Page 7: Research news on paleoceanography

Paleoceanography is the scientific study of past ocean states, processes, and variability on geological timescales, using physical, chemical, biological, and isotopic proxies preserved in marine sediments, microfossils, corals, and other archives. It reconstructs parameters such as sea-surface and deep-water temperatures, salinity, circulation patterns, biogeochemical cycles, ice volume, and sea level, often through analyses of stable and radiogenic isotopes, trace metals, and sedimentological characteristics. Paleoceanography is central to understanding ocean–climate feedbacks, carbon cycle dynamics, and the response of the ocean system to external forcings, and it provides critical boundary conditions and validation targets for climate and Earth system models.

An ancient warming event may have lasted longer than we thought

Fifty-six million years ago, during the Paleocene-Eocene Thermal Maximum (PETM), global temperatures rose by more than 5°C over 100,000 or more years. Between 3,000 and 20,000 petagrams of carbon were released into the atmosphere ...

Earth's oceans once turned green—and they could change again

Nearly three-fourths of Earth is covered by oceans, making the planet look like a pale blue dot from space. But Japanese researchers have made a compelling case that Earth's oceans were once green, in a study published in ...

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