42 results on '"Lindhorst, K."'
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2. Application of efficient surrogate modeling to aeroelastic analyses of an aircraft wing
- Author
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Sommerwerk, K., Michels, B., Lindhorst, K., Haupt, M.C., and Horst, P.
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- 2016
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3. Nonlinear Reduced Order Modeling for Aeroelastic Simulation with Neural Networks
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Lindhorst, K., Haupt, M. C., Horst, P., Kroll, Norbert, editor, Radespiel, Rolf, editor, Burg, Jan Willem, editor, and Sørensen, Kaare, editor
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- 2013
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4. Active Faulting in Lake Constance (Austria, Germany, Switzerland) Unraveled by Multi-Vintage Reflection Seismic Data
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Fabbri, S.C., primary, Affentranger, C., additional, Krastel, S., additional, Lindhorst, K., additional, Wessels, M., additional, Madritsch, Herfried, additional, Allenbach, R., additional, Herwegh, M., additional, Heuberger, S., additional, Wielandt-Schuster, U., additional, Pomella, H., additional, Schwestermann, T., additional, and Anselmetti, F.S., additional
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- 2021
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5. Sedimentological, geochemical, petrophysical, and geochronological data on drill cores and samples from the 2019 Lake Constance (Germany) drilling campaign with Hipercorig
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Harms, U., Schaller, S., Raschke, U., Anselmetti, F., Boettcher, M., Buechi, M., Epp, L., Fabbri, S., Gribenski, N., Krastel, S., Liebezeit, A., Lindhorst, K., Schleheck, D., Schmiedinger, I., Schwalb, A., Vogel, H., Wessels, M., and Wittig, V.
- Abstract
The basin sediments of Lake Constance encompass superior records of glacial to late glacial and Holocene environmental conditions but were hitherto not recovered from greater depths due to the lack of high-quality but inexpensive coring instruments. In a test and commissioning campaign in 2019, a new scientific coring device, called Hipercorig, was deployed and recovered from two parallel boreholes a 20 and a 24 m long drillcore and one two-m-long surface core (Harms et al. 2020, Schaller et al. 2022). The drill site is in 200 m deep waters close to the northwestern lake shoreline near the town of Hagnau and was selected based on new seismic surveys. They revealed an up to 150 m thick sediment fill of the overdeepened Lake Constance basin created by several advance and retreat cycles of the Rhine Glacier during the mid to late Quaternary. The deposits comprise proglacial sediments overlain by glaciolacustrine and finally lake strata. The latter make up the top 12 m of the core recovered while below sandy intercalations indicate downward increasing influence of dynamic sedimentation pulses that were deposited through subaquatic channel systems fed by declining glaciers and meltwater pulses from the north. The cores retrieved were sampled for microbiology and pore fluids at University of Constance (Germany). They were opened at Bern University (Switzerland) in fall 2019, sedimentologically described, instrumentally logged, and sampled for further studies including age dating. These data served to identify 14 lithotypes that were differentiated into three chronostratigraphic units based on a 14C- and OSL-based age model. The cores section base with the proglacial unit is about 13.7 ka BP old while the lacustrine strata cover Bølling-Alerød and Holocene ages. A prominent turbiditic event layer could be dated at 9.5 ka BP, coeval with the largest Holocene Alpine rock slide, the Flimser Bergsturz, that caused damming of the river Rhine and finally an outburst reaching as turbidite even northern Lake Constance. These initially gained data sets and the instruments utilized are described in the data description.
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- 2021
6. Climate and sea-level controlling internal architecture of a Quaternary carbonate ramp (Northwest Shelf of Australia)
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Hiatt, E, Hallenberger, M, Reuning, L, Back, S, Gallagher, SJ, Iwatani, H, Lindhorst, K, Hiatt, E, Hallenberger, M, Reuning, L, Back, S, Gallagher, SJ, Iwatani, H, and Lindhorst, K
- Abstract
The continental shelf of Northwest Australia hosts an extensive tropical carbonate ramp that forms an important template for the interpretation of similar systems in the sedimentary record. Yet, little is known about its development from the middle to late Quaternary, a period of high frequency glacioeustatic changes in sea-level and climate. This research describes core and seismic-reflection data from a mid-ramp to outer ramp transect at the Northwest Shelf. Core material includes the upper 70 m of International Ocean Discovery Program Site U1461 (Expedition 356), which covers the last 500 kyr. During arid glacials, sedimentation is characterized by inorganically precipitated carbonates, including aragonite-needle mud and ooids. Ooids developed under shallow marine conditions on small-scale flat-topped platforms. Seismic and sedimentological evidence indicates that these platforms developed locally on top of the present-day mid-ramp and were typically only active during a single glacial period. Aragonite-needle mud precipitated (inorganically) in shallow-water areas. Much of these fine sediments were subsequently exported into deeper water where they mixed with pelagic carbonates. Humid interglacials are generally characterized by reduced sedimentation across the Northwest Shelf of Australia, resulting in the amalgamation of glacial lowstand deposits. Yet, substantial amounts of skeletal carbonates were deposited at the studied location during the Holocene and Marine Isotope Stage 11. These sediment accumulations are interpreted as a local feature caused by a decline in current energy. The study presented highlights a ramp system where climate is as important as sea-level in controlling carbonate deposition.
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- 2021
7. Mediterranean winter rainfall in phase with African monsoons during the past 1.36 million years
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Wagner, B. Vogel, H. Francke, A. Friedrich, T. Donders, T. Lacey, J.H. Leng, M.J. Regattieri, E. Sadori, L. Wilke, T. Zanchetta, G. Albrecht, C. Bertini, A. Combourieu-Nebout, N. Cvetkoska, A. Giaccio, B. Grazhdani, A. Hauffe, T. Holtvoeth, J. Joannin, S. Jovanovska, E. Just, J. Kouli, K. Kousis, I. Koutsodendris, A. Krastel, S. Lagos, M. Leicher, N. Levkov, Z. Lindhorst, K. Masi, A. Melles, M. Mercuri, A.M. Nomade, S. Nowaczyk, N. Panagiotopoulos, K. Peyron, O. Reed, J.M. Sagnotti, L. Sinopoli, G. Stelbrink, B. Sulpizio, R. Timmermann, A. Tofilovska, S. Torri, P. Wagner-Cremer, F. Wonik, T. Zhang, X.
- Abstract
Mediterranean climates are characterized by strong seasonal contrasts between dry summers and wet winters. Changes in winter rainfall are critical for regional socioeconomic development, but are difficult to simulate accurately1 and reconstruct on Quaternary timescales. This is partly because regional hydroclimate records that cover multiple glacial–interglacial cycles2,3 with different orbital geometries, global ice volume and atmospheric greenhouse gas concentrations are scarce. Moreover, the underlying mechanisms of change and their persistence remain unexplored. Here we show that, over the past 1.36 million years, wet winters in the northcentral Mediterranean tend to occur with high contrasts in local, seasonal insolation and a vigorous African summer monsoon. Our proxy time series from Lake Ohrid on the Balkan Peninsula, together with a 784,000-year transient climate model hindcast, suggest that increased sea surface temperatures amplify local cyclone development and refuel North Atlantic low-pressure systems that enter the Mediterranean during phases of low continental ice volume and high concentrations of atmospheric greenhouse gases. A comparison with modern reanalysis data shows that current drivers of the amount of rainfall in the Mediterranean share some similarities to those that drive the reconstructed increases in precipitation. Our data cover multiple insolation maxima and are therefore an important benchmark for testing climate model performance. © 2019, The Author(s), under exclusive licence to Springer Nature Limited.
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- 2019
8. Submarine Landslides - Subaqueous Mass Transport Deposits from Outcrops to Seismic Profiles
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Sammartini, M., Moernaut, J., Anselmetti, F., Hilbe, M., Lindhorst, K., Preat, N., Strasser, M.
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- 2019
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9. North Atlantic Subtropical Gyre Azores Front (NASGAF), Cruise No. MSM58/1, September 10, 2016 - October 7, 2016, Reykjavik (Iceland) - Ponta Delgada (Azores, Portugal)
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Repschläger, J., Auderset, A., Blanz, T., Bremer, K., Böttner, C., Eich, C., Kausch, T., Keigwin, L., Keul, N., Kiefer, J., Krupp, A., Lindhorst, K., Macholdt, D., Petersen, J., Schiebel, R., Schneider, R., Schulze, I., Steen, E., and Weis, U.
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Earth sciences and geology ,Earth Science - Abstract
The overarching goal of MSM58 was to gain knowledge about the natural variability of the Subtropical Gyre (STG) and Azores Front (AF) system as well as of changes in the deepwater composition and geometry in the eastern and western North Atlantic Basins, particularly during warm periods and during times of significant warming and ice sheet melting as during the last 25,000 years. For this purpose a sediment and water column sampling program was carried out along the Mid Atlantic Ridge (MAR) from 32�� to 41��N and in four E-W depth transects on the MAR flanks. Prior to sediment sampling with multi corer/box corer and gravity corer, small interridge basins were hydroacoustically mapped using the onboard multibeam swath bathymetry and sediment echosounder systems to identify proper locations for coring sequences of Last Glacial to Holocene sediments with high sedimentation rates. After hydroacoustic surveys, sediment sampling was carried out in 6 working areas at 30 stations between 1300 and 4100m water depth. In total 205 m of sediment were gathered. Water column sampling for plankton and seawater took place at 16 stations. Preliminary sediment inspection indicates that the cores contain the Holocene and up to three glacial-interglacial cycles. As expected, sedimentation rates decrease from North to South and from East to West following the decline in nutrient supply from the subpolar to subtropical North Atlantic. This was also evident in decreasing abundances of planktonic foraminifera and increasing numbers of denitrifying cyanobacteria Trichodesmium in the water column., MARIA S. MERIAN-Berichte
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- 2018
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10. The environmental and evolutionary history of Lake Ohrid (FYROM/Albania): Interim results from the SCOPSCO deep drilling project
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Wagner, B. Wilke, T. Francke, A. Albrecht, C. Baumgarten, H. Bertini, A. Combourieu-Nebout, N. Cvetkoska, A. D'Addabbo, M. Donders, T.H. Föller, K. Giaccio, B. Grazhdani, A. Hauffe, T. Holtvoeth, J. Joannin, S. Jovanovska, E. Just, J. Kouli, K. Koutsodendris, A. Krastel, S. Lacey, J.H. Leicher, N. Leng, M.J. Levkov, Z. Lindhorst, K. Masi, A. Mercuri, A.M. Nomade, S. Nowaczyk, N. Panagiotopoulos, K. Peyron, O. Reed, J.M. Regattieri, E. Sadori, L. Sagnotti, L. Stelbrink, B. Sulpizio, R. Tofilovska, S. Torri, P. Vogel, H. Wagner, T. Wagner-Cremer, F. Wolff, G.A. Wonik, T. Zanchetta, G. Zhang, X.S.
- Abstract
This study reviews and synthesises existing information generated within the SCOPSCO (Scientific Collaboration on Past Speciation Conditions in Lake Ohrid) deep drilling project. The four main aims of the project are to infer (i) the age and origin of Lake Ohrid (Former Yugoslav Republic of Macedonia/Republic of Albania), (ii) its regional seismotectonic history, (iii) volcanic activity and climate change in the central northern Mediterranean region, and (iv) the influence of major geological events on the evolution of its endemic species. The Ohrid basin formed by transtension during the Miocene, opened during the Pliocene and Pleistocene, and the lake established de novo in the still relatively narrow valley between 1.9 and 1.3 Ma. The lake history is recorded in a 584 m long sediment sequence, which was recovered within the framework of the International Continental Scientific Drilling Program (ICDP) from the central part (DEEP site) of the lake in spring 2013. To date, 54 tephra and cryptotephra horizons have been found in the upper 460 m of this sequence. Tephrochronology and tuning biogeochemical proxy data to orbital parameters revealed that the upper 247.8 m represent the last 637 kyr. The multi-proxy data set covering these 637 kyr indicates long-term variability. Some proxies show a change from generally cooler and wetter to drier and warmer glacial and interglacial periods around 300 ka. Short-term environmental change caused, for example, by tephra deposition or the climatic impact of millennial-scale Dansgaard-Oeschger and Heinrich events are superimposed on the long-term trends. Evolutionary studies on the extant fauna indicate that Lake Ohrid was not a refugial area for regional freshwater animals. This differs from the surrounding catchment, where the mountainous setting with relatively high water availability provided a refuge for temperate and montane trees during the relatively cold and dry glacial periods. Although Lake Ohrid experienced significant environmental change over the last 637 kyr, preliminary molecular data from extant microgastropod species do not indicate significant changes in diversification rate during this period. The reasons for this constant rate remain largely unknown, but a possible lack of environmentally induced extinction events in Lake Ohrid and/or the high resilience of the ecosystems may have played a role. © Author(s) 2017.
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- 2017
11. Linear and non-linear responses of vegetation and soils to glacial-interglacial climate change in a Mediterranean refuge
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Holtvoeth, J., Vogel, H., Valsecchi, V., Lindhorst, K., Schouten, S., Wagner, B., Wolff, G.A., Holtvoeth, J., Vogel, H., Valsecchi, V., Lindhorst, K., Schouten, S., Wagner, B., and Wolff, G.A.
- Abstract
The impact of past global climate change on local terrestrial ecosystems and their vegetation and soilorganic matter (OM) pools is often non-linear and poorly constrained. To address this, we investigatedthe response of a temperate habitat influenced by global climate change in a key glacial refuge, LakeOhrid (Albania, Macedonia). We applied independent geochemical and palynological proxies to asedimentary archive from the lake over the penultimate glacial-interglacial transition (MIS 6–5) andthe following interglacial (MIS 5e-c), targeting lake surface temperature as an indicator of regionalclimatic development and the supply of pollen and biomarkers from the vegetation and soil OM poolsto determine local habitat response. Climate fluctuations strongly influenced the ecosystem, however,lake level controls the extent of terrace surfaces between the shoreline and mountain slopes and hencelocal vegetation, soil development and OM export to the lake sediments. There were two phases oftransgressional soil erosion from terrace surfaces during lake-level rise in the MIS 6–5 transition thatled to habitat loss for the locally dominant pine vegetation as the terraces drowned. Our observationsconfirm that catchment morphology plays a key role in providing refuges with low groundwater depthand stable soils during variable climate.
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- 2017
12. Lake level fluctuations and catchment dynamics at Lake Ohrid (Macedonia, Albania) during MIS6 and MIS5
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Francke, A., Wagner, B., Just, J., Sadori, Laura, Masi, Alessia, Vogel, H., Lindhorst, K., Krastel, S., Dosseto, A., Rothacker, L., Leicher, N., and Gromig, R.
- Published
- 2016
13. The SCOPSCO drilling project recovers more than 1.2 million years of history from Lake Ohrid
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Wagner, B., Wilke, T., Krastel, S., Zanchetta, G., Sulpizio, R., Reicherter, K., Leng, M. J., Grazhdani, A., Trajanovski, S., Francke, A., Lindhorst, K., Levkov, Z., Cvetkoska, Aleksandra, Reed, J. M., Zhang, X., Lacey, J. H., Wonik, T., Baumgarten, H., Vogel, H., Palaeo-ecologie, Coastal dynamics, Fluvial systems and Global change, Palaeo-ecologie, and Coastal dynamics, Fluvial systems and Global change
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Environmental change ,Scientific drilling ,Mechanical Engineering ,Energy Engineering and Power Technology ,lcsh:QE1-996.5 ,Logging ,Well logging ,Sediment ,Drilling ,Ecological succession ,15. Life on land ,Coring ,lcsh:Geology ,Paleontology ,Oceanography ,Geology ,550 Earth sciences & geology - Abstract
The Scientific Collaboration on Past Speciation Conditions in Lake Ohrid (SCOPSCO) project is an international research initiative to study the influence of major geological and environmental events on the biological evolution of lake taxa. SCOPSCO drilling campaigns were carried out in 2011 and 2013. In 2011 we used gravity and piston coring at one of the five proposed drill sites, and in 2013 we undertook deep drilling with the Deep Lake Drilling System (DLDS) of Drilling, Observation and Sampling of the Earth's Continental Crust (DOSECC). In April and May 2013, a total of 2100 m sediments were recovered from four drill sites with water depths ranging from 125 to 260 m. The maximum drill depth was 569 m below the lake floor in the centre of the lake. By retrieving overlapping sediment sequences, 95% of the sediment succession was recovered. Initial data from borehole logging, core logging and geochemical measurements indicate that the sediment succession covers >1.2 million years (Ma) in a quasi-continuous sequence. These early findings suggest that the record from Lake Ohrid will substantially improve the knowledge of long-term environmental change and short-term geological events in the northeastern Mediterranean region, which forms the basis for improving understanding of the influence of major geological and environmental events on the biological evolution of endemic species.
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- 2014
14. Reduced-order modelling of non-linear, transient aerodynamics of the HIRENASD wing
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Lindhorst, K., primary, Haupt, M.C., additional, and Horst, P., additional
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- 2016
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15. Fluid-Structure-Interaction in Rocket Thrust Chambers Simulation and Validation
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Haupt, M.C., primary, Kowollik, D., additional, Lindhorst, K., additional, and Hötte, F., additional
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- 2016
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16. Sedimentary and tectonic evolution of Lake Ohrid (Macedonia/Albania)
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Lindhorst, K., Krastel, S., Reicherter, K., Stipp, M., Wagner, B., Schwenk, T., Lindhorst, K., Krastel, S., Reicherter, K., Stipp, M., Wagner, B., and Schwenk, T.
- Abstract
Lake Ohrid, located on the Balkan Peninsula within the Dinaride-Albanide-Hellenide mountain belt, is a tectonically active graben within the South Balkan Extensional Regime (SBER). Interpretation of multichannel seismic cross sections and bathymetric data reveals that Lake Ohrid formed during two main phases of deformation: (1) a transtensional phase which opened a pull-apart basin, and (2) an extensional phase which led to the present geometry of Lake Ohrid. After the initial opening, a symmetrical graben formed during the Late Miocene, bounded by major normal faults on each side in a pull-apart type basin. The early-stage geometry of the basin has a typical rhomboidal shape restricted by two sets of major normal faults. Thick undisturbed sediments are present today at the site where the acoustic basement is deepest, illustrating that Lake Ohrid is a potential target for drilling a long and continuous sediment core for studying environmental changes within the Mediterranean region. Neotectonic activity since the Pliocene takes place along the roughly N-S-striking Eastern and Western Major Boundary Normal Faults that are partly exposed at the present lake floor. The tectono-sedimentary structure of the basin is divided into three main seismic units overlying the acoustic basement associated with fluvial deposits and lacustrine sediments. A seismic facies analysis reveals a prominent cyclic pattern of high- and low-amplitude reflectors. We correlate this facies cyclicity with vegetation changes within the surrounding area that are associated with glacial/interglacial cycles. A clear correlation is possible back to ca. 450kyrs. Extrapolation of average sedimentation rates for the above mentioned period results in age estimate of ca. 2Myrs for the oldest sediments in Lake Ohrid.
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- 2015
17. Neural networks as surrogate models for nonlinear, transient aerodynamics within an aeroelastic coupling-scheme in the time domain
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Lindhorst, K., Matthias Haupt, and Horst, P.
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Finite element method ,Aeroelasticity, Reduced Order Modelling, Neural Networks, NLR7301 ,Elements finits, Mètode dels ,Coupled problems (Complex systems) -- Numerical solutions ,Matemàtiques i estadística::Anàlisi numèrica::Mètodes en elements finits [Àrees temàtiques de la UPC] ,Computer Science::Databases - Abstract
In this paper the creation of a nonlinear, transient surrogate model is described that can be used within an aeroelastic coupling-scheme in the transonic range. The method is based on the theory of artifical neural networks as well as the autoregressive moving average method (ARMA). It can be shown that the method is able to approximate the nonlinear aeroelastic behaviour of the NLR7301 airfoil. Also limit cycle oscillations can be approximated with acceptable accuracy.
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- 2011
18. Aeroelastic Analyses of the High-Reynolds-Number-Aerostructural-Dynamics Configuration Using a Nonlinear Surrogate Model Approach
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Lindhorst, K., primary, Haupt, M. C., additional, and Horst, P., additional
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- 2015
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19. Modeling Submarine Landslide-Generated Waves in Lake Ohrid, Macedonia/Albania
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Lindhorst, K., Krastel, S., Papenberg, C., Heidarzadeh, M., Lindhorst, K., Krastel, S., Papenberg, C., and Heidarzadeh, M.
- Abstract
We study potential tsunami hazards associated with submarine landslides in Lake Ohrid, Macedonia/Albania. The transboundary Lake Ohrid located on the Balkan Peninsula shared by Macedonia and Albania is considered to be the oldest- continuously existing lake in Europe (2–5 Ma), though the age and the origin are not completely unraveled to date. Previous studies by means of hydroacoustic methods have shown that the western margin of Lake Ohrid has a long history of mass wasting. Based on seismic data, slide deposits are found in different stratigraphic levels as well as on the lake floor where they have affected a large area. This study is focused on the well-studied Udenisht Slide Complex covering an area of 27 km2 within the southwestern part of Lake Ohrid. The Udenisht slide is by far the largest mass movement with an average thickness of 30–40 m and an estimated volume of about 0.11 km3. It is therefore well within the limits of submarine landslides that are known to be capable of triggering tsunamis. Using numerical modeling, the propagation of a landslide-generated tsunami with an initial wave height of more than 5 m has been calculated. Run-up heights estimated for coastal communities around the lake are moderate in the north (2–3 m) can reach up to 10 m directly at the site where the slide initiated. This study is a first generation of landslide tsunami hazard assessment for Lake Ohrid and further detailed modeling is recommended for the region.
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- 2014
20. The SCOPSCO drilling project recovers more than 1.2 million years of history from Lake Ohrid
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Palaeo-ecologie, Coastal dynamics, Fluvial systems and Global change, Wagner, B., Wilke, T., Krastel, S., Zanchetta, G., Sulpizio, R., Reicherter, K., Leng, M. J., Grazhdani, A., Trajanovski, S., Francke, A., Lindhorst, K., Levkov, Z., Cvetkoska, Aleksandra, Reed, J. M., Zhang, X., Lacey, J. H., Wonik, T., Baumgarten, H., Vogel, H., Palaeo-ecologie, Coastal dynamics, Fluvial systems and Global change, Wagner, B., Wilke, T., Krastel, S., Zanchetta, G., Sulpizio, R., Reicherter, K., Leng, M. J., Grazhdani, A., Trajanovski, S., Francke, A., Lindhorst, K., Levkov, Z., Cvetkoska, Aleksandra, Reed, J. M., Zhang, X., Lacey, J. H., Wonik, T., Baumgarten, H., and Vogel, H.
- Published
- 2014
21. Efficient Surrogate Modelling of Nonlinear Aerodynamics in Aerostructural Coupling Schemes
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Lindhorst, K., primary, Haupt, M. C., additional, and Horst, P., additional
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- 2014
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22. Sedimentary and tectonic evolution of Lake Ohrid (Macedonia/Albania)
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Lindhorst, K., primary, Krastel, S., additional, Reicherter, K., additional, Stipp, M., additional, Wagner, B., additional, and Schwenk, T., additional
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- 2014
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23. The SCOPSCO drilling project recovers more than 1.2 million years of history from Lake Ohrid
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Wagner, B., primary, Wilke, T., additional, Krastel, S., additional, Zanchetta, G., additional, Sulpizio, R., additional, Reicherter, K., additional, Leng, M. J., additional, Grazhdani, A., additional, Trajanovski, S., additional, Francke, A., additional, Lindhorst, K., additional, Levkov, Z., additional, Cvetkoska, A., additional, Reed, J. M., additional, Zhang, X., additional, Lacey, J. H., additional, Wonik, T., additional, Baumgarten, H., additional, and Vogel, H., additional
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- 2014
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24. Possible earthquake trigger for 6th century mass wasting deposit at Lake Ohrid (Macedonia/Albania)
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Wagner, Bernd, Francke, Alexander, Sulpizio, Roberto, Zanchetta, Giovanni, Lindhorst, K, Krastel, S, Vogel, Hendrik, Rethemeyer, Janet, Daut, G, Grazhdani, A, Lushaj, B, Trajanovski, S, Wagner, Bernd, Francke, Alexander, Sulpizio, Roberto, Zanchetta, Giovanni, Lindhorst, K, Krastel, S, Vogel, Hendrik, Rethemeyer, Janet, Daut, G, Grazhdani, A, Lushaj, B, and Trajanovski, S
- Abstract
Lake Ohrid shared by the Republics of Albania and Macedonia is formed by a tectonically active graben within the south Balkans and suggested to be the oldest lake in Europe. Several studies have shown that the lake provides a valuable record of climatic and environmental changes and a distal tephrostratigraphic record of volcanic eruptions from Italy. Fault structures identified in seismic data demonstrate that sediments have also the potential to record tectonic activity in the region. Here, we provide an example of linking seismic and sedimentological information with tectonic activity and historical documents. Historical documents indicate that a major earthquake destroyed the city of Lychnidus (today: city of Ohrid) in the early 6th century AD. Multichannel seismic profiles, parametric sediment echosounder profiles, and a 10.08 m long sediment record from the western part of the lake indicate a 2 m thick mass wasting deposit, which is tentatively correlated with this earthquake. The mass wasting deposit is chronologically well constrained, as it directly overlays the AD 472/AD 512 tephra. Moreover, radiocarbon dates and cross correlation with other sediment sequences with similar geochemical characteristics of the Holocene indicate that the mass wasting event took place prior to the onset of the Medieval Warm Period, and is attributed it to one of the known earthquakes in the region in the early 6th century AD.
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- 2012
25. Possible earthquake trigger for 6th century mass wasting deposit at Lake Ohrid (Macedonia/Albania)
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Wagner, B., primary, Francke, A., additional, Sulpizio, R., additional, Zanchetta, G., additional, Lindhorst, K., additional, Krastel, S., additional, Vogel, H., additional, Rethemeyer, J., additional, Daut, G., additional, Grazhdani, A., additional, Lushaj, B., additional, and Trajanovski, S., additional
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- 2012
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26. Seismic and sedimentological evidence of an early 6th century AD earthquake at Lake Ohrid (Macedonia/Albania)
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Wagner, B., primary, Francke, A., additional, Sulpizio, R., additional, Zanchetta, G., additional, Lindhorst, K., additional, Krastel, S., additional, Vogel, H., additional, Daut, G., additional, Grazhdani, A., additional, Lushaj, B., additional, and Trajanovski, S., additional
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- 2012
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27. Stratigraphic analysis of lake level fluctuations in Lake Ohrid: an integration of high resolution hydro-acoustic data and sediment cores
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Lindhorst, K., primary, Vogel, H., additional, Krastel, S., additional, Wagner, B., additional, Hilgers, A., additional, Zander, A., additional, Schwenk, T., additional, Wessels, M., additional, and Daut, G., additional
- Published
- 2010
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28. Combination of the material force concept and the extended finite element method for mixed mode crack growth simulations
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Häusler, S. M., primary, Lindhorst, K., additional, and Horst, P., additional
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- 2010
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29. Sedimentary and tectonic evolution of Lake Ohrid ( Macedonia/ Albania).
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Lindhorst, K., Krastel, S., Reicherter, K., Stipp, M., Wagner, B., and Schwenk, T.
- Subjects
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TECTONIC landforms , *NORMAL faults (Geology) , *GLOBAL environmental change , *VEGETATION dynamics , *NEOTECTONICS - Abstract
Lake Ohrid, located on the Balkan Peninsula within the Dinaride- Albanide- Hellenide mountain belt, is a tectonically active graben within the South Balkan Extensional Regime ( SBER). Interpretation of multichannel seismic cross sections and bathymetric data reveals that Lake Ohrid formed during two main phases of deformation: (1) a transtensional phase which opened a pull-apart basin, and (2) an extensional phase which led to the present geometry of Lake Ohrid. After the initial opening, a symmetrical graben formed during the Late Miocene, bounded by major normal faults on each side in a pull-apart type basin. The early-stage geometry of the basin has a typical rhomboidal shape restricted by two sets of major normal faults. Thick undisturbed sediments are present today at the site where the acoustic basement is deepest, illustrating that Lake Ohrid is a potential target for drilling a long and continuous sediment core for studying environmental changes within the Mediterranean region. Neotectonic activity since the Pliocene takes place along the roughly N-S-striking Eastern and Western Major Boundary Normal Faults that are partly exposed at the present lake floor. The tectono-sedimentary structure of the basin is divided into three main seismic units overlying the acoustic basement associated with fluvial deposits and lacustrine sediments. A seismic facies analysis reveals a prominent cyclic pattern of high- and low-amplitude reflectors. We correlate this facies cyclicity with vegetation changes within the surrounding area that are associated with glacial/interglacial cycles. A clear correlation is possible back to ca. 450 kyrs. Extrapolation of average sedimentation rates for the above mentioned period results in age estimate of ca. 2 Myrs for the oldest sediments in Lake Ohrid. [ABSTRACT FROM AUTHOR]
- Published
- 2015
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30. Seismic and sedimentological evidence of an early 6th century AD earthquake at Lake Ohrid (Macedonia/Albania).
- Author
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Wagner, B., Francke, A., Sulpizio, R., Zanchetta, G., Lindhorst, K., Krastel, S., Vogel, H., Daut, G., Grazhdani, A., Lushaj, B., and Trajanovski, S.
- Abstract
Lake Ohrid shared by the Republics of Albania and Macedonia is formed by a tectonically active graben within the South Balkan and suggested to be the oldest lake in Europe. Several studies have shown that the lake provides a valuable record of climatic and environmental changes and a distal tephrostratigraphic record of volcanic eruptions from Italy. Fault structures identified in seismic data demonstrate that sediments have also the potential to record tectonic activity in the region. Here, we provide an example of linking tephrostratigraphic information and environmental changes with tectonic activity and anthropogenic impact. Historical documents indicate that a major earthquake destroyed the city of Ohrid in the early 6th century AD. This earthquake is documented in multichannel seismic profiles, in parametric sediment echosounder profiles, and in a ca. 10m long sediment record from the western part of the lake. The sediment record exhibits a ca. 2m thick mass wasting deposit, which is chronologically well constrained by the underlying 472 AD/512AD tephra and cross correlation with 15 other sediment sequences with similar geochemical characteristics of the Holocene. [ABSTRACT FROM AUTHOR]
- Published
- 2012
- Full Text
- View/download PDF
31. Combination of the material force concept and the extended finite element method for mixed mode crack growth simulations.
- Author
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Häusler, S. M., Lindhorst, K., and Horst, P.
- Published
- 2011
- Full Text
- View/download PDF
32. The environmental and evolutionary history of Lake Ohrid (FYROM/Albania): interim results from the SCOPSCO deep drilling project
- Author
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Wagner-Cremer, F., Torri, P., Lacey, J. H., Stelbrink, B., Baumgarten, H., Föller, K., Mercuri, A. M., Wagner, T., Joannin, S., Zhang, Xi, Cvetkoska, A., Levkov, Z., Wilke, T., Leng, M. J., Kouli, K., Combourieu-Nebout, N., Just, J., Nomade, S., Peyron, O., Giaccio, B., Hauffe, T., Wonik, T., Nowaczyk, N., Wolff, G. A., Bertini, A., Vogel, Hendrik, Regattieri, E., Krastel, S., Wagner, B., Grazhdani, A., Masi, A., Reed, J. M., Tofilovska, S., Francke, A., Sulpizio, R., Leicher, N., Lindhorst, K., Zanchetta, G., Donders, T. H., Sagnotti, L., Koutsodendris, A., Panagiotopoulos, K., Holtvoeth, J., Sadori, L., D'Addabbo, M., Jovanovska, E., and Albrecht, C.
- Subjects
13. Climate action ,550 Earth sciences & geology ,15. Life on land ,580 Plants (Botany) - Abstract
This study reviews and synthesises existing information generated within the SCOPSCO (Scientific Collaboration on Past Speciation Conditions in Lake Ohrid) deep drilling project. The four main aims of the project are to infer (i) the age and origin of Lake Ohrid (Former Yugoslav Republic of Macedonia/Republic of Albania), (ii) its regional seismotectonic history, (iii) volcanic activity and climate change in the central northern Mediterranean region, and (iv) the influence of major geological events on the evolution of its endemic species. The Ohrid basin formed by transtension during the Miocene, opened during the Pliocene and Pleistocene, and the lake established de novo in the still relatively narrow valley between 1.9 and 1.3 Ma. The lake history is recorded in a 584 m long sediment sequence, which was recovered within the framework of the International Continental Scientific Drilling Program (ICDP) from the central part (DEEP site) of the lake in spring 2013. To date, 54 tephra and cryptotephra horizons have been found in the upper 460 m of this sequence. Tephrochronology and tuning biogeochemical proxy data to orbital parameters revealed that the upper 247.8 m represent the last 637 kyr. The multi-proxy data set covering these 637 kyr indicates long-term variability. Some proxies show a change from generally cooler and wetter to drier and warmer glacial and interglacial periods around 300 ka. Short-term environmental change caused, for example, by tephra deposition or the climatic impact of millennial-scale Dansgaard–Oeschger and Heinrich events are superimposed on the long-term trends. Evolutionary studies on the extant fauna indicate that Lake Ohrid was not a refugial area for regional freshwater animals. This differs from the surrounding catchment, where the mountainous setting with relatively high water availability provided a refuge for temperate and montane trees during the relatively cold and dry glacial periods. Although Lake Ohrid experienced significant environmental change over the last 637 kyr, preliminary molecular data from extant microgastropod species do not indicate significant changes in diversification rate during this period. The reasons for this constant rate remain largely unknown, but a possible lack of environmentally induced extinction events in Lake Ohrid and/or the high resilience of the ecosystems may have played a role.
33. Stratigraphic analysis of lake level fluctuations in Lake Ohrid: an integration of high resolution hydro-acoustic data and sediment cores
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Vogel, Hendrik, Schwenk, T., Wagner, B., Wessels, M., Krastel, S., Daut, G., Lindhorst, K., Hilgers, A., and Zander, A.
- Subjects
550 Earth sciences & geology ,14. Life underwater ,15. Life on land - Abstract
Ancient Lake Ohrid is a steep-sided, oligotrophic, karst lake that was tectonically formed most likely within the Pliocene and often referred to as a hotspot of endemic biodiversity. This study aims on tracing significant lake level fluctuations at Lake Ohrid using high-resolution acoustic data in combination with lithological, geochemical, and chronological information from two sediment cores recovered from sub-aquatic terrace levels at ca. 32 and 60m water depth. According to our data, significant lake level fluctuations with prominent lowstands of ca. 60 and 35m below the present water level occurred during Marine Isotope Stage (MIS) 6 and MIS 5, respectively. The effect of these lowstands on biodiversity in most coastal parts of the lake is negligible, due to only small changes in lake surface area, coastline, and habitat. In contrast, biodiversity in shallower areas was more severely affected due to disconnection of today sublacustrine springs from the main water body. Multichannel seismic data from deeper parts of the lake clearly image several clinoform structures stacked on top of each other. These stacked clinoforms indicate significantly lower lake levels prior to MIS 6 and a stepwise rise of water level with intermittent stillstands since its existence as water-filled body, which might have caused enhanced expansion of endemic species within Lake Ohrid.
34. GEM no. 260. Emergency food bags offer more than food.
- Author
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Starkey LJ and Lindhorst K
- Published
- 1996
35. Network Oncolgy Specialist Advisory Service - A Survey of the Psychosocial Situation of Long Term Cancer Survivors During Childhood or Adolescents.
- Author
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Toenne R, Baumeister R, Koch A, Lindhorst K, Reinhardt D, and Kremeike K
- Subjects
- Adolescent, Adult, Consultants, Humans, Surveys and Questionnaires, Young Adult, Cancer Survivors, Neoplasms therapy
- Abstract
Background: The number of long term cancer survivors during childhood or adolescence is increasing steadily. Survivors often suffer from physical or psychosocial long term effects. There is currently little data on the arrangement of long term aftercare in the field of psychosocial care., Methods: In November 2017 a questionnaire was sent to 1900 cancer survivors aged between 18 and 35 years whose diagnosis dated at least five years prior. The obtained data serve as a condition and needs assessment, how the (psychosocial) long-term aftercare is perceived by the survivors and what else is desired. The analysis was conducted using descriptive statistics as well as the calculation of bivariate correlations., Results: The response rate was 54.9% (n=1.043). The median interval from the first diagnosis was 20 years. In total 666 survivors (63.9%) stated that they suffered from at least one long term effect. Within this, especially neurocognitive themes played a role. 87.2% of the respondents had the feeling that they had overcome the illness/therapy well., Conclusion: Through a stronger patient-focussed orientation concerning the current care and advisory services, the situation of long term survivors could be improved. This especially includes access to relevant information that focuses on the available psychosocial and welfare services, as well as to advisory and care services. Additionally, the development and expansion of care structures in the areas of neurocognition and psychotherapy is important to ensure long term participation attendance., Hintergrund: Die Zahl der Langzeitüberlebenden nach einer Krebserkrankung im Kindes- oder Jugendalter (Survivor) steigt stetig. Survivor leiden nicht selten unter körperlichen oder psychosozialen Spätfolgen. Für die Gestaltung der Langzeitnachsorge im Bereich der psychosozialen Versorgung liegen bislang kaum Daten vor., Methode: 11/2017 wurde deutschlandweit ein Fragebogen an 1.900 Survivor im Alter von 18 bis 35 Jahren versandt, deren Erstdiagnose zum Befragungszeitpunkt mindestens fünf Jahre zurücklag. Die erhobenen Daten dienen als Zustands- und Bedarfserhebung, wie die (psychosozialen) Langzeitnachsorge von den Survivorn wahrgenommen und was darüber hinaus gewünscht wird. Die Auswertung erfolgte mittels deskriptiver Statistik sowie der Berechnung bivariater Korrelationen., Ergebnisse: Der Rücklauf betrug 54,9% (n=1.043). Der mediane Abstand zur Erst-Diagnose betrug 20 Jahre. Insgesamt gaben 666 Survivor (63,9%) an, mindestens eines der abgefragten Items/Symptome bei sich zu beobachten. Hierbei spielen besonders neurokognitive Themen eine Rolle. Viele Angebote der Langzeitnachsorge sind den Survivorn nicht bekannt. 87,2% der Befragten haben das Gefühl, die Erkrankung/Therapie gut gemeistert zu haben., Schlussfolgerung: Eine stärkere patientenorientierte Ausrichtung der derzeitigen Versorgungs- und Beratungsangebote könnte die Situation von Langzeitüberlebenden noch verbessern. Zentral sind hierbei der Zugang zu gezielten Informationen, eine psychosoziale und sozialrechtliche Betreuung sowie der Zugang zu Beratungs- und Versorgungsangeboten. Auch der Auf- und Ausbau von Versorgungsstrukturen im Bereich der Neurokognition und Psychotherapie ist für die langfristige Sicherstellung von Partizipation wünschenswert., Competing Interests: The authors declare that they have no conflcit of interest., (Thieme. All rights reserved.)
- Published
- 2022
- Full Text
- View/download PDF
36. Deep drilling reveals massive shifts in evolutionary dynamics after formation of ancient ecosystem.
- Author
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Wilke T, Hauffe T, Jovanovska E, Cvetkoska A, Donders T, Ekschmitt K, Francke A, Lacey JH, Levkov Z, Marshall CR, Neubauer TA, Silvestro D, Stelbrink B, Vogel H, Albrecht C, Holtvoeth J, Krastel S, Leicher N, Leng MJ, Lindhorst K, Masi A, Ognjanova-Rumenova N, Panagiotopoulos K, Reed JM, Sadori L, Tofilovska S, Van Bocxlaer B, Wagner-Cremer F, Wesselingh FP, Wolters V, Zanchetta G, Zhang X, and Wagner B
- Subjects
- Biodiversity, Climate Change, Fossils, Lakes, Biological Evolution, Ecosystem
- Abstract
The scarcity of high-resolution empirical data directly tracking diversity over time limits our understanding of speciation and extinction dynamics and the drivers of rate changes. Here, we analyze a continuous species-level fossil record of endemic diatoms from ancient Lake Ohrid, along with environmental and climate indicator time series since lake formation 1.36 million years (Ma) ago. We show that speciation and extinction rates nearly simultaneously decreased in the environmentally dynamic phase after ecosystem formation and stabilized after deep-water conditions established in Lake Ohrid. As the lake deepens, we also see a switch in the macroevolutionary trade-off, resulting in a transition from a volatile assemblage of short-lived endemic species to a stable community of long-lived species. Our results emphasize the importance of the interplay between environmental/climate change, ecosystem stability, and environmental limits to diversity for diversification processes. The study also provides a new understanding of evolutionary dynamics in long-lived ecosystems., (Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).)
- Published
- 2020
- Full Text
- View/download PDF
37. Mediterranean winter rainfall in phase with African monsoons during the past 1.36 million years.
- Author
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Wagner B, Vogel H, Francke A, Friedrich T, Donders T, Lacey JH, Leng MJ, Regattieri E, Sadori L, Wilke T, Zanchetta G, Albrecht C, Bertini A, Combourieu-Nebout N, Cvetkoska A, Giaccio B, Grazhdani A, Hauffe T, Holtvoeth J, Joannin S, Jovanovska E, Just J, Kouli K, Kousis I, Koutsodendris A, Krastel S, Lagos M, Leicher N, Levkov Z, Lindhorst K, Masi A, Melles M, Mercuri AM, Nomade S, Nowaczyk N, Panagiotopoulos K, Peyron O, Reed JM, Sagnotti L, Sinopoli G, Stelbrink B, Sulpizio R, Timmermann A, Tofilovska S, Torri P, Wagner-Cremer F, Wonik T, and Zhang X
- Subjects
- Africa, Mediterranean Region, Models, Theoretical, Climate, Rain, Seasons
- Abstract
Mediterranean climates are characterized by strong seasonal contrasts between dry summers and wet winters. Changes in winter rainfall are critical for regional socioeconomic development, but are difficult to simulate accurately
1 and reconstruct on Quaternary timescales. This is partly because regional hydroclimate records that cover multiple glacial-interglacial cycles2,3 with different orbital geometries, global ice volume and atmospheric greenhouse gas concentrations are scarce. Moreover, the underlying mechanisms of change and their persistence remain unexplored. Here we show that, over the past 1.36 million years, wet winters in the northcentral Mediterranean tend to occur with high contrasts in local, seasonal insolation and a vigorous African summer monsoon. Our proxy time series from Lake Ohrid on the Balkan Peninsula, together with a 784,000-year transient climate model hindcast, suggest that increased sea surface temperatures amplify local cyclone development and refuel North Atlantic low-pressure systems that enter the Mediterranean during phases of low continental ice volume and high concentrations of atmospheric greenhouse gases. A comparison with modern reanalysis data shows that current drivers of the amount of rainfall in the Mediterranean share some similarities to those that drive the reconstructed increases in precipitation. Our data cover multiple insolation maxima and are therefore an important benchmark for testing climate model performance.- Published
- 2019
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- View/download PDF
38. Reconstructing the sediment concentration of a giant submarine gravity flow.
- Author
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Stevenson CJ, Feldens P, Georgiopoulou A, Schӧnke M, Krastel S, Piper DJW, Lindhorst K, and Mosher D
- Abstract
Submarine gravity flows are responsible for the largest sediment accumulations on the planet, but are notoriously difficult to measure in action. Giant flows transport 100s of km
3 of sediment with run-out distances over 2000 km. Sediment concentration is a first order control on flow dynamics and deposit character. It has never been measured directly nor convincingly estimated in large submarine flows. Here we reconstruct the sediment concentration of a historic giant submarine flow, the 1929 "Grand Banks" event, using two independent approaches, each validated by estimates of flow speed from cable breaks. The calculated average bulk sediment concentration of the flow was 2.7-5.4% by volume. This is orders of magnitude higher than directly-measured smaller-volume flows in river deltas and submarine canyons. The new concentration estimate provides a test case for scaled experiments and numerical simulations, and a major step towards a quantitative understanding of these prodigious flows.- Published
- 2018
- Full Text
- View/download PDF
39. Linear and non-linear responses of vegetation and soils to glacial-interglacial climate change in a Mediterranean refuge.
- Author
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Holtvoeth J, Vogel H, Valsecchi V, Lindhorst K, Schouten S, Wagner B, and Wolff GA
- Abstract
The impact of past global climate change on local terrestrial ecosystems and their vegetation and soil organic matter (OM) pools is often non-linear and poorly constrained. To address this, we investigated the response of a temperate habitat influenced by global climate change in a key glacial refuge, Lake Ohrid (Albania, Macedonia). We applied independent geochemical and palynological proxies to a sedimentary archive from the lake over the penultimate glacial-interglacial transition (MIS 6-5) and the following interglacial (MIS 5e-c), targeting lake surface temperature as an indicator of regional climatic development and the supply of pollen and biomarkers from the vegetation and soil OM pools to determine local habitat response. Climate fluctuations strongly influenced the ecosystem, however, lake level controls the extent of terrace surfaces between the shoreline and mountain slopes and hence local vegetation, soil development and OM export to the lake sediments. There were two phases of transgressional soil erosion from terrace surfaces during lake-level rise in the MIS 6-5 transition that led to habitat loss for the locally dominant pine vegetation as the terraces drowned. Our observations confirm that catchment morphology plays a key role in providing refuges with low groundwater depth and stable soils during variable climate.
- Published
- 2017
- Full Text
- View/download PDF
40. From callus to embryo: a proteomic view on the development and maturation of somatic embryos in Cyclamen persicum.
- Author
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Rode C, Lindhorst K, Braun HP, and Winkelmann T
- Subjects
- Cell Differentiation, Cell Proliferation, Plant Growth Regulators metabolism, Plant Somatic Embryogenesis Techniques, Proteomics, Seeds metabolism, Two-Dimensional Difference Gel Electrophoresis, Abscisic Acid metabolism, Cyclamen embryology, Plant Proteins metabolism, Seeds cytology, Seeds growth & development, Sucrose metabolism
- Abstract
In this study, the proteome structures following the pathway in somatic embryogenesis of Cyclamen persicum were analysed via high-resolution 2D-SDS-PAGE with two objectives: (1) to identify the significant physiological processes during somatic embryogenesis in Cyclamen and (2) to improve the maturation of somatic embryos. Therefore, the effects of maturation-promoting plant growth regulator abscisic acid (ABA) and high sucrose levels on torpedo-shaped embryos were investigated. In total, 108 proteins of differential abundance were identified using a combination of tandem mass spectrometry and a digital proteome reference map. In callus, enzymes related to energy supply were especially distinct, most likely due to energy demand caused by fast growth and cell division. The switch from callus to globular embryo as well as from globular to torpedo-shaped embryo was associated with controlled proteolysis via the ubiquitin-26S proteasome pathway. Storage compound accumulation was first detected 21 days after transfer to plant growth regulator (PGR)-free medium in early torpedo-shaped embryos. Increase in abundance of auxin-amidohydrolase during embryogenesis suggests a possible increase in auxin release in the late embryo stages of Cyclamen. A development-specific isoelectric point switch of catalases has been reported for the first time for somatic embryogenesis. Several proteins were identified to represent markers for the different developmental stages analysed. High sucrose levels and ABA treatment promoted the accumulation of storage compounds in torpedo-shaped embryos. Additionally, proteins of the primary metabolic pathways were decreased in the proteomes of ABA-treated embryos. Thus, ABA and high sucrose concentration in the culture medium improved maturation and consequently the quality of somatic embryos in C. persicum.
- Published
- 2012
- Full Text
- View/download PDF
41. Rural consumers' attitudes towards nutrition labelling.
- Author
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Lindhorst K, Corby L, Roberts S, and Zeiler S
- Subjects
- Adolescent, Adult, Aged, Educational Status, Female, Health Behavior, Humans, Income, Male, Middle Aged, Rural Population, Surveys and Questionnaires, Attitude to Health, Food Labeling, Health Knowledge, Attitudes, Practice
- Abstract
Purpose: Consumer workshops in rural and remote locations were evaluated for their efficacy in changing participants' self-perceived attitudes and behaviours related to nutrition labelling., Methods: Project-trained community health educators used pilot-tested workshop resources to facilitate 18 workshops across the country. Participants completed pre-workshop questionnaires to permit the identification of demographic characteristics and attitudes and behaviours related to nutrition labelling at point-of-purchase., Results: The majority of the 259 consumers who submitted questionnaires were women (81%), and aged 35 to 54 (35%); 51% reported more than a high school education and 34% had less than $25,000 as a yearly family income. Self-perceived attitudes and behaviours related to nutrition labelling differed only slightly by family income before the workshop. Workshops were rated positively (mode=4 [range 2 to 5]). Thirty-five consumers were surveyed three months after the workshop; the majority were women (89%), were aged 35 to 54 (43%), and had completed high school (51%). Self-perceived attitudes and behaviours for all respondents (n=35) had improved. Use of acquired knowledge and skills at point-of-purchase was high for all respondents (mode=4 [range 2 to 5]; five-point Likert scale)., Conclusions: Providing in-person consumer workshops with pilot-tested materials in rural and remote locations had positive impacts on attitudes and behaviours related to the use of nutrition labelling.
- Published
- 2007
- Full Text
- View/download PDF
42. [Radiation sensitivity of malignant tumors following pretreatment with photosensitizing tetracycline].
- Author
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Dell M, Klemm J, Lindhorst K, and Schlegel D
- Subjects
- Animals, Fluorescence, Photosensitivity Disorders, Radiation-Sensitizing Agents, Rats, Ultraviolet Rays, Sarcoma, Yoshida radiotherapy, Tetracycline pharmacology
- Published
- 1970
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