title: Sustaining Management of Indigenous-Owned Resources: rationale for multi-dimensional training in a multi-million dollar mahogany industry in Fiji

authors: Nabalarua, Eci K

subjects: Fiji economy

abstract: This paper contributes to an emerging discourse relating to new pathways towards engaging in holistic development measures among grassroots communities in the Pacific Islands by using the notion of critical mass as a viable option for sustaining real growth in small rural economies. It is argued here that the multi-dimensional training techniques applied in the case of a project involving capacity building among indigenous women in Tailevu Province in Fiji could be applied with equal validity to the multi-million dollar mahogany industry in Fiji. This insight into mahogany suggests by implication that multi-dimensional training has great potential for sustaining effective management of indigenous-based and indigenous-owned resources.

text: Sustaining Management of Indigenous-Owned Resources: rationale for multi-dimensional training in a multi-million dollar mahogany industry in Fiji This paper contributes to an emerging discourse relating to new pathways towards engaging in holistic development measures among grassroots communities in the Pacific Islands by using the notion of critical mass as a viable option for sustaining real growth in small rural economies. It is argued here that the multi-dimensional training techniques applied in the case of a project involving capacity building among indigenous women in Tailevu Province in Fiji could be applied with equal validity to the multi-million dollar mahogany industry in Fiji. This insight into mahogany suggests by implication that multi-dimensional training has great potential for sustaining effective management of indigenous-based and indigenous-owned resources.

year: 2002-07-22

title: Textural variations in Neogene pelagic carbonate ooze at DSDP Site 593, southern Tasman Sea, and their paleoceanographic implications

authors: Cooke, Penelope J.

subjects: Tasman Sea

abstract: Changes in Neogene sediment texture in pelagic carbonate-rich oozes on the Challenger Plateau, southern Tasman Sea, are used to infer changes in depositional paleocurrent velocities. The most obvious record of textural change is in the mud:sand ratio. Increases in the sand content are inferred to indicate a general up-core trend towards increasing winnowing of sediments resulting from increasing flow velocity of Southern Component Intermediate Water (SCIW), the forerunner of Antarctic Intermediate Water. In particular, the intervals c. 19-14.5 Ma, c. 9.5-8 Ma, and after 5 Ma are suggested to be times of increased SCIW velocity and strong sediment winnowing. Within the mud fraction, the fine silt to coarse clay sizes from 15.6 to 2 µm make the greatest contribution to the sediments and are composed of nannofossil plates. During extreme winnowing events it is the fine silt to very coarse clay material (13-3 µm) within this range that is preferentially removed, suggesting the 10 µm cohesive silt boundary reported for siliciclastic sediments does not apply to calcitic skeletal grains. The winnowed sediment comprises coccolithophore placoliths and spheres, represented by a mode at 4-7 µm.
Further support for seafloor winnowing is gained from the presence in Hole 593 of a condensed sedimentary section from c. 18 to 14 Ma where the sand content increases to c. 20% of the bulk sample. Associated with the condensed section is a 6 m thick orange unit representing sediments subjected to particularly oxygen-rich, late early to early middle Miocene SCIW. Together these are inferred to indicate increased SCIW velocity resulting in winnowed sediment associated with faster arrival of oxygen-rich surface water subducted to form SCIW. Glacial development of Antarctica has been recorded from many deep-sea sites, with extreme glacials providing the mechanism to increase watermass flow. Miocene glacial zones Mi1b-Mi6 are identified in an associated oxygen isotope record from Hole 593, and correspond with times of particularly invigorated paleocirculation, bottom winnowing, and sediment textural changes.

text: Textural variations in Neogene pelagic carbonate ooze at DSDP Site 593, southern Tasman Sea, and their paleoceanographic implications Changes in Neogene sediment texture in pelagic carbonate-rich oozes on the Challenger Plateau, southern Tasman Sea, are used to infer changes in depositional paleocurrent velocities. The most obvious record of textural change is in the mud:sand ratio. Increases in the sand content are inferred to indicate a general up-core trend towards increasing winnowing of sediments resulting from increasing flow velocity of Southern Component Intermediate Water (SCIW), the forerunner of Antarctic Intermediate Water. In particular, the intervals c. 19-14.5 Ma, c. 9.5-8 Ma, and after 5 Ma are suggested to be times of increased SCIW velocity and strong sediment winnowing. Within the mud fraction, the fine silt to coarse clay sizes from 15.6 to 2 µm make the greatest contribution to the sediments and are composed of nannofossil plates. During extreme winnowing events it is the fine silt to very coarse clay material (13-3 µm) within this range that is preferentially removed, suggesting the 10 µm cohesive silt boundary reported for siliciclastic sediments does not apply to calcitic skeletal grains. The winnowed sediment comprises coccolithophore placoliths and spheres, represented by a mode at 4-7 µm.
Further support for seafloor winnowing is gained from the presence in Hole 593 of a condensed sedimentary section from c. 18 to 14 Ma where the sand content increases to c. 20% of the bulk sample. Associated with the condensed section is a 6 m thick orange unit representing sediments subjected to particularly oxygen-rich, late early to early middle Miocene SCIW. Together these are inferred to indicate increased SCIW velocity resulting in winnowed sediment associated with faster arrival of oxygen-rich surface water subducted to form SCIW. Glacial development of Antarctica has been recorded from many deep-sea sites, with extreme glacials providing the mechanism to increase watermass flow. Miocene glacial zones Mi1b-Mi6 are identified in an associated oxygen isotope record from Hole 593, and correspond with times of particularly invigorated paleocirculation, bottom winnowing, and sediment textural changes.

year: 2004-12-01

title: How Māori precariate families navigate social services

authors: King, Delta

abstract: We are living in a period in which the increasingly precarious nature of employment and welfare support systems has dramatically amplified the hardships faced by many people.¹ Correspondingly, much still needs to be written about the rise of the precariat. ² International literature asserts that post World War II paid employment was commonly full-time and secure up until the 1970s, when the rise of more insecure work increased as neoliberal policies and globalisation began dominating public deliberations regarding work and social life. ³ Subsequent recessions across many OECD countries contributed to labour market transformations back towards increased 'flexibility' and- the casualisation of employment. These labour market shifts have resulted in insecure work and income situations for many households, which for some means frequent cycles of paid employment and welfare dependency. People experiencing such insecure employment face insecure and unliveable incomes while grappling with inadequate state support - these are the people increasingly known as 'the precariat'.

text: How Māori precariate families navigate social services We are living in a period in which the increasingly precarious nature of employment and welfare support systems has dramatically amplified the hardships faced by many people.¹ Correspondingly, much still needs to be written about the rise of the precariat. ² International literature asserts that post World War II paid employment was commonly full-time and secure up until the 1970s, when the rise of more insecure work increased as neoliberal policies and globalisation began dominating public deliberations regarding work and social life. ³ Subsequent recessions across many OECD countries contributed to labour market transformations back towards increased 'flexibility' and- the casualisation of employment. These labour market shifts have resulted in insecure work and income situations for many households, which for some means frequent cycles of paid employment and welfare dependency. People experiencing such insecure employment face insecure and unliveable incomes while grappling with inadequate state support - these are the people increasingly known as 'the precariat'.

year: 2017