Logo image
A late Quaternary vegetation history for far northern New Zealand
Journal article   Peer reviewed

A late Quaternary vegetation history for far northern New Zealand

J.R. Dodson, N.J. Enright and R.F. McLean
Journal of Biogeography, Vol.15(4), pp.647-656
1988
url
Link to Published Version *Subscription may be requiredView

Abstract

Pollen diagrams are described for 2 sites near Cape Regina from far N North Island. Forest persisted throughout the last 17 000 yr and while initially containing cooler elements change indicating a maximum in diversity and complexity was attained between 10 000-6800 BP. This was the warmest and probably most mesic environment represented in the record. Nothofagus was never an important element and Dacrydium cupressinum, Podocarpus spp. and tree ferns dominated throughout. Agathis australis expanded from c11 500 BP but declined after 3000 BP, perhaps associated with increased droughtiness. Shrubland also occurred throughout the record; natural fire was an important component in their function. Fire incidence increased in the recent past suggesting it was an agent in forest destruction following human occupance

Details

UN Sustainable Development Goals (SDGs)

This output has contributed to the advancement of the following goals:

#13 Climate Action

Source: InCites

Metrics

InCites Highlights

These are selected metrics from InCites Benchmarking & Analytics tool, related to this output

Collaboration types
Domestic collaboration
International collaboration
Citation topics
8 Earth Sciences
8.93 Archaeology
8.93.8 Holocene
Web Of Science research areas
Ecology
Geography, Physical
ESI research areas
Environment/Ecology
Logo image