Controls on the distribution of calcareous Foraminifera in the Lower Carboniferous of Ireland

Microfacies analyses of thin sections from over 650 samples of Asbian and Brigantian (late Viséan) platform carbonates from Ireland shows that foraminiferal assemblages are controlled by the relative abundance of echinoderms (mainly crinoids), bryozoans and calcareous algae: Koninckopora, Ungdarella and palaeoberesellids. Archaediscidae, Valvulinella and Tetrataxidae thrived in algal-poor crinoid and bryozoan thickets at or below fair-weather wavebase. Late Viséan algal limestones contain abundant Endothyridae and Palaeotextulariidae, and are interpreted to have been deposited at depths between 5 and 10 m. The morphology of the Foraminifera studied is related closely to their facies distribution. Many taxa inhabited high energy shallow marine algal meadow facies, these include: Bibradya, Cribrospira, Nevillella and Bradyina with cribrate apertures and other specialised test features that protected the protoplasm from damage, Gigasbia, Omphalotis, Globoendothyra and Pseudoendothyra with large, rotund or keeled, multilayered tests and Forschiidae with large thick-walled tests. Infaunal taxa such as the Lituotubella, Nevillella, Gigasbia and the palaeotextulariids are recorded from algal facies and appear to have been unable to survive on bryozoan and crinoidal substrates. Pseudoammodiscus and Earlandia, characterized by simple morphologies and single layered walls, and Endothyranopsis, Endothyra and Eostaffella, planispirally coiled with multilayered micritic tests, are regarded as the least facies-controlled of the taxa studied. The encrusting nature of Pseudolituotuba and Scalebrina ensured survival in a wide range of platformal palaeoenvironments, though algal meadows were not generally suitable substrates for the Pseudolituotubidae. The secondary deposits in the umbilical region of the Asteroarchaediscinae may have been an adaptation for survival in the dense crinoidal bryozoan thickets where they lived. Delicate Planoarchaediscus occurs in algal-poor wackestone to packstone facies typical of low energy palaeoenvironments possibly at depths below 20 m. Howchinia, which occurs with Fasciella (a probable alga) in intraclastic wackestone facies may also have lived in water deeper than 20 m. Major changes in foraminiferal assemblages through the Asbian and Brigantian stages of the late Viséan are attributed to changes in associated biotic constituents. Early Asbian endothyrid and forschiid dominated assemblages were controlled by the relative abundance of bryozoans, Koninckopora and palaeoberesellids. By the late Asbian, the foraminiferal assemblages were controlled by the presence or absence of palaeoberesellids, Ungdarella and to a lesser extent bryozoans. Asbian assemblages were similar, although foraminifers such as bradyinids, Cribrospira and Globoendothyra became abundant in the late Asbian. A switch to predominantly echinoderm (mainly crinoid) and bryozoan substrates in the Brigantian may have caused the major change from late Asbian endothyrid and palaeotextulariid assemblages to archaediscid and tetrataxid dominated assemblages.     

<Emphasis Type="Italic">Remalcis</Emphasis> and <Emphasis Type="Italic">Epiphyton</Emphasis> as different stages in the life cycle of calcareous algae

Although the calcareous algae Renalcis and Epiphyton, which were main reef-constructors at the end of the Late Proterozoic, beginning of the Cambrian, and, partially, in the Devonian, long attracted the attention of scientists, their nature long remained enigmatic. Numerous revisions inclined to the opinion that Renalcis only existed and considered Chabakovia, Shuguria, Izhella, and even Epiphyton as synonyms of the former genus. However, convincing proofs for this conclusion were lacking. I propose a new morphological interpretation of the Renalcis group, based on Gemma with its unique preservation of monospores within the colony, which overgrew outside the colony first in Korilophyton and then in Epiphyton. It was concluded that the life cycle of Epiphyton included heteromorphous stages of Renalcis (Izhella), Chabakovia (Shuguria), Gemma, and dendroid Korilophyton.     

广西隆林祥播中二叠世生物礁的钙藻化石

本文描述了广西隆林祥播中二叠世茅口期生物礁中的钙藻化石17属18种,其中新属5个:Paralithoporella gen. nov., Guangxilamina gen. nov., Favoporella gen. nov., Sinophyllum gen. nov.,和Monostysisyrinx gen. nov.; 新种9个:Solenopora guangxien sis sp. nov., Paralithoporella sincrisis gen. et sp. nov., Guangxilamina incompta gen. et sp. nov., Favoporella hexagona gen. et sp. nov., Ivanovia permica sp. nov., Anchicodium expressum sp. nov., Sinophyllum hexagonum gen. et sp. nov., Sphaeroporella minima gen. et sp. nov., Monostysisyrinx circula ris gen. et sp. nov.。本文还建立一新科——Monostysi sy rinaceae。在当前生物礁中,钙藻是重要的造礁生物,可以起造架、粘结、障积等作用,也可作为居礁生物或造粒生物     

Facies analysis of lower permian platform carbonates,sverdrup basin,canadian arctic archipelago

Summary The Asselian-Sakmarian strata of the Fosheim-Hamilton subbasin represent a distinct 15 000 km² depocentre located at the northeast margin of the main Sverdrup Basin in the Canadian Arctic Archipelago. Approximately 35 high-frequency cycles composed mainly of platformal carbonates with subaqueous evaporites accumulated at a time of renewed rifting activity in this subbasin. A general depositional model based on the facies analysis of the Asselian-Sakmarian strata shows that the carbonate platforms surrounding the Fosheim-Hamilton subbasin were segmented by the position of critical interfaces including the: 1) base of the fairweather wave abrasion zone; 2) base of the storm wave abrasion zone; and 3) base of the photic zone. The base of the fairweather wave abrasion zone divided the platforms into two broad parts; an inner shelf with a relatively quiet, semi-restricted lagoon and more agitated, open marine barries and shoals and an open marine mid-shelf with numerous reefal and non-reefal subenvironments extending from the base of fairweather wave abrasion zone to below the photic zone. Outer shelf and associated slope and basin were not present within the Fosheim-Hamilton subbasin but were present farther west along the margin of the main Sverdrup Basin.     

中国新疆塔里木盆地上奥陶统良里塔格组的钙藻化石

钙藻是可以发生生物钙化作用形成钙质"骨骼"的分属多个门类的藻类的俗称。钙藻最早出现于寒武纪,奥陶纪发生第一次辐射演化。本文系统讨论了绿藻门绒枝藻目(Dasycladales)、羽藻目钙扇藻科(Udoteaceae)的科和属级分类标准和红藻门珊瑚藻科、管孔藻科(Solenoporaceae)属级分类标准及其中各属分类中存在的问题。塔里木盆地晚奥陶世在塔中—巴楚台地和塔北台地发育了一套礁滩相良里塔格组碳酸盐岩,其中含有丰富的钙藻化石。本文系统描述了来自塔里木盆地塔中、巴楚、塔北地区取心井上奥陶统良里塔格组岩层中的钙藻化石11个属15个种。包括绿藻门绒枝藻目西莱特藻科(Seletonellaceae)的Dasyporella,Kazakhstanelia,Vermiporella,Aphroporella,Arthroporella,绿藻门的羽藻目Bryopsidales(siphonales)的钙扇藻科的Dimor phosiphon,Palaeo porella,红藻门珊瑚藻目(Corallinales)的管孔藻科的Solenopora,Parachaetetes及Corallinales incertus familiae的Petro-phyton,以及分类位置不明的Monili porella。其中绒枝藻Ajakmalajsoria被视作Kazakhstanelia的同义名。     

从塔北隆起奥陶纪钙藻化石探讨奥陶纪的古环境

塔里木盆地塔北隆起轮南46井、英买1、2井奥陶纪石灰岩内含有大量的钙藻化石、蓝细菌以及疑难微体化石。这些钻井岩芯均在深达5000-6200m的地下深部取得。钙藻主要为绿藻类的Dasyporella,Ver‘miporella,Moniliporella以及?Plexa;红藻类的管孔藻类Solenoporaceans;钙化蓝细菌则有Girvanella,Botomaella,?Subtifloria等;疑难微体化石有Bevocastria,Nuia,Rothpletzella。这些钙藻生活于热带或亚热带正常盐度的浅海水内,其水深不到20m。世界各地的奥陶纪Vermiporella均位于古赤道的两侧,这表明它们是在气候炎热、温暖海水中生活的一类海洋藻类。Girvanella以藻灰结核和内碎屑最为常见,某些球粒可能代表Girvanella破碎后形成的单管或小棒。塔里木盆地钙藻植物群相似于哈萨克斯坦、波罗的海周围地区以及北美同时代植物群,这表明这些钙藻和蓝细菌化石具有遍布于全球的性质。塔北隆起早、中奥陶世沉积属于典型的碳酸盐岩台地相沉积。到晚奥陶世时,碳酸盐岩沉积被浅水陆棚沉积所取代,以陆源碎屑岩为主,夹少量的碳酸盐岩。     

Polysaccharides of Calcareous Algae and Their Effect on the Calcification Process

The composition and structure of polysaccharides from several groups of calcareous algae (including calcareous cyanobacteria), which differ in the calcification mode (extracellular, cell wall, or intracellular), are reviewed. Two families of marine algae, Corallinaceae (Rhodophyta) and Coccolithophoraceae (Prymnesiophyta = Haptophyta), are considered in detail; they exhibit the cell wall and intracellular calcification modes, respectively, and synthesize unusual polysaccharides that seem to directly participate in the calcification process.     

两种钙藻热解产出的气态和液态烃类

在２００℃至４００℃高温和还原条件下分别对仙掌藻和乳节藻两种钙质藻类进行热模拟降解实验,分离获得气态和液态烃类化合物。随着热解温度升高,两种钙藻产烃气量明显上升,其中甲烷与乙烷气的增加最多,同时两种钙藻产出的乙烷与乙烯比值都有规律地增加,但仙掌藻产烃气量高于乳节藻。这表明钙质藻类可能是天然气的一种重要母质来源。虽然这两种钙藻随温度增加热解产出的可溶有机质及族组分的变化规律不明显,但它们的正烷烃分布特征具有相类似的变化。未经热解时它们都以Ｃ１７为主峰的低碳数正烷烃占优势;当热解温度从２００℃增加到４００℃时,它们都又表现出以Ｃ２５或Ｃ２３为主峰的较高碳数正烷烃占优势的分布特征。这与富含钙藻化石的沉积岩样品中正烷烃的分布特征相一致,说明Ｃ２５或Ｃ２３为主峰的较高碳数正烷烃占优势的分布特征可能是钙藻热解有机质的一种判识标志．     

Coralline-algal assemblages of a Burdigalian platform slope: implications for carbonate platform reconstruction (northern Sardinia,western Mediterranean Sea)

The rhodolithic slope deposits of a Burdigalian carbonate platform in Sardinia near Sedini were analyzed to reconstruct facies and palaeobathymetry. There is a distinct red-algal growth zonation along the platform slope. The clinoform rollover area consists of coralline-algal bindstones, which downslope change into a zone where rhodoliths are locally fused by progressive encrustation. Mid-slope rhodoliths are moderately branched, and downslope rhodoliths have fruticose protuberances, resulting in branching rhodolith growth patterns. There is a sharp change from the rhodolitic rudstones to the basinal, bivalve-dominated rudstones at the clinoform bottomsets. Red-algal genera identified include Sporolithon, Lithophyllum, Spongites, Hydrolithon, Mesophyllum, Lithoporella, Neogoniolithon, and other mastophoroids and melobesioids. Genera and subfamilies show a zonation along the clinoforms, allowing palaeobathymetric estimates. The clinoform rollovers formed at a water depth of around 40 m and the bottomsets around 60 m. Results from geometrical reconstruction show that coral reefs in the inner platform formed at water depths of around 20 m. Therefore, the Sedini carbonate platform is an example of a reef-bearing platform in which the edge or the platform-interior reefs do not build up to sea level.     

Biostratigraphic subdivision and correlation of Uppermost Carboniferous/Lower Permian sediments in the Southern Alps: Fusulinoidean and condont faunas from the Carnic Alps (Austria/Italy), Karavanke Mountains (Slovenia), and Southern Urals (Russia)

Summary In order to establish a refined biostratigraphic subdivision and correlation of the Uppermost Carboniferous/Lower Permian deposits of the Southern Alps (Carnic Alps, Karavanke Mountains; Austria/Italy/Slovenia), two major microfossil groups (fusulinoideans, conodonts) were investigated within the same sample. The fusulinoidean species diversity (71 species, including five new species and three new subspecies) and generic composition were reviewed and complemented. Additionally, the data on fusulinoidean assemblages were supplemented by co-occurring conodont faunas (seven species). Accompanying studies on material from the type sections of the Southern Urals (Russia) were made to improve the biostratigraphic correlation with the Russian standard zonation and to discuss paleobiogeographical aspects of the faunal associations. An integrated microfacies analysis of the sampled material in the Southern Alps serves to evaluate the relationships between certain genera and specific microfacies types. The fusulinoidean fauna of the Lower “Pseudoschwagerina” Limestone is of late Gzhelian age. The Carboniferous/Permian boundary is close to the base of the Grenzland Formation, which covers the entire Asselian and a part of the Sakmarian. The Upper “Pseudoschwagerina” Limestone and Trogkofel Limestone are Lake Sakmarian to Artinskian. The studies sequences in the Karavanke Mountains. formerly known as “carbonate and clastic Trogkofel beds”, correlate to the Lower “Pseudoschwagerina” Limestone, respectively with parts of the Grenzland Formation. Due to the lithologic differences, new formation names (Dolzanova Soteska Fm., Born Fm.) were introduced for the so-called “Trogkofel” Limestone along the Dolzanova Soteska. Whereas late Gzhelian/Asselian fusulinoidean faunas of the Southern Alps correspond to the Southern Uralian faunas to a large extent, Sakmarian and Artinskian faunas reveal an increasing divergence in species and genus composition. Climatic as well as geographic barriers may have prevennted the dispersal of Paleotethyan taxa into the Southern Urals. Biostratigraphic correlation of Sakmarian to Artinskian deposits is therefore possible only on the basis of the sparse conodont faunas.     

罗马尼亚特提斯区的早白垩世粗枝藻化石SELIPORELLA NEOCOMIENSIS RADOICIC,1975 (NON 1963), NOV. COMB.

本文对藻类Seloporella的系统分类进行了评论。根据Barattolo等人,1992年对该属的评论,结合对产自罗马尼亚阿朴塞尼山区(Apuseni Mountains),早白垩世的Triploporella neocomiensis Radoicic及与己发表的资料进行了对比研究,提出了Seliporella neocomiensis的新组合,同时与该化石组合形态非常相似的“Diplopora” johnsoni Praturlon,1964进行了对比。     

Coralline red algal assemblage from the Middle Pliocene shallow-water temperate carbonates of the Monte Cetona (Northern Apennines,Italy)

During the Pliocene and Pleistocene, the Monte Cetona (Northern Apennines, central Italy) was part of an elongated island. The Middle Pliocene deposits around the Monte Cetona are represented by shallow-water marine carbonates rich in coralline red algae and bryozoans. These skeletal carbonates, characterising a coralline algal-dominated factory, were analysed in terms of microfacies, taxonomy, and growth-forms of coralline red algal assemblage. Three microfacies were distinguished on the basis of component distribution and fabric analysis: coralline algal rudstones, coralline algal floatstones, and bioclastic packstones. Skeletal components are commonly abraded, bioeroded, and encrusted. The shallow-water skeletal carbonates are strongly bioturbated and any primary sedimentary structure is obliterated. The distribution of the coralline growth-forms suggests a decreasing hydrodynamic gradient from the coralline algal rudstone, through the coralline algal floatstone to the bioclastic packstone microfacies. The coralline algal flora consists of eight species representing the subfamilies Lithophylloideae, Mastophoroideae and Melobesioideae. The assemblage is dominated by lithophylloids. Other biogenic components are bryozoans, barnacles, echinoderms, and benthic foraminifera. These coralline algal assemblages were deposited just above the fair-weather wave base and indicate a shallow-marine temperate water setting for the eastern Tyrrhenian Sea during the Mid Pliocene.     

间断下体负压暴露方式对下体负压耐力的影响

目的：探讨不同方式反复下体负压锻炼对下体负压耐力的影响,以期筛选最佳的负压锻炼方式。方法：27名男性健康受试者随机分成3组,分别进行－5.33kPa8min(A组）、6.67kPa4min（B组）、6.67kPa8min（C组）的下体负压锻炼后累积应激指数（CSI）、总耐受时间（DNP）较锻炼前显著提高,A、B组上述指标无显著变化,下体负压暴露时的心率较平静状态显著升高,收缩压显著降低,舒张压无显著变化。结论：经过－6.67kPa/d8min连续8d的间断下体负压可以显著提高下体负压耐力。     

广西、贵州和川东二叠纪生物礁的钙藻化石及其古生态环境

广西,贵州和川东二叠纪礁相岩石和礁后相岩层内获得了红藻Solenoporella,Gymnocodium,Permocalcu-lus;绿藻Anthracoporella,Mizzia以及显微疑难藻类化石Pseudovermiporella,Tubiphytes等,除了广西隆林有中二叠世茅口期藻类化石外,其它均属于晚二叠世乐平世的分子,这些藻类植物一般生活于热带和亚热带,正常盐度的浅海水内,其水深不大于30m,川东,鄂西晚二叠世礁属于浅水海绵礁,而非深水礁。