TY - JOUR A1 - Wagner, Nicole D. A1 - Hillebrand, Helmut A1 - Wacker, Alexander A1 - Frost, Paul C. T1 - Nutritional indicators and their uses in ecology JF - Ecology letters N2 - The nutrition of animal consumers is an important regulator of ecological processes due to its effects on their physiology, life-history and behaviour. Understanding the ecological effects of poor nutrition depends on correctly diagnosing the nature and strength of nutritional limitation. Despite the need to assess nutritional limitation, current approaches to delineating nutritional constraints can be non-specific and imprecise. Here, we consider the need and potential to develop new complementary approaches to the study of nutritional constraints on animal consumers by studying and using a suite of established and emerging biochemical and molecular responses. These nutritional indicators include gene expression, transcript regulators, protein profiling and activity, and gross biochemical and elemental composition. The potential applications of nutritional indicators to ecological studies are highlighted to demonstrate the value that this approach would have to future studies in community and ecosystem ecology. KW - Ecological stoichiometry KW - lipid profiling KW - metabolism KW - nutrient-stress KW - nutrition KW - proteomics KW - transcriptomics Y1 - 2013 U6 - https://doi.org/10.1111/ele.12067 SN - 1461-023X VL - 16 IS - 4 SP - 535 EP - 544 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Mechie, James A1 - Ben-Avraham, Zvi A1 - Weber, Michael H. A1 - Götze, Hans-Jürgen A1 - Koulakov, Ivan A1 - Mohsen, A. A1 - Stiller, M. T1 - The distribution of Moho depths beneath the Arabian plate and margins JF - TECTONOPHYSICS N2 - In this study three new maps of Moho depths beneath the Arabian plate and margins are presented. The first map is based on the combined gravity model, EIGEN 06C, which includes data from satellite missions and ground-based studies, and thus covers the whole region between 31 degrees E and 60 inverted perpendicular E and between 12 degrees N and 36 degrees N. The second map is based on seismological and ground-based gravity data while the third map is based only on seismological data. Both these maps show gaps due to lack of data coverage especially in the interior of the Arabian plate. Beneath the interior of the Arabian plate the Moho lies between 32 and 45 km depth below sea level. There is a tendency for higher Pn and Sn velocities beneath the northeastern parts of the plate interior with respect to the southwestern parts of the plate interior. Across the northern, destructive margin with the Eurasian plate, the Moho depths increase to over 50 km beneath the Zagros mountains. Across the conservative western margin, the Dead Sea Transform (DST). Moho depths decrease from almost 40 km beneath the highlands east of the DST to about 21-23 km under the southeastern Mediterranean Sea. This decrease seems to be modulated by a slight depression in the Moho beneath the southern DST. The constructive southwestern and southeastern margins of the Arabian plate also show the Moho shallowing from the plate interior towards the plate boundaries. A comparison of the abruptness of the Moho shallowing between the margins of the Arabian plate, the conjugate African margin at 26 degrees N and several Atlantic margins shows a complex picture and suggests that the abruptness of the Moho shallowing may reflect fundamental differences in the original structure of the margins. (C) 2012 Elsevier B.V. All rights reserved. KW - Moho depths KW - Arabian plate KW - Red Sea KW - Velocity models KW - Receiver functions KW - Satellite gravity data Y1 - 2013 U6 - https://doi.org/10.1016/j.tecto.2012.11.015 SN - 0040-1951 SN - 1879-3266 VL - 609 SP - 234 EP - 249 PB - ELSEVIER SCIENCE BV CY - AMSTERDAM ER - TY - JOUR A1 - Ast, Sandra A1 - Fischer, Tobias A1 - Müller, Holger A1 - Mickler, Wulfhard A1 - Schwichtenberg, Mathias A1 - Rurack, Knut A1 - Holdt, Hans-Jürgen T1 - Integration of the 1,2,3-Triazole "Click" Motif as a potent signalling element in metal ion responsive fluorescent probes JF - Chemistry - a European journal N2 - In a systematic approach we synthesized a new series of fluorescent probes incorporating donoracceptor (D-A) substituted 1,2,3-triazoles as conjugative -linkers between the alkali metal ion receptor N-phenylaza-[18]crown-6 and different fluorophoric groups with different electron-acceptor properties (4-naphthalimide, meso-phenyl-BODIPY and 9-anthracene) and investigated their performance in organic and aqueous environments (physiological conditions). In the charge-transfer (CT) type probes 1, 2 and 7, the fluorescence is almost completely quenched by intramolecular CT (ICT) processes involving charge-separated states. In the presence of Na+ and K+ ICT is interrupted, which resulted in a lighting-up of the fluorescence in acetonitrile. Among the investigated fluoroionophores, compound 7, which contains a 9-anthracenyl moiety as the electron-accepting fluorophore, is the only probe which retains light-up features in water and works as a highly K+/Na+-selective probe under simulated physiological conditions. Virtually decoupled BODIPY-based 6 and photoinduced electron transfer (PET) type probes 35, where the 10-substituted anthracen-9-yl fluorophores are connected to the 1,2,3-triazole through a methylene spacer, show strong ion-induced fluorescence enhancement in acetonitrile, but not under physiological conditions. Electrochemical studies and theoretical calculations were used to assess and support the underlying mechanisms for the new ICT and PET 1,2,3-triazole fluoroionophores. KW - charge transfer KW - click chemistry KW - electron transfer KW - fluorescent probes KW - metal ions Y1 - 2013 U6 - https://doi.org/10.1002/chem.201201575 SN - 0947-6539 VL - 19 IS - 9 SP - 2990 EP - 3005 PB - Wiley-VCH CY - Weinheim ER - TY - JOUR A1 - Sibly, Richard M. A1 - Grimm, Volker A1 - Martin, Benjamin T. A1 - Johnston, Alice S. A. A1 - Kulakowska, Katarzyna A1 - Topping, Christopher J. A1 - Calow, Peter A1 - Nabe-Nielsen, Jacob A1 - Thorbek, Pernille A1 - DeAngelis, Donald L. T1 - Representing the acquisition and use of energy by individuals in agent-based models of animal populations JF - Methods in ecology and evolution : an official journal of the British Ecological Society N2 - Agent-based models (ABMs) are widely used to predict how populations respond to changing environments. As the availability of food varies in space and time, individuals should have their own energy budgets, but there is no consensus as to how these should be modelled. Here, we use knowledge of physiological ecology to identify major issues confronting the modeller and to make recommendations about how energy budgets for use in ABMs should be constructed. Our proposal is that modelled animals forage as necessary to supply their energy needs for maintenance, growth and reproduction. If there is sufficient energy intake, an animal allocates the energy obtained in the order: maintenance, growth, reproduction, energy storage, until its energy stores reach an optimal level. If there is a shortfall, the priorities for maintenance and growth/reproduction remain the same until reserves fall to a critical threshold below which all are allocated to maintenance. Rates of ingestion and allocation depend on body mass and temperature. We make suggestions for how each of these processes should be modelled mathematically. Mortality rates vary with body mass and temperature according to known relationships, and these can be used to obtain estimates of background mortality rate. If parameter values cannot be obtained directly, then values may provisionally be obtained by parameter borrowing, pattern-oriented modelling, artificial evolution or from allometric equations. The development of ABMs incorporating individual energy budgets is essential for realistic modelling of populations affected by food availability. Such ABMs are already being used to guide conservation planning of nature reserves and shell fisheries, to assess environmental impacts of building proposals including wind farms and highways and to assess the effects on nontarget organisms of chemicals for the control of agricultural pests. KW - bioenergetics KW - energy budget KW - individual-based models KW - population dynamics Y1 - 2013 U6 - https://doi.org/10.1111/2041-210x.12002 SN - 2041-210X VL - 4 IS - 2 SP - 151 EP - 161 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Sorge, Arndt T1 - Disintegrating Democracy at Work: Labor Unions and the Future of Good Jobs in the Service Economy JF - British journal of industrial relations : an international journal of employment relations Y1 - 2013 U6 - https://doi.org/10.1177/0094306113514539i SN - 0007-1080 VL - 51 IS - 1 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Sodoudi, Forough A1 - Yuan, Xiaohui A1 - Kind, Rainer A1 - Lebedev, Sergei A1 - Adam, Joanne M-C. A1 - Kästle, Emanuel A1 - Tilmann, Frederik T1 - Seismic evidence for stratification in composition and anisotropic fabric within the thick lithosphere of Kalahari Craton JF - Geochemistry, geophysics, geosystems N2 - Based on joint consideration of S receiver functions and surface-wave anisotropy we present evidence for the existence of a thick and layered lithosphere beneath the Kalahari Craton. Our results show that frozen-in anisotropy and compositional changes can generate sharp Mid-Lithospheric Discontinuities (MLD) at depths of 85 and 150-200 km, respectively. We found that a 50 km thick anisotropic layer, containing 3% S wave anisotropy and with a fast-velocity axis different from that in the layer beneath, can account for the first MLD at about 85 km depth. Significant correlation between the depths of an apparent boundary separating the depleted and metasomatised lithosphere, as inferred from chemical tomography, and those of our second MLD led us to characterize it as a compositional boundary, most likely due to the modification of the cratonic mantle lithosphere by magma infiltration. The deepening of this boundary from 150 to 200 km is spatially correlated with the surficial expression of the Thabazimbi-Murchison Lineament (TML), implying that the TML isolates the lithosphere of the Limpopo terrane from that of the ancient Kaapvaal terrane. The largest velocity contrast (3.6-4.7%) is observed at a boundary located at depths of 260-280 km beneath the Archean domains and the older Proterozoic belt. This boundary most likely represents the lithosphere-asthenosphere boundary, which shallows to about 200 km beneath the younger Proterozoic belt. Thus, the Kalahari lithosphere may have survived multiple episodes of intense magmatism and collisional rifting during the billions of years of its history, which left their imprint in its internal layering. KW - lithospheric layering KW - S receiver functions Y1 - 2013 U6 - https://doi.org/10.1002/2013GC004955 SN - 1525-2027 VL - 14 IS - 12 SP - 5393 EP - 5412 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Scheiner, Ricarda A1 - Abramson, Charles I. A1 - Brodschneider, Robert A1 - Crailsheim, Karl A1 - Farina, Walter M. A1 - Fuchs, Stefan A1 - Grünewald, Bernd A1 - Hahshold, Sybille A1 - Karrer, Marlene A1 - Koeniger, Gudrun A1 - Königer, Niko A1 - Menzel, Randolf A1 - Mujagic, Samir A1 - Radspieler, Gerald A1 - Schmickl, Thomas A1 - Schneider, Christof A1 - Siegel, Adam J. A1 - Szopek, Martina A1 - Thenius, Ronald T1 - Standard methods for behavioural studies of Apis mellifera JF - Journal of apicultural research N2 - In this BEEBOOK paper we present a set of established methods for quantifying honey bee behaviour. We start with general methods for preparing bees for behavioural assays. Then we introduce assays for quantifying sensory responsiveness to gustatory, visual and olfactory stimuli. Presentation of more complex behaviours like appetitive and aversive learning under controlled laboratory conditions and learning paradigms under free-flying conditions will allow the reader to investigate a large range of cognitive skills in honey bees. Honey bees are very sensitive to changing temperatures. We therefore present experiments which aim at analysing honey bee locomotion in temperature gradients. The complex flight behaviour of honey bees can be investigated under controlled conditions in the laboratory or with sophisticated technologies like harmonic radar or RFID in the field. These methods will be explained in detail in different sections. Honey bees are model organisms in behavioural biology for their complex yet plastic division of labour. To observe the daily behaviour of individual bees in a colony, classical observation hives are very useful. The setting up and use of typical observation hives will be the focus of another section. The honey bee dance language has important characteristics of a real language and has been the focus of numerous studies. We here discuss the background of the honey bee dance language and describe how it can be studied. Finally, the mating of a honey bee queen with drones is essential to survival of the entire colony. We here give detailed and structured information how the mating behaviour of drones and queens can be observed and experimentally manipulated. The ultimate goal of this chapter is to provide the reader with a comprehensive set of experimental protocols for detailed studies on all aspects of honey bee behaviour including investigation of pesticide and insecticide effects. KW - COLOSS KW - BEEBOOK KW - honey bee KW - behaviour KW - gustatory responsiveness KW - olfactory responsiveness KW - phototaxis KW - non-associative learning KW - associative learning KW - appetitive learning KW - aversive learning KW - locomotion KW - temperature sensing KW - honey bee flight KW - observation hive KW - honey bee dance KW - honey bee navigation KW - harmonic radar KW - BeeScan KW - RFID KW - honey bee mating KW - free-flying honey bees Y1 - 2013 U6 - https://doi.org/10.3896/IBRA.1.52.4.04 SN - 0021-8839 SN - 2078-6913 VL - 52 IS - 4 PB - International Bee Research Association CY - Cardiff ER - TY - JOUR A1 - Stecker, Christian T1 - Parliaments and coalitions: - the role of legislative institutions in multiparty governance JF - Politische Vierteljahresschrift : Zeitschrift der Deutschen Vereinigung für Politische Wissenschaft Y1 - 2013 SN - 0032-3470 VL - 54 IS - 2 SP - 383 EP - 385 PB - Nomos CY - Hannover ER - TY - JOUR A1 - Sharma, Tripti A1 - Dreyer, Ingo A1 - Riedelsberger, Janin T1 - The role of K+ channels in uptake and redistribution of potassium in the model plant Arabidopsis thaliana JF - Frontiers in plant science N2 - Potassium (K+) is inevitable for plant growth and development. It plays a crucial role in the regulation of enzyme activities, in adjusting the electrical membrane potential and the cellular turgor, in regulating cellular homeostasis and in the stabilization of protein synthesis. Uptake of K+ from the soil and its transport to growing organs is essential for a healthy plant development. Uptake and allocation of K+ are performed by K+ channels and transporters belonging to different protein families. In this review we summarize the knowledge on the versatile physiological roles of plant K+ channels and their behavior under stress conditions in the model plant Arabidopsis thaliana. KW - plant potassium channel KW - Shaker KW - TPK KW - K-ir-like KW - Arabidopsis thaliana KW - voltage-dependent KW - voltage-independent Y1 - 2013 U6 - https://doi.org/10.3389/fpls.2013.00224 SN - 1664-462X VL - 4 PB - Frontiers Research Foundation CY - Lausanne ER - TY - JOUR A1 - Jolivet, Laurent A1 - Faccenna, Claudio A1 - Huet, Benjamin A1 - Labrousse, Loic A1 - Le Pourhiet, Laetitia A1 - Lacombe, Olivier A1 - Lecomte, Emmanuel A1 - Burov, Evguenii A1 - Denele, Yoann A1 - Brun, Jean-Pierre A1 - Philippon, Melody A1 - Paul, Anne A1 - Salaue, Gwenaelle A1 - Karabulut, Hayrullah A1 - Piromallo, Claudia A1 - Monie, Patrick A1 - Gueydan, Frederic A1 - Okay, Aral I. A1 - Oberhänsli, Roland A1 - Pourteau, Amaury A1 - Augier, Romain A1 - Gadenne, Leslie A1 - Driussi, Olivier T1 - Aegean tectonics strain localisation, slab tearing and trench retreat JF - Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth N2 - We review the geodynamic evolution of the Aegean-Anatolia region and discuss strain localisation there over geological times. From Late Eocene to Present, crustal deformation in the Aegean backarc has localised progressively during slab retreat. Extension started with the formation of the Rhodope Metamorphic Core Complex (Eocene) and migrated to the Cyclades and the northern Menderes Massif (Oligocene and Miocene), accommodated by crustal-scale detachments and a first series of core complexes (MCCs). Extension then localised in Western Turkey, the Corinth Rift and the external Hellenic arc after Messinian times, while the North Anatolian Fault penetrated the Aegean Sea. Through time the direction and style of extension have not changed significantly except in terms of localisation. The contributions of progressive slab retreat and tearing, basal drag, extrusion tectonics and tectonic inheritance are discussed and we favour a model (I) where slab retreat is the main driving engine, (2) successive slab tearing episodes are the main causes of this stepwise strain localisation and (3) the inherited heterogeneity of the crust is a major factor for localising detachments. The continental crust has an inherited strong heterogeneity and crustal-scale contacts such as major thrust planes act as weak zones or as zones of contrast of resistance and viscosity that can localise later deformation. The dynamics of slabs at depth and the asthenospheric flow due to slab retreat also have influence strain localisation in the upper plate. Successive slab ruptures from the Middle Miocene to the late Miocene have isolated a narrow strip of lithosphere, still attached to the African lithosphere below Crete. The formation of the North Anatolian Fault is partly a consequence of this evolution. The extrusion of Anatolia and the Aegean extension are partly driven from below (asthenospheric flow) and from above (extrusion of a lid of rigid crust). KW - Backarc extension KW - Slab retreat KW - Asthenospheric flow KW - Strain localisation KW - Aegean Sea KW - Metamorphic core complex Y1 - 2013 U6 - https://doi.org/10.1016/j.tecto.2012.06.011 SN - 0040-1951 VL - 597 SP - 1 EP - 33 PB - Elsevier CY - Amsterdam ER -