Orbital- to millennial-scale variability in Gulf of Mexico sea surface temperature and salinity during the late Pleistocene
Sea surface temperature (SST) reconstructions from the low latitudes indicate the tropics/subtropics warmed significantly before glacial-interglacial decreases in global ice volume, suggesting the importance of tropical and subtropical climate in driving glacial terminations. ODP Site 625, drilled a...
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| Format: | Others |
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Scholar Commons
2008
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| Online Access: | https://scholarcommons.usf.edu/etd/561 https://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=1560&context=etd |