{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,5,5]],"date-time":"2026-05-05T20:26:54Z","timestamp":1778012814614,"version":"3.51.4"},"reference-count":91,"publisher":"Copernicus GmbH","issue":"2","license":[{"start":{"date-parts":[[2019,4,2]],"date-time":"2019-04-02T00:00:00Z","timestamp":1554163200000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001659","name":"Deutsche Forschungsgemeinschaft","doi-asserted-by":"publisher","award":["SFB1266\/1"],"award-info":[{"award-number":["SFB1266\/1"]}],"id":[{"id":"10.13039\/501100001659","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Clim. Past"],"abstract":"<jats:p>Abstract. To assess the regional multi-decadal to multi-centennial climate variability along the\nsouthern Iberian Peninsula during the mid- to late-Holocene record of paleo-environmental\nindicators from marine sediments were established for two sites in the Alboran Sea\n(ODP-161-976A) and the Gulf of C\u00e1diz (GeoB5901-2). High-resolution records of organic\ngeochemical properties and planktic foraminiferal assemblages are used to decipher\nprecipitation and vegetation changes as well as hydrological conditions with respect to\nsea surface temperature (SST) and marine primary productivity (MPP). As a proxy for\nprecipitation change, records of plant-derived n-alkane composition suggest a series of\nfive distinct dry episodes in southern Iberia at 5.4\u00b10.3\u2009ka\u2009cal\u2009BP, from 5.1 to\n4.9\u00b10.1\u2009ka\u2009cal\u2009BP, from 4.8 to 4.7\u00b10.1\u2009ka\u2009cal\u2009BP, from 4.4 to 4.3\u00b10.1\u2009ka\u2009cal\u2009BP, and at 3.7\u00b10.1\u2009ka\u2009cal\u2009BP. During each dry episode the\nvegetation suffered from reduced water availability. Interestingly, the dry phase from\n4.4 to 4.3\u00b10.1\u2009ka\u2009cal\u2009BP is followed by a rapid shift towards wetter conditions\nrevealing a more complex pattern in terms of its timing and duration than was described\nfor the 4.2\u2009ka event in other regions. The series of dry episodes as well as closely\nconnected hydrological variability in the Alboran Sea were probably driven by NAO-like\n(North Atlantic Oscillation) variability. In contrast, surface waters in the Gulf of\nC\u00e1diz appear to have responded more directly to North Atlantic cooling associated\nwith Bond events. In particular, during Bond events\u00a03 and 4, a pronounced increase in\nseasonality with summer warming and winter cooling is found.<\/jats:p>","DOI":"10.5194\/cp-15-617-2019","type":"journal-article","created":{"date-parts":[[2019,4,2]],"date-time":"2019-04-02T07:42:19Z","timestamp":1554190939000},"page":"617-634","source":"Crossref","is-referenced-by-count":21,"title":["Multi-decadal atmospheric and marine climate variability in southern Iberia during the mid- to late-Holocene"],"prefix":"10.5194","volume":"15","author":[{"given":"Julien","family":"Schirrmacher","sequence":"first","affiliation":[]},{"given":"Mara","family":"Weinelt","sequence":"additional","affiliation":[]},{"given":"Thomas","family":"Blanz","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4148-6791","authenticated-orcid":false,"given":"Nils","family":"Andersen","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0003-1000-2977","authenticated-orcid":false,"given":"Em\u00edlia","family":"Salgueiro","sequence":"additional","affiliation":[]},{"given":"Ralph R.","family":"Schneider","sequence":"additional","affiliation":[]}],"member":"3145","published-online":{"date-parts":[[2019,4,2]]},"reference":[{"key":"ref1","doi-asserted-by":"crossref","unstructured":"Abrantes, F., Rodrigues, T., Rufino, M., Salgueiro, E., Oliveira, D., Gomes,\nS., Oliveira, P., Costa, A., Mil-Homens, M., Drago, T., and Naughton, F.: The\nclimate of the Common Era off the Iberian Peninsula, Clim. 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