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In order to understand the coastal evolution and the major drivers in the Minho area, Portugal, we have combined micropaleontological and sedimentological data, where the chronological framework is provided by 13 radiocarbon ages. The stratigraphic reconstruction is in agreement with regional models of evolution and provides new sea-level index points that support a regional isostatic model producing the first complete Holocene sea-level curve from this area. Field data and model reconstructions present a good agreement for the region considered and vertical land movement estimates derived from the isostatic model are in agreement with GPS vertical velocities. At regional scale, our results support a north\u2013south trend for SW Europe, where isostatic rebound seems to be minimized in the south of the Iberian Peninsula while local factors (sedimentation, local geomorphology, etc.) tend to dominate during the late Holocene. This newly produced sea-level curve has helped to improve isostatic model predictions and provide pre-anthropogenic sea-level rise rates against which modern rates can be compared.<\/jats:p>","DOI":"10.1177\/0959683612460786","type":"journal-article","created":{"date-parts":[[2012,10,22]],"date-time":"2012-10-22T22:18:06Z","timestamp":1350944286000},"page":"353-363","update-policy":"https:\/\/doi.org\/10.1177\/sage-journals-update-policy","source":"Crossref","is-referenced-by-count":32,"title":["Lateglacial and Holocene coastal evolution in the Minho estuary (N Portugal): Implications for understanding sea-level changes in Atlantic Iberia"],"prefix":"10.1177","volume":"23","author":[{"given":"Eduardo","family":"Leorri","sequence":"first","affiliation":[{"name":"East Carolina University, USA"}]},{"given":"Francisco","family":"Fatela","sequence":"additional","affiliation":[{"name":"Universidade de Lisboa, Portugal"}]},{"given":"Teresa","family":"Drago","sequence":"additional","affiliation":[{"name":"Instituto Instituto Portugu\u00eas do Mar e da Atmosfera, Portugal"}]},{"given":"Sarah Louise","family":"Bradley","sequence":"additional","affiliation":[{"name":"University of Bristol, UK"}]},{"given":"Jo\u00e3o","family":"Moreno","sequence":"additional","affiliation":[{"name":"Universidade de Lisboa, Portugal"}]},{"given":"Alejandro","family":"Cearreta","sequence":"additional","affiliation":[{"name":"Universidad del Pais Vasco, Spain"}]}],"member":"179","published-online":{"date-parts":[[2012,10,22]]},"reference":[{"key":"bibr1-0959683612460786","first-page":"378","volume":"63","author":"Allen GP","year":"1993","journal-title":"Journal of Sedimentary Petrology"},{"key":"bibr2-0959683612460786","doi-asserted-by":"publisher","DOI":"10.1016\/j.palaeo.2006.10.019"},{"key":"bibr3-0959683612460786","doi-asserted-by":"publisher","DOI":"10.1016\/S0272-7714(03)00069-6"},{"key":"bibr4-0959683612460786","doi-asserted-by":"publisher","DOI":"10.1126\/science.1111575"},{"key":"bibr5-0959683612460786","doi-asserted-by":"publisher","DOI":"10.1016\/j.quascirev.2009.09.029"},{"key":"bibr6-0959683612460786","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-246X.2009.04411.x"},{"key":"bibr7-0959683612460786","unstructured":"Bradley SL (2011) Using sea-level and land motion data to develop an improved glacial isostatic adjustment model for the British Isles. 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