Oceans

Overview

The Atlantic, Pacific, Indian, Arctic, and Southern Oceans are the interconnected bodies of salt water that cover about 71% of Earth's surface. Containing 97% of the planet's surface water, oceans harbor an estimated 2 million marine species, including the photosynthetic algae that produce half of all atmospheric oxygen. The oceans buffer against abrupt climate change and regulate and redistribute moisture and solar energy through interactions with the atmosphere, supporting widespread planetary biodiversity.

The water that formed the oceans is hypothesized to have been expelled from Earth's interior by volcanoes before condensing as precipitation, though some may have been delivered by comets and asteroids. Geologic dating of rocks formed only during underwater eruptions or when sediments accumulated in underwater layers indicates that oceans formed at least 3.8 billion years ago. These underwater volcanoes, alongside runoff of minerals from eroded rocks, continue to add salts to seawater, which many organisms extract to build shells and skeletons.

By absorbing more than 90% of the excess thermal energy trapped by greenhouse gases, the oceans fuel extreme weather events, such as hurricanes, and can amplify climate patterns, such as El Niño. Oceans also absorb 30% of carbon dioxide emissions, with the resulting acidification threatening marine life, habitats, and food webs.

1440 Findings

Hours of research by our editors, distilled into minutes of clarity.

  • Posted by

    Just as landmasses have been divided into distinct nations, the world ocean has been divided into multiple oceans for various geographical, practical, and scientific reasons.

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    Earth's first oceans may have been as much as 230 degrees Celsius (446 degrees Fahrenheit), with atmospheric pressure preventing them from boiling.

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    Watch a visualization of global ocean currents from NASA's Estimating the Circulation and Climate of the Ocean project.

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    Surface ocean currents are primarily driven by wind, tides, and Earth's rotation, while deep-ocean currents are driven by differences in temperature and salt concentration.

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    The warmest waters in the ocean are found at hydrothermal vents—hot springs on the seafloor that discharge plumes of mineral-rich water.

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