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dc.contributor.authorMargalef, Olga-
dc.contributor.authorCañellas-Boltà, Núria-
dc.contributor.authorPla-Rabes, S.-
dc.contributor.authorGiralt, Santiago-
dc.contributor.authorPueyo Mur, Juan José-
dc.contributor.authorJoosten, Hans-
dc.contributor.authorRull, Valentí-
dc.contributor.authorBuchaca, Teresa-
dc.contributor.authorHernández, Armand-
dc.contributor.authorValero-Garcés, Blas L.-
dc.contributor.authorMoreno, Ana-
dc.contributor.authorSáez, Alberto-
dc.date.accessioned2013-12-19T13:31:05Z-
dc.date.available2013-12-19T13:31:05Z-
dc.date.issued2013-
dc.identifier.citationGlobal and Planetary Change 108 : 72-84 (2013)es_ES
dc.identifier.issn0921-8181-
dc.identifier.urihttp://hdl.handle.net/10261/88874-
dc.description13 páginas, 7 figuras, 2 tablas.es_ES
dc.description.abstractThe Rano Aroi mire on Easter Island (also known as Rapa Nui; 27°09′S, 109°27′W, 430 m above sea level) provides a unique non-marine record in the central South Pacific Ocean for reconstructing Late Pleistocene environmental changes. The results of amultiproxy study on two cores fromthe center and margin of the Rano Aroimire, including peat stratigraphy, facies analysis, elemental and isotope geochemistry on bulk organic matter, X-ray fluorescence (XRF) core scanning and macrofossil analysis, were used to infer past water levels and vegetation changes. The chronology was based on 18 14C AMS dates for the upper 8.7 m. The extrapolated age for the base of the sequence is 70 kyr,which implies that this record is the oldest paleolimnological record on Easter Island. The recovered Rano Aroi sequence consists of a radicel peat formed primarily from the remains of sedges, grasses and Polygonaceae that have accumulated since Marine Isotopic Stage (MIS) 4 (70 kyr BP) to the present. From 60 to 40 kyr BP (MIS 3), high precipitation/runoff events were recorded as organicmud facies with lighter δ13C, low C/N values and high Ti content, indicating higher detritic input to themire. A gradual shift in δ13C bulk organic matter from −14% to −26%, recorded between 50 and 45 cal kyr BP, suggests a progressive change in local peat-forming vegetation from C4 to C3 plant types. Post-depositional Ca and Fe enrichment during sub-aerial peat exposure and very low sedimentation rates indicate lower water tables during Late MIS 3 (39– 31 cal kyr BP). During MIS 2 (27.8–19 cal kyr BP), peat production rates were very low, most likely due to cold temperatures, as reconstructed from other Easter Island records during the Last Glacial Maximum (LGM). Geochemical and macrofossil evidence shows that peat accumulation reactivates at approximately 17.5 cal kyr BP, reaching the highest accumulation rates at 14 cal kyr BP. Peat accretion decreased from 5.0 to 2.5 cal kyr BP, coinciding with a regional Holocene aridity phase. The main hydrological and environmental changes in Rano Aroi reflect variations in the South Pacific Convergence Zone (SPCZ), Southern Westerlies (SW) storm track, and South Pacific Anticyclone (SPA) locations.es_ES
dc.description.sponsorshipThis research was funded by the Spanish Ministry of Science and Education through the projects LAVOLTER (CGL2004-00683/BTE), GEOBILA (CGL2007-60932/BTE) and CONSOLIDER GRACCIE (CSD2007-00067) and an undergraduate grant JAE (BOE 04/03/2008) to Olga Margalef.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsclosedAccesses_ES
dc.subjectSouth Pacific paleoclimatees_ES
dc.subjectPeat geochemistryes_ES
dc.subjectStable isotopeses_ES
dc.subjectX-ray fluorescence core scanneres_ES
dc.subjectMarine Isotope Stage 3es_ES
dc.subjectLast Glacial Maximumes_ES
dc.subjectHolocenees_ES
dc.titleA 70,000 year multiproxy record of climatic and environmental change from Rano Aroi peatland (Easter Island)es_ES
dc.typeArtículoes_ES
dc.identifier.doi10.1016/j.gloplacha.2013.05.016-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.gloplacha.2013.05.016es_ES
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