Up to fifty tephras, ranging in age from ca. 500 to 50 ka, are recorde
d in a terrestrial sequence of loess and paleosols in the eastern Bay
of Plenty, North Island, New Zealand. Tephra correlations are based on
the distinctive physical characteristics of the airfall beds and conf
irmed by microprobe analysis of glass shards. The deposits are divided
into six subgroups with their boundaries marked by either major tephr
as or significant changes in the paleo-climate indicator deposits such
as loess and paleosols. Age control on these tephras has been provide
d by fitting the paleoclimatic data seen in the field to the SPECMAP o
xygen isotope curve, with correlations to a few well dated tephras and
ignimbrites providing key time planes within this record. Copyright (
C) 1996 INQUA/Elsevier Science Ltd