Stable isotope analysis and temperature reconstruction data from DSDP Hole 94-609B and ODP Hole 162-984B

The Greenland ice sheet is accepted as a key factor controlling the Quaternary glacial scenario. However, the origin and mechanisms of major Arctic glaciation starting at 3.15 Ma and culminating at 2.74 Ma are still controversial. For this phase of intense cooling Ravelo et al. proposed a complex gr...

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Bibliographic Details
Main Authors: Bartoli, Gretta, Sarnthein, Michael, Weinelt, Mara, Erlenkeuser, Helmut, Garbe-Schönberg, Dieter, Lea, David W
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.484677
https://doi.org/10.1594/PANGAEA.484677