Generation of basaltic magma: H. S. Yoder, 1976, National Academy of Sciences Publishing Office,Washington, DC. US$5.50, 265 pp     

D.H. Green 《Geochimica et cosmochimica acta》1977,41(10):1537

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The role of moral economy in two British Columbia fisheries: Confronting neoliberal policies     

《Marine Policy》2015

What have been the moral values and practices allowing equitable economic opportunities and a sense of fairness in North American small-scale fisheries? How have these “moral economies” been affected by neoliberal policies with their emphasis on efficiency, rational self-interest, and wealth accumulation? Focusing especially on the salmon and halibut fisheries in British Columbia, Canada, this discussion summarizes key findings on the manner in which small-scale fisheries and their moral practices tend to be marginalized and undervalued under neoliberal regimes. The paper considers the value of these moral economies for promoting social, economic, and ecological welfare as grounds for the expansion of small-scale fisheries.  相似文献   

Late Pliocene glaciation and landscape evolution of Vestfirðir,Northwest Iceland     

《Quaternary Science Reviews》2007,26(1-2):243-263

Vestfirðir, Northwest Iceland, has been extensively modified by glacial activity, but the timing and landscape impact of pre-Last Glacial Maximum (LGM) glacial activity is not well known. We present new geochemical and chronological data from two tephras, Óþoli and Hjallanes, which constrain the age of high altitude ice-dammed lake sediments near the plateau surface of Skagafjall, located on the outer westernmost fjords of Vestfirðir. Our findings provide the first dated evidence of Late Pliocene glaciation on Vestfirðir. The 2.26±0.11 Ma fission-track age of the airfall rhyolitic Óþoli tephra is compatible with reversed palaeomagnetic polarity data and suggests an ice-dammed lake existed on Skagafjall at broadly the same time as a major and well-documented Late Pliocene downturn in global climate. We assess the likely impact of Late Pliocene and subsequent glacial activity on Vestfirðir landscapes and propose that: (1) geomorphological features and sedimentary deposits on or near the Skagafjall plateau surface could have survived beneath relatively low basal velocity areas and/or relatively non-erosive areas of glacial maxima ice sheets on Vestfirðir at glacial maxima, and (2) the heavily incised fjord network, the principal macroscale landscape feature of Vestfirðir, existed in the Late Pliocene.  相似文献   

3D mapping of buried underworld infrastructure using dynamic Bayesian network based multi-sensory image data fusion     

《Journal of Applied Geophysics》2013

The successful operation of buried infrastructure within urban environments is fundamental to the conservation of modern living standards. In this paper a novel multi-sensor image fusion framework has been proposed and investigated using dynamic Bayesian network for automatic detection of buried underworld infrastructure. Experimental multi-sensors images were acquired for a known buried plastic water pipe using Vibro-acoustic sensor based location methods and Ground Penetrating Radar imaging system. Computationally intelligent conventional image processing techniques were used to process three types of sensory images. Independently extracted depth and location information from different images regarding the target pipe were fused together using dynamic Bayesian network to predict the maximum probable location and depth of the pipe. The outcome from this study was very encouraging as it was able to detect the target pipe with high accuracy compared with the currently existing pipe survey map. The approach was also applied successfully to produce a best probable 3D buried asset map.  相似文献   

Thorium-234 as a tracer of spatial,temporal and vertical variability in particle flux in the North Pacific     

K.O. Buesseler  S. Pike  K. Maiti  C.H. Lamborg  D.A. Siegel  T.W. Trull 《Deep Sea Research Part I: Oceanographic Research Papers》2009,56(7):1143-1167

An extensive ²³⁴Th data set was collected at two sites in the North Pacific: ALOHA, an oligotrophic site near Hawaii, and K2, a mesotrophic HNLC site in the NW Pacific as part of the VERTIGO (VERtical Transport In the Global Ocean) study. Total ²³⁴Th:²³⁸U activity ratios near 1.0 indicated low particle fluxes at ALOHA, while ²³⁴Th:²³⁸U ～0.6 in the euphotic zone at K2 indicated higher particle export. However, spatial variability was large at both sites—even greater than seasonal variability as reported in prior studies. This variability in space and time confounds the use of single profiles of ²³⁴Th for sediment trap calibration purposes. At K2, there was a decrease in export flux and increase in ²³⁴Th activities over time associated with the declining phase of a summer diatom bloom, which required the use of non-steady state models for flux predictions. This variability in space and time confounds the use of single profiles of ²³⁴Th for sediment trap calibration purposes. High vertical resolution profiles show narrow layers (20–30 m) of excess ²³⁴Th below the deep chlorophyll maximum at K2 associated with particle remineralization resulting in a decrease in flux at depth that may be missed with standard sampling for ²³⁴Th and/or with sediment traps. Also, the application of ²³⁴Th as POC flux tracer relies on accurate sampling of particulate POC/²³⁴Th ratios and here the ratio is similar on sinking particles and mid-sized particles collected by in-situ filtration (>10–50 μm at ALOHA and >5–350 μm at K2). To further address variability in particle fluxes at K2, a simple model of the drawdown of ²³⁴Th and nutrients is used to demonstrate that while coupled during export, their ratios in the water column will vary with time and depth after export. Overall these ²³⁴Th data provide a detailed view into particle flux and remineralization in the North Pacific over time and space scales that are varying over days to weeks, and 10's–100's km at a resolution that is difficult to obtain with other methods.  相似文献   

The development of world oceans & coasts and concepts of sustainability     

《Marine Policy》2013

The current phase of technological development and expansion in the world economy is leading to greater human activity and development offshore. Some have described this as the colonisation of the oceans, one phase in the wider history of world industrialisation. This study empirically tests notions of ‘industrialisation’ and ‘colonisation’ in the oceans for the first time. It finds that human activity in the oceans has increased by multiple factors in the most recent long term wave of economic development. The methods include the combined use of Raster and R! to overcome methodological challenges to analyse large spatial datasets which map the footprint of human activity. In response to increasing human activity in the oceans, nations and supranational institutions are developing new governance regimes. These regimes are characterised by policy integration and a commitment to sustainability. Sustainable development is a central tenet of most national and international policies for the world's oceans. An analysis of sustainable development terminology within coastal and ocean policy is provided for seven major maritime governance regimes: Australia, Canada, New Zealand, EU, South Africa, UK and the US. The results show that sustainability is highly differentiated in the context of ‘the blue planet’ (oceans and coasts). The diverse interpretations of sustainability present an impasse to measuring progress in the field. Therefore the paper concludes by offering a framework for explanation and interpretation of sustainable development, by linking it to foundational assumptions held by systems of thought or philosophical traditions.  相似文献   

Dispersion measure variations and their effect on precision pulsar timing     

X. P. You  G. Hobbs  W. A. Coles  R. N. Manchester  R. Edwards  M. Bailes  J. Sarkissian  J. P. W. Verbiest  W. van Straten  A. Hotan  S. Ord  F. Jenet  N. D. R. Bhat  A. Teoh 《Monthly notices of the Royal Astronomical Society》2007,378(2):493-506

We present an analysis of the variations seen in the dispersion measures (DMs) of 20-ms pulsars observed as part of the Parkes Pulsar Timing Array project. We carry out a statistically rigorous structure function analysis for each pulsar and show that the variations seen for most pulsars are consistent with those expected for an interstellar medium characterized by a Kolmogorov turbulence spectrum. The structure functions for PSRs J1045−4509 and J1909−3744 provide the first clear evidence for a large inner scale, possibly due to ion–neutral damping. We also show the effect of the solar wind on the DMs and show that the simple models presently implemented into pulsar timing packages cannot reliably correct for this effect. For the first time we clearly show how DM variations affect pulsar timing residuals and how they can be corrected in order to obtain the highest possible timing precision. Even with our presently limited data span, the residuals (and all parameters derived from the timing) for six of our pulsars have been significantly improved by correcting for the DM variations.  相似文献   

Bounce Rock—A shergottite‐like basalt encountered at Meridiani Planum,Mars     

Jutta ZIPFEL  Bradley L. JOLLIFF  Ralf GELLERT  Kenneth E. HERKENHOFF  Rudolf RIEDER  Robert ANDERSON  James F. BELL III  Johannes BRÜCKNER  Joy A. CRISP  Philip R. CHRISTENSEN  Benton C. CLARK  Paulo A. De SOUZA Jr.  Gerlind DREIBUS  Claude D’USTON  Thanasis ECONOMOU  Steven P. GOREVAN  Brian C. HAHN  Göstar KLINGELHÖFER  Timothy J. McCOY  Harry Y. McSWEEN Jr.  Douglas W. MING  Richard V. MORRIS  Daniel S. RODIONOV  Steven W. SQUYRES  Heinrich WÄNKE  Shawn P. WRIGHT  Michael B. WYATT  Albert S. YEN 《Meteoritics & planetary science》2011,46(1):1-20

Abstract– The Opportunity rover of the Mars Exploration Rover mission encountered an isolated rock fragment with textural, mineralogical, and chemical properties similar to basaltic shergottites. This finding was confirmed by all rover instruments, and a comprehensive study of these results is reported here. Spectra from the miniature thermal emission spectrometer and the Panoramic Camera reveal a pyroxene‐rich mineralogy, which is also evident in Mössbauer spectra and in normative mineralogy derived from bulk chemistry measured by the alpha particle X‐ray spectrometer. The correspondence of Bounce Rock’s chemical composition with the composition of certain basaltic shergottites, especially Elephant Moraine (EET) 79001 lithology B and Queen Alexandra Range (QUE) 94201, is very close, with only Cl, Fe, and Ti exhibiting deviations. Chemical analyses further demonstrate characteristics typical of Mars such as the Fe/Mn ratio and P concentrations. Possible shock features support the idea that Bounce Rock was ejected from an impact crater, most likely in the Meridiani Planum region. Bopolu crater, 19.3 km in diameter, located 75 km to the southwest could be the source crater. To date, no other rocks of this composition have been encountered by any of the rovers on Mars. The finding of Bounce Rock by the Opportunity rover provides further direct evidence for an origin of basaltic shergottite meteorites from Mars.  相似文献   

A major element,PGE and Re–Os isotope study of Middle Atlas (Morocco) peridotite xenoliths: Evidence for coupled introduction of metasomatic sulphides and clinopyroxene     

Nadine Wittig  D. Graham Pearson  Joel A. Baker  Svend Duggen  Kaj Hoernle 《Lithos》2010,115(1-4):15-26

We present major element and PGE (platinum-group-element) abundances in addition to Re–Os isotope data for 11 spinel-facies whole rock peridotites from a single maar from the Middle Atlas Mountains, Morocco.Major element systematics of these xenoliths are generally correlated with indices of depletion. FeO–MgO systematics appear to suggest spinel-facies melting in the range of 5 to 25%. However, Al₂O₃ abundances in these xenoliths appear elevated relative to primitive mantle (Prima). The Al₂O₃ abundances in conjunction with other major elements require distinct re-enrichment of the Middle Atlas continental mantle root due to melt/rock reaction and precipitation of amphibole and/or clinopyroxene from passing silicate melts akin to MORB or OIB that evolved in reverse direction along the melting curves in e.g. FeO–MgO space. Sc and V confirm the range of apparent depletion and also indicate that the currently preserved fO₂ in these peridotites is distinctly different from fO₂ conditions observed in subduction zones.The majority of these xenoliths have low Os and Ir (I-PGEs) concentrations relative to Prima and modelled sulphide- and clinopyroxene-depleted residues of mantle melting under low fO₂, mid-ocean ridge-like conditions. Moreover, Pt and Pd (P-PGE) abundances are elevated when compared to their expected abundances after substantial melt extraction. Importantly, the systematically low Ir abundances in the majority of samples show well-correlated trends with Al₂O₃, MgO and Cu that are inconsistent with established melting trends. Os isotopes in the Middle Atlas xenoliths range from ¹⁸⁷Os/¹⁸⁸Os = 0.11604 to 0.12664 although most samples are close to chondritic. The Os isotope ratios are decoupled from ¹⁸⁷Re/¹⁸⁸Os but, together with Re abundances, also exhibit a good correlation with Al₂O₃, MgO and Cu.The major element, I-PGE and Os isotope correlations suggest that the initial melt depletion led to the exhaustion of sulphide and clinopyroxene (20 to 30%) without significant stabilization of I-PGE-rich alloys. During later modal metasomatism of the refractory Middle Atlas continental mantle root with silicate melts akin to MORB or OIB the introduction of clinopyroxene/amphibole reduced the volume of the melt inducing sulphur saturation in these melts causing precipitation of secondary sulphides. This coupled crystallization of pyroxenes and sulphides (chalcopyrite) resulted in the two-component mixing systematics exhibited by I-PGEs, Os isotopes with major elements and Cu preserved in the Middle Atlas continental mantle root.  相似文献   

Species distribution modelling to support marine conservation planning: The next steps     

《Marine Policy》2014

Species distribution models (SDMs) offer great potential for inclusion into the toolbox of today's marine environmental manager, especially with regard to marine conservation and planning. The application of SDMs in the marine environment over recent years has been varied but there are still relatively few examples in comparison with terrestrial application, and this is especially true in deep-sea marine ecosystems. This short article builds upon two recent review articles concerning the application of species distribution modelling studies in the marine realm, offering additional practical considerations for discussion. Recommendations for progressing the improved application of SDMs to support marine conservation planning are given, including combining model outputs with other data layers, metadata standards and model error. SDMs have both an urgent and long term contribution to make to marine conservation planning globally, and it is hoped that this article, in combination with developing research on marine SDMs, will contribute to some much needed discussion and inform best practice and new research to enable these models to be of greater use to marine managers.  相似文献