title: Re-identification of c. 15 700 cal yr BP tephra bed at Kaipo Bog, eastern North Island: implications for dispersal of Rotorua and Puketarata tephra beds.

authors: Shane, Phil A.R.

subjects: Tephra

abstract: A 10 mm thick, c. 15 700 calendar yr BP (c. 13 100 14C yr BP) rhyolitic tephra bed in the well-studied montane Kaipo Bog sequence of eastern North Island was previously correlated with Maroa-derived Puketarata Tephra. We revise this correlation to Okataina-derived Rotorua Tephra based on new compositional data from biotite phenocrysts and glass. The new correlation limits the known dispersal of Puketarata Tephra (sensu stricto, c. 16 800 cal yr BP) and eliminates requirements to either reassess its age or to invoke dual Puketarata eruptive events. Our data show that Rotorua Tephra comprises two glass-shard types: an early-erupted low-K2O type that was dispersed mostly to the northwest, and a high-K2O type dispersed mostly to the south and southeast, contemporary with late-stage lava extrusion. Late-stage Rotorua eruptives contain biotite that is enriched in FeO compared with biotite from Puketarata pyroclastics. The occurrence of Rotorua Tephra in Kaipo Bog (100 km from the source) substantially extends its known distribution to the southeast. Our analyses demonstrate that unrecognised syn-eruption compositional and dispersal changes can cause errors in fingerprinting tephra deposits. However, the compositional complexity, once recognised, provides additional fingerprinting criteria, and also documents magmatic and dispersal processes.

text: Re-identification of c. 15 700 cal yr BP tephra bed at Kaipo Bog, eastern North Island: implications for dispersal of Rotorua and Puketarata tephra beds. A 10 mm thick, c. 15 700 calendar yr BP (c. 13 100 14C yr BP) rhyolitic tephra bed in the well-studied montane Kaipo Bog sequence of eastern North Island was previously correlated with Maroa-derived Puketarata Tephra. We revise this correlation to Okataina-derived Rotorua Tephra based on new compositional data from biotite phenocrysts and glass. The new correlation limits the known dispersal of Puketarata Tephra (sensu stricto, c. 16 800 cal yr BP) and eliminates requirements to either reassess its age or to invoke dual Puketarata eruptive events. Our data show that Rotorua Tephra comprises two glass-shard types: an early-erupted low-K2O type that was dispersed mostly to the northwest, and a high-K2O type dispersed mostly to the south and southeast, contemporary with late-stage lava extrusion. Late-stage Rotorua eruptives contain biotite that is enriched in FeO compared with biotite from Puketarata pyroclastics. The occurrence of Rotorua Tephra in Kaipo Bog (100 km from the source) substantially extends its known distribution to the southeast. Our analyses demonstrate that unrecognised syn-eruption compositional and dispersal changes can cause errors in fingerprinting tephra deposits. However, the compositional complexity, once recognised, provides additional fingerprinting criteria, and also documents magmatic and dispersal processes.

year: 2003-12-01

title: Radiocarbon and linguistic dates for occupation of the South Wellesley Islands, Northern Australia

authors: Ulm, Sean

subjects: radiocarbon dates

abstract: Radiocarbon dates from three Kaiadilt Aboriginal sites on the South Wellesley Islands, southern Gulf of Carpentaria, demonstrate occupation dating to c.1600 years ago. These results are at odds with published linguistic models for colonisation of the South Wellesley archipelago suggesting initial occupation in the last 1000 years, but are consonant with archaeological evidence for post-4200 BP occupation of islands across northern Australia, particularly in the last 2000 years.

text: Radiocarbon and linguistic dates for occupation of the South Wellesley Islands, Northern Australia Radiocarbon dates from three Kaiadilt Aboriginal sites on the South Wellesley Islands, southern Gulf of Carpentaria, demonstrate occupation dating to c.1600 years ago. These results are at odds with published linguistic models for colonisation of the South Wellesley archipelago suggesting initial occupation in the last 1000 years, but are consonant with archaeological evidence for post-4200 BP occupation of islands across northern Australia, particularly in the last 2000 years.

year: 2010

title: Five imperial adventures in the Waikato

authors: Moffat, Kirstine

abstract: Some late nineteenth-century exponents of the 'Novel of Adventure', or imperial adventure-romance, regarded colonial New Zealand as an attractive canvas for their tales of masculine daring in an exotic, rugged environment.3 Five such authors set their narratives, in part or in full, in the Waikato of the 1860s, drawn to the backdrop of inter-racial conflict provided by the New Zealand Wars. While references to specific events and people associated with colonial Waikato do ground many of these texts in historical reality, it has to be said that, regardless of whether the authors write from experience, careful research, or flights of imaginative fantasy, the Waikato that is described in their narratives has been selected for its frontier possibilities rather than its distinctive geography.

text: Five imperial adventures in the Waikato Some late nineteenth-century exponents of the 'Novel of Adventure', or imperial adventure-romance, regarded colonial New Zealand as an attractive canvas for their tales of masculine daring in an exotic, rugged environment.3 Five such authors set their narratives, in part or in full, in the Waikato of the 1860s, drawn to the backdrop of inter-racial conflict provided by the New Zealand Wars. While references to specific events and people associated with colonial Waikato do ground many of these texts in historical reality, it has to be said that, regardless of whether the authors write from experience, careful research, or flights of imaginative fantasy, the Waikato that is described in their narratives has been selected for its frontier possibilities rather than its distinctive geography.

year: 2013