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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Melting Sea Ice and Drooping Corals
This blog was written by Ruth Teichroeb, a former journalist and communications professional at Oceans North and Ocean Conservancy. She is b...
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