首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献，搜索用时 31 毫秒
1.
This study examines the political uses of “conflict diamond” discourse in global debates about commodity certification and socially responsible mining in Zimbabwe. Engaging critical literature on “conflict-free” corporate branding initiatives, the study focuses on representations of conflict in Marange, in Zimbabwe’s eastern highlands. In 2006, a diamond rush in Marange drew in tens of thousands of artisanal miners from across Zimbabwe as well as foreigners, and the government initiated military crackdowns in 2008. In a highly contested vote in 2009, the international government delegates who comprised the voting members in the Kimberley Process Certification System (KPCS) ruled that conflict in Marange did not meet the KPCS definitions of “conflict diamond.” The study examines discourses of key stakeholders in the multinational diamond industry, human rights organizations, policymakers as well as artisanal miners in Zimbabwe between 2006 and 2014. The article argues that advocacies against diamond certification as well as advocacies favouring certification both tended to overlook the interests of artisanal miners, focusing narrowly on certain forms of conflict while associating artisanal mining with illicitness. The Marange case illustrates how conventional discourses on “conflict diamonds” not only obscure the complex nature of conflicts in contemporary capitalist accumulation processes; they also risk contributing to new forms of structural violence. This analysis highlights the need to pay careful attention to how global commodity certification discourses inter-relate with political agendas at multiple scales. The study draws attention to dilemmas for geographers when portraying the interests of marginalized groups in – and affected by – the diamond mining sector.  相似文献   

2.
This largely programmatic paper offers a new way of thinking through the incorporation of farmland into financial markets. Building on the notion of “operations of capital”, it sketches analytical entry points for scrutinizing the inner workings of agri-finance capital formation. The concept of operations can make two useful contributions to the existing discussion. First, it helps provide a more nuanced historicization of the entanglement between finance and farmland. Finance has a long history of penetrating agriculture and the new quality of the contemporary coupling of finance and farmland only becomes fully visible when adopting a more nuanced historical perspective. Rather than imagining the history of capitalism as one where industrial capitalism gives way to financialized capitalism, the concept of operations sensitizes us for the situated modes, processes and practices of financial economization that have reworked economy, society and nature at specific historical conjunctures.Second, it allows us to move beyond simply treating “financialization” as explanans. Shifting attention to the situated practical activities of global finance, it eventually helps us explore central categories of financial economization (“capital”, “resources”, “property” and “value”) as practical accomplishments rather than taking them for granted. Only then can we come to terms with how finance works through farmland in different geographical settings. Empirical material from an ongoing research project will support my arguments.  相似文献   

3.
This article contributes an empirically rich account of a social enterprise project embedded in local urban economies of Nairobi, Kenya. The confluence of rapid, unplanned urbanisation and economic liberalisation has led to growing formations of informal settlements and a vibrant informal sector across post-colonial cities. These “slum” neighbourhoods, housing the majority of the urban population on a fraction of the city’s land, are often ignored and marginalized by the state and municipal authorities, particularly with regards to basic service provision. At the same time, slum economies provide entry-points for various enterprise-led development schemes seeking to commercially engage both entrepreneurial individuals and their existing customer base in order to scale access to unmet needs. The discussion is based on an ethnographic study in one of Nairobi’s largest informal settlements, which focused on the everyday practices of a local micro-franchise called “Community Cleaning Services”. The article illustrates how waste workers and self-proclaimed “hustlers” were turned into micro-franchisee entrepreneurs providing a sanitation service to residential customers, through their engagement with Community Cleaning Services. This ethnographic account raises two potentially contradictory but inter-related debates that are rarely considered alongside one another in the existing literature on corporate involvement in low-income markets. First, it reframes the critiques of enterprise-led initiatives to “poverty alleviation” by focusing on the implications of commercialising “basic” services and on the logistical and cultural challenges of turning social needs into market demands. Second, it emphasises the often-invisible role of grassroots informal economies in enabling access to vital services in the absence of an adequately resourced and responsive municipality. The article concludes with a broader reflection on the effects and limitations of corporate-led development schemes targeting the urban poor and points to the contrasting logics of grassroots entrepreneurial urbanism and corporate—albeit “socially responsible”—parameters of success.  相似文献   

4.
  相似文献   

5.
Surfaces of phosphorite nodules and pebbles from the “Cambridge Green Sand” (Cenomanian, South England) yielded several discernible types of scratches. These originated before the burial of nodules/pebbles as evidenced by fossil epibiotic oysters cemented to cover the scratches. The individual forms of scratches differ in size and shape; therefore, the set of “scratching instruments” also had to be different. The scratches described differ from scratches generated by glacial processes, namely by the regularity of length and intervals, parallel orientation, existence of recurrent forms and placement along the nodule edges. We interpret the scratches as trace fossils of the ichnogenus Machichnus. Three new species, namely M. normani, M. harlandi and M. jeansi, are erected for them herein. The series of scratches originated probably by teeth on a couple of jaws; the makers possibly scraped bacterial or algal film off the surface of nodules that were covered with the phosphate gel. Both homodont and heterodont animals (probably fish) were involved.  相似文献   

6.
This article shows how paramilitaries and allied companies put grassroots development discourses of political participation and subsidiarity, environmental conservation, and ethnic empowerment to work in executing and ratifying their massive land grab in northwest Colombia. More than a case of trying to “whitewash” their malfeasance with fashionable and politically correct development-speak, I argue that the grassroots development apparatus—its discourses, institutional forms, and practices—became utterly instrumental to the illegal land seizures. Moreover, when operating alongside practices of land parcelization, iterative transactions, producers’ cooperatives, and third-party intermediaries, grassroots development facilitated what could be called “land laundering.” In the process, grassroots development became a conduit for paramilitary-backed state formation in which projects of liberal governance commonly associated with the imperatives of institution building, good governance, and the rule of law became perversely compatible with the region’s economies of violence. With the World Bank increasingly concerned over the conflation of fragile states, violent conflict, and alarming land grabs, this article raises questions about how the grassroots solutions currently being endorsed by the Bank can in some cases actually facilitate dispossession, illicit economies, and violent political projects. The way paramilitaries harnessed grassroots development also has critical implications for debates about post-development.  相似文献   

7.
A new soft-shelled turtle (“Trionyx” jixiensis sp. nov.) from the Lower Cretaceous Chengzihe Formation, Jixi city, Heilongjiang Province, China is described on the basis of a nearly complete carapace. The new species is diagnosed by the absence of suprascapular fontanelles and absence of a preneural; eight neurals, tetragonal fifth neural; and eight pairs of costals, with the large eighth costals meeting after the eighth neural. Due to the incompleteness of the specimen and confused classification of the genera of trionychids, the new species cannot be included in any genus of Trionychinae and is temporarily assigned to “Trionyx” (sensu lato). “Trionyx” jixiensis is one of the earliest trionychids, its discovery indicates that the family was already diversified during the Early Cretaceous in Asia.  相似文献   

8.
This paper demonstrates how the global commodity chain approach has mutated from a critical tool for studying the production of inequality in the global economy to an instrument of development policy that extends the frontiers of marketization to so-called “peripheries” in the Global South. Taking an outgrower scheme for the global production of organic mangoes in northern Ghana as point of departure, and situating this case study within the broader context of market experiments in the Ghanaian agricultural sector, it develops an account of global capitalism as a diverse, heterogeneous and messy arrangement of local borderlands. As a zone of inclusive exclusion these borderlands are brought into being by an economic discourse which separates the inside of the capitalist world from its supposed outside. The so-called integration of smallholders into global markets relies on exclusionary representations and the forging of new associations. First, economic practices in northern Ghana are portrayed by economists as defective and in doing so determine what lies outside the market. Second, within this “outside” – on which the “inside” actually depends – global capitalism mediated through the market models and rhetoric of international development organizations now literally touches the ground in specific geographical settings. Hence Frontier regions as represented by our case study bear the paradoxical character of the work of economics and are an instructive example for the performative power of economic theories. Marketization is revealed as a complex and socio-technically entangled process full of hidden prerequisites and unforeseen consequences that open up new social spaces of multiple ontological reconfigurations.  相似文献   

9.
The simultaneous but incompatible desires for both “tradition” and “advancement” have produced the “ambiguity of modernity” in the areas of minority nationalities (shaoshu minzu diqu) on China’s southwest frontier. This paper, in accordance, directly addresses the ambiguity of modernity through the investigation of the tea landscape in Yunnan. This essay builds on Aihwa Ong and Stephen Collier’s “global assemblage” framework to analyze the relationship between the “global form” of modernity and the situated assemblages of “ambiguity of modernity” in southwest China. Data are based on ethnographic research in the village of Mangjing, located in Jingmai Mountain, a renowned tea mountain in Yunnan. Most of the villagers in Mangjing are one of the minority nationalities of China, Bulang. I discuss the state-led project in transforming the modern tea plantation for “restoring” a landscape deemed as “ancient tea forest” (guchalin) in Mangjing. In addition, I address Bulang villagers’ and government officials’ multiple responses to the transformation of tea landscapes. I argue that the transformation of tea landscapes has been the practice to turn the “global form” of modernity into the shifting “assemblages” amongst tradition, modernity, science, and nature. The ambiguity of modernity has emerged from the shifting assemblages, providing both the state and Bulang villagers more leeway to symbolically and physically (re)produce meanings for the tea landscapes to meet the contingent market demand for tea. The transformation of tea landscapes, however, has become another process to perpetuate Bulang villagers’ social status of being “low quality” as China’s minority nationalities.  相似文献   

10.
Geological events, such as emplacement of granite or growth of slaty cleavage, may be ordered into a sequence by two methods. One is to assign each event a place in a time scale, such as years before the present, which amounts to assigning events an age designation from the set of real numbers. In ordering such a list, the algebra of real numbers applies. A second method is to determine the time relations of events in pairs, such as a fold is of type (S1, S2) or granite intrudes conglomerate. These binary relations between events may be used to order events into a sequence using the transitive properties of the relation “older than.” It is shown, however, that the binary relations between events do not follow the familiar rules for the algebra of real or integral numbers and it is necessary to erect a new system of relations called the “algebra of events.” The fundamental relation is “older than or equivalent to” and this may be used to define the relations “older than”, “younger than”, “equivalent to”, “incomparable to”, and “covers.” The essential difference from the algebra of integers is that the reflexive relation (“equal to”) is replaced by two such relations (“equivalent to” and “incomparable to”) in the algebra of events. A number of binary relations between events may be assembled into an event matrix which is basically a truth table for the relation “older than.” This may be ordered and stacked by operations termed ORDER and STACK. The relationship of each event to every other event may be determined by simple inspection of an ordered, stacked matrix, and from this a geological history may be assembled. If there are contradictions in the field data, ordering into a proper sequence is impossible and may be detected. If there are ambiguities in the field data, there are several different orders that are proper sequences so that the event matrix may be ordered. However, the ambiguities occur as voids in the stacked matrix.  相似文献   

11.
A relatively diverse microbiota, preserved in-situ, has been discovered in cherty stratiform stromatolites of the middle Proterozoic Wumishan Formation (c. 1200–1300 Maold), Jixian Group, in the Ming Tombs area of Beijing. This microfossil assemblage consists of two parts: (1) the mat-building and mat-dwelling benthos which mostly belong to “long-lasting” taxa and are mostly common with those of other Proterozoic microbiotas; and (2) allochthonous elements including some plankton and peculiar structures which are either new forms first described here or taxa shared with some contemporaneous or penecontemporaneous microbiotas elsewhere. The latter may have more stratigraphic significance.Bivariate analysis on two characters measured (length and width) has been used in the classification of the elongate microfossils, and the results demonstrate that biometrical methods are effective in the taxonomy of some Precambrian microfossils.The following new taxa are described:Archaeoellipsoides obesus sp. nov., Archaeoellipsoides conjunctivus sp. nov., Bactrophycus oblongum gen. et sp. nov., Bactrophycus dolichum gen. et sp. nov., Callosicoccus crauros gen. et sp. nov.  相似文献   

12.
The stratigraphic record in the James and Hudson Bay Lowlands indicates that the sequence of glacial events at the geographical center of the 12.6 × 106 km2 Laurentide Ice Sheet may have been more complex than hitherto imagined. Isoleucine epimerization ratios of in situ and transported shells recovered from till and associated marine and fluvial sediments cluster into at least 4 discrete groups. Two alternative explanations of the data are offered, of which we strongly favor the first. Hypothesis 1: Setting the age of the “last interglacial” marine incursion, the Bell Sea, at 130,000 yr B.P. results in a long-term average diagenetic temperature for the lowlands of +0.6°C. Using this temperature enables us to predict the age of shells intermediate in age between the “last interglaciation” and the incursion of the Tyrrell Sea 8000 yr ago. Between these two interglacial marine inundations, Hudson Bay is predicted to have been free of ice along its southern shore about 35,000, 75,000, and 105,000 yr ago based on amino acid ratios from shells occurring as erratics in several superimposed tills and fluvial sediments. These results suggest (1) that traditional concepts of ice-sheet build-up and decay must be reexamined; (2) that “high” sea levels may have occurred during the Wisconsin Glaciation; and (3) that a critical reappraisal is required of the open ocean δ18O record as a simple indicator of global ice volume. An alternative, Hypothesis 2, is also examined. It is based on the assumption that the 35,000-yr-old deposits calculated on the basis of Hypothesis 1 date from the “last interglaciation”; this, in effect, indicates that the Missinaibi Formation, commonly accepted as sediments of the “last interglaciation,” are about 500,000 yr old and that the effective diagenetic temperature in the lowlands during approximately the last 130,000 yr has been close to ?6°C. We argue for rejection of this alternative hypothesis.  相似文献   

13.
The word “mazuku” in Swahili means “evil wind”. It corresponds to lowland (depressions) where carbon dioxide is released and, being heavier than air, accumulates at high – often lethal – concentrations (10 vol.% of CO2 in atmosphere can be considered as the deadly threshold, even for a short time exposure). Mazuku are abundant in Goma and surrounding areas and particularly in the area south of the large volcanic edifices of Nyiragongo and Nyamulagira volcanoes located in the most eastern part of DR Congo, W branch of the East African Rift System (EARS). Our extensive field surveys have indicated that mazuku are concentrated within to and around the densely populated city of Goma close to the N shores of Lake Kivu, mainly near fault or fissure networks. At a more local scale, depressions allowing CO2-rich gas accumulation are created by lava flow superposition, lava tunnels or cavity collapses, or directly associated with open fractures. People are killed by mazuku every year. Given political and social unrest coupled with the current important demographic and urban growths around Goma, the risks associated to mazuku are increasing accordingly. Mazuku are currently the most important natural risk in terms of human loss for the area and there is an urgent need for further research, more systematic mapping and monitoring of mazuku and for appropriate risk management to be implemented. This paper summarizes the current scientific knowledge on mazuku as well as new advances and a preliminary risk assessment performed recently in the frame of the GORISK project.  相似文献   

14.
The six peculiar multicusped teeth described here were collected from sediments of the Upper Cretaceous of São José do Rio Preto Formation, near Ibirá (northeastern São Paulo, Brazil). Their bulbous crowns are slightly labio-lingual compressed, and bear a main plus two accessory cusps, which conceal a well developed cingulum. Wear facets are seen on the main and distal accessory cusps. Comparison to the known Crocodyliformes with multicusped teeth show that the new material is not referable to “protosuchians” or eusuchians, nor related to two unnamed forms from Morocco and “notosuchians” such as Uruguaysuchus, Chiamaerasuchus, and Simosuchus. On the other hand, possible affinities with Candidodon and Malawisuchus were maintained based on shared traits. This includes teeth with the main cusp and some accessory cusps arranged in more than one axis, a previously defined unambiguous apomorphy of the putative clade composed of Candidodon plus Malawisuchus. The term Candidodontidae can be applied to this group, and defined as all taxa closer to Candidodon itapecuruensis than to Notosuchus terrestris, Uruguaysuchus aznarezi, Comahuesuchus brachybuccalis, Sphagesaurus huenei, Baurusuchus pachecoi, and Crocodylus niloticus.  相似文献   

15.
We propose a population model for Middle Pleistocene Europe that is based on demographic “sources” and “sinks”. The former were a small number of “core” or populations in glacial refugia in southern Europe from which hominins expanded northwards in interstadial and interglacial periods; occupation outside glacial refugia would have been restricted to warm or temperate periods, and populations at the northern limit of the Middle Pleistocene range would have been “sink” populations in that they depended upon recruitment from source populations further south. Southwest Asia would also have been a likely source of immigrant, source populations. We argue as an alternative to an “ebb and flow” model in which groups retreated to refugia when conditions worsened that local extinction outside refugia would have been frequent. In extreme situations, Europe may have been a population “sink” (i.e. unpopulated) that was replenished from source populations in Southwest Asia. We suggest that this pattern of repeated colonisation and extinction may help explain the morphological variability of European Middle Pleistocene hominins, particularly Homo heidelbergensis and its apparent non-lineal evolution towards Homo neanderthalensis.  相似文献   

16.
Peter North 《Geoforum》2010,41(4):585-594
This paper critically but sympathetically examines eco-localisation as a response to ‘peak oil’ and to reduce the emission of CO2 to avoid dangerous climate change. Rather than seeing the politics of climate change and peak oil as in some way ‘post-political’, the paper argues that protagonists of localised economies are developing radical new conceptions of livelihood and economy that directly cut against the logic of growth-based capitalist economic strategies and elite conceptualisations of economic development. Building on development theory, the paper develops a conceptualisation of ‘immanent’ and ‘intentional’ localisation, with the former a simple move by businesses of economic activities that have high transport costs closer to their markets. Advocates of intentional localisation are working more pro actively at grassroots level to develop local solutions to peak oil and climate change based on developing less resource-intensive yet enjoyable and fulfilling livelihoods in more localised economies. In discussing the contested nature of localisation, the paper engages with critiques of eco-localisation from neoliberal advocates and from the left, before concluding that localisation should be seen more as a different calculation of where economic activities would be located, which aims to reduce oil consumption and CO2 emissions, rather than a call for autarky. The paper concludes by arguing that analyses of the scale of economic networks need to pay more attention of the materiality of oil consumption and CO2 emissions, and that scales cannot be seen as socially constructed.  相似文献   

17.
This paper presents new major and trace element data from 150 garnet xenocrysts from the V. Grib kimberlite pipe located in the central part of the Arkhangelsk diamondiferous province (ADP). Based on the concentrations of Cr2O3, CaO, TiO2 and rare earth elements (REE) the garnets were divided into seven groups: (1) lherzolitic “depleted” garnets (“Lz 1”), (2) lherzolitic garnets with normal REE patterns (“Lz 2”), (3) lherzolitic garnets with weakly sinusoidal REE patterns (“Lz 3”), (4) lherzolitic garnets with strongly sinusoidal REE patterns (“Lz 4”), (5) harzburgitic garnets with sinusoidal REE patterns (“Hz”), (6) wehrlitic garnets with weakly sinusoidal REE patterns (“W”), (7) garnets of megacryst paragenesis with normal REE patterns (“Meg”). Detailed mineralogical and geochemical garnet studies and modeling results suggest several stages of mantle metasomatism influenced by carbonatite and silicate melts. Carbonatitic metasomatism at the first stage resulted in refertilization of the lithospheric mantle, which is evidenced by a nearly vertical CaO-Cr2O3 trend from harzburgitic (“Hz”) to lherzolitic (“Lz 4”) garnet composition. Harzburgitic garnets (“Hz”) have probably been formed by interactions between carbonatite melts and exsolved garnets in high-degree melt extraction residues. At the second stage of metasomatism, garnets with weakly sinusoidal REE patterns (“Lz 3”, “W”) were affected by a silicate melt possessing a REE composition similar to that of ADP alkaline mica-poor picrites. At the last stage, the garnets interacted with basaltic melts, which resulted in the decrease CaO-Cr2O3 trend of “Lz 2” garnet composition. Cr-poor garnets of megacryst paragenesis (“Meg”) could crystallize directly from the silicate melt which has a REE composition close to that of ADP alkaline mica-poor picrites. P-T estimates of the garnet xenocrysts indicate that the interval of ～60–110 km of the lithospheric mantle beneath the V. Grib pipe was predominantly affected by the silicate melts, whereas the lithospheric mantle deeper than 150 km was influenced by the carbonatite melts.  相似文献   

18.
  相似文献   

19.
N. L. Dobretsov 《Petrology》2010,18(1):84-106
Geological-petrological and geochemical data on subduction-related magmatism (including the volumes and compositions of the corresponding magmatic series) are compared to the results of experiments and numerical simulation. The subduction zone is subdivided into five depth sectors and volcanic zones I, II, and III: 1 is the accretionary wedge that controls the geodynamic stability of subduction; 2 is the sector of dehydration and fluid filtration; 3 is the zone of eclogitization and initial partial melting in the slab above which boninite volcanic zone I is formed during early stages; 4 is the main zone of melting of the sedimentary-basite layer and the development of volcanic zone II with the predominance of andesites; and 5 is the zone of higher degree melting, above which volcanic zone III (basaltic andesite and alkali basalt) is formed. The criterion of volcanism intensity, which was obtained within the scope of the melting model, is proportional to the subduction velocity and the thickness of the melting zone, and the distance between the groups of volcanics along the subduction zone is 75–100 km, at a thickness of the melting zone of 15–20 km. The calculated isotherm of 600°C, which controls the stability of serpentine and chlorite, is not identified at depth above 150 km, and this is confirmed by the composition and P-T conditions of the high-pressure rocks (containing diamond and coesite), which were brought from depths of 150–200 km in subduction zones. Seismic sections constructed with regard for the amplitude characteristics of seismic waves show two melting zones (“wet” melting at a depth of 100–200 km and “dry” melting at a depth of 150–200 km) and a complicated thermal structure of the suprasthenospheric wedge, which can include slant magma conduits. The mineralogical and geochemical features of arc magmatic series are formed at a decisive role of an H2O-CO2 fluid and an elevated oxidation potential. The predominant buffer minerals are as follows: garnet in the slab melting zone; magnetite, Ca-pyroxene, and amphibole in intermediate magmatic chambers; and amphibole, protoenstatite-bronzite (in place of olivine), and Cr-spinel (in place of magnetite) for boninite series generated in a “hot” asthenospheric wedge at interaction with fluids or water-rich melts. Actively disputable problems are the interactions scale of melts and fluids generated in a subduction zone with a “hot” mantle wedge, the possibility of transporting water-rich minerals deep into the mantle (to depths greater than 150 km), and the evolution of the scale at which young continental crust is generated by subduction melts.  相似文献   

20.
A. Delabroye  M. Vecoli 《Earth》2010,98(3-4):269-282
This paper proposes a global review of Hirnantian event stratigraphy. The Hirnantian GSSP in south China is tentatively correlated with latest Ordovician strata from the peri-Gondwanan “glacial” regions. Problems of biostratigraphical correlation are highlighted. At a worldwide scale, the major biostratigraphically useful fossil groups (graptolites, chitinozoans, brachiopods, conodonts, acritarchs) are analysed and their limits for global correlation of the uppermost Ordovician are discussed. Palaeobiogeographical disparities are invoked as the primary cause of the difficulty in establishing an effective Late Ordovician global biostratigraphical scheme. As an alternative correlative tool, the HICE (Hirnantian Isotopic Curve Excursion) event is often put forward in the literature. However, carbon isotope chemostratigraphy shows, like biostratigraphy, some limits to the present state of knowledge. No good independent biostratigraphical control of the HICE exists in both shallow carbonate deposits and deeper shaly ones. Recent studies have also demonstrated inconsistencies between carbon isotopic signals obtained from organic (δ13Corg) and inorganic (δ13Ccarb) carbon species, further complicating the use of the HICE as an isochronous benchmark.All of these difficulties for Hirnantian event stratigraphy are discussed in detail in order to enable them to be overcome in the future. Precise Late Ordovician and early Silurian event stratigraphies are essential for the understanding of the mechanisms linked to the first of the “Big Five” extinctions.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号