| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5780133 | Earth and Planetary Science Letters | 2017 | 9 Pages |
Abstract
- New Zealand climate since Oligocene time is inferred from >2300 pollen samples.
- Oligocene warming until peak warmth of middle Miocene, cooling through late Neogene.
- Seasonality increased after middle Miocene, as winters cooled through the Neogene.
- Record reflects greater range of biomes following late Neogene mountain uplift.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Joseph G. Prebble, Tammo Reichgelt, Dallas C. Mildenhall, David R. Greenwood, J. Ian Raine, Elizabeth M. Kennedy, Hannu C. Seebeck,