title: Can large taonga bivalves speed up recovery in degraded estuaries?

authors: Prinz, Natalie

abstract: THE QUESTION:
Will there introduction of adult, long-lived bivalves with differing functional traits speed up recovery of degraded soft sediment habitats in estuaries?
RESULTS:
Average bivalve survival after one year was 18% in + tuangi plot sand 59% in + hanikura plots. Sediment oxygen consumption (SOC) after one month was enhanced by 116% in treatments containing tuangi compared to control treatments. After one year those were similar to ambient levels, still showed higher SOC than control plots.

text: Can large taonga bivalves speed up recovery in degraded estuaries? THE QUESTION:
Will there introduction of adult, long-lived bivalves with differing functional traits speed up recovery of degraded soft sediment habitats in estuaries?
RESULTS:
Average bivalve survival after one year was 18% in + tuangi plot sand 59% in + hanikura plots. Sediment oxygen consumption (SOC) after one month was enhanced by 116% in treatments containing tuangi compared to control treatments. After one year those were similar to ambient levels, still showed higher SOC than control plots.

year: 2023

title: A collaborative approach to improving youth mental health.

authors: Goodwin, Debbie Waireka Tuhi

subjects: Maori

abstract: Nga Taiohi Whai Marama / Youth Connex was developed collaboratively by three organisations: Health Waikato Mental Health, Te Runanga o Kirikiriroa, and Linkage. These organisations had a vision of creating greater integration and improved pathways between youth and mental health services, as well as providing a service explicitly based on youth-friendly principles. The key aims of Whai Marama Youth Connex are to improve youth’s access to services and contribute to the development of a youth service-provider network. To fulfil this we aim to provide a range of services, integrated pathways and capacity building on several levels, the client level, the provider level and the funder level. Debbie Goodwin (Tuhoe) was employed as the Manager of the service and has a key role in developing the organisation, planning and shaping its services, and employing and managing its’ staff. She will give an overview of how the service is developing in partnership and biculturally, how youth-friendly principles are enacted, and what some of the key issues have been in its early stages.

text: A collaborative approach to improving youth mental health. Nga Taiohi Whai Marama / Youth Connex was developed collaboratively by three organisations: Health Waikato Mental Health, Te Runanga o Kirikiriroa, and Linkage. These organisations had a vision of creating greater integration and improved pathways between youth and mental health services, as well as providing a service explicitly based on youth-friendly principles. The key aims of Whai Marama Youth Connex are to improve youth’s access to services and contribute to the development of a youth service-provider network. To fulfil this we aim to provide a range of services, integrated pathways and capacity building on several levels, the client level, the provider level and the funder level. Debbie Goodwin (Tuhoe) was employed as the Manager of the service and has a key role in developing the organisation, planning and shaping its services, and employing and managing its’ staff. She will give an overview of how the service is developing in partnership and biculturally, how youth-friendly principles are enacted, and what some of the key issues have been in its early stages.

year: 2003

title: Ages on weathered Plio-Pleistocene tephra sequences, western North Island, New Zealand

authors: Lowe, David J.

subjects: tephra

abstract: Using the zircon fission-track method, we have obtained five ages on members of two strongly-weathered silicic, Pliocene-Pleistocene tephra sequences, the Kauroa and Hamilton Ash formations, in western North Island, New Zealand. These are the first numerical ages to be obtained directly on these deposits. Of the Kauroa Ash sequence, member K1 (basal unit) was dated at 2.24 ± 0.29 Ma, confirming a previous age of c. 2.25 Ma obtained (via tephrochronology)from K/Ar ages on associated basalt lava. Members K2 and K3 gave indistinguishable ages between 1.68 ± 0.12 and 1.43 ± 0.17 Ma. Member K12, a correlative of Oparau Tephra and probably also Ongatiti Ignimbrite, was dated at 1.28 ± 0.11 Ma, consistent with an age of 1.23 ± 0.02 Ma obtained by various methods on Ongatiti Ignimbrite. Palaeomagnetic measurements indicated that members K13 to K15 (top unit, Waiterimu Ash) are aged between c. 1.2 Ma and 0.78 Ma. Possible sources of the Kauroa Ash Formation include younger volcanic centres in the southern Coromandel Volcanic Zone or older volcanic centres in the Taupo Volcanic Zone, or both. Of the Hamilton Ash sequence, the basal member Ohinewai Ash (HI) was dated at 0.38 ± 0.04 Ma. This age matches those obtained by various methods on Rangitawa Tephra of 0.34-0.35 Ma, supporting correlation with this Whakamaru-caldera derived deposit. The origin of the other Hamilton Ash beds is unknown but various younger volcanic centres in the Taupo Volcanic Zone are possible sources. The topmost member, Tikotiko Ash (H6-H7), is estimated to be aged between c. 0.18 and 0.08 Ma. Various silicic pyroclastic deposits documented in North Island and in marine cores may be co-eval with members of the Kauroa Ash and Hamilton Ash sequences on the basis of their age.

text: Ages on weathered Plio-Pleistocene tephra sequences, western North Island, New Zealand Using the zircon fission-track method, we have obtained five ages on members of two strongly-weathered silicic, Pliocene-Pleistocene tephra sequences, the Kauroa and Hamilton Ash formations, in western North Island, New Zealand. These are the first numerical ages to be obtained directly on these deposits. Of the Kauroa Ash sequence, member K1 (basal unit) was dated at 2.24 ± 0.29 Ma, confirming a previous age of c. 2.25 Ma obtained (via tephrochronology)from K/Ar ages on associated basalt lava. Members K2 and K3 gave indistinguishable ages between 1.68 ± 0.12 and 1.43 ± 0.17 Ma. Member K12, a correlative of Oparau Tephra and probably also Ongatiti Ignimbrite, was dated at 1.28 ± 0.11 Ma, consistent with an age of 1.23 ± 0.02 Ma obtained by various methods on Ongatiti Ignimbrite. Palaeomagnetic measurements indicated that members K13 to K15 (top unit, Waiterimu Ash) are aged between c. 1.2 Ma and 0.78 Ma. Possible sources of the Kauroa Ash Formation include younger volcanic centres in the southern Coromandel Volcanic Zone or older volcanic centres in the Taupo Volcanic Zone, or both. Of the Hamilton Ash sequence, the basal member Ohinewai Ash (HI) was dated at 0.38 ± 0.04 Ma. This age matches those obtained by various methods on Rangitawa Tephra of 0.34-0.35 Ma, supporting correlation with this Whakamaru-caldera derived deposit. The origin of the other Hamilton Ash beds is unknown but various younger volcanic centres in the Taupo Volcanic Zone are possible sources. The topmost member, Tikotiko Ash (H6-H7), is estimated to be aged between c. 0.18 and 0.08 Ma. Various silicic pyroclastic deposits documented in North Island and in marine cores may be co-eval with members of the Kauroa Ash and Hamilton Ash sequences on the basis of their age.

year: 2001