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Paleoceanographic proxies offer insights into past climate changes, oceanography, and biochemical cycles. These proxies serve as measurable indicators for unobservable environmental variables like temperature, salinity, and nutrient content. They are utilized similarly to oceanographic methods, where water masses are characterized by their physical and chemical properties and linked to specific organism assemblages or element distributions. A variety of established proxies are available; for example, marine microfossil assemblages help reconstruct surface-water temperatures. The calcareous shells of planktonic and benthic microorganisms contain valuable isotopic and elemental information. Stable oxygen isotope measurements can indicate ice volume, while Mg/Ca ratios correlate with water temperatures. Additionally, organic material can shed light on past productivity conditions; analyzing the stable carbon isotope composition of organic matter provides insights into historical surface-water CO2 levels, given certain assumptions. The field of paleoceanography is dynamic, with existing proxies evolving and new ones being researched and developed. Methodologies are enhanced through the analysis of water column samples, surface sediments, and laboratory experiments.
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Use of proxies in paleoceanography, Gerhard Fischer
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- 1999
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