<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-14T04:43:36Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2445/163196" metadataPrefix="oai_dc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2445/163196</identifier><datestamp>2025-12-05T17:09:05Z</datestamp><setSpec>com_2072_1057</setSpec><setSpec>col_2072_478804</setSpec><setSpec>col_2072_478917</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <dc:title>Registro de la variabilidad climática de escala milenaria durante el último cliclo glaciar en los sedimentos de la cuenca Argelo-Balear</dc:title>
   <dc:creator>Frigola Ferrer, Jaime I.</dc:creator>
   <dc:creator>Moreno Caballud, Ana</dc:creator>
   <dc:creator>Canals Artigas, Miquel</dc:creator>
   <dc:creator>Cacho Lascorz, Isabel</dc:creator>
   <dc:creator>Colmenero, E.</dc:creator>
   <dc:creator>Sierro Sánchez, Francisco Javier</dc:creator>
   <dc:creator>Flores Villarejo, José Abel</dc:creator>
   <dc:subject>Paleoclimatologia</dc:subject>
   <dc:subject>Sediments glacials</dc:subject>
   <dc:subject>Paleoclimatology</dc:subject>
   <dc:subject>Drift</dc:subject>
   <dc:description>bulk element composition and grain-size distribution to characterize the temporal evolution of the terrigenous input to this area throughout the last 50 ka. The high-resolution elementary profiles show high frequency oscillations, particularly of Si, Ti and K contents, associated with terrigenous input variability. These fluctuations mark significant changes in the source areas and/or in the nature of transport and sedimentation processes most likely related to abrupt changes in oceanographic and atmospheric conditions. The Menorca core records were compared with the geochemical results of a previously studied core from the Alboran Sea, from where it became obvious a similar behaviour in some of the terrigeneous elements at both core locations. The obtained records vary with a clear Dansgaard-Oeschger periodicity reaching higher values during the North Atlantic's Heinrich Events. These results evidence the presence of a millennial-scale synchronous pattern in the Western Mediterranean in terms of deposition of terrigenous material. In addition, grain-size analyses of Menorca core reveal rhythmic episodes of coarser particle inputs during the Holocene likely related to shifts in the intensity of deep-water currents.</dc:description>
   <dc:date>2020-05-30T07:31:05Z</dc:date>
   <dc:date>2020-05-30T07:31:05Z</dc:date>
   <dc:date>2004</dc:date>
   <dc:date>2020-05-30T07:31:06Z</dc:date>
   <dc:type>info:eu-repo/semantics/article</dc:type>
   <dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
   <dc:identifier>1576-5172</dc:identifier>
   <dc:identifier>https://hdl.handle.net/2445/163196</dc:identifier>
   <dc:identifier>549898</dc:identifier>
   <dc:language>spa</dc:language>
   <dc:relation>Reproducció del document publicat a:</dc:relation>
   <dc:relation>Geo-Temas, 2004, vol. 6, num. 5, p. 97-100</dc:relation>
   <dc:rights>(c) Sociedad Geológica de España, 2004</dc:rights>
   <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
   <dc:format>4 p.</dc:format>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Sociedad Geológica de España</dc:publisher>
   <dc:source>Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)</dc:source>
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