Benk, S.; Yan, L.; Lehmann, R.; Roth, V.-N.; Schwab, V. F.; Totsche, K. U.; Küsel, K.; Gleixner, G.: Fueling diversity in the subsurface: Composition and age of dissolved organic matter in the critical zone. Frontiers in Earth Science 7, 296 (2019)
Simon, C.; Roth, V.-N.; Dittmar, T.; Gleixner, G.: Molecular signals of heterogeneous terrestrial environments identified in dissolved organic matter: a comparative analysis of orbitrap and ion cyclotron resonance mass spectrometers. Frontiers in Earth Science 6, 138 (2018)
Seifert, A.-G.; Roth, V.-N.; Dittmar, T.; Gleixner, G.; Breuer, L.; Houska, T.; Marxsen, J.: Comparing molecular composition of dissolved organic matter in soil and stream water: Influence of land use and chemical characteristics. Science of the Total Environment 571, pp. 142 - 152 (2016)
Roth, V.-N.; Dittmar, T.; Gaupp, R.; Gleixner, G.: The molecular composition of dissolved organic matter in forest soils as a function of pH and temperature. PLoS One 10 (3), e0119188 (2015)
Roth, V.-N.; Dittmar, T.; Gaupp, R.; Gleixner, G.: Latitude and pH driven trends in the molecular composition of DOM across a north south transect along the Yenisei River. Geochimica et Cosmochimica Acta 123, pp. 93 - 105 (2013)
Roth, V.-N.: Molecular characterization of dissolved organic matter by ultrahigh-resolution mass spectrometry. Dissertation, Friedrich Schiller University Jena, Jena (2013)
Extreme precipitation should increase with warmer temperatures. Data from tropical regions show that this correlation is obscured by the cooling effect of clouds. When cloud effects are corrected, the increase in extreme precipitation with rising temperatures becomes apparent.
More frequent strong storms are destroying ever larger areas of the Amazon rainforest. Storm damage was mapped between 1985 and 2020. The total area of affected forests roughly quadrupled in the period studied.
The Global Carbon Project shows that fossil CO2 emissions will continue to rise in 2024. There is no sign of the rapid and substantial decline in emissions that would be needed to limit the impact of climate change
The Chinese Academy of Sciences (CAS) and the German National Academy of Sciences Leopoldina will hold a joint conference on the challenges of achieving carbon neutrality in Berlin on October 29-30, 2024.
Experts from science, journalism, local authorities and non-governmental organizations consider a change of course in communication on climate issues to be urgently needed. The appeal was published on the occasion of the K3 Congress on Climate Communication with around 400 participants in Graz.
A study by Leipzig University, the German Centre for Integrative Biodiversity Research Halle-Jena-Leipzig (iDiv) and the MPI for Biogeochemistry shows that gaps in the canopy of a mixed floodplain forest have a direct influence on the temperature and moisture in the forest soil, but only a minor effect on soil activity.
EU funds the international research project AI4PEX to further improve Earth system models and thus scientific predictions of climate change. Participating scientists from 9 countries met at the end of May 2024 to launch the project at the MPI for Biogeochemistry in Jena, which is leading the project.
Thuringia is severely affected by climate change, which is already reflected in extreme weather events and rising temperatures. The Climate Council is calling for the consistent implementation and tightening of climate policy targets in order to achieve climate neutrality by 2045. The coming legislative period is crucial for the future of Thuringia.
From the Greek philosopher Aristotle to Charles Darwin to the present day, scientists have dealt with this fundamental question of biology. Contrary to public perception, however, it is still largely unresolved. Scientists have now presented a new approach for the identification and delimitation of species using artificial intelligence (AI).
When it comes to studying climate change, we generally assume that the total amount of carbon emissions determines how much the planet will warm. A new study suggests that not only the amount, but also the timing of those emissions controls the amount of surface warming that occurs on human time-scale.