Articles | Volume 13, issue 1
https://doi.org/10.5194/essd-13-171-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/essd-13-171-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Review article
| 
28 Jan 2021
Review article |
| 28 Jan 2021
| 28 Jan 2021
Last interglacial (MIS 5e) sea-level proxies in southeastern South America
Evan J. Gowan
CORRESPONDING AUTHOR
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
MARUM, University of Bremen, Bremen, Germany
Alessio Rovere
MARUM, University of Bremen, Bremen, Germany
Deirdre D. Ryan
MARUM, University of Bremen, Bremen, Germany
Sebastian Richiano
Instituto Patagónico de Geología y Paleontología, IPGP CENPAT CONICET, Puerto Madryn, Argentina
Alejandro Montes
Antártida e Islas del Atlántico Sur, Instituto de Ciencias Polares, Ambiente y Recursos Naturales, Universidad Nacional de Tierra del Fuego, Ushuaia, Tierra del Fuego, Argentina
Laboratorio de Geomorfología y Cuaternario, Centro Austral de Investigaciones Científicas (CADIC-CONICET), Ushuaia, Argentina
Marta Pappalardo
Department of Earth Sciences, University of Pisa, Pisa, Italy
Marina L. Aguirre
CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, La Plata, Argentina
Facultad de Ciencias Naturales y Museo (FCNyM), Universidad Nacional de La Plata (UNLP),La Plata, Argentina
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- New fossil woods (upper Pleistocene) from the lower-middle Uruguay river basin (South America) reveal the past distribution of Aspidosperma (Apocynaceae) R. Ramos et al. 10.1016/j.quaint.2024.03.004
- Modeled storm surge changes in a warmer world: the Last Interglacial P. Scussolini et al. 10.5194/cp-19-141-2023
- Late Quaternary bioerosion pattern controlled by upwelling events at Puerto Lobos (Chubut, Argentina) L. Giachetti et al. 10.1016/j.quaint.2024.05.009
- History matters: evolutionary and demographic reconstruction of the Southwest Atlantic loggerheads (Testudinata: Cheloniidae) S. Ludwig et al. 10.1007/s10682-024-10312-5
- Palaeoenvironmental implications of Late Quaternary bioerosion traces in central Patagonia (Southern Atlantic, Argentina) L. Giachetti et al. 10.1002/jqs.3657
- Revisiting Battistini: Pleistocene Coastal Evolution of Southwestern Madagascar P. Boyden et al. 10.5334/oq.112
- Beach ridge evolution during the Holocene Climatic Optimum at Río de la Plata estuary, Argentina: Former answers for future questions? S. Richiano et al. 10.1016/j.quaint.2022.02.013
- A review of last interglacial sea-level proxies in the western Atlantic and southwestern Caribbean, from Brazil to Honduras K. Rubio-Sandoval et al. 10.5194/essd-13-4819-2021
- Taphonomic Signature of Glycymeris longior Shells (Bivalvia) and its Potential as Paleoenvironmental Proxy for the Quaternary of Northern Patagonia (Argentina) S. Bayer et al. 10.5710/AMGH.10.07.2023.3552
- Model-Based Analyses Suggest Pleistocene Refugia over Ancient Divergence as Main Diversification Driver for a Neotropical Open-Habitat Treefrog F. Brusquetti et al. 10.1007/s11692-023-09614-3
- The World Atlas of Last Interglacial Shorelines (version 1.0) A. Rovere et al. 10.5194/essd-15-1-2023
- Shell strength of Eucallista purpurata (Bivalvia) from life and death assemblages on sandy beaches of the Bonaerense coast, southwest Atlantic Argentina P. Cristini & J. Ballarre 10.1080/08912963.2024.2370994
- Quaternary and Pliocene sea-level changes at Camarones, central Patagonia, Argentina K. Rubio-Sandoval et al. 10.1016/j.quascirev.2024.108999
- Stratigraphy and evolution of the late Pleistocene (MIS 5) coastal Barrier III in southern Brazil R. Lopes et al. 10.1017/qua.2023.67
Latest update: 20 Nov 2024
Short summary
During the last interglacial (130 to 115 ka), global sea level was higher than present. The World Atlas of Last Interglacial Shorelines (WALIS) has been created to document this. In this paper, we have compiled data for southeastern South America. There are landforms that indicate that sea level was 5 to 25 m higher than present during this time period. However, the quality of these data is hampered by limitations on elevation measurements, chronology, and geological descriptions.
During the last interglacial (130 to 115 ka), global sea level was higher than present. The...
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