Page 2: 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.

When tropical oceans were oxygen oases

Research reveals when and why ancient tropical seas transitioned from oxygen oases to marine dead zones, providing clues to the long-term evolution of oceanic environments.

What past global warming reveals about future rainfall

To understand how global warming could influence future climate, scientists look to the Paleogene Period that began 66 million years ago, covering a time when Earth's atmospheric carbon dioxide levels were two to four times ...

How oxygen first reached Earth's oceans

For roughly 2 billion years of Earth's early history, the atmosphere contained no oxygen, the essential ingredient required for complex life. Oxygen began building up during the period known as the Great Oxidation Event (GOE), ...

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