Enrique Fernández-Palacios, Margarita Jambrina-Enríquez, Susan M. Mentzer, Caterina Rodríguez de Vera, Ada Dinckal, Natalia Égüez, Antonio V. Herrera-Herrera, Juan Francisco Navarro Mederos, Efraín Marrero Salas, Christopher E. Miller, Carolina Mallol
{"title":"通过多元地质考古方法重建加那利群岛Belmaco洞穴(西班牙拉帕尔马)土著遗址的形成过程","authors":"Enrique Fernández-Palacios, Margarita Jambrina-Enríquez, Susan M. Mentzer, Caterina Rodríguez de Vera, Ada Dinckal, Natalia Égüez, Antonio V. Herrera-Herrera, Juan Francisco Navarro Mederos, Efraín Marrero Salas, Christopher E. Miller, Carolina Mallol","doi":"10.1002/gea.21972","DOIUrl":null,"url":null,"abstract":"<p>The indigenous populations of La Palma (Canary Islands), who arrived on the island from Northwest Africa ca. 2000 years B.P., were predominantly pastoralists. Yet, many aspects of their subsistence economy such as the procurement, management, and use of wild plant resources remain largely unknown. To explore this, we studied the 600–1100-year-old archaeological site of Belmaco Cave, which comprises a stratified sedimentary deposit representative of a <i>fumier</i>. Here, we present a high-resolution, multiproxy geoarchaeological study combining soil micromorphology, lipid biomarker analysis, X-ray diffraction, μ-X-ray diffraction, μ-X-ray fluorescence, Fourier transform infrared spectroscopy, and μ-Fourier transform infrared spectroscopy, to characterize formation processes and explore plant sources. Recurrent goat/sheep habitation and maintenance activities are represented by interstratified layers of unburned dung, charcoal-rich sediment, and dung ash. Lipid biomarker data show a herd diet mainly composed of herbaceous plants, which is key to understanding the mobility of indigenous shepherds. Our results also revealed an unusual suite of authigenic minerals including hazenite, aragonite, and sylvite, possibly formed through diagenetic processes involving interaction between ash, dung, urine, volcanogenic components, and bacterial activity, coupled with arid and alkaline conditions. Our study shows the potential of a multiproxy approach to a <i>fumier</i> deposit in a volcanogenic sedimentary context.</p>","PeriodicalId":55117,"journal":{"name":"Geoarchaeology-An International Journal","volume":"38 6","pages":"713-739"},"PeriodicalIF":1.4000,"publicationDate":"2023-07-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/gea.21972","citationCount":"2","resultStr":"{\"title\":\"Reconstructing formation processes at the Canary Islands indigenous site of Belmaco Cave (La Palma, Spain) through a multiproxy geoarchaeological approach\",\"authors\":\"Enrique Fernández-Palacios, Margarita Jambrina-Enríquez, Susan M. Mentzer, Caterina Rodríguez de Vera, Ada Dinckal, Natalia Égüez, Antonio V. Herrera-Herrera, Juan Francisco Navarro Mederos, Efraín Marrero Salas, Christopher E. Miller, Carolina Mallol\",\"doi\":\"10.1002/gea.21972\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>The indigenous populations of La Palma (Canary Islands), who arrived on the island from Northwest Africa ca. 2000 years B.P., were predominantly pastoralists. Yet, many aspects of their subsistence economy such as the procurement, management, and use of wild plant resources remain largely unknown. To explore this, we studied the 600–1100-year-old archaeological site of Belmaco Cave, which comprises a stratified sedimentary deposit representative of a <i>fumier</i>. Here, we present a high-resolution, multiproxy geoarchaeological study combining soil micromorphology, lipid biomarker analysis, X-ray diffraction, μ-X-ray diffraction, μ-X-ray fluorescence, Fourier transform infrared spectroscopy, and μ-Fourier transform infrared spectroscopy, to characterize formation processes and explore plant sources. Recurrent goat/sheep habitation and maintenance activities are represented by interstratified layers of unburned dung, charcoal-rich sediment, and dung ash. Lipid biomarker data show a herd diet mainly composed of herbaceous plants, which is key to understanding the mobility of indigenous shepherds. Our results also revealed an unusual suite of authigenic minerals including hazenite, aragonite, and sylvite, possibly formed through diagenetic processes involving interaction between ash, dung, urine, volcanogenic components, and bacterial activity, coupled with arid and alkaline conditions. 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Reconstructing formation processes at the Canary Islands indigenous site of Belmaco Cave (La Palma, Spain) through a multiproxy geoarchaeological approach
The indigenous populations of La Palma (Canary Islands), who arrived on the island from Northwest Africa ca. 2000 years B.P., were predominantly pastoralists. Yet, many aspects of their subsistence economy such as the procurement, management, and use of wild plant resources remain largely unknown. To explore this, we studied the 600–1100-year-old archaeological site of Belmaco Cave, which comprises a stratified sedimentary deposit representative of a fumier. Here, we present a high-resolution, multiproxy geoarchaeological study combining soil micromorphology, lipid biomarker analysis, X-ray diffraction, μ-X-ray diffraction, μ-X-ray fluorescence, Fourier transform infrared spectroscopy, and μ-Fourier transform infrared spectroscopy, to characterize formation processes and explore plant sources. Recurrent goat/sheep habitation and maintenance activities are represented by interstratified layers of unburned dung, charcoal-rich sediment, and dung ash. Lipid biomarker data show a herd diet mainly composed of herbaceous plants, which is key to understanding the mobility of indigenous shepherds. Our results also revealed an unusual suite of authigenic minerals including hazenite, aragonite, and sylvite, possibly formed through diagenetic processes involving interaction between ash, dung, urine, volcanogenic components, and bacterial activity, coupled with arid and alkaline conditions. Our study shows the potential of a multiproxy approach to a fumier deposit in a volcanogenic sedimentary context.
期刊介绍:
Geoarchaeology is an interdisciplinary journal published six times per year (in January, March, May, July, September and November). It presents the results of original research at the methodological and theoretical interface between archaeology and the geosciences and includes within its scope: interdisciplinary work focusing on understanding archaeological sites, their environmental context, and particularly site formation processes and how the analysis of sedimentary records can enhance our understanding of human activity in Quaternary environments. Manuscripts should examine the interrelationship between archaeology and the various disciplines within Quaternary science and the Earth Sciences more generally, including, for example: geology, geography, geomorphology, pedology, climatology, oceanography, geochemistry, geochronology, and geophysics. We also welcome papers that deal with the biological record of past human activity through the analysis of faunal and botanical remains and palaeoecological reconstructions that shed light on past human-environment interactions. The journal also welcomes manuscripts concerning the examination and geological context of human fossil remains as well as papers that employ analytical techniques to advance understanding of the composition and origin or material culture such as, for example, ceramics, metals, lithics, building stones, plasters, and cements. Such composition and provenance studies should be strongly grounded in their geological context through, for example, the systematic analysis of potential source materials.