Articles | Volume 13, issue 1
https://doi.org/10.5194/essd-13-171-2021
https://doi.org/10.5194/essd-13-171-2021
Review article
 | 
28 Jan 2021
Review article |  | 28 Jan 2021

Last interglacial (MIS 5e) sea-level proxies in southeastern South America

Evan J. Gowan, Alessio Rovere, Deirdre D. Ryan, Sebastian Richiano, Alejandro Montes, Marta Pappalardo, and Marina L. Aguirre

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Cited articles

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Aguirre, M. L.: Late Pleistocene and Holocene palaeoenvironments in Golfo San Jorge, Patagonia: molluscan evidence, Mar. Geol., 194, 3–30, https://doi.org/10.1016/S0025-3227(02)00696-5, 2003. a
Aguirre, M. L. and Whatley, R. C.: Late Quaternary marginal marine deposits and palaeoenvironments from northeastern Buenos Aires Province, Argentina: a review, Quaternary Sci. Rev., 14, 223–254, https://doi.org/10.1016/0277-3791(95)00009-E, 1995. a, b, c, d, e, f, g
Aguirre, M. L., Bowen, D. Q., Sykes, G. A., and Whatley, R. C.: A provisional aminostratigraphical framework for late Quaternary marine deposits in Buenos Aires province, Argentina, Mar. Geol., 128, 85–104, https://doi.org/10.1016/0025-3227(95)00058-7, 1995. a, b, c, d, e, f, g, h
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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.
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