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There is no other supporting archaeological evidence for human occupation.Sediment records show a huge increase in charcoal and bracken spores around the 13th and 14th centuries.His research focuses on new ways to measure, understand and model streamflow generation processes.Jeff co-edited the Elsevier textbook “Isotope Tracers in Catchment Hydrology”.Are you ready to meet someone who shares your values and lifestyle? Christchurch is emerging as a city renewed, in no small part due to the strength and optimism of its people.Indeed, the city has won world renown for being able to retain its opportunistic entrepreneurial edge and hopeful spirit in the face of hardship.

Delivered to you by leading scientists in groundwater age dating research from the world’s most accurate tritium and water dating lab – GNS Science Water Dating Research Laboratory (IAEA Inter-lab Comparison 2012).Only small, occasional fires occurred in the forests.These are shown by minor, temporary declines in pollen from tall forest and shrub species, along with increases in charcoal, and in spores and pollen from bracken, grasses and other pioneer species (the first plants to grow in a cleared area).Before people arrived, more than 80% of New Zealand was covered in dense forest.Pollen and charcoal records from over 150 lake, swamp or peat bog sediment core samples give a clear picture of the country’s vegetation and fire history since the end of the last ice age, about 14,000 years ago.