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The Anthropocene is functionally and stratigraphically distinct from the HoloceneWhen did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimalBenthic foraminifera as indicators of habitat change in anthropogenically impacted coastal wetlands of the Ebro Delta (NE Iberian Peninsula).A 130 year record of pollution in the Suances estuary (southern Bay of Biscay): implications for environmental management.Geochemical and microfaunal proxies to assess environmental quality conditions during the recovery process of a heavily polluted estuary: the Bilbao estuary case (N. Spain).Environmental transformation of the Bilbao estuary, N. Spain: microfaunal and geochemical proxies in the recent sedimentary record.A 700 year record of combustion-derived pollution in northern Spain: tools to identify the Holocene/Anthropocene transition in coastal environments.Stratigraphic and Earth System approaches to defining the AnthropoceneBenthic foraminifera as indicators of habitat in a Mediterranean delta: implications for ecological and palaeoenvironmental studiesAgricultural fingerprints in salt-marsh sediments and adaptation to sea-level rise in the eastern Cantabrian coast (N. Spain)Accretion rates in coastal wetlands of the southeastern Gulf of California and their relationship with sea-level riseThe Anthropocene: a conspicuous stratigraphical signal of anthropogenic changes in production and consumption across the biosphereThe geological cycle of plastics and their use as a stratigraphic indicator of the AnthropoceneRelative sea-level changes in the Basque coast (northern Spain, Bay of Biscay) during the Holocene and Anthropocene: The Urdaibai estuary caseSand-spit accumulations at the mouths of the eastern Cantabrian estuaries: The example of the Oka estuary (Urdaibai Biosphere Reserve)Can nuclear weapons fallout mark the beginning of the Anthropocene Epoch?Chemostratigraphic and lithostratigraphic signatures of the Anthropocene in estuarine areas from the eastern Cantabrian coast (N. Spain)Colonization of the Americas, ‘Little Ice Age’ climate, and bomb-produced carbon: Their role in defining the AnthropoceneQuaternary of the Western Pyrenean region: Multidisciplinary ResearchTribute to Lydia ZapataAn evaluation of the Rouse theory for sand transport in the Oka estuary, SpainAnthropogenic disruptions of the sedimentary record in coastal marshes: Examples from the southern Bay of Biscay (N. Spain)Anthropogenic impacts on Iberoamerican coastal areas: Historical processes, present challenges, and consequences for coastal zone managementLateglacial and Holocene coastal evolution in the Minho estuary (N Portugal): Implications for understanding sea-level changes in Atlantic IberiaMorphodynamic consequences of dredging and dumping activities along the lower Oka estuary (Urdaibai Biosphere Reserve, southeastern Bay of Biscay, Spain)Recent environmental evolution of regenerated salt marshes in the southern Bay of Biscay: Anthropogenic evidences in their sedimentary recordRecord of anthropogenic activities on the coastal environments of Iberoamerica (Antropicosta)Relative sea-level rise in the Basque coast (N Spain): Different environmental consequences on the coastal areaField observations and modelling of Holocene sea-level changes in the southern Bay of Biscay: implication for understanding current rates of relative sea-level change and vertical land motion along the Atlantic coast of SW EuropeHistorical signature of Roman mining activities in the Bidasoa estuary (Basque Country, northern Spain): an integrated micropalaeontological, geochemical and archaeological approachAssessing the performance of a foraminifera-based transfer function to estimate sea-level changes in northern PortugalDistribution of foraminifera in salt marshes along the Atlantic coast of SW Europe: Tools to reconstruct past sea-level variationsQuantitative assessment of the salinity gradient within the estuarine systems in the southern Bay of Biscay using benthic foraminiferaRecent sea-level changes in the southern Bay of Biscay: transfer function reconstructions from salt-marshes compared with instrumental dataA foraminifera-based transfer function as a tool for sea-level reconstructions in the southern Bay of BiscayDevelopment of a foraminifera-based transfer function in the Basque marshes, N. Spain: Implications for sea-level studies in the Bay of BiscayThe Mendieta site (Sopelana, Biscay province, northern Spain): Palaeoenvironment and formation processes of a Lower Palaeolithic open-air archaeological depositPOSTGLACIAL FORAMINIFERA AND PALEOENVIRONMENTS OF THE MELIDES LAGOON (SW PORTUGAL): TOWARDS A REGIONAL MODEL OF COASTAL EVOLUTIONMicropalaeontological record of Holocene estuarine and marine stages in the Corgo do Porto rivulet (Mira River, SW Portugal)Human activities along the Basque coast during the last two centuries: geological perspective of recent anthropogenic impact on the coast and its environmental consequences
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