Mg/Ca-derived temperature estimates for ODP Site 202-1236
Here we use Mg/Ca temperature estimates from subsurface and thermocline dwelling foraminifera to reconstruct the meridional Plio‐Pleistocene evolution of the Southeast Pacific thermocline, in relation to atmospheric circulation changes. Our data indicate a change in the thermocline, responding to th...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2018
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.896166 https://doi.org/10.1594/PANGAEA.896166 |
Summary: | Here we use Mg/Ca temperature estimates from subsurface and thermocline dwelling foraminifera to reconstruct the meridional Plio‐Pleistocene evolution of the Southeast Pacific thermocline, in relation to atmospheric circulation changes. Our data indicate a change in the thermocline, responding to the northward displacement of the Intertropical Convergence Zone/South Pacific High system between ~3.8 and 3.5 Ma. After 3.5 Ma, we record a second major phase of thermocline shoaling, which points to the ITCZ/SPH‐system movement toward its modern position along with the gradual cooling of the Northern Hemisphere and its associated glaciation. |
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