δ18O of Fissurella maxima as a proxy for reconstructing Early Holocene sea surface temperatures in the coastal Atacama desert (25°S)

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dc.contributor.authorFlores, Carola
dc.contributor.authorGayo Hernández, Eugenia Monserrat
dc.contributor.authorSalazar, Diego
dc.contributor.authorBroitman Rojas, Bernardo Oscar
dc.date.accessioned2020-12-10T22:43:11Z
dc.date.available2020-12-10T22:43:11Z
dc.date.issued2018
dc.fuente.origenConveris
dc.identifier.doi10.1016/j.palaeo.2018.03.031
dc.identifier.issn0031-0182
dc.identifier.urihttps://doi.org/10.1016/j.palaeo.2018.03.031
dc.identifier.urihttps://repositorio.uc.cl/handle/11534/49661
dc.language.isoen
dc.nota.accesoContenido parcial
dc.pagina.final34
dc.pagina.inicio22
dc.revistaPalaeogeography, Palaeoclimatology, Palaeoecologyes_ES
dc.rightsacceso restringido
dc.titleδ18O of Fissurella maxima as a proxy for reconstructing Early Holocene sea surface temperatures in the coastal Atacama desert (25°S)es_ES
dc.typeartículo
dc.volumenVol. 499
sipa.codpersvinculados158192
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