Zero to moderate methane emissions in a densely rooted, pristine Patagonian bog - biogeochemical controls as revealed from isotopic evidence Wiebke Münchberger1, 2, Klaus-Holger Knorr1, Christian Blodau1, †, Verónica A. Pancotto3, 4, Till 5 Kleinebecker2, 5 1Ecohydrology and Biogeochemistry Research Group, Institute of Landscape Ecology, University of Muenster, Heisenbergstraße 2, 48149 Muenster, Germany 2Biodiversity and Ecosystem Research Group, Institute of Landscape Ecology, University of Muenster, Heisenbergstraße 2, 48149 Muenster, Germany 10 3Centro Austral de Investigaciones Científicas (CADIC-CONICET), B. Houssay 200, 9410 Ushuaia, Tierra del Fuego, Argentina 4Instituto de Ciencias Polares y Ambiente (ICPA-UNTDF), Fuegia Basket, 9410 Ushuaia, Tierra del Fuego, Argentina 5Institute of Landscape Ecology and Resources Management, Giessen University, Heinrich-Buff-Ring 26, 35392 Gießen, Germany 15 †deceased, July 2016 Correspondence to: Wiebke Münchberger (
[email protected]), Klaus-Holger Knorr (kh.knorr@uni- muenster.de) Abstract. Peatlands are significant global methane (CH4) sources, but processes governing CH4 dynamics have been predominantly studied on the northern hemisphere. Southern hemispheric and tropical bogs can be dominated by cushion- 20 forming vascular plants (e.g. Astelia pumila, Donatia fascicularis). These cushion bogs are found in many (mostly southern) parts of the world but could also serve as extreme examples for densely rooted northern hemispheric bogs dominated by rushes and sedges. We report