ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Other Sources  (367)
Collection
Language
  • 11
    Publication Date: 2024-03-18
    Description: Various environmental variables drive gross primary productivity (GPP) and light use efficiency (LUE) of forest ecosystems. However, due to their intertwined nature and the complexity of measuring absorbed photosynthetically active radiation (APAR) of forest canopies, the assessment of LUE and the importance of its environmental drivers are difficult. Here, we present a unique combination of measurements during the 2021 growing season including eddy covariance derived GPP, sap flow, Sentinel‐2 derived canopy chlorophyll content and in situ measured APAR. The importance of environmental variables for GPP models is quantified with state‐of‐the‐art machine learning techniques. A special focus is put on photosynthesis‐limiting conditions, which are identified by a comparison of GPP and sap flow hysteretic responses to Vapor pressure deficit (VPD) and APAR. Results demonstrate that (a) LUE of the canopy's green part was on average 4.0% ± 2.3%, (b) canopy chlorophyll content as a seasonal variable for photosynthetic capacity was important for GPP predictions, and (c) on days with high VPD, tree‐scale sap flow and ecosystem‐scale GPP both shift to a clockwise hysteretic response to APAR. We demonstrate that the onset of such a clockwise hysteretic pattern of sap flow to APAR is a good indicator of stomatal closure related to water‐limiting conditions at the ecosystem‐scale.
    Description: Plain Language Summary: The efficiency by which a forest uses sunlight to perform photosynthesis is an important feature for climate and ecosystem modeling. However, the light that is actually captured by forests and is useable for photosynthesis is difficult to assess. Here, we show a sophisticated approach to estimate the light use efficiency of a spruce forest in Germany and analyze environmental influences on it and on photosynthesis. Our results indicate that about 4% of the light useable for photosynthesis was actually used by the forest during the 2021 growing season and that seasonal variations of chlorophyll in the canopy are a good indicator for carbon capture.
    Description: Key Points: A seasonal variable such as canopy chlorophyll content was useful to predict gross primary productivity with machine learning models. A clockwise hysteretic pattern of sap flow to radiation is a good indicator of water‐related stomatal closure. The light use efficiency of green parts of a spruce forest was 4.0% with a standard deviation of 2.3% during the 2021 growing season.
    Description: RWTH Aachen University http://dx.doi.org/10.13039/501100007210
    Description: University of Alberta http://dx.doi.org/10.13039/501100000190
    Description: Excellence Strategy of the Federal Government and the Länder
    Description: Waldklimafonds http://dx.doi.org/10.13039/501100010297
    Description: German Federal Ministry of Food and Agriculture
    Description: German Federal Ministry for the Environment, Nature Conservation, Nuclear Safety and Consumer Protection
    Description: TERENO project
    Description: Helmholtz research infrastructure Modular Observation Solutions for Earth Systems
    Description: http://doi.org/10.5281/zenodo.7014604
    Description: https://www.opengeodata.nrw.de/produkte/geobasis/hm/3dm_l_las/3dm_l_las/
    Description: https://scihub.copernicus.eu/
    Keywords: ddc:634.9 ; photosynthetically active radiation ; canopy chlorophyll content ; hysteresis ; sap flow ; variable importance ; Picea abies
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 12
    facet.materialart.
    Unknown
    American Chemistry Society
    In:  Environmental Science & Technology, 48 (16). pp. 9037-9042.
    Publication Date: 2017-05-24
    Description: Sunscreens have been shown to give the most effective protection for human skin from ultraviolet (UV) radiation. Chemicals from sunscreens (i.e., UV filters) accumulate in the sea and have toxic effects on marine organisms. In this report, we demonstrate that photoexcitation of inorganic UV filters (i.e., TiO2 and ZnO nanoparticles) under solar radiation produces significant amounts of hydrogen peroxide (H2O2), a strong oxidizing agent that generates high levels of stress on marine phytoplankton. Our results indicate that the inorganic oxide nanoparticle content in 1 g of commercial sunscreen produces rates of H2O2 in seawater of up to 463 nM/h, directly affecting the growth of phytoplankton. Conservative estimates for a Mediterranean beach reveal that tourism activities during a summer day may release on the order of 4 kg of TiO2 nanoparticles to the water and produce an increment in the concentration of H2O2 of 270 nM/day. Our results, together with the data provided by tourism records in the Mediterranean, point to TiO2 nanoparticles as the major oxidizing agent entering coastal waters, with direct ecological consequences on the ecosystem.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 13
    Publication Date: 2022-01-31
    Description: The Mediterranean community represented in this paper is the result of more than 30 years of EU and nationally funded coordination, which has led to key contributions in science concepts and operational initiatives. Together with the establishment of operational services, the community has coordinated with universities, research centers, research infrastructures and private companies to implement advanced multi-platform and integrated observing and forecasting systems that facilitate the advancement of operational services, scientific achievements and mission-oriented innovation. Thus, the community can respond to societal challenges and stakeholders needs, developing a variety of fit-for-purpose services such as the Copernicus Marine Service. The combination of state-of-the-art observations and forecasting provides new opportunities for downstream services in response to the needs of the heavily populated Mediterranean coastal areas and to climate change. The challenge over the next decade is to sustain ocean observations within the research community, to monitor the variability at small scales, e.g., the mesoscale/submesoscale, to resolve the sub-basin/seasonal and inter-annual variability in the circulation, and thus establish the decadal variability, understand and correct the model-associated biases and to enhance model-data integration and ensemble forecasting for uncertainty estimation. Better knowledge and understanding of the level of Mediterranean variability will enable a subsequent evaluation of the impacts and mitigation of the effect of human activities and climate change on the biodiversity and the ecosystem, which will support environmental assessments and decisions. Further challenges include extending the science-based added-value products into societal relevant downstream services and engaging with communities to build initiatives that will contribute to the 2030 Agenda and more specifically to SDG14 and the UN's Decade of Ocean Science for sustainable development, by this contributing to bridge the science-policy gap. The Mediterranean observing and forecasting capacity was built on the basis of community best practices in monitoring and modeling, and can serve as a basis for the development of an integrated global ocean observing system.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 14
  • 15
    Publication Date: 2024-02-07
    Description: The use of cephalopod beaks in ecological and population dynamics studies has allowed major advances of our knowledge on the role of cephalopods in marine ecosystems in the last 60 years. Since the 1960’s, with the pioneering research by Malcolm Clarke and colleagues, cephalopod beaks (also named jaws or mandibles) have been described to species level and their measurements have been shown to be related to cephalopod body size and mass, which permitted important information to be obtained on numerous biological and ecological aspects of cephalopods in marine ecosystems. In the last decade, a range of new techniques has been applied to cephalopod beaks, permitting new kinds of insight into cephalopod biology and ecology. The workshop on cephalopod beaks of the Cephalopod International Advisory Council Conference (Sesimbra, Portugal) in 2022 aimed to review the most recent scientific developments in this field and to identify future challenges, particularly in relation to taxonomy, age, growth, chemical composition (i.e., DNA, proteomics, stable isotopes, trace elements) and physical (i.e., structural) analyses. In terms of taxonomy, new techniques (e.g., 3D geometric morphometrics) for identifying cephalopods from their beaks are being developed with promising results, although the need for experts and reference collections of cephalopod beaks will continue. The use of beak microstructure for age and growth studies has been validated. Stable isotope analyses on beaks have proven to be an excellent technique to get valuable information on the ecology of cephalopods (namely habitat and trophic position). Trace element analyses is also possible using beaks, where concentrations are significantly lower than in other tissues (e.g., muscle, digestive gland, gills). Extracting DNA from beaks was only possible in one study so far. Protein analyses can also be made using cephalopod beaks. Future challenges in research using cephalopod beaks are also discussed.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 16
    Publication Date: 2023-07-18
    Description: This paper presents the main messages of a South American expert roundtable (ERT) on the unintended side effects (unseens) of digital transformation. The input of the ERT comprised 39 propositions from 20 experts representing 11 different perspectives. The two-day ERT discussed the main drivers and challenges as well as vulnerabilities or unseens and provided suggestions for: (i) the mechanisms underlying major unseens; (ii) understanding possible ways in which rebound effects of digital transformation may become the subject of overarching research in three main categories of impact: development factors, society, and individuals; and (iii) a set of potential action domains for transdisciplinary follow-up processes, including a case study in Brazil. A content analysis of the propositions and related mechanisms provided insights in the genesis of unseens by identifying 15 interrelated causal mechanisms related to critical issues/concerns. Additionally, a cluster analysis (CLA) was applied to structure the challenges and critical developments in South America. The discussion elaborated the genesis, dynamics, and impacts of (groups of) unseens such as the digital divide (that affects most countries that are not included in the development of digital business, management, production, etc. tools) or the challenge of restructuring small- and medium-sized enterprises (whose service is digitally substituted by digital devices). We identify specific issues and effects (for most South American countries) such as lack of governmental structure, challenging geographical structures (e.g., inclusion in high-performance transmission power), or the digital readiness of (wide parts) of society. One scientific contribution of the paper is related to the presented methodology that provides insights into the phenomena, the causal chains underlying “wanted/positive” and “unwanted/negative” effects, and the processes and mechanisms of societal changes caused by digitalization.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 17
    Publication Date: 2021-03-29
    Description: Dada la importancia que revisten los suelos en los procesos que ocurren en la zona crítica (zona de interacción entre agua, suelo, aire, organismos), en este trabajo presentamos la distribución temporal y espacial de una secuencia de paleosuelos arcillosos con carbonatos secundarios (capas de caliches y carbonatos diseminados) en el sector nororiental de la Cuenca de México, particularmente en el valle de Teotihuacán. El propósito de este trabajo consiste en reconstruir la distribución temporal y espacial de la cubierta de suelos del pasado para entender su relación con la estructura actual de suelos y sedimentos en este sector semiárido de la cuenca de México. Con esta información, determinar la participación de estos materiales en la Zona Crítica (ZC). Para ello, se ha llevado a cabo un transecto de dirección norte-sur, que inicia en las elevaciones del Cerro Gordo, cruza el valle de Teotihuacán y termina en la Sierra Patlachique, describiendo perfiles de suelo en diferentes posiciones geomorfológicas. El marco cronológico se ha establecido con base en fechamientos de radiocarbono realizados en las capas de caliches. De acuerdo a la cronología, al tipo y grado de pedogénesis, y a los procesos de sedimentación, se han reconocido cuatro unidades. La primera unidad, denominada Paleosuelos del Pleistoceno, fase I (50000 – 20000 años AP), está compuesta de paleosuelos arcillosos, los cuales son Luvisoles crómicos y estágnicos, dependiendo de su posición en el paisaje. Estos paleosuelos muestran tanto carbonatos secundarios diseminados y en fracturas, como capas de caliches. En la segunda unidad, Paleosuelos del Pleistoceno, fase II (20000 –10000 años AP), dominan los sedimentos sobre los suelos; únicamente en el fondo del Valle, se han encontrado Gleysoles cortados por canales aluviales. La unidad, Paleosuelos del Holoceno, fase I (10000 a 1000 años AP) se caracteriza por presentar suelos poligenéticos (Vertisoles), fuertemente modificados por los procesos antrópicos, durante las diversas fases de ocupación pre-hispánica. La última unidad, Suelos del Holoceno, fase II, abarca el último milenio, en donde se destacan procesos de erosión e inestabilidad del paisaje. La tendencia principal en la distribución espacial de los paleosuelos es la siguiente: las unidades antiguas (Luvisoles, capas de caliches y Vertisoles) están sepultadas profundamente en el fondo del valle. Sin embargo, en los taludes y elevaciones montañosas, pueden aparecer cerca o directamente sobre la superficie, siendo incorporados en el manto de suelos actual. Las interrelaciones entre los diferentes paleosuelos a lo largo del transecto estudiado, junto con las observaciones micromorfológicas, apoyan la hipótesis de una relación evolutiva entre los Luvisoles pleistocénicos y los Vertisoles del Holoceno. Consideramos que estas diferentes unidades repercuten en los procesos hidrológicos en el valle y que las capas de caliche formadas en los ambientes pleistocénicos pueden afectar la geoquímica del agua subterránea así como sus firmas isotópicas.
    Description: As soils are important elements for the processes involved in the critical zone (the zone of interaction between water, soil, air, and organisms), in this work we present the temporal and spatial distribution of a clayey-paleosol sequence with secondary carbonates (layers of caliche and disseminated carbonates) in the northeast sector of the Mexico Basin, particularly in the Teotihuacan Valley. The goal of this paper is the temporal and spatial reconstruction of the past soil cover to understand its relationship with the present day soils and sediments in this semiarid sector of the Mexico Basin. With this information the involvement of these materials in the critical zone could be determined. To comply with these objectives, a north-south transect was carried out, starting in the Cerro Gordo, crossing the Teotihuacan valley and ending in the Sierra Patlachique, describing soil profiles located in different geomorphological positions. The chronological framework has been established with radiocarbon dates of the caliche layers. According to this chronology, the type and degree of pedogenesis, as well as the sedimentation processes, four units have been recognized. The first unit is named the Pleistocene Paleosols, phase I (50000 – 20000 years BP), and is composed of clayey paleosols, chromic and stagnic Luvisols, depending on their position in the landscape. These paleosols contain pedogenic carbonates, disseminated and in fractures, and caliche layers. In the second unit, the Pleistocene Paleosols, phase II (20000 –10000 years BP), sediments predominate over soils; only in the valley floor some Gleysols are found to be cut by alluvial channels. The unit, Paleosols of the Holocene Paleosols unit, phase I (10000 to 1000 years BP), is characterized by polygenetic soils (Vertisols) strongly modified by anthropic processes during distinct phases of pre-hispanic occupation. The last unit, the Holocene Soils, phase II, covers the last millennium when erosional processes and unstable landscape dominate. The paleosols (Luvisols, caliche layers, and Vertisols) are deeply buried at the bottom of the valley. However, on the slopes and hilltop positions, they can appear close to or directly on the surface, being incorporated in the present day soil mantle. Spatial interrelations of different paleosols along the studied transect together with micromorphological observations support the hypothesis of an evolutionary link between the Pleistocene Luvisols and the Holocene Vertisols. We propose that these different units are involved in the hydrological processes in the valley and that the caliche layers, formed in the Pleistocene environments, can affect the geochemistry of the groundwater as well as its isotopic signatures.
    Keywords: paleosuelos; Teotihuacán; caliches; Luvisoles; Vertisoles; cuenca de México; paleosols; Teotihuacan; caliches; Luvisols; Vertisols; Basin of Mexico ; 551
    Language: Spanish
    Type: article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 18
    Publication Date: 2021-06-26
    Description: The high‐precision X‐ray diffraction setup for work with diamond anvil cells (DACs) in interaction chamber 2 (IC2) of the High Energy Density instrument of the European X‐ray Free‐Electron Laser is described. This includes beamline optics, sample positioning and detector systems located in the multipurpose vacuum chamber. Concepts for pump–probe X‐ray diffraction experiments in the DAC are described and their implementation demonstrated during the First User Community Assisted Commissioning experiment. X‐ray heating and diffraction of Bi under pressure, obtained using 20 fs X‐ray pulses at 17.8 keV and 2.2 MHz repetition, is illustrated through splitting of diffraction peaks, and interpreted employing finite element modeling of the sample chamber in the DAC.
    Description: The high‐precision X‐ray diffraction (XRD) setup for work with diamond anvil cells (DACs) in Interaction Chamber 2 of the High Energy Density (HED) instrument of the European X‐ray Free‐Electron Laser is described. image
    Keywords: 548 ; diamond anvil cells ; X‐ray free‐electron lasers ; high‐precision X‐ray diffraction ; finite element modeling
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 19
    Publication Date: 2021-07-21
    Description: Coastal vegetated habitats like seagrass meadows can mitigate anthropogenic carbon emissions by sequestering CO2 as “blue carbon” (BC). Already, some coastal ecosystems are actively managed to enhance BC storage, with associated BC stocks included in national greenhouse gas inventories. However, the extent to which BC burial fluxes are enhanced or counteracted by other carbon fluxes, especially air‐water CO2 flux (FCO2) remains poorly understood. In this study, we synthesized all available direct FCO2 measurements over seagrass meadows made using atmospheric Eddy Covariance, across a globally representative range of ecotypes. Of the four sites with seasonal data coverage, two were net CO2 sources, with average FCO2 equivalent to 44%–115% of the global average BC burial rate. At the remaining sites, net CO2 uptake was 101%–888% of average BC burial. A wavelet coherence analysis demonstrated that FCO2 was most strongly related to physical factors like temperature, wind, and tides. In particular, tidal forcing was a key driver of global‐scale patterns in FCO2, likely due to a combination of lateral carbon exchange, bottom‐driven turbulence, and pore‐water pumping. Lastly, sea‐surface drag coefficients were always greater than the prediction for the open ocean, supporting a universal enhancement of gas‐transfer in shallow coastal waters. Our study points to the need for a more comprehensive approach to BC assessments, considering not only organic carbon storage, but also air‐water CO2 exchange, and its complex biogeochemical and physical drivers.
    Description: Plain Language Summary: Carbon storage is a valuable ecosystem service of seagrass meadows, serving as a possible pathway to draw down atmospheric carbon dioxide (CO2) levels. However, this approach may be unsuccessful if carbon storage in sediments is exceeded by the release of CO2 from the water. To better understand the scope of this problem, we compiled all available measurements of air‐water CO2 exchange over seagrass meadows. We found that rates of CO2 release or uptake were indeed large, even when compared with potential rates of carbon storage in seagrass soils. However, these large air‐water exchanges of CO2 did not occur for the same reason everywhere. While light availability was sometimes a strong predictor of air‐water CO2 exchange, tidal mixing and temperature were also very important, revealing a much more complex network of drivers than previously thought. Despite these diverse conditions, we found one key similarity across all sites, in that rates of air‐water gas transfer appear to always be greater than would be expected for the open ocean. Taken together, the results of our study show that assessments of carbon storage in coastal seagrass ecosystems will be incomplete if they do not consider exchanges of CO2 between the water and air.
    Description: Key Points: Direct measurements show that air‐water CO2 exchange over seagrass meadows is of similar magnitude to carbon burial rates. Key drivers are tides, temperature, light, and wind, which off in importance over hourly seasonal time scales. Surface drag coefficients were greater than open water prediction, suggesting a near‐universal gas transfer enhancement across all sites.
    Description: Bundesministerium für Bildung und Forschung (BMBF) http://dx.doi.org/10.13039/501100002347
    Description: Florida Coastal Everglades LTER
    Description: Consejo Nacional de Ciencia y Tecnología (CONACYT) http://dx.doi.org/10.13039/501100003141
    Description: MEXT, Japan Society for the Promotion of Science (JSPS) http://dx.doi.org/10.13039/501100001691
    Description: Ethicon Endo‐Surgery http://dx.doi.org/10.13039/100005566
    Description: Deutscher Akademischer Austauschdienst http://dx.doi.org/10.13039/501100001655
    Description: National Science Foundation http://dx.doi.org/10.13039/100000001
    Description: Vetenskapsrådet http://dx.doi.org/10.13039/501100004359
    Description: Uppsala Universitet http://dx.doi.org/10.13039/501100007051
    Description: Agence Nationale de la Recherche http://dx.doi.org/10.13039/501100001665
    Description: Université de Bordeaux http://dx.doi.org/10.13039/501100006251
    Description: Institut National de la Recherche Agronomique http://dx.doi.org/10.13039/501100006488
    Keywords: 577.144 ; Seagrass ; Blue Carbon ; CO2 Flux ; Eddy Covariance ; Carbon Cycle ; Air‐sea interaction
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 20
    facet.materialart.
    Unknown
    In:  Geophys. J. Int., Stuttgart, Pergamon, vol. 129, no. B8, pp. 571-578, pp. 2316, (ISSN: 1340-4202)
    Publication Date: 1997
    Keywords: Three dimensional ; Body waves ; Rayleigh waves ; P-waves ; Shear waves ; Diffraction ; GJI ; Sanchez ; Rodriguez ; Zuniga ; Luzon ; Garcia ; Martin
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...