Journal articles on the topic 'Archaeological chemistry'

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1

Rice, Prudence M., Curt W. Beck, Robert F. Gould, Giles F. Carter, Joseph B. Lambert, M. Joan Comstock, and Zvi Goffer. "Archaeological Chemistry." American Antiquity 52, no. 1 (January 1987): 202. http://dx.doi.org/10.2307/281079.

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2

Lambert, Joseph B. "Archaeological Chemistry." Accounts of Chemical Research 35, no. 8 (August 2002): 583–84. http://dx.doi.org/10.1021/ar020159b.

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3

Grieken, Van, and M. Adriaens. "Archaeological chemistry." Analytica Chimica Acta 338, no. 1-2 (February 1997): 164. http://dx.doi.org/10.1016/s0003-2670(97)85325-1.

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4

Thomas, Jacob, Louis J. Thibodeaux, Ann F. Ramenofsky, Stephen P. Field, Bob J. Miller, and Ann M. Whitmer. "Archaeological chemistry." Environmental Science & Technology 22, no. 5 (May 1988): 480–87. http://dx.doi.org/10.1021/es00170a001.

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5

Green, Christopher. "Archaeological chemistry." Endeavour 20, no. 3 (January 1996): 134. http://dx.doi.org/10.1016/0160-9327(96)88971-x.

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6

Burton, James H. "Archaeological chemistry." Geoarchaeology 12, no. 5 (August 1997): 497–99. http://dx.doi.org/10.1002/(sici)1520-6548(199708)12:5<497::aid-gea4>3.0.co;2-v.

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7

Oddy, W. A., and Joseph B. Lambert. "Archaeological Chemistry III." Studies in Conservation 30, no. 1 (February 1985): 43. http://dx.doi.org/10.2307/1506135.

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8

Scott, David A., and Ralph O. Allen. "Archaeological Chemistry IV." Studies in Conservation 35, no. 3 (August 1990): 166. http://dx.doi.org/10.2307/1506172.

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9

Stech, Tamara, and Joseph B. Lambert. "Archaeological Chemistry 3." American Journal of Archaeology 89, no. 2 (April 1985): 357. http://dx.doi.org/10.2307/504338.

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10

Burton, James H. "Archaeological Chemistry. Zvi Goffer." Journal of Anthropological Research 65, no. 1 (April 2009): 119–20. http://dx.doi.org/10.1086/jar.65.1.25608156.

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11

Evershed, Richard P., Stephanie N. Dudd, Mark S. Copley, Robert Berstan, Andrew W. Stott, Hazel Mottram, Stephen A. Buckley, and Zoe Crossman. "Chemistry of Archaeological Animal Fats." Accounts of Chemical Research 35, no. 8 (August 2002): 660–68. http://dx.doi.org/10.1021/ar000200f.

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12

Nigra, Benjamin T., Kym F. Faull, and Hans Barnard. "Analytical Chemistry in Archaeological Research." Analytical Chemistry 87, no. 1 (November 12, 2014): 3–18. http://dx.doi.org/10.1021/ac5029616.

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13

Salisbury, Roderick. "Advances in Archaeological Soil Chemistry in Central Europe." Interdisciplinaria Archaeologica, Natural Sciences in Archaeology XI, no. 2 (December 17, 2020): 199–211. http://dx.doi.org/10.24916/iansa.2020.2.5.

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Analytical technologies for the evaluation of archaeological soils have developed rapidly in recent decades, and now support a range of innovative research and interpretations of archaeological sites and landscapes. Established methods, including phosphates and multi-element ICP-MS/OES, have provided interpretations of the use of space within settlements and houses, and the function of specific archaeological features. Recently, portable X-Ray Fluorescence has been introduced to archaeological soil science, but published results have generated knowledge gaps. The correspondence between archaeological geochemical anomalies and specific human activities is partly dependent on geology (including sediment type and relative acidity and permeability of the soil), topography, and formation processes, as well as influence of human activities. At the same time, which elements, and fractions of elements, are measured is largely dependent on instrument parameters and extraction methods. This paper provides an overview of archaeological soil chemistry in Central Europe, and the current state-of-the-art, followed by an assessment of future developments in archaeological soil chemistry, molecular biogeochemistry, and the significance of geoarchaeology in multi-disciplinary research.
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14

Spriggs, James A., R. M. Rowell, and R. J. Barbour. "Archaeological Wood--Properties, Chemistry, and Preservation." Journal of Field Archaeology 18, no. 2 (1991): 249. http://dx.doi.org/10.2307/530270.

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15

Moshenska, Gabriel. "Michael Faraday's Contributions to Archaeological Chemistry." Ambix 62, no. 3 (August 2015): 266–86. http://dx.doi.org/10.1179/1745823415y.0000000004.

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16

Harper, Clare S., Faith V. Macdonald, and Kevin L. Braun. "Lipid Residue Analysis of Archaeological Pottery: An Introductory Laboratory Experiment in Archaeological Chemistry." Journal of Chemical Education 94, no. 9 (July 21, 2017): 1309–13. http://dx.doi.org/10.1021/acs.jchemed.7b00225.

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17

Oddy, Andrew, and Mary Virginia Orna. "Archaeological Chemistry: Organic, Inorganic, and Biochemical Analysis." Studies in Conservation 43, no. 1 (1998): 60. http://dx.doi.org/10.2307/1506638.

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18

Oddy, W. A. "Chemistry in the conservation of archaeological materials." Science of The Total Environment 143, no. 1 (March 1994): 121–26. http://dx.doi.org/10.1016/0048-9697(94)90538-x.

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19

Schweizer, François. "Chemistry and the conservation of archaeological metals." Science of The Total Environment 143, no. 1 (March 1994): 127–29. http://dx.doi.org/10.1016/0048-9697(94)90539-8.

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20

Redman, J. E., M. I. Stewart, and A. M. Gernaey. "Ancient tuberculosis and lipid chemistry – odd bedfellows!" European Journal of Archaeology 5, no. 1 (2002): 112–20. http://dx.doi.org/10.1179/eja.2002.5.1.112.

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Tuberculosis (TB), the disease caused byMycobacterium tuberculosis, has afflicted mankind for millennia. Currently, the diagnosis of TB from archaeological specimens relies on the identification of bone changes. This method is problematic, since the bone changes seen in TB are not exclusive to the disease. Here, we examine the state-of-the-art of ancient TB diagnosis using the biomarker approach. The development of biomarkers for the detection of ancient TB will provide a reliable means of diagnosis and provide archaeology with a useful tool for the investigation of the disease in archaeological populations.
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21

Rowe, M. W. "Archaeological dating." Journal of Chemical Education 63, no. 1 (January 1986): 16. http://dx.doi.org/10.1021/ed063p16.

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22

HARBOTTLE, G. "ChemInform Abstract: Neutron Activation Analysis in Archaeological Chemistry." ChemInform 22, no. 1 (August 23, 2010): no. http://dx.doi.org/10.1002/chin.199101383.

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23

Costa, Marcondes Lima da, Gaspar Morcote Rios, Mônia Maria Carvalho da Silva, Glayce Jholy da Silva, and Uliana Molano-Valdes. "Mineralogy and chemistry of archaeological ceramic fragments from archaeological Dark Earth site in Colombian Amazon." Rem: Revista Escola de Minas 64, no. 1 (March 2011): 17–23. http://dx.doi.org/10.1590/s0370-44672011000100002.

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Several Archaeological Dark Earth (ADE) sites have been already found in the Colombian Amazon forest showing high content of archaeological ceramic fragments similarly to those in the Brazilian Amazon represented by Quebrada Tacana site. Their fragments are yellow to grey colour, display a burned clayey matrix which involves fragments of cariapé and coal and ash particles, besides grains of quartz and micas. The clay matrix is made of metakaolinite, quartz, and some mica flakes, chlorite and sepiolite. Cariapé and cauixi spicules are constituted of cristobalite, which is also the main mineral component of the coal and ashes. Although not detected by X-ray diffraction, the phosphate minerals should be present, since the contents of phosphor reach up to 2.90 Wt.% P2O5. Possibly it occurs as aluminium-phosphate, since Ca contents fall below 0.1 Wt.%. These mineralogical and chemical characteristics allow to correlate these ceramic fragments with those found in the ADE in Brazil and reinforce phosphor as an important chemical component, which indicates human activity by the daily use of pottery all over the Amazon region.
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24

Dumanov, Boyan, Zhivko Uzunov, Bilyana Kostova, Irena Dimitrova, and Ventsislava Ivanova. "Archaeological and Geological Approaches in the Work on the Project “Materiality and ancient environmental knowledge reconstruction trough archaeological chemistry analytical techniques (RE:MATRIARCHES)”." Annual of Natural Sciences Department 6 (November 19, 2021): 63–72. http://dx.doi.org/10.33919/ansd.20-21.6.6.

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The study discusses new approaches designed for the purposeful selection of archeological and geological sites and sample collection for analysis via archaeological chemistry techniques. The approaches discussed provide opportunities for coherent interpretation of analytical data in view of the project’s objectives: gaining fundamental knowledge of material culture in different archaeological periods as well as of people’s knowledge of the environment in ancient times.
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25

Parker, Andrew, and A. Mark Pollard. "Archaeological geochemistry." Applied Geochemistry 21, no. 10 (October 2006): 1625. http://dx.doi.org/10.1016/j.apgeochem.2006.07.001.

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26

Scott, Catherine B. "Integrating Multi-Scalar Sampling Strategies for Archaeological Sediment Chemistry." Journal of Field Archaeology 45, no. 8 (August 30, 2020): 588–607. http://dx.doi.org/10.1080/00934690.2020.1808751.

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27

Karapanagiotis, Ioannis. "A Review on the Archaeological Chemistry of Shellfish Purple." Sustainability 11, no. 13 (June 29, 2019): 3595. http://dx.doi.org/10.3390/su11133595.

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Shellfish purple, also known as Tyrian purple and royal purple, has a long history, which has been revealed and documented in recent years through valid physicochemical studies using sophisticated techniques. The aim of the work was to summarize the conclusions of these studies and to describe the results of two unpublished investigations regarding the (i) identification of shellfish purple in a textile (4th century BCE) from ancient Macedonia and (ii) dramatic effect of the dyeing conditions on the composition of the purple dye. Moreover, a critical discussion is included about the discovery of the shellfish pigment and dye based on the available scientific evidence. Previously published reports describing the identification of the shellfish colorant in objects of the cultural heritage were carefully summarized. Shellfish purple was not used only as colorant, but it served other purposes as emphasized in this review. In particular, examples for the use of shellfish purple in medicine, grave goods and fillers and plasters in walls, were described. Examples of materials and methods that were used in the past to produce “fake” purple, imitating the aesthetic result of the valuable royal marine material were summarized. Finally, the solubility of indigoids was discussed using modern approaches of physical chemistry.
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28

Wells, E. Christian. "Sampling Design and Inferential Bias in Archaeological Soil Chemistry." Journal of Archaeological Method and Theory 17, no. 3 (July 9, 2010): 209–30. http://dx.doi.org/10.1007/s10816-010-9087-7.

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29

Pollard, A. M. "Why teach Heisenberg to archaeologists?" Antiquity 69, no. 263 (June 1995): 242–47. http://dx.doi.org/10.1017/s0003598x00064668.

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The archaeological department at the University of Bradford is the only one in Britain to be called a Department of Archaeological Sciences. Its Professor–whose own background was in physics and then chemistry before archaeology–explores the relationship of archaeology to the sciences in a contribution adapted from his talk given at Harvard University on Science and archaeology.
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30

Sillen, Andrew, Judith C. Sealy, and Nikolaas J. van der Merwe. "Chemistry and Paleodietary Research: No More Easy Answers." American Antiquity 54, no. 3 (July 1989): 504–12. http://dx.doi.org/10.2307/280778.

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While isotopic and elemental analyses of prehistoric skeletons have made an important contribution to paleodietary research over the last 10 years, certain problems in the application of these techniques only now are emerging. These problems, affecting both isotopic and trace-element studies, mainly are due to the peculiar interdisciplinary nature of the field, rather than to any technological barrier. With minor exceptions, techniques developed largely in other sciences have been grafted on to archaeological problems. This no longer suffices because gaps remain in the scientific grounding of these techniques that need to be addressed before more complicated archaeological questions can be resolved. While the necessary studies may seem to be of little immediate anthropological interest, they are vital if continued progress in paleodietary research is to characterize the years ahead.
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31

Ezzo, Joseph A. "Putting the "Chemistry" Back into Archaeological Bone Chemistry Analysis: Modeling Potential Paleodietary Indicators." Journal of Anthropological Archaeology 13, no. 1 (March 1994): 1–34. http://dx.doi.org/10.1006/jaar.1994.1002.

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32

Service, Robert F. "Rock Chemistry Traces Ancient Traders." Science 274, no. 5295 (December 20, 1996): 2012–13. http://dx.doi.org/10.1126/science.274.5295.2012.b.

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Boston—At a meeting of the Materials Research Society here earlier this month, a Malaysian and an American researcher presented a chemical analysis that links volcanic glass at a 6000-year-old archaeological site on Borneo to sources on islands 3500 kilometers to the east. The finding pushes back the earliest dates for long-distance sea trading on the Pacific by 2500 years, to 4000 B.C.
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33

Pennetta, Antonio, and Giuseppe E. De Benedetto. "New Evidence on the Reliable Use of Stable Isotopes of Bitumen Fractions in Archaeological Research." Molecules 28, no. 4 (February 18, 2023): 1962. http://dx.doi.org/10.3390/molecules28041962.

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One of the goals of archaeological studies is to determine how material goods and ideas moved among human populations, and bitumen is a worthy proxy because it has been used since prehistory. As a result, when bitumen is excavated from archaeological sites, determining its provenance is important because it sheds light on the trade and communication of populations at a given time. During the study of archaeological bitumen from coastal sites in central and southern Puglia (Italy), we observed that stable isotope ratios of saturated and aromatic fractions were incompatible with those obtained from asphaltenes, supporting the absorption of a foreign substance. Experiments showed that lipids are absorbed by bitumen and, in the case of oils, are distributed mainly in the saturated and aromatic fractions as their isotopic ratios change. The same experiments showed that the isotopic ratios of the asphaltenes do not change. Lipid absorption on the archaeological bitumen may have occurred before the bitumen was applied to the pottery, during the use of the pottery or while underground, before being excavated. These hypotheses are discussed, and it is concluded that the isotopic ratio of asphaltenes is a reliable proxy for provenance, whereas those of the saturated and aromatic fractions should be considered with caution due to possible lipid absorption. Nevertheless, they provide new information on pottery use that can be used in archaeological chemistry.
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34

Katzenberg, M. Anne, and Roman G. Harrison. "What's in a bone? Recent advances in archaeological bone chemistry." Journal of Archaeological Research 5, no. 3 (September 1997): 265–93. http://dx.doi.org/10.1007/bf02229154.

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35

Giannossa, Lorena Carla, Tiziana Forleo, and Annarosa Mangone. "The Distinctive Role of Chemical Composition in Archaeometry. The Case of Apulian Red Figure Pottery." Applied Sciences 11, no. 7 (March 30, 2021): 3073. http://dx.doi.org/10.3390/app11073073.

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Correlation of the scientific approach to the archaeological investigation and vice versa is considered, for at least the past 30 years, as the best strategy to answer questions in cultural heritage. Many archaeological queries have merged archaeological and scientific studies and have been carried out with a multidisciplinary approach that uses complementary analytical techniques. Here, we focused our efforts on outlining the strong relevance of elemental composition in chemistry and mineralogical investigations to answer important archaeological questions in the case of Apulian red figure pottery. This ceramic class is the most important quantitative handcraft production group of figured pottery in Magna Grecia and the most widespread and commercialized production from the third quarter of the fifth century to the end of the next century. The results obtained indicate that, by exploring chemical elements in the ceramic mixture, it is possible to extract information about provenance, manufacturing processes, originality and restoration techniques.
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36

Boiko, R. S., V. D. Virich, F. A. Danevich, T. I. Dovbush, G. P. Kovtun, S. S. Nagornyi, S. Nisi, A. I. Samchuk, D. A. Solopikhin, and A. P. Shcherban’. "Ultrapurification of archaeological lead." Inorganic Materials 47, no. 6 (May 25, 2011): 645–48. http://dx.doi.org/10.1134/s0020168511060069.

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37

Kaye, Barry. "Conservation of waterlogged archaeological wood." Chemical Society Reviews 24, no. 1 (1995): 35. http://dx.doi.org/10.1039/cs9952400035.

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38

Munita, C. S., R. P. Paiva, M. A. Alves, P. M. S. de Oliveira, and E. F. Momose. "Provenance Study of Archaeological Ceramic." Journal of Trace and Microprobe Techniques 21, no. 4 (January 2, 2003): 697–706. http://dx.doi.org/10.1081/tma-120025819.

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39

Truică, Georgiana, Eugenia Teodor, Simona Litescu, and Gabriel Radu. "LC-MS and FT-IR characterization of amber artifacts." Open Chemistry 10, no. 6 (December 1, 2012): 1882–89. http://dx.doi.org/10.2478/s11532-012-0103-5.

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AbstractThis work focuses on using analytical methods, such as Fourier transform Infrared spectroscopy (FTIR) and high performance liquid chromatography (HPLC) with mass spectrometry (MS) detection to assess archaeological and geological amber. The main goal of this study is to apply the previously developed and optimized analytical methods in verifying criteria to ascribe and characterize the origin of materials found in archaeological sites. The proposed LC-MS method was successfully applied for the quantification of succinic acid content both in geological and archaeological samples of amber and offers excellent linearity between 0.1 and 5µg mL−1. The developed FTIR method provided some criteria which is able to differentiate between Baltic and Romanian amber (Romanite) that furthermore validates on archaeological amber artefacts.
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40

Warrick, Gary, Bonnie Glencross, and Louis Lesage. "The Importance of Minimally Invasive Remote Sensing Methods in Huron-Wendat Archaeology." Advances in Archaeological Practice 9, no. 3 (May 20, 2021): 238–49. http://dx.doi.org/10.1017/aap.2021.7.

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AbstractThe Huron-Wendat have had their ancestors’ villages and burial sites investigated archaeologically for over 170 years. Past and ongoing land disturbance and invasive archaeological excavation have erased dozens of Huron-Wendat village sites in Ontario, hindering Huron-Wendat duty to care for their ancestors. Consequently, over the last 20 years, in addition to large-scale repatriation of ancestral remains, the Huron-Wendat have requested that archaeologists make every effort to avoid any further excavation of ancestral sites. This poses a new challenge for archaeologists about how to learn about the Huron-Wendat past with minimal disturbance to ancestral sites. Honoring the cultural responsibilities of the Huron-Wendat, the authors have employed minimally invasive remote sensing methods of investigation on Ahatsistari, a forested early seventeenth-century Huron-Wendat village site in Simcoe County, Ontario. Remote sensing methods (e.g., magnetic susceptibility survey, high-resolution soil chemistry sampling, and metal detector survey) have revealed village limits and the possible location and orientation of longhouses, providing essential information in support of the Huron-Wendat imperative to find, assess, and preserve as many of their archaeological sites as possible. This is to protect the ancestors, learn from the ancestors, and preserve ancestral sites and related landscapes for future generations.
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41

Ghavidel, Amir, Jana Gelbrich, Aldi Kuqo, Viorica Vasilache, and Ion Sandu. "Investigation of Archaeological European White Elm (Ulmus laevis) for Identifying and Characterizing the Kind of Biological Degradation." Heritage 3, no. 4 (September 26, 2020): 1083–93. http://dx.doi.org/10.3390/heritage3040060.

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The current work aims at the study of the biological degradation of archaeological European white elm via microscopy and chemical analysis in order to identify the kind of biological degradation and characterize the state of preservation of this type of wood. Profound knowledge of the chemical constituents and biological degradation in fresh-cut and archaeological elm wood will simplify the process of restoration and conservation of the investigated artifacts. Therefore, fresh-cut and archaeological elm were compared in terms of extractive, chlorite holocellulose, α-cellulose, lignin, and ash contents. In the fresh-cut elm wood, the contents of Kürschner–Hoffer cellulose, chlorite holocellulose, α-cellulose, and hemicellulose were significantly higher than that of the archaeological elm, confirmed by the degradation of native wood hemicelluloses by erosion bacteria during soil contact. Naturally, the mass percentage of lignin increases as the amount of chlorite holocellulose in the wood decreases. These wet chemistry results were also confirmed by FTIR analysis, where bands mainly attributed to hemicellulose and cellulose decreased significantly and bands belonging to lignin display higher intensity for the archaeological specimens. Ash and cyclohexane–ethanol extract contents of archaeological elm wood were significantly higher due to the movement of mineral components arising out of the soil into the wood specimens. Based on the microscopic investigation and given the fact that wood decay fungi need oxygen to degrade wood and the investigated archaeological elm specimens were buried to a 10 m depth in the soil, we might conclude that the wood degradation was caused by erosion bacteria.
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42

Cook, Phil K., Elise Dufour, Marie-Angélique Languille, Cristian Mocuta, Solenn Réguer, and Loïc Bertrand. "Strontium speciation in archaeological otoliths." Journal of Analytical Atomic Spectrometry 31, no. 3 (2016): 700–711. http://dx.doi.org/10.1039/c5ja00426h.

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43

Colonese, André C., Thomas Farrell, Alexandre Lucquin, Daniel Firth, Sophy Charlton, Harry K. Robson, Michelle Alexander, and Oliver E. Craig. "Archaeological bone lipids as palaeodietary markers." Rapid Communications in Mass Spectrometry 29, no. 7 (April 15, 2015): 611–18. http://dx.doi.org/10.1002/rcm.7144.

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44

Ganesan, Sathiyanarayanan, Mathilde Monachon, Sarah M. James, and Edith Joseph. "Microbes for Archaeological Wood Conservation." CHIMIA 76, no. 9 (September 21, 2022): 772. http://dx.doi.org/10.2533/chimia.2022.772.

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This project focuses on innovative biological methods of extraction for the preservation of waterlogged wood suffering from salt precipitation and acidification. The principal investigator and her team proposed to exploit biomineralization capacities of some bacteria for anticipating the extraction of iron and sulfur compounds when wood is still wet. A comprehensive assessment of the extraction performances achieved on wood objects from lake and marine environments will allow a versatile extraction method to be proposed to end-users.
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45

Komarova, Ya M., N. L. Aluker, V. V. Bobrov, and N. V. Sorokina. "Thermoluminescent dating of archaeological pottery." Inorganic Materials 47, no. 5 (May 2011): 544–48. http://dx.doi.org/10.1134/s0020168511050128.

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46

TAGUCHI, ISAMU, and TSUTOMU SAITO. "NON-DESTRUCTIVE ANALYSIS OF ARCHAEOLOGICAL MATERIALS." Analytical Sciences 7, Supple (1991): 659–62. http://dx.doi.org/10.2116/analsci.7.supple_659.

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47

Harry, Karen G. "Cation-Ratio Dating of Varnished Artifacts: Testing the Assumptions." American Antiquity 60, no. 1 (January 1995): 118–30. http://dx.doi.org/10.2307/282079.

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Dorn (1983) has proposed that changes in rock varnish chemistry can be used to date varnished artifacts. Specifically, he suggests that the varnish cation ratio, (K + Ca)/Ti, decreases as the age of the varnished surface increases. Although the method is generating significant archaeological interest, many of its underlying assumptions remain undemonstrated. This paper examines one premise of the method, that the varnishing process is regular. Data obtained from varnish distributional studies challenge this assumption and, when compared with the chemical data obtained from the same archaeological site, suggest that the cation-ratio dating technique may not be able to provide accurate dates for most varnished artifacts.
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48

Niknami, Kamal Aldin. "Iran: archaeological heritage in crisis." Journal of Cultural Heritage 6, no. 4 (December 2005): 345–50. http://dx.doi.org/10.1016/j.culher.2005.02.005.

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49

Dudko, А. А., Yu A. Vasileva, and A. V. Veretennikov. "Results of Archaeological Exploration in the Development Zone of the Karachiyaksky Coal Deposit in Novokuznetsk District of Kemerovo Region – Kuzbass in 2021." Problems of Archaeology, Ethnography, Anthropology of Siberia and Neighboring Territories 27 (2021): 951–57. http://dx.doi.org/10.17746/2658-6193.2021.27.0951-0957.

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In June 2021, the Kuzbass team of the Department of Rescue Archaeological Work of the IAE SB RAS, together with employees of the Laboratory of Archeology of the Federal Research Center of Coal and Coal Chemistry of the SB RAS, carried out archaeological exploration as a part of the state historical and cultural expertise of the land plot intended for inclusion into development area of the Karachiyak coal deposit (The Korchakolsky and Korchakolsky Glubokyi sections) of the Kuznetskinveststroi Company in Novokuznetsk District of Kemerovo Region - Kuzbass. Presently, over thirty sites of archaeological heritage belonging to the Final Upper Paleolithic - Early Holocene are known in the Kondoma River basin. The land plot which was assigned for coal mining is located on the left bank of the KondomaRiver Valley around the village of Taylep; on the northern side it is bounded by the Taylep River and is closely adjacent to the Korchakol coal mine on the west. As a result of the works, 285 pits were made over a total area of546 sq. m, and five objects of archaeological heritage, preliminarily dated to the Final Upper Paleolithic - Early Holocene, were discovered. Thirty artifacts were found in archaeological pits, including cores, burins, scrapers, blade, spalls, flakes, and fragments. The raw materials of lithic industries at the Taylep 4-8 sites were pebbles, which widely appear in channel alluvium of the Kondoma River. According to its technical and typological features, the complex of lithic industry from the Taylep 4-8 sites forms a single cluster with the evidence from the Taylep 1 and 2 sites (lower cultural horizon) which were studied during the rescue archaeological excavations in 2020.
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GÜNDÜZ, Serkan. "UAV Image-Based Plan Drawing Method in Submerged Terrestrial Archaeological Settlements: The case of Kibotos." International Journal of Environment and Geoinformatics 10, no. 1 (March 15, 2023): 139–45. http://dx.doi.org/10.30897/ijegeo.1231224.

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Abstract:
Documentation with drawing and photography is one of the most important stages in archaeological excavations and surveys. It takes a long time to draw walls by stone by stone during the excavations. Carrying out these studies on land that does not belong to human habitats, such as underwater, is an activity that requires extra effort, time, and experience. This article will examine the possibility of drawing the plans of the structures unearthed or detected in the archaeological underwater excavations and surface surveys in shallow waters with the help of aerial photographs in a shorter time and with less effort. The research results show that the photograph-based archaeological plan drawing is an excellent and suitable method for shallow water archaeological excavation and surveys. It reveals that it can save time and labour in surveys and rescue excavations where time is limited.
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