FN Archimer Export Format
PT J
TI Geochemistry of an endorheic thalassohaline ecosystem: the Dziani Dzaha crater lake (Mayotte Archipelago, Indian Ocean)
BT 
AF Sarazin, Gérard
   Jezequel, Didier
   LEBOULANGER, Christophe
   FOUILLAND, Eric
   LE FLOC'H, Emilie
   Bouvy, Marc
   Gerard, Emmanuelle
   Agogué, Hélène
   Bernard, Cédric
   Hugoni, Mylène
   Grossi, Vincent
   Trousselier, Marc
   Ader, Magali
AS 1:1;2:1;3:7;4:2;5:2;6:2;7:1;8:3;9:4;10:5;11:6;12:2;13:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;
C1 Université de Paris, Institut de Physique du Globe de Paris, CNRS, F-75005 Paris, France
   UMR 9190, MARBEC, CNRS-Université deMontpellier -IRD - IFREMER, 34095 Montpellier Cedex 5, France
   UMR 7266 LIENSs, La Rochelle Université–CNRS, 17000 La Rochelle, France
   Museum National d’Histoire Naturelle, CP 39, 75231 Paris cedex 05, France
   Univ Lyon, Université Claude Bernard Lyon 1, CNRS, INRAE, VetAgro Sup, UMR EcologieMicrobienne, F-69622 Villeurbanne, France
   Univ Lyon, Univ Lyon 1, CNRS, ENSL, Laboratoire de Géologie de Lyon : Terre, Planètes, Environnement, F-69622 Villeurbanne, France
   UMR 9190, MARBEC, CNRS-Université deMontpellier -IRD - IFREMER, 34095 Montpellier Cedex 5, France
C2 IPGP, FRANCE
   CNRS, FRANCE
   UNIV LA ROCHELLE, FRANCE
   MNHN, FRANCE
   UNIV LYON, FRANCE
   UNIV LYON, FRANCE
   IRD, FRANCE
UM MARBEC
IN WOS Cotutelle UMR
   copubli-france
   copubli-univ-france
IF 2.241
TC 6
UR https://archimer.ifremer.fr/doc/00667/77948/80128.pdf
   https://archimer.ifremer.fr/doc/00667/77948/81365.pdf
LA English
DT Article
DE ;Thalassohaline lake;Endorheic ecosystem;Cyanobacteria;Methane emission;Biogeochemistry;Mayotte
AB Dziani Dzaha is a maar the age of which is close to 4000 years. While its water is thought to have originated from seawater it is now considered as an extreme environment due to its hypersaline and alkaline characteristics. Those extreme features have led to the simplification of the trophic network. Cyanobacteria account for up to 95% of the photosynthetic biomass. The main biogeochemical processes, i.e. photosynthesis, bacterial sulfate reduction and methanogenesis could explain the current water composition. As far as we know, this ecosystem could be unique on Earth, extending the nature and chemical limits of aquatic inland ecosystems 
PY 2020
SO Comptes Rendus Geoscience
SN 1631-0713
PU Elsevier
VL 352
IS 8
UT 000613921700002
BP 559
EP 577
DI 10.5802/crgeos.43
ID 77948
ER

EF