Vegetation dynamics at Raraku Lake catchment (Easter Island) during the past 34,000 years

dc.contributor.authorCañellas Boltà, Núria
dc.contributor.authorRull del Castillo, Valentí
dc.contributor.authorSáez, Alberto
dc.contributor.authorMargalef Marrasé, Olga
dc.contributor.authorPla Rabés, Sergi
dc.contributor.authorValero Garcés, Blas Lorenzo
dc.contributor.authorGiralt Romeu, Santiago
dc.date.accessioned2016-02-05T17:31:25Z
dc.date.available2018-01-15T23:01:17Z
dc.date.issued2016-01-15
dc.date.updated2016-02-05T17:31:25Z
dc.description.abstractEaster Island is a paradigmatic example of human impact on ecosystems. The role of climate changes in recent vegetation shifts has commonly been rejected without proper assessment. A palynological study of a long sediment core from Raraku Lake documents the vegetation dynamics for the last 34 ka and investigates their driving forces, particularly the effects of climate variability on vegetation changes. Significant relationships between pollen assemblage changes and sedimentary and geochemical proxies demonstrate the rapid response of vegetation to lake crater basin hydrology and climatic changes. The lake surroundings were occupied by an open mixed palm grove during the Last Glacial period. Poaceae and Sophora increased at the expense of palms and Triumfetta, and Coprosma practically disappeared, in response to slightly wetter and/or colder climate during the Last Glacial Maximum. Palms and Triumfetta thrived in awarmer and/or drier climate during the deglaciation. Minor vegetation changes (a slight increase in Sophora and a drop in Asteraceae and Poaceae) occurred between 13.2 and 11.8 cal ka BP and can be related to rapid changes in the Younger Dryas chronozone. The increase in herbaceous taxa indicates a gradual shallowing of the lake and development of a mire during the Holocene, caused by sediment infilling and warmer and drier climate. Relatively rapid vegetation changes in the Holocene were caused by climate and by plant succession on the expanding mire. The rates of vegetation change observed in the mirewere similar to those at the initial stages of human impact identified in a previous study. These results reveal significant vegetation changes prior to human presence, due to the interplay of climate variations (temperature and moisture), changes in lake basin form by infilling and intrinsic dynamics of plant succession. Hence, the potential contribution of these factors in vegetation shifts during the period of human presence should not be neglected.
dc.format.extent15 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec656684
dc.identifier.issn0031-0182
dc.identifier.urihttps://hdl.handle.net/2445/69293
dc.language.isoeng
dc.publisherElsevier B.V.
dc.relation.isformatofVersió postprint del document publicat a: 10.1016/j.palaeo.2016.01.019
dc.relation.ispartofPalaeogeography Palaeoclimatology Palaeoecology, 2016, vol. 446, p. 55-69
dc.relation.urihttp://dx.doi.org/10.1016/j.palaeo.2016.01.019
dc.rightscc-by-nc-nd (c) Elsevier B.V., 2016
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)
dc.subject.classificationPaleoclimatologia
dc.subject.classificationQuaternari
dc.subject.otherPaleoclimatology
dc.subject.otherQuaternary
dc.titleVegetation dynamics at Raraku Lake catchment (Easter Island) during the past 34,000 years
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/acceptedVersion

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