Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-156 Manuscript under review for journal Biogeosciences Discussion started: 8 May 2019 c Author(s) 2019. CC BY 4.0 License. Cushion bogs are stronger carbon dioxide net sinks than moss-dominated bogs as revealed by eddy covariance measurements on Tierra del Fuego, Argentina David Holl1, Verónica Pancotto2,3, Adrian Heger1, Sergio Jose Camargo3,4, and Lars Kutzbach1 1Institute of Soil Science, Center for Earth System Research and Sustainability (CEN), Universität Hamburg, Hamburg, Germany 2Centro Austral de Investigaciones Científicas (CADIC-CONICET), Ushuaia, Argentina 3Universidad de Tierra del Fuego (ICPA-UNTDF), Ushuaia, Argentina 4 Dirección de Cambio Climático (DCC), Secretaría de Estado de Ambiente, Desarrollo Sostenible y Cambio Climático (SADSyCC), Ushuaia, Argentina Correspondence: David Holl (
[email protected]) Abstract. The near-pristine bog ecosystems of Tierra del Fuego in southernmost Patagonia have so far not been studied in terms of their current carbon dioxide (CO2) sink strength. CO2 flux data from southern hemisphere peatlands is scarce in general. In this study, we present CO2 net ecosystem exchange (NEE) fluxes from two Fuegian bog ecosystems with contrasting vegetation communities. One site is located in a glaciogenic valley and developed as a peat moss-dominated raised bog, the 5 other site is a vascular plant-dominated cushion bog located at the coast of the Beagle Channel. We measured NEE fluxes with two identical eddy covariance (EC) setups at both sites for more than two years. With the EC method, we were able to observe NEE fluxes on ecosystem level and at high temporal resolution.