Paleoceanography

Uses your system voice; voice and rate in settings.

Snapshot

≈ 1 min read

Names in other languages

No names in other languages are held for this entry yet.

Article bodies are English and are not machine-translated. A name in another language is not a translation of the article.

Paleoceanography is the study of the history of the oceans in the geologic past with regard to biology, chemistry, circulation, geology, and patterns of biological productivity and sedimentation. Paleoceanographic studies using environment models and different proxies enable the scientific community to assess the role of the oceanic processes in the global climate by the re-construction of past climate at various intervals. Paleoceanographic research is also intimately tied to paleoclimatology.

Paleoceanography is the study of the history of the oceans in the geologic past with regard to biology, chemistry, circulation, geology, and patterns of biological productivity and sedimentation. Paleoceanographic studies using environment models and different proxies enable the scientific community to assess the role of the oceanic processes in the global climate by the re-construction of past climate at various intervals. Paleoceanographic research is also intimately tied to paleoclimatology. \mathrm{Mg/Ca} = 0.867 \pm 0.049*\exp(0.109 \pm 0.007*\mathrm{BWT}) where Mg/Ca is the Mg/Ca ratio found in the benthic foraminifera and BWT is the bottom water temperature.

See also

Paleothermometer — Study of ancient temperatures Paleomaps – Maps showing the past shapes of continents

References

External links

Text derived from https://en.wikipedia.org/w/index.php?oldid=1373974324 under CC BY-SA 4.0; modifications have been made.

Sources cited in this revision

Extracted from the cited revision's reference blocks; absent citations are not invented.