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Traces Of Possible Ancient Life From Mars To Earth: An Assessment Of The
                            Microbial Ecology Of Salda Lake And Its Protection

               The mineralogical and morphological properties of the carbonate units in
            the Jezero crater indicate that the formation patterns of these structures may
            be similar to Salda Lake (Garczynski et al., 2020). By taking into account the
            scientific data on the formation of these carbonate units, NASA which has been
            researching ecosystems on Earth similar to Mars for the last decade, stated
            that Salda Lake is a unique lake on Earth that has geological, geochemical,
            and mineralogical similarities with the ancient lake environment in Jezero
            Crater in Mars, and accepted Salda Lake as and analogue for Mars - Jezero
            Crater (Garczynski et al., 2019).
               In  the  photo  published  on  the  official  website  of  the  American  National
            Aeronautics and Space Administration (NASA), the similarity between Jezero
            Crater and Salda Lake is shown (Figure 4). This similarity makes Salda Lake a
            key area for studying the microbial diversity of analogue environments on Earth
            during the search for possible biological traces on Mars (Garczynski et al., 2019).

             a)                               b)

















                        Figure 4. (a) Salda Lake (2020) (b) Jezero Crater (NASA, 2017)
               Salda Lake is an alkaline lake located in the northwest of Burdur, in Yeşilova
            district of Burdur Province. Salda Lake is located in the Region of Lakes which
            also includes a group of lakes such as Acıgöl, Burdur Lake, Yarışlı Lake and
            Akgöl. Salda Lake is one of the deepest freshwater lakes with a surface area of
            45 km2.  The deepest section is about 200 meters. The lake has no significant
            and permanent surface flow and is mainly fed by meteoric waters (Braithwaite
            & Zedef, 1995; Balci et al., 2018). Microbialites with hydromagnesite (aqueous
            magnesium  carbonate)  content  that  develop  in  a  lake-specific  ecosystem
            (Figure 5) are the most characteristic feature of Salda Lake (Ince et al., 2021).
            These layered, sedimentary structures in Salda Lake have the morphology
            of cauliflower (Figure 6) and contain fossil and living microbial communities
            (Balci et al., 2018) .





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