Palynofacies and sea-level changes in the Middle Coniacian–Late Campanian (Late Cretaceous) of the East Coast Basin, New Zealand

2002 ◽  
Vol 188 (3-4) ◽  
pp. 101-125 ◽  
Author(s):  
Poul Schiøler ◽  
James S Crampton ◽  
Malcolm G Laird
1988 ◽  
Vol 29 (2) ◽  
pp. 176-185 ◽  
Author(s):  
Brad Pillans ◽  
Geoff Holgate ◽  
Matt McGlone

Strata at Landguard Bluff, near Wanganui, New Zealand preserve a clear record of relative sea-level changes during oxygen-isotope stage 7. Two relative high sea-level stands (during stages 7a about 210,000 yr ago and 7c about 240,000 yr ago) are separated by a relative low sea level (stage 7b) that was at least 32 m lower than present. Pollen analysis of sediment deposited during stage 7b indicates climate at the time was up to 3°C cooler than present. The climate and sea-level evidence from Landguard Bluff are consistent with oxygen-isotopic evidence from deep-sea cores indicating a marked cooling during stage 7, which is closely associated with a summer radiation minimum centered at about 230,000 yr ago in the Northern Hemisphere.


1999 ◽  
Vol 152 (1-2) ◽  
pp. 101-127 ◽  
Author(s):  
James Shulmeister ◽  
Jane M. Soons ◽  
Glenn W. Berger ◽  
Margaret Harper ◽  
Sarah Holt ◽  
...  

2007 ◽  
Vol 247 (3-4) ◽  
pp. 357-381 ◽  
Author(s):  
F. Fluteau ◽  
Gilles Ramstein ◽  
Jean Besse ◽  
R. Guiraud ◽  
J.P Masse

2000 ◽  
Vol 178 (1) ◽  
pp. 147-176 ◽  
Author(s):  
M. R. House ◽  
V. V. Menner ◽  
R. T. Becker ◽  
G. Klapper ◽  
N. S. Ovnatanova ◽  
...  

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