Articles | Volume 14, issue 8
https://doi.org/10.5194/gmd-14-5285-2021
https://doi.org/10.5194/gmd-14-5285-2021
Model description paper
 | 
23 Aug 2021
Model description paper |  | 23 Aug 2021

PALEOSTRIPv1.0 – a user-friendly 3D backtracking software to reconstruct paleo-bathymetries

Florence Colleoni, Laura De Santis, Enrico Pochini, Edy Forlin, Riccardo Geletti, Giuseppe Brancatelli, Magdala Tesauro, Martina Busetti, and Carla Braitenberg

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Cited articles

Allen, P. A. and Allen, J. R.: Basin Analysis: Principles and Applications, Wiley, 2nd edn., 2013. a
Amadori, C., Garcia‐Castellanos, D., Toscani, G., Sternai, P., Fantoni, R., Ghielmi, M., and Di Giulio, A.: Restored topography of the Po Plain‐Northern Adriatic region during the Messinian base‐level drop – Implications for the physiography and compartmentalization of the palaeo‐Mediterranean basin, Basin Res., 30, 1247–1263, 2018. a
Arndt, J. E., Schenke, H. W., Jakobsson, M., Nitsche, F. O., Buys, G., Goleby, B., Rebesco, M., Bohoyo, F., Hong, J., Black, J., Greku, R., Udintsev, G., Barrios, F., Reynoso-Peralta, W., Taisei, M., and Wigley, R.: The International Bathymetric Chart of the Southern Ocean (IBCSO) Version 1.0 – A new bathymetric compilation covering circum-Antarctic waters, Geophys. Res. Lett., 40, 3111–3117, 2013. a
Austermann, J., Pollard, D., Mitrovica, J. X., Moucha, R., Forte, A. M., DeConto, R. M., Rowley, D. B., and Raymo, M. E.: The impact of dynamic topography change on Antarctic ice sheet stability during the mid-Pliocene warm period, Geology, 43, 927–930, 2015. a
Austermann, J., Mitrovica, J. X., Huybers, P., and Rovere, A.: Detection of a dynamic topography signal in last interglacial sea-level records, Science Advances, 3, e1700457, https://doi.org/10.1126/sciadv.1700457, 2017. a
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Short summary
PALEOSTRIP has been developed in the framework of past Antarctic ice sheet reconstructions for periods when bathymetry around Antarctica differed substantially from today. It has been designed for users with no knowledge of numerical modelling and allows users to switch on and off the processes involved in backtracking and backstripping. Applications are broad, and it can be used to restore any continental margin bathymetry or sediment thickness and to perform basin analysis.