Living benthic foraminifera of the Okhotsk Sea: Faunal composition, standing stocks and microhabitats

Live (Rose Bengal stained) benthic foraminifera were investigated in surface sediment samples from the Okhotsk Sea to reveal the relationship between faunal characteristics and environmental parameters. Live benthic foraminifera were quantified in the size fraction > 125 µm in the upper 8 cm of replicate sediment cores, recovered with a multicorer at five stations along the Sakhalin margin, and at three stations on the southwestern Kamchatka slope. The stations are from water depths between 625 to 1752 m, located close or within the present Okhotsk Sea oxygen minimum zone, with oxygen levels between 0.3 and 1.5 ml l^- 1. At the high-productivity and ice-free Kamchatka stations, live benthic foraminifera are characterized by maximal standing stocks (about 1700-3700 individuals per 50 cm²), strong dominance of calcareous species (up to 87-91% of total live faunas), and maximal habitat depths (down to 5.2-6.7 cm depth). Vertical distributions of total faunal abundances exhibit a clear subsurface maximum in sediments. At the Sakhalin stations, which are seasonally ice-covered and less productive, live benthic foraminifera show lower standing stocks (about 200-1100 individuals per 50 cm²), lower abundance of calcareous species (10-64% of total live faunas), and shallower habitat depths (down to 2.5-5.4 cm depth). Faunal vertical distributions are characterized by maximum in the uppermost surface sediments. It is suggested that 1) lower and strongly seasonal organic matter flux, caused by the seasonal sea ice cover and seasonal upwelling, 2) lower bottom water oxygenation (0.3-1.1 ml l^- 1), and 3) more pronounced influence of carbonate undersaturated bottom water along the Sakhalin margin are the main factors responsible for the observed faunal differences. According to species downcore distributions and average living depths, common calcareous species were identified as preferentially shallow, intermediate and deep infaunal. Foraminiferal microhabitat occupation correlates with the organic matter flux and the depth of the oxygenated layer in sediments.     

山西庞泉沟自然保护区步甲物种组成及多样性格局

利用巴氏罐诱法,对山西庞泉沟国家自然保护区的不同功能区——核心区（绿色长廊）、缓冲区（八道沟）、远离农田实验区（神尾沟）及靠近农田实验区（八水沟）——林地地表甲虫步甲物种多样性进行了调查和比较,目的在于探明该保护区有代表性林地步甲物种的组成及受不同程度人为干扰下的多样性格局。结果表明：（1）本研究共捕获步甲物种42种,38种是该保护区的新记录种类,其中粗皱步甲Carabus crassesculptus和沟步甲C. canaliculatus 为优势种,与尖角通缘步甲Pterostichus eschscholtzii,强足通缘步甲P. fortipes,罕丽步甲C. manifestus和长叶步甲C. vladimirskyi一起构成研究地的常见种。（2）不同功能区物种组成和数量分布各不相同,多样性各项指标均是靠近农田的实验区最高,核心区最低。（3）各功能区具有特有的指示性种类,其中黄条春步甲Notiophilus reitteri为核心区指示种; 凹唇春步甲N. impressifrons 为缓冲区指示种; 粒步甲C．granulatus,刻翅步甲C．sculptipennis 和中华通缘步甲P．chinensis为实验区指示种。（4）群落相似性分析表明缓冲区与核心区及远离农田实验区之间具有较高的相似性,靠近农田实验区与其他3个地点相似性较低。结果提示适度干扰可提高物种丰富度,但降低人为干扰（如旅游和交通压力）有利于步甲多样性的保护。     

Active zone proteins are dynamically associated with synaptic ribbons in rat pinealocytes

Synaptic ribbons (SRs) are prominent organelles that are abundant in the ribbon synapses of sensory neurons where they represent a specialization of the cytomatrix at the active zone (CAZ). SRs occur not only in neurons, but also in neuroendocrine pinealocytes where their function is still obscure. In this study, we report that pinealocyte SRs are associated with CAZ proteins such as Bassoon, Piccolo, CtBP1, Munc13-1, and the motorprotein KIF3A and, therefore, consist of a protein complex that resembles the ribbon complex of retinal and other sensory ribbon synapses. The pinealocyte ribbon complex is biochemically dynamic. Its protein composition changes in favor of Bassoon, Piccolo, and Munc13-1 at night and in favor of KIF3A during the day, whereas CtBP1 is equally present during the night and day. The diurnal dynamics of the ribbon complex persist under constant darkness and decrease after stimulus deprivation of the pineal gland by constant light. Our findings indicate that neuroendocrine pinealocytes possess a protein complex that resembles the CAZ of ribbon synapses in sensory organs and whose dynamics are under circadian regulation.     

Skull variation in the Siberian roe deer <Emphasis Type="Italic">Capreolus pygargus</Emphasis> from the Far East: a revision of the distribution of the subspecies

Extremely widespread in the Palaearctic, roe deer are heterogeneous in many ways including their morphology. At present, two roe deer species and four basic subspecies are acknowledged. The taxonomic system of the Siberian roe deer is poorly developed compared to that of the European roe deer. One of the principal points of roe deer systematics is the determination of the boundaries of the ranges of the roe deer subspecies requiring a thorough study of the species’ diversity. By using craniometry, one of the most adequate systematics techniques, we have analyzed geographical distribution of the Suberian roe deer in the Russian Far East and adjacent areas. All studied specimens were separated into three groups, the distributions of craniometric parameters of two of which did not overlap. One of the groups corresponds to Capreolus pygargus pygargus Pallas, 1771, while the other two do not correspond to any of the Siberian roe deer subspecies presently acknowledged. We have shown that the C. pygargus pygargus range extends to the east to the Northern Primorye, i.e., it is 2,000 to 3,000 km wider than previously believed. The subspecies status of Capreolus pygargus tianschanicus Satunin, 1906 was not confirmed. The Southern Primorye and left bank of the Amur River are thus a part of the range of Capreolus pygargus melanotis Miller, 1911, penetrating here from the Northeastern China.     

Distribution of <Emphasis Type="Italic">Boroecia borealis</Emphasis> (Ostracoda: Halocyprididae) in the Arctic Ocean and adjacent waters of the Atlantic

The geographical and vertical distribution of Boroecia borealis was studied based on literature data and materials collected by Soviet and Russian expeditions in the Arctic Ocean and adjacent waters of the Atlantic during the period from 1929 to 1993. In the region of study, this species occurs at a temperature from 0.5 to 17.7°C. In the Arctic basin, B. borealis is predominantly found in the warm deep Atlantic layer. The central Arctic region is not a zone of exclusion of this species, but is a part of the species’ range, where its apparently dependent populations occur. In the northern Atlantic, B. borealis can reach into the low latitudes as far as 30°N.     

Analysis of the interactions between the peptides from secreted human CKLF1 and heparin using capillary zone electrophoresis.

The Chemokine-like factor 1 (CKLF1) is a novel human cytokine and exhibits chemotactic activities on leukocytes. Two peptides named CKLF1-C27 and CKLF1-C19, were obtained from secreted CKLF1. In this study, a selective high-performance analytical method based on capillary zone electrophoresis (CZE) to investigate interactions between heparin and CKLF1-C27/CKLF1-C19 was developed. Samples containing CKLF1-C27/CKLF1-C19 and heparin at various ratios were incubated at room temperature and then separated by CZE with Tris-acetate buffer at pH 7.2. Both qualitative and quantitative characterizations of the binding were determined. The binding constants of the interactions between CKLF1-C27/CKLF1-C19 and heparin were calculated as (3.38 +/- 0.49) x 10(5) M(-1) and (1.10 +/- 0.02) x 10(5) M(-1) by Scatchard analysis. To study structural requirements, CKLF1-C19pm and CKLF1-C19km have been synthesized, and their interactions with heparin have been studied by CZE. We found that the Pro or Lys to Ala substitution within the residues of CKLF1-C19 (CKLF1-C19pm or CKLF1-C19km) strongly decreased or abolished its interaction with heparin, suggesting that the residues of Pro affect the affinity of CKLF1-C19 for heparin, and the residues of Lys of CKLF1-C19 play the important role for the interaction of CKLF1-C19 and heparin, respectively. The methodology presented should be generally applicable to study peptides and heparin interactions quantitatively and qualitatively. Copyright (c) 2008 European Peptide Society and John Wiley & Sons, Ltd.     

Osmotic concentration in three races of honey bee,Apis mellifera L. under environmental conditions of arid zone

Hemolymph osmolarity has great effect on honey bee health, especially in arid and semi-arid zones. It regulates water and nutrients in stressed tissues. Osmotic concentration in three races (Apis mellifera ligustica, A. m. carnica and A. m. jemenitica) of Apis mellifera was tested in central Saudi Arabia during spring and summer seasons in 2015. Newly emerged bee workers were first marked and later their hemolymph was extracted after intervals of 1, 5, 10, 15, 20 and 25 days. A significant positive correlation between age and osmolarity was found in all three races during spring and summer seasons. The lowest combined osmotic concentration for all three races was found after 1 day interval, while the highest osmotic concentration was recorded after 25 days. Among all races, A. m. ligustica showed significantly high osmotic concentration after 25 days in spring and summer seasons as compared to the other two races. Only A. m. jemenitica showed similar osmotic concentration after 10 and 15 days in both spring and summer seasons compared to other two races. Mean osmotic concentration of all three races was significantly different after 20 and 25 days in spring and summer seasons. Overall mean recorded during summer was significantly higher than the mean of spring season. Combined osmotic concentration in young drones of all races was significantly lower than that of old drones during spring and summer seasons.     

Rediscovery of the “extinct” blind ground beetle (Coleoptera: Carabidae: Trechinae)

The blind ground beetle Ishikawatrechus intermedius (Coleoptera: Carabidae: Trechinae), called Kadota‐mekurachibigomimushi in Japanese, was first found in 1952 in the cave Ôchi‐dô, Kôchi Prefecture, Japan. However, this cave and a large part of the surrounding hill were destroyed by limestone mining in the 1970s. Because most species of blind ground beetles are restricted to specific caves or cave systems, I. intermedius has been considered endemic to very narrow areas of the cave Ôchi‐dô and the upper hypogean zone around the cave. Therefore, I. intermedius was considered to have become extinct. In this study, during 2011–2015, we collected ten individuals of a blind ground beetle, which appeared to be I. intermedius, from the upper hypogean zone, approximately 0.3–1.0 m below ground, in the southern part of the type locality. A comparison with type specimens indicated that the individuals were indeed I. intermedius. Therefore, we conclude that I. intermedius survives in the upper hypogean zone near the type locality. The results of this study will be useful for quickly establishing conservation measures for threatened or vulnerable species of Trechinae beetles.     

Effects of increased flooding on riparian vegetation: Field experiments simulating climate change along five European lowland streams

In many parts of the world, the magnitude and frequency of cold‐season precipitation are expected to increase in the near future. This will result in an increased magnitude and duration of winter and spring flooding by rain‐fed streams and rivers. Such climate‐driven increases in flooding are likely to affect riparian plant communities, but future vegetation changes are hard to predict due to current lack of data. To fill this knowledge gap, we experimentally modified the hydrology of five streams across three countries in north‐western Europe during late winter/early spring over a period of 3 years. We assessed the responses in riparian plant species richness, biomass, plant‐available nitrogen and phosphorus and seed deposition to increased flooding depth (+18 cm on average at the lowest positions along the riparian gradient) and prolonged flooding duration (6 weeks on average). After 3 years of increased flooding, there was an overall decline in riparian species richness, while riparian plant biomass increased. Extractable soil nitrogen and phosphorus also increased and are likely to have contributed to the increased biomass. Increased flooding resulted in the arrival of more seeds of additional species to the riparian zone, thereby potentially facilitating the shifts in riparian plant species composition we observed. The results of our concerted experimental effort demonstrate that changes in stream riparian plant communities can occur rapidly following increased winter flooding, leading to strong reductions in plant species diversity.     

Unexpected release of phosphate and organic carbon to streams linked to declining nitrogen depositions

Reductions in emissions have successfully led to a regional decline in atmospheric nitrogen depositions over the past 20 years. By analyzing long‐term data from 110 mountainous streams draining into German drinking water reservoirs, nitrate concentrations indeed declined in the majority of catchments. Furthermore, our meta‐analysis indicates that the declining nitrate levels are linked to the release of dissolved iron to streams likely due to a reductive dissolution of iron(III) minerals in riparian wetland soils. This dissolution process mobilized adsorbed compounds, such as phosphate, dissolved organic carbon and arsenic, resulting in concentration increases in the streams and higher inputs to receiving drinking water reservoirs. Reductive mobilization was most significant in catchments with stream nitrate concentrations <6 mg L^?1. Here, nitrate, as a competing electron acceptor, was too low in concentration to inhibit microbial iron(III) reduction. Consequently, observed trends were strongest in forested catchments, where nitrate concentrations were unaffected by agricultural and urban sources and which were therefore sensitive to reductions of atmospheric nitrogen depositions. We conclude that there is strong evidence that the decline in nitrogen deposition toward pre‐industrial conditions lowers the redox buffer in riparian soils, destabilizing formerly fixed problematic compounds, and results in serious implications for water quality.