Sea-Level Highstands is a geological phenomenon characterized by periods in Earth's history when global sea levels attained relative maxima above long-term average levels, typically due to reduced storage of water in ice sheets and expanded ocean volume during warmer climatic intervals.
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Magnitudes of sea-level lowstands of the past 500,000 years
Eelco J. Rohling, M.M. Fenton, Frans Jorissen et al. · Nature · 1998 · 636 citations · Full text
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Royal Netherlands Institute for Sea Research, Netherlands
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Utrecht, The Netherlands
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United States Geological Survey
Reston, United States
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Southampton, United Kingdom
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