Geochemical and palynological results of IODP Hole 302-M0004A from Lomonosov Ridge, Arctic Ocean
Several episodes of abrupt and transient warming, each lasting between 50,000 and 200,000 years, punctuated the long-term warming during the Late Palaeocene and Early Eocene (58 to 51 Myr ago) epochs**1,2. These hyperthermal events, such as the Eocene Thermal Maximum 2 (ETM2) that took place about 5...
Main Authors: | , , , , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2010
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.735745 https://doi.org/10.1594/PANGAEA.735745 |