Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Viktoria Unger"'
Autor:
Dominik Zak, Cyril Roth, Viktoria Unger, Tobias Goldhammer, Nathalie Fenner, Chris Freeman, Gerald Jurasinski
Publikováno v:
Frontiers in Environmental Science, Vol 7 (2019)
There have been widespread attempts to rewet peatlands in Europe and elsewhere in the world to restore their unique biodiversity as well as their important function as nutrient and carbon sinks. However, changes in hydrological regime and therefore o
Externí odkaz:
https://doaj.org/article/d5b88d9a05f54070879207eaf7f5c8ec
Autor:
Gerald Jurasinski, Manon Janssen, Maren Voss, Michael E. Böttcher, Martin Brede, Hans Burchard, Stefan Forster, Lennart Gosch, Ulf Gräwe, Sigrid Gründling-Pfaff, Fouzia Haider, Miriam Ibenthal, Nils Karow, Ulf Karsten, Matthias Kreuzburg, Xaver Lange, Peter Leinweber, Gudrun Massmann, Thomas Ptak, Fereidoun Rezanezhad, Gregor Rehder, Katharina Romoth, Hanna Schade, Hendrik Schubert, Heide Schulz-Vogt, Inna M. Sokolova, Robert Strehse, Viktoria Unger, Julia Westphal, Bernd Lennartz
Publikováno v:
Frontiers in Marine Science, Vol 5 (2018)
Coastal zones connect terrestrial and marine ecosystems forming a unique environment that is under increasing anthropogenic pressure. Rising sea levels, sinking coasts, and changing precipitation patterns modify hydrodynamic gradients and may enhance
Externí odkaz:
https://doaj.org/article/27607c044f5840ea9a5f69f363de401c
Autor:
Cordula Nina Gutekunst, Susanne Liebner, Anna-Kathrina Jenner, Klaus-Holger Knorr, Viktoria Unger, Franziska Koebsch, Erwin Don Racasa, Sizhong Yang, Michael Ernst Böttcher, Manon Janssen, Jens Kallmeyer, Denise Otto, Iris Schmiedinger, Lucas Winski, Gerald Jurasinski
Publikováno v:
Biogeosciences
eISSN
eISSN
Rewetted peatlands can be a significant source of methane (CH4), but in coastal ecosystems, input of sulfate-rich seawater could potentially mitigate these emissions. The presence of sulfate as an electron acceptor during organic matter decomposition
Autor:
Cordula Nina Gutekunst, Susanne Liebner, Anna-Kathrina Jenner, Klaus-Holger Knorr, Viktoria Unger, Franziska Koebsch, Erwin Don Racasa, Sizhong Yang, Michael Ernst Böttcher, Manon Janssen, Jens Kallmeyer, Denise Otto, Iris Schmiedinger, Lucas Winski, Gerald Jurasinski
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df98d958f05331dd0eb613dc4530319d
https://doi.org/10.5194/egusphere-2022-65-supplement
https://doi.org/10.5194/egusphere-2022-65-supplement
Autor:
Cordula Gutekunst, Susanne Liebner, Anna-Kathrina Jenner, Klaus-Holger Knorr, Viktoria Unger, Franziska Koebsch, Erwin Don Racasa, Sizhong Yang, Michael Ernst Böttcher, Manon Janssen, Jens Kallmeyer, Denise Otto, Iris Schmiedinger, Lucas Winski, Gerald Jurasinski
Publikováno v:
Abstracts
Rewetted peatlands can be a significant source of methane, but in coastal systems, input of sulfate-rich seawater could potentially reduce these emissions. The presence of sulfate is known to suppress methanogenesis, by encouraging the growth of sulf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1e63e568cbbdb7c8ffd4473025e88049
https://doi.org/10.5194/egusphere-egu22-8384
https://doi.org/10.5194/egusphere-egu22-8384
Autor:
Anna-K. Jenner, Klaus-Holger Knorr, Franziska Koebsch, Gerald Jurasinski, Cordula Gutekunst, Susanne Liebner, Michael E. Böttcher, Viktoria Unger, Jens Kallmeyer, Sizhong Yang
Drainage of peatlands for intensive and long-term agricultural use leads to higher mineralization rates of the organic material and thus, increased carbon dioxide (CO2) emissions. However, when degraded peatlands are rewetted, high methane (CH4) emis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec01848972f90b338e32fe4ecff9f699
https://doi.org/10.5194/egusphere-egu21-3328
https://doi.org/10.5194/egusphere-egu21-3328
Autor:
Vytas Huth, Susanne Liebner, Florian Beyer, Franziska Koebsch, Daniel Köhn, Marian Koch, Anke Günther, Viktoria Unger, Cordula Gutekunst, Gerald Jurasinski
Although peatlands cover only about 3% of the land surface of the Earth they store approx. 42% of all soil carbon, if not considerably more, as newest model approaches suggest. Only a minor fraction of all peatlands (5%) is drained, making up a total
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0124ef9c683109638a074050c086a7e
https://doi.org/10.5194/egusphere-egu2020-10302
https://doi.org/10.5194/egusphere-egu2020-10302
Autor:
Viktoria Unger, Sizhong Yang, Susanne Liebner, Torsten Sachs, Klaus-Holger Knorr, Jens Kallmeyer, Gregor Rehder, Franziska Koebsch, Pia Gottschalk, Fabian Horn, Gerald Jurasinski
Publikováno v:
Soil Biology and Biochemistry
Both the frequency and intensity of drought events are expected to increase, with unresolved alterations to peatland methane cycling and the involved microbial communities. While existing studies have assessed drought effects via experimental approac
Publikováno v:
Estuarine, Coastal and Shelf Science. 182:179-189
Organic carbon sequestration in salt marsh soils is a function of factors that influence both spatial variability and chemical stability of accumulating carbon. Refractory carbon (slowly decomposed) may be the most important in terms of long-term seq
Autor:
Franziska Koebsch, Matthias Winkel, Susanne Liebner, Bo Liu, Julia Westphal, Iris Schmiedinger, Alejandro Spitzy, Matthias Gehre, Gerald Jurasinski, Stefan Köhler, Viktoria Unger, Marian Koch, Torsten Sachs, Michael E. Böttcher
Publikováno v:
Biogeosciences Discussions
EPIC3Biogeosciences, 16(9), pp. 1937-1953
Biogeosciences
EPIC3Biogeosciences, 16(9), pp. 1937-1953
Biogeosciences
In natural coastal wetlands, high supplies of marine sulfate suppress methanogenesis. Coastal wetlands are, however, often subject to disturbance by diking and drainage for agricultural use and can turn to potent methane sources when rewetted for rem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::27e852391d8f4a8f74cc4fb97d4eb30b
https://doi.org/10.5194/bg-2018-416
https://doi.org/10.5194/bg-2018-416