和东部沿海地区越冬的雁鸭类和鸻鹬类水鸟,夏季迁徙到俄罗斯的哈巴罗夫斯克、萨哈林岛、勘察加半岛、雅库特、楚科奇等远东地区繁殖。此外,勺嘴鹬的主要繁殖繁殖地梅内皮尔吉诺周边苔原地区存在着巢址被洪水淹没、卵和雏鸟遭天敌捕食等风险;在勺嘴鹬迁徙路线上的重要迁徙停歇地和越冬地的退化、环境污染和人为活动是导致勺嘴鹬种群数量下降的重要因素。研究结果表明,需要进一步加强中俄双方勺嘴鹬保护的合作与交流,共同保护鸟类的栖息地。     

Butterflies (Lepidoptera,Diurna) in temperate forests of the southern Far East of Russia

The species groups of butterflies in temperate forests and adjoining forest-steppes of the Russian Far East are analyzed. The contribution of species with different distribution types into the total species composition is considered. A classification analysis of the species lists of sixteen local faunas from Amur and Sakhalin Provinces, Khabarovsk and Primorskii Territories, and the Jewish Autonomous Region was performed. A uniform faunal core is shown to be present in the forests (including deciduous ones) of the Russian Far East temperate zone.     

The atmospheric deposition of phosphorus in Lake Victoria (East Africa)

Wet and dry atmospheric fluxes of total phosphorus (TP) and soluble reactive phosphorus (SRP) measured at four sites over a 12-month period were used to estimate lake-wide atmospheric phosphorus (P) deposition to Lake Victoria, East Africa. Atmospheric samples were collected in plastic buckets with top diameter of 25.5 cm by 30 cm deep. The highest P loading rates of 2.7 (TP) and 0.8 (SRP) kg ha^–2 year^–1 were measured at Mwanza compared to less than 1.9 (TP) and 0.65 (SRP) kg ha^–2 year^–1 measured in other three sites. By applying these loading rates to the lake surface, it was estimated that 13.5 ktons (13.5 × 10³ kg) of TP were deposited annually into the lake from the atmosphere. Thirty-two percent of the total was found to be in the SRP form. Dryfall, a component ignored in previous studies exceeded wet deposition by contributing 75% of the total P input. However, materials deposited by dryfall made a lesser contribution to soluble form of phosphorus, as SRP concentrations in the wet samples were 2–3 times higher than SRP concentrations in dry samples. The annual fluxes of phosphorus measured on the south and western shores of Lake Victoria (1.8–2.7 kg ha^–2 year^–1) are near the upper range of similar fluxes measured in the tropics. In comparison with the existing estimates of municipal and runoff P inputs from other studies, it is estimated that atmospheric deposition represent 55% of the total phosphorus input to the Lake Victoria. The four sampling sites were fairly clustered and wet and dry P deposition data were collected from shore/land stations and applied to open lake areas to estimate lake-wide P deposition. In this regard, the estimates determined here should be viewed as a first order approximation of actual P load deposited into the lake.     

Decreased prevalence of Orientia tsutsugamushi in trombiculid mites and wild rodents in the Primorye region, Far East Russia

The isolation of Orientia tsutsugamushi was attempted from 249 rodents and approximately 14,000 trombiculid mites captured in the Primorye region, Far East Russia in 1993 and 1994, where high infection rates were recorded in both rodents and mites in the 1960s. However, no rickettsia was isolated from the samples. Low antibody titers against O. tsutsugamushi were detected in 7.1% of the rodents. These results indicate that the prevalence of O. tsutsugamushi in the Primorye region has decreased considerably in the past 30 years.     

Persistent surface water acidification in an organic soil-dominated upland region subject to high atmospheric deposition: The North York Moors,UK

The North York Moors National Park, in Northeast England, is one of the few upland areas of the United Kingdom located immediately downwind of major sulphur and nitrogen emission sources. Despite this, few studies of air pollution impacts have been undertaken, and there is no formal long-term upland water quality monitoring site. We examined the condition of surface waters in the National Park based on (1) a unique 20 year stream pH record from three locations; and (2) a snapshot survey of 51 surface waters draining moorland and conifer plantations. Interpretation was supported by sulphur isotope analysis of a subset of water samples, and a diatom survey of one of the monitoring streams. Long-term pH data for a stream draining the peat plateau demonstrate extreme, year-round acidification, with recovery only evident in the last few years. Lower-elevation sites are less acidic, but show similar temporal trends, and are characterised by frequent and severe acid episodes. The snapshot survey confirmed that acidification of the moorland area is widespread, to a degree observed in few other areas globally; out of 37 moorland streams sampled, 32 had an acid neutralising capacity (ANC) below −50 μequiv. l⁻¹. Sulphate was found to be (by far) the dominant cause of acidification, and sulphur isotope analysis confirmed that this derives primarily from atmospheric deposition. Nitrate concentrations remain low, indicating that the organic moorland soils continue to retain most incoming nitrogen. It appears that conifer planting has exacerbated acidification, leading to fivefold higher nitrate and threefold higher aluminium concentrations compared to the moorland sites. Available biological data suggest that waters in the region have been impoverished by acidification. We speculate that the slow recovery of surface waters in the North York Moors is due to the release of a legacy of stored sulphur from the peats, released during droughts. We conclude that: (1) acidification is far from being a solved problem in this sensitive near-source upland region, despite reductions in sulphur deposition; (2) plantation forestry has exacerbated the effects of atmospheric pollution, and triggered nitrogen saturation; (3) the lack of any formal long-term monitoring in the North York Moors represents a major gap in the current evidence base for the effects of long-range air pollutants on UK upland ecosystems.     

Virulence genotypes and drug resistance of Helicobacter pylori from Vladivostok, Russia: another feature in the Far East

Helicobacter pylori in Vladivostok, Far Eastern Russia, was investigated during 2004 to 2009. The genotype cagA(+) vacA(+) (s1/m1 or m2) accounted for 74.7%, with cagA(-) vacA(+) (s2/m2) at 11.2%. The CagA EPIYA type was mainly Western ABC, with minor types (ABCCC and novel AAABC) or non-Western/non-East Asia type (AB). Regarding drug resistance, metronidazole resistance was the highest, with a marked decrease in 6 years (from 71.4% to 30.8%); in contrast, levofloxacin and clarithromycin resistance increased. The data indicate that in Vladivostok, H. pylori was mainly the Western (not East Asian) type and dynamic changes in drug resistance occurred during 6 years.     

Faunistic complexes of the Cladocera (Crustacea,Branchiopoda) of Eastern Siberia and the Far East of Russia

Faunistic complexes of 155 species of the Cladocera found in Eastern Siberia and the Far East of Russian Federation are described. The eight complexes are specified: unrevised widely spread species (51), the widespread Eurasian faunistic complex (34 species), the circumpolar complex (4 species), the East Asian and American (Beringian) complex (8 species), the endemic East Asian complex (19 species), the southern thermophilic complex (12 species), the mountainous endemic complex (3 species), and the Baikal endemic complex (8 species). Directions for further studies are suggested. Faunistic investigations of the modern level in the East Palearctic represent an independent task, which should be accomplished by taxonomists in close cooperation with specialists on local faunas.     

1961-2010年中国区域氮沉降时空格局模拟研究

由于人类活动的干扰,近年来,通过沉降和施肥形式进入陆地生态系统的氮素持续增加,众多研究表明,中国已经成为继欧洲和北美之后的第三大氮沉降区。氮与陆地生态系统生物地球化学循环的一系列过程都相互联系,碳循环及其格局也受到氮的影响,因此大气氮沉降的变化受到广泛关注,探明区域大气氮沉降的时空格局对评估氮沉降对陆地生态系统碳循环的影响具有重要意义。构建了一个基于降水、能源消费和施肥数据的氮沉降时空格局模拟方法,通过与观测数据的比较说明该模拟方法能够较好地模拟氮沉降的时空变化,在此基础上,利用该方法模拟了1961-2010年中国区域氮沉降的时空格局。结果表明:(1)1961-2010年中国区域年平均氮沉降速率为0.81 g N m^-2 a^-1,由20世纪60年代的0.31 g N m^-2 a^-1增加到21世纪初的1.71 g N m^-2 a^-1,年增长率为0.04 g N m^-2 a^-1。总氮沉降量由20世纪60年代的2.85 TgN/a增加至15.68 TgN/a。(2)NH_x-N的沉降速率大约是NO_y-N的4倍,是主要的氮沉降形式。1961-2010年我国湿沉降平均速率为0.63 g N m^-2 a^-1,是干沉降速率(0.17 g N m^-2 a^-1)的3.63倍,是氮素进入陆地生态系统的重要途径。(3)在空间上,我国的大气氮沉降速率呈现出由东南向西北梯度递减的格局,华北、华中和东北的农田是氮沉降速率最大的区域,同时也是氮沉降速率增长最快的区域。