Land–sea correlations in the Australian region: 460 ka of changes recorded in a deep-sea core offshore Tasmania. Part 2: the marine compared with the terrestrial record     

P. De Deckker  T. T. Barrows  J.-B. W. Stuut  S. van der Kaars  M. A. Ayress  J. Rogers 《Australian Journal of Earth Sciences》2019,66(1):17-36

We present an array of new proxy data and review existing ones from core Fr1/94-GC3 from the East Tasman Plateau. This core is positioned at the southern extreme of the East Australia Current and simultaneously records changes in both oceanography and environments both in offshore and in southeastern Australia. Microfossils, including planktonic and benthic foraminifera, ostracods, coccoliths and radiolarians, were studied to interpret palaeo-oceanographic changes. Sea-surface temperature was estimated using planktonic foraminifera, alkenones and radiolaria. From the silicate sediment fraction, the mean grain size of quartz grains was measured to detect the changes in wind strength. An XRF scan of the entire core was used to determine the elemental composition to identify provenance of the sediment. We also compare these data with a pollen record from the same core provided in an accompanying article that provides the longest well-dated record of vegetation change in southeastern Australia. In an area of slow sedimentation, Fr1/94-GC3 provides a continuous record of change in southeastern Australia and the southern Tasman Sea over approximately the last 460?ka. We determine that the East Australian Current varied in intensity through time and did not reach the core site during glacial periods but was present east of Tasmania during all interglacial periods. The four glacial–interglacial periods recorded at the site vary distinctly in character, with Marine Isotope Stage (MIS) 9 being the warmest and MIS 5 the longest. Through time, glacial periods have progressively become warmer and shorter. Deposition of airborne dust at the core site is more substantial during interglacial periods than glacials and is believed to derive from mainland Australia and not Tasmania. It is likely that the source and direction of the dust plume varied significantly with the wind regimes between glacials and interglacials as mean effective precipitation changed.  相似文献   

Microseismicity but no tremor accompanying slow slip in the Hikurangi subduction zone,New Zealand     

E.J. Delahaye  J. Townend  M.E. Reyners  G. Rogers 《Earth and Planetary Science Letters》2009,277(1-2):21-28

Geodetically-detected episodes of slow slip appear in several subduction zones to be accompanied by bursts of low-frequency coherent noise known as seismic tremor, but whether a single physical process governs this association or even whether slow slip is invariably accompanied by tremor remains unresolved. Detailed analysis of broadband seismic data spanning a slow slip episode in the Hikurangi subduction zone, New Zealand, reveals that slow slip was accompanied by distinct reverse-faulting microearthquakes, rather than tremor. The timing, location, and faulting style of these earthquakes are consistent with stress triggering down-dip of the slow slip patch, either on the subduction interface or just below it. These results indicate that tremor is not ubiquitous during subduction zone slow slip, and that slow slip in subduction zone environments is capable of triggering high-frequency earthquakes near the base of the locked subduction thrust. In this and other locations (Hawaii, Boso Peninsula) where slow slip is accompanied by triggered microseismicity, the estimated upper extent of the slow slip is shallower (less than ~ 20 km) than in those locations from which tremor has been reported. This suggests that ambient temperature- or pressure-dependent factors govern the character of the seismic response to slow slip on subduction thrusts and other large faults, with rheological or lithological conditions at shallow depths triggering high-frequency microearthquakes and those at greater depths triggering seismic tremor.  相似文献   

Substrate influence and temporal changes on periphytic biomass accrual and metabolism in a tropical humic lagoon     

Rafael D. Guariento  Adriano Caliman  Francisco A. Esteves  Reinaldo L. Bozelli  Alex Enrich-Prast  Vinicius F. Farjalla   《Limnologica》2009,39(3):209-218

We performed a field experiment in a tropical humic coastal lagoon to evaluate periphyton biomass accrual and metabolism on three different substrates (1) plastic ribbons, (2) green and (3) senescent leaves of the emergent macrophyte Typha domingensis) over 30 days. The contribution of autotrophic biomass decreased as total biomass increased over the time. Mean periphytic ash free dry weight ranged from 0.8 to 5.6 mg cm⁻², but periphyton chlorophyll a concentrations presented shorter amplitudes, which oscillated from 0.12 to 0.44 μg cm⁻² throughout the experiment. Periphyton metabolism was overall heterotrophic on all substrates, especially on senescent leaves. Our data show that substrate type influenced both biomass accrual and periphyton net productivity and respiration rates throughout periphyton development and highlighted the dominance of heterotrophic metabolism. The periphyton respiration may be subsidized by both water- and substrate-derived allochthonous energy pathways, shedding light on the role of periphytic assemblages to the carbon cycling, as a source of CO₂ to the system.  相似文献   

The Theses on Feuerbach as a political ecology of the possible   总被引：1，自引：0，他引：1  

Alex Loftus 《Area》2009,41(2):157-166

This paper argues that Marx's Theses on Feuerbach offer a tremendous and yet neglected resource for work in political ecology and the production of nature. Whilst not calling for a dramatic shift in the way in which such work is conducted, the paper shows how the Theses offer a firm and concise foundation on which to base the ontological and epistemological claims of work on the politicised environment. Ontologically, nature is a differentiated unity, best understood as sensuous activity or practice. This fits well with Smith's claims that nature is produced, whilst not limiting production to capitalist activity. Environments are thereby made up of everyday activity. Subverting the apparent anthropocentrism of this claim, the paper shows how (as Gramsci recognised) the Theses on Feuerbach have an incipient sense of the socio-natural. Post-humanist critiques of Smith's (humanist) production of nature thesis are thereby disrupted. Production realises a differentiated unity of socio-natural relations. Epistemologically, the paper demonstrates how the Theses push political ecologists to construct knowledge claims from practical activity. An ecological politics thereby emerges from the situated knowledges of different actors. Building on this, the paper argues that Marx's 'notes to himself' give us a sense of possible worlds and possible ecologies beyond the topsy-turvy one we have made in the present. Through the concept of praxis evinced in the Theses , a vision of the engaged scholar activist, committed to learning about the world through changing it (and vice-versa), emerges .  相似文献   

Assessment of a Bayesian Belief Network-GIS framework as a practical tool to support marine planning     

V. Stelzenmüller  J. Lee  S.I. Rogers 《Marine pollution bulletin》2010,60(10):1743-1754

For the UK continental shelf we developed a Bayesian Belief Network-GIS framework to visualise relationships between cumulative human pressures, sensitive marine landscapes and landscape vulnerability, to assess the consequences of potential marine planning objectives, and to map uncertainty-related changes in management measures. Results revealed that the spatial assessment of footprints and intensities of human activities had more influence on landscape vulnerabilities than the type of landscape sensitivity measure used. We addressed questions regarding consequences of potential planning targets, and necessary management measures with spatially-explicit assessment of their consequences. We conclude that the BN-GIS framework is a practical tool allowing for the visualisation of relationships, the spatial assessment of uncertainty related to spatial management scenarios, the engagement of different stakeholder views, and enables a quick update of new spatial data and relationships. Ultimately, such BN-GIS based tools can support the decision-making process used in adaptive marine management.  相似文献   

Corrigendum to ‘‘Seismic damage evaluation in urban areas using a capacity spectrum based method: Application to Barcelona’’ [Soil Dynamics and Earthquake Engineering 28 (10–11) (2008) 851–865]     

Alex H Barbat  Luis G. Pujades  Nieves Lantada  Rosangel Moreno 《Soil Dynamics and Earthquake Engineering》2010

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The COPAS’08 expedition to the Patagonian Shelf: Physical and environmental conditions during the 2008 coccolithophore bloom     

Stuart C. Painter  Alex J. Poulton  John T. Allen  Rosalind Pidcock  William M. Balch 《Continental Shelf Research》2010

Here we present observations of the hydrography of the Patagonian Shelf, shelf break and offshore waters, with reference to the environmental conditions present during the period of peak coccolithophore abundance. Analysis of a hydrographic dataset collected in December 2008 (austral spring/summer), as part of the Coccolithophores of the Patagonian Shelf (COPAS) research cruise, identified 5 distinct surface water masses in the region between 37°S and 55°S. These water masses, identified through salinity gradients, displayed varying mixed layer depths, macronutrient inventories and chlorophyll-a fluorescence. Subantarctic Shelf Water (SSW), located to the north of the Falkland Islands and extending north along the shelf break, was also host to a large coccolithophore bloom. The similarities between the distribution of calcite, as seen in remote sensing data, and SSW indicate that the coccolithophore bloom encountered conditions conducive to bloom development within this water mass. Analysis of chemical and environmental data also collected during the COPAS cruise revealed that many of the commonly cited conditions for coccolithophore bloom development were present within SSW (e.g. low N:P ratio, high N:Si ratio, shallow mixed layer depth). In the other water masses present on the Patagonian Shelf greater variability in these same parameters may explain the more diffuse concentration of calcite, and the smaller size of possible coccolithophore blooms. The distribution of SSW is strongly influenced by the latitudinal variation in shelf break frontal width, which varies from 20 to 200 km, and consequently strong hydrographic controls underlie the position of the coccolithophore bloom during austral summer.  相似文献   

A review of conventional techniques for subsurface characterization of landslides     

J. David Rogers  Jaewon Chung 《Environmental Earth Sciences》2017,76(3):120

Naturally occurring landslides can be difficult to characterize and often exhibit anomalies in controlling geometry and consistency. The characterization of landslides in engineering geology practice is usually based on program of subsurface exploration; focused on identifying subsurface materials, structure and stratigraphy, hydrologic conditions, and appropriate strength parameters. On native slopes bereft of anthropogenic modification (excavation), geomorphic evidence of previous movement and its relative depth and scale are often discernible to the experienced eye. This paper seeks to describe the various techniques that have been successfully employed in site-specific subsurface investigations of prehistoric landslides. These include considerations of limiting geometry (for planning subsurface exploration and sampling), overcoming problems with site access, exploratory trenches, small diameter borings, downhole logging of large diameter borings, and geophysical techniques. These procedures can be combined to develop more realistic cross sections along the vector of maximum landslide movement, so the displaced mass can be realistically analyzed. The respective advantages and disadvantages of these techniques are discussed, with baseline references on subsurface exploration.  相似文献   

Assessment of coastal communities’ vulnerability to floods using indicator-based approach: a case study of Greater Accra Metropolitan Area,Ghana     

Paul William Kojo Yankson  Alex Barimah Owusu  George Owusu  John Boakye-Danquah  Jacob Doku Tetteh 《Natural Hazards》2017,89(2):661-689

Coastal towns along the coast of Africa are among the most vulnerable to climate change impacts such as flooding and sea level rise. Yet, because coastal conditions in many parts of the region are poorly understood, knowledge on which population groups are at the most risk is less known, particularly in the Greater Accra Metropolitan Area (GAMA) of Ghana, where the capital city Accra is located. Without adequate information about the risk levels and why, the implementation of locally appropriate adaptation plans may be less effective. This study enriches our understanding of the levels of flood risks along the coast of GAMA and contributes knowledge to improve understanding of place-specific adaptation plans. The study uses data from a 300-household survey, stakeholder meetings, and interviews with local community leaders to construct an integrated vulnerability index. The index includes seven components made up of: dwelling type; house and house environment; household socioeconomic characteristics; experience and perception of flood risk; household and community flood adaptation strategies; house location, and physical characteristics. Our findings show that exposure to floods, particularly from local flash floods is relatively high in all communities. However, significant differences in sensitivity and adaptive capacity of the communities were observed due to differences in location, socioeconomic characteristics, and perception of risks to flooding and sea level rise. The complexity of factors involved in the determination of local-level vulnerability requires that the implementation of adaptation strategies needs to involve cross-sectorial partnerships, involving local communities, in building a comprehensive multi-risk adaptation strategy.  相似文献   

Kinematics and dynamics of the southeastern margin of the Tibetan Plateau   总被引：4，自引：0，他引：4  

Alex Copley 《Geophysical Journal International》2008,174(3):1081-1100

On the southeastern margin of the Tibetan Plateau lies a large region which seismicity and GPS data show to be actively deforming. This paper describes the active faulting in the region, and how it relates to the velocity field observed with GPS. In places the velocity field is accommodated by rotations about vertical axes, and most or all of the strain at the surface in the region appears to be released seismically. GPS velocities are then compared to velocities calculated using a model for deformation driven by gravitational driving forces. Using rheologies estimated from experimentally derived mineral flow laws, the model provides velocities that are in good agreement with observed GPS velocities. It is not possible to uniquely determine the rheology or flow velocity at depth, and there are two forms of model solution which match the observed horizontal surface velocities. In one of these, vertical planes deform by pure shear, and in the other vertical gradients of horizontal velocity are present within the crust. Two distinct regions of normal-faulting earthquakes are present in the region, and have mechanisms which are most easily explained by gravity-driven deformation.  相似文献