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- W2954673909 endingPage "434" @default.
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- W2954673909 abstract "Earth history is defined by a series of greenhouse and icehouse periods associated with cycles of sea-level rise and fall. Throughout time great oceans such as the Tethys have opened and closed and have seen the beginning of life on Earth. Sea-level variation is driven by a variety of factors including orbital (Milankovitch) cyclicity and the Wilson cycle of the formation and break-up of continents which controls the volume of ocean basins. The volume of water in the oceans is also strongly controlled by the volume of water locked up in ice sheets and glaciers, and is therefore linked to changes in mean global temperatures. Consequently, eustatic sea-level rise and fall occurs synchronously with the retreat and expansion of ice sheets, respectively. Interpretations of sea-level change in geological time have traditionally been made using sequence stratigraphic concepts. However, increasing recognition of the non-uniqueness of sedimentary deposits, particularly through the use of numerical forward models, is challenging this approach. Instead, unequivocal evidence for changes in paleobathymetry must be identified to interpret ancient sea-level change in the rock record. This evidence may come from sea temperature studies using oxygen isotopes as a proxy for sea-level change or from direct evidence for bathymetric change from fossil assemblages that are unique to particular depositional settings. Understanding sea-level change in geological time has applications to modern day climate change research and enables scientists to anticipate the likely response of marine ecosystems to global warming and associated sea-level rise." @default.
- W2954673909 created "2019-07-12" @default.
- W2954673909 creator A5029577879 @default.
- W2954673909 date "2021-01-01" @default.
- W2954673909 modified "2023-09-25" @default.
- W2954673909 title "Sea-Level Change in Geological Time" @default.
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- W2954673909 doi "https://doi.org/10.1016/b978-0-12-409548-9.11899-8" @default.
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