Microscopic remains of plants, hairs, blood, bone, and sinew have been detected on Stone Age impl... more Microscopic remains of plants, hairs, blood, bone, and sinew have been detected on Stone Age implements as evidence of the ways the tools were used. Together with use-wear analysis, microresidues enable us to obtain additional information of artefact biographies. However, the preservation of residues is not a straightforward issue. Although bones, plant matter, and wood have a tendency to decompose rapidly in acidic podzol soils, the acidity favours the preservation of keratinous tissues such as hairs and feathers. Because the analysis of microresidues has not been applied on Finnish quartz artefacts, this paper presents a preliminary testing of the method in a Late Stone Age settlement site in Kraakanmäki 3, western Finland. As a result, we found microscopic remains of hairs, feathers, and plants, which enable us to speak for the careful handling of quartz and stone tools at the excavations for further analyses.
Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the p... more Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the potential is promising. Most formal Finnish stone tools beside quartz are made from ground metamorphic stone, which often has a specific source of collection. Geochemistry can reveal compositional and trace element links between the sources and tools found in various Stone Age settlement sites. Discoveries about technological properties of the stone types can be a helpful comparison, since many geochemical methods can produce data that has inconsistencies. In this thesis both geochemical and technological aspects of two lithic material sources are examined. Samples were collected from two lithic material sources: Rakkaviita and Rieskapaikka in Tervola, Southern Lapland. The 62 collected samples were measured with a Bruker S1 Titan portable x-ray fluorescence device as a preliminary method. Three samples from Rakkaviita and two samples from Rieskapaikka were chosen for the primary method, which was the PANalytical Axios mAX 4 kW, Wavelength Dispersive X-Ray fluorescence spectrometer in the Department of Geosciences in the University of Helsinki. The data from these measurements is evaluated and plotted to reveal geochemical properties of the stone. In this study, the properties of these stone materials are documented for the first time, so it can also be considered as a mapping study. The measurements revealed differentiation between methods, especially on the SiO2 percentages. The WD-XRF measurements are done without sample specific calibration, which obscures the quantitative proportions of some elements. The content of the stone revealed various components in different proportions. The result of major components was a coarsely qualitative definition of stone from both sources, which can be used in further material studies of stone tools. The trace element comparison between yttrium (Y) and strontium (Sr) revealed clear similarity between sources, excluding one sample that had significantly different tool production properties than others. According to this study, methods that handle trace elements well like ICP-MS are best suited for provenance studies on this type of stone. With trace elements it’s likely that these types of stones can be successfully sourced by geological region. The technological properties of the material are studied to find out the potential of the raw material as a stone to make and use tools with. Differences in the technological properties of the two sources is reflected in the composition and formation differences. Rieskapaikka included more mafic, porphyritic and fine-grained samples while Rakkaviita stones were more foliated and deteriorated.
Geochemical Comparison of two Tervola Volcanite Deposits as Plausible Stone Tool Material Sources in Kemijoki, 2020
Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the p... more Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the potential is promising. Most formal Finnish stone tools beside quartz are made from ground metamorphic stone, which often has a specific source of collection. Geochemistry can reveal compositional and trace element links between the sources and tools found in various Stone Age settlement sites. Discoveries about technological properties of the stone types can be a helpful comparison, since many geochemical methods can produce data that has inconsistencies. In this thesis both geochemical and technological aspects of two lithic material sources are examined. Samples were collected from two lithic material sources: Rakkaviita and Rieskapaikka in Tervola, Southern Lapland. The 62 collected samples were measured with a Bruker S1 Titan portable x-ray fluorescence device as a preliminary method. Three samples from Rakkaviita and two samples from Rieskapaikka were chosen for the primary method, which was the PANalytical Axios mAX 4 kW, Wavelength Dispersive X-Ray fluorescence spectrometer in the Department of Geosciences in the University of Helsinki. The data from these measurements is evaluated and plotted to reveal geochemical properties of the stone. In this study, the properties of these stone materials are documented for the first time, so it can also be considered as a mapping study. The measurements revealed differentiation between methods, especially on the SiO2 percentages. The WD-XRF measurements are done without sample specific calibration, which obscures the quantitative proportions of some elements. The content of the stone revealed various components in different proportions. The result of major components was a coarsely qualitative definition of stone from both sources, which can be used in further material studies of stone tools. The trace element comparison between yttrium (Y) and strontium (Sr) revealed clear similarity between sources, excluding one sample that had significantly different tool production properties than others. According to this study, methods that handle trace elements well like ICP-MS are best suited for provenance studies on this type of stone. With trace elements it’s likely that these types of stones can be successfully sourced by geological region. The technological properties of the material are studied to find out the potential of the raw material as a stone to make and use tools with. Differences in the technological properties of the two sources is reflected in the composition and formation differences. Rieskapaikka included more mafic, porphyritic and fine-grained samples while Rakkaviita stones were more foliated and deteriorated.
Microscopic remains of plants, hairs, blood, bone, and sinew have been detected on Stone Age impl... more Microscopic remains of plants, hairs, blood, bone, and sinew have been detected on Stone Age implements as evidence of the ways the tools were used. Together with use-wear analysis, microresidues enable us to obtain additional information of artefact biographies. However, the preservation of residues is not a straightforward issue. Although bones, plant matter, and wood have a tendency to decompose rapidly in acidic podzol soils, the acidity favours the preservation of keratinous tissues such as hairs and feathers. Because the analysis of microresidues has not been applied on Finnish quartz artefacts, this paper presents a preliminary testing of the method in a Late Stone Age settlement site in Kraakanmäki 3, western Finland. As a result, we found microscopic remains of hairs, feathers, and plants, which enable us to speak for the careful handling of quartz and stone tools at the excavations for further analyses.
Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the p... more Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the potential is promising. Most formal Finnish stone tools beside quartz are made from ground metamorphic stone, which often has a specific source of collection. Geochemistry can reveal compositional and trace element links between the sources and tools found in various Stone Age settlement sites. Discoveries about technological properties of the stone types can be a helpful comparison, since many geochemical methods can produce data that has inconsistencies. In this thesis both geochemical and technological aspects of two lithic material sources are examined. Samples were collected from two lithic material sources: Rakkaviita and Rieskapaikka in Tervola, Southern Lapland. The 62 collected samples were measured with a Bruker S1 Titan portable x-ray fluorescence device as a preliminary method. Three samples from Rakkaviita and two samples from Rieskapaikka were chosen for the primary method, which was the PANalytical Axios mAX 4 kW, Wavelength Dispersive X-Ray fluorescence spectrometer in the Department of Geosciences in the University of Helsinki. The data from these measurements is evaluated and plotted to reveal geochemical properties of the stone. In this study, the properties of these stone materials are documented for the first time, so it can also be considered as a mapping study. The measurements revealed differentiation between methods, especially on the SiO2 percentages. The WD-XRF measurements are done without sample specific calibration, which obscures the quantitative proportions of some elements. The content of the stone revealed various components in different proportions. The result of major components was a coarsely qualitative definition of stone from both sources, which can be used in further material studies of stone tools. The trace element comparison between yttrium (Y) and strontium (Sr) revealed clear similarity between sources, excluding one sample that had significantly different tool production properties than others. According to this study, methods that handle trace elements well like ICP-MS are best suited for provenance studies on this type of stone. With trace elements it’s likely that these types of stones can be successfully sourced by geological region. The technological properties of the material are studied to find out the potential of the raw material as a stone to make and use tools with. Differences in the technological properties of the two sources is reflected in the composition and formation differences. Rieskapaikka included more mafic, porphyritic and fine-grained samples while Rakkaviita stones were more foliated and deteriorated.
Geochemical Comparison of two Tervola Volcanite Deposits as Plausible Stone Tool Material Sources in Kemijoki, 2020
Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the p... more Geochemistry of stone tools and sources remains largely unknown in Finnish archaeology, but the potential is promising. Most formal Finnish stone tools beside quartz are made from ground metamorphic stone, which often has a specific source of collection. Geochemistry can reveal compositional and trace element links between the sources and tools found in various Stone Age settlement sites. Discoveries about technological properties of the stone types can be a helpful comparison, since many geochemical methods can produce data that has inconsistencies. In this thesis both geochemical and technological aspects of two lithic material sources are examined. Samples were collected from two lithic material sources: Rakkaviita and Rieskapaikka in Tervola, Southern Lapland. The 62 collected samples were measured with a Bruker S1 Titan portable x-ray fluorescence device as a preliminary method. Three samples from Rakkaviita and two samples from Rieskapaikka were chosen for the primary method, which was the PANalytical Axios mAX 4 kW, Wavelength Dispersive X-Ray fluorescence spectrometer in the Department of Geosciences in the University of Helsinki. The data from these measurements is evaluated and plotted to reveal geochemical properties of the stone. In this study, the properties of these stone materials are documented for the first time, so it can also be considered as a mapping study. The measurements revealed differentiation between methods, especially on the SiO2 percentages. The WD-XRF measurements are done without sample specific calibration, which obscures the quantitative proportions of some elements. The content of the stone revealed various components in different proportions. The result of major components was a coarsely qualitative definition of stone from both sources, which can be used in further material studies of stone tools. The trace element comparison between yttrium (Y) and strontium (Sr) revealed clear similarity between sources, excluding one sample that had significantly different tool production properties than others. According to this study, methods that handle trace elements well like ICP-MS are best suited for provenance studies on this type of stone. With trace elements it’s likely that these types of stones can be successfully sourced by geological region. The technological properties of the material are studied to find out the potential of the raw material as a stone to make and use tools with. Differences in the technological properties of the two sources is reflected in the composition and formation differences. Rieskapaikka included more mafic, porphyritic and fine-grained samples while Rakkaviita stones were more foliated and deteriorated.
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promising. Most formal Finnish stone tools beside quartz are made from ground metamorphic stone, which often
has a specific source of collection. Geochemistry can reveal compositional and trace element links between the
sources and tools found in various Stone Age settlement sites. Discoveries about technological properties of the
stone types can be a helpful comparison, since many geochemical methods can produce data that has
inconsistencies.
In this thesis both geochemical and technological aspects of two lithic material sources are examined. Samples
were collected from two lithic material sources: Rakkaviita and Rieskapaikka in Tervola, Southern Lapland. The
62 collected samples were measured with a Bruker S1 Titan portable x-ray fluorescence device as a preliminary
method. Three samples from Rakkaviita and two samples from Rieskapaikka were chosen for the primary
method, which was the PANalytical Axios mAX 4 kW, Wavelength Dispersive X-Ray fluorescence spectrometer
in the Department of Geosciences in the University of Helsinki. The data from these measurements is evaluated
and plotted to reveal geochemical properties of the stone. In this study, the properties of these stone materials
are documented for the first time, so it can also be considered as a mapping study.
The measurements revealed differentiation between methods, especially on the SiO2 percentages. The WD-XRF
measurements are done without sample specific calibration, which obscures the quantitative proportions of some
elements. The content of the stone revealed various components in different proportions. The result of major
components was a coarsely qualitative definition of stone from both sources, which can be used in further
material studies of stone tools. The trace element comparison between yttrium (Y) and strontium (Sr) revealed
clear similarity between sources, excluding one sample that had significantly different tool production properties
than others. According to this study, methods that handle trace elements well like ICP-MS are best suited for
provenance studies on this type of stone. With trace elements it’s likely that these types of stones can be
successfully sourced by geological region.
The technological properties of the material are studied to find out the potential of the raw material as a stone to
make and use tools with. Differences in the technological properties of the two sources is reflected in the
composition and formation differences. Rieskapaikka included more mafic, porphyritic and fine-grained samples
while Rakkaviita stones were more foliated and deteriorated.
promising. Most formal Finnish stone tools beside quartz are made from ground metamorphic stone, which often
has a specific source of collection. Geochemistry can reveal compositional and trace element links between the
sources and tools found in various Stone Age settlement sites. Discoveries about technological properties of the
stone types can be a helpful comparison, since many geochemical methods can produce data that has
inconsistencies.
In this thesis both geochemical and technological aspects of two lithic material sources are examined. Samples
were collected from two lithic material sources: Rakkaviita and Rieskapaikka in Tervola, Southern Lapland. The
62 collected samples were measured with a Bruker S1 Titan portable x-ray fluorescence device as a preliminary
method. Three samples from Rakkaviita and two samples from Rieskapaikka were chosen for the primary
method, which was the PANalytical Axios mAX 4 kW, Wavelength Dispersive X-Ray fluorescence spectrometer
in the Department of Geosciences in the University of Helsinki. The data from these measurements is evaluated
and plotted to reveal geochemical properties of the stone. In this study, the properties of these stone materials
are documented for the first time, so it can also be considered as a mapping study.
The measurements revealed differentiation between methods, especially on the SiO2 percentages. The WD-XRF
measurements are done without sample specific calibration, which obscures the quantitative proportions of some
elements. The content of the stone revealed various components in different proportions. The result of major
components was a coarsely qualitative definition of stone from both sources, which can be used in further
material studies of stone tools. The trace element comparison between yttrium (Y) and strontium (Sr) revealed
clear similarity between sources, excluding one sample that had significantly different tool production properties
than others. According to this study, methods that handle trace elements well like ICP-MS are best suited for
provenance studies on this type of stone. With trace elements it’s likely that these types of stones can be
successfully sourced by geological region.
The technological properties of the material are studied to find out the potential of the raw material as a stone to
make and use tools with. Differences in the technological properties of the two sources is reflected in the
composition and formation differences. Rieskapaikka included more mafic, porphyritic and fine-grained samples
while Rakkaviita stones were more foliated and deteriorated.