Coastal southeast South America is one of the classic locations where there are robust, spatially extensive records of past high sea level. Sea-level proxies interpreted as being Last Interglacial (Marine Isotope Stage - MIS 5e) exist along the length of the Uruguayan and Argentinian coast, with exceptional preservation especially in Patagonia. Many coastal deposits are 5 correlated to MIS 5e solely because they form the next highest terrace level above the Holocene highstand; however, dating control exists for some landforms from amino acid racemization, U/Th (on molluscs), electron spin resonance (ESR), and optically stimulated luminescence (OSL) dating. As part of the World Atlas of Last Interglacial Shorelines (WALIS) database, we...
Patagonia Argentina is a key area for the study of sea level changes in the southern hemisphere, but...
Because global sea level during the last interglacial (LIG; 130–115 ka) was higher than today, the L...
There are areas in the world where our understanding of past sea-level changes is less robust than i...
Coastal southeast South America is one of the classic locations where there are robust, spatially ex...
Coastal southeast South America is one of the classic locations where there are robust, spatially ex...
Coastal southeast South America is one of the classic locations where there are robust, spatially ex...
Marine Isotope Stage 5e (MIS 5e; the Last Interglacial, 125 ka) represents a process analog for a wa...
As part of the World Atlas of Last Interglacial Shorelines (WALIS), we critically review existing ch...
We use a standardized template for Pleistocene sea-level data to review last interglacial (Marine Is...
Reconstructions of global mean sea level from earlier warm periods in Earth’s history can help const...
A detailed geomorphological survey was undertaken in the area of Puerto Deseado (Santa Cruz Province...
In this paper, we describe a sea-level database compiled using published last interglacial, Marine I...
To understand past and future sea-level variability, it is important to know if during an interglaci...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
We describe a database of Last Interglacial (Marine Isotopic Stage 5) sea-level proxies for the west...
Patagonia Argentina is a key area for the study of sea level changes in the southern hemisphere, but...
Because global sea level during the last interglacial (LIG; 130–115 ka) was higher than today, the L...
There are areas in the world where our understanding of past sea-level changes is less robust than i...
Coastal southeast South America is one of the classic locations where there are robust, spatially ex...
Coastal southeast South America is one of the classic locations where there are robust, spatially ex...
Coastal southeast South America is one of the classic locations where there are robust, spatially ex...
Marine Isotope Stage 5e (MIS 5e; the Last Interglacial, 125 ka) represents a process analog for a wa...
As part of the World Atlas of Last Interglacial Shorelines (WALIS), we critically review existing ch...
We use a standardized template for Pleistocene sea-level data to review last interglacial (Marine Is...
Reconstructions of global mean sea level from earlier warm periods in Earth’s history can help const...
A detailed geomorphological survey was undertaken in the area of Puerto Deseado (Santa Cruz Province...
In this paper, we describe a sea-level database compiled using published last interglacial, Marine I...
To understand past and future sea-level variability, it is important to know if during an interglaci...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
We describe a database of Last Interglacial (Marine Isotopic Stage 5) sea-level proxies for the west...
Patagonia Argentina is a key area for the study of sea level changes in the southern hemisphere, but...
Because global sea level during the last interglacial (LIG; 130–115 ka) was higher than today, the L...
There are areas in the world where our understanding of past sea-level changes is less robust than i...