Sub-oxycline methane oxidation can fully uptake CH4 produced in sediments: case study of a lake in Siberia

It is commonly assumed that methane (CH4) released by lakes into the atmosphere is mainly produced in anoxic sediment and transported by diffusion or ebullition through the water column to the surface of the lake. In contrast to that prevailing idea, it has been gradually established that the epilim...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Thalasso, Frédéric, Sepulveda-Jauregui, Armando, Gandois, Laure, Martinez-Cruz, Karla, Gerardo-Nieto, Oscar, Astorga-Espana, Maria S, Teisserenc, Roman, Lavergne, Céline, Tananaev, Nikita, Barret, Maialen, Cabrol, Léa
Other Authors: Aix-Marseille Université - AMU (FRANCE), Centre National de la Recherche Scientifique - CNRS (FRANCE), Center for Climate and Resilience Research - CR2 (CHILE), Institut National Polytechnique de Toulouse - Toulouse INP (FRANCE), Institut de Recherche pour le Développement - IRD (FRANCE), Université Toulouse III - Paul Sabatier - UT3 (FRANCE), Université du Sud Toulon-Var - USTV (FRANCE), Centro de Investigación y de Estudios Avanzados del Instituto Politécnico Nacional - CINVESTAV-IPN (MEXICO), Melnikov Permafrost Institute (RUSSIA), Universidad de Valparaiso - UV (CHILE), Laboratoire Ecologie fonctionnelle et Environnement - EcoLab (Toulouse, France), Institut Méditerranéen d'Océanologie (MIO)
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2020
Subjects:
Environnement et Société
Arctic
Methanotroph
Thermokarst
Boreal ecology
Carbon cycle
Freshwater ecology
Limnology
Siberia
Online Access:https://oatao.univ-toulouse.fr/28944/
https://oatao.univ-toulouse.fr/28944/1/Thalasso_28944.pdf
https://doi.org/10.1038/s41598-020-60394-8
Description
Summary:It is commonly assumed that methane (CH4) released by lakes into the atmosphere is mainly produced in anoxic sediment and transported by diffusion or ebullition through the water column to the surface of the lake. In contrast to that prevailing idea, it has been gradually established that the epilimnetic CH4 does not originate exclusively from sediments but is also locally produced or laterally transported from the littoral zone. Therefore, CH4 cycling in the epilimnion and the hypolimnion might not be as closely linked as previously thought. We utilized a high-resolution method used to determine dissolved CH4 concentration to analyze a Siberian lake in which epilimnetic and hypolimnetic CH4 cycles were fully segregated by a section of the water column where CH4 was not detected. This layer, with no detected CH4, was well below the oxycline and the photic zone and thus assumed to be anaerobic. However, on the basis of a diffusion-reaction model, molecular biology, and stable isotope analyses, we determined that this layer takes up all the CH4 produced in the sediments and the deepest section of the hypolimnion. We concluded that there was no CH4 exchange between the hypolimnion (dominated by methanotrophy and methanogenesis) and the epilimnion (dominated by methane lateral transport and/or oxic production), resulting in a vertically segregated lake internal CH4 cycle.

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