Martínez and Rojas (2013) published a paper about the relative sea level during the Holocene in Uruguay. The paper of Martínez and Rojas could be handled as an attempt to construct a sea-level curve from data collected from different sources: open-ocean coast, the Río de la Plata coastline and the outlet of Uruguay River. In this sense, several processes were involved: storm effects at open-ocean beaches, the Holocene enclosing of coastal lagoons, storms within the funnel-shaped estuary and the floods of the Uruguay River. However, they included a series of omissions, inaccuracies, errors and critics to our work, that need to be amended, rectified and argued. In response we present a historical background about the research on this issue in...
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Provinc...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Dear Editor, we are thankful to C. Morhange, C. Flaux, P.A. Pirazzoli and M.B. Carre for their comme...
This study critically reviews the relative sea-level (RSL) data from the Río de la Plata (RDP) (Arge...
ABSTRACT Interpretation of sea-level indicators is essential when studying paleo sea-level fluctuati...
ABSTRACT The present work discusses and reinterprets paleo-sea level indicators used to build Holoce...
ABSTRACT Discussions are useful to the advance of science, and we appreciate the opportunity to disc...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
Available sea level data from the Tierra del Fuego region cannot be combined Into a meaningful sea l...
Although paleolimnological studies in the Argentinean and Uruguayan Pampas are relatively incipien...
There are areas in the world where our understanding of past sea-level changes is less robust than i...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Identifying the causes for historical sea-level changes in coastal tide-gauge records is important f...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
In May 2009, Orson van de Plassche sadly passed away. In a paper that was partially written after hi...
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Provinc...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Dear Editor, we are thankful to C. Morhange, C. Flaux, P.A. Pirazzoli and M.B. Carre for their comme...
This study critically reviews the relative sea-level (RSL) data from the Río de la Plata (RDP) (Arge...
ABSTRACT Interpretation of sea-level indicators is essential when studying paleo sea-level fluctuati...
ABSTRACT The present work discusses and reinterprets paleo-sea level indicators used to build Holoce...
ABSTRACT Discussions are useful to the advance of science, and we appreciate the opportunity to disc...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
Available sea level data from the Tierra del Fuego region cannot be combined Into a meaningful sea l...
Although paleolimnological studies in the Argentinean and Uruguayan Pampas are relatively incipien...
There are areas in the world where our understanding of past sea-level changes is less robust than i...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Identifying the causes for historical sea-level changes in coastal tide-gauge records is important f...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
In May 2009, Orson van de Plassche sadly passed away. In a paper that was partially written after hi...
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Provinc...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Dear Editor, we are thankful to C. Morhange, C. Flaux, P.A. Pirazzoli and M.B. Carre for their comme...