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Rendiconti Lincei

, Volume 25, Supplement 2, pp 231–240 | Cite as

Late Quaternary environmental evolution of the intermontane Valle Caudina basin, southern Italy

  • Micla Pennetta
  • Filippo Russo
  • Carlo DonadioEmail author
Intermontane basins in central-southern Italy

Abstract

The Valle Caudina intermontane basin in the southern Apennines (Italy) lies between the Mt. Taburno on the North and the Avella–Partenio mountains on the South. An analysis of its present-day landscape, and of its stratigraphic and geoarcheological features, has been carried out to reconstruct the Late Quaternary evolution of the basin, filled by alluvial, colluvial and volcaniclastic deposits. The depositional pattern and geomorphological context allow to recognize lacustrine and fluvial–lacustrine sediments, interbedded with ignimbritic layers originating from the Phlegrean Fields and with a Vesuvius pumice level, that represent significant chronological markers. The two lacustrine episodes are connected with volcanic events radiometrically dated (De Vivo et al. in Mt. Somma Vesuvius and Volcanism of the Campania Plain. Spec Issue, Mineral Petrol. Springer, Berlin, vol 73, pp 47–65, 2001). The older predates the Campanian Ignimbrite deposit (~39 kyr BP), while the younger deposited before 5 kyr BP, as indicated by the recovery of Neolithic artifacts. The presence of Roman ruins in the center of the valley suggests that the lake has suffered a substantial downsizing or has disappeared between 5 kyr BP and the Roman Age. A clayey deposit testifies a first lacustrine phase, which has affected the whole plain. Above this unit, heterogeneous deposits indicate the end of the lacustrine phase and the beginning of a clear fluvial sedimentation. Volcaniclastic deposits from the erosion of the Campanian Ignimbrite follow. They are overlapped by a widespread second lacustrine unit. Finally, a reworked and altered volcaniclastic level closes the stratigraphic sequence, while particularly fertile topsoil covered all the plain.

Keywords

Geomorphology Intermontane basins Quaternary Southern Apennines Italy 

Notes

Acknowledgments

The authors wish to thank all the referees for their careful and painstaking work in reviewing this paper, which has been vastly improved from the original submission as a result of their labors.

References

  1. Abate D, De Pippo T, Massaro E, Pennetta M (1998) Evoluzione morfologica tardo-quaternaria della Valle Caudina (Benevento, Italia). Il Quaternario, It J Quat Sci 11(2):255–264Google Scholar
  2. Abbruzzese V (ed) (1979) Studi e ricerche idriche in Valle Caudina. Ente per l’irrigazione e la trasformazione fondiaria in Puglia e Lucania. Poligrafica Ruggiero, AvellinoGoogle Scholar
  3. Albore Livadie C (ed) (1986) Tremblements de terre, éruptions volcaniques et vie des hommes dans la Campanie antique. Centre Jean Bérard, Bibl de l’Inst Français de Naples, 2nd Sep, 7, p 233Google Scholar
  4. Albore Livadie C, Gangemi G (1985) Nuovi dati sul Neolitico in Campania. Atti 26a Riun Scient Ist It Preistoria e Protostoria. Il Neolitico in Italia. Firenze (Italy), 7–10 November, I:287–297Google Scholar
  5. Albore Livadie C, Campajola L, D’Onofrio A, Moniot RK, Roca V, Romano M, Russo F, Terrasi F (1998) Evidence of the adverse impact of the « Avellino Pumices » eruption of Somma-Vesuvius on old bronze age sites in the Campania Region (Southern Italy). Quaternaire 9(1):37–43CrossRefGoogle Scholar
  6. Berglund BE (2003) Human impact and climate changes—synchronous events and a causal link? Quatern Int 105:7–12CrossRefGoogle Scholar
  7. Bergomi C, Manfredini M, Martelli G (1975) Note illustrative della carta geologica d’Italia. Foglio 173, BeneventoGoogle Scholar
  8. Bordoni P, Valensise G (1998) Deformation of the 125 ka marine terrace in Italy: tectonic implications. In: Coastal Tectonics. Geol Soc London, Spec Publ 146:71–110Google Scholar
  9. Brancaccio L, Cinque A (1988) L’evoluzione geomorfologica dell’Appennino campano-lucano. Mem Soc Geol It 41:83–86Google Scholar
  10. Brancaccio L, Cinque A, Sgrosso I (1979) Forma e genesi di alcuni versanti di faglia in rocce carbonatiche: il riscontro naturale di un modello teorico. Rend Accad Sci Fis e Mat Napoli, ser 4(46):7–22Google Scholar
  11. Bravi S, Civile D, Martino C, Putignano ML (2006) La struttura da interferenza nei carbonati mesozoici della dorsale di Monte Fellino (Appennino Campano). Boll Soc Geol Italiana, Ital J Geosci 125:105–116Google Scholar
  12. Ceccarelli M, Pignone N, Russo F (1999) Geomorfologia, G.I.S. e rischi naturali in Valle Caudina. Proc. Conf. “Le Pianure. Conoscenza e salvaguardia. Il contributo delle Scienze della Terra”, 8–11 Nov, Ferrara (Italy) 278–281Google Scholar
  13. Cinque A (1992) Distribuzione spazio-temporale dei movimenti tettonici verticali nell’Appennino campano-lucano: alcune riflessioni. St Geol Camerti, vol spec 1992(1):33–38Google Scholar
  14. Comentale B (2010) Le massif du Taburno-Camposauro, une montagne calcaire en position de charnière à l’échelle de l’Apennin méridional (Italie du Sud). Physio-Géo 4:27–42CrossRefGoogle Scholar
  15. D’Argenio B (1967) Geologia del gruppo Taburno-Camposauro (Appennino campano). Atti Acc Sc Fis Mat, ser 3a 6(2):35–218Google Scholar
  16. D’Argenio B, Pescatore T, Scandone P (1973) Schema geologico dell’Appennino Meridionale (Campania, Lucania). Atti Conv “Moderne vedute sulla geologia dell’Appennino”. Acc Naz Lincei Q 183:49–72Google Scholar
  17. De Pippo T, Donadio C, Pennetta M (2001) Evoluzione morfologica della Laguna di Sabàudia (Mar Tirreno, Italia centrale). Geol Romana 36:1–12Google Scholar
  18. De Pippo T, Donadio C, Pennetta M (2004) Morphological control on sediment dispersal along the southern Tyrrhenian coasts (Italy). Geol Romana 37:113–121Google Scholar
  19. De Pippo T, Donadio C, Guida M, Petrosino C (2006) The case of Sarno River (southern Italy). Effects of geomorphology on the environmental impacts. Environ Sc Pollut Res 13(3):184–191CrossRefGoogle Scholar
  20. De Pippo T, Donadio C, Pennetta M, Petrosino C (2008) Land units of Sarno River basin (southern Italy) for land evaluation. Geogr Fis Dinam Q 31:21–36Google Scholar
  21. De Vivo B, Rolandi G, Gans PB, Calvert A, Bohrson WA, Spera FJ, Belkin HE (2001) New constraints on the pyroclastic eruptive history of the Campanian volcanic plain (Italy). In:(eds) Mt. Somma Vesuvius and volcanism of the Campania plain, Spec Issue, Mineral Petrol, Springer 73:47–65Google Scholar
  22. Di Girolamo P (1968) Piroclastiti stratificate riferibili al 2° periodo flegreo nella pianura campana tra il Volturno e Napoli. Period Mineral 37:341–371Google Scholar
  23. Di Girolamo P, Ghiara MR, Lirer L, Munno R, Rolandi G, Stanzione D (1984) Vulcanologia e petrologia dei Campi Flegrei. Boll Soc Geol It 103:349–413Google Scholar
  24. Lirer L, Pescatore T, Booth B, Walker GPL (1973) Two plinian pumice fall deposits from Somma-Vesuvius, Italy. Geol Soc Am Bull 84:759–772CrossRefGoogle Scholar
  25. Magliulo P (2005) Quaternary deposits and geomorphological evolution of the Telesina valley (Southern Apennines). Geogr Fis Dinam Q 28:125–146Google Scholar
  26. Magliulo P, Russo F (2005) Segnalazione e significato dei paleosuoli nel quadro geomorfologico della Valle Telesina (Benevento, Appennino campano). Suppl Geogr Fis Dinam Quat 7:211–217Google Scholar
  27. Magliulo P, Russo F, Valente A (2007) Tectonic significance of geomorphological features in the Telesina valley (Campanian Apennines). Boll Soc Geol It, Ital J Geosci 126(2):397–409Google Scholar
  28. Mastrolorenzo G, Petrone P, Pappalardo L, Sheridan M (2006) The Avellino 3780-yr-B.P. catastrophe as a worst-case scenario for a future eruption at Vesuvius. Proc Natl Acad Sci USA 103(12):4366–4370CrossRefGoogle Scholar
  29. Ortolani F, Pagliuca S, Schiattarella M (1992) Evoluzione geomorfologica e tettonica quaternaria dell’Appennino centro-meridionale. Guida all’escursione, Convegno-Escursione 8–9 luglio, Dip. Sc. Terra, Univ. degli Studi di Camerino - Dip. Sc. Terra, Univ. degli Studi di Napoli Federico IIGoogle Scholar
  30. Pedrera A, Galindo-Zaldívar J, Tello A, Marín-Lechado C (2010) Intramontane basin development related to contractional and extensional structure interaction at the termination of a major sinistral fault: the Huércal-Overa Basin (Eastern Betic Cordillera). J Geodyn 48(5):271–286CrossRefGoogle Scholar
  31. Pescatore T (1964) Ricerche sedimentologiche su argille plioceniche della Valle Caudina (Campania). Boll Soc Nat in Napoli 73:139–154Google Scholar
  32. Pizzi A, Calamita F, Coltorti M, Pieruccini P (2002) Quaternary normal faults, intramontane basins and seismicity in the Umbria-Marche-Abruzzi Apennine ridge (Italy): contribution of neotectonic analysis to seismic hazard assessment. Boll Soc Geol It, vol spec 1:923–929Google Scholar
  33. Porreca M, Mattei M (2010) Tectonic and environmental evolution of Quaternary intramontane basins in Southern Apennines (Italy): insights from palaeomagnetic and rock magnetic investigations. Geophys J Int 182(2):682–698CrossRefGoogle Scholar
  34. Rodríguez-Fernández J, Sanz de Galdeano C (2006) Late orogenic intramontane basin development: the Granada basin, Betics (southern Spain). Basin Res 18(1):85–102CrossRefGoogle Scholar
  35. Scandone R, Bellucci F, Lirer L, Rolandi G (1991) The structure of the Campanian plain and the activity of the Neapolitan volcanoes (Italy). J Volcan Geoth Res 48:1–31CrossRefGoogle Scholar
  36. Vallario A (1973) Geologia e franosità dell’area ad oriente del Taburno Camposauro e del Partenio (Province di Benevento ed Avellino). Geol Appl Idrog 7(2):19–88Google Scholar
  37. Vezzani L, Festa A, Ghisetti FC (2010) Geology and tectonic evolution of the central-southern Apennines, Italy. Geol Soc Am Special Papers 469:1–58CrossRefGoogle Scholar
  38. Zembo I, Trombino L, Bersezio R, Felletti F, Dapiaggi M (2012) Climatic and tectonic controls on pedogenesis and landscape evolution in a Quaternary intramontane basin (Val D’agri basin, Southern Apennines, Italy). J Sedim Res 82:283–309CrossRefGoogle Scholar

Copyright information

© Accademia Nazionale dei Lincei 2014

Authors and Affiliations

  1. 1.Department of Earth Sciences, Environment and ResourcesUniversity of Naples Federico IINaplesItaly
  2. 2.Department of Science and TechnologyUniversity of SannioBeneventoItaly

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