The role of Egmont-sourced tephra in evaluating the paleoclimatic correspondence between the bio- and soil-stratigraphic records of central Taranaki, New Zealand-Reference-Cited by-同舟云学术

The role of Egmont-sourced tephra in evaluating the paleoclimatic correspondence between the bio- and soil-stratigraphic records of central Taranaki, New Zealand

Published:1992-01 Issue: Volume:13-14 Page:187-194
ISSN:1040-6182
Container-title:Quaternary International
language:en
Short-container-title:Quaternary International

Author:

Alloway Brent V.,McGlone Matthew S.,Neall Vincent E.,Vucetich Colin G.

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference12 articles.

1. Late Quaternary cover bed stratigraphy and tephrochronology of north-eastern and central Taranaki, New Zealand;Alloway,1989

2. Climatic changes of the last 18,000 years: Observations and model simulations;Anderson;Science,1988

3. Submarine evidence from New Zealand of a rapid rise in sea level at 11,000 years B.P.;Cullen;Palaeogeography, Palaeoclimatology, Palaeoecology,1967

4. Late Quaternary palynology of the southern Ruahine Range, North Island, New Zealand;Lees;New Zealand Journal of Botany,1986

5. The Ascarina decline and post-glacial climatic change in New Zealand;McGlone;New Zealand Journal of Botany,1977

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