3,785 research outputs found

    Loudly sing cuckoo : More-than-human seasonalities in Britain

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    This research was funded by a grant from the Arts and Humanities Research Council, grant number AH/E009573/1.Peer reviewedPostprin

    Linguistic incompetence: giving an account of researching multilingually

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    This paper considers the place of linguistic competence and incompetence in the context of researching multilingually. It offers a critique of the concept of competence and explores the performative dimensions of multilingual research and its narration, through the philosophy of Judith Butler, and in particular her study Giving an account of oneself. It explores aspects of risk, justice, narrative limit and a morality of multilingualism in emergent multilingual research frameworks. These theoretical dimensions are explored through consideration of ‘linguistically incompetent’ ethnographic work with refugees and asylum seekers, in contexts of hospitality and in life long learning research in the Gaza Strip, and of early attempts to learn new languages. The paper offers a prospect of a relational approach to researching multilingually and affirms the vulnerability at the heart of linguistic hospitality

    Things of the ground: Children's medicine, motherhood and memory in the Cameroon grassfields

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    Copyright @ 2011 Cambridge University PressSoon after birth, infants in the Cameroon Grassfields chiefdom of Oku are submitted by their parents to rites known generically as ‘children's medicine’ (k∂fu ∂bwan). Ostensibly performed to protect infants from harm and illness, the rites are in fact fraught with tension: they embrace contradictory perspectives regarding the social role of the mother and belie the normative ideal extolling her as a figure of nurture and protection. The article argues that, beyond their overt purpose and symbolism as rites of passage, the rites evoke collective memories of child abductions and contemporary anxieties regarding the anticipated departure of older children and adolescents into foster care or migrant labour. Going beyond a classic tripartite model, the article takes a long-term view that sees life-crisis rituals as a form of collective memory that bears witness to social tensions that cannot be resolved – in this case the contradictions inherent within the hallowed image of the mother and the compromised nature of parental love

    Flow and retreat of the Late Quaternary Pine Island-Thwaites palaeo-ice stream, West Antarctica

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    Multibeam swath bathymetry and sub-bottom profiler data are used to establish constraints on the flow and retreat history of a major palaeo-ice stream that carried the combined discharge from the parts of the West Antarctic Ice Sheet now occupied by the Pine Island and Thwaites glacier basins. Sets of highly elongated bedforms show that, at the last glacial maximum, the route of the Pine Island-Thwaites palaeo-ice stream arced north-northeast following a prominent cross-shelf trough. In this area, the grounding line advanced to within similar to 68 km of, and probably reached, the shelf edge. Minimum ice thickness is estimated at 715 m on the outer shelf, and we estimate a minimum ice discharge of similar to 108 km(3) yr(-1) assuming velocities similar to today's Pine Island glacier (similar to 2.5 km yr(-1)). Additional bed forms observed in a trough northwest of Pine Island Bay likely formed via diachronous ice flows across the outer shelf and demonstrate switching ice stream behavior. The "style" of ice retreat is also evident in five grounding zone wedges, which suggest episodic deglaciation characterized by halts in grounding line migration up-trough. Stillstands occurred in association with changes in ice bed gradient, and phases of inferred rapid retreat correlate to higher bed slopes, supporting theoretical studies that show bed geometry as a control on ice margin recession. However, estimates that individual wedges could have formed within several centuries still imply a relatively rapid overall retreat. Our findings show that the ice stream channeled a substantial fraction of West Antarctica's discharge in the past, just as the Pine Island and Thwaites glaciers do today
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