Environmental magnetic implications of magnetofossil occurrence during the Middle Eocene Climatic Optimum (MECO) in pelagic sediments from the equatorial Indian Ocean
Magnetic properties of pelagic marine sediments that record the Middle Eocene Climatic Optimum (MECO) at ~. 40. Ma provide information about major environmental changes. The main variations observed during this transient warming event reflect a bacterial magnetofossil signal, but the cause of the linkage between bacterial production and climate remains unclear. We present an environmental magnetic study of middle Eocene deep-sea sediments from the northern edge of Madingley Rise (Ocean Drilling...[Show more]
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|Source:||Palaeogeography, Palaeoclimatology, Palaeoecology|
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