Paleoceanography of the eastern equatorial Pacific over the past 4 million years and the geologic origins of modern Galápagos upwelling
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文摘
Paleo records show the modern SST gradient across the Galápagos emerged ∼1.6 Ma. Models confirm emergence of SST gradient is due to Galápagos blocking undercurrent. Implications for geological and biogeographical mysteries are discussed. Studies of Pliocene Pan-Pacific SST gradient should consider geologic forcing. Results support gradual development of the modern Pan-Pacific SST gradient.

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