Almus agates which are forms of nodules like egg-shaped are located in the Eocene aged Almus volcanics in Tokat (Turkey). These nodules are surprise eggs in spherical or oval form ranging from a few cm to 25–30 cm. It is thought that the most effective reason for the formation of the magnificent texture and color combinations of the agates in the region is the iron element. In thin section studies, agate formations are composed of length-slow zebraic chalcedony and quart zine. In addition, curved fossil like structures composed of iron oxide minerals offer visual richness.
The host rock in which the Almus agates are located is trachyte, which consists of sanidine, plagioclase microlites and small opaque minerals, in which microlithic porphyritic and flow (trachytic) texture are observed. As a result of the multipoint eds (field emission scanning electron microscope), it was determined that the quartz is composed of Si, O and Fe. The content of the iron element, which is thought to cause color, was observed in the range of ca 1–1.5 wt.%. According to XRF analysis results, in Almus agates, there is depletion of Fe2O3 content in fine crystalline regions (ca 1 wt.%) compared to coarse crystalline zones (ca 1.5 wt.%).
In order to determine the usability of Almus agates as gemstone, various cabochon shapes were made in Ümit Ulus Gemstone Processing workshop. It has been observed that these agates can be used for both collection and gemstone purposes due to their unique patterns and color compensation.

Ch-chalcedony is a green colored member of the quartz group of gem stones. The appearance of Ch-chalcedony is very similar to that of chrysoprase. Differently, Ch-chalsedonies have a chromium element instead of a nickel element as a trace element. Green quartz used in jewelery as a seal stone, in necklaces and rings and has been one of the most valuable quartz varieties throughout history, with its beautiful green color,more rare than other quartz varieties. The Ch-chalcedonies in the North Anatolian region is yellowish-white, brownish gray, light green to dark green in color ranging from several centimeters to one meter thick in veins and lenses in the Lower-Middle Eocene dolomitic limestones. Ch-chalcedonies are composed of fine-grained and occasionally fibrous needle-like quartz; in some examples, quartz is present together with cristobalite, tridimite and cuspidine minerals. According to geochemical investigations in Ch-chalcedonies, the main oxides that were determined are as follows: SiO2 was observed in the range of 95.86–97.81%, Fe2O3 was observed in the range of 0.61–0.91% and Cr2O3 was observed in the range of 0.125–0.168%. A trace element analysis of Ch-chalcedonies, shows their significant enrichments in: Ni, Mo, Cu, Mn, V, Cr and W, especially in the Cr (up to 705 ppm). The green color of the studied Cr-chalcedonies originates from the element chromium. Taking the possible reserves into account, the hardness, color, massive structures, mineralogical, petrographical and gemological features of Ch-chalcedonies in the region are evaluated together. It is determined that they are suitable for the production of jewelry and ornaments.

The aim of this study is to determine the protective efficacy of anise in cerebral ischemia and reperfusion injury in rats. In this study, 28 Wistar Albino rats, weighing 250-300 grams (g), were used. Four groups were formed with 7 rats in each group. Group 1 (n=7): Control group, Group 2 (n=7): Anise group, 5 mL/kg/day of anise aqueous extract prepared according to Gamberini’s protocol was given orally by gavage for 30 days. Group 3 (n=7): Cerebral ischemia reperfusion (CIR) group, at the beginning of the experiment, 30 minutes of cerebral ischemia and 1 hour of reperfusion were induced and the animals were sacrificed by exanguination. Group 4 (n=7): Anise+ CIR group, After administering 30 days of anise’s aqueous extract, CIR was induced and the study was terminated. TOS values of the Anise+ CIR group was significantly lower than that of the CIR group (p<0.05). Il-6 and TNF-α values of the CIR group were significantly higher than the Anise+ CIR group (p<0,05). Our study revealed that anise ameliorates oxidative damage and inflammation due to cerebral ischemia/reperfusion, by reducing the levels of inflammatory cytokines (TNF-α, Il-6).