TY - JOUR A1 - Soergel, Bjoern A1 - Kriegler, Elmar A1 - Weindl, Isabelle A1 - Rauner, Sebastian A1 - Dirnaichner, Alois A1 - Ruhe, Constantin A1 - Hofmann, Matthias A1 - Bauer, Nico A1 - Bertram, Christoph A1 - Bodirsky, Benjamin Leon A1 - Leimbach, Marian A1 - Leininger, Julia A1 - Levesque, Antoine A1 - Luderer, Gunnar A1 - Pehl, Michaja A1 - Wingens, Christopher A1 - Baumstark, Lavinia A1 - Beier, Felicitas A1 - Dietrich, Jan Philipp A1 - Humpenöder, Florian A1 - von Jeetze, Patrick A1 - Klein, David A1 - Koch, Johannes A1 - Pietzcker, Robert C. A1 - Strefler, Jessica A1 - Lotze-Campen, Hermann A1 - Popp, Alexander T1 - A sustainable development pathway for climate action within the UN 2030 Agenda JF - Nature climate change N2 - Ambitious climate policies, as well as economic development, education, technological progress and less resource-intensive lifestyles, are crucial elements for progress towards the UN Sustainable Development Goals (SDGs). However, using an integrated modelling framework covering 56 indicators or proxies across all 17 SDGs, we show that they are insufficient to reach the targets. An additional sustainable development package, including international climate finance, progressive redistribution of carbon pricing revenues, sufficient and healthy nutrition and improved access to modern energy, enables a more comprehensive sustainable development pathway. We quantify climate and SDG outcomes, showing that these interventions substantially boost progress towards many aspects of the UN Agenda 2030 and simultaneously facilitate reaching ambitious climate targets. Nonetheless, several important gaps remain; for example, with respect to the eradication of extreme poverty (180 million people remaining in 2030). These gaps can be closed by 2050 for many SDGs while also respecting the 1.5 °C target and several other planetary boundaries. KW - climate-change mitigation KW - climate-change policy KW - socioeconomic scenarios KW - sustainability Y1 - 2021 U6 - https://doi.org/10.1038/s41558-021-01098-3 SN - 1758-678X SN - 1758-6798 VL - 11 IS - 8 SP - 656 EP - 664 PB - Nature Publishing Group CY - London ER - TY - JOUR A1 - Koebsch, Franziska A1 - Winkel, Matthias A1 - Liebner, Susanne A1 - Liu, Bo A1 - Westphal, Julia A1 - Schmiedinger, Iris A1 - Spitzy, Alejandro A1 - Gehre, Matthias A1 - Jurasinski, Gerald A1 - Köhler, Stefan A1 - Unger, Viktoria A1 - Koch, Marian A1 - Sachs, Torsten A1 - Böttcher, Michael E. T1 - Sulfate deprivation triggers high methane production in a disturbed and rewetted coastal peatland JF - Biogeosciences N2 - 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 remediation. This suggests that preceding land use measures can suspend the sulfate-related methane suppressing mechanisms. Here, we unravel the hydrological relocation and biogeochemical S and C transformation processes that induced high methane emissions in a disturbed and rewetted peatland despite former brackish impact. The underlying processes were investigated along a transect of increasing distance to the coastline using a combination of concentration patterns, stable isotope partitioning, and analysis of the microbial community structure. We found that diking and freshwater rewetting caused a distinct freshening and an efficient depletion of the brackish sulfate reservoir by dissimilatory sulfate reduction (DSR). Despite some legacy effects of brackish impact expressed as high amounts of sedimentary S and elevated electrical conductivities, contemporary metabolic processes operated mainly under sulfate-limited conditions. This opened up favorable conditions for the establishment of a prospering methanogenic community in the top 30-40 cm of peat, the structure and physiology of which resemble those of terrestrial organic-rich environments. Locally, high amounts of sulfate persisted in deeper peat layers through the inhibition of DSR, probably by competitive electron acceptors of terrestrial origin, for example Fe(III). However, as sulfate occurred only in peat layers below 30-40 cm, it did not interfere with high methane emissions on an ecosystem scale. Our results indicate that the climate effect of disturbed and remediated coastal wetlands cannot simply be derived by analogy with their natural counterparts. From a greenhouse gas perspective, the re-exposure of diked wetlands to natural coastal dynamics would literally open up the floodgates for a replenishment of the marine sulfate pool and therefore constitute an efficient measure to reduce methane emissions. Y1 - 2019 U6 - https://doi.org/10.5194/bg-16-1937-2019 SN - 1726-4170 SN - 1726-4189 VL - 16 IS - 9 SP - 1937 EP - 1953 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Zborowski, Krzysztof Kazimierz A1 - Koch, Andreas A1 - Kleinpeter, Erich A1 - Proniewicz, Leonard Marian T1 - Searching for aromatic celate rings. Oxygen versus Thio and Seleno Ligands JF - Zeitschrift für physikalische Chemie : international journal of research in physical chemistry and chemical physics N2 - As a part of searching for fully aromatic chelate compounds, copper complexes of malondialdehyde as well as its sulfur and selenium derivatives were investigated using the DFT quantum chemical methods. Chelate complexes of both Cu(I) and Cu(II) ions wereconsidered. Aromaticity of the metal complexes studied were analyzed using NICS(0), NICS(1), PDI, I-ring, MCI, ICMCI and I-B aromaticity indices, and by TSNMRS visualizations of the spatial magnetic properties. It seems that partial aromaticityof studied chelates increases when oxygen atoms in malondialdehyde are replaced by sulfur and selenium. KW - Aromaticity KW - Chelatoaromaticity KW - Copper Metal Complexes KW - Quantum Chemical Calculations Y1 - 2014 U6 - https://doi.org/10.1515/zpch-2014-0528 SN - 0942-9352 VL - 228 IS - 8 SP - 869 EP - 878 PB - De Gruyter CY - Berlin ER -