八臂仙母虫(Eoandromeda octobrachiata)新材料及其意义

在中国贵州江口地区陡山沱组新发现的化石材料表明,伊迪卡拉/震旦纪(Ediacaran/Sinian)的宏体化石——八臂仙母虫Eoandromeda octobrachiata的原始生活状态可能为一个较高的圆锥形生命体,具有沿着侧面锥状螺旋排列的八条旋臂.旋臂表面保存有与栉水母动物的栉板可能同源的横向有机质条带,规则排列...     

Investigative approaches to determine exchange processes in the hyporheic zone of a low permeability riverbank

The hydraulic and hydrochemical interactions of surface water and groundwater in the riverbank of an alluvial stream in the Grand Duchy of Luxembourg were investigated. Hydraulic conductivity in the riverbank is low and the aquifer is confined. Gauged surface-water levels and groundwater levels were recorded over several months to observe potential effluent and influent aquifer conditions. Water samples were taken under different hydraulic conditions in the stream and from three observation wells in the riverbank. Samples were analysed for inorganic parameters and selected dissolved pharmaceuticals. The recorded groundwater levels in the riverbank responded almost without delay to changes in stream stage, which is very dynamic. Frequent changes from effluent to influent aquifer conditions were observed. The analyses for selected ions and pharmaceuticals support the assumption that the pharmaceutical compounds enter the riverbank via the stream only. The chosen trace organics are therefore suitable as anthropogenic tracers for groundwater and surface-water interactions at this field site. They prove that water exchanges also take place in riverbanks even where the hydraulic conductivity is low and for this reason indicate the existence of a hyporheic zone in the investigated section of the stream.     

Exhumation and uplift of the Sierras Pampeanas: preliminary implications from K–Ar fault gouge dating and low-T thermochronology in the Sierra de Comechingones (Argentina)

The Sierras Pampeanas in central and north-western Argentina constitute a distinct morphotectonic feature between 27°S and 33°S. The last stage of uplift and deformation in this area are interpreted to be closely related to the Andean flat-slab subduction of the Nazca plate beneath the South American plate. K–Ar fault gouge dating and low-temperature thermochronology along two transects within the Sierra de Comechingones reveal a minimum age for the onset of brittle deformation about 340 Ma, very low exhumation rates since Late Paleozoic time, as well as a total exhumation of about 2.3 km since the Late Cretaceous. New Ar–Ar ages (7.54–1.91 Ma) of volcanic rocks from the San Luis volcanic belt support the eastward propagation of the flat-slab magmatic front, confirming the onset of flat-slab related deformation in this region at 11.2 Ma. Although low-temperature thermochronology does not clearly constrain the signal of the Andean uplift, it is understood that the current structural relief related to the Comechingones range has been achieved after the exhumation of both fault walls (circa 80–70 Ma).     

Short-term distributional consequences of climate change impacts on the power sector: who gains and who loses?

Climate change tends to negatively affect the power sector, inter alia, by causing cooling problems in power plants and impairing the water supply required for hydropower generation. In the future, when global warming is expected to increase, autonomous adaptation to climate change via international electricity markets inducing reallocations of power generation may not be sufficient to prevent supply disruptions anymore. Furthermore, the consequent changes of supply patterns and electricity prices might cause an undesirable redistribution of wealth both between individual power suppliers and between suppliers and consumers. This study ascertains changes in European power supply patterns and electricity prices caused by on-going global warming as well as the associated redistribution of wealth for different climate change scenarios. The focus of the analysis is on short-term effects. Our results confirm that autonomous adaptation in the power sector should be complemented by planned public adaptation in order to preserve energy security and to prevent undesired distributional effects.     

The impact of discharge change on physical instream habitats and its response to river morphology

The impact of climate-induced discharge change on fish habitats, based on 1951–2008 time series, was investigated within the crystalline catchment of the Grosse Mühl River in Northern Austria. A significant trend change of air temperature, based on Mann–Whitney statistical testing, was recorded for spring 1989 (P?=?98.9 %) and summer 1990 (P?=?99.9 %). This led to a pronounced increase in summer low flow periods. Hydrodynamic-numerical (one-dimensional/two-dimensional) modelling was applied to simulate the changing habitat characteristics due to decreasing discharge in relation to various morphological patterns (riffle-pool/plane-bed reaches). Using bathymetric data, which were sampled on cross sectional measurements, we clearly determined that plane-bed reaches (featureless bed forms) are sensitive to climate-related, reduced discharge, whereas riffle-pool reaches continued to exhibit suitable physical fish habitats even under extreme low-flow conditions. The impact of the decreased summer discharge on instream habitats was strong for subadult and adult grayling which have been used as target fish species. In situ measurements in microhabitats (velocity/depth) revealed habitat suitabilities. These values were taken as biotic input for habitat evaluation on the micro scale. The findings clearly show that river morphology is a decisive parameter in terms of habitat preservation and restoration in the context of the future impacts of climate change (decreased discharge).     

Vulnerability of solar energy infrastructure and output to climate change

This paper reviews the potential vulnerability of solar energy systems to future extreme event risks as a consequence of climate change. We describe the three main technologies likely to be used to harness sunlight—thermal heating, photovoltaic (PV), and concentrating solar power (CSP)—and identify critical climate vulnerabilities for each one. We then compare these vulnerabilities with assessments of future changes in mean conditions and extreme event risk levels. We do not identify any vulnerabilities severe enough to halt development of any of the technologies mentioned, although we do find a potential value in exploring options for making PV cells more heat-resilient and for improving the design of cooling systems for CSP.     

The monsoonal regimes of upper‐hydrospheric structure in the tropical Indian Ocean

Abstract

In response to the alternations between the boreal summer Southwest and the winter Northeast monsoons, the upper‐hydrospheric structure of the tropical Indian Ocean experiences drastic seasonal changes. All year‐round the zone 10–20°S is characterized by a thick and deep thermocline and a ridge in ocean surface topography, while at 0–10°S a tongue protruding from the African coast eastward features a thin and shallow thermocline and a trough in the ocean surface. The trough and ridge mark the equatorial and polar boundaries of the South Equatorial Current. The eastward depression of isotherms and the rise of the ocean surface along the equator are most pronounced around May‐June and November‐December, or lagging somewhat behind the jet‐like surface currents, which are forced by the strong westerly winds sweeping the equatorial zone during limited intervals of the monsoon transitions. Monsoonal changes are particularly dramatic in the northwestern Indian Ocean. From June to August, the thermocline rises and surface waters cool off the coasts of Somalia and Arabia, while in the south‐central Arabian Sea isothermal surfaces bulge downward and the thermocline deepens, with two different centres that appear related to the well known pair of whirls in the surface circulation. During the boreal summer Southwest monsoon, relatively fresh waters appear off the coasts of Somalia and Arabia, further reflecting coastal upwelling; by contrast, downwelling in the central Arabian Sea is accompanied by a core of relatively saline waters. Salinity is overall smallest in the rainfall‐abundant Southeast Asian waters and the Bay of Bengal and large in the desertic regions of the Red Sea and the Persian Gulf. Particularly prominent is a tongue of relatively fresh waters centred somewhat to the south of 10°S extending from the Timor Sea towards the western Indian Ocean and reflecting intrusion from the Southeast Asian seas and the Western Pacific.     

Evidence for accretion disc reprocessing in QSO 0957+561

We use archival g - and r -band photometry of the gravitational lens system QSO 0957+561A, B to estimate the intrinsic variability of the quasar during 1996 February–June. The light curves span 234 d with temporal resolutions of about 2.5 d. Both light curves display a single large-amplitude event, of ∼0.1 mag (max-to-min) in about 100 d, followed by small-amplitude variations of ∼0.02 mag on time-scales of tens of days. We find the r -band variations lag those at g by 3.4_−1.4^+1.5 d for the large-amplitude event. This lag is greater than zero at no less than 98 per cent confidence. The delayed coupling of the rest-frame UV intrinsic variations strongly suggests the existence of a stratified reprocessing region extending ∼light-days from the putative central black hole source. The observed lag is consistent with that expected from a reverberation within an irradiated accretion disc structure. However, any definitive statement requires further detailed theoretical modelling and high-quality, signal-to-noise ratio of about 100, optical/IR simultaneous monitoring with about 3-d resolution for approximately 6 months.     

UV and optical spectral properties in early-type galaxies

We investigate UV and optical spectra of a sample of nearby early-type galaxies with evidence of nuclear line emission. The spectral signatures of various contributors to the UV, such as the interstellar medium and various stellar populations are analyzed and compared with the optical spectral properties. We discuss the impact of these effects on the observational properties of galaxy evolution. This revised version was published online in August 2006 with corrections to the Cover Date.     

Hemispheric Imaging of Galactic Neutral Hydrogen with a Phased Array Antenna System

The thousand element array (THEA) system is a phased array system consisting of 1 m² tiles having 64 Vivaldi elements each, arranged on a regular 8-by-8 grid, which has been developed as a demonstrator of technology and applicability for SKA. In this paper we present imaging results of Galactic neutral hydrogen with THEA. Measurements have been taken using a dense 2-by-2 array of four tiles as a four tile adder. The results are compared with results from the Leiden-Dwingeloo Survey, showing qualitative agreement, but also indicating that further studies are needed on the instrumental characteristics.