The Role of Mineral and Organic Composition on the Phosphorus Content of Prehistoric Pottery (Middle Neolithic to Late Bronze Age) from NW Spain

被引:0
作者
Gonzalez, Maria Guadalupe Castro [1 ,2 ]
Martinez, Maria Pilar Prieto [1 ,2 ]
Cortizas, Antonio Martinez [3 ,4 ]
机构
[1] Ctr Invest Interuniv Paisajes Atlanticos Culturale, Edificio Fontan, Santiago De Compostela 15707, Spain
[2] Univ Santiago de Compostela, EcoPast, Fac Xeog & Hist, Santiago De Compostela 15782, Spain
[3] Univ Santiago de Compostela, Ctr Invest Interdisciplinar Tecnoloxias Ambientais, EcoPast, Fac Biol, Campus Vida,Rua Lope Gomez de Marzoa 15, Santiago De Compostela 15782, Spain
[4] Stockholm Univ, Bolin Ctr Climate Res, S-10691 Stockholm, Sweden
关键词
phosphorus; prehistoric pottery; NW Spain; XRF; XRD; FTIR-ATR; albite; K-feldspar; aromatics phosphorylation; ANCIENT CERAMICS; SOIL; BONE; PHOSPHATE; DIAGENESIS; POTS; SITE; ORGANIZATION; DECORATION; IDENTITY;
D O I
10.3390/min14090880
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Phosphorus is a key element for identifying past human activity. Recently, phosphorus analyses have been extended to archaeological objects, aiming at distinguishing how depositional contexts contribute to its enrichment. In archaeological pottery, phosphorus might depend on several manufacturing and postdepositional processes (i.e., addition of organic temper, pigments, diagenetic incorporation). We analyzed by XRD, XRF, and mid-infrared (FTIR-ATR) spectroscopy 178 pots from eight NW Spain archaeological sites. These sites encompass different chronologies, contexts, and local geology. The phosphorus content was highly variable (224-27,722 mg kg-1) overall but also between archeological sites (1644 +/- 487 to 13,635 +/- 6623 mg kg-1) and within archaeological sites (4-36, max/min ratio). No phosphate minerals were identified by XRD nor FTIR-ATR, but correlations between phosphorus content and MIR absorbances showed maxima at 1515 and 980 cm-1, suggesting the presence of two sources: one organic (i.e., phosphorylated aromatic compounds) and another inorganic (i.e., albite and K-feldspar). Phosphorylated aromatics were most likely formed during pottery firing and were preserved due to their high resistance to temperature and oxidation. Meanwhile, albite and K-feldspar are among the P-bearing minerals with higher P concentrations. Our results suggest that P content is related to intentional and non-intentional actions taken in the pottery production process.
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页数:18
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