Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090
The cold upwelling 'tongue' of the eastern equatorial Pacific is a central energetic feature of the ocean, dominating both the mean state and temporal variability of climate in the tropics and beyond. Recent evidence for the development of the modern cold tongue during the Pliocene-Pleisto...
Main Authors: | , , , , |
---|---|
Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2010
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.771708 https://doi.org/10.1594/PANGAEA.771708 |