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. 2013 Jun;79(11):3425–3437. doi: 10.1128/AEM.00254-13

Fig 1.

Fig 1

Temperature and salinity profiles of Atlantis II (a) and Discovery (b) sampling sites. Values were obtained with a high-range CTD device. For Atlantis II, four layers of stable temperature and salinity were clearly observed and labeled, while for Discovery, a single homogeneous convective layer was observed. An upper convective layer seems to be forming above the lower convective layer of Discovery Deep. Sampling depths are indicated with the arrows on the temperature lines.