title: Feeling at home? Former Bhutanese refugee women and girls in New Zealand

authors: Basnet, Sunita

abstract: This article explores the meaning of home and homemaking practices for former Bhutanese refugees, especially women and girls living in Auckland, Christchurch, Nelson, and Palmerston North in New Zealand under the refugees’ quota programme. I examine how and in what ways these women and girls experience New Zealand as ‘home’ and explore their feelings of (not) belonging. The fieldwork is part of my PhD research and was conducted between February and September 2015. A total of 42 in-depth semi-structured interviews with former Bhutanese refugees were conducted. These were mainly with women and girls, but eight men were also interviewed. In addition to individual interviews, I used a focus group interview with four girls aged between 12-15 who sketched images of their actual or imagine home. The findings are that just providing a ‘house’ to refugees does not necessarily mean that they feel at home in New Zealand. Many participants reported that family is their home. Another finding is that strong neighborhood ties contributed to feeling at home (or not). Participants also discussed what it means to be a citizen in New Zealand. Finally, I argue that researching former refugees’ home and homemaking everyday practices is useful for understanding resettlement processes and senses of belonging in New Zealand.

text: Feeling at home? Former Bhutanese refugee women and girls in New Zealand This article explores the meaning of home and homemaking practices for former Bhutanese refugees, especially women and girls living in Auckland, Christchurch, Nelson, and Palmerston North in New Zealand under the refugees’ quota programme. I examine how and in what ways these women and girls experience New Zealand as ‘home’ and explore their feelings of (not) belonging. The fieldwork is part of my PhD research and was conducted between February and September 2015. A total of 42 in-depth semi-structured interviews with former Bhutanese refugees were conducted. These were mainly with women and girls, but eight men were also interviewed. In addition to individual interviews, I used a focus group interview with four girls aged between 12-15 who sketched images of their actual or imagine home. The findings are that just providing a ‘house’ to refugees does not necessarily mean that they feel at home in New Zealand. Many participants reported that family is their home. Another finding is that strong neighborhood ties contributed to feeling at home (or not). Participants also discussed what it means to be a citizen in New Zealand. Finally, I argue that researching former refugees’ home and homemaking everyday practices is useful for understanding resettlement processes and senses of belonging in New Zealand.

year: 2016

title: History of oceanic front development in the New Zealand sector of the Southern Ocean during the Cenozoic--a synthesis

authors: Nelson, Campbell S.

subjects: New Zealand

abstract: The New Zealand sector of the Southern Ocean (NZSSO) has opened about the Indian-Pacific spreading ridge throughout the Cenozoic. Today the NZSSO is characterised by broad zonal belts of antarctic (cold), subantarctic (cool), and subtropical (warm) surface-water masses separated by prominent oceanic fronts: the Subtropical Front (STF) c. 43deg.S, Subantarctic Front (SAF) c. 50deg.S, and Antarctic Polar Front (AAPF) c. 60deg.S. Despite a meagre database, the broad pattern of Cenozoic evolution of these fronts is reviewed from the results of Deep Sea Drilling Project-based studies of sediment facies, microfossil assemblages and diversity, and stable isotope records, as well as from evidence in onland New Zealand Cenozoic sequences. Results are depicted schematically on seven paleogeographic maps covering the NZSSO at 10 m.y. intervals through the Cenozoic. 
During the Paleocene and most of the Eocene (65-35 Ma), the entire NZSSO was under the influence of warm to cool subtropical waters, with no detectable oceanic fronts. In the latest Eocene (c. 35 Ma), a proto-STF is shown separating subantarctic and subtropical waters offshore from Antarctica, near 65deg.S paleolatitude. During the earliest Oligocene, this front was displaced northwards by development of an AAPF following major global cooling and biotic turnover associated with ice sheet expansion to sea level on East Antarctica. Early Oligocene full opening (c. 31 Ma) of the Tasmanian gateway initiated vigorous proto-circum-Antarctic flow of cold/cool waters, possibly through a West Antarctic seaway linking the southern Pacific and Atlantic Oceans, including detached northwards "jetting" onto the New Zealand plateau where condensation and unconformity development was widespread in cool-water carbonate facies. Since this time, a broad tripartite division of antarctic, subantarctic, and subtropical waters has existed in the NZSSO, including possible development of a proto-SAF within the subantarctic belt. In the Early-early Middle Miocene (25-15 Ma), warm subtropical waters expanded southwards into the northern NZSSO, possibly associated with reduced ice volume on East Antarctica but particularly with restriction of the Indonesian gateway and redirection of intensified warm surface flows southwards into the Tasman Sea, as well as complete opening of the Drake gateway by 23 Ma allowing more complete decoupling of cool circum-Antarctic flow from the subtropical waters. During the late Middle-Late Miocene (15-5 Ma), both the STF and SAF proper were established in their present relative positions across and about the Campbell Plateau, respectively, accompanying renewed ice buildup on East Antarctica and formation of a permanent ice sheet on West Antarctica, as well as generally more expansive and intensified circum-Antarctic flow. 
The ultimate control on the history of oceanic front development in the NZSSO has been plate tectonics through its influence on the paleogeographic changes of the Australian-New Zealand-Antarctic continents and their intervening oceanic basins, the timing of opening and closing of critical seaways, the potential for submarine ridges and plateaus to exert some bathymetric control on the location of fronts, and the evolving ice budget on the Antarctic continent. The broad trends of the Cenozoic climate curve for New Zealand deduced from fossil evidence in the uplifted marine sedimentary record correspond well to the principal paleoceanographic events controlling the evolution and migration of the oceanic fronts in the NZSSO.

text: History of oceanic front development in the New Zealand sector of the Southern Ocean during the Cenozoic--a synthesis The New Zealand sector of the Southern Ocean (NZSSO) has opened about the Indian-Pacific spreading ridge throughout the Cenozoic. Today the NZSSO is characterised by broad zonal belts of antarctic (cold), subantarctic (cool), and subtropical (warm) surface-water masses separated by prominent oceanic fronts: the Subtropical Front (STF) c. 43deg.S, Subantarctic Front (SAF) c. 50deg.S, and Antarctic Polar Front (AAPF) c. 60deg.S. Despite a meagre database, the broad pattern of Cenozoic evolution of these fronts is reviewed from the results of Deep Sea Drilling Project-based studies of sediment facies, microfossil assemblages and diversity, and stable isotope records, as well as from evidence in onland New Zealand Cenozoic sequences. Results are depicted schematically on seven paleogeographic maps covering the NZSSO at 10 m.y. intervals through the Cenozoic. 
During the Paleocene and most of the Eocene (65-35 Ma), the entire NZSSO was under the influence of warm to cool subtropical waters, with no detectable oceanic fronts. In the latest Eocene (c. 35 Ma), a proto-STF is shown separating subantarctic and subtropical waters offshore from Antarctica, near 65deg.S paleolatitude. During the earliest Oligocene, this front was displaced northwards by development of an AAPF following major global cooling and biotic turnover associated with ice sheet expansion to sea level on East Antarctica. Early Oligocene full opening (c. 31 Ma) of the Tasmanian gateway initiated vigorous proto-circum-Antarctic flow of cold/cool waters, possibly through a West Antarctic seaway linking the southern Pacific and Atlantic Oceans, including detached northwards "jetting" onto the New Zealand plateau where condensation and unconformity development was widespread in cool-water carbonate facies. Since this time, a broad tripartite division of antarctic, subantarctic, and subtropical waters has existed in the NZSSO, including possible development of a proto-SAF within the subantarctic belt. In the Early-early Middle Miocene (25-15 Ma), warm subtropical waters expanded southwards into the northern NZSSO, possibly associated with reduced ice volume on East Antarctica but particularly with restriction of the Indonesian gateway and redirection of intensified warm surface flows southwards into the Tasman Sea, as well as complete opening of the Drake gateway by 23 Ma allowing more complete decoupling of cool circum-Antarctic flow from the subtropical waters. During the late Middle-Late Miocene (15-5 Ma), both the STF and SAF proper were established in their present relative positions across and about the Campbell Plateau, respectively, accompanying renewed ice buildup on East Antarctica and formation of a permanent ice sheet on West Antarctica, as well as generally more expansive and intensified circum-Antarctic flow. 
The ultimate control on the history of oceanic front development in the NZSSO has been plate tectonics through its influence on the paleogeographic changes of the Australian-New Zealand-Antarctic continents and their intervening oceanic basins, the timing of opening and closing of critical seaways, the potential for submarine ridges and plateaus to exert some bathymetric control on the location of fronts, and the evolving ice budget on the Antarctic continent. The broad trends of the Cenozoic climate curve for New Zealand deduced from fossil evidence in the uplifted marine sedimentary record correspond well to the principal paleoceanographic events controlling the evolution and migration of the oceanic fronts in the NZSSO.

year: 2001-12-01

title: A literary and linguistic critique of a Māori lullaby

authors: August, Tipene

subjects: waiata Māori

abstract: Māori song poems surviving from pre-colonial times can provide a valuable source of information about the artistic and cultural heritage of Māoridom. However, they present a number of challenges for the contemporary analyst. On the basis of a stylistic analysis of a Māori lullaby, a number of hypotheses about Māori song poems in general, and the lullaby in particular, are put forward and it is suggested that these hypotheses could be tested in relation to a corpus of song poems. It is hoped that the approach to stylistic analysis adopted here will be of use to scholars of Māori song poems and, perhaps, also to others who are interested in indigenous art forms more generally.

text: A literary and linguistic critique of a Māori lullaby Māori song poems surviving from pre-colonial times can provide a valuable source of information about the artistic and cultural heritage of Māoridom. However, they present a number of challenges for the contemporary analyst. On the basis of a stylistic analysis of a Māori lullaby, a number of hypotheses about Māori song poems in general, and the lullaby in particular, are put forward and it is suggested that these hypotheses could be tested in relation to a corpus of song poems. It is hoped that the approach to stylistic analysis adopted here will be of use to scholars of Māori song poems and, perhaps, also to others who are interested in indigenous art forms more generally.

year: 2001-02