Isotope records from the Southern Ocean imply that prolonged epochs of time between glacial and interglacial periods through the Mid-Pleistocene Transition were caused by a reduction in deep waters mixing with the surface and the positive feedback it created with the salinity gradient.
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What is the High Seas Treaty and Why Does It Matter?
You may have seen headlines recently about a new global treaty that went into effect just as news broke that the United States would be with...
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