Sea-Level Lowstands is a chronostratigraphic concept referring to discrete intervals of significantly reduced global ocean volume, distinguished from other sea-level states by their position as relative minima in the sea-level curve, typically associated with periods of extensive continental glaciation.
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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
Highstand shedding of carbonate platforms
VU Research Portal · 1994 · 264 citations
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Centre National de la Recherche Scientifique
Paris, France
7 h-index
13 publications
2.8K citations
Qingdao National Laboratory for Marine Science and Technology
Qingdao, China
4 h-index
10 publications
441 citations
National Oceanography Centre
Southampton, United Kingdom
4 h-index
6 publications
1.5K citations
Shell (Netherlands)
The Hague, The Netherlands
4 h-index
4 publications
192 citations
Chinese Academy of Sciences
Beijing, China
4 h-index
14 publications
1.2K citations
Louisiana State University
Baton Rouge, United States
4 h-index
4 publications
645 citations
Institute of Oceanology
Qingdao, China
3 h-index
13 publications
1.1K citations
University of Delaware
Newark, United States
3 h-index
5 publications
210 citations
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- Geological Society London Special Publications
6 publications · 677 citations
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- Canadian Journal of Earth Sciences
5 publications · 294 citations
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- Geology
5 publications · 430 citations
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- Marine Geology
4 publications · 312 citations
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- Journal of Biogeography
3 publications · 352 citations
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