aDipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari, Via Orabona 4, 70124 Bari, Italy; bDipartimento di Scienze della Terra, Sapienza, Università di Roma, Piazzale Aldo Moro 5, 00185 Roma, Italy
Abstract This study focuses on the analysis of a carbonate bioclastic pocket beach located along a coastal sector of the Apulia Ionian Sea, Le Dune beach, South Italy. The beach develops for about 800 m and it is exposed to the south-westerly and southerly seas. Coastal sediments range from very coarse to medium-fine sands and they are mainly composed of bioclasts (more than 90%) which include molluscs, foraminifers, echinoderms, algae branched, bryozoans, spicules of sponges and arthropods. The study area is one part of a marine protected reserve characterised by 15 different habitats of the typical Mediterranean submerged populations and the presence of Posidonia oceanica meadows. The aim of our research is to highlight the correlation between physical and biological processes influencing Le Dune beach dynamics and its sediment provenance by analysing the textural and compositional characteristics of beach sands, which is fundamental for pocket beach conservation. The beach sand analysis, deriving from textural, compositional and bioclast investigations, underlines that one of the main indicators of the beach dynamics is the bioclast component, which provides relevant information about sand provenance and sediment transport. The beach constitutes a semi-close system only nourished by the shells of organisms and by the erosion of headlands and dunes without important sediment interchange with adjacent littoral sectors.
[1] Ambrosano E., Ferretti O., andFalcinelli F., 1986. Tipologia geomorfologica costiera e caratterizzazione mineralogica dei sedimenti di spiaggia del litorale pugliese.Indagine Ambientale del Sistema Marino Costiero della Regione Puglia, ENEA, 55-67. [2] Basterretxea G., Orfila A., Jordi A., Casas B., Lynett P., Liu P.L.F., Duarte C.M., andTintoré J., 2004. Seasonal dynamics of a Microtidal Pocket Beach withPosidonia oceanica Seabeds (Mallorca, Spain). Journal of Coastal Research, 204, 1155-1164. [3] Bird E.,2008. Coastal Geomorphology. An Introduction. II Edition.J. Wiley and Sons, 411 pp. [4] Bowman D., Rosas V., andPranzini E., 2013. Pocket beaches of Elba Island (Italy) - Planview geometry, depth of closure and sediment dispersal.Estuarine, Coastal and Shelf Science, 138(1), 37-46. [5] Brandano M., Cuffaro M., Gaglianone G., Petricca P., Stagno V., andMateu-Vicens, G., 2016. Evaluating the role of seagrass in Cenozoic CO2 variations. Frontiers in Environmental Science, 4, 72. https://doi.org/10.3389/fenvs.2016.00072. [6] Ciaranfi N., Pieri P., andRicchetti G., 1988. Note illustrative alla carta geologica delle Murge e del Salento (Puglia centromeridionale). Memorie della Società Geologica Italiana, 41, 449-460. [7] Cipriani L.E., Pranzini E., Rosas V., andWetzel L,2011. Landuse changes and erosion of pocket beaches in Elba Island (Tuscany, Italy).Journal of Coastal Research 64, 1774-1778. [8] De Falco G., Baroli M., Simeone S., andPiergallini G., 2002. La rimozione della posidonia dalle spiagge: Conseguenze sulla stabilità dei litorali.Report of ARENA Project, IMC Foundation, 1-17. [9] De Falco G., Molinaroli E., Baroli M., andBellacicco S., 2003. Grain size and compositional trends of sediments fromPosidonia oceanica meadows to beach shore, Sardinia, western Mediterranean. Estuarine, Coastal and Shelf Science, 58, 299-309. [10] De Falco G., Simeone S., andBaroli M., 2008. Management of beach-castPosidonia oceanica seagrass on the island of Sardinia (Italy, Western Mediterranean). Journal of Coastal Research, 24(4C), 69-75. [11] De Pippo T., Donadio C., Mazzarella G., Paolillo G., andPennetta M., 2004b. Fractal geometry applied to coastal and submarine features.Zeitschrift für Geomorphologie N.F., 48, 185-199. [12] De Pippo T., Donadio C., Pennetta M., Terlizzi F., andVecchione C., 2004a. Evoluzione morfologica del settore costiero di Porto Cesareo (Penisola Salentina, Puglia).Studi Costieri, 8, 37-48. [13] Folk R.L.,1959. Practical petrographic classification of limestones.AAPG (American Association of Petroleum Geologists) Bulletin, 43, 1-38. [14] Gaglianone G., Brandano M., andMateu-Vicens G., 2017. The sedimentary facies of Posidonia oceanica seagrass meadows from the central Mediterranean Sea. Facies, 63, 28. https://doi.org/10.1007/s10347-017-0511-2. [15] Gaglianone G., Frezza V., Mateu-Vicens G., andBrandano M., 2014. Posidonia oceanica seagrass meadows facies from western Mediterranean Sea. Rend Online Soc Geol It, 31(Suppl. 1), 187. [16] Klein A.H.F., andMenezes J.T., 2001. Beach morphodynamics and profile sequence for a headland bay coast.Journal of Coastal Research, 17, 198-215. [17] Lisco S., Moretti M., Moretti V., Cardone F., Corriero G., andLongo C., 2017. Sedimentological features of Sabellaria spinulosa bioconstructions.Marine and Petroleum Geology, 87, 203-212. [18] Mastronuzzi G., Palmentola G., andRicchetti C., 1989. Aspetti della evoluzione olocenica della costa pugliese.Memorie della Società Geologica Italiana 42, 287-300. [19] Mastronuzzi G., Palmentola G., andSansò P., 2002. Lineamenti e dinamica della costa pugliese.Studi Costieri, 5, 9-22. [20] Milli S., Girasoli D.E., Tentori D., andTortora P., 2017. Sedimentology and coastal dynamics of carbonate pocket beaches: The Ionian-Sea Apulia coast between Torre Colimena and Porto Cesareo (Southern Italy).Journal of Mediterranean Earth Sciences, 9, 29-66. [21] Moreno L.J., andKraus N.C., 1999. Equilibrium shape of headland-bay beaches for engineering design. In: Proceedings of the Coastal Sediments’ 99, American Society of Civil Engineers, 1, pp. 860-875. [22] Moretti M., Tropeano M., Van Loon A.J.T., Acquafredda P., Baldacconi R., Festa V., Lisco S., Mastronuzzi G., Moretti V., Scotti R., 2016. Texture and composition of the Rosa Marina beach sands (Adriatic coast, southern Italy): A sedimentological/ecological approach.Geologos, 22(2), 87-103. [23] Mount J.,1985. Mixed siliciclastic and carbonate sediments: A proposed first-order textural and compositional classification.Sedimentology, 32, 435-442. [24] Pennetta M.,1985. Caratteri granulometrici dei sedimenti del Golfo di Taranto (Alto Ionio).Annali Istituto Universitario Navale di Napoli, 54, 29-30. [25] Petrillo A.F., Bruno M.F., andNobile B., 2014. Supporto scientifico per la redazione del piano comunale delle coste del Comune di Porto Cesareo (Le). Report, Politecnico di Bari, Italy. [26] Pettijohn F.J.,1975. Sedimentary Rocks, Third Edition. Harper and Row. [27] Poppe L.J., Eliason A.H., Fredericks J.J., Rendigs R.R., Blackwood D., andPolloni C.F., 2000. Grain-size analysis of marine sediments - methodology and data processing. In: Poppe, L.J., Hastings, M.E., Eliason, A.H., Fredericks, J.J., Rendigs, R.R., and Blackwood, D.S., (Eds.). U.S.G.S. East-coast Sediment Analysis: Procedures, Database, and Georeferenced Displays. U.S. Geological Survey, Woods Hole, MA. U.S. Geological Survey Open File Report, 00e358. [28] Pranzini E., andRosas V., 2007. Pocket beach response to high magnitude-low frequency floods (Elba Island, Italy).Journal of Coastal Research, 50, 969-977. [29] Pranzini E., Rosas V., Jackson N.L., andNordstrom K., 2013. Beach changes from sediment delivered by streams to pocket beaches during a major flood.Geomorphology, 199, 36-47. [30] Rossi D.,1969. Note illustrative della Carta Geologica d’Italia, Foglio 203, 204, 213 “Brindisi-Lecce-Maruggio”. Servizio Geologico d'Italia, Roma, 42 pp. [31] Roy P.S., Cowell P.J., Ferland M.A., andThom B.G., 1994. Wave dominated coasts. In: Carter, R.W.G., and Woodroffe, C.D., (Eds.). Coastal Evolution, Late Quaternary Shoreline Morphodynamics. Cambridge University Press, pp. 121-186. [32] Satta A., Ceccherelli G., Cappucci S., Carboni S., Cossu A., Costa M., De Luca M., Dessy C., Farris E., Gazale V., Ginesu S., Manca E., Pascucci V., Russino G., Saba G., Saba T., andVargiu P., 2013. Linee guida per la gestione integrata delle spiagge. I quaderni della conservatoria delle coste 1. Regione Autonoma della Sardegna. [33] Short A.D.,1985. Rip-current type, spacing and persistence, Narrabeen Beach, Australia.Marine Geology, 65, 47-71. [34] Short A.D., Cowell P.J., Cadee M., Hall W., andVan Dijck, B., 1995. Beach rotation and possible relation to the Southern Oscillation. In: Aung, T.H., (Ed.). Ocean and Atmosphere Pacific Conference, Adelaide, pp. 329-334. [35] Short F., Carruthers T., Dennison W., andWaycott M., 2007. Global seagrass distribution and diversity: A bioregional model.Journal of Experimental Marine Biology and Ecology, 350, 3-20. [36] Simeone S., Molinaroli E., Conforti A., andDe Falco G., 2018. Impact of ocean acidification on the carbonate sediment budget of a temperate mixed beach.Climatic Change, 150, 227-242. [37] Simeoni U., Corbau C., Pranzini E., andGinesu S., 2012. Le Pocket Beach, Dinamica e gestione delle piccole spiagge. Franco Angeli, 176 pp. [38] Van Loon, A.J.T., Moretti, M., Tropeano, M., Acquafredda, P., Baldacconi, R., Festa, V., Lisco, S., Mastronuzzi, G., Moretti, V., and Scotti, R., 2017. Tracing the source of bio/siliciclastic beach sands at Rosa Marina, Apulian coast (SE Italy). In: Sediment Provenance - Influences on Compositional Change from Source to Sink, Chapter 3, Mazumder, pp. 25-47. [39] Zingg T.,1935. Beitrage zur Shottenanalyse. Schweizerische mineralogische und petrographische Mitteilungen, 15, 39-40. https://doi.org/10.3929/ETHZ-A-000103455. [40] Zuffa G.G.,1980. Hybrid arenites: Their composition and classification.Journal of Sedimentary Petrology, 50, 21-29. [41] Zuffa G.G.,1985. Optical analysis of arenites: Influence of methodology on compositional results. In: Zuffa, G.G., (Ed.). Provenance of Arenites. Dordrecht(Reidel), pp. 165-189.