Palynological and sedimentological evidence for a radiocarbon chronology of environmental change and Polynesian deforestation from Lakes Taumatawhana, Northland, New Zealand

Abstract

We present pollen diagrams and sedimentological analyses from a lake site within an extensive dune system on the Aupouri Peninsula. Five thousand years ago, a regional Agathis australis-podocarp-broadleaf forest dominated the vegetation, which manifested an increasing preponderance of conifer species. Climate was cooler and drier than at present. From ca. 3400 BP, warmth-loving species such as A. australis and drought-intolerant species, Dacrydium cupressinum and Ascarina lucida, became common, implying a warm and moist climate. The pollen record also suggests a windier climate. The most significant event in the record, however, occurred after ca. 900 BP (800 cal BP) when anthropogenic deforestation commenced. A dramatic decline in forest taxa followed. Fire almost certainly caused this.