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.

Measuring deep-ocean oxygen with microscopic magnetic fossils

Humanity's ongoing disruption of atmospheric carbon dioxide (CO₂) concentrations, temperatures, and global nutrient cycles is starving the oceans of oxygen. Although we can measure ongoing changes to ocean circulation and ...

How ocean chemistry helped life keep breathing

Scientists have helped solve a longstanding mystery about how Earth remained habitable after oxygen first accumulated in its atmosphere more than 2 billion years ago, providing evidence that ancient ocean chemistry sustained ...

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