Figure 2 | Scientific Reports

Figure 2

From: Modern dolomite formation caused by seasonal cycling of oxygenic phototrophs and anoxygenic phototrophs in a hypersaline sabkha

Figure 2

[Top]: Vertical microsensor profiles oxygen [μmol L−1] from KAAS-1 and KAAS-2 from March and October 2016, as well as February 2018. [Middle]: Vertical microsensor profiles of pH from KAAS-1 and KAAS-2 from March and October 2016, as well as February 2018. [Bottom]: Vertical microsensor profiles of redox [mV] from KAAS-1 and KAAS-2 from March and October 2016, as well as February 2018.

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