Keywords

These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Adaptation in Haloalkaliphiles and Natronophilic Bacteria

  • Horia L. Banciu &
  • Dimitry Y. Sorokin 

  1. Department of Molecular Biology and Biotechnology, Babes-Bolyai University of Cluj-Napoca, 400084, Cluj-Napoca, Romania

    Horia L. Banciu

  2. Winogradsky Institute of Microbiology, Russian Academy of Sciences, 119991, Moscow, Russia

    Dimitry Y. Sorokin

  3. Department of Biotechnology, Delft University of Technology, Delft, The Netherlands

    Dimitry Y. Sorokin

The title for this chapter should read “Adaptation Mechanisms in Haloalkaliphilic and Natronophilic Bacteria” instead of “Adaptation in Haloalkaliphiles and Natronophilic Bacteria”.

Deep Hypersaline Anoxic Basins as Model Systems for Environmental Selection of Microbial Plankton

  • Alexandra Stock,
  • Sabine Filker,
  • Michail Yakimov &
  • Thorsten Stoeck 

  1. Department of Ecology, University of Kaiserslautern, 67663, Kaiserslautern, Germany

    Alexandra Stock, Sabine Filker & Thorsten Stoeck

  2. Institute for Coastal Marine Environment (IAMC), CNR, 98122, Messina, Italy

    Michail Yakimov

No permission has been received for the use of the Bathymetric maps of two Mediterranean DHABs (Figure 1) and the image of the seafloor, as taken during a mapping dive of the ROV Jason (Figure 3) and therefore Chapter 22 Fig. 1 and Fig. 3 have been greyed out.

Figure 1. Bathymetric maps of two Mediterranean DHABs. Brines occur in a depth of around 3,550 and 3,500 m for (a) Discovery Basin and (b) Urania Basin, respectively.

Figure 3. Image of the sea?oor (left) showing the transition (interphase) from seawater into the brine layer (right, dark area) (The picture was taken during a mapping dive of the ROV Jason (WHOI)).