title: Culture and climate change: A study of future-proofing Māori tourism businesses

authors: Tawhai, Crystal Candace

subjects: culture

abstract: This thesis explores how prepared Māori tourism businesses are to adapt to climate change and how Māori values may influence the business's perception of responses to climate change. As climate impacts are growing in New Zealand, as a result of increasing extreme weather events, how can Māori tourism businesses protect their taonga (resources)? Taonga in the context of this study includes Māori values, lands, seas and their businesses. Furthermore, the literature indicates that Māori tourism significantly contributes to the economic, social and cultural wellbeing for Māori and wider New Zealand (NZ Māori Tourism, 2018). 
At a specific level, the study focuses on three Māori tourism businesses. Two of the businesses are North Island-based whānau-owned enterprises, one on Kāpiti Island and the other in Napier. The third is a hapū-owned business located in Kaikoura in the South Island. Drawing on kaupapa Māori frameworks built on Māori struggles for tino rangatiratanga and mana motuhake (self-determination), the study adheres to kaupapa Māori principles of carrying out research by Māori to benefit Māori. The primary data for the study was collected through semi-structured interviews with each of the businesses, taking care to ensure the cultural safety of the participants and using appropriate tikanga (protocol) in each interview. 

The findings of the study show that Māori tourism businesses are adapting to environmental changes but are unsure about the pace of climate change. The uncertainties are due to a lack of access to information and competing priorities within their businesses. The research also shows how decisions made by local government as well as business perceptions of local and central government institutions negatively impacts on the ability of businesses to adapt to climate change. While there were differences in the businesses’ treatment of science and scientific information, all of them prioritised Māori cultural values. Significantly, these values underpin all the activities of the businesses, including, environmental enhancement and protection. An emphasis on Māori values in facilitated partnerships between tourism businesses, government bodies, and other community stakeholders on co-designing climate change adaptation strategies can help the tourism sector to prepare for a changing climate.

text: Culture and climate change: A study of future-proofing Māori tourism businesses This thesis explores how prepared Māori tourism businesses are to adapt to climate change and how Māori values may influence the business's perception of responses to climate change. As climate impacts are growing in New Zealand, as a result of increasing extreme weather events, how can Māori tourism businesses protect their taonga (resources)? Taonga in the context of this study includes Māori values, lands, seas and their businesses. Furthermore, the literature indicates that Māori tourism significantly contributes to the economic, social and cultural wellbeing for Māori and wider New Zealand (NZ Māori Tourism, 2018). 
At a specific level, the study focuses on three Māori tourism businesses. Two of the businesses are North Island-based whānau-owned enterprises, one on Kāpiti Island and the other in Napier. The third is a hapū-owned business located in Kaikoura in the South Island. Drawing on kaupapa Māori frameworks built on Māori struggles for tino rangatiratanga and mana motuhake (self-determination), the study adheres to kaupapa Māori principles of carrying out research by Māori to benefit Māori. The primary data for the study was collected through semi-structured interviews with each of the businesses, taking care to ensure the cultural safety of the participants and using appropriate tikanga (protocol) in each interview. 

The findings of the study show that Māori tourism businesses are adapting to environmental changes but are unsure about the pace of climate change. The uncertainties are due to a lack of access to information and competing priorities within their businesses. The research also shows how decisions made by local government as well as business perceptions of local and central government institutions negatively impacts on the ability of businesses to adapt to climate change. While there were differences in the businesses’ treatment of science and scientific information, all of them prioritised Māori cultural values. Significantly, these values underpin all the activities of the businesses, including, environmental enhancement and protection. An emphasis on Māori values in facilitated partnerships between tourism businesses, government bodies, and other community stakeholders on co-designing climate change adaptation strategies can help the tourism sector to prepare for a changing climate.

year: 2020

title: Te Kōtihitihi: Ngā Tuhinga Reo Māori, Putanga 1

authors: Ngāpō, Korohere

abstract: Koinei te katoa o te Putanga 1 o te puka hautaka, Te Kōtihitihi.

text: Te Kōtihitihi: Ngā Tuhinga Reo Māori, Putanga 1 Koinei te katoa o te Putanga 1 o te puka hautaka, Te Kōtihitihi.

year: 2011-04

title: Provenance and geochemistry of exotic clasts in conglomerates of the Oligocene Torehina Formation, Coromandel Peninsula, New Zealand

authors: Nelson, Campbell S.

subjects: Coromandel Peninsula

abstract: Non-marine pebble to cobble conglomerates of the lower Torehina Formation (Oligocene) crop out along western Coromandel Peninsula and overlie, with strong angular discordance, continental-margin metasedimentary rocks (Manaia Hill Group) of Mesozoic (Late Jurassic to ?Early Cretaceous) age. The conglomerates contain provenance information that identifies a pre-Oligocene depositional history obscured by the unconformable juxtaposition of these Tertiary and Mesozoic strata. Most clasts in the lower Torehina Formation are visually similar to local bedrock lithologies, including metamorphosed sandstones and argillites, but are kaolinitic and contain more detrital and authigenic chert, quartz, and potash feldspar. Local derivation of these clasts seems unlikely. By comparing geochemical ratios with those defined for continental margin sandstones, and well characterised New Zealand tectonic terranes, we interpret the majority of clasts in the lower Torehina Formation to have been derived from a dissected orogen, with mixtures of felsic and volcanogenic-derived sediment. The most likely sources are the Waipapa and Torlesse Terranes. The remaining 20–30% of the clasts in the lower Torehina Formation were originally friable, are coarse grained, and appear to be lithologically exotic relative to known metamorphosed sandstones in basement terrane sources on North Island. Some clasts contain coal laminae and particles, and all contain detrital kaolinite as lithic fragments and matrix. Such characteristics imply a non-marine to marginal-marine source containing sediment derived from strongly weathered granite or granodiorite. Mechanical fragility implies a likely proximal, easily erodible source. We propose that this group of clasts was derived from an Upper Cretaceous sedimentary cover, either part of a locally developed basin fill or part of a once regionally extensive cover on North Island. Either case defines a more widely distributed Cretaceous source than found today.

text: Provenance and geochemistry of exotic clasts in conglomerates of the Oligocene Torehina Formation, Coromandel Peninsula, New Zealand Non-marine pebble to cobble conglomerates of the lower Torehina Formation (Oligocene) crop out along western Coromandel Peninsula and overlie, with strong angular discordance, continental-margin metasedimentary rocks (Manaia Hill Group) of Mesozoic (Late Jurassic to ?Early Cretaceous) age. The conglomerates contain provenance information that identifies a pre-Oligocene depositional history obscured by the unconformable juxtaposition of these Tertiary and Mesozoic strata. Most clasts in the lower Torehina Formation are visually similar to local bedrock lithologies, including metamorphosed sandstones and argillites, but are kaolinitic and contain more detrital and authigenic chert, quartz, and potash feldspar. Local derivation of these clasts seems unlikely. By comparing geochemical ratios with those defined for continental margin sandstones, and well characterised New Zealand tectonic terranes, we interpret the majority of clasts in the lower Torehina Formation to have been derived from a dissected orogen, with mixtures of felsic and volcanogenic-derived sediment. The most likely sources are the Waipapa and Torlesse Terranes. The remaining 20–30% of the clasts in the lower Torehina Formation were originally friable, are coarse grained, and appear to be lithologically exotic relative to known metamorphosed sandstones in basement terrane sources on North Island. Some clasts contain coal laminae and particles, and all contain detrital kaolinite as lithic fragments and matrix. Such characteristics imply a non-marine to marginal-marine source containing sediment derived from strongly weathered granite or granodiorite. Mechanical fragility implies a likely proximal, easily erodible source. We propose that this group of clasts was derived from an Upper Cretaceous sedimentary cover, either part of a locally developed basin fill or part of a once regionally extensive cover on North Island. Either case defines a more widely distributed Cretaceous source than found today.

year: 2003