Academia.eduAcademia.edu

Figure 3 – uploaded by Alex Pryor

See full PDFdownloadDownload figure
hand to expose the section instead. Samples were then mounted onto glass slides using Araldite 2020 resin and ground manually using 35 um, 15.3 um, 10.3 tm and 5 um grits to 80-100 um thickness. Sections were finished by polishing with 0.3 um alumina oxide powder using a Logitech automatic polishing machine.

Figure 3 hand to expose the section instead. Samples were then mounted onto glass slides using Araldite 2020 resin and ground manually using 35 um, 15.3 um, 10.3 tm and 5 um grits to 80-100 um thickness. Sections were finished by polishing with 0.3 um alumina oxide powder using a Logitech automatic polishing machine.

Related Figures (11)

Fig. 1. Topographic map of southern Poland showing the location of Krakow Spadzista with respect to key landscape features including mountains, hills and river valleys. The Krak6éw Spadzista site complex lies on a promontory of the Saint Bronistawa hill at the eastern end of Sowiniec horst at a height of 50 m above the floodplain of the Rudawa River in southern Poland (Fig. 1). Excavations between 1967 and 2017 have revealed substantial quan- tities of lithics and faunal material deposited across an area of almost 2 ha associated with a weakly developed and periglacially deformed soil (Lanczont et al., 2015; Wilczynski et al., 2012b). The southern and north-eastern sides of the horst where the site is located are high and descend steeply, or sometimes vertically, into the Vistula and Rudawa river valleys below (Lanczont et al., 2015). It is suggested that the large accumulations of woolly mammoth bones found at the site formed as Upper Palaeolithic hunters took advantage of this natural morphology
Fig. 1. Topographic map of southern Poland showing the location of Krakow Spadzista with respect to key landscape features including mountains, hills and river valleys. The Krak6éw Spadzista site complex lies on a promontory of the Saint Bronistawa hill at the eastern end of Sowiniec horst at a height of 50 m above the floodplain of the Rudawa River in southern Poland (Fig. 1). Excavations between 1967 and 2017 have revealed substantial quan- tities of lithics and faunal material deposited across an area of almost 2 ha associated with a weakly developed and periglacially deformed soil (Lanczont et al., 2015; Wilczynski et al., 2012b). The southern and north-eastern sides of the horst where the site is located are high and descend steeply, or sometimes vertically, into the Vistula and Rudawa river valleys below (Lanczont et al., 2015). It is suggested that the large accumulations of woolly mammoth bones found at the site formed as Upper Palaeolithic hunters took advantage of this natural morphology
Fig. 2. Geological map of Poland and Czechia at 1:1,000,000 (EGDI, accessed 1st March 2020), annotated with datapoints numbered 1-32 used to infer spatial variability in bioavailable strontium isotope ratios or otherwise mentioned in the text. Further information on the bioavailable strontium isotope data including references is given in Table 3. The Fennoscandian icesheet is shown according to Ehlers et al. (2011), and loess cover according to Haase et al. (2007). A topographic map of the area marked by a rectangle is shown in Fig. 1.
Fig. 2. Geological map of Poland and Czechia at 1:1,000,000 (EGDI, accessed 1st March 2020), annotated with datapoints numbered 1-32 used to infer spatial variability in bioavailable strontium isotope ratios or otherwise mentioned in the text. Further information on the bioavailable strontium isotope data including references is given in Table 3. The Fennoscandian icesheet is shown according to Ehlers et al. (2011), and loess cover according to Haase et al. (2007). A topographic map of the area marked by a rectangle is shown in Fig. 1.
Dental cementum results.
Dental cementum results.
Strontium isotope results. Table 2
Strontium isotope results. Table 2
Fig. 4. Strontium isotope profiles and summary boxplots of the five investigated Arctic fox teeth. Profiles are based on a moving 10-point mean average of th individual laser ablation measurements. Dark grey shading around the lines indicates measurement error, calculated as the standard mean error. The strontiur isotope ratio of the loess at Krakéw Spadzista is indicated by the light grey shaded bar, based on measurements of dentine in the five investigated teeth. Arrow indicate periods of potential mobility in individuals KSF101 and KSF103.
Fig. 4. Strontium isotope profiles and summary boxplots of the five investigated Arctic fox teeth. Profiles are based on a moving 10-point mean average of th individual laser ablation measurements. Dark grey shading around the lines indicates measurement error, calculated as the standard mean error. The strontiur isotope ratio of the loess at Krakéw Spadzista is indicated by the light grey shaded bar, based on measurements of dentine in the five investigated teeth. Arrow indicate periods of potential mobility in individuals KSF101 and KSF103.
Table 3
Table 3
Fig. 5. Summary of strontium isotope data from the five investigated foxes alongside bioavailable strontium data listed by region (Table 3; Fig. 2).
Fig. 5. Summary of strontium isotope data from the five investigated foxes alongside bioavailable strontium data listed by region (Table 3; Fig. 2).
References
References
580 California St., Suite 400
San Francisco, CA, 94104
© 2025 Academia. All rights reserved