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Yanarta? fluids are slightly impacted by reaction with bedrock, sitting just to the right of the local meteoric water line (MWL) and averaged local precipitation (based on data from Antalya, Turkey��Dirican et al., 2005) (Figure ?(Figure5B).5B). The presence of relict flow paths and preserved microterracettes suggest that the fluid seep is ephemeral, but has been present for a long period of time. The possible intermittent nature of the flow is consistent with observations in previous reports that stated that there was a lack of springs in the area (Etiope et al., 2011). Figure 5 Fluid analysis of the Yanarta? seep, shown with other globally significant serpentinizing fluids for reference. Non-Yanarta? data are from the following reports: Barnes et al. (1978), Neal and Shand (2002), www.selleckchem.com/products/AZD6244.html Cipolli et al. (2004), Boschetti ... YT-0m fluids are extremely high pH and [Ca+2], with negligible DIC (Figures 5A,C, ?,6,6, Table ?Table1);1); this water is a classic Ca+2-OH? type solution MDV3100 cell line that is generally associated with active serpentinization (Barnes et al., 1967; Neal and Shand, 2002). Elevated Fe, Cr, Mn, Co, and Ni at YT-S8.8m co-occur with elevated Mg, suggesting that water at this site is dominated by a Mg+2-HCO?3 type water produced after the source fluid has passed over and weathered serpentinite/serpentine soils, accumulating products of chemical weathering (Table ?(Table1,1, Figure ?Figure66). Figure 6 (A) Range of [Ca+2] and pH values found in serpentinizing seeps worldwide. (B) Piper plot showing relationships in fluid composition among the same seeps. Non-Yanarta? data are from the following reports: Barnes et al. (1978), Neal and Shand ( ... Figures ?Figures5,5, ?,66 allow comparison of Yanarta? fluids with other serpentinizing seeps worldwide. Fluid emanating from the source at Yanarta?, (YT-0m), most closely resembles that found in seeps at the Tablelands Winterhouse Creek location sampling the ��ultrabasic endmember�� of the seep system (Szponar et al., 2013). Figure ?Figure66 shows Telomerase the wide range of pH and [Ca+2] featured by serpentinizing seeps; site YT-S8.8m falls within this range at the lower end of both variables, most similar to several sites in Cyprus (Neal and Shand, 2002). Site YT-0m falls within the cluster of Ca+2-OH? type waters in Figure ?Figure66 and records some of the highest [Ca+2], and lowest [Mg+2] values in the terrestrial serpentinizing seep literature (Figure ?(Figure6).6). Future cataloging of the microbial communities from the five Yanarta? sample locations will allow further comparison with the Tablelands and Cyprus ecosystems. Fluid emanating from the source at pH 11.9 decreases in pH as it flows down the outflow channels.