Abstract
AbstractSea surface temperatures (SSTs) of the tropical Pacific Ocean exert powerful controls on regional and global climates. Previous studies have suggested that during warm climate phases, the east‐west temperature gradient collapsed. To date, there has been no high‐resolution reconstruction of sea surface conditions in both the east and west Pacific Ocean during the Miocene Climate Optimum (MCO) and across the middle Miocene climate transition (MMCT); therefore, our understanding of the mean oceanographic state during this major global climatic shift is limited. Here, we present new SST reconstructions for the eastern Pacific Ocean (15.5–13.3 Ma) which show a clear east‐west temperature gradient of ∼4°C during the warmest interval of the Neogene, implying that the oceanographic processes that produce the modern gradient were present and active. There is no shift in the east‐west gradient across the MMCT indicating that the gradient was not impacted by global cooling and ice growth. We find a 2°C sea surface cooling in the eastern equatorial Pacific, that lags the benthic foraminiferal δ18O positive shift by 150 kyr, indicating that tropical temperature did not decrease synchronously with the expansion of the Antarctic ice sheet. Reconstructed variations in the δ18O composition of seawater, determined by combining our Mg/Ca and δ18O records, reveal a freshening in the eastern Pacific Ocean after 13.8 Ma, suggesting changes in the hydrological cycle and in tropical fronts in response to the new icehouse regime.
Highlights
The Pacific Ocean is a key component of the global climate system as it represents the world's largest oceanic source of water vapor and CO2 to the atmosphere, and substantially influences global atmospheric circulation patterns (Lea et al, 2000)
Surface water conditions in the tropical Pacific Ocean are characterized by a strong east-west (E-W) gradient in sea surface temperatures (SSTs) (∼4°C–5°C offset) and in thermocline depth (∼50 m in the Eastern Equatorial Pacific (EEP) vs. >150 m in the Western Equatorial Pacific), with a tight coupling of the thermocline and nutricline (Lea et al, 2000; Nathan & Leckie, 2009)
Given that ice volume changes would impact δ18O in both planktonic and benthic foraminifera at the same time and to the same extent, the minor δ18O variations of in the planktonic foraminifera data would suggest the δ18O record is counterbalanced by surface water salinity variations
Summary
The Pacific Ocean is a key component of the global climate system as it represents the world's largest oceanic source of water vapor and CO2 to the atmosphere, and substantially influences global atmospheric circulation patterns (Lea et al, 2000). The formation of the modern circulation system in the tropical Pacific Ocean is believed to have developed at around ∼12 Ma in response to the tectonic constriction of the Indonesian and Central American seaways. These events resulted in the restriction of Indonesian Throughflow and the development of a “proto-warm pool” in the west Pacific Ocean (Matsui et al, 2017; Nathan & Leckie, 2009), whereas trans-equatorial Pacific circulation existed prior to this (Kennett et al, 1985).
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