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.

Were Martian tides strong enough to shape its ancient landscape?

You're an anaerobic microbe sunbathing on a Martian beach billions of years ago listening to the small waves hit the shoreline as you take in the perchlorates in the Martian regolith. This is because while Mars is warm and ...

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