中国东北晚侏罗世短角亚目化石一新属二新种(双翅目:独须虻科)(英语)

本文记述短角亚目1新属Alleremonomus,2新种:Alleremonomus xingi sp.nov,Alleremonomusliaoningensis sp.nov,其分类位置归于双翅目、短角亚目、独须虻科(Eremochaetidae).化石采自辽宁北票晚侏罗世沉积物中.对独须虻科的化石记录作了简要的回顾.     

CHLOROPHYLL A:B RATIOS IN SOME SIPHONOUS GREEN ALGAE IN RELATION TO SPECIES AND ENVIRONMENT1

The chlorophyll a:b ratios measured in several species of Caulerpa and in Bryopsia plumosa (Hudson) C. Ag. gave values close to 2.00 or below. Values obtained for Ulva lactuca L. taken from the same site gave a higher value of 2.44, and the sea-grass Heterozostera tasmanica (Martens ex Aschers) den Hartog a value of 2.98. Although there were changes in a:b ratios observed when Caulerpa plants were, stored for up to 10 days in dim light, the values did not suggest that chlorophyll a:b ratios were directly controlled by light intensity. It is conducted that the a:b ratios described in this paper, are a characteristic of the species themselves and are not a result of their growth in extremely shaded situations.     

准噶尔盆地北缘谢家阶底界—推荐界线层型及其生物—年代地层和环境演变意义

新疆准噶尔盆地北缘铁尔斯哈巴合地层剖面构造简单并含有丰富的晚渐新世及早中新世哺乳动物化石。其中铁尔斯哈巴合组及索索泉组沉积基本连续,两组界线位于剖面米距33m处。依据该剖面中8个层位和相邻的XJ99005剖面中18个层位上采集的化石以及它们的上下关系和生物组合性质,划分出5个哺乳动物组合带,其中两个位于铁尔斯哈巴合组中(铁-Ⅱ带),3个在索索泉组下部(索-Ⅰ,Ⅱ,Ⅲ带)。从剖面的铁尔斯哈巴合组、索索泉组和哈拉玛盖组中以0．5m的间距采集了348组古地磁样品,获得的磁性剖面包含了16个正向带和16个反向带(事件),其中包含了相当于地磁极时间表中C7n～C5E段的完整磁极带。铁-Ⅰ～Ⅱ带与塔本布鲁克哺乳动物群相近,为中国已知位置最西、构成门类和数量最多的一个晚渐新世哺乳动物组合。索-Ⅰ带应为中国目前所知的最晚渐新世的哺乳动物带。早中新世索-Ⅱ带与谢家动物群和蒙古中部渐新世—中新世过渡带D带可以对比。早中新世索-Ⅲ带相当于过去使用的“索索泉动物群”,时代大致与乌尔图动物群相当。根据地磁极时间校正,铁尔斯哈巴合剖面中铁尔斯哈巴合组和索索泉组跨越了从24．5Ma(地磁极时带C7n．2n)到18Ma(地磁极时带C5Dr．2r)大约6．5Ma的时间,岩体平均沉积速率大约为2．5cm/千年。剖面中5个生物组合带的时间跨度大致分别为：铁-Ⅰ带：24．4～24．15Ma;铁-Ⅱ带：23．2～23．1Ma;索-Ⅰ带接近但还未到达渐新世/中新世界线的23．03Ma;索-Ⅱ带：21．9～21．7 Ma;索-Ⅲ带：21．68～21．15Ma。我们推荐将铁尔斯哈巴合剖面作为中国区域年代地层单位谢家阶(期)底界界线层型的一个候选剖面。与谢家阶底界相对应的界线暂定在剖面由底向上40．25m处,对应于地磁极时带C6Cn．2n底界。该界线位于索索泉组内部,索-Ⅰ和索-Ⅱ带之间。根据定义,该界线也分别对应于阿基坦阶、中新统以及新近系的底界,年龄为23．03Ma。文章还讨论了下列问题：1)索索泉组的绝大部分应当和谢家阶以及山旺阶地层对比,仅其底部含有索-Ⅰ带化石组合的部分可与塔本布鲁克阶地层对比。2)在进行生物地层对比时尽量使用不同的索索泉组哺乳动物组合带,传统的“索索泉动物群”仅大体相当于索-Ⅲ带。3)许多过去认为的渐新世哺乳动物分子的生存时代实际上延伸到了早中新世,仅以这些分子的存在,不能说明一个动物群及其地层的确切年代。4)塔本布鲁克动物群及相关的期、阶名为有效名称,具有合法性;该阶底界有待确立。5)如果山旺阶底界(谢家阶顶界)位于地磁极时带C6An．1r底,年代为20．43Ma,相应的界线应位于铁尔斯哈巴合剖面89．25m处,因此,铁尔斯哈巴合剖面中有可能产生谢家阶的单位层型,该阶的地质时间跨度为2．6Ma。6)5个生物带都是以兔形类、啮齿类以及食虫类等小哺乳动物为主要分子,而且同门类的属种问具有相当近的演化关系,说明这个地区从晚渐新世到早中新世的一段时期中,动物群性质没有明显变化,总体上反映了一个从早渐新世以来就比较干旱的环境;渐新世和中新世动物群成分在种一级上仍有明显差异;而相当于谢家动物群的索-Ⅱ带则带有明显的过渡性质。7)从索索泉组的岩性、分布的地理部位以及与甘肃秦安剖面相近的时代和动物群等来看,不排除含有风成沉积物的可能。     

准噶尔盆地北缘谢家阶底界一推荐界线层型及其生物一年代地层和环境演变意义

新疆准噶尔盆地北缘铁尔斯哈巴合地层剖面构造简单并含有丰富的晚渐新世及早中新世哺乳动物化石.其中铁尔斯哈巴合组及索索泉组沉积基本连续,两组界线位于剖面米距33 m处.依据该剖面中8个层位和相邻的XJ99005剖面中18个层位上采集的化石以及它们的上下关系和生物组合性质,划分出5个哺乳动物组合带,其中两个位于铁尔斯哈巴合组中(铁-Ⅰ,Ⅱ带),3个在索索泉组下部(索-Ⅰ,Ⅱ,Ⅲ带).从剖面的铁尔斯哈巴合组、索索泉组和哈拉玛盖组中以0.5 m的间距采集了348组古地磁样品,获得的磁性剖面包含了16个正向带和16个反向带(事件),其中包含了相当于地磁极时间表中C7n～C5E段的完整磁极带.铁-Ⅰ～Ⅱ带与塔本布鲁克哺乳动物群相近,为中国已知位置最西、构成门类和数量最多的一个晚渐新世哺乳动物组合.索-Ⅰ带应为中国目前所知的最晚渐新世的哺乳动物带.早中新世索-Ⅱ带与谢家动物群和蒙古中部渐新世-中新世过渡带D带可以对比.早中新世索-Ⅲ带相当于过去使用的"索索泉动物群",时代大致与乌尔图动物群相当.根据地磁极时间校正,铁尔斯哈巴合剖面中铁尔斯哈巴合组和索索泉组跨越了从24.5 Ma(地磁极时带C7n.2n)到18 Ma(地磁极时带C5Dr.2r)大约6.5 Ma的时间,岩体平均沉积速率大约为2.5 cm/千年.剖面中5个生物组合带的时间跨度大致分别为:铁-Ⅰ带:24.4～24.15 Ma;铁-Ⅱ带:23.2～23.1 Ma;索-Ⅰ带接近但还未到达渐新世/中新世界线的23.03 Ma;索-Ⅱ带:21.9～21.7Ma;索-Ⅲ带:21.68～21.15 Ma.我们推荐将铁尔斯哈巴合剖面作为中国区域年代地层单位谢家阶(期)底界界线层型的一个候选剖面.与谢家阶底界相对应的界线暂定在剖面由底向上40.25 m处,对应于地磁极时带C6Cn.2n底界.该界线位于索索泉组内部,索-Ⅰ和索-Ⅱ带之间.根据定义,该界线也分别对应于阿基坦阶、中新统以及新近系的底界,年龄为23.03 Ma.文章还讨论了下列问题:1)索索泉组的绝大部分应当和谢家阶以及山旺阶地层对比,仅其底部含有索-Ⅰ带化石组合的部分可与塔本布鲁克阶地层对比.2)在进行生物地层对比时尽量使用不同的索索泉组哺乳动物组合带,传统的"索索泉动物群"仅大体相当于索-Ⅲ带.3)许多过去认为的渐新世哺乳动物分子的生存时代实际上延伸到了早中新世,仅以这些分子的存在,不能说明一个动物群及其地层的确切年代.4)塔本布鲁克动物群及相关的期、阶名为有效名称,具有合法性;该阶底界有待确立.5)如果山旺阶底界(谢家阶顶界)位于地磁极时带C6An.1r底,年代为20.43 Ma,相应的界线应位于铁尔斯哈巴合剖面89.25 m处,因此,铁尔斯哈巴合剖面中有可能产生谢家阶的单位层型,该阶的地质时间跨度为2.6 Ma.6)5个生物带都是以兔形类、啮齿类以及食虫类等小哺乳动物为主要分子,而且同门类的属种间具有相当近的演化关系,说明这个地区从晚渐新世到早中新世的一段时期中,动物群性质没有明显变化,总体上反映了一个从早渐新世以来就比较干旱的环境;渐新世和中新世动物群成分在种一级上仍有明显差异;而相当于谢家动物群的索-Ⅱ带则带有明显的过渡性质.7)从索索泉组的岩性、分布的地理部位以及与甘肃秦安剖面相近的时代和动物群等来看,不排除含有风成沉积物的可能.     

内蒙古眼蕈蚊五新种及—中国新记录属(双翅目:眼蕈蚊科)

眼蕈蚊科(Sciaridae)为双翅目中小型暗色的蚊类,触角16节,复眼向背面尖突形成眼桥。眼蕈蚊的种类多、数量大,幼虫多生活在富有腐植质的土壤中,常危害植物的地下部分及野生和栽培的菌蕈。我国的眼蕈蚊种类相当多,但内蒙古缺乏调查,本文就现有的标本记述了5新种,代表5个属,内有一中国新记录属。新种的模式标本保存在北京农业大学昆虫标本室。     

四川大鲵寄生吸虫一新属新种（吸虫纲：复殖目）

本文描述寄生在大鲵肠道内隐殖科,隐殖亚科吸虫一新种,沐川新鲵居吸虫Ｎｅｏａｎｄｒｉｎｃｏｌａ ｍｕｃｈｕａｎｅｎｓｉｓ ｓｐ．ｎｏｖ．并建立了新属,即新鲵居吸虫属Ｎｅｏａｎｄｒｉｎｃｏｌａ ｇｅｎ．ｎｏｖ．标本采自四川省沭县。模式标本保存在四川农业大学兽医学系。     

THE USE OF TOXICITY TESTING IN EFFLUENT REGULATION AND CONTROL: A NEW DIMENSION TO ASSESSMENT AND MANAGEMENT OF WATER QUALITY IN SOUTH AFRICA

Summary

Efficient management tools are continually required to cope with increasing demands placed on the quality and quantity of aquatic resources. Recent developments in environmental monitoring indicate the importance of incorporating biological indicators in assessment programmes. Aquatic toxicology has consequently become an important monitoring and regulatory science. Applications of aquatic toxicity testing include: deriving water quality criteria; toxicological evaluations of whole effluents and receiving waters; and the estimation of ecological risk. Toxicity testing can potentially play a significant role in improving water quality in years to come, especially through its application in effluent regulation. Currently however, few environmental laboratories in South Africa have the required expertise and facilities to carry out a representative range of toxicity tests. Training and funding are required to build the capacity for the necessary developmental research, before toxicity testing can routinely be implemented.

The significant problems we face cannot be solved at the same level of thinking we were at when we created them. Albert Einstein.     

TRANSFER OF PROTEINS FROM THE CHLOROPLAST TO VACUOLES IN CHLAMYDOMONAS REINHARDTII (CHLOROPHYTA): A PATHWAY FOR DEGRADATION

Several chloroplast proteins were detected by immunoelectron microscopy within dense granules in cytoplasmic vacuoles in the alga Chlamydomonas reinhardtii Dangeard. Transfer from chloroplast to vacuoles of two major, pulse-labeled polypeptides, the large subunit of rubisco and the α subunit of ATPase, which are synthesized on chloroplast ribosomes, was demonstrated by the recovery of these polypeptides in vacuolar granules over a several-hour time period. The ultrastructure of cryofixed algal cells was examined to search for structures that would provide insight into the transfer of chloroplast proteins to vacuoles. Micrographs showed that the two membranes of the envelope were appressed, with no detectable intermembrane space, over most of the chloroplast surface. Protrusions of the outer membrane of the envelope were occasionally found that enclosed stroma, with particles similar in size to chloroplast ribosomes, but generally not thylakoid membranes. These observations suggest that chloroplast material, especially the stromal phase, was extruded from the chloroplast in membrane-bound structures, which then interacted with Golgi-derived vesicles for degradation of the contents by typical lysosomal activities. A protein normally targeted to vacuoles through the endomembrane system for incorporation into the cell wall was detected in Golgi structures and vacuolar granules but not the chloroplast.     

CACO3 OPTICAL DETECTION WITH FLUORESCENT IN SITU HYBRIDIZATION: A NEW METHOD TO IDENTIFY AND QUANTIFY CALCIFYING MICROORGANISMS FROM THE OCEANS1

Open oceanic calcification is mainly driven by unicellular organisms and in particular by eukaryotes such as coccolithophores and foraminifers. Open ocean microcalcifiers, like most planktonic protists, are characterized by extremely fast generation times and occasional sexual reproduction. Populations can alternate between diploid and haploid stages, which often build different kinds of cell covers. In the most important pelagic calcifiers, the coccolithophores, the diploid and haploid stages, which can self‐replicate and grow independently, display radically different morphologies with different modes of calcification or even with the absence of calcification in at least one life cycle stage. Although life cycle strategies seem likely to fundamentally influence the where and when of open ocean calcification, this issue has yet to be seriously addressed in the natural environment. Here, we introduce a new morphogenetic method, “combined CaCO₃ optical detection with fluorescent in situ hybridization,” or COD‐FISH, which is based on a combination of TSA‐FISH and polarized optical microscopy. This technique allows simultaneous assessment of the taxonomic and life cycle status of single coccolithophore cells collected from the ocean. We demonstrate the application of COD‐FISH using both laboratory culture and field samples and discuss its potential value for assessing the ecology, biodiversity, population structure, and life cycles of coccolithophores and other open ocean unicellular calcifiers.