Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya)

We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site h...
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Autor*in:	Zerboni, Andrea [verfasserIn] Mori, Lucia Bosi, Giovanna Buldrini, Fabrizio Bernasconi, Andrea Gatto, Maria Carmela Mercuri, Anna Maria

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2017transfer abstract

Schlagwörter:	Anthracology Thin section micromorphology Tamarix Fuel Domestic fireplaces Gypsum redistribution Late Holocene Saharan oasis

Umfang:	16

Übergeordnetes Werk:	Enthalten in: Effects of heating intensity on the transient natural convection flows in open cavities - Zamora, Blas ELSEVIER, 2016, Kidlington
Übergeordnetes Werk:	volume:144 ; year:2017 ; pages:123-138 ; extent:16

Links:	Volltext

DOI / URN:	10.1016/j.jaridenv.2017.03.012

Katalog-ID:	ELV025024957

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520			\|a We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals.
520			\|a We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals.
650		7	\|a Anthracology \|2 Elsevier
650		7	\|a Thin section micromorphology \|2 Elsevier
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650		7	\|a Fuel \|2 Elsevier
650		7	\|a Domestic fireplaces \|2 Elsevier
650		7	\|a Gypsum redistribution \|2 Elsevier
650		7	\|a Late Holocene Saharan oasis \|2 Elsevier
700	1		\|a Mori, Lucia \|4 oth
700	1		\|a Bosi, Giovanna \|4 oth
700	1		\|a Buldrini, Fabrizio \|4 oth
700	1		\|a Bernasconi, Andrea \|4 oth
700	1		\|a Gatto, Maria Carmela \|4 oth
700	1		\|a Mercuri, Anna Maria \|4 oth
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allfields	10.1016/j.jaridenv.2017.03.012 doi GBVA2017002000009.pica (DE-627)ELV025024957 (ELSEVIER)S0140-1963(17)30056-3 DE-627 ger DE-627 rakwb eng 333.7 910 333.7 DE-600 910 DE-600 620 VZ 600 VZ 51.79 bkl 51.45 bkl Zerboni, Andrea verfasserin aut Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya) 2017transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. Anthracology Elsevier Thin section micromorphology Elsevier Tamarix Elsevier Fuel Elsevier Domestic fireplaces Elsevier Gypsum redistribution Elsevier Late Holocene Saharan oasis Elsevier Mori, Lucia oth Bosi, Giovanna oth Buldrini, Fabrizio oth Bernasconi, Andrea oth Gatto, Maria Carmela oth Mercuri, Anna Maria oth Enthalten in Elsevier Zamora, Blas ELSEVIER Effects of heating intensity on the transient natural convection flows in open cavities 2016 Kidlington (DE-627)ELV014628236 volume:144 year:2017 pages:123-138 extent:16 https://doi.org/10.1016/j.jaridenv.2017.03.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_22 GBV_ILN_40 GBV_ILN_105 GBV_ILN_2021 51.79 Sonstige Werkstoffe VZ 51.45 Werkstoffe mit besonderen Eigenschaften VZ AR 144 2017 123-138 16 045F 333.7
spelling	10.1016/j.jaridenv.2017.03.012 doi GBVA2017002000009.pica (DE-627)ELV025024957 (ELSEVIER)S0140-1963(17)30056-3 DE-627 ger DE-627 rakwb eng 333.7 910 333.7 DE-600 910 DE-600 620 VZ 600 VZ 51.79 bkl 51.45 bkl Zerboni, Andrea verfasserin aut Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya) 2017transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. Anthracology Elsevier Thin section micromorphology Elsevier Tamarix Elsevier Fuel Elsevier Domestic fireplaces Elsevier Gypsum redistribution Elsevier Late Holocene Saharan oasis Elsevier Mori, Lucia oth Bosi, Giovanna oth Buldrini, Fabrizio oth Bernasconi, Andrea oth Gatto, Maria Carmela oth Mercuri, Anna Maria oth Enthalten in Elsevier Zamora, Blas ELSEVIER Effects of heating intensity on the transient natural convection flows in open cavities 2016 Kidlington (DE-627)ELV014628236 volume:144 year:2017 pages:123-138 extent:16 https://doi.org/10.1016/j.jaridenv.2017.03.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_22 GBV_ILN_40 GBV_ILN_105 GBV_ILN_2021 51.79 Sonstige Werkstoffe VZ 51.45 Werkstoffe mit besonderen Eigenschaften VZ AR 144 2017 123-138 16 045F 333.7
allfields_unstemmed	10.1016/j.jaridenv.2017.03.012 doi GBVA2017002000009.pica (DE-627)ELV025024957 (ELSEVIER)S0140-1963(17)30056-3 DE-627 ger DE-627 rakwb eng 333.7 910 333.7 DE-600 910 DE-600 620 VZ 600 VZ 51.79 bkl 51.45 bkl Zerboni, Andrea verfasserin aut Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya) 2017transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. Anthracology Elsevier Thin section micromorphology Elsevier Tamarix Elsevier Fuel Elsevier Domestic fireplaces Elsevier Gypsum redistribution Elsevier Late Holocene Saharan oasis Elsevier Mori, Lucia oth Bosi, Giovanna oth Buldrini, Fabrizio oth Bernasconi, Andrea oth Gatto, Maria Carmela oth Mercuri, Anna Maria oth Enthalten in Elsevier Zamora, Blas ELSEVIER Effects of heating intensity on the transient natural convection flows in open cavities 2016 Kidlington (DE-627)ELV014628236 volume:144 year:2017 pages:123-138 extent:16 https://doi.org/10.1016/j.jaridenv.2017.03.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_22 GBV_ILN_40 GBV_ILN_105 GBV_ILN_2021 51.79 Sonstige Werkstoffe VZ 51.45 Werkstoffe mit besonderen Eigenschaften VZ AR 144 2017 123-138 16 045F 333.7
allfieldsGer	10.1016/j.jaridenv.2017.03.012 doi GBVA2017002000009.pica (DE-627)ELV025024957 (ELSEVIER)S0140-1963(17)30056-3 DE-627 ger DE-627 rakwb eng 333.7 910 333.7 DE-600 910 DE-600 620 VZ 600 VZ 51.79 bkl 51.45 bkl Zerboni, Andrea verfasserin aut Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya) 2017transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. Anthracology Elsevier Thin section micromorphology Elsevier Tamarix Elsevier Fuel Elsevier Domestic fireplaces Elsevier Gypsum redistribution Elsevier Late Holocene Saharan oasis Elsevier Mori, Lucia oth Bosi, Giovanna oth Buldrini, Fabrizio oth Bernasconi, Andrea oth Gatto, Maria Carmela oth Mercuri, Anna Maria oth Enthalten in Elsevier Zamora, Blas ELSEVIER Effects of heating intensity on the transient natural convection flows in open cavities 2016 Kidlington (DE-627)ELV014628236 volume:144 year:2017 pages:123-138 extent:16 https://doi.org/10.1016/j.jaridenv.2017.03.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_22 GBV_ILN_40 GBV_ILN_105 GBV_ILN_2021 51.79 Sonstige Werkstoffe VZ 51.45 Werkstoffe mit besonderen Eigenschaften VZ AR 144 2017 123-138 16 045F 333.7
allfieldsSound	10.1016/j.jaridenv.2017.03.012 doi GBVA2017002000009.pica (DE-627)ELV025024957 (ELSEVIER)S0140-1963(17)30056-3 DE-627 ger DE-627 rakwb eng 333.7 910 333.7 DE-600 910 DE-600 620 VZ 600 VZ 51.79 bkl 51.45 bkl Zerboni, Andrea verfasserin aut Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya) 2017transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals. Anthracology Elsevier Thin section micromorphology Elsevier Tamarix Elsevier Fuel Elsevier Domestic fireplaces Elsevier Gypsum redistribution Elsevier Late Holocene Saharan oasis Elsevier Mori, Lucia oth Bosi, Giovanna oth Buldrini, Fabrizio oth Bernasconi, Andrea oth Gatto, Maria Carmela oth Mercuri, Anna Maria oth Enthalten in Elsevier Zamora, Blas ELSEVIER Effects of heating intensity on the transient natural convection flows in open cavities 2016 Kidlington (DE-627)ELV014628236 volume:144 year:2017 pages:123-138 extent:16 https://doi.org/10.1016/j.jaridenv.2017.03.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_22 GBV_ILN_40 GBV_ILN_105 GBV_ILN_2021 51.79 Sonstige Werkstoffe VZ 51.45 Werkstoffe mit besonderen Eigenschaften VZ AR 144 2017 123-138 16 045F 333.7
language	English
source	Enthalten in Effects of heating intensity on the transient natural convection flows in open cavities Kidlington volume:144 year:2017 pages:123-138 extent:16
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authorswithroles_txt_mv	Zerboni, Andrea @@aut@@ Mori, Lucia @@oth@@ Bosi, Giovanna @@oth@@ Buldrini, Fabrizio @@oth@@ Bernasconi, Andrea @@oth@@ Gatto, Maria Carmela @@oth@@ Mercuri, Anna Maria @@oth@@
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author	Zerboni, Andrea
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title	Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya)
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title_full	Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya)
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title_sort	domestic firing activities and fuel consumption in a saharan oasis: micromorphological and archaeobotanical evidence from the garamantian site of fewet (central sahara, sw libya)
title_auth	Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya)
abstract	We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals.
abstractGer	We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals.
abstract_unstemmed	We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals.
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title_short	Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya)
url	https://doi.org/10.1016/j.jaridenv.2017.03.012
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author2	Mori, Lucia Bosi, Giovanna Buldrini, Fabrizio Bernasconi, Andrea Gatto, Maria Carmela Mercuri, Anna Maria
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up_date	2024-07-06T23:01:02.026Z
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This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">We describe a combined geoarchaeological and archaeobotanical approach applied to the study of firing activities that have been carried out at Fewet, a Garamantian compound in the Central Sahara (Libya), between the 3rd century BC and the 1st century AD. The archaeological stratigraphy of the site has been sealed by several mud-brick wall collapses, preserving an interesting sequence of living floors, whose micromorphological study is unique for the Central Sahara. This investigation together with the mineralogical analysis of sediments, confirms the field attribution of archaeological features as domestic fireplaces, and identified the living floors as areas devoted to animal penning, probably subjected to periodical firing. The investigation also highlights an exceptional concentration of gypsum pedofeatures, presumably determined by the wood type selected for fuel. The archaeobotanical study identified a good quantity of charcoal and other plant remains in the same layers. Most of the charcoal has been identified as Central Tamarix, which is the most common tree living in the oasis today. This suggests that tamarisk wood was the most exploited tree for fuel, and its combustion led to the dispersion of gypsum from the plant tissue, later recrystallized in the shape of microcrystalline nodules, lenses, and euhedral crystals.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Anthracology</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Thin section micromorphology</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Tamarix</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Fuel</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Domestic fireplaces</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Gypsum redistribution</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Late Holocene Saharan oasis</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mori, Lucia</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bosi, Giovanna</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Buldrini, Fabrizio</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bernasconi, Andrea</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gatto, Maria Carmela</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mercuri, Anna Maria</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier</subfield><subfield code="a">Zamora, Blas ELSEVIER</subfield><subfield code="t">Effects of heating intensity on the transient natural convection flows in open cavities</subfield><subfield code="d">2016</subfield><subfield code="g">Kidlington</subfield><subfield code="w">(DE-627)ELV014628236</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:144</subfield><subfield code="g">year:2017</subfield><subfield code="g">pages:123-138</subfield><subfield code="g">extent:16</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.jaridenv.2017.03.012</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">51.79</subfield><subfield code="j">Sonstige Werkstoffe</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">51.45</subfield><subfield code="j">Werkstoffe mit besonderen Eigenschaften</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">144</subfield><subfield code="j">2017</subfield><subfield code="h">123-138</subfield><subfield code="g">16</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">333.7</subfield></datafield></record></collection>
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Domestic firing activities and fuel consumption in a Saharan oasis: Micromorphological and archaeobotanical evidence from the Garamantian site of Fewet (Central Sahara, SW Libya)

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