Blar i forfatter Artikler, rapporter og annet (geovitenskap) "van de Flierdt, T."

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    • A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude 

      Marschalek, J. W.; Zurli, L.; Talarico, F.; van de Flierdt, T.; Vermeesch, P.; Carter, A.; Beny, F.; Bout-Roumazeilles, V.; Sangiorgi, F.; Hemming, S. R.; Pérez, L. F.; Colleoni, F.; Prebble, J. G.; van Peer, T. E.; Perotti, M.; Shevenell, A. E.; Browne, I.; Kulhanek, D. K.; Levy, R.; Harwood, D.; Sullivan, N. B.; Meyers, S. R.; Griffith, E. M.; Hillenbrand, C. D.; Gasson, E.; Siegert, M. J.; Keisling, B.; Licht, K. J.; Kuhn, G.; Dodd, J. P.; Boshuis, C.; de Santis, L.; McKay, R. M.; Ash, J.; Cortese, G.; Esper, O. V.; Gales, J. A.; Ishino, S.; Kim, Sookwan; Kim, Sunghan; Laberg, Jan Sverre; Leckie, R. M.; Muller, J.; Patterson, M. O.; Romans, B. W.; Romero, O. E.; Seki, O.; Singh, S. M.; Cordeiro de Sousa, I. M.; Sugisaki, S. T. (Journal article; Tidsskriftartikkel; Peer reviewed, 2021)
      Early to Middle Miocene sea-level oscillations of approximately 40–60 m estimated from far-field records1,2,3 are interpreted to reflect the loss of virtually all East Antarctic ice during peak warmth2. This contrasts with ice-sheet model experiments suggesting most terrestrial ice in East Antarctica was retained even during the warmest intervals of the Middle Miocene4,5. Data and model outputs can ...