148 results on '"Nicolaus M"'
Search Results
2. Does genetic differentiation underlie behavioral divergence in response to migration barriers in sticklebacks? A common garden experiment
- Author
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Ramesh, A., Domingues, M. M., Stamhuis, E. J., Groothuis, T. G. G., Weissing, F. J., and Nicolaus, M.
- Published
- 2021
3. Exploring the therapeutic potential of autologous hematopoietic stem cell transplantation in progressive multiple sclerosis—a systematic review.
- Author
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Braun, Bente, Fischbach, Felix, Pfeffer, Lena Kristina, Richter, Johanna, Janson, Dietlinde, Kröger, Nicolaus M., Mariottini, Alice, Heesen, Christoph, and Häußler, Vivien
- Subjects
HEMATOPOIETIC stem cell transplantation ,DISABILITIES ,PREMENSTRUAL syndrome ,MULTIPLE sclerosis ,CLINICAL trials - Abstract
Background and Purpose: The aim was to determine the value of autologous haematopoietic stem cell transplantation (aHSCT) as a therapeutic intervention for progressive multiple sclerosis (PMS) based on a systematic review of the current literature. Methods: All studies from the databases PubMed and Google Scholar published in English before February 2024 which provided individual data for PMS patients were systematically reviewed. PICO was defined as population (P), primary progressive MS and secondary progressive MS patients; intervention (I), treatment with aHSCT; comparison (C), none, disease‐modifying therapy treated/relapsing–remitting MS cohorts if available; outcome (O), transplant‐related mortality, progression‐free survival (PFS) and no evidence of disease activity. Results: A total of 15 studies met the criteria including 665 patients with PMS (74 primary progressive MS, 591 secondary progressive MS) and 801 patients with relapsing–remitting MS as controls. PFS data were available for 647 patients. PMS patients showed more severe disability at baseline than relapsing–remitting MS patients. The average transplant‐related mortality for PMS in 10 studies was 1.9%, with 10 deaths in 528 patients. PFS ranged from 0% to 78% in PMS groups 5 years after treatment initiation, demonstrating a high variability. No evidence of disease activity scores at 5 years ranged from 0% to 75%. Conclusion: Based on the available data, aHSCT does not halt progression in people with PMS. However, there appears to be evidence of improved outcome in selected patients. Due to the heterogeneity of the available data, more comprehensive clinical trials assessing the efficacy of aHSCT across different patient groups are urgently needed to reduce variability and improve patient stratification. [ABSTRACT FROM AUTHOR]
- Published
- 2024
- Full Text
- View/download PDF
4. Regeneration of High Pressure Turbine Blades. Development of a Hybrid Brazing and Aluminizing Process by Means of Thermal Spraying
- Author
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Nicolaus, M., Möhwald, K., and Maier, H.J.
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- 2017
- Full Text
- View/download PDF
5. Future regeneration processes for high-pressure turbine blades
- Author
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Nicolaus, M., Rottwinkel, B., Alfred, I., Möhwald, K., Nölke, C., Kaierle, S., Maier, H. J., and Wesling, V.
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- 2018
- Full Text
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6. Reduced-Intensity Allografting as First Transplantation Approach in Relapsed/Refractory Grades One and Two Follicular Lymphoma Provides Improved Outcomes in Long-Term Survivors
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Klyuchnikov, Evgeny, Bacher, Ulrike, Kröger, Nicolaus M., Hari, Parameswaran N., Ahn, Kwang Woo, Carreras, Jeanette, Bachanova, Veronika, Bashey, Asad, Cohen, Jonathon B., D'Souza, Anita, Freytes, César O., Gale, Robert Peter, Ganguly, Siddhartha, Hertzberg, Mark S., Holmberg, Leona A., Kharfan-Dabaja, Mohamed A., Klein, Andreas, Ku, Grace H., Laport, Ginna G., Lazarus, Hillard M., Miller, Alan M., Mussetti, Alberto, Olsson, Richard F., Slavin, Shimon, Usmani, Saad Z., Vij, Ravi, Wood, William A., Maloney, David G., Sureda, Anna M., Smith, Sonali M., and Hamadani, Mehdi
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- 2015
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- View/download PDF
7. A Combined Brazing and Aluminizing Process for Repairing Turbine Blades by Thermal Spraying Using the Coating System NiCrSi/NiCoCrAlY/Al
- Author
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Nicolaus, M., Möhwald, K., and Maier, H. J.
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- 2017
- Full Text
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8. Janus Kinase Inhibitors and Allogeneic Stem Cell Transplantation for Myelofibrosis
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Gupta, Vikas, Gotlib, Jason, Radich, Jerald P., Kröger, Nicolaus M., Rondelli, Damiano, Verstovsek, Srdan, and Deeg, H. Joachim
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- 2014
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9. Closing the loop – Approaches to monitoring the state of the Arctic Mediterranean during the International Polar Year 2007–2008
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Mauritzen, C., Hansen, E., Andersson, M., Berx, B., Beszczynska-Möller, A., Burud, I., Christensen, K.H., Debernard, J., de Steur, L., Dodd, P., Gerland, S., Godøy, Ø., Hansen, B., Hudson, S., Høydalsvik, F., Ingvaldsen, R., Isachsen, P.E., Kasajima, Y., Koszalka, I., Kovacs, K.M., Køltzow, M., LaCasce, J., Lee, C.M., Lavergne, T., Lydersen, C., Nicolaus, M., Nilsen, F., Nøst, O.A., Orvik, K.A., Reigstad, M., Schyberg, H., Seuthe, L., Skagseth, Ø., Skarðhamar, J., Skogseth, R., Sperrevik, A., Svensen, C., Søiland, H., Teigen, S.H., Tverberg, V., and Wexels Riser, C.
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- 2011
- Full Text
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10. Physical properties of sea ice cores for biogeochemistry studies measured on legs 1 to 3 of the MOSAiC expedition
- Author
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Angelopoulos, M., Damm, E., Simões Pereira, P., Abrahamsson, K., Bauch, D., Bowman, J., Castellani, G., Creamean, J., Divine, D., Dumitrascu, A., Eggers, L., Fong, A., Fons, S., Gradinger, R., Granskog, M., Grosse, J., Haapala, J., Haas, C., Hoppe, C., Høyland, K., Immerz, A., Kolabutin, N., Krumpen, T., Lei, R., Marsay, C., Maus, S., Nicolaus, M., Nubom, A., Oggier, M., Olsen, L., Rember, R., Ren, J., Rinke, A., Sachs, T., Sheikin, I., Shimanchuk, E., Spahic, S., Stefels, J., Stephens, M., Torres-Valdés, S., Torstensson, A., Ulfsbo, A., Verdugo, J., Wang, L., Wischnewski, L., and Zhan, L.
- Abstract
We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
- Published
- 2022
11. Physical properties of sea ice cores from site MCS_FYI measured on legs 1 to 3 of the MOSAiC expedition
- Author
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Angelopoulos, M., Abrahamsson, K., Bauch, D., Bowman, J., Castellani, G., Creamean, J., Damm, E., Divine, D., Dumitrascu, A., Eggers, L., Fong, A., Fons, S., Gradinger, R., Granskog, M., Grosse, J., Haapala, J., Haas, C., Hoppe, C., Høyland, K., Immerz, A., Kolabutin, N., Krumpen, T., Lei, R., Marsay, C., Maus, S., Nicolaus, M., Nubom, A., Oggier, M., Olsen, L., Rember, R., Ren, J., Rinke, A., Sachs, T., Sheikin, I., Shimanchuk, E., Simões Pereira, P., Spahic, S., Stefels, J., Stephens, M., Torres-Valdés, S., Torstensson, A., Ulfsbo, A., Verdugo, J., Wang, L., Wischnewski, L., and Zhan, L.
- Abstract
We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
- Published
- 2022
12. Physical properties of sea ice cores from site MCS-SYI measured on legs 1 to 3 of the MOSAiC expedition
- Author
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Angelopoulos, M., Abrahamsson, K., Bauch, D., Bowman, J., Castellani, G., Creamean, J., Damm, E., Divine, D., Dumitrascu, A., Eggers, L., Fong, A., Fons, S., Gradinger, R., Granskog, M., Grosse, J., Haapala, J., Haas, C., Hoppe, C., Høyland, K., Immerz, A., Kolabutin, N., Krumpen, T., Lei, R., Marsay, C., Maus, S., Nicolaus, M., Nubom, A., Oggier, M., Olsen, L., Rember, R., Ren, J., Rinke, A., Sachs, T., Sheikin, I., Shimanchuk, E., Simões Pereira, P., Spahic, S., Stefels, J., Stephens, M., Torres-Valdés, S., Torstensson, A., Ulfsbo, A., Verdugo, J., Wang, L., Wischnewski, L., and Zhan, L.
- Abstract
We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
- Published
- 2022
13. Overview of the MOSAiC expedition:atmosphere
- Author
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Shupe, M. D. (Matthew D.), Rex, M. (Markus), Blomquist, B. (Byron), Persson, P. O. (P. Ola G.), Schmale, J. (Julia), Uttal, T. (Taneil), Althausen, D. (Dietrich), Angot, H. (Helene), Archer, S. (Stephen), Bariteau, L. (Ludovic), Beck, I. (Ivo), Bilberry, J. (John), Bucci, S. (Silvia), Buck, C. (Clifton), Boyer, M. (Matt), Brasseur, Z. (Zoe), Brooks, I. M. (Ian M.), Calmer, R. (Radiance), Cassano, J. (John), Castro, V. (Vagner), Chu, D. (David), Costa, D. (David), Cox, C. J. (Christopher J.), Creamean, J. (Jessie), Crewell, S. (Susanne), Dahlke, S. (Sandro), Damm, E. (Ellen), de Boer, G. (Gijs), Deckelmann, H. (Holger), Dethloff, K. (Klaus), Duetsch, M. (Marina), Ebell, K. (Kerstin), Ehrlich, A. (Andre), Ellis, J. (Jody), Engelmann, R. (Ronny), Fong, A. A. (Allison A.), Frey, M. M. (Markus M.), Gallagher, M. R. (Michael R.), Ganzeveld, L. (Laurens), Gradinger, R. (Rolf), Graeser, J. (Juergen), Greenamyer, V. (Vernon), Griesche, H. (Hannes), Griffiths, S. (Steele), Hamilton, J. (Jonathan), Heinemann, G. (Guenther), Helmig, D. (Detlev), Herber, A. (Andreas), Heuze, C. (Celine), Hofer, J. (Julian), Houchens, T. (Todd), Howard, D. (Dean), Inoue, J. (Jun), Jacobi, H.-W. (Hans-Werner), Jaiser, R. (Ralf), Jokinen, T. (Tuija), Jourdan, O. (Olivier), Jozef, G. (Gina), King, W. (Wessley), Kirchgaessner, A. (Amelie), Klingebiel, M. (Marcus), Krassovski, M. (Misha), Krumpen, T. (Thomas), Lampert, A. (Astrid), Landing, W. (William), Laurila, T. (Tiia), Lawrence, D. (Dale), Lonardi, M. (Michael), Loose, B. (Brice), Luepkes, C. (Christof), Maahn, M. (Maximilian), Macke, A. (Andreas), Maslowski, W. (Wieslaw), Marsay, C. (Christopher), Maturilli, M. (Marion), Mech, M. (Mario), Morris, S. (Sara), Moser, M. (Manuel), Nicolaus, M. (Marcel), Ortega, P. (Paul), Osborn, J. (Jackson), Paetzold, F. (Falk), Perovich, D. K. (Donald K.), Petäjä, T. (Tuukka), Pilz, C. (Christian), Pirazzini, R. (Roberta), Posman, K. (Kevin), Powers, H. (Heath), Pratt, K. A. (Kerri A.), Preusser, A. (Andreas), Quelever, L. (Lauriane), Radenz, M. (Martin), Rabe, B. (Benjamin), Rinke, A. (Annette), Sachs, T. (Torsten), Schulz, A. (Alexander), Siebert, H. (Holger), Silva, T. (Tercio), Solomon, A. (Amy), Sommerfeld, A. (Anja), Spreen, G. (Gunnar), Stephens, M. (Mark), Stohl, A. (Andreas), Svensson, G. (Gunilla), Uin, J. (Janek), Viegas, J. (Juarez), Voigt, C. (Christiane), von der Gathen, P. (Peter), Wehner, B. (Birgit), Welker, J. M. (Jeffrey M.), Wendisch, M. (Manfred), Werner, M. (Martin), Xie, Z. (ZhouQing), and Yue, F. (Fange)
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Arctic ,Field campaign ,Atmosphere - Abstract
With the Arctic rapidly changing, the needs to observe, understand, and model the changes are essential. To support these needs, an annual cycle of observations of atmospheric properties, processes, and interactions were made while drifting with the sea ice across the central Arctic during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition from October 2019 to September 2020. An international team designed and implemented the comprehensive program to document and characterize all aspects of the Arctic atmospheric system in unprecedented detail, using a variety of approaches, and across multiple scales. These measurements were coordinated with other observational teams to explore crosscutting and coupled interactions with the Arctic Ocean, sea ice, and ecosystem through a variety of physical and biogeochemical processes. This overview outlines the breadth and complexity of the atmospheric research program, which was organized into 4 subgroups: atmospheric state, clouds and precipitation, gases and aerosols, and energy budgets. Atmospheric variability over the annual cycle revealed important influences from a persistent large-scale winter circulation pattern, leading to some storms with pressure and winds that were outside the interquartile range of past conditions suggested by long-term reanalysis. Similarly, the MOSAiC location was warmer and wetter in summer than the reanalysis climatology, in part due to its close proximity to the sea ice edge. The comprehensiveness of the observational program for characterizing and analyzing atmospheric phenomena is demonstrated via a winter case study examining air mass transitions and a summer case study examining vertical atmospheric evolution. Overall, the MOSAiC atmospheric program successfully met its objectives and was the most comprehensive atmospheric measurement program to date conducted over the Arctic sea ice. The obtained data will support a broad range of coupled-system scientific research and provide an important foundation for advancing multiscale modeling capabilities in the Arctic.
- Published
- 2022
14. Chimeric antigen receptor T-cell therapy and fludarabine: precision dosing imperatives
- Author
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Wicha, Sebastian G., Wansing, Eva M. A., Dadkhah, Adrin, Ayuk, Francis A., Kröger, Nicolaus M., and Langebrake, Claudia
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- 2024
- Full Text
- View/download PDF
15. Micafungin as antifungal prophylaxis in recipients of allogeneic hematopoietic stem cell transplantation: results of different dosage levels in clinical practice
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Langebrake, Claudia, Rohde, Holger, Lellek, Heinrich, Wolschke, Christine, and Kröger, Nicolaus M.
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- 2014
- Full Text
- View/download PDF
16. Importance of changes in gastric emptying for postprandial plasma glucose fluxes in healthy humans
- Author
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Woerle, H.-J., Albrecht, M., Linke, R., Zschau, S., Neumann, C., Nicolaus, M., Gerich, J., Goke, B., and Schirra, J.
- Subjects
Glucose metabolism -- Physiological aspects ,Homeostasis -- Observations ,Gastrointestinal system -- Motility ,Gastrointestinal system -- Observations ,Biological sciences - Abstract
Objective: Regulation of postprandial (pp) plasma glucose excursions is complex. Insulin and glucagon are thought to play the predominant role. Nevertheless, only 50% of the variation in pp plasma glucose excursions is explained by variations by the latter. Theoretically, gastric emptying (GE) should be another important factor. However, its impact on pp glucose homeostasis is unknown. Research Design and Methods: We examined the consequences of pramlintide-induced delay in GE on pp glycemia and glucose fluxes, determined isotopically. GE was recorded by scintigraphy. Fourteen healthy subjects (8 men, 6 women; age 40 [+ or -] 3 yr, body mass index 27.8 [+ or -] 1.1 kg/[m.sup.2]) ate a mixed meal, and 30 [micro]g of pramlintide (PRAM) or placebo (PBO) were injected subcutaneously. Results: At 60 min, greater proportions of the initial gastric contents remained in the stomach (PBO vs. PRAM). Thereafter, GE slopes paralleled until 240 min. Fifty percent retention times were lower when PBO was given (P < 0.001). GE was greater from 240 min to the end of the PRAM experiments, so that only slightly greater proportions of the meal remained in the stomach at 330 min. Reductions of GE lowered pp glucose (7.5 [+ or -] 0.3 vs. 6.0 [+ or -] 0.2 mmol/1, P < 0.001), even though plasma insulin was lower with PRAM (164 [+ or -] 13 vs. 138 [+ or -] 13 pmol/ml, both P < 0.01). Reduction in total glucose appearance (P < 0.001) was due to reduced meal-derived glucose appearance (10.2 [+ or -] 0.5 vs. 7.0 [+ or -] 0.4 [micro]mol x [kg.sup.-1] x [min.sup.-1], P < 0.001). Endogenous glucose appearance was greater with PRAM (P < 0.001). Splanchnic glucose uptake was greater with PRAM (26.5 [+ or -] 1.6 vs. 32.5 [+ or -] 2.1%, P = 0.014). Conclusions: These data support the concept that GE is an important physiological regulator of pp glucose homeostasis in humans.
- Published
- 2008
17. Endogenous glucagon-like peptide 1 controls endocrine pancreatic secretion and antro-pyloro-duodenal motility in humans
- Author
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Schirra, J., Nicolaus, M., Roggel, R., Katschinski, M., Storr, M., Woerle, H.J., and Goke, B.
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Glucagon -- Research ,Pancreas -- Secretions ,Pancreas -- Physiological aspects ,Gastrointestinal system -- Motility ,Gastrointestinal system -- Physiological aspects ,Health - Published
- 2006
18. Exploring patterns of variation in clutch size–density reaction norms in a wild passerine bird
- Author
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Nicolaus, M., Brommer, J. E., Ubels, R., Tinbergen, J. M., and Dingemanse, N. J.
- Published
- 2013
- Full Text
- View/download PDF
19. Additional cytogenetic features determine outcome in patients allografted for TP53 mutant acute myeloid leukemia.
- Author
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Loke, Justin, Labopin, Myriam, Craddock, Charles, Cornelissen, Jan J., Labussière‐Wallet, Hélène, Wagner‐Drouet, Eva Maria, Van Gorkom, Gwendolyn, Schaap, Nicolaas P.M., Kröger, Nicolaus M., Veelken, Joan Hendrik, Rovira, Montserrat, Menard, Anne Lise, Bug, Gesine, Bazarbachi, Ali, Giebel, Sebastian, Brissot, Eolia, Nagler, Arnon, Esteve, Jordi, and Mohty, Mohamad
- Abstract
BACKGROUND: The presence of TP53 mutations is associated with an unfavorable outcome in patients allografted for acute myeloid leukemia (AML), leading some to question the benefit of an allogeneic stem cell transplantation (allo‐SCT) for this patient group, although this has not been studied in a large cohort. METHODS: A total of 780 patients with AML in first complete remission, with either intermediate‐ or adverse‐risk cytogenetics, whose TP53 mutation status was reported, were included in this study from the European Society for Blood and Marrow Transplantation. RESULTS: Two‐year overall survival (OS) was impaired in patients (n = 179) with evidence of a TP53 mutation at diagnosis (35.1%; 95% confidence interval [CI], 26.7–43.7) as compared to the cohort without (n = 601) (64%; 95% CI, 59.1–68.4; P =.001). In patients with mutant TP53 AML with no evidence of either chromosome 17p loss (17p–) and/or complex karyotype (CK) (n = 53, 29.6%), 2‐year OS was 65.2% (95% CI, 48.4–77.6). This was not significantly different to patients without TP53 mutations. In patients with mutant TP53 AML with either 17p– and/or CK (n = 126, 70.4%), the OS was lower (24.6%; 95% CI, 16.2–34; P =.001). CONCLUSIONS: In summary, the adverse prognostic effect of TP53 mutations in AML following an allo‐SCT is not evident in patients with neither co‐occurring 17p– and/or CK, and these data inform decisions regarding allo‐SCT in patients with TP53 mutant AML. [ABSTRACT FROM AUTHOR]
- Published
- 2022
- Full Text
- View/download PDF
20. Sea Ice
- Author
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Perovich, D, Gerland, S, Hendricks, S, Meier, Walter N, Nicolaus, M, Richter-Menge, J, and Tschudi, M
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Meteorology And Climatology - Abstract
During 2013, Arctic sea ice extent remained well below normal, but the September 2013 minimum extent was substantially higher than the record-breaking minimum in 2012. Nonetheless, the minimum was still much lower than normal and the long-term trend Arctic September extent is -13.7 per decade relative to the 1981-2010 average. The less extreme conditions this year compared to 2012 were due to cooler temperatures and wind patterns that favored retention of ice through the summer. Sea ice thickness and volume remained near record-low levels, though indications are of slightly thicker ice compared to the record low of 2012.
- Published
- 2013
21. GLP-1 regulates gastroduodenal motility involving cholinergic pathways
- Author
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SCHIRRA, J., NICOLAUS, M., WOERLE, H. J., STRUCKMEIER, C., KATSCHINSKI, M., and GÖKE, B.
- Published
- 2009
- Full Text
- View/download PDF
22. Net heterotrophy in High Arctic first-year and multi-year spring sea ice.
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Campbell, Karley, Lange, B. A., Landy, J. C., Katlein, C., Nicolaus, M., Anhaus, P., Matero, I., Gradinger, R., Charette, J., Duerksen, S., Tremblay, P., Rysgaard, S., Tranter, M., Haas, C., and Michel, C.
- Published
- 2022
- Full Text
- View/download PDF
23. From Bright Windows to Dark Spots: Snow Cover Controls Melt Pond Optical Properties During Refreezing.
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Anhaus, P., Katlein, C., Nicolaus, M., Hoppmann, M., and Haas, C.
- Subjects
SNOW cover ,SEA ice ,OPTICAL properties ,PONDS ,SOLAR radiation ,SURFACE energy - Abstract
Melt ponds have a strong impact on the Arctic surface energy balance and the ice‐associated ecosystem because they transmit more solar radiation compared to bare ice. In the existing literature, melt ponds are considered as bright windows to the ocean, even during freeze‐up in autumn. In the central Arctic during the summer‐autumn transition in 2018, we encountered a situation where more snow accumulated on refrozen melt ponds compared to the adjacent bare ice, leading to a reduction in light transmittance of the ponds even below that of bare ice. Results from a radiative transfer model support this finding. This situation has not been described in the literature before, but has potentially strong implications for example on autumn ecosystem activity, oceanic heat budget, and thermodynamic ice growth. Plain Language Summary: Arctic sea ice is covered with snow during autumn, winter and spring. During summer, melt ponds evolve in response to surface melting. After snow fall starts again in autumn, these ponds can be filled with a lot of snow compared to bare ice because of their recessed surface. Indeed, during an expedition close to the North Pole in summer and autumn 2018, we measured a thick snow cover on ponds. This thick snow cover reduced the light availability underneath the ponds to levels below that underneath adjacent bare ice. This is a surprising finding, because it is different from the established theory of high light availability underneath melt ponds during both summer and autumn and how this is described in most computer models. It has consequences for our understanding of the ice‐associated ecosystem (organisms that live in and under sea ice). It might also impact the mass and energy balance of central Arctic sea ice during summer‐autumn transition when new sea ice starts forming. Key Points: Refrozen melt ponds may collect a thicker snow cover compared to bare sea ice due to their recessed topographySuch snow‐covered melt ponds transmit less light compared to bare ice of similar typeThis scenario has not been documented before and should be accounted for in studies involving light in a refreezing Arctic Ocean [ABSTRACT FROM AUTHOR]
- Published
- 2021
- Full Text
- View/download PDF
24. Photosynthetic production in the central Arctic Ocean during the record sea-ice minimum in 2012
- Author
-
Fernández-Méndez, M., Katlein, C., Rabe, B., Nicolaus, M., Peeken, I., Bakker, K., Flores, H., and Boetius, A.
- Abstract
The ice-covered central Arctic Ocean is characterized by low primary productivity due to light and nutrient limitations. The recent reduction in ice cover has the potential to substantially increase phytoplankton primary production, but little is yet known about the fate of the ice-associated primary production and of the nutrient supply with increasing warming. This study presents results from the central Arctic Ocean collected during summer 2012, when sea-ice extent reached its lowest ever recorded since the onset of satellite observations. Net primary productivity (NPP) was measured in the water column, sea ice and melt ponds by 14CO2 uptake at different irradiances. Photosynthesis vs. irradiance (PI) curves were established in laboratory experiments and used to upscale measured NPP to the deep Eurasian Basin (north of 78° N) using the irradiance-based Central Arctic Ocean Primary Productivity (CAOPP) model. In addition, new annual production has been calculated from the seasonal nutrient drawdown in the mixed layer since last winter. Results show that ice algae can contribute up to 60% to primary production in the central Arctic Ocean at the end of the productive season (August–September). The ice-covered water column has lower NPP rates than open water due to light limitation in late summer. As indicated by the nutrient ratios in the euphotic zone, nitrate was limiting primary production in the deep Eurasian Basin close to the Laptev Sea area, while silicate was the main limiting nutrient at the ice margin near the Atlantic inflow. Although sea-ice cover was substantially reduced in 2012, total annual new production in the Eurasian Basin was 17 ± 7 Tg C yr−1, which is within the range of estimates of previous years. However, when adding the contribution by sub-ice algae, the annual production for the deep Eurasian Basin (north of 78° N) could double previous estimates for that area with a surplus of 16 Tg C yr−1. Our data suggest that sub-ice algae are an important component of the productivity in the ice-covered Eurasian Basin of the central Arctic Ocean. It remains an important question whether their contribution to productivity is on the rise with thinning ice, or whether it will decline due to overall sea-ice retreat and be replaced by phytoplankton.
- Published
- 2018
25. Iron Chelation With Deferasirox Increases Busulfan AUC During Conditioning Chemotherapy Prior to Allogeneic Stem Cell Transplantation
- Author
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Essmann, Sonja, Dadkhah, Adrin, Janson, Dietlinde, Wolschke, Christine, Ayuk, Francis, Kröger, Nicolaus M, and Langebrake, Claudia
- Published
- 2022
- Full Text
- View/download PDF
26. Associated factors for multidimensional attitudes and behaviors of reproductive health toward pregnancy among early and late adolescents in Tanzania: a cross-sectional study
- Author
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Naoki Hirose, Chen Sanmei, Mariko Okamoto, Frida E. Madeni, Nicolaus Madeni, Ayaka Teshima, Yasunobu Ando, Koji Takahama, Mayu Yoshikawa, Yu Kunimoto, and Yoko Shimpuku
- Subjects
Reproductive health ,Adolescent pregnancy ,Tanzania ,Risk factor analyses ,Gynecology and obstetrics ,RG1-991 - Abstract
Abstract Background Adolescent pregnancy is a serious reproductive health problem in Tanzania. However, the risk factors for multidimensional attitudes and behaviors of reproductive health toward pregnancy in Tanzanian adolescents remain unexplored. Methods We collected baseline characteristics and information on attitudes and behaviors of reproductive health from 4161 Tanzanian adolescents in all 54 primary and secondary schools in the Korogwe district. We applied mixed effect multiple regression analyses stratified by sex to find the factors related to reproductive health attitudes and behaviors toward pregnancy. Results In female students, regarding the attitudes of reproductive health, higher age, hope for marriage in the future, a talk with a parent about sex or pregnancy, and a higher hope score were significantly associated with a lower score. For the behaviors of reproductive health, higher age, a talk with a parent about sex or pregnancy, time to talk with a parent about daily life, and a higher hope score were significantly associated with a lower score. In male students, regarding the attitudes of reproductive health, a higher hope score was significantly associated with a lower score. For the behaviors of reproductive health, higher age, time to talk with a parent about daily life, and a higher hope score was significantly associated with a lower score. Conclusions The heterogeneous factor-outcomes association between female and male students suggested that sex-specialized interventions may be required to change their risky attitudes or behaviors of reproductive health. Although we cannot conclude as points of intervention, our study suggested that it may be practical to improve parent-adolescents communication about sex or reproductive health and change adolescents’ views of pregnancy or marriage for gaining financial or social status.
- Published
- 2023
- Full Text
- View/download PDF
27. Online sea-ice knowledge and data platform
- Author
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Grosfeld, K., Treffeisen, R., Asseng, J., Bartsch, A., Bräuer, B., Fritzsch, B., Gerdes, R., Hendricks, S., Hiller, W., Heygster, G., Krumpen, T., Lemke, P., Melsheimer, C., Nicolaus, M., Ricker, R., and Weigelt, M.
- Subjects
Earth sciences and geology ,Earth Science - Abstract
The combination of multi-disciplinary sea ice science and the rising demand of society for up-to-date information and user customized products on climate change emphasis the need for addressing the challenges posed by environmental change in the Polar Regions by means of creating new ways of communication. The new knowledge platform “meereisportal.de” is a contribution to the cross-linking of scientifically qualified information on climate change and focuses deliberately on the theme: “sea ice” in both Polar Regions. With “meereisportal. de” the science opens to changing societal demands and goes new ways of communication between science and society. “meereisportal. de” is the first comprehensive German speaking knowledge platform on sea ice that went online 2013. It was developed in the frame of the Helmholtz Climate Initiative, Regional Climate Change (REKLIM) as a joint project of the University of Bremen (Institute of Environmental Physics) and the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research under the management of the Helmholtz Regional Climate Office for Polar Regions and Sea Level change. This paper describes the concept and the development of the knowledge platform, different usage examples and user-specific products. Moreover, an outlook on the planned activities in the future will be given. Die Kombination der zunehmend multi-disziplinären Meereisforschung und die steigende Nachfrage der Gesellschaft nach aktuellen Informationen und benutzerorientierten Produkten zum Thema Klimawandel erfordert neue Wege der Wissenskommunikation, um den Herausforderungen der zunehmenden Umweltveränderungen, insbesondere in den Polarregionen, zu begegnen. Die neue Wissensplattform “meereisportal.de” ist ein Beitrag zum Vernetzen von wissenschaftlich qualifizierten Fachinformationen zum Thema Klimawandel und fokussiert dabei bewusst auf ein Thema: “Meereis” in beiden Polargebieten. Mit “meereisportal.de” öffnet sich die Wissenschaft gegenüber sich verändernden gesellschaftlichen Anforderungen und geht neue Wege der Kommunikation zwischen Wissenschaft und Gesellschaft. “meereisportal. de” ist 2013 als erste umfassende, deutschsprachige Wissensplattform rund um das Thema Meereis in der Arktis und Antarktis online gegangen. Sie wurde im Rahmen des Helmholtz-Verbundes Regionale Klimaveränderungen (REKLIM) als Gemeinschaftsprojekt der Universität Bremen (Institut für Umweltphysik) und des Alfred-Wegener-Institutes, Helmholtz-Zentrum für Polar- und Meeresforschung unter der Federführung des regionalen Helmholtz Klimabüros für Polargebiete und Meeresspiegelanstieg entwickelt. Dieser Beitrag beschreibt die Entstehung, das Konzept und die Entwicklung der Wissensplattform, verschiedene Anwendungsbeispiele sowie nutzerspezifische Produkte. Darüber hinaus wird ein Ausblick über die in Zukunft geplanten Aktivitäten gegeben.
- Published
- 2016
- Full Text
- View/download PDF
28. Benefits of aHSCT over alemtuzumab in patients with multiple sclerosis besides disability and relapses: Sustained improvement in cognition and quality of life.
- Author
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Braun, Bente, Fischbach, Felix, Richter, Johanna, Pfeffer, Lena Kristina, Fay, Heike, Reinhardt, Stefanie, Friese, Manuel A, Stellmann, Jan-P., Kröger, Nicolaus M., Heesen, Christoph, and Häußler, Vivien
- Abstract
• NEDA-3 status at five years was higher in the aHSCT group compared to alemtuzumab (p = 0.012). • Relapse free survival at five years was significantly higher in the aHSCT group. • aHSCT-treated patients showed improved QoL on HAQUAMS scaling for up to 10 years. • aHSCT showed improvements over alemtuzumab in five out of 12 cognitive tests. Autologous hematopoietic stem cell transplantation (aHSCT) exhibits promising results for multiple sclerosis (MS) in the short term. We investigated the long-term outcome differences in disease progression and cognitive impairment after aHSCT and alemtuzumab treatment. 20 patients receiving aHSCT and 21 patients treated with alemtuzumab between 2007 and 2020 were included in this monocentric observational cohort study. The primary objective was to compare the outcome of both groups with regards to achieving No Evidence of Disease Activity (NEDA-3), defined by the absence of relapses, EDSS progression, and MRI activity. Secondary endpoints in the study included the assessment of neurocognitive functioning, quality of life (QoL), Multiple Sclerosis Functional Composite (MSFC), and EDSS improvement. Baseline characteristics between both groups were comparable, except for a longer disease duration in the alemtuzumab group of 11.3 years compared to 5.4 years in aHSCT-treated patients (p = 0.002) and a longer mean follow-up time in the aHSCT cohort of 9.0 (range 2.8–15.7) years compared to 5.9 years (range 0.9–9.2) in alemtuzumab patients. NEDA-3 was more frequently observed in the aHSCT group with 75.0 % and 55.0 % at five and 10 years, respectively, than in the alemtuzumab group with only 40.0 % at five years (p = 0.012). Relapse free survival was higher in the aHSCT group (p < 0.001). None of the aHSCT-treated patients showed new T2-lesions six months after therapy initiation until the end of the observational period in contrast to 35.0 % of the alemtuzumab-treated patients showing new T2-lesions (95 %CI 14.2–98.9, p = 0.002). aHSCT-treated patients showed significantly improved cognitive performance in five out of 12 cognitive tests whereas alemtuzumab treated patients deteriorated in four out of 12 tests. Quality of life remained on a constant level for up to 10 years in patients receiving aHSCT with improved scores for the subscale fatigue (p = 0.013). aHSCT seems to be superior to alemtuzumab in maintaining long-term NEDA-3 status, improving cognition and stabilizing quality of life for up to 10 years. [ABSTRACT FROM AUTHOR]
- Published
- 2024
- Full Text
- View/download PDF
29. The common fate of ice and fish : Linkages between polar cod, sea ice properties and under-ice communities in the Arctic Ocean
- Author
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David, Carmen, Lange, B., Kohlbach, D., Flores, H., Graeve, M., Peeken, I., Nicolaus, M., Rabe, B., Krumpen, Thomas, Schaafsma, F.L., van Franeker, J.A., and Brandt, A.
- Subjects
Aquatic Ecology and Water Quality Management ,Ecosystemen ,Life Science ,Aquatische Ecologie en Waterkwaliteitsbeheer - Abstract
The Arctic Ocean faces a complete loss of the summer sea ice cover in the coming decades. Sea ice is an important habitat for microalgae ('ice algae') and a diverse ice-associated community. Hence, the rapid deterioration of sea ice habitats will cause major repercussions on the structure and functioning of Arctic ecosystems. How sea ice habitat structure shapes the ice-associated community, however, is barely understood. Using an under-ice trawl equipped with a bio-environmental sensor array throughout the Eurasian Basin, we investigated (1) the relationship between sea ice properties, and under-ice community structure; (2) the under-ice distribution of polar cod Boreogadus saida, an important carbon source for Arctic endotherms, and (3) the significance of ice algal carbon for a number of key species from the under-ice habitat. According to sea ice structure and other parameters, the environment was separated in two distinct regimes, which was resembled in the under-ice community structure. Polar cod were ubiquitous throughout the Eurasian Basin. Higher fish abundance was associated with thicker ice, higher ice coverage and lower surface salinity. Back-tracking of the ice floes hosting polar cod indicated potential areas of under-ice recruitment on the Siberian shelf. First results from fatty acid and stable isotope analysis indicate a significant contribution of ice algal carbon to the carbon budget of the food web at multiple trophic levels. This, in combination with the observed response in community composition to different environmental regimes indicates potential long-term alterations in Arctic marine ecosystems as the Arctic Ocean continues to change. Additionally, the omnipresence of polar cod in the Eurasian Basin indicates that the central Arctic under-ice habitats may constitute a potential vector of genetic exchange and a recruitment source for coastal populations around the Arctic Ocean.
- Published
- 2015
30. Commentary: Deficiencies in Socioeconomic Training During Neurosurgical Training.
- Author
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Karsy, Michael, Park, Michael S, Bekelis, Kimon, Braca, John A, Nahed, Brian V, Colen, Chaim B, Barbaro, Nicolaus M, Berger, Mitchel S, and Mukherjee, Debraj
- Published
- 2019
- Full Text
- View/download PDF
31. Export of algal biomass from the melting Arctic Sea ice
- Author
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Boetius, A., Albrecht, S., Bakker, K., Bienhold, C., Felden, J., Fernández-Méndez, M., Hendricks, S., Katlein, C., Lalande, C., Krumpen, T., Nicolaus, M., Peeken, I., Rabe, B., Rogacheva, A., Rybakova, E., Somavilla, R., Wenzhöfer, F., and Shipboard Science Party
- Abstract
In the Arctic, under-ice primary production is limited to summer months and is restricted not only by ice thickness and snow cover but also by the stratification of the water column, which constrains nutrient supply for algal growth. Research Vessel Polarstern visited the ice-covered eastern-central basins between 82° to 89°N and 30° to 130°E in summer 2012, when Arctic sea ice declined to a record minimum. During this cruise, we observed a widespread deposition of ice algal biomass of on average 9 grams of carbon per square meter to the deep-sea floor of the central Arctic basins. Data from this cruise will contribute to assessing the effect of current climate change on Arctic productivity, biodiversity, and ecological function.
- Published
- 2013
32. Ice - Ocean Interactions underneath the Antarctic Ice Shelf Ekstr��misen
- Author
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Nicolaus, M. and Grosfeld, K.
- Subjects
Science - Abstract
Polarforschung
- Published
- 2004
- Full Text
- View/download PDF
33. Regeneration of High Pressure Turbine Blades. Development of a Hybrid Brazing and Aluminizing Process by Means of Thermal Spraying.
- Author
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Nicolaus, M., Möhwald, K., and Maier, H.J.
- Abstract
Besides welding, high temperature vacuum repair-brazing is already established for nickel-based alloy turbine blades in the aerospace and power plant industries. After the worn turbine blade has been decoated to its substrate material, the filler metal is deposited as a paste, (melt-spin) foil or tape which also consists of a nickel-based alloy. Following this, the hot-gas corrosion protective coating (e.g. NiCoCrAlY) is applied using thermal spraying. The brazed turbine blade is ground or milled to size and subsequently aluminized to further increase its corrosion resistance. Using the current state of technology, a turbine blade can undergo approximately 3 to 4 repair cycles. In the present study, the development of a two-stage hybrid technology for repairing turbine blades is considered which incorporates, on the one hand, a process technology and manufacturing aspects and, on the other hand, considers material-technological mechanisms. During the first stage of this hybrid technology, the filler metal together with the hot-gas corrosion protective coating is applied using thermal spraying. The subsequent second stage combines the brazing and aluminizing processes. The technology developed here brings technical and economic advantages whilst enabling the current state-of-the-art's corresponding process chain for repairing turbine blades to be shortened. [ABSTRACT FROM AUTHOR]
- Published
- 2016
- Full Text
- View/download PDF
34. The correlation between coloration and exploration behaviour varies across hierarchical levels in a wild passerine bird.
- Author
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Nicolaus, M., Piault, R., Ubels, R., Tinbergen, J. M., and Dingemanse, N. J.
- Subjects
- *
PASSERIFORMES , *BIRD behavior , *COLOR of birds , *MELANINS , *STATISTICAL correlation - Abstract
In vertebrates, darker individuals are often found to be more active and willing to take risks (representing characteristics of a 'proactive' coping style), whereas lighter individuals are instead more cautious and less active (representing characteristics of a 'reactive' coping style). It is thus generally expected that melanin-based coloration and proactivity form a suite of positively integrated traits at the among-individual level. Here, we use a multigenerational pedigree of free-living great tits ( Parus major) to partition variation in, and the correlation between, melanin-based breast stripe ('tie') size and exploration behaviour (a proxy for coping style) into its among- and within-individual components. We show that both traits harbour heritable variation. Against predictions, tie size and speed of exploration were negatively correlated at the among-individual level due to the combined influences of permanent environmental and additive genetic effects. By contrast, the two traits were weakly positively correlated within individuals (i.e. individuals increasing in tie size after moult tended to become more explorative). The patterns of among-individual covariance were not caused by correlational selection as we found additive and opposite selection pressures acting on the two traits. These findings imply that testing hypotheses regarding the existence of a 'syndrome' at the among-individual level strictly requires variance partitioning to avoid inappropriate interpretations as the negative 'unpartitioned' phenotypic correlation between exploration and tie size resulted from counteracting effects of within- and among-individual correlations. Identifying sources and levels of (co)variation in phenotypic traits is thus critical to our understanding of biological patterns and evolutionary processes. [ABSTRACT FROM AUTHOR]
- Published
- 2016
- Full Text
- View/download PDF
35. Photosynthetic production in the central Arctic Ocean during the record sea-ice minimum in 2012.
- Author
-
Fernández-Méndez, M., Katlein, C., Rabe, B., Nicolaus, M., Peeken, I., Bakker, K., Flores, H., and Boetius, A.
- Subjects
PHOTOSYNTHESIS ,SEA ice ,PHYTOPLANKTON ,MELT ponds ,NUTRIENT pollution of water - Abstract
The ice-covered central Arctic Ocean is characterized by low primary productivity due to light and nutrient limitations. The recent reduction in ice cover has the poten-tial to substantially increase phytoplankton primary production, but little is yet known about the fate of the ice-associated primary production and of the nutrient supply with increasing warming. This study presents results from the central Arctic Ocean collected during summer 2012, when sea-ice extent reached its lowest ever recorded since the onset of satellite observations. Net primary productivity (NPP) was measured in the water column, sea ice and melt ponds by
14 CO2 uptake at different irradiances. Photosynthesis vs. irradiance (PI) curves were established in laboratory experiments and used to upscale measured NPP to the deep Eurasian Basin (north of 78° N) using the irradiance-based Central Arctic Ocean Primary Productivity (CAOPP) model. In addition, new annual production has been calculated from the seasonal nutrient drawdown in the mixed layer since last winter. Results show that ice algae can contribute up to 60 % to primary production in the central Arctic Ocean at the end of the productive season (August-September). The ice-covered water column has lower NPP rates than open water due to light limitation in late summer. As indicated by the nutrient ratios in the euphotic zone, nitrate was limiting primary production in the deep Eurasian Basin close to the Laptev Sea area, while silicate was the main limiting nutrient at the ice margin near the Atlantic inflow. Although sea-ice cover was substantially reduced in 2012, total annual new production in the Eurasian Basin was 17 ± 7 Tg C yr-1 , which is within the range of estimates of previous years. However, when adding the contribution by sub-ice algae, the annual production for the deep Eurasian Basin (north of 78° N) could double previous estimates for that area with a surplus of 16 Tg C yr-1 . Our data suggest that sub-ice algae are an important component of the productivity in the ice-covered Eurasian Basin of the central Arctic Ocean. It remains an important question whether their contribution to productivity is on the rise with thinning ice, or whether it will decline due to overall sea-ice retreat and be replaced by phytoplankton. [ABSTRACT FROM AUTHOR]- Published
- 2015
- Full Text
- View/download PDF
36. Seasonal evolution of an ice-shelf influenced fast-ice regime, derived from an autonomous thermistor chain.
- Author
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Hoppmann, M., Nicolaus, M., Hunkeler, P. A., Heil, P., Behrens, L.-K., König-Langlo, G., and Gerdes, R.
- Published
- 2015
- Full Text
- View/download PDF
37. Anti Thymocyte Globuline Allows for Successful Transplantation from HLA Mismatched Unrelated Donors.
- Author
-
Bilko, Nadja M., Ostertag, Wolfram, Stocking, Carol, Zander, Axel R., Zabelina, Tatjana, Ayuk, Francis, Wolschke, Christine, Waschke, Olga, Amtsfeld, Gitta, Eiermann, Thomas, Kabisch, Hartmut, Fehse, Boris, Berger, Jürgen, Erttmann, Rudolf, and Kröger, Nicolaus M.
- Abstract
Allogeneic hemopoietic stem cell transplantation of matched unrelated donors carries an increased risk of graft versus host disease (GvHD) and transplant related mortality (TRM). We introduced ATG Fresenius at median dose of 90 mg/kg body weight as part of the conditioning regimen for prevention of serious GvHD. We compared 48 recipients of mismatched transplants with 170 recipients of an HLA-matched transplant. The mismatches involved one or two loci. The groups differed in age [HLA-matched: 33 years (0,9-61) HLA-mismatched: 21 years (0,9-51)] and graft source, bone marrow versus peripheral blood stem cell (matched 67% bone marrow, mismatched 83% bone marrow). They were comparable in diagnosis, stage of disease and conditioning. Key words: Mismatched unrelated donor, anti-thymocyte-globuline, stem cell transplantation [ABSTRACT FROM AUTHOR]
- Published
- 2007
- Full Text
- View/download PDF
38. Photosynthetic production in the Central Arctic during the record sea-ice minimum in 2012.
- Author
-
Fernández-Méndez, M., Katlein, C., Rabe, B., Nicolaus, M., Peeken, I., Bakker, K., Flores, H., and Boetius, A.
- Subjects
PHOTOSYNTHESIS ,SEA ice ,ICE sheets ,PHYTOPLANKTON ,PLANT productivity ,PLANT nutrients - Abstract
The ice-covered Central Arctic Ocean is characterized by low primary productivity due to light and nutrient limitations. The recent reduction in ice cover has the potential to substantially increase phytoplankton primary production, but little is yet known about the fate of the ice-associated primary production and of the nutrient supply with increasing warming. This study presents results from the Central Arctic Ocean collected during summer 2012, when sea-ice reached a minimum extent since the onset of satellite observations. Net primary productivity (NPP) was measured in the water column, sea ice and melt ponds by
14 CO2 uptake at different irradiances. Photosynthesis vs. irradiance (PI) curves were established in laboratory experiments and used to upscale measured NPP to the deep Eurasian Basin (north of 78° N) using the irradiance-based Central Arctic Ocean Primary Productivity (CAOPP) model. In addition, new annual production was calculated from the seasonal nutrient drawdown in the mixed layer since last winter. Results show that ice algae can contribute up to 60% to primary production in the Central Arctic at the end of the season. The ice-covered water column has lower NPP rates than open water due to light limitation. As indicated by the nutrient ratios in the euphotic zone, nitrate was limiting primary production in the deep Eurasian Basin close to the Laptev Sea area, while silicate was the main limiting nutrient at the ice margin near the Atlantic inflow. Although sea-ice cover was substantially reduced in 2012, total annual new production in the Eurasian Basin was 17 ± 7TgCyr-1 which is within the range of estimates of previous years. However, when adding the contribution by sub-ice algae, the annual production for the deep Eurasian Basin (north of 78° N) could double previous estimates for that area with a surplus of 16 TgCyr-1 . Our data suggest that sub-ice algae are an important component of the ice-covered Central Arctic productivity. It remains an important question if their contribution to productivity is on the rise with thinning ice, or if it will decline due to overall sea-ice retreat and be replaced by phytoplankton. [ABSTRACT FROM AUTHOR]- Published
- 2015
- Full Text
- View/download PDF
39. Variability of light transmission through Arctic land-fast sea ice during spring.
- Author
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Nicolaus, M., Petrich, C., Hudson, S. R., and Granskog, M. A.
- Subjects
- *
LIGHT transmission , *SHORE-fast ice , *SEA ice , *SPRING , *SOLAR radiation , *CHLOROPHYLL analysis - Abstract
The amount of solar radiation transmitted through Arctic sea ice is determined by the thickness and physical properties of snow and sea ice. Light transmittance is highly variable in space and time since thickness and physical properties of snow and sea ice are highly heterogeneous on variable time and length scales. We present field measurements of under-ice irradiance along transects under undeformed land-fast sea ice at Barrow, Alaska (March, May, and June 2010). The measurements were performed with a spectral radiometer mounted on a floating under-ice sled. The objective was to quantify the spatial variability of light transmittance through snow and sea ice, and to compare this variability along its seasonal evolution. Along with optical measurements, snow depth, sea ice thickness, and freeboard were recorded, and ice cores were analyzed for chlorophyll a and particulate matter. Our results show that snow cover variability prior to onset of snow melt causes as much relative spatial variability of light transmittance as the contrast of ponded and white ice during summer. Both before and after melt onset, measured transmittances fell in a range from one third to three times the mean value. In addition, we found a twentyfold increase of light transmittance as a result of partial snowmelt, showing the seasonal evolution of transmittance through sea ice far exceeds the spatial variability. However, prior melt onset, light transmittance was time invariant and differences in under-ice irradiance were directly related to the spatial variability of the snow cover. [ABSTRACT FROM AUTHOR]
- Published
- 2013
- Full Text
- View/download PDF
40. Mixing, heat fluxes and heat content evolution of the Arctic Ocean mixed layer.
- Author
-
Sirevaag, A., de la Rosa, S., Fer, I., Nicolaus, M., Tjernström, M., and McPhee, M. G.
- Subjects
HEAT flux ,OCEANIC mixing ,SEA ice drift ,FREEZING points ,INFERENCE (Logic) ,HYDROGRAPHY - Abstract
A comprehensive measurement program was conducted during 16 days of a 3 week long ice pack drift, from 15 August to 1 September 2008 in the central Amundsen Basin, Arctic Ocean. The data, sampled as part of the Arctic Summer Cloud Ocean Study (ASCOS), included upper ocean stratification, mixing and heat transfer as well as transmittance solar radiation through the ice. The observations give insight into the evolution of the upper layers of the Arctic Ocean in the transition period from melting to freezing. The ocean mixed layer was found to be heated from above and, for summer conditions, the net heat flux through the ice accounted for 22% of the observed change in mixed layer heat content. Heat was mixed downward within the mixed layer and a small, downward heat flux across the base of the mixed layer accounted for the accumulated heat in the upper cold halocline during the melting season. On average, the ocean mixed layer was cooled by an ocean heat flux at the ice/ocean interface (1.2 W m
-2 ) and heated by solar radiation through the ice (-2.6 W m-2 ). An abrupt change in surface conditions halfway into the drift due to freezing and snowfall showed distinct signatures in the data set and allowed for inferences and comparisons to be made for cases of contrasting forcing conditions. Transmittance of solar radiation was reduced by 59 % in the latter period. From hydrographic observations obtained earlier in the melting season, in the same region, we infer a total fresh water equivalent of 3.3 m accumulated in the upper ocean, which together with the observed saltier winter mixed layer indicates a transition towards a more seasonal ice cover in the Arctic. [ABSTRACT FROM AUTHOR]- Published
- 2011
- Full Text
- View/download PDF
41. Stängelkristallitbildung beim Hartlöten von Stählen sowie Nickel- und Titanlegierungen.
- Author
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Bach, Fr.-W., Holländer, U., Möhwald, K., and Nicolaus, M.
- Published
- 2010
- Full Text
- View/download PDF
42. Population biology of the wandering albatross ( Diomedea exulans) in the Crozet and Kerguelen archipelagos, southern Indian Ocean, approached through genetic and demographic methods.
- Author
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Bried, J., Nicolaus, M., Jarne, P., Dubois, M.-P., and Jouventin, P.
- Subjects
- *
SEA birds , *ANIMAL species , *BIRD populations , *BIRD breeding , *MICROSATELLITE repeats - Abstract
In many seabird species, the genetic structure of the populations remains poorly known despite potential consequences for conservation. The globally threatened wandering albatross Diomedea exulans displays specific traits, including limited population size, strong philopatry, adults almost always returning to breed on the island where they made their first breeding attempt, delayed maturity, high longevity and low fecundity. Using both genetic and demographic methods, we evaluated how these traits might affect the structure within (inbreeding, low variability) and among (restricted gene flow) discrete wandering albatross colonies. Our study was conducted on Possession Island, Crozet archipelago, and in the Kerguelen archipelago. The genetic approach was based on three colonies and 10 microsatellite loci. The demographic approach used data from a 36-year capture–mark–recapture survey of the entire population from Possession Island. Inbreeding occurred as often as expected under random pairing. Genetic variability in each colony did not exceed 6.3 alleles per locus. However, no genetic bottleneck was detected. No significant genetic differentiation occurred between the two main colonies from Possession Island ( Fst<0.01), consistent with our demographic estimates of dispersal. Conversely, the genetic differentiation between Possession Island and Kerguelen was significant. Although males are more philopatric than females, genetic differentiation among colonies was not higher in males and no significant genetic differentiation between sexes was observed. Finally, we propose that the population from Crozet and that from Kerguelen are considered as distinct management units. [ABSTRACT FROM AUTHOR]
- Published
- 2007
- Full Text
- View/download PDF
43. Modellierung der Stängelkristallitbildung beim Hartlöten von Kohlenstoffstählen mit Kupfer.
- Author
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Bach, Fr.-W., Möhwald, K., Holländer, U., and Nicolaus, M.
- Published
- 2007
- Full Text
- View/download PDF
44. Acknowledgments
- Author
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Michael Walzer and Nicolaus Mills
- Published
- 2009
45. Index
- Author
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Michael Walzer and Nicolaus Mills
- Published
- 2009
46. List of Contributors
- Author
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Michael Walzer and Nicolaus Mills
- Published
- 2009
47. 11: It Isn’t Over
- Author
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Michael Walzer and Nicolaus Mills
- Published
- 2009
48. 10: Departing Responsibly
- Author
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Michael Walzer and Nicolaus Mills
- Published
- 2009
49. 6: Vietnam and the United States: The Price of Intransigence
- Author
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Michael Walzer and Nicolaus Mills
- Published
- 2009
50. 4: The Surprising Success: The United States and Korea
- Author
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Michael Walzer and Nicolaus Mills
- Published
- 2009
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