Coastal southeast South America is one of the classic locations where there are robust, spatially ex- tensive records of past high sea level. Sea-level proxies interpreted as last interglacial (Marine Isotope Stage 5e, MIS 5e) exist along the length of the Uruguayan and Argentinian coast with exceptional preservation especially in Patagonia. Many coastal deposits are correlated to MIS 5e solely because they form the next-highest ter- race level above the Holocene highstand; however, dating control exists for some landforms from amino acid racemization, U/Th (on molluscs), electron spin resonance (ESR), optically stimulated luminescence (OSL), infrared stimulated luminescence (IRSL), and radiocarbon dating (which provides minimum ages). As p...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
Because global sea level during the last interglacial (LIG; 130–115 ka) was higher than today, the L...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
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...
A detailed geomorphological survey was undertaken in the area of Puerto Deseado (Santa Cruz Province...
Reconstructions of global mean sea level from earlier warm periods in Earth’s history can help const...
In this paper, we describe a sea-level database compiled using published last interglacial, Marine I...
We describe a database of Last Interglacial (Marine Isotopic Stage 5) sea-level proxies for the west...
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...
Because global sea level during the last interglacial (LIG; 130–115 ka) was higher than today, the L...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
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...
A detailed geomorphological survey was undertaken in the area of Puerto Deseado (Santa Cruz Province...
Reconstructions of global mean sea level from earlier warm periods in Earth’s history can help const...
In this paper, we describe a sea-level database compiled using published last interglacial, Marine I...
We describe a database of Last Interglacial (Marine Isotopic Stage 5) sea-level proxies for the west...
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...
Because global sea level during the last interglacial (LIG; 130–115 ka) was higher than today, the L...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...