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Palaeoecological potential of the marine organic deposits of Posidonia oceanica: A case study in the NE Iberian Peninsula
Authors:José A. López-Sáez  Lourdes López-Merino  Miguel Á. Mateo  Óscar Serrano  Sebastián Pérez-Díaz  Laura Serrano
Affiliation:1. Department of Environmental Biology, Sapienza University, Piazzale Aldo Moro, 5, Roma, Italy;2. Department of Earth Sciences, Sapienza University, Piazzale Aldo Moro, 5, Roma, Italy;1. CAS Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 164 Xingang Xilu, Guangzhou 510301, China;2. College of Biological Sciences, University of California Davis, Davis, One Shields Avenue, CA 95616, USA;1. ICREA, Pg. Lluís Companys 23, 08010 Barcelona, Catalonia, Spain;2. IPHES, Institut Català de Paleoecologia Humana i Evolució Social, Campus Sescelades URV, edifici W3, 43007 Tarragona, Catalonia, Spain;3. URV, Universitat Rovira i Virgili, Àrea de Prehistòria, Avinguda Catalunya 35, 43002 Tarragona, Catalonia, Spain;4. UAB, Universitat Autònoma de Barcelona, Departament de Biologia Animal de Biologia Vegetal i d''Ecologia, 08193 Bellaterra, Catalonia, Spain;5. UIB, Universitat de les Illes Balears, ArqueoUIB, Palma, Mallorca, Spain;6. UMR 7209 Archéozoologie, Archéobotanique: Sociétés, Pratiques et Environnements, Muséum National d''Historire Naturelle, Centre National de la Recherhce Scientifique, Paris, France;7. UAB, Universitat Autònoma de Barcelona, Departament de Prehistòria, 08193 Bellaterra, Catalonia, Spain
Abstract:A high-resolution sedimentary sequence sampled from the Portlligat Bay (NE Iberian Peninsula) has been studied in order to assess its palaeoecological potential. This sedimentary sequence is considered a very particular one, as it is a peat-like deposit derived from the accumulation of the belowground dead parts of the marine phanerogam Posidonia oceanica through the last 1600 years. This study represents the first attempt to explore the palaeoecological potential of such deposits from a palynological point of view, and has allowed the reconstruction of the vegetation dynamics and changes, human impact and the palaeoclimatic characteristics, demonstrating the value of these sedimentary records in palaeopalynological studies.
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