Hostname: page-component-cd9895bd7-fscjk Total loading time: 0 Render date: 2024-12-25T18:15:11.048Z Has data issue: false hasContentIssue false
  • English
  • Français

Glacio-Eustatic Control of Continental–Shallow Marine Cyclicity from Late Quaternary Deposits of the Southeastern Po Plain, Northern Italy

Published online by Cambridge University Press:  20 January 2017

Alessandro Amorosi ,
Maria Luisa Colalongo ,
Fabio Fusco ,
Giancarlo Pasini  and
Flavia Fiorini
Alessandro Amorosi
Affiliation:
Dipartimento di Scienze della Terra e Geologico-Ambientali, Università di Bologna, Via Zamboni 67, 40127, Bologna, Italy
Maria Luisa Colalongo
Affiliation:
Dipartimento di Scienze della Terra e Geologico-Ambientali, Università di Bologna, Via Zamboni 67, 40127, Bologna, Italy
Fabio Fusco
Affiliation:
Dipartimento di Scienze della Terra e Geologico-Ambientali, Università di Bologna, Via Zamboni 67, 40127, Bologna, Italy
Giancarlo Pasini
Affiliation:
Istituto di Geologia Marina, C.N.R. Via Gobetti 101, 40129, Bologna, Italy
Flavia Fiorini
Affiliation:
Dipartimento di Scienze della Terra e Geologico-Ambientali, Università di Bologna, Via Zamboni 67, 40127, Bologna, Italy
Get access Rights & Permissions [Opens in a new window]

Abstract

Integrated sedimentological and micropaleontological (foraminifera, ostracods, pollens) investigations of a 173-m-long continuous core in the subsurface of the SE Po Plain reveal a cyclic facies distribution of continental to shallow-marine deposits. Radiometric and pollen data enable an age attribution of the study units to the late Middle Pleistocene–Holocene. Glacioeustasy appears to have exerted a major control on facies development, as documented by the close relationships between cyclic lithofacies patterns and the curves of eustatic fluctuation. Particularly, relative sea-level falls and lowstand phases were characterized by the development of alluvial sedimentation, whereas major transgressive pulses and subsequent highstands are reflected by abrupt shifts to paralic and shallow-marine deposits. This facies architecture is paralleled by a distinctive pollen distribution, reflecting the alternation of a glacial type of vegetation, dominated by Pinus and nonarboreal pollen types, with interglacial mixed deciduous broad-leaved forests.

Keywords

cyclostratigraphycontinental depositsmarine depositsbenthic foraminiferaostracodspalynologyPo Plain, Italy
Type
Research Article
Information
Quaternary Research , Volume 52 , Issue 1 , July 1999 , pp. 1 - 13
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Aharon, P., Chappell, J..(1986). Oxygen isotopes, sea level changes and the temperature history of a coral reef environment in New Guinea over the last 105 year. Palaeogeography, Palaeoclimatology, Palaeoecology. 56, (1986). 337–379.Google Scholar
Amorosi, A., Farina, M..(1995). Large-scale architecture of a thrust-related alluvial complex from subsurface data: The Quaternary succession of the Po Basin in the Bologna area (northern Italy). Giornale di Geologia. 57, (1995). 3–16.Google Scholar
Amorosi, A., Colalongo, M.L., Pasini, G., Preti, D..(1999). Sedimentary response to Late Quaternary sea-level changes in the Romagna coastal plain (northern Italy). Sedimentology. 46, (1999). 99–121.CrossRefGoogle Scholar
Athersuch, J., Horne, D.J., Whittaker, J.E..(1989). Marine and Brackish Water Ostracods. Kermack, D.M., Barnes, R.S.K..Synopses of the British Fauna. (1989). Brill, Leiden, New York, Kopenaghen, Köln.Google Scholar
Bard, E., Hamelin, B., Fairbanks, R.G..(1990). U-Th ages obtained by mass spectrometry in corals from Barbados: Sea level during the past 130000 year. Nature. 346, (1990). 456–458.Google Scholar
Barmawidjaja, D.M., Jorissen, F.J., Puskaric, S., Van der Zwaan, G.J..(192). Microhabitat selection by benthic foraminifera in the northern Adriatic Sea. Journal of Foraminiferal Research. 22, (1992). 297–317.Google Scholar
Bellotti, P., Carboni, M.G., Di Bella, L., Palagi, I..(1994). Benthic foraminiferal assemblages in the depositional sequence of the Tiber Delta. Matteucci, R..Studies on Ecology and Palaeoecology of Benthic Communities. (1994). 29–40.Google Scholar
Bertoldi, R..(1995). Palinostratigrafia dei bacini intermontani dell'Appennino nordorientale. Il Quaternario. 8, (1995). 61–70.Google Scholar
de Beaulieu, J.J., Reille, M..(1992). The last climatic cycle at La Grand Pile (Vosges, France): A new pollen profile. Quaternary Science Review. 11, (1992). 431–438.Google Scholar
Devoto, G..(1965). Lacustrine Pleistocene in the Lower Liri Valley (Southern Latium). Geologica Romana. 4, (1965). 291–368.Google Scholar
Faegri, K., Iversen, J..Text Book in Pollen Analysis. (1992). Wiley & Sons, Chichester.Google Scholar
Follieri, M., Magri, D., Sadori, L..(1995). 250,000-year pollen record from Valle di Castiglione (Roma). Pollen et Spores. 30, (1988). 329–356.Google Scholar
Follieri, M., Magri, D., Sadori, L..(1989). Pollen stratigraphical synthesis from Valle di Castiglione (Roma). Quaternary International. 3/4, (1989). 81–84.Google Scholar
Helland-Hansen, W., Gjelberg, J.G..(1994). Conceptual basis and variability in sequence stratigraphy: A different perspective. Sedimentary Geology. 92, (1994). 31–52.CrossRefGoogle Scholar
Henderson, P.A..(1990). Freshwater ostracods. Kermack, D.M., Barnes, R.S.K..Synopses of the British Fauna. (1990). Universal Book Services, Dr. W. Backhuys, Oegstgeest.Google Scholar
Hunt, D., Tucker, M.E..(1992). Stranded parasequences and the forced regressive wedge systems tract: Deposition during base-level fall. Sedimentary Geology. 81, (1992). 1–9.Google Scholar
Jorissen, F.J..(1987). The distribution of benthic foraminifera in the Adriatic Sea. Marine Micropalaeontology. 12, (1987). 21–48.CrossRefGoogle Scholar
Jorissen, F.J..(1988). Benthic foraminifera from the Adriatic Sea: Principles of phenotypic variation. Utrecht Micropaleontological Bulletins. 37, (1988). 1–176.Google Scholar
Langer, M.R..(1993). Epiphytic foraminifera. Marine Micropalaeontology. 20, (1993). 235–265.CrossRefGoogle Scholar
Martinson, D.G., Pisias, N.G., Hayes, J.D., Imbrie, J., Moore, T.C., Shackleton, N.J..(1987). Age dating and the orbital theory of the ice ages—Development of a high-resolution 0 to 300,000 year chronostratigraphy. Quaternary Research. 27, (1987). 1–29.Google Scholar
Montenegro, M.E., Pugliese, N..(1995). Ostracodi della laguna di Orbetello: Tolleranza ed opportunismo. Atti del Museo di Geologia e Paleontologia di Monfalcone, Quaderno speciale. 3, (1995). 71–80.Google Scholar
Moore, P.D., Webb, J.A., Collinson, M.E..(1992). Pollen Analysis. (1992). Blackwell Sci, Oxford.Google Scholar
Nummedal, D., Swift, D.J.P..(1987). Transgressive stratigraphy at sequence-bounding unconformities: Some principles derived from Holocene and Cretaceous examples. Nummedal, D., Pilkey, O.H., Howard, J.D..Sea-Level Fluctuation and Coastal Evolution. (1987). 241–260.Google Scholar
Pirazzoli, P.A..(1993). Global sea-level changes and their measurement. Global and Planetary Change. 8, (1993). 135–148.Google Scholar
Posamentier, H.W., Jervey, M.T., Vail, P.R..(1988). Eustatic controls on clastic deposition. I. Conceptual framework. Wilgus, C.K., Hastings, B.S., St. C. Kendall, C.G., Posamentier, H.W., Ross, C.A., Van Wagoner, J.C..Sea Level Changes: An Integrated Approach. (1988). 109–124.Google Scholar
Posamentier, H.W., Allen, G.P., James, D.P., Tesson, M..(1992). Forced regressions in a sequence stratigraphic framework: Concepts, examples and sequence stratigraphic significance. American Association of Petroleum Geologists Bulletin. 76, (1992). 1687–1709.Google Scholar
Regione Emilia-Romagna and ENI-AGIP (1998). Riserve idriche sotterranee della Regione Emilia-Romagna. A cura di G. Di Dio. S.EL.CA., Firenze.Google Scholar
Reille, M., de Beaulieu, J.-L..(1990). Pollen analysis of a long upper Pleistocene continental sequence in a Velay maar (Massif Central, France). Palaeogeography, Palaeoclimatology, Palaeoecology. 80, (1990). 35–48.CrossRefGoogle Scholar
Sgarrella, F., Moncharmont Zei, M..(1993). Benthic Foraminifera of the Gulf of Naples (Italy): Systematics and autoecology. Bollettino della Società Paleontologica Italiana. 32, (1993). 145–264.Google Scholar
Socac, A..(1978). Pleistocene ostracode fauna of the Pannonian basin in Croatia. Palaeontologica Jugoslavica. 20, (1978). 1–51.Google Scholar
Stockmarr, J..(1971). Tablets with spores in absolute pollen analysis. Pollen et Spores. 13, (1971). 615–621.Google Scholar
Swift, D.J.P..(1968). Coastal erosion and transgressive stratigraphy. Journal of Geology. 76, (1968). 444–456.Google Scholar
Tzedakis, P.C..(1993). Long-term tree population in northwest Greece through multiple Quaternary climatic cycles. Nature. 364, (1993). 437–440.Google Scholar
Tzedakis, P.C..(1994). Vegetation change through glacial-interglacial cycles: A long pollen sequence perspective. Philosophical Transactions of the Royal Society of London, B. 345, (1994). 403–432.Google Scholar
Tzedakis, P.C., Andrieu, V., de Beaulieu, J.-L., Crowhurst, S., Follieri, M., Hooghiemstra, H., Magri, D., Reille, M., Sadori, L., Shackleton, N.J., Wijmstra, T.A..(1997). Comparison of terrestrial and marine records of changing climate of the last 500,000 year. Earth and Planetary Science Letters. 150, (1997). 171–176.Google Scholar
Van der Zwaan, G.J., Jorissen, F.J..(1991). Biofacial patterns in river-induced shelf anoxia. Tyson, R.V., Pearson, T.H..Modern and Ancient Continental Shelf Anoxia. (1991). 65–82.Google Scholar
Van Frausum, A., Wouters, K..(1990). Ostracoda from Holocene calcareous tufa deposits in southern Belgium: A palaeoenvironmental analysis. Whatley, R., Maybury, C..Ostracoda and Global Events. (1990). Chapman & Hall, London, New York., 505–514.Google Scholar
Veggiani, A. (1974). Le variazioni idrografiche del basso corso del fiume Po negli ultimi 3000 anni. Padusa, 1–2, Rovigo, 39–60.Google Scholar
Verhallen, P.J.J.M..(1991). Late Pliocene to early Pleistocene Mediterranean mud-dwelling foraminifera: Influence of a changing environment on community structure and evolution. Utrecht Micropaleontological Bulletins. 40, (1991). 1–220.Google Scholar
Wijmstra, T.A..(1969). Palynology of the first 30 m of a 120 m deep section in Northern Greece. Acta Botanica Neerlandica. 18, (1969). 511–527.Google Scholar
Wijmstra, T.A., Smit, A..(1976). Palynology of the middle part (30–78 metres) of the 120 m deep section in Northern Greece (Macedonia). Acta Botanica Neerlandica. 25, (1976). 297–312.Google Scholar
Woillard, G.M..(1978). Grand Pile peat bog: A continuous pollen record for the last 140.000 year. Quaternary Research. 9, (1978). 1–21.Google Scholar