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dc.contributor.author
Bracco, Roberto  
dc.contributor.author
Inda, Hugo  
dc.contributor.author
del Puerto, Laura  
dc.contributor.author
Capdepont, Irina  
dc.contributor.author
Panario, Daniel  
dc.contributor.author
Castiñeira Latorre, Carola  
dc.contributor.author
Garcia Rodriguez, Felipe  
dc.date.available
2018-01-08T16:48:01Z  
dc.date.issued
2014-05  
dc.identifier.citation
Garcia Rodriguez, Felipe; Bracco, Roberto; del Puerto, Laura; Panario, Daniel; Castiñeira Latorre, Carola; Capdepont, Irina; et al.; A reply to “Relative sea level during the Holocene in Uruguay”; Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 401; 5-2014; 166-170  
dc.identifier.issn
0031-0182  
dc.identifier.uri
http://hdl.handle.net/11336/32516  
dc.description.abstract
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 Uruguay. We refute the comments about the empirical framework used to construct the first sea-level curve for Uruguay (Bracco et al., 2008, 2011b). We point out that the assumptions on which the curve proposed by Martínez and Rojas (2013) is based are mistaken. In addition, there are limitations of the performed statistical techniques, and errors — mainly systematic — within their formulation. We present evidence that the decrease in sea level from middle Holocene would not have been constant. Instead, a rapid sea level decrease would have taken place by 4300 yr BP. Finally, we not only compare our sea level curve with that proposed by Martínez and Rojas, but also we corrected the altimetry errors incurred in their formulation. We conclude that the similarity supports the validity of our curve.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Elsevier Science  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Holocene  
dc.subject
Sea Level Change  
dc.subject
Uruguay  
dc.subject.classification
Historia  
dc.subject.classification
Historia y Arqueología  
dc.subject.classification
HUMANIDADES  
dc.title
A reply to “Relative sea level during the Holocene in Uruguay”  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2017-12-26T14:30:29Z  
dc.journal.volume
401  
dc.journal.pagination
166-170  
dc.journal.pais
Países Bajos  
dc.journal.ciudad
Amsterdam  
dc.description.fil
Fil: Bracco, Roberto. Universidad de la República; Uruguay  
dc.description.fil
Fil: Inda, Hugo. Universidad de la República; Uruguay  
dc.description.fil
Fil: del Puerto, Laura. Universidad de la República; Uruguay  
dc.description.fil
Fil: Capdepont, Irina. Universidad de la República; Uruguay  
dc.description.fil
Fil: Panario, Daniel. Universidad de la República; Uruguay  
dc.description.fil
Fil: Castiñeira Latorre, Carola. Universidad Nacional de la Plata. Facultad de Ciencias Naturales y Museo. División Mineralogía y Petrología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina  
dc.description.fil
Fil: Garcia Rodriguez, Felipe. Universidad de la República; Uruguay  
dc.journal.title
Palaeogeography, Palaeoclimatology, Palaeoecology  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.palaeo.2013.10.012  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018213004689