Broecker, W. S.; Klas, M.; Clark, E.; Trumbore, S. E.; Bonani, G.; Wölfli, W.; Ivy, S.: Accelerator mass spectrometric radiocarbon measurements on Foraminifera shells from deep-sea cores. Radiocarbon 32 (2), pp. 119 - 133 (1990)
Schiff, S. L.; Aravena, R.; Trumbore, S. E.; Dillon, P. J.: Dissolved organic carbon cycling in forested watersheds: a carbon isotope approach. Water Resources Research 26 (12), pp. 2949 - 2957 (1990)
Trumbore, S. E.; Keller, M.; Wofsy, S. C.; Dacosta, J. M.: Measurements of soil and canopy exchange-rates in the Amazon rain-forest using 222RN. Journal of Geophysical Research: Atmospheres 95 (D10), pp. 16865 - 16873 (1990)
Broecker, W. S.; Kennett, J. P.; Flower, B. P.; Teller, J. T.; Trumbore, S. E.; Bonani, G.; Wolfli, W.: Routing of meltwater from the laurentide ice-sheet during the younger dryas cold episode. Nature 341 (6240), pp. 318 - 321 (1989)
Damon, P. E.; Donahue, D. J.; Gore, B. H.; Hatheway, A. L.; Jull, A. J. T.; Linick, T. W.; Sercel, P. J.; Toolin, L. J.; Bronk, C. R.; Hall, E. T.et al.; Hedges, R. E. M.; Housley, R.; Law, I. A.; Perry, C.; Bonani, G.; Trumbore, S. E.; Woelfli, W.; Ambers, J. C.; Bowman, S. G. E.; Leese, M. N.; Tite, M. S.: Radiocarbon dating of the shroud of turin. Nature 337 (6208), pp. 611 - 615 (1989)
Trumbore, S. E.; Vogel, J. S.; Southon, J. R.: AMS 14C measurements of fractionated soil organic-matter - an approach to deciphering the soil carbon-cycle. Radiocarbon 31 (3), pp. 644 - 654 (1989)
Toggweiler, J. R.; Trumbore, S. E.: Bomb-test 90SR in pacific and indian-ocean surface-water as recorded by banded corals. Earth and Planetary Science Letters 74 (4), pp. 306 - 314 (1985)
Peng, T. H.; Broecker, W. S.; Freyer, H. D.; Trumbore, S. E.: A deconvolution of the tree-ring based delta-13C record. Journal of Geophysical Research: Atmospheres 88 (NC6), pp. 3609 - 3620 (1983)
Schuur, E. A.G.; Druffel, E. R.M.; Trumbore, S. E. (Eds.): Radiocarbon and Global Change: Mechanisms, Applications and Laboratory Techniques. Springer, Cham (2016), 315 pp.
Rapalee, G.; Davidson, E. A.; Harden, J. W.; Trumbore, S. E.; Veldhuis, H.; Saf, S. A. F.: Mapping drainage patterns and carbon stocks of boreal forest soils in northern Manitoba. Soc Amer Foresters, Washington (1996), 414-415 pp.
Schuur, E. A. G.; Trumbore, S. E.; Druffel, E. R. M.; Southon, J. R.; Steinhof, A.; Taylor, R. E.; Turnbull, J. C.: Radiocarbon and the global carbon cycle. In: Radiocarbon and Global Change, pp. 1 - 20 (Eds. Schuur, E. A. G.; Druffel, E. R. M.; Trumbore, S. E.). Springer, Cham (2016)
Trumbore, S. E.; Sierra, C.; Pries, C. E. H.: Radiocarbon nomenclature, theory, models, and interpretation: measuring age, determing cycling rates, and tracing source pools. In: Radiocarbon and Global Change, pp. 45 - 82 (Eds. Schuur, E. A. G.; Druffel, E. R. M.; Trumbore, S. E.). Springer, Cham (2016)
Trumbore, S. E.; Xu, X.; Santos, G. M.; Czimczik, C. I.; Beaupré, S. R.; Pack, M. A.; Hopkins, F. M.; Stills, A.; Lupascu, M.; Ziolkowski, L.: Preparation for radiocarbon analysis. In: Radiocarbon and Global Change, pp. 279 - 315 (Eds. Schuur, E. A. G.; Druffel, E. R. M.; Trumbore, S. E.). Springer, Cham (2016)
Trumbore, S. E.; Camargo, P. B. D.: Soil Carbon Dynamics. In: Amazonia and Global Change, Vol. 186, pp. 451 - 462 (Eds. Keller, M.; Bustamante, M.; Gash, J.; Dias, P. S.) (2009)
Asman, W. A. H.; Andreae, M. O.; Conrad, R.; Denmead, O. T.; Ganzeveld, L. N.; Helder, W.; Kaminski, T.; Sofiev, M. A.; Trumbore, S. E.: Working group report how can fluxes of trace gases be validated between different scales? In: Approaches to Scaling of Trace Gas Fluxes in Ecosystems, pp. 87 - 97 (Ed. Bouwman, A. F.). Elsevier Science Bv, Amsterdam (1998)
Trumbore, S. E.: Role of isotopes and tracers in scaling trace gas fluxes. In: Approaches to Scaling of Trace Gas Fluxes in Ecosystems, pp. 259 - 274 (Ed. Bouwman, A. F.). Elsevier Science Bv, Amsterdam (1998)
Aravena, R.; Schiff, S. L.; Warner, B.; Devito, K.; Trumbore, S. E.: Application of environmental isotopes in hydrological and geochemical studies in wetlands. In: Isotopes in Water Resources Management, Vol. 1, pp. 361 - 363. Int Atomic Energy Agency, Vienna (1996)
Post, W. M.; Anderson, D. W.; Dahmke, A.; Houghton, R. A.; Huc, A. Y.; Lassiter, R.; Najjar, R. G.; Neue, H. U.; Pedersen, T. F.; Trumbore, S. E.et al.; Vaikmae, R.: Group report: What is the role of nonliving organic matter cycling on the global scale? In: Role of Nonliving Organic Matter in the Earth's Carbon Cycle, pp. 155 - 174 (Eds. Zepp, R. G.; Sonntag, C.). John Wiley & Sons Ltd, Chichester (1995)
Removing a tonne of CO2 from the air and thus undoing a tonne of emissions? Doesn't quite work, says a study. And provides four objections in view of Earth systems.
The new report by the Global Carbon Project shows: Fossil CO2 emissions will reach a record high in 2023. If emissions remain this high, the carbon budget that remains before reaching the 1.5°C limit will probably be used up in seven years. Although emissions from land use are decreasing slightly, they are still too high to be compensated by renewable forests and reforestation.
Storing carbon in the soil can help to mitigate climate change. Soil organic matter bound to minerals in particular can store carbon in the long term. A new study shows that the formation of mineral-associated organic matter depends primarily on the type of mineral, but is also influenced by land use and cultivation intensity.
The Deutsche Forschungsgemeinschaft (DFG) is to fund a Research Unit in the Jena Experiment for a further four years with around five million euros. The new focus is on the stabilising effect of biodiversity against extreme climate events such as heat, frost or heavy rainfall.
Carbon sinks on the land surface mitigate the greenhouse effect. An international team of scientists has now determined that the vast majority of Europe’s total above-ground carbon storage is provided by the forests of Eastern Europe. However, this carbon sink has declined, mainly due to changes in land use.
Dr. Ana Bastos, group leader at Max Planck Institute for Biogeochemistry in Jena, was awarded the Beutenberg Campus science award in the category „outstanding junior research scientist”.
The Global Carbon Project presents its new report on global greenhouse gas budget trends. For the current year, CO2 emissions are projected to be slightly higher than before the pandemic, only slightly below the 2019 peak. If emissions remain at this high level, stabilization of the climate and achievement of the Paris climate targets is questionable.
A new study reveals that surprisingly small increases in atmospheric CO2 lead to detectable effects on ecosystem functioning. Using simulations of the land surface model developed at the Max Planck Institute for Biogeochemistry, an international team of scientists finds that enhanced CO2 first affects entities of the carbon cycle such as vegetation productivity and the extension of leaf area.
Microorganisms in aquifers deep below the earth’s surface produce similar amounts of biomass as those in some marine waters. Applying a unique, ultra-sensitive measurement method using radioactive carbon, researchers were able to demonstrate for the first time that these biotic communities in absolute darkness do not depend on sunlight.
Microorganisms decompose falling leaves, thus improving soil quality and counteracting climate change. But how do these single-celled organisms coordinate their distribution of tasks? An international research team has investigated this hitherto poorly understood process.