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)
A new study shows a natural solution to mitigate the effects of climate change such as extreme weather events. Researchers found that a diverse plant community acts as a buffer against fluctuations in soil temperature. This buffer, in turn, can have a decisive influence on important ecosystem processes.
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 future of the Amazon rainforest and its influence on the global climate were the focus of the visit by Frank-Walter Steinmeier and Steffi Lemke to the ATTO in Brazil. The President and the Federal Minister for the Environment visited the German-Brazilian research station on January 2nd.
Dr. Henrik Hartmann, group leader at the MPI for Biogeochemistry, takes over the management of the newly founded Institute for Forest Conservation at the Julius Kühn Institute (JKI) in Quedlinburg. We are happy with him about his new area of responsibility and we will stay in touch.
As part of the German-Brazilian cooperation project Amazon Tall Tower Observatory (ATTO), international scientists are studying the Amazon rainforest and its interaction with the atmosphere and climate. The recent project workshop clearly confirmed that ATTO has developed into a research site with globally unique capabilities – despite the pandemic and challenging field conditions.