Articles | Volume 2, issue 2
https://doi.org/10.5194/gchron-2-367-2020
https://doi.org/10.5194/gchron-2-367-2020
Research article
 | 
15 Dec 2020
Research article |  | 15 Dec 2020

Development of a multi-method chronology spanning the Last Glacial Interval from Orakei maar lake, Auckland, New Zealand

Leonie Peti, Kathryn E. Fitzsimmons, Jenni L. Hopkins, Andreas Nilsson, Toshiyuki Fujioka, David Fink, Charles Mifsud, Marcus Christl, Raimund Muscheler, and Paul C. Augustinus

Data sets

Beryllium-10 in sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand. Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C https://doi.org/10.1594/PANGAEA.920773

Rhyolitic tephra composition in sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand. Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C https://doi.org/10.1594/PANGAEA.921121

Basaltic tephra composition in sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand. Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C https://doi.org/10.1594/PANGAEA.921122

Paleomagnetic data from sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand. Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C https://doi.org/10.1594/PANGAEA.921134

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Short summary
Orakei Basin – a former maar lake in Auckland, New Zealand – provides an outstanding sediment record over the last ca. 130 000 years, but an age model is required to allow the reconstruction of climate change and volcanic eruptions contained in the sequence. To construct a relationship between depth in the sediment core and age of deposition, we combined tephrochronology, radiocarbon dating, luminescence dating, and the relative intensity of the paleomagnetic field in a Bayesian age–depth model.