(Table 1) Age control points used for paleomagnetic timescale at DSDP Site 94-607
For most of the Northern Hemisphere Ice Ages, from ~3.0 to 0.8 m.y., global ice volume varied predominantly at the 41,000 year period of Earth's orbital obliquity. However, summer (or summer caloric half year) insolation at high latitudes, which is widely believed to be the major influence on h...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
2003
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.842277 https://doi.org/10.1594/PANGAEA.842277 |