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Sea Level Change, Last 250 Million Years

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Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Introduction

One of the most fundamental geological observations has been that the seas once inundated large areas of the Earth’s surface that are now exposed on land. Early observers attributed these marine incursions to one or multiple “Noachian” floods, but empirical science prevailed as uniformitarian concepts were applied to the stratigraphic record. Charles Lyell (1830) recognized that changes in sea level due to volcanic activity were responsible for the submergence and subsequent emergence of the temple at Serapis near Naples, Italy (see discussion by Gould, 1999). Observing cycles of shallow-water sedimentation across Europe, Lyell reasoned that apparent rises in sea level could explain the flooding of the continents (geologists call these “transgressions”) and the subsequent retreat of the seas (called “regressions”). For over a century after Lyell’s work, geologists mapped these advances and retreats of the sea, noting that during intervals such as the middle Cretaceous...

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© 2009 Springer-Verlag

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Miller, K.G. (2009). Sea Level Change, Last 250 Million Years. In: Gornitz, V. (eds) Encyclopedia of Paleoclimatology and Ancient Environments. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4411-3_206

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