Abstract
The primary aim of this thesis is to reconstruct the evolution of the cryosphere, global ocean temperatures and the carbon cycle during the Oligocene-Miocene interval; using high-resolution foraminiferal stable isotope records with accurate chronological control provided by astronomically tuned age models.
| Original language | English |
|---|---|
| Qualification | Doctor of Philosophy |
| Awarding Institution |
|
| Supervisors/Advisors |
|
| Thesis sponsors | |
| Award date | 27 May 2016 |
| Place of Publication | Utrecht |
| Publisher | |
| Print ISBNs | 978-90-6266-425-2 |
| Publication status | Published - 27 May 2016 |