Post-Last Glacial Maximum fluvial incision and sediment generation in the unglaciated Waipaoa catchment, North Island, New Zealand

Geomorphology ◽  
2014 ◽  
Vol 214 ◽  
pp. 283-306 ◽  
Author(s):  
M. Marden ◽  
H. Betts ◽  
A. Palmer ◽  
R. Taylor ◽  
E. Bilderback ◽  
...  
Keyword(s):  
New Zealand ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Last Glacial ◽  
Fluvial Incision

scholarly journals A palaeoenvironmental record of the Southern Hemisphere last glacial maximum from the Mount Cass loess section, North Canterbury, Aotearoa/New Zealand

2020 ◽  
pp. 1-15
Author(s):  
Peter C. Almond ◽  
Sándor Gulyás ◽  
Pál Sümegi ◽  
Balázs P. Sümegi ◽  
Stephen Covey-Crump ◽  
...  
Keyword(s):  
New Zealand ◽  
Southern Hemisphere ◽  
Last Glacial Maximum ◽  
Climatic Variability ◽  
Glacial Maximum ◽  
Pollen Record ◽  
Good Correspondence ◽  
Last Glacial ◽  
Event Stratigraphy ◽  
Westerly Winds

Abstract Calcareous loess in North Canterbury, eastern South Island, New Zealand (NZ), preserves subfossil bird bone, terrestrial gastropods, and eggshell, whose abundances and radiocarbon ages allowed us to reconstruct aspects of palaeoenvironment at high resolution through 25 to 21 cal ka BP. This interval includes millennial-scale climatic variability during the extended last glacial maximum (30–18 ka) of Australasia. Our loess palaeoclimatic record shows good correspondence with stadial and interstadial climate events of the NZ Climate Event Stratigraphy, which were defined from a pollen record on the western side of South Island. An interstade from 25.4 to 24 cal ka BP was warm but also relatively humid on eastern South Island, and loess grain size may indicate reduced vigour of the Southern Hemisphere westerly winds. The subsequent stade (24–22.6 cal ka BP) was drier, colder, and probably windier. The next interstade remained relatively dry on eastern South Island, and westerly winds remained vigorous. The 25.4–24 ka interstade is synchronous with Heinrich stade 2, which may have driven a southward migration of the subtropical front, leading to warming and wetting of northern and central South Island and retreat of Southern Alps glaciers at ca. 26.5 ka.

A review of New Zealand palaeoclimate from the Last Interglacial to the global Last Glacial Maximum

2015 ◽  
Vol 110 ◽  
pp. 92-106 ◽  
Author(s):  
Paul W. Williams ◽  
Matt McGlone ◽  
Helen Neil ◽  
Jian-Xin Zhao
Keyword(s):  
New Zealand ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Last Interglacial ◽  
Last Glacial

scholarly journals The Tekapo Glacier, New Zealand, during the Last Glacial Maximum: An active temperate glacier influenced by intermittent surge activity

Geomorphology ◽  
2019 ◽  
Vol 343 ◽  
pp. 183-210 ◽  
Author(s):  
Jenna L. Sutherland ◽  
Jonathan L. Carrivick ◽  
David J.A. Evans ◽  
James Shulmeister ◽  
Duncan J. Quincey
Keyword(s):  
New Zealand ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Export production in the New-Zealand region since the Last Glacial Maximum

2017 ◽  
Vol 469 ◽  
pp. 110-122 ◽  
Author(s):  
Axel Durand ◽  
Zanna Chase ◽  
Taryn L. Noble ◽  
Helen Bostock ◽  
Samuel L. Jaccard ◽  
...  
Keyword(s):  
New Zealand ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Export Production ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial

The Last Glacial Maximum at 44°S documented by a 10Be moraine chronology at Lake Ohau, Southern Alps of New Zealand

2013 ◽  
Vol 62 ◽  
pp. 114-141 ◽  
Author(s):  
Aaron E. Putnam ◽  
Joerg M. Schaefer ◽  
George H. Denton ◽  
David J.A. Barrell ◽  
Sean D. Birkel ◽  
...  
Keyword(s):  
New Zealand ◽  
Last Glacial Maximum ◽  
Southern Alps ◽  
Glacial Maximum ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial
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