Buccheri, G., Capretto, G., Di Donato, V., Esposito, P., Ferruzza, G., Pecatore, T., Ermolli, E.R., Senatore, M.R., Sprovieri, M., Bertoldo, M., Carella, D. and Madonia, G. (2002) A High Resolution Record of the Last Deglaciation in the Southern Tyrrhenian Sea: Environmental and Climatic Evolution. Marine Geology, 186, 447-470.
http://dx.doi.org/10.1016/S0025-3227(02)00270-0

has been cited by the following article:

• TITLE: Analysis of Post-Burial Soil Developments of Pre-AD 79 Roman Paleosols near Pompeii (Italy)

  AUTHORS: Sebastian Vogel, Michael Märker

  KEYWORDS: Soil Liquid Phase, Soil Solid Phase, Post-Burial Soil Developments, Pre-AD 79 Roman Paleosol, Pompeii, Somma-Vesuvius

  JOURNAL NAME: Open Journal of Soil Science, Vol.4 No.10, October 17, 2014

  ABSTRACT: The AD 79 eruption of Somma-Vesuvius completely buried the ancient landscape around Pompeii (Italy) to some extent conserving the pre-AD 79 Roman paleosols of the Sarno River plain. To estimate potential post-burial soil developments of these paleosols detailed soil liquid and solid phase analysis were carried out. Firstly, an in-situ soil hydrological monitoring was conducted within a pre-AD 79 paleosol in natural undisturbed stratification. The results show that soil water flow and nutrient transport from the overlying volcanic deposits into the pre-AD 79 paleosol take place. Secondly, to estimate their influence on the paleosol’s mineral soil properties, the solid phase of four pre-AD 79 paleosols and associated modern unburied soils were analysed and compared. By combining the data from the soil liquid and solid phase analysis, potential post-burial changes in the paleosols were estimated. Finally, a rise of the mean groundwater table was determined since AD 79. This distinguishes the Sarno River plain into two different zones of post-burial soil developments: 1) lower altitudes where formerly terrestrial paleosols are now influenced by groundwater dynamics and 2) higher altitudes where the paleosols are still part of the vadose zone and rather influenced by infiltration water or interflow. Thus, the mechanism of potential post-burial soil development being active in the pre-AD 79 paleosols is not uniform for the entire Sarno River plain but strongly depends on the paleotopographic situation.