Diatoms in Acid Mine Drainage and Their Role in the Formation of Iron-Rich Stromatolites

Adverse conditions in the acid mine drainage (AMD) system at the Green Valley mine, Indiana, limit diatom diversity to one species, Nitzschia tubicola. It is present in three distinct microbial consortia: Euglena mutabilis-dominated biofilm, diatomdominated biofilm, and diatom-exclusive biofilm. E. mutabilis dominates the most extensive biofilm, with lesser numbers of N. tubicola, other eukaryotes, and bacteria. Diatom-dominated biofilm occurs as isolated patches containing N. tubicola with minor fungal hyphae, filamentous algae, E. mutabilis, and bacteria. Diatom-exclusive biofilm is rare, composed entirely of N. tubicola.

Diatom distribution is influenced by seasonal and intraseasonal changes in water temperature and chemistry. Diatoms are absent in winter due to cool water temperatures. In summer, isolated patchy communities are present due to warmer water temperatures. In 2001, the diatom community expanded its distribution following a major rainfall that temporarily diluted the effluent, creating hospitable conditions for diatom growth. After several weeks when effluent returned to preexisting conditions, the diatom biofilm retreated to isolated patches, and E. mutabilis biofilm flourished.

Iron-rich stromatolites underlie the biofilms and consist of distinct laminae, recording spatial and temporal oscillations in physicochemical conditions and microbial activity. The stromatolites are composed of thin, wavy laminae with partially decayed E. mutabilis biofilm, representing microbial activity and iron precipitation under normal AMD conditions. Alternating with the wavy layers are thicker, porous, spongelike laminae composed of iron precipitated on and incorporated into radiating colonies of diatoms. These layers indicate episodic changes in water chemistry, allowing diatoms to temporarily dominate the system.     

The rattan trade of Northern Myanmar: Species, supplies, and sustainability

Although Myanmar exports millions of dollars of rattan cane each year, the last systematic treatment of rattans in this country was done over 100 years ago, and virtually nothing has been written about the collection and trade of this important forest resource. Here we report the results from a study of rattans in the Hukaung Valley Tiger Reserve in northern Myanmar. A total of 15 species of rattan were encountered; seven species are new records for Myanmar and two species are new to science. Inventory transects revealed that the density of commercial rattans in local forests averages 40.5 canes ≽4m long/hectare. Populations of all species appear to be actively regenerating. The current pattern of rattan exploitation, however, is largely uncontrolled and will eventually lead to resource depletion unless some form of management is implemented.     

Effects of antler breakage on mating behavior in male tule elk (<Emphasis Type="Italic">Cervus elaphus nannodes</Emphasis>)

Although antler size has been identified as a primary determinant of dominance, fighting success, and reproductive success in male cervids, >80% of the male tule elk (Cervus elaphus nannodes) in the Owens Valley, California, experience antler breakage. To determine the effect of antler breakage on male mating success, we recorded antler morphology, body size, and mating behavior of male elk throughout the rut. Antler breakage, regardless of severity, had no effect on male–male assessment, fighting success, or harem-holding status. The factor consistently associated with our indices of male mating success was not antler size but body size. Although antler size is frequently emphasized as a key factor in male dominance and social rank, this association may reflect the correlation between antler size and body size. In the Owens Valley, it appears that male elk are not assessing competitors based on antler morphology but on other characteristics. An erratum to this article can be found at     

Macroscopic and Microscopic Morphological Features of Stromatolites Related To Activity of Eukaryote-Dominated Biofilms in an Acid Mine Drainage Environment: Biosignatures and Understanding Preservation of Stromatolites as Trace Fossils

Euglena-, diatom-, and algae-dominated biofilms are the principal producers of iron-rich biolaminates that result in biosedimentary structures, or stromatolites, in an acid mine drainage (AMD) environment in Indiana. These structures are considered trace fossils because they are produced by organism-sediment interactions and record physicochemical conditions of the environment. Our purpose was to link the biofilm types to specific micro- and micromorphological features and the physicochemical conditions under which they were formed. Analyses revealed that Euglena-dominated biofilm produced thin, porous microlaminae by trapping, binding, and relocating AMD precipitates as the biofilm kept pace with chemical sedimentation. More massive microlaminae were produced by high rates of chemical sedimentation brought on by increased discharge and dilution of acidity. Diatom- and algae-dominated biofilms produced thick, mm–cm-scale, porous, spongelike micro- to macrolaminae through oxygenic photosynthesis and/or metal uptake in extracellular polymeric substances, which promoted mineral precipitation on cell walls to create a rigid, porous structure. The variations in biolaminate textures within the stromatolites record seasonal changes in the microbial populations and physicochemical conditions of the AMD environment. These iron-rich stromatolites represent trace fossils that record morphological biosignatures of eukaryote-dominated microbial biofilms and may serve as appropriate proxies in the search for similar evidence of eukaryotic life in other iron-rich paleoenvironments, such as those on early Earth and Mars.     

Plant biodiversity and its conservation strategy in the in-undation and resettlement districts of the Yangtze Three Gorges, China

The investigation on and conservation project of plant biodiversity in the inundation and resettlement districts of the Three Gorges region were carried out with the ongoing construction of the Three Gorges Dam. Based on the first-hand specimens collected for many years and the historical records, we found that there were about 1784 higher plant species, belonging to 762 genera of 170 families, which accounted for 59.19%, 75.30% and 85.85% of the total amount of species, genera and families in the Three Gorges region, including 27 species specific in these two districts. The shrub and grass communities were mostly distributed along the low-altitude river bank zone of the Yangtze River and were largely influenced by the dynamic water level of the Three Gorges reservoir area. The measurement of Shannon-Wiener and Pielou evenness indexes on 21 Pinus massoniana (Masson pine) communities distributed in the Three Gorges reservoir area was carried out, and results showed that the biodiversity of shrub layers was the highest, followed by grass layers, the middle, and tree layers, the lowest. Among the 11 typical shrub communities in this region, the abundance of shrub layers of Form. Rhus chinensis, Form. Cotinus coggygria var. cinerea, Form. Vitex negundo var. cannabifoliaand and Form. Coriaria sinica was relatively higher, which were 16, 26, 29 and 15, respectively. These four shrubs also showed high biodiversity index (H′), which were 1.791, 3.427, 2.949 and 1.718, respectively. Among the 9 grasslands mainly distributed along the river bank zone, 4 grassland communities with higher altitude (Form. Dicranopteris dichotoma, Form. Miscanthus floridutus, Form. Imperata cylindrica var. major and Form. Arthraxon hispidus) showed higher abundance and biodiversity, which were 1.697, 1.354, 1.144 and 1.018, respectively. Considering the inundation and resettlement districts, there were 22 vegetation types threatened by submersion, including 4 woody plant communities, 9 shrub communities and 9 grassland communities. The 6 shrub communities of Form. Securinega wuxiensis, Form. Bauhinia brachycarpa, Form. Geum aleppicum, Form. Distylium chinense, Form. Buxus henryi and Form. Myrsine africana would be fully submerged and part of Adianthum reniforme var. sinensis and Buxus ichangensis would be also submerged. At present, plant species conservation and monitoring stations in the Three Gorges region have been constructed, and more than 200 plant species have already been transplanted and conserved, including 37 threatened species listed in the China Plant Red Data Book and 11 local constructive species.     

辽河流域栽培稻对二化螟(Chilo suppressalis)的抗性

采用活体成株鉴定法测定了辽河流域主栽水稻品种对二化螟发育和为害的影响,同时测定了不同品种的主要形态特性、硅细胞数量和主要生化特性,评价这些品种对二化螟的抗性、分析其发生的可能机制。盐丰47对二化螟幼虫表现出较好的抗性,在沈农265上二化螟幼虫体重最小。在所测定的特性中,螟害株率与不同品种倒二叶叶角的自然对数之间具有显著的正相关关系,与稻茎Si含量之间具有显著的负线性相关关系;二化螟幼虫体重只与不同品种稻茎直径之间具有显著的正线性相关关系．研究结果对水稻品种杭件利用和未来水稻抗件育种的意义。     

宁夏黄河流域景观破碎化时空变化特征

基于RS和GIS技术,以土地利用数据为基础,采用有效粒度尺寸对宁夏黄河流域1985年和2010年的景观破碎化进行时空变化分析。结果显示:流域整体的有效粒度尺寸(meff)从1985年的6326.62 km2下降到2010年的2974.32 km2,破碎化程度呈显著加剧变化;从流域内部来看,景观破碎化程度最大的是黄左区间,破碎化程度最小的是苦水河和红柳沟;除引黄区间外,其余分区景观破碎化程度在25年间均有所加剧。特征尺度分析结果显示研究区景观破碎化空间变异分析的合适尺度为4500 m;景观破碎化指数的空间变异结果表明破碎化程度较大的区域面积明显多于破碎化程度弱的区域,景观破碎化空间异质性在25年间表现出明显的上升趋势。在海拔背景条件下,2400 m以下区域的景观破碎化程度较高,2400m以上区域破碎化程度较低,且随海拔的升高有降低的趋势;流域景观破碎化受人为干扰影响强烈,在人为干扰较强的1000—1500 m区段的景观破碎化程度最大;景观破碎化在时间上的变化受人为干扰影响产生的变化最为显著,由自然条件改变产生的影响有限。研究结果可为西北地区景观格局及景观破碎化的研究提供参考,并为区域景观格局优化和土地的有效管理提供依据。     

Humidity and seasonality drives body size patterns in males of the bush cricket Isophya rizeensis Sevgili, 2003 （Orthoptera： Tettigoniidae： Phaneropterinae）

Two primary patterns of body size variation have been recorded in ectotherms in relation to latitudinal/altitudinal shifts. In some, body size increases with increasing latitude/altitude whereas, in others, body size decreases with increasing latitude/altitude. This clinal variation is generally assumed to be caused by local adaptation to environmental conditions however the selective variable（s） （temperature, humidity, diet quality, etc.） is still heavily debated. Here we investigate geographic variation in body size of dark and pale color morphs of males of the bush-cricket lsophya rizeensis collected from 15 locations along an elevation gradient ranging from 350 to 2 500 m. Using an information theoretical approach we evaluate the relative support of four different hypotheses （the temperature size rule, the moisture gradient hypothesis, the seasonal constraint hypothesis, and the primary productivity hypothesis） explaining body size variation along the altitudinal gradient. Body size variation in pale color morphs showed a curvilinear relationship with altitude while dark color morphs showed no variation in body size. Body size variation in pale color morphs was highly correlated with precipitation and temperature seasonality values thus giving strong support for the moisture gradient and seasonal constraint hypothesis. Our results reinforce the importance of gradients in humidity and seasonality over temperature in the creation of altitudinal body size clines and the role of selection for resistance to stress factors in the establishment of these clines. Whether a body size cline is observed or not might also depend on the phenotypic properties of the individuals, like coloration.