Shackleton, Nicholas J; Opdyke, Neil D (1977): Stable carbon record and paleomagnetic of sediment core V28-179. PANGAEA, https://doi.org/10.1594/PANGAEA.733937, Supplement to: Shackleton, NJ; Opdyke, ND (1977): Oxygen isotope and palaeomagnetic evidence for early Northern Hemisphere glaciation. Nature, 270, 216-219, https://doi.org/10.1038/270216a0
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Oxygen isotope and palaeomagnetic analysis of the lower half of LDGO piston core V28-179 shows that glacial-interglacial fluctuations have characterised Eart's climate for the past 3.2 Myr, before shich there was a period of stable 'interglacial' or 'preglacial' climate. The scale of glaciations increased about 2.5 Myr ago.
Latitude: 4.617000 * Longitude: -139.600000
Date/Time Start: 1971-02-25T00:00:00 * Date/Time End: 1971-02-25T00:00:00
Datasets listed in this publication series
- Shackleton, NJ; Opdyke, ND (1977): (Table 1) Magnetic boundaries of sediment core V28-179. https://doi.org/10.1594/PANGAEA.733935
- Shackleton, NJ; Opdyke, ND (1977): (Table 2) Stable carbon and oxygen isotope ratios of Globocassidulina subglobosa from sediment core V28-179. https://doi.org/10.1594/PANGAEA.733936