How do ocean floor sediments indicate past ocean temperatures?

How do ocean floor sediments indicate past ocean temperatures?

• A. By analyzing the color of sediment layers
• B. By examining fossilized marine life
• C. By analyzing the isotopic composition of oxygen in sediment cores
• D. By measuring sediment thickness

Answer: (C)

Sediments on the ocean floor can provide significant insights into past ocean temperatures, particularly through the analysis of the isotopic composition of oxygen in sediment cores. The ratio of oxygen isotopes, specifically oxygen-16 and oxygen-18, found in the calcium carbonate shells of marine organisms within the sediment cores reflects the temperature of the ocean at the time those organisms were alive. When ocean temperatures are warmer, the lighter isotope (oxygen-16) tends to preferentially evaporate, resulting in a higher prevalence of the heavier isotope (oxygen-18) in the seawater. Consequently, when marine organisms incorporate these oxygen isotopes into their shells, a shift in the ratio of these isotopes can be recorded in the sediments. By examining these ratios in core samples, scientists can reconstruct historical temperature profiles of the ocean, offering insights into climatic changes over geological timeframes. In contrast, while the color of sediment layers or sediment thickness may provide some information about environmental conditions, they do not directly indicate past temperatures. Fossilized marine life can also offer indirect clues about environmental conditions during specific periods, but the isotopic analysis is a more precise method for quantifying historical temperatures. Thus, the isotopic composition of oxygen serves as a robust and informative indicator of past

Sediments on the ocean floor can provide significant insights into past ocean temperatures, particularly through the analysis of the isotopic composition of oxygen in sediment cores. The ratio of oxygen isotopes, specifically oxygen-16 and oxygen-18, found in the calcium carbonate shells of marine organisms within the sediment cores reflects the temperature of the ocean at the time those organisms were alive.

When ocean temperatures are warmer, the lighter isotope (oxygen-16) tends to preferentially evaporate, resulting in a higher prevalence of the heavier isotope (oxygen-18) in the seawater. Consequently, when marine organisms incorporate these oxygen isotopes into their shells, a shift in the ratio of these isotopes can be recorded in the sediments. By examining these ratios in core samples, scientists can reconstruct historical temperature profiles of the ocean, offering insights into climatic changes over geological timeframes.

In contrast, while the color of sediment layers or sediment thickness may provide some information about environmental conditions, they do not directly indicate past temperatures. Fossilized marine life can also offer indirect clues about environmental conditions during specific periods, but the isotopic analysis is a more precise method for quantifying historical temperatures. Thus, the isotopic composition of oxygen serves as a robust and informative indicator of past