Deep-water stromatolites andFrutexites Maslov from the early and Middle Jurassic of S-Germany and Austria

Summary Despite extensive discussions during the last 20 years stromatolites are still used by many geologists as unequivocal indicators of very shallow-water conditions. We investigated four stratigraphic units from the Lower and Middle Jurassic of southern Germany (Posidonien-Schiefer, Amaltheen-Ton) and of the Northern Calcareous Alps (Adneter Kalk, Klauskalk), which were formerly interpreted as shallow marine sediments by some authors due to the occurrence of stromatolites. Our interpretations of the macro-, micro- and ultrafacies of these sediments are not compatible with shallow-water settings. We therefore propose a deep-marine, aphotic origin of these stromatolites. Former interpretations of the Posidonien-Schiefer as a shallow-water deposit are mainly based on the occurrence of stromatolites. We favour the model of a temporarily stagnant, deep, aphotic basin for these planktonrich sediments. Particles resembling ooids, but lying within mudstones cannot be taken as evidence for shallow agitated water. They either formed within the mud or are allochthonous. The deep-water setting of the red limestone of the Alpine Early and Middle Jurassic is indicated by a lack of platform-typical components like coated grains and phototrophic benthos and by shells of plankton and nekton forming a major part of the sediment. Stromatolites occur on the steep slope of a drowned Rhaetian reef with an estimated relief of 50–100 m and immediately below and within radiolarian limestones, deposited below the aragonite compensation depth (ACD). The aphotic stromatolites show some morphological differences to their shallow water counterparts. In all of our sections they occurred during intervals of reduced sedimentation. They form only thin horizons and probably grew very slowly. Mineralizations by Fe−Mn oxides and phosphate are very common. The presence of a microbial film is evident from binding of sedimentary particles, but the nature of the microbes is not known. Growth habits within the very distinct environments of red limestone and black shales show some common features, but also clear differences. The microproblematicumFrutexites Maslov is a very common component in deep-water stromatolites, but may also itself form small crusts or dendrolites. It occurs in two different forms. Opaque, slender forms with indistinct outlines probably grew within the weakly lithified sediment. Thicker, transparent forms with well defined outlines are found in cavities and probably also grew on the seafloor. Well preserved specimens display an internal fabric of radially arranged fibres of Fe−Mn oxides and calcite. It is suggested that calcite or aragonite were one original mineralogy ofFrutexites, which was later replaced by Fe−Mn oxides or phosphate. It is not certain whetherFrutexites is an organic, biomineralized structure or an inorganic mineralization, but the variable mineralogy and growth forms in different environments point to an organic origin. But even if organic, the occurrence in cryptic habitats and negative phototactic growth-directions make it clear thatFrutexites was not phototrophic.     

茶叶中总硒含量及其影响因素的研究

茶叶中硒素总量测定结果表明：土壤含硒量的高低是直接影响茶叶中硒的总量。茶树根、茎、叶、果中均有硒元素,叶片是茶硒积累的主要器官,尤其是老叶,其含量是嫩叶的几倍．茶树品种间含量的差异显著,最大差异达10倍以上．毛茶加工的成品茶含硒量受加工技术措施影响较大,其不同等级的含硒量与级别没有线性关系．     

利用荧光SSR标记鉴定茶树自然杂交后代遗传背景

为研究茶树自然杂交后代遗传背景,分析不同茶树自然杂交后代遗传差异,本研究利用24对EST-SSR标记对82个茶树自然杂交后代和34个福建主要栽培品种进行分子标记,分析了茶树自然杂交后代的亲缘关系、群体遗传多样性、亲本模拟分析。结果表明：(1)24对SSR标记共检测到157个多态性位点,平均等位位点数为6.542个,Nei’s多样性指数平均为0.588,Shannon’s 信息指数平均为1.182,平均观测杂合度和期望杂合度分别为0.577和 0.591。(2)遗传距离聚类将个供试样品划分为4类,群体1主要为‘丹桂’及其自然杂交后代;群体2主要为‘丹桂’、‘黄观音’自然杂交后代与福建省乌龙茶品种;群体3主要为‘白鸡冠’及其自然杂交后代;群体4主要为福建省绿茶品种。(3)‘丹桂’、‘白鸡冠’、‘黄观音’自然杂交后代群体与福建主要栽培品种的遗传距离分别为0.079、0.117、0.107。(4)群体1亚群b内‘丹桂’自然杂交后代模拟亲本准确率为77.8%,模拟父本主要为福建乌龙茶品种,与群体2(亚群a)的遗传相似度、遗传分化系数、基因流分别为0.899、0.043、5.480。(5)AMOVA分析结果显示,有88.52%的遗传变异来自群体内部的个体间,表明遗传变异主要发生在群体内。     

茶树品种‘金牡丹’自然杂交后代遗传鉴定

为了对‘金牡丹’茶树自然杂交后代进行遗传鉴定,利用EST-SSR毛细管电泳荧光标记技术对65个金牡丹自然杂交后代进行研究。结果表明,28对SSR标记共扩增出192个等位片段,平均等位基因数(Na)、平均观测杂合度(Ho)及遗传多态信息量(PIC)分别为6.86、0.540、0.532。单亲基因型已知时的累积排除概率为0.999,说明选择的28对SSR标记位点具有高度的多态性和较高的排除概率,适用于遗传分析和个体的亲子鉴定。15个‘金牡丹’自然杂交后代的遗传鉴定结果表明,MD44、JMD45、JMD47、JMD32为早生绿茶类型;JMD51、JMD53为闽北肉桂乌龙茶类型;MD2、JMD56为闽南‘铁观音’乌龙茶类型;JMD24、JMD26、JMD29、JMD55、JMD59、JMD27、JMD61为‘黄棪’乌龙茶类型。     

良种茶树芽叶中氨基酸研究

本文报导利用日立－ＥＧ型氨基酸自动分析仪测定的六个茶树良种芽叶中十九种氨基酸组成情况,并以此为依据对良好的品质风格进行了探讨。     

Rehabilitating degraded forests in Central Europe into self–sustaining forest ecosystems

There is a need for a consistent forest restoration strategy for the `Black Triangle', Central Europe. In the past 50 years, forests in this area have been heavily affected by industrial pollution. Recently, the amount of pollutants has decreased. This means that effective forest restoration programmes can be started. Forest decline must be seen as an ecological disturbance which cannot be solved by applying technical measures only. An ecosystem approach to forest restoration must be introduced into restoration policy and management. Basic principles and working methods of such an approach are briefly described and proposals are made for forest restoration policy, management and research in the area.     

Biomass and feeding activity of phagotrophic mixotrophs in the northwestern Black Sea during the summer 1995

Biomass and activities of planktonicmicroorganisms (bacteria, nanoplankton andmicroplankton) were measured in the northwestern BlackSea during summer 1995. The method based on theuptake of fluorescently labeled prey was chosen todetermine the ingestion rate of bacteria andnanoplankton by phagotrophic microorganisms. Thismethod revealed the presence of mixotrophic organismssuch as ’plastid-retaining ciliates‘ in the wholecoastal area. Mixotrophic ciliates were dominated bymicro-sized forms and maximum biomasses were recorded inthe water masses characterised by low nutrientconcentrations but high food particle concentrations. Mixotrophic nanoflagellates were absentand mixotrophic dinoflagellates were observed at onestation only. Mixotrophic ciliates were shown to ingestpreferably bacteria while mixotrophic dinoflagellateswere grazing almost exclusively on nanoflagellates.Although the biomass of mixotrophic organisms weresignificantly lower than those of aplastidic protozoa,their feeding activity contributed to 14 and 24% ofthe ingestion of bacteria and nanoplankton, respectively.This is due to the high specificingestion rate of mixotrophic micro-sized ciliates anddinoflagellates, which were two and three times higher,respectively, than the specific ingestion rate ofbacteria and nanoplankton by aplastidic protozoa. Thissuggests a significant contribution of phagotrophicmixotrophs to the microbial network of thenorthwestern Black Sea. This revised version was published online in July 2006 with corrections to the Cover Date.     

On the production,elemental composition (C,N, P) and distribution of photosynthetic organic matter in the Southern Black Sea

Chemical oceanographic understanding of the southernBlack Sea has been improved by recent measurements ofthe optical transparency, phytoplankton biomass (interms of chlorophyll-a and particulate organic matter)and primary productivity. During the spring-autmunperiod of 1995–1996, light generally penetrated onlyinto the upper 15–40 m, with an attenuation coefficientvarying between 0.125 and 0.350 m^2122;1. The averagechlorophyll-a (Chl-a) concentrations for the euphoticzone ranged from 0.1 to 1.5 μg l^2122;1. Coherentsub-surface Chl-a maxima were formed near the base ofthe euphotic zone only in summer. Production rate variedbetween 247 and 1925 in the spring and between 405 and687 mgC m^2122;2 d^2122;1 in the summer-autumn period.The average POM concentrations in the euphotic zonevaried regionally and seasonally between 3.8 and28.6 μm for POC, 0.5 and 3.1 μm for PON and0.02 and 0.1 μm for PP. Atomic ratios of C/N, C/Pand N/P, derived from the regressions of POM data,ranged between 7.5 and 9.6, 109 and 165, and 11.2 and16.6, respectively. In the suboxic/anoxic interface,the elemental ratios change substantially due to anaccumulation of PP cohering to Fe and Mn oxides. Thechemocline boundaries and the distinct chemicalfeatures of the oxic/anoxic transition layer (the so-called suboxic zone) are all located at specificdensity surfaces; however, they exhibit remarkablespatial and temporal variations both in their positionand in their magnitude, which permit the definition of long-term changes in the biochemical properties of theBlack Sea upper layer. This revised version was published online in July 2006 with corrections to the Cover Date.     

Regeneration and autotomy exhibited by the Black Widow spider,Latrodectus variolus walckenaer

Summary Crustaceans, insects and to a lesser degree arachnids have been employed in regeneration studies. Amputation and ligation of the legs was used to determine occurring in a Black Widow spider complied with the developmental gradient model of regeneration. The occurrence of autotomy in this species was also documented. Amputation indicated the most proximal point from which regeneration of the leg could occur was the femoral mid-point. Amputation proximal to that area did not result in leg regeneration. Autotomy following amputation was not observed. Ligation of the legs resulted in autotomy when applied at and proximal to the mid-point of the tibia, increasing in frequency as more proximal segments were ligated. Autotomy always occurred at the trochanter-coxa joint. Autotomized legs did not regenerate. The regeneration observed complied with the developmental gradient model.