Landscape history,calcareous fen development and historical events in the Slovak Eastern Carpathians

We explored interactions among human activities, landscape development and changes in biotic proxies in two small calcareous spring fens in the Slovak Eastern Carpathians. These date back to cal. a.d. 930. Results of pollen, plant macrofossil, and mollusc analyses were compared with the settlement history. The regional pollen record reflected historical events and changes in the settlement density very well at both study sites. The natural mixed fir-beech-spruce forests with fern undergrowth were suppressed and replaced by light-demanding trees in the periods of high human impact (e.g. Wallachian colonization). The study area was affected several times by wars and raids followed by a consequent decline in the settlement density. Some of these events are well reflected in the pollen records that document tree recovery and decline of cereals, weeds, and pasture indicators. In comparison, only some landscape changes were reflected in the local fen development. Both spring fens originated after deforestation, Ro?kovce around a.d. 1347 and Mirol'a around a.d. 929. The most pronounced change involving the water regime stabilization and undisturbed development of plant and mollusc communities took place after the decline in human impact. We conclude that humans were the main drivers of landscape transformation in the last millennium; they directly created spring-fen ecosystems through deforestation and influenced fen species composition through husbandry activities.     

Occurrence of Giant Borings of Osprioneides kampto in the Lower Silurian (Sheinwoodian) Stromatoporoids of Saaremaa,Estonia

The distribution of Osprioneides is more environmentally limited than that of Trypanites in the Silurian of Baltica. Osprioneides probably occurred only in large hard substrates of relatively deepwater muddy bottom open shelf environments. Osprioneides were relatively rare, occurring in 4.7% of all stromatoporoid specimens in that environment, in contrast to small Trypanites-Palaeosabella borings, which occur in 88.4% of stromatoporoids and 88.9% of heliolitid corals. Osprioneides is reported only from the lower Sheinwoodian stromatoporoids of the exposed Silurian of Saaremaa (Wenlock to Pridoli). Osprioneides borings probably played a minor role in the general bioerosion in the Silurian of Baltica.     

Influence of management on the seed production and seed bank of calcareous fen species

Abstract. The dynamics of the seed production and seed bank of two dominant perennial species of calcareous fens were investigated in response to different mowing frequency, fallow or pasture. The production of fertile shoots responded strongly to management practices. On sites where mowing alternated with fallow, autumn mowing led to an increase of fertile shoot density in Schoenus ferrugineus and a decrease in Molinia caerulea in the subsequent season. Repeated annual mowing after long-term fallow raised the density in Schoenus and inhibited initiation of flowering shoots in Molinia. Seed set and viability were influenced mainly by climatic or other factors. Variation of seed production between sites and in consecutive years at the same site could thus be large. The relationship between total seed production and seed bank was weak, but it improved when germination rates were included in the calculation. As the seed bank was generally smaller than the viable seed production, low survival and a high turnover of seeds in the upper soil layers is assumed for both species. Implications for recruitment strategies are discussed.     

A palaeoecological approach to the last 21 000 years in the pyrenees: The peat bog of Freychinede (alt. 1350 m, Ariege, South France)

Local palaeoclimatic and palaeoecological reconstructions in the Ariège Pyrenees were applied to palynological and sedimentological investigations of the Freychinède peat bog (alt. 1350 m), complemented by a geomorphological study of the neighbouring area. Correlations are possible between local glacial evolution, deposition in the lake and the history of the vegetational cover for the period from about 21 300 B.P. to 13 000 B.P. The altitude of the cirque floors indicates mean July temperatures probably ranging between 6.5°C and 8.5°C from 21 300 B.P. to 15 000 B.P.; 7°C and 9°C from 15 000 B.P. to 13 150 B.P.; 7.5°C and 9.5°C from 13 150 B.P. to the beginning of the final transitional phase.

Based on the comparison of the palynological data with the modern plant communities of the area, especially with the subalpine and alpine communities, the local climate would have been favourable to the development of Boreo-arctic plants at the altitude of the lake during the cold phase.

The Postglacial period begins near 10 650 B.P. with the extension of Quercus. Abies spread at about 7000 B.P. followed by Tilia cordata. From 5000 to 3900 B.P., Fagus spread moderately, but its strongest development occurred after about 3900-3800 B.P., when human activity began on the mountain forest and many beech—fir forests developed. Middle Ages, in many valleys of Ariège, the mountain and subalpine forests were destroyed. The modern landscape has large treeless zones with scattered recent populations of beech where fir is beginning to develop.     

The age of the Kaali meteorite craters and the effect of the impact on the environment and man: evidence from inside the Kaali craters,island of Saaremaa,Estonia

The Kaali meteorite impact crater field, which consists of a 110 m diameter main crater and eight satellite craters on the island of Saaremaa, Estonia is a unique object as its meteoritic origin is well proven, it lies in a densely populated area and fell in the relatively recent past. The precise age of the impact that generated the craters is still disputed. We investigated the basal sediment section from the main crater lake, Kaali järv, consisting of crushed and in-washed dolomite diamiction. AMS dating of terrestrial macrofossils from these sediment layers places the age of the impact at 1690–1510 B.C. The age is about 1000 years older than revealed from the impact marker-horizon in a contemporaneous peat sequence 6 km northwest of the Kaali crater. The pollen, diatom and chemical data suggest the instant formation of a shallow hard-water lake environment in the main crater depression after the impact, and a rapid post-impact sedimentation of crushed dolomite dust. Archaeological evidence on the crater slopes points to human activity around 700–200 B.C., indicating that the crater ring wall was inhabited by Bronze Age people soon after the impact event, and the structure of the main crater is mimicked in nearby archaeological sites.

Solar ultraviolet-B radiation influence on Sphagnum bog and Carex fen ecosystems: first field season findings in Tierra del Fuego, Argentina

Stratospheric ozone depletion occurs over Tierra del Fuego, southern Argentina and Chile, in the austral spring and summer due to the precession of the Antarctic ‘ozone hole’ and the general erosion of the ozone layer. Plots receiving either near-ambient or reduced UV-B radiation were established using different louvered plastic film filters over Sphagnum bog and Carex fen ecosystems in October 1996. In the Sphagnum bog system, growth measurements during the late spring and summer showed no significant differences in the moss Sphagnum magellanicum, or the vascular plants (Empetrum rubrum, Nothofagus antarctica, and Tetroncium magellanicum) between near-ambient and attenuated UV-B radiation treatments. In the Carex fen system, leaf length and spike height did not differ in the two dominant species, Carex decidua and C. curta, between UV-B radiation treatments. The length of individual spikelets of C. curta under near-ambient UV-B radiation was less than under the reduced UV-B radiation treatment, but this was not evident in C. decidua. No differences in seed number, seed mass, or viability were seen in either Carex species between the UV-B treatments. Two important constituents of the microfauna that inhabit the Sphagnum bog are testate amoebae and rotifers. These both appeared to be more numerous under near-ambient UV-B radiation than under reduced UV-B radiation. The subtle responses of the Sphagnum and Carex ecosystems may become more apparent in subsequent years as the treatments are continued. Trophic-level changes, such as the differences in number of amoebae and rotifers, may be more sensitive to solar UV-B radiation than growth and productivity of the vegetation.     

Holocene development of two calcareous spring fens at the Carpathian-Pannonian interface controlled by climate and human impact

There is still not enough palaeoecological data from the southwestern part of the Western Carpathians, where mountain ridges steeply rise from the dry and warm Pannonian basin. The reason is a low availability of sites with sediments harbouring fossil remains. In the Pova?ský Inovec Mts, two small protected calcareous wetlands occur in different geographical position and contain suitable sediments. One represents a foothill site (initiated ca 13,000 cal. BP) whereas the other a low-mountain site (initiated ca 7,400 cal. BP). We investigated fossil pollen, spores, and macroscopic remains of plants and molluscs from their sediments. We further reviewed archaeological data, constructed a macrophysical climate model (MCM) and confronted it with other palaeoclimatic proxies. Temperate deciduous trees (Quercus, Corylus and Ulmus) occurred since the Allerød, but their expansion was blocked by a harsh climate in Younger Dryas, when Larix, Pinus and Betula nana still occurred. The climate firstly moistened at ca 9,500 cal. BP and more distinctly at ca 8,500 cal. BP, which was reflected by a strong calcium carbonate precipitation and expansion of Tilia cordata t., Hedera helix, and Ustulina. Although the MCM predicted a rather stable climate since 8,000 cal. BP, certain changes in aquatic mollusc abundances may indicate hydrological fluctuations, as they are paralleled by changes in climate humidity indicated by other evidence from the Western Carpathians. Younger hydrological fluctuations may be alternatively explained by human activities as they correspond with macro-charcoal abundance and indicators of wetland openness. During their existence, both fens harboured only few fen plant and mollusc species specialized to low-productive sedge-moss fens. In the Middle Holocene both sites were encroached by woody plants (Alnus, Picea and Salix), as most other spring fens in the Western Carpathians. Contrary to some other spring fens with similar site conditions in the Western Carpathians, few fen specialists established in the study sites since deforestation, presumably because of severe disturbances caused by grazing and/or hemp retting instead of the usual mowing.     

Microbial community structure and activity linked to contrasting biogeochemical gradients in bog and fen environments of the glacial lake agassiz peatland

The abundances, compositions, and activities of microbial communities were investigated at bog and fen sites in the Glacial Lake Agassiz Peatland of northwestern Minnesota. These sites contrast in the reactivity of dissolved organic matter (DOM) and the presence or absence of groundwater inputs. Microbial community composition was characterized using pyrosequencing and clone library construction of phylogenetic marker genes. Microbial distribution patterns were linked to pH, concentrations of dissolved organic carbon and nitrogen, C/N ratios, optical properties of DOM, and activities of laccase and peroxidase enzymes. Both bacterial and archaeal richness and rRNA gene abundance were >2 times higher on average in the fen than in the bog, in agreement with a higher pH, labile DOM content, and enhanced enzyme activities in the fen. Fungi were equivalent to an average of 1.4% of total prokaryotes in gene abundance assayed by quantitative PCR. Results revealed statistically distinct spatial patterns between bacterial and fungal communities. Fungal distribution did not covary with pH and DOM optical properties and was vertically stratified, with a prevalence of Ascomycota and Basidiomycota near the surface and much higher representation of Zygomycota in the subsurface. In contrast, bacterial community composition largely varied between environments, with the bog dominated by Acidobacteria (61% of total sequences), while the Firmicutes (52%) dominated in the fen. Acetoclastic Methanosarcinales showed a much higher relative abundance in the bog, in contrast to the dominance of diverse hydrogenotrophic methanogens in the fen. This is the first quantitative and compositional analysis of three microbial domains in peatlands and demonstrates that the microbial abundance, diversity, and activity parallel with the pronounced differences in environmental variables between bog and fen sites.     

Relations between suspended bacteria, epiphytic bacteria and submerged vegetation over the spring growing season in a calcareous headstream

SUMMARY. 1. Quantitative observations on suspended bacteria, epiphytic bacteria and submerged vegetation, in a calcareous headstream in North Humberside, were made at regular intervals from January to June 1984.
2. Downstream increase in concentration of suspended bacteria was observed along a 135 m richly-vegetated section but not over a 150 m vegetation-free section, hence there was measurable drift loss of bacteria only from within the vegetated section.
3. The total number of epiphytic bacteria within the vegetated section was estimated from the density of epiphytic bacteria per unit dry weight of submerged vegetation and the total dry weight of submerged vegetation.
4. The total number of epiphytic baeteria within the vegetated section decreased frtim 2.5 × 10¹⁵ in January to 0.8 × l0¹⁵ March before increasing to 4.7 × 10¹⁵ by June. This pattern was related to deerease and subsequent increase in density of epiphytic bacteria per unit dry weight of vegetation. The total dry weight of submerged vegetation inereased throughout the study period.
5. The daily drift loss of bacteria from the vegetated section averaged 53% (range 9–132%) of the total epiphytic bacteria, a loss rate which might reasonably be supported by the epiphyte population.
6. The dimensions and volume of suspended bacteria increased, between the source and the downstream limit of the vegetated section, to resemble those of epiphytic bacteria.
7. The results suggested that released epiphytic bacteria might largely be the source of suspended bacteria in this headstream.     

From synapses to behavior: development of a sensory-motor circuit in the leech

The development of neuronal circuits has been advanced greatly by the use of imaging techniques that reveal the activity of neurons during the period when they are constructing synapses and forming circuits. This review focuses on experiments performed in leech embryos to characterize the development of a neuronal circuit that produces a simple segmental behavior called "local bending." The experiments combined electrophysiology, anatomy, and FRET-based voltage-sensitive dyes (VSDs). The VSDs offered two major advantages in these experiments: they allowed us to record simultaneously the activity of many neurons, and unlike other imaging techniques, they revealed inhibition as well as excitation. The results indicated that connections within the circuit are formed in a predictable sequence: initially neurons in the circuit are connected by electrical synapses, forming a network that itself generates an embryonic behavior and prefigures the adult circuit; later chemical synapses, including inhibitory connections, appear, "sculpting" the circuit to generate a different, mature behavior. In this developmental process, some of the electrical connections are completely replaced by chemical synapses, others are maintained into adulthood, and still others persist and share their targets with chemical synaptic connections.     

Effects of short-term drying and irrigation on CO2 and CH4 production and emission from mesocosms of a northern bog and an alpine fen

Atmospheric CO₂ and CH₄ exchange in peatlands is controlled by water table levels and soil moisture, but impacts of short periods of dryness and rainfall are poorly known. We conducted drying-rewetting experiments with mesocosms from an ombrotrophic northern bog and an alpine, minerotrophic fen. Efflux of CO₂ and CH₄ was measured using static chambers and turnover and diffusion rates were calculated from depth profiles of gas concentrations. Due to a much lower macroporosity in the fen compared to the bog peat, water table fluctuated more strongly when irrigation was stopped and resumed, about 11 cm in the fen and 5 cm in the bog peat. Small changes in air filled porosity caused CO₂ and CH₄ concentrations in the fen peat to be insensitive to changes in water table position. CO₂ emission was by a factor of 5 higher in the fen than in the bog mesocosms and changed little with water table position in both peats. This was probably caused by the importance of the uppermost, permanently unsaturated zone for auto- and heterotrophic CO₂ production, and a decoupling of air filled porosity from water table position. CH₄ emission was <0.4 mmol m^?2 day^?1 in the bog peat, and up to >12.6 mmol m^?2 day^?1 in the fen peat, where it was lowered by water table fluctuations. CH₄ production was limited to the saturated zone in the bog peat but proceeded in the capillary fringe of the fen peat. Water table drawdown partly led to inhibition of methanogenesis in the newly unsaturated zone, but CH₄ production appeared to continue after irrigation without time-lag. The identified effects of irrigation on soil moisture and respiration highlight the importance of peat physical properties for respiratory dynamics; but the atmospheric carbon exchange was fairly insensitive to the small-scale fluctuations induced.     

New data on the exoskeleton of the osteostracan genus Aestiaspis (Agnatha) from the Silurian of Saaremaa Island (Estonia) and the Severnaya Zemlya Archipelago (Russia)

The histological structure of exoskeleton of the osteostracan genus Aestiaspis Janvier et Lelievre, 1994 from the Silurian of Saaremaa Island is examined for the first time. The preservation of the material enables the fine exoskeleton structure to be described in detail. The study of Aestiaspis from Saaremaa Island and the Severnaya Zemlya Archipelago has shown structural details of exoskeleton sculpture. The formation of consolidated cephalothoracic shield in the phylogeny of Tremataspidoidei is discussed. The taxonomic position of the genus Aestiaspis in the Osteostraci system is analyzed.     

Vegetation development at a mountain settlement site in the Swedish Scandes during the late Holocene: palaeoecological evidence of human-induced deforestation

A palaeoecological study was conducted close to the forest limit in the northern Scandinavian mountain range. The aim was to elucidate the degree to which human impact has affected the vegetation at Hiednikvalta, a Stállo settlement site. Stállo settlements consist of round hut foundations that have a hearth in the middle and are surrounded by a low turf wall. They were probably established by Sámi people using the mountain areas for hunting and/or reindeer herding. In order to separate the effects of humans and climate on the vegetation, a reference area approach was adopted, i.e. the vegetation development at the Stállo settlement site Hiednikvalta was compared with the vegetation development in a forested reference area Avvuhatjåhkkå, at the same altitude as Hiednikvalta but with no archaeological remains of settlements. Peat stratigraphies were retrieved at the two sites and pollen analysis, loss-on-ignition (LOI), pollen accumulation rates (PAR), macrofossil analysis and Betula pollen size statistics were all examined. The results indicate that Hiednikvalta was forested with Betula trees prior to the Stállo settlement period, which occurred between the eighth and thirteenth centuries. Human activities resulted in a decrease in tree cover at the site, as found in a previous study at Adamvalta, another Stállo settlement site in the region. However, the magnitude of vegetation change, and the post-Stállo vegetation development differed between the two areas, suggesting that site-specific factors are important. The use of reference areas in palynological studies is also discussed.     

A palaeoecological study of holocene peat bog sections in Germany and The Netherlands,based on the analysis of pollen,spores and macro- and microscopic remains of fungi,algae, cormophytes and animals

A Holocene peat section of the Engbertsdijksveen (The Netherlands) was analysed at centrimetre intervals for all kinds of micro- and macrofossils in order to obtain maximum information regarding local vegetation and animal succession and regional changes in the prevailing vegetation types. The analysed micro- and macrofossils are illustrated, described and interpreted. Among them are about 70 fungal taxa, about 25 animal taxa, at least 4 algae, and about 15 fossils of unknown identity or origin.The taxonomic designation, matrix, host- or substrate specificity and indicator value of representatives of five different groups of fossils have been tabulated.The fruit-bodies of several taxa distinguished as spore types were found during the macrofossil analysis, e.g., ascospores, mycelium and fruit-bodies of the parasite Meliola cf. niessleana (Type 14) are present in the levels in which Calluna vulgaris played a role in the local vegetation.The ascomycete Geoglossum sphagnophilum was, according to its spore distribution, a common element in the bog vegetation during the Atlantic and Subboreal periods.Zygospores of Mougeotia cf. gracillima (Type 61) and other Zygnemataceae indicate the levels where these algae could grow during the local succession in the peat bog. The zygospores indicate phases of shallow, stagnant, mesotrophic open water during spring.Conventional analysis of pollen and macro-remains with a high resolution in time (centimetre diagrams), the above-mentioned new information, and the correlation of events inside and outside the site of the peat bog lead to the following main conclusions:The Atlantic-Subboreal transition, well known for its elm decline, could be correlated with a local change in bog vegetation. Following the alteration of wet Scheuchzeria palustris vegetation with hummock vegetation in the Atlantic period, the appearance of a Molinia coerulea peat coincides with the elm decline. According to the present ecology of M. coerulea, this change must have been caused by a seasonally recurring, considerable lowering of the groundwater level during summer. During winter the groundwater rose so far that in spring shallow open water prevailed and Mougeotia cf. gracillima could develop. This local vegetational succession indicates an unstable climatic period with pronounced dry seasons during the early Subboreal.During the climatic deterioration of the Subboreal-Subatlantic transition the incidence of Corylus avellana decreased. The Corylus pollen curve shows several cyclic fluctuations during this period (1400-600 B.C.). Depressions in the Corylus pollen curve correspond with particularly wet local vegetation (more oceanic, possibly cooler phases), Corylus pollen maxima correspond with relatively dry bog vegetation (less oceanic, possibly warmer phases). These cyclic fluctuations correspond to approximately 150–200 historical years each. The increasing oceanicity ultimately resulted in the formation of peat by Sphagnum species of the section Cymbifolia. In this Subatlantic Cymbifolia peat the fluctuations of the minor constituent Sphagnum cf. rubellum are clearly correlated with the fluctuations of the curve of the rhizopod Amphitrema flavum. This phenomenon is interpreted as a reflection of more and less oceanic phases during the Subatlantic period.All available data were expressed in curves, in order to indicate changes in local and perhaps regional moisture conditions.Ther percentages of plants indicating human influence are relatively low during the Neolithic and Bronze Age. During the Iron Age the influence of prehistoric man was relatively important. Secale cereale was already grown during the secondary century B.C. Population density decreased again during the second century A.D.The present study is intended as a first step towards a more detailed knowledge of the changing ecosystems of bogs and forests and in their response to changing environmental factors, such as minor and major climatic cycles.     

Seropositivity to Helicobacter pylori heat shock protein 60 is strongly associated with intensity of chronic inflammation, particularly in antrum mucosa: an extension of an 18-year follow-up study of chronic gastritis in Saaremaa, Estonia

Helicobacter pylori is a cause of chronic gastritis and leads to development of atrophy in some cases. There is evidence that the heat shock protein 60 (HSP60) of H. pylori is involved in induction of chronic inflammation. Seroprevalence of IgG antibodies to H. pylori HSP60 in an adult cohort from Saaremaa, Estonia (68 persons, median age 57 years), with a high prevalence of antibodies to cell surface proteins of H. pylori (92%) and a well characterized dynamics of chronic gastritis in an 18-year follow-up study, was tested using purified H. pylori HSP60 at a concentration of 1 microg ml(-1) with ELISA. The state of the gastric mucosa and the presence of H. pylori in histological sections in the samples of 1979 and 1997 were assessed in accordance with the Sydney system. Seropositivity for H. pylori HSP60 was 65%. Immunological response to H. pylori HSP60 is associated with the morphological presence of H. pylori in the antrum and corpus (P=0.01) and is strongly correlated with the grade of chronic inflammation, particularly in the antrum mucosa (r=0.34; P=0.003; OR=5.97 (95% CI 1.21-29.3)), but is not associated with development of atrophy during 18 years of follow-up, or with the activity of gastritis. This finding supports the evidence that immunological response to H. pylori HSP60 may play a role in triggering of the inflammatory process in the gastric mucosa.     

Sex,gender, and pharmaceutical politics: From drug development to marketing

Background: Biological sex differences and sociocultural gender norms affect the provision of health care products and services, but there has been little explicit analysis of the impact of sex differences and gender norms on the regulation of pharmaceutical development and marketing.Objectives: This article provides an overview of the regulation of pharmaceuticals and examines the ways that regulatory agencies account for sex and gender in their review of scientific data and marketing materials.Methods: The primary focus is on the US context, but information is also included about regulatory models in Europe, Canada, and Japan for comparative purposes. Specific examples show how sex differences and gender norms influence scientific and policy decisions about pharmaceuticals.Results: The United States and Canada were found to be the only countries that have explicit requirements to include women in clinical trials and to perform sex-based subgroup analysis on study results. The potential influence of politics on regulatory decisions may have led to an uneven application of standards, as seen through the examples of mifepristone (for abortion) and sildenafil citrate (for erectile dysfunction). Three detailed case studies illustrate the importance of considering sex and gender in pharmaceutical development and marketing: Phase I clinical trials; human papillomavirus quadrivalent vaccine; and tegaserod, a drug for irritable bowel syndrome.Conclusions: Sex and gender play important roles in pharmaceutical regulation, from the design of clinical trials and the approval of new drugs to advertising and postmarketing surveillance. However, regulatory agencies pay insufficient attention to both biological sex differences and sociocultural gender norms. This disregard perpetuates inequalities by ignoring drug safety problems that predominate in women and by allowing misleading drug marketing that reinforces gender stereotypes. Recommendations have been made to improve the regulation of pharmaceuticals in regard to sex and gender.