ISTerre, IRD, CNRS, Université Grenoble-Alpes, Saint-Martin-d'Hères, 38400, France
Res. Group of Paleoclimate & Paleoenvironment, Res. Centr. for Climate and Atmosphere, Res. Org. of Earth Sciences and Maritime, National Research and Innovation Agency, Bandung, 40135, Indonesia
ENS de Lyon, CNRS, LGL-TPE, Université Claude Bernard Lyon 1, Villeurbanne, 69100, France
Navid Hedjazian
ENS de Lyon, CNRS, LGL-TPE, Université Claude Bernard Lyon 1, Villeurbanne, 69100, France
ISTerre, IRD, CNRS, Université Grenoble-Alpes, Saint-Martin-d'Hères, 38400, France
Kevin Pedoja
Laboratoire Morphodynamique Continentale et Côtière, Université de Caen Normandie, Caen, 14000, France
Tubagus Solihuddin
Res. Group of Paleoclimate & Paleoenvironment, Res. Centr. for Climate and Atmosphere, Res. Org. of Earth Sciences and Maritime, National Research and Innovation Agency, Bandung, 40135, Indonesia
Sri Yudawati Cahyarini
Res. Group of Paleoclimate & Paleoenvironment, Res. Centr. for Climate and Atmosphere, Res. Org. of Earth Sciences and Maritime, National Research and Innovation Agency, Bandung, 40135, Indonesia
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Total article views: 1,720 (including HTML, PDF, and XML)
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1,720
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48
56
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Supplement: 58
BibTeX: 48
EndNote: 56
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Total article views: 2,326 (including HTML, PDF, and XML)
Thereof 2,269 with geography defined
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Total article views: 1,720 (including HTML, PDF, and XML)
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Total article views: 606 (including HTML, PDF, and XML)
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Marine terrace sequences – staircase-shaped coastal landforms – record sea-level changes, vertical motions, and erosional processes that are difficult to untangle. To achieve this, we developed a numerical inversion approach: using the observed landscape as input, we constrained the ensemble of parameter ranges that could have created this landscape. We applied the model to marine terrace sequences in Santa Cruz (US) and Corinth (Greece) to reveal past sea or lake levels, uplift rates, and hydroclimates.