TY - GEN A1 - Lyu, Yu-Xuan A1 - Fu, Qiang A1 - Wilczok, Dominika A1 - Ying, Kejun A1 - King, Aaron A1 - Antebi, Adam A1 - Vojta, Aleksandar A1 - Stolzing, Alexandra A1 - Moskalev, Alexey A1 - Georgievskaya, Anastasia A1 - Maier, Andrea B. A1 - Olsen, Andrea A1 - Groth, Anja A1 - Simon, Anna Katharina A1 - Brunet, Anne A1 - Jamil, Aisyah A1 - Kulaga, Anton A1 - Bhatti, Asif A1 - Yaden, Benjamin A1 - Pedersen, Bente Klarlund A1 - Schumacher, Björn A1 - Djordjevic, Boris A1 - Kennedy, Brian A1 - Chen, Chieh A1 - Huang, Christine Yuan A1 - Correll, Christoph U. A1 - Murphy, Coleen T. A1 - Ewald, Collin Y. A1 - Chen, Danica A1 - Valenzano, Dario Riccardo A1 - Sołdacki, Dariusz A1 - Erritzoe, David A1 - Meyer, David A1 - Sinclair, David A. A1 - Chini, Eduardo Nunes A1 - Teeling, Emma C. A1 - Morgen, Eric A1 - Verdin, Eric A1 - Vernet, Erik A1 - Pinilla, Estefano A1 - Fang, Evandro F. A1 - Bischof, Evelyne A1 - Mercken, Evi M. A1 - Finger, Fabian A1 - Kuipers, Folkert A1 - Pun, Frank W. A1 - Gyülveszi, Gabor A1 - Civiletto, Gabriele A1 - Zmudze, Garri A1 - Blander, Gil A1 - Pincus, Harold A. A1 - McClure, Joshua A1 - Kirkland, James L. A1 - Peyer, James A1 - Justice, Jamie N. A1 - Vijg, Jan A1 - Gruhn, Jennifer R. A1 - McLaughlin, Jerry A1 - Mannick, Joan A1 - Passos, João A1 - Baur, Joseph A. A1 - Betts-LaCroix, Joe A1 - Sedivy, John M. A1 - Speakman, John R. A1 - Shlain, Jordan A1 - Maltzahn, Julia von A1 - Andreasson, Katrin I. A1 - Moody, Kelsey A1 - Palikaras, Konstantinos A1 - Fortney, Kristen A1 - Niedernhofer, Laura J. A1 - Rasmussen, Lene Juel A1 - Veenhoff, Liesbeth M. A1 - Melton, Lisa A1 - Ferrucci, Luigi A1 - Quarta, Marco A1 - Koval, Maria A1 - Marinova, Maria A1 - Hamalainen, Mark A1 - Unfried, Maximilian A1 - Ringel, Michael S. A1 - Filipovic, Milos A1 - Topors, Mourad A1 - Mitin, Natalia A1 - Roy, Nawal A1 - Pintar, Nika A1 - Barzilai, Nir A1 - Binetti, Paolo A1 - Singh, Parminder A1 - Kohlhaas, Paul A1 - Robbins, Paul D. A1 - Rubin, Paul A1 - Fedichev, Peter O. A1 - Kamya, Petrina A1 - Muñoz-Canoves, Pura A1 - de Cabo, Rafael A1 - Faragher, Richard G. A. A1 - Konrad, Rob A1 - Ripa, Roberto A1 - Mansukhani, Robin A1 - Büttner, Sabrina A1 - Wickström, Sara A. A1 - Brunemeier, Sebastian A1 - Jakimov, Sergey A1 - Luo, Shan A1 - Rosenzweig-Lipson, Sharon A1 - Tsai, Shih-Yin A1 - Dimmeler, Stefanie A1 - Rando, Thomas A. A1 - Peterson, Tim R. A1 - Woods, Tina A1 - Wyss-Coray, Tony A1 - Finkel, Toren A1 - Strauss, Tzipora A1 - Gladyshev, Vadim N. A1 - Longo, Valter D. A1 - Dwaraka, Varun B. A1 - Gorbunova, Vera A1 - Acosta-Rodríguez, Victoria A. A1 - Sorrentino, Vincenzo A1 - Sebastiano, Vittorio A1 - Li, Wenbin A1 - Suh, Yousin A1 - Zhavoronkov, Alex A1 - Scheibye-Knudsen, Morten A1 - Bakula, Daniela T1 - Longevity biotechnology: bridging AI, biomarkers, geroscience and clinical applications for healthy longevity T2 - Aging Y1 - 2024 U6 - https://doi.org/10.18632/aging.206135 SN - 1945-4589 VL - 16 IS - 20 SP - 12955 EP - 12976 PB - Impact Journals, LLC ER - TY - GEN A1 - Jouy, Florent A1 - Schüle, Maren A1 - Adhikari, Yojana A1 - Binder, Anja A1 - Clerc, Danica A1 - Gerwin, Werner A1 - Heinken, Thilo A1 - Raab, Thomas A1 - Repmann, Frank A1 - Rönnefarth, Susanne A1 - Schirrmacher, Marina A1 - Schmehl, Marie-Therese A1 - Schröder, Jens A1 - Ibisch, Pierre L. T1 - Factors impacting the variability of post-fire forest regeneration in central European pine plantations T2 - Restoration Ecology N2 - Fire is increasingly posing a risk to forests and plantations, even in the temperate latitudes of central Europe. Little is known about fire ecology in this region, and therefore, appropriate approaches for the management and reforestation of burned sites are mostly lacking. In a Scots pine plantation region in Brandenburg (northeast Germany), the early tree regeneration of two nearby areas that burned 1 year apart was investigated. We observed that 3 years after the fire events, the forest in one study area showed a relatively high regeneration with a mean density of 7765 saplings/ha, clearly dominated by European aspen (93%); whereas the other study area showed a lower mean density of 5061 saplings/ha, dominated by Scots pine (71%) and aspen (15%). Three years after the fires, the difference in aspen density was 11-fold between the two areas. We studied the effects of several variables about soil and environmental properties on the aspen establishment in these two study areas in the second and third years after the fire events. We found that the post-fire aspen regeneration was influenced by several factors, including soil texture, soil disturbance from forest management, volume of deadwood, and browsing. We also discussed that weather conditions during seed production and germination might have played a role in the difference in aspen establishment between the two study areas. We concluded that the post-fire forest regeneration potential in the study region is highly variable and could come under critical pressure as climate change progresses. Y1 - 2025 UR - https://onlinelibrary.wiley.com/doi/full/10.1111/rec.70017 U6 - https://doi.org/10.1111/rec.70017 ER - TY - GEN A1 - Raab, Thomas A1 - Hinz, Christoph A1 - Gerwin, Werner A1 - Lehmkuhl, Frank T1 - Editorial for the Special Issue “Anthropogenic Geomorphology – Geomorphology in the Anthropocene” T2 - Geomorphology Y1 - 2023 U6 - https://doi.org/10.1016/j.geomorph.2022.108528 SN - 0169-555X VL - 422 ER - TY - CHAP A1 - Raab, Alexandra A1 - Raab, Thomas A1 - Schneider, Anna A1 - Hirsch, Florian A1 - Takla, Melanie A1 - Nicolay, Alexander A1 - Bonhage, Alexander A1 - Müller, Frank A1 - Heußner, Karl-Uwe A1 - Rösler, Horst T1 - Reconstructing anthropogenic landscape transformation in the surroundings of the ironwork Peitz (SE Brandenburg, Germany) - 16th to mid-19th centuries T2 - 4th International Landscape Archaeology Conference, Uppsala, 22nd - 25th August 2016 N2 - Various sources provide information about land use history and landscape transformation. For a variety of reasons, the quality of information differs and is often discontinuous or incomplete. In this interdisciplinary study we take advantage of comprehensive archaeological data gathered by large-scale excavations that were necessary because of opencast lignite mining in Lusatia, Brandenburg, Germany. By using a GIS we integrate these archaeological findings with results from archival and literature studies, from historical maps, from landforms and soils as well as from analyses of shaded-relief maps derived from up-to-date LiDAR data. The long-term aim is to develop a palaeoenvironmental model and thus to reconstruct landscape changes caused by human activities. The focus of the study is the Peitz ironwork in SE Brandenburg, which was a large consumer of commodities for about 300 years. During the time it operated, extensive transformations are supposed to have affected the landscape in the vicinity because of wood consumption and especially charcoal production. Digital datasets about forested areas for different timespans reconstructed from historical maps were made available. In combination with dendrochronological dating of charred trees, the spatiotemporal dimension of charcoal kilns was determined. Also, sites of former bog iron ore mining could be identified. Moreover, the different sources contain further information about other forms of land uses such as agriculture, pastoralism and even viticulture. In conclusion we can highlight that the mosaic of past land use systems is different from the modern structure but that major changes in the forests have been retained. Y1 - 2016 UR - http://www.arkeologi.uu.se/digitalAssets/447/c_447246-l_1-k_20160816_lac_booklet.pdf SP - S. 152 PB - Department of archaeology and ancient history, Uppsala university, CY - Uppsala ER - TY - CHAP A1 - Takla, Melanie A1 - Müller, Frank A1 - Rösler, Horst A1 - Raab, Alexandra A1 - Raab, Thomas T1 - Forestry and charcoal burning in the vicinity of the ironwork Peitz (South Brandenburg, Germany) - What do we know from historical and archaeological data? T2 - European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April – 02 May 2014 N2 - The former royal forest districts around Peitz (South Brandenburg, Germany) were used to produce charcoal for the ironwork Peitz (1554 to 1856). More than 800 archaeologically excavated ground plans of charcoal kilns give evidence of the burning activity in the study area “Jänschwalde Heide” which is only a small part of the whole forest district. The study area in the apron of the active lignite mine Jänschwalde comprises the royal forest “Jänschwalder Heide” and the surrounding community forests. Our study approach combines archaeological research, a GIS-based approach (historical maps, airborne laser scanning (ALS) data, etc.) and archival studies. Y1 - 2014 UR - http://meetingorganizer.copernicus.org/EGU2014/EGU2014-3858-1.pdf N1 - EGU2014-3858-1 PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - CHAP A1 - Takla, Melanie A1 - Müller, Frank A1 - Rösler, Horst A1 - Raab, Alexandra A1 - Raab, Thomas ED - Schwab, Markus J. ED - Theuerkauf, Martin ED - Brauer, Achim ED - Wilmking, Martin ED - Lampe, Reinhard T1 - Forestry and charcoal burning in the vicinity of the ironwork Peitz (South Brandenburg, Germany) – What do we know from historical and archaeological data? T2 - 3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age Y1 - 2014 U6 - https://doi.org/10.2312/GFZ.b103-14028 SP - 51 PB - GFZ German Research Centre for Geosciences CY - Potsdam ER - TY - GEN A1 - Dümig, Alexander A1 - Veste, Maik A1 - Hagedorn, Frank A1 - Fischer, Thomas A1 - Lange, Philipp A1 - Spröte, Roland A1 - Kögel-Knabner, Ingrid T1 - Biological soil crusts on initial soils: organic carbon dynamics and chemistry under temperate climatic conditions T2 - Biogeosciences Discussion Y1 - 2012 SN - 1810-6285 VL - 10 IS - 1 SP - 851 EP - 894 ER - TY - GEN A1 - Dümig, Alexander A1 - Veste, Maik A1 - Hagedorn, Frank A1 - Fischer, Thomas A1 - Lange, Philipp A1 - Spröte, Roland A1 - Kögel-Knabner, Ingrid T1 - Organic matter from biological soil crusts induces the initial formation of sandy temperate soils T2 - Catena N2 - Different development stages of algae-dominated and moss-dominated biological soil crusts (BSCs) were sampled on a natural sand dune (b17 years old) and on an experimental sand dune (b8 years old) along a catena, including gradients of vegetation cover, location on the slope, as well as composition and thickness of BSC organisms in northeastern Germany. The accumulation of BSC-derived organic carbon (OC)was determined for bulk materials and fractions less than 63 μm. The OC composition was characterized by solid-state 13C NMR spectroscopy and the carbohydrate-C signature. 14C contents were determined to assess the origin and dynamics of OC. From the radiocarbon contents, two OC pools were differentiated: recent BSC-derived and lignite-derived “old” OC. Downward movement of OC into the underlying substratewas found only undermoss-dominated BSCs at the old sand dune. BSC-derived OC was mainly composed of carbohydrate-C and, to a lesser extent, alkyl C and N-alkyl C, with considerably higher contributions of alkyl C in the young dune, indicating differences in the composition of extracellular polymeric substances produced by the BSCs with age. This is consistent with higher proportions of water-soluble OC of moss-dominated BSCs at the old dune, which is leached in the underlying substrate and initiates soil formation. Because of the channeling effect of mosses, OC depth translocation along with suspended colloidal substances contribute to OC accumulation in substrates. Y1 - 2014 U6 - https://doi.org/10.1016/j.catena.2014.06.011 VL - 122 SP - 196 EP - 208 ER - TY - GEN A1 - Gerwin, Werner A1 - Repmann, Frank A1 - Schaaf, Wolfgang A1 - Raab, Thomas T1 - Bodenveränderungen durch Waldbrände – Stoffvorräte und Stoffverlagerungen T2 - Jahrestagung der DBG 2022 "Grenzen überwinden, Skalen überschreiten" 5. - 8. September 2022 in Trier N2 - Die zurückliegenden trocken-heißen Sommer haben im Süden Brandenburgs zu zahlreichen Bränden in den dominierenden Kiefernwäldern geführt, einige davon mit katastrophalen Ausmaßen. Dazu gehören die extremen Brandereignisse 2018 bei Treuenbrietzen sowie 2019 bei Jüterbog und Lieberose, die zusammen weit über 1000 ha Waldfläche zerstört und dabei auch Veränderungen der betroffenen Waldböden verursacht haben. Das seit Mai 2020 von der FNR geförderte Verbundvorhaben Pyrophob befasst sich mit den Auswirkungen von Waldbränden im Süden Brandenburgs auf die Waldökosysteme und mit waldbaulichen Maßnahmen, die mittelfristig zu einer Verringerung der Brandanfälligkeit der Wälder beitragen sollen. Im Rahmen des auf eine fünfjährige Laufzeit ausgelegten Verbundvorhabens finden bodenkundliche Untersuchungen auf zwölf Versuchsflächen bei Treuenbrietzen und Jüterbog statt. An beiden Standorten werden unverbrannte Referenzflächen mit einbezogen. Ergänzend konnten bei Lieberose bereits 2019 nur kurz nach dem Brandgeschehen erste Bodenuntersuchungen durchgeführt werden. Die untersuchten Brandflächen bei Jüterbog und Lieberose sind als Totalreservate ausgewiesen, auf denen auch nach dem Brand waldbauliche Maßnahmen vollständig unterbleiben. Auf den Flächen bei Treuenbrietzen wurden verschiedene Behandlungsvarianten durchgeführt, zu denen auf einem Teil der Flächen die vollständige Entfernung der abgestorbenen Bäume gehörte, während auf anderen Teilflächen Totholz auf der Fläche verblieb. Ziel der bodenkundlichen Arbeiten in Pyrophob ist zum einen eine Charakterisierung der direkten Auswirkungen des Brandes auf Humus und Mineralboden hinsichtlich des Stoffbestandes und bodenbiologischer Prozesse. Zum anderen wird der Stoffaustrag aus dem Oberboden erfasst. Der etwaige Einfluss der unterschiedlichen waldbaulichen Vorgehensweise auf die Bodenverhältnisse wird dabei als ein Indikator für die Auswahl geeigneter Maßnahmen berücksichtigt. In den verschiedenen Untersuchungsvarianten des Vorhabens wurden zu diesem Zweck Humus- und Mineralbodenprofile untersucht. Zudem wurden Mischproben aus dem Ober- und Unterboden entnommen und auf ihren Stoffhaushalt hin analysiert. Auf jeder Untersuchungsfläche wurden je drei frei dränende Kleinlysimeter in 10 cm Bodentiefe installiert, um die zeitlichen Veränderungen der Sickerwasserzusammensetzung und die durch den Brand initiierten Stoffausträge aus dem Oberboden zu quantifizieren. Ergänzend finden Untersuchungen zu möglichen Auswirkungen der Brände auf bodenbiologische Prozesse wie Streuabbau und Stickstoffmineralisation statt. Y1 - 2022 UR - https://www.dbges.de/de/system/files/Trier2022/programmheft-dbg_2022_ou_17052022_lores.pdf SP - 48 ER - TY - GEN A1 - Sut-Lohmann, Magdalena A1 - Repmann, Frank A1 - Raab, Thomas T1 - Stability of Prussian Blue in Soils of a Former Manufactured Gas Plant Site T2 - Soil and Sediment Contamination N2 - Soil contamination with iron-cyanide complexes is a common problem at former manufactured gas plant (MGP) sites. Dissolution of the cyanide, from Prussian Blue (ferric ferrocyanide), creates an environmental hazard, whereas the risk of groundwater contamination depends on the stability of dissolved iron–cyanide complexes. Lack of a standard leaching method to determine the water-soluble (plant-available) cyanide fraction generates potential limitations for implementing remediation strategies like phytoremediation. Applicability of neutral solution extraction to determine the water-soluble cyanide fraction and the stability of Prussian Blue in surface and near-surface soils of an MGP site in Cottbus, undersaturated and unsaturated water conditions, was studied in column leaching and batch extraction experiments. MGP soils used in the long-term tests varied according to the pH (5.0–7.7) and the total cyanide content (40–1718 mg kg−1). Column leaching, after four months of percolation, still yielded effluent concentrations exceeding the German drinking water limit (> 50 μg L−1) and the solubility of Prussian Blue reported in the literature (< 1 mg L−1) from both alkaline and acidic soils. Long-term (1344 h) extraction of MGP soils with distilled water was sufficient to dissolve 97% of the total cyanide from the slightly alkaline soils and up to 78% from the acidic soils. Both experiments revealed that dissolution of ferric ferrocyanide under circum-neutral pH and oxic water conditions is a function of time, where the released amount is dependent on the soil pH and total cyanide content. Unexpectedly high and continuous solubility of Prussian Blue, both in acidic and slightly alkaline MGP soils, implies the need to introduce an additional cyanide fraction (“readily soluble fraction”) to improve and specify cyanide leaching methods. Long-term extraction of cyanide-contaminated soil in neutral solution seems to be a promising approach to evaluate the potential hazard of groundwater pollution at the MGP sites. Y1 - 2014 U6 - https://doi.org/10.1080/15320383.2014.839626 SN - 1549-7887 VL - 23 IS - 5 SP - 504 EP - 522 ER -