Upwelling generates a nutrient-rich “cold tongue” within the jap equatorial Pacific Ocean (EEP), with impacts on world local climate, oceanic biological productivity, and the carbon cycle. The cold tongue used to be reduced for the length of the Pliocene Epoch, a feature …
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- Persistent jap equatorial Pacific Ocean upwelling since the nice and comfortable Pliocene | Science
Persistent jap equatorial Pacific Ocean upwelling since the nice and comfortable Pliocene | Science
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