Microstratigraphy and diagenesis at the upper Pleistocene site of Esquilleu Cave (Cantabria, Spain)
FTIR and soil micromorphology were applied to selected sediments from the archaeological deposit of Esquilleu Cave, a late Middle Palaeolithic site in Cantabria, Spain. The main goal was to assess the integrity of the archaeological record before continuing with further excavation and research at th...
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| Published in | Quaternary international Vol. 214; no. 1; pp. 70 - 81 |
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| Main Authors | , , |
| Format | Journal Article |
| Language | English |
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01.03.2010
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| Abstract | FTIR and soil micromorphology were applied to selected sediments from the archaeological deposit of Esquilleu Cave, a late Middle Palaeolithic site in Cantabria, Spain. The main goal was to assess the integrity of the archaeological record before continuing with further excavation and research at the site. Field observations and previous sedimentological studies point to diagenetic alteration of part of the deposit, but the extent and precise nature of such processes had not been established. The results show that the upper layers are composed of fresh elements and have not undergone diagenetic transformations, although their components have been physically disturbed by cryoturbation. The rest of the deposit is well preserved with mild phosphatization due to partial dissolution of bone and calcitic ash contained in the sediment, and compression from trampling. Further excavation is necessary to have a more complete picture of the taphonomic processes taking place at the site. |
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| AbstractList | FTIR and soil micromorphology were applied to selected sediments from the archaeological deposit of Esquilleu Cave, a late Middle Palaeolithic site in Cantabria, Spain. The main goal was to assess the integrity of the archaeological record before continuing with further excavation and research at the site. Field observations and previous sedimentological studies point to diagenetic alteration of part of the deposit, but the extent and precise nature of such processes had not been established. The results show that the upper layers are composed of fresh elements and have not undergone diagenetic transformations, although their components have been physically disturbed by cryoturbation. The rest of the deposit is well preserved with mild phosphatization due to partial dissolution of bone and calcitic ash contained in the sediment, and compression from trampling. Further excavation is necessary to have a more complete picture of the taphonomic processes taking place at the site. |
| Author | Mallol, Carolina Baena, Javier Cabanes, Dan |
| Author_xml | – sequence: 1 givenname: Carolina surname: Mallol fullname: Mallol, Carolina email: carolina.mallol@gmail.com organization: Universidad de La Laguna, Departamento de Prehistoria, Antropología e Historia Antigua, Campus de Guajara, La Laguna 38071, Tenerife, Spain – sequence: 2 givenname: Dan surname: Cabanes fullname: Cabanes, Dan organization: Kimmel Center for Archaeological Science, Weizmann Institute of Science, Rehovot, Israel – sequence: 3 givenname: Javier surname: Baena fullname: Baena, Javier organization: Universidad Autónoma de Madrid, Departamento de Prehistoria y Arqueología, Campus de Cantoblanco, Madrid, Spain |
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| Cites_doi | 10.1016/j.jas.2003.12.003 10.1006/jhev.1999.0350 10.1006/jasc.2001.0790 10.1007/s12520-009-0008-1 10.1006/jasc.1996.0128 10.1016/S0341-8162(79)80013-2 10.1016/j.jas.2007.06.024 10.1006/jasc.1998.0354 10.1006/jasc.1999.0506 10.1016/S0003-5521(01)80050-9 10.1006/jasc.2001.0742 10.1006/jasc.1996.0071 10.1016/0305-4403(90)90058-D |
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| References_xml | – year: 1989 ident: bib6 article-title: Soil Micromorphology in Archaeology contributor: fullname: Macphail – year: 2003 ident: bib18 article-title: Guidelines for Analysis and Description of Soil and Regolith Thin Sections. 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