Palynological correlation of the upper devonian and lower carboniferous in central Ireland

Miospore assemblages assigned to the PL, NV, CM and Pu Zones have been recorded from a number of boreholes which penetrated Upper Devonian and Lower Carboniferous (Tournaisian and early Visean) rocks in central Ireland. The palynomorphs occur in both marine and non-marine successions, permitting correlation between these two facies. The boundary between the PC and CM Zones has been located within three sections. The palynological data suggest that the base of the marine sequence is of mid-Tournaisian (Tn2) age at Ballyvergin in the south of the area described and of uppermost Tournaisian (Tn3) or earliest Visean age around Clew Bay in the northwest.     

Aspects of late triassic palynology. 3. Palynology of latest triassic and earliest jurassic deposits of the northern limestone alps in Austria and southern Germany,with special reference to a palynological characterization of the Rhaetian stage in Europe

The present paper provides a palynological analysis of samples from the “Kössener Schichten”, “Schattwalder Schichten” and the ammonoid (Psiloceras planorbe)-bearing beds of the “Fleckenmergel/Fleckenkalk” found in the vicinity of Salzburg (Austria and adjacent part of Germany).It is shown that the compositional development of latest Triassic—earliest Jurassic palynological assemblages from Alpine sequences matches the situation in the Germanic realm. A characteristic phase in this development is interpreted in terms of the Rhaetipollis germanicus Assemblage Zone. It is considered that this zone could well be regarded as a palynological characterization of the Rhaetian Stage in Europe and North America.Although palynology does not support the Rhaetian concept based on the occurrence of the species Choristoceras marshi exclusively, the traditional ammonoid-based Triassic—Jurassic boundary can be palynologically recognized.     

Environmental change and marsupial assemblages in Holocene successions of Southern Brazil

In the last few years, studies about climate successions in Rio Grande do Sul State (southern Brazil) during the Quaternary increased significantly, mostly due to palynological studies. The knowledge about Quaternary small mammals from Rio Grande do Sul is very poor. However, among the results obtained by archeological research there is an interesting collection of small mammals exhumated from rock shelter deposits. Here we describe the marsupial fauna found in two sites: Garivaldino and Sangão. Both sites are located at the boundary between two large Neotropical subregions, Chaco and Parana. Sediments from these two sites are from the early, middle, and part of the late Holocene. Additionally, we discuss paleobiogeographic, paleoenvironmental, and paleoclimatic aspects, on the basis of the seven taxa recorded: Gracilinanus microtarsus, G. agilis, Monodelphis americana, Thylamys velutinus, Thylamys cf. T. velutinus, Philander opossum, and Didelphis sp. Paleoenvironmental aspects inferred for both sites are consistent: the emergence of typical elements of the current Parana biogeographic subregion was probably established by the end of the early Holocene or the beginning of the middle Holocene. Conclusions are also coherent with the results previously obtained from palynological sequences in these same localities. The micro-marsupials sequence suggests that the environmental changes were not abrupt but gradual during the Holocene in Rio Grande do Sul State.     

Spatial and temporal variation in species composition of dung beetle assemblages in southern Ireland

Abstract. 1. This study attempts to identify the main community characteristics that contribute to variability in dung beetle assemblage composition and structure across a range of spatial and temporal scales.
2. Dung beetle assemblages ( Aphodius , Sphaeridium, and Geotrupes species) were monitored by dung-baited pitfall trapping at 10-day intervals during the seasonally active period at eleven sites in southern Ireland. Three of the sites were monitored over at least 2 years between 1991 and 1996.
3. Although the species composition of the above taxonomic groups was comparable among sites and years, relative abundances of component species varied considerably. Detrended correspondence analysis ordinations indicated a similar level of variability in dung beetle assemblage structure among years, and among sites ≈1–180 km apart.
4. Processes that may contribute to spatio-temporal variability in dung beetle assemblages are discussed, and strategies for future research are suggested.     

Aspects of late triassic palynology. 1. On the morphology,taxonomy and stratigraphical/geographical distribution of the form genus Ovalipollis

Morphological and taxonomic problems related to the form genus Ovalipollis are discussed in some detail. A reconsideration has led to an emended generic diagnosis emphasizing the presence of two lateral tenuitates.Because of the continuous variation in different morphological features a broad species concept seems to be justified. It is considered at present that only one species can be readily distinguished, viz. Ovalipollis pseudoalatus (Thiergart, 1949) Schuurman nov. comb. The known distribution of Ovalipollis in its present concept is confined to the uppermost Middle Triassic—Lower Lias of North America, Europe, North Africa and theMiddlee East.There is evidence of the existence of a progressive, possibly time-proportionate size increase of Ovalipollis.     

The Southern California Twin Register at the University of Southern California.

The Southern California Twin Register is the result of an effort to recruit twins of all ages in the city of Los Angeles and surrounding areas. The register currently includes an ethnically diverse sample of more than 2600 twin pairs. The most recently recruited pairs have been drawn primarily from computerized records of enrollments in local public school districts, and are comparable in sex and ethnic distributions to the general public school population. An ongoing twin study of social and moral development in children, based on 600 pairs of 9-year-old twins from this register, is also described briefly in this paper.     

Taxonomic composition and growth rates of phytoplankton assemblages at the Subtropical Convergence east of New Zealand

Off the eastern coast of New Zealand, warm, saline, nutrient-poorSubtropical Waters (STW) are separated from cool, fresher, relativelynutrient-rich Sub-Antarctic Waters (SAW) by the SubtropicalConvergence (STC). The Chatham Rise, a submarine rise, restrictsthe latitudinal movement of the STC as well as mixing of STWand SAW. Due to this restriction, this sector of the STC ischaracterized by sharp gradients in temperature, macro- (nitrate,silicate and phosphate) and micro- (iron) nutrient concentrations.Shipboard incubations were conducted during austral spring 2000and 2001 to test the hypothesis that these gradients affectthe taxonomic composition and/or growth rates of phytoplanktonon either side of and at the STC. Maximum chlorophyll a concentrationsduring 2000 were 0.39 µg L^–1, but were an orderof magnitude higher in 2001. During both years, STC phytoplanktonwere dominated by diatoms (77% of the total chlorophyll a duringaustral spring 2000 and 70% during spring 2001), whereas cryptophytesand prasinophytes dominated STW assemblages (27 and 36% during2000, and 63 and 17% during 2001). Chlorophyll in the SAW wasdominated by procaryotes and photosynthetic nanoflagellatesduring 2000 (17% procaryotes, 68% nanoflagellates), and by diatomsduring the austral spring 2001 cruise (53%). Growth rates ofthe phytoplankton assemblage were determined by ¹⁴C-labelingof chlorophyll a and photosynthetic pigments. During 2000, temperature-normalizedgrowth rates were near maximal at the STC, and decreased onaverage to less than half of the maximum north and south ofthat front, whereas in 2001 both absolute and relative growthrates were low at all stations. Growth rates did not closelyparallel biomass of the various taxa, suggesting that nutrientlimitation and/or grazing were significantly impacting standingstocks. It appeared that growth was strongly influenced by nutrientsand light, but that biomass was more strongly influenced bygrazing. The STC is a globally important region of enhancedbiomass and productivity; however, the phytoplankton assemblagereflects control by both top–down and bottom–upprocesses that makes a predictive understanding of the area'sbiogeochemical cycles extremely difficult.     

The relationship between early and late radiation damage in rodents' skin.

A study is made of the relationship between early and late damage after irradiation of the feet or ears of rats. In one type of experiment in which large groups of animals were given the same dose, there was a good correlation between the early and late forms of damage. In another experiment, the relationship between these two forms of radiation damage was found to be unaltered by a single dose of X-rays given 8 months earlier. Thus, both types of experiment point to the early and late forms of reaction in the skin of rodents resulting from a common cause. Other relevant experimental data and their relationship to clinical observations are discussed.     

Vegetation history of mid- to western Ireland in the 2nd millennium a.d.; fresh evidence from tephra-dated palynological investigations

The historic Icelandic tephra layers, from Hekla in a.d. 1104 and Öræfajökull in a.d. 1362 that have been found in four peat profiles obtained from lowland and upland mid to western Irish bogs, provide the dating for high-resolution palynological investigations of regional land use over the last thousand years. Marginal agriculture is investigated through the study of an upland blanket peat and a lowland Atlantic blanket peat. At the lowland site, the landscape has been altered, primarily by removal of hazel scrub, while in the uplands, there has been little scrub woodland throughout the last millennium. Pastoral agriculture has a long, unbroken history at both sites, with a short period of arable agriculture, dated to the early 19th century, detected in the uplands. At the two lowland sites, changes in land use associated with medieval monastic and secular activity were similar but not synchronous. The a.d. 1362 tephra in one lowland profile provides high-resolution dating of the palynological evidence for agricultural collapse in the aftermath of the Black Death. The palynological evidence of late medieval woodland clearance is contrasted with the written record. The effects of 19th century population expansion on land use are considered. A synthesis of regional land use in Ireland during the last thousand years is presented.     

Aspects of the epizootiology of pancreas disease in farmed Atlantic salmon Salmo salar in Ireland.

A computerised database containing information on over 17.8 million salmon contained within 49 separate marine populations was used to study the epidemiology of pancreas disease (PD) in Ireland. Of the 43 recorded PD outbreaks, 57% occurred in the 3 mo period August to October inclusive (17 to 32 wk post-transfer). Analysis of variance of mortality rates during PD outbreaks occurring on 6 marine sites over a 5 yr period showed that mortality rates vary significantly between sites (p < 0.001) but not between years over this time period. The mortality rate during PD outbreaks ranged from 0.1 to 63%. Mortality rates were significantly higher when PD outbreaks occurred earlier in the year (y = -1.28x + 59, SE of b 0.33). The mean length of a PD outbreak was 112 d (SE = 7.7, n = 37). There was no correlation between PD mortality rate and smolt input weight, initial stocking density and transfer mortality.     

Aspects of the nitrogen cycle in peatland and plantation forest ecosystems in western Ireland

Extensive plantation forests cover large areas of blanket peatland in western Ireland. Sites are characterised by the ombrotrophic nature of the peat and the often extreme maritime conditions prevailing. The study area is located close to two coastlines and in consequence, ions of marine origin are dominant in the bulk precipitation. Mean annual nitrogen deposition is 2.26 kg ha^-1. Forestry development in the region dates from the early 1950s. Deficiency of phosphorus is universally encountered, sometimes accompanied by a shortage of nitrogen. A fertilizer experiment in the study area was maintained for 16 years. The principal response was to applied phosphorus and although nitrogen had a positive influence on growth in the early years, it was of little consequence in the longer term.Over 900 kg N ha^-1 was accumulated in the forest floor. In a mineralisation study of peat collected from plots fertilized 14 years previously, differences in total mineral nitrogen production between treatments were small, but in nitrogen-treated plots a higher proportion of the mineral nitrogen was as nitrate than in those which had not received fertilizer nitrogen. Throughfall measurements in pole-stage crops of Sitka spruce and lodgepole pine which had received no fertilizer nitrogen, showed significantly greater quantities of nitrogen than bulk precipitation.     

The effect of wrack composition and diversity on macrofaunal assemblages in intertidal marine sediments

Wrack (dead, washed-up seaweed and seagrass) buried in soft substrata may increase the organic content and alter the physical structure of sediments. These effects may influence the composition and structure of macrofaunal assemblages in the sediment. Such influences can be expected to vary according to the type and amount of wrack as well as the presence of invasive seaweeds in the wrack. In this study, we deliberately buried different amounts of the invasive species Sargassum muticum in isolation or mixed to the native species Ulva sp. and Fucus vesiculosus, in two intertidal sandflats to test some hypotheses about the response of macrofaunal assemblages. We tested whether (1) diversity of detritus (i.e. different mixtures), and (2) the amount of detritus of S. muticum influenced the composition and the relative abundance of macrofaunal assemblages. We also assessed whether the sediment organic carbon and the biomass of benthic microalgae varied depending on the diversity of detritus and the amount of detritus of S. muticum. Finally, we tested if these effects of wrack were consistent across sites. Results indicated that buried wrack affected the composition and structure of macrofaunal assemblages in short-term (i.e. 4 weeks), but there were no differences depending on detritus diversity or the amount of S. muticum. In addition, sediment organic matter and microalgal biomass were not affected by the addition of wrack. They instead varied greatly among small spatial scales (i.e. plots). Wrack composition or abundance of the invasive species S. muticum played thus a small role in shaping the structure of macrofaunal assemblages or the biomass of benthic microalgae in these intertidal sediments, probably because these sediments are frequently affected by various inputs of organic matter and benthic assemblages are already adapted to organically enriched sediments.     

The effect of sieve mesh size on the abundance and composition of macrophyte-associated macrofaunal assemblages

Sampling efficiency of several sieve mesh sizes (2, 1, 0.5, 0.2 and 0.1 mm) was tested in invertebrate assemblages associated to Sargassum stenophyllum. Samples of this brown algae were collected in southeastern Brazil to determine whether different sampling devices resulted in differences on the abundance and composition of the macrofauna. The 1 and 2 mm mesh sizes sampled less organisms, resulting in smaller abundances, densities, number of species and diversity, when compared to the other three mesh sizes, that achieved similar results. The most efficient sieve was the 0.5 mm mesh, sampling 85.8% and 94.5% of gammaridean and caprellidean amphipods, respectively, and 93.1% of gastropods. However, polychaetes and isopods were best sampled with the 0.2 mm sieve. Our results suggest that caution should be exercised when deciding on which sieve to use, as mesh sizes commonly used in benthic studies (1 and 0.5 mm) may result in very different estimates of diversity and abundance, as well as community structure patterns. This revised version was published online in July 2006 with corrections to the Cover Date.     

Algae as indicators of a biogeographical zonation in the early carboniferous of the Urals,Siberia and Northeast Russia

Summary Algal assemblages of the Urals and Siberia belong to two biogeographical belts: The equatorial Mediterranean and the Siberian belt. They differ in the composition of their agla floras. The end of the Famennian and the beginning of the tournaisian were indicated by smaller differences due to short-term connections of the basins which lie in different climatic belts. The development of the microfloras of the Urals and Siberias during the late Tournaisian exhibits two different trends. These differences were intensified during the Visean and reached their climax in the Serpukhovian. In general, redalgae, especially Stacheinaceae, were predominant in the late Carboniferous basins of the Urals. The Visean and Serpukhovian algae of Siberia comprising usually more than 20 genera (e.g.Calcifolium, Fasciella, Ungdarella) were widely distributed in the Urals as well as in other provinces of the Mediterranean belt. The biogeographical zonation based on the study of algal floras confirms the existence of an Eurasian realm in the Mediterranean belt and several Siberian provinces as well as an intermediate Taimyr-Chukotkian area, which had already been postulated from earlier foraminiferal studies. All of these provinces exhibit distinct features in the development of their algal associations, e.g. the Kolyma-Omolon province is characterized by its predominance of green algae, while in the Altai-Sayan and the Verkhoyansk provinces red algae prevail. These characteristic trends can be observed over rather long stretches of time.