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  • archaeological stratigraphy  (1)
  • biological markers  (1)
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  • 1
    Publication Date: 2019-03-29
    Description: This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast derived from sea-level index points whose elevation was determined by a differential global position system (DGPS). Bioencrustations from outcrops located near Camarones, Chubut, Argentina, consist of autochthonous deposits characterized by Austromegabalanus psittacus (Molina, 1782), encrusting acervulinid foraminifera, coralline red algae and bryozoans. The association of the different organisms is interpreted as being associated with an intertidal environment, and they have been used as index points to establish the relative sea-level position. The main conclusion is that the relative sea-level between c. 7000 and 5300 cal. yr BP was in the range of c. 2–4 m a.s.l., with a mean value of c. 3.5 m a.s.l. Our data seem to support the existence of different rates of relative sea-level fall in different sectors of Atlantic Patagonia during the Holocene and highlight the importance of a more precise and accurate relative sea-level estimation by producing new data and revisiting the indicative meaning of most of the indicators so far used in the area.
    Description: Published
    Description: 56–64
    Description: 5A. Paleoclima e ricerche polari
    Description: JCR Journal
    Keywords: Patagonia ; biological markers ; Holocene ; sea level
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2018-03-30
    Description: The results of a Ground-penetrating radar (GPR) survey were compared with the archaeological excavation outcomes of a twelfth century abbey site (Badia Pozzeveri). The goal was to associate the types of reflections recorded in GPR profiles and high-amplitude features visible in amplitude maps with unearthed archaeological features. GPR profiles crossing the walls evidenced axes of hyperbolic point source reflections and short planar reflections respectively generated by the stones forming the lateral sides/upper corners and the top of the structure. Moreover, the stones in the core of the wall caused small hyperbolic point source reflections with interfering axes, which produced a chaotic reflection profile. The resampling and gridding of these reflections collectively generated high-amplitude linear features in the amplitude maps. The presence in the graves of bones generates small hyperbolic point source reflections with interfering axes in the GPR profile, with a consequently chaotic reflection profile. Moreover, the existence of lythic slabs topping and/or siding the graves generates short planar reflections and axes of hyperbolic point source reflections. The resampling and gridding of these types of reflections generates in the amplitude map features that cannot be locally distinguished from those caused by the local aggregation of sediments with no archaeological relevance. The GPR profiles crossing trenches and pit-kiln showed dipping reflectors unconformably resting on a basal planar reflector. Disconformity marks the onset of trench and pit-kiln decommissioning with the infilling of clayey silty layers and anthropogenic remains. These features in the amplitude maps correspond to medium to high-amplitude areas. The results show that types of reflection can be associated to specific elements of archaeological structure for a detailed interpretation of a complex subsurface setting. Furthermore, it is evidenced that the interpretation of GPR profiles must be considered an indispensable pre-requisite for a full comprehension of amplitude maps
    Description: CA.RI.LU grant (2012-13): “New high resolution Georadar techniques for archeological contexts analysis” (Leader. A. Ribolini).
    Description: Published
    Description: 141 – 156
    Description: 7T. Struttura della Terra e geodinamica
    Description: JCR Journal
    Keywords: Ground-penetrating radar ; archaeological stratigraphy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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