Paleosea-level Change
Paleosea-Level Change is a scientific construct that refers to the reconstruction of historical variations in global or regional sea level over geological timescales, derived from proxy data and stratigraphic evidence, to distinguish it from instrumental or observational sea-level records of the modern era.
21
Publications
1.3K
Citations
77
Authors
51
Institutions
Publications per year
2017–2026
3
Variants
Paleosealevel Change
Parents
21
1–5 of 21
77
3
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51

University of Wollongong
Wollongong, Australia
3 h-index
10 publications
542 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
2 h-index
5 publications
129 citations
Instytut Nauk Geologicznych
Warsaw, Poland
2 h-index
2 publications
154 citations

University of Toronto
Toronto, Canada
2 h-index
2 publications
106 citations

University of Hawaii System
Honolulu, United States
1 h-index
2 publications
294 citations
Fundación Ciencias Exactas y Naturales
Buenos Aires, Argentina
1 h-index
1 publications
44 citations
Nanjing University
Nanjing, China
1 h-index
3 publications
210 citations

University of Warsaw
Warsaw, Poland
1 h-index
1 publications
121 citations
1–8 of 51
3 publications · 215 citations
3
h-index
QR · 2 publications · 186 citations
2
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2 publications · 122 citations
2
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2 publications · 80 citations
2
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1 publications · 33 citations
1
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1–5