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 |
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Qualification | Doctor of Philosophy |
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Award date | 27 May 2016 |
Place of Publication | Utrecht |
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Print ISBNs | 978-90-6266-425-2 |
Publication status | Published - 27 May 2016 |