TY  - JOUR
A1  - Wen, Xi
A1  - Unger, Viktoria
A1  - Jurasinski, Gerald
A1  - Koebsch, Franziska
A1  - Horn, Fabian
A1  - Rehder, Gregor
A1  - Sachs, Torsten
A1  - Zak, Dominik
A1  - Lischeid, Gunnar
A1  - Knorr, Klaus-Holger
A1  - Boettcher, Michael E.
A1  - Winkel, Matthias
A1  - Bodelier, Paul L. E.
A1  - Liebner, Susanne
T1  - Predominance of methanogens over methanotrophs in rewetted fens characterized by high methane emissions
JF  - Biogeosciences
N2  - The rewetting of drained peatlands alters peat geochemistry and often leads to sustained elevated methane emission. Although this methane is produced entirely by microbial activity, the distribution and abundance of methane-cycling microbes in rewetted peatlands, especially in fens, is rarely described. In this study, we compare the community composition and abundance of methane-cycling microbes in relation to peat porewater geochemistry in two rewetted fens in northeastern Germany, a coastal brackish fen and a freshwater riparian fen, with known high methane fluxes. We utilized 16S rRNA high-throughput sequencing and quantitative polymerase chain reaction (qPCR) on 16S rRNA, mcrA, and pmoA genes to determine microbial community composition and the abundance of total bacteria, methanogens, and methanotrophs. Electrical conductivity (EC) was more than 3 times higher in the coastal fen than in the riparian fen, averaging 5.3 and 1.5 mS cm(-1), respectively. Porewater concentrations of terminal electron acceptors (TEAs) varied within and among the fens. This was also reflected in similarly high intra- and inter-site variations of microbial community composition. Despite these differences in environmental conditions and electron acceptor availability, we found a low abundance of methanotrophs and a high abundance of methanogens, represented in particular by Methanosaetaceae, in both fens. This suggests that rapid (re) establishment of methanogens and slow (re) establishment of methanotrophs contributes to prolonged increased methane emissions following rewetting.
Y1  - 2018
U6  - https://doi.org/10.5194/bg-15-6519-2018
SN  - 1726-4170
SN  - 1726-4189
VL  - 15
IS  - 21
SP  - 6519
EP  - 6536
PB  - Copernicus
CY  - Göttingen
ER  - 
TY  - JOUR
A1  - Premke, Katrin
A1  - Attermeyer, Katrin
A1  - Augustin, Jürgen
A1  - Cabezas, Alvaro
A1  - Casper, Peter
A1  - Deumlich, Detlef
A1  - Gelbrecht, Jörg
A1  - Gerke, Horst H.
A1  - Gessler, Arthur
A1  - Großart, Hans-Peter
A1  - Hilt, Sabine
A1  - Hupfer, Michael
A1  - Kalettka, Thomas
A1  - Kayler, Zachary
A1  - Lischeid, Gunnar
A1  - Sommer, Michael
A1  - Zak, Dominik
T1  - The importance of landscape diversity for carbon fluxes at the landscape level: small-scale heterogeneity matters
JF  - Wiley Interdisciplinary Reviews : Water
N2  - Landscapes can be viewed as spatially heterogeneous areas encompassing terrestrial and aquatic domains. To date, most landscape carbon (C) fluxes have been estimated by accounting for terrestrial ecosystems, while aquatic ecosystems have been largely neglected. However, a robust assessment of C fluxes on the landscape scale requires the estimation of fluxes within and between both landscape components. Here, we compiled data from the literature on C fluxes across the air–water interface from various landscape components. We simulated C emissions and uptake for five different scenarios which represent a gradient of increasing spatial heterogeneity within a temperate young moraine landscape: (I) a homogeneous landscape with only cropland and large lakes; (II) separation of the terrestrial domain into cropland and forest; (III) further separation into cropland, forest, and grassland; (IV) additional division of the aquatic area into large lakes and peatlands; and (V) further separation of the aquatic area into large lakes, peatlands, running waters, and small water bodies These simulations suggest that C fluxes at the landscape scale might depend on spatial heterogeneity and landscape diversity, among other factors. When we consider spatial heterogeneity and diversity alone, small inland waters appear to play a pivotal and previously underestimated role in landscape greenhouse gas emissions that may be regarded as C hot spots. Approaches focusing on the landscape scale will also enable improved projections of ecosystems’ responses to perturbations, e.g., due to global change and anthropogenic activities, and evaluations of the specific role individual landscape components play in regional C fluxes. WIREs Water 2016, 3:601–617. doi: 10.1002/wat2.1147
Y1  - 2016
U6  - https://doi.org/10.1002/wat2.1147
SN  - 2049-1948
SN  - 2049-1948
VL  - 3
SP  - 601
EP  - 617
PB  - Wiley
CY  - Hoboken
ER  -