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The results of a ground-penetrating radar survey and multiproxy studies of the sediment cores collected from two lakes in the Valdai Highlands (East European Plain) provide new insights into the late glacial and Holocene environmental history of the region situated in the marginal zone of the last Scandinavian ice sheet. The cores were analyzed for organic carbon and nitrogen content, as well as for pollen and diatoms. The chronology of the cores is based on radiocarbon dates and pollen-based stratigraphy. The studied records document that vast dead ice masses and associated ice-dammed lakes existed in the Valdai Highlands area until ∼14 cal ka BP. Open tundra-steppe communities dominated the study area during the Oldest Dryas, Bølling, and Older Dryas (between ca. 17 and 14 cal ka BP), but dwarf birch (Betula nana), shrub alder (Alnus fruticosa), and willow (Salix) were also common. Scots pine forest (Pinus sylvestris) became common for a short interval during the Bølling warming (ca. 14.9 and 14.4 cal ka BP). The appearance of spruce (Picea) forest in the landscape occurred in the beginning of the Allerød warming (∼14 cal ka BP), but the open steppe-like plant communities remained common until the onset of the Holocene. The modern lake systems emerged at ∼10 cal ka BP, marked by an onset of organic-type sedimentation and the appearance of modern-type forests. The Mid-Holocene (∼8–4 cal ka BP) was the warmest time, as documented by the maximal distribution of temperate and broadleaved taxa in the region. The onset of agricultural land use and simultaneous trend of increasing lake trophic state and increasing paludification in the area is recorded at ∼2.5 cal ka BP.
The non-uniform evaporation rate at the liquid–gas interface of binary droplets induces solutal Marangoni flows. In glycerol–water mixtures (positive Marangoni number, where the more volatile fluid has higher surface tension), these flows stabilise into steady patterns. Conversely, in water–ethanol mixtures (negative Marangoni number, where the less volatile fluid has higher surface tension), Marangoni instabilities emerge, producing seemingly chaotic flows. This behaviour arises from the opposing signs of the Marangoni number. Perturbations locally reducing surface tension at the interface drive Marangoni flows away from the perturbed region. Continuity of the fluid enforces a return flow, drawing fluid from the bulk towards the interface. In mixtures with a negative Marangoni number, preferential evaporation of the lower-surface-tension component leads to a higher concentration of the higher-surface-tension component at the interface as compared with the bulk. The return flow therefore creates a positive feedback loop, further reducing surface tension in the perturbed region and enhancing the instability. This study investigates bistable quasi-stationary solutions in evaporating binary droplets with negative Marangoni numbers (e.g. water–ethanol) and examines symmetry breaking across a range of Marangoni numbers and contact angles. Bistable domains exhibit hysteresis. Remarkably, flat droplets (small contact angles) show instabilities at much lower critical Marangoni numbers than droplets with larger contact angles. Our numerical simulations reveal that interactions between droplet height profiles and non-uniform evaporation rates trigger azimuthal Marangoni instabilities in flat droplets. This geometrically confined instability can even destabilise mixtures with positive Marangoni numbers, particularly for concave liquid–gas interfaces, as in wells. Finally, through a Lyapunov exponent analysis, we confirm the chaotic nature of flows in droplets with a negative Marangoni number. We emphasise that the numerical models are intentionally simplified to isolate and clarify the underlying mechanisms, rather than to quantitatively predict specific experimental outcomes; in particular, the model becomes increasingly limited in regimes of rapid evaporation.
The search for biosignatures of past microbial life has promoted the interest in halophilic archaea trapped inside fluid inclusions of salt crystals. These hypersaline environments are promising targets for the preservation of microbial cell envelope biomolecules. In this study, we focused on the preservation of bacterioruberin, a carotenoid pigment found in the cell envelope of Halobacterium salinarum, within fluid inclusions of salt crystals mimicking early Mars environments and modern Earth. Halite (NaCl) and sylvite (KCl) crystals were subjected to Mars-like proton irradiation, and the preservation of carotenoids was assessed using in situ and ex situ Raman spectroscopy. Our findings demonstrate that Raman spectroscopy efficiently detected carotenoids within fluid inclusions in non-irradiated crystals. However, post-irradiation analyses posed great challenges due to fluorescence induced by the formation of colour centres in the crystal lattice, which suppressed the carotenoid signal. Cleavage of irradiated crystals revealed preserved carotenoid pigments beyond the radiation penetration depth, suggesting potential preservation of biomolecules in deeper inclusions within larger crystals. Furthermore, in some cases, carotenoids were detected even within fluorescent zones, suggesting extensive preservation. This study underscores the potential of Raman spectroscopy for the detection of carotenoids as biosignatures in planetary exploration contexts, particularly as a preliminary screening tool. However, it also highlights the need for optimized protocols to overcome fluorescence-related limitations. These findings contribute to the methodologies for detecting and interpreting biosignatures in salt deposits, advancing the search for possible traces of past microbial life beyond Earth.
The study of the ground surface temperature (GST) regimes from 2007 to 2021 at different stations on Livingston and Deception islands, South Shetland Islands, in the north-western sector of the Antarctic Peninsula (AP), shows that soils undergo similar cooling in early winter before a shallow snow mantle covers the sites. All monitoring sites along the study period go through seasonal phases of cooling, attenuation, insulation, fusion and zero curtain during winter, although thermal equilibrium is only reached at some stations located at lower elevations on Livingston Island. GST evolution at these stations and the duration of snow periods show oscillations, with turning points in the years 2014 and 2015, when temperatures were at their minimum and snow durations were at their maximum, in agreement with the cooling period occurring in the north-western AP in the early twenty-first century. The thermal regime is mainly controlled by snow cover and its onset and offset dates based only on descriptive patterns, not on statistical testing, more than by altitudinal, topographical, geological or geomorphological factors.
The present study documents the lithostratigraphy, biostratigraphy, facies evolution and depositional environments of the Eocene El Kohol Formation exposed on the southern flank of the Central Saharan Atlas (Algeria), through the integration of lithological characteristics, fossil and ichnofossil assemblages, and microfacies analysis. The succession is subdivided into two formal members: the Marly El Kohol Member, comprising a lower marlstone-dominated interval, and the Siliciclastic Kheneg ed Dis Member, representing an upper sandstone-dominated succession. The boundary between these members is marked by a transition from pale, carbonate-rich deposits to darker clastic sediments.
Field observations and microscopic analyses have enabled the recognition of sixteen facies types (Ft1–Ft16), which are interpreted in terms of depositional environment and grouped into four main facies associations (FA1–FA4): (FA1) an inland lake environment; (FA2) a palustrine environment, characterized by carbonate deposition in freshwater to brackish conditions with subaerial exposure and paedogenic modification; and alluvial settings comprising (FA3) fluvial channel and (FA4) floodplain deposits.
Palaeontological analyses have produced new micropalaeontological data for the region, including charophytes (Sphaerochara parvula, Nodosochara [Turbochara] sp., Gyrogona sp., Harrisichara cf. leptocera, Lamprothamnium papulosum, Peckichara torulosa var. varians, Raskyella cf. sahariana and Nitellopsis cf. [Tectochara] dutempleii), ostracods (Neocyprideis meguerchiensis, Paracypris? sp. 1, Paracypris? sp. 2 and Thalassocypria? sp. 1) and actinopterygian fish microremains (primarily from polypterids and alestids). Additionally, fragmentary remains of the terrestrial proboscidean Numidotherium koholense have been recovered. Ichnological analysis of the succession identified five ichnotaxa: Ophiomorpha isp., Palaeophycus isp., Skolithos annulatus, Skolithos linearis and Thalassinoides horizontalis.
This study contributes to refining the regional and North African understanding of the spatial extent and palaeoenvironmental evolution of the Eocene succession and helps to complete the ichnological and palaeontological records of the Eocene in the area.
Biologically inspired aero/hydrodynamics attracts considerable interest because of promising efficiency and manoeuvring capabilities. Yet, the influence that external perturbations, typical of realistic environments, can have over the flow physics and aerodynamic performance remains a scarcely investigated issue. In this work, we focus on the impact of free stream turbulence (FST) on the aerodynamics of a flapping wing with a prescribed (heaving and pitching) motion at a chord-based Reynolds number of 1000. The problem is tackled by means of direct numerical simulations using an immersed boundary method and a synthetic turbulence generator. The effect of two key parameters, i.e. the turbulence intensity and integral length scale of FST, is described by characterising the phase- and spanwise-averaged flows and aerodynamic coefficients. In particular, we show how FST effectively enhances the dissipation of the vortices generated by the flapping wing once they are sufficiently downstream of the leading edge. The net (i.e. time-averaged) thrust is found to be marginally sensitive to the presence of FST, whereas the characteristic aerodynamic fluctuations appear to scale linearly with the turbulence intensity and sublinearly with the integral length scale. Moreover, we reveal a simple mechanism where FST triggers the leading-edge vortex breakup, which in turns provides the main source of aerodynamic disturbances experienced by the wing. Finally, we show how the frequency spectra of the aerodynamic fluctuations are governed by the characteristic time scales involved in the problem.
Interactions between shock waves and gas bubbles in a liquid can lead to bubble collapse and high-speed liquid jet formation, relevant to biomedical applications such as shock wave lithotripsy and targeted drug delivery. This study reveals a complex interplay between acceleration-induced instabilities that drive jet formation and radial accelerations causing overall bubble collapse under shock wave pressure. Using high-speed synchrotron X-ray phase contrast imaging, the dynamics of micrometre-sized air bubbles interacting with laser-induced underwater shock waves are visualised. These images offer full optical access to phase discontinuities along the X-ray path, including jet formation, its propagation inside the bubble, and penetration through the distal side. Jet formation from laser-induced shock waves is suggested to be an acceleration-driven process. A model predicting jet speed based on the perturbation growth rate of a single-mode Richtmyer–Meshkov instability shows good agreement with experimental data, despite uncertainties in the jet-driving mechanisms. The jet initially follows a linear growth phase, transitioning into a nonlinear regime as it evolves. To capture this transition, a heuristic model bridging the linear and nonlinear growth phases is introduced, also approximating jet shape as a single-mode instability, again matching experimental observations. Upon piercing the distal bubble surface, jets can entrain gas and form a toroidal secondary bubble. Linear scaling laws are identified for the pinch-off time and volume of the ejected bubble relative to the jet’s Weber number, characterising the balance of inertia and surface tension. At low speeds, jets destabilise due to capillary effects, resulting in ligament pinch-off.
We present the mineralogy and whole rock geochemistry of the lamproites dykes from the Kawardha area of the Western Bastar Craton. These dykes are characterized by phenocrysts and microphenocrysts of olivine, phlogopite, ulvo-spinel, Cr-spinel and magnetite within the chlorite and carbonate-rich groundmass with rutile and apatite as accessory phases. Mineral chemistry indicates that the lamproites in Kawardha are similar to olivine-phlogopite lamproites and are geochemically similar to other lamproites in the eastern Bastar craton. The Kawardha lamproites are characterized by higher concentrations of MgO (12–20.29 wt%), V (193–502 ppm), Ni (206–823 ppm), Cr (146–1130 ppm), Nb (101–260 ppm), Zr (301–635 ppm), Hf (6–13 ppm) and LREEs. Positive Nb-Ta anomalies and Th, Hf and Zr variations are comparable to other intra-cratonic rift-related lamproites. The geochemical variations (such as REE, HFSE and LILE) are consistent with an asthenospheric mantle source similar to the other lamproites in Bastar craton. Trace element modelling implies a low-degree partial melting (0.1–2%) of phlogopite-bearing garnet-lherzolite and/or phlogopite-bearing spinel-lherzolite mantle source. The widespread Proterozoic rifting events in the Bastar craton likely led to the melting and upwelling of the asthenospheric mantle and which further interacted with the metasomatized lithospheric mantle to form the parental melts of the lamproite dykes of the Kawardha area.
This paper theoretically introduces a new architecture for pumping leaky-dielectric fluids. For two such fluids layered in a channel, the mechanism utilises Maxwell stresses on fluid interfaces (referred to as menisci) induced by a periodic array of electrode pairs inserted between the two fluids and separated by the menisci. The electrode pairs are asymmetrically spaced and held at different potentials, generating an electric field with variation along the menisci. To induce surface charge accumulation, an electric field (and thus current flow) is also imposed in the direction normal to the menisci, using flat upper and lower electrodes, one in each fluid. The existence of both normal and tangential electric fields gives rise to Maxwell stresses on each meniscus, driving the flow in opposite directions on adjacent menisci. If the two menisci are the same length, then a vortex array is generated that results in no net flow; however, if the spacing is asymmetric, then the longer meniscus dominates, causing a net pumping in one direction. The pumping direction can be controlled by the (four) potentials of the electrodes, and the electrical properties of the two fluids. In the analysis, an asymptotic approximation is made that the interfacial electrode period is small compared to the fluid layer thicknesses, which reduces the analytical difficulty to an inner region close to the menisci. Closed-form solutions are presented for the potentials, velocity field and resulting pumping speed, for which maximum values are estimated, with reference to the electrical power required and feasibility.
We present a theoretical approach that derives the wavenumber $k^{-1}$ spectral scaling in turbulent velocity spectra using random field theory without assuming specific eddy correlation forms or Kolmogorov’s inertial-range scaling. We argue for the mechanism by Nikora (1999 Phys. Rev. Lett.83 (4), 734), modelling turbulence as a superposition of eddy clusters with eddy numbers inversely proportional to their characteristic length scale. Statistical mixing of integral scales within these clusters naturally yields the $k^{-1}$ scaling as an intermediate asymptotic regime. Building on the spectrum modelling introduced in Jetti et al. (2025b Z. Angew. Math. Physik.74 (3), 123), we develop and apply an integral formulation of the general velocity spectrum that reproduces the $k^{-1}$ regime observed in field spectra, thereby bridging theoretical derivation and empirical observations. The model is validated using wind data at a coastal site, and tidal data in a riverine environment where the –1 scaling persists beyond the surface layer logarithmic region. The results confirm the robustness of the model at various flow conditions, offering new insights into the spectral energy distribution in geophysical and engineering flows.
Crystallisation of the earliest minerals typically affects the composition of minerals subsequently formed, being controlled by their abundance and the compatibility/incompatibility of the relevant elements. Here we have investigated the effects of early tourmaline crystallisation on the formation of primary Be minerals (beryl and helvine–danalite) in metaluminous intragranitic NYF pegmatites of the Třebíč Pluton, Czech Republic. Tourmaline occurs in different textural-paragenetic types: (a) coarse- to medium-grained aggregates; (b) graphic (Tur+Qz) intergrowths; (c) fine-grained nodules (Tur+Qz+Pl+Kfs); (d) tourmaline pseudomorphs after biotite; (e) interstitial tourmaline; and (f) replacing helvine–danalite. The compositions of primary tourmalines (a), (b) and (c) vary from Ca- and Ti-rich Fe-dravite to Mg-poor schorl and dutrowite, and to magnesio-dutrowite, showing low to moderate Al (5.1–6.1 apfu), variable Mg (0.1–1.9 apfu) and Fe (1.3–2.2 apfu), low Mn (≤0.1 apfu), low to moderate Ca (0.1–0.4 apfu), and high Ti (≤0.55 apfu). Type (f) secondary tourmaline is poor in Mg, Ca and Ti (all ≤0.07 apfu), but rich in Na (0.64–0.81 apfu), Fe (0.68–2.17 apfu), Mn (0.31–0.80 apfu), Al (6.57–7.61 apfu), and F (0.37–0.58 apfu). Two distinct assemblages of early-formed Be minerals were recognised: the assemblage beryl ± phenakite occurs in pegmatites with rare interstitial tourmaline (e), whereas the assemblage helvine–danalite ± phenakite is characteristic of pegmatites with abundant early tourmaline (a). The assemblages of primary Be minerals in the individual pegmatites reflect how crystallisation and abundance of early tourmaline control the origin and composition of successive primary Be minerals. The crystallisation of abundant early-formed tourmaline depletes the residual melt of elements that are incorporated preferentially into the tourmaline structure (Al, Mg, Zn), whereas incompatible Mn accumulates, leading to the formation of Mn-rich helvine–danalite. In contrast, beryl only occurs in pegmatites where early-formed tourmaline is absent. The early crystallisation of tourmaline might thus affect the species and composition of later crystallising minerals.
Interactions between hyperelastic bio-membranes and fluid play a crucial role in the flight (or swimming) motion of many creatures, such as bats, flying squirrels and lemurs. Bio-membranes are characterised by high stretchability and micro-bending stiffness, leading to unique fluid–solid coupling properties (Mathai et al., 2023, Phys. Rev. Lett., vol. 131, 114003). This study presents a high-fidelity numerical exploration of the hyperelastic characteristics of a pitching foil inspired by bio-membranes in fluid within a low Reynolds number regime. The focus is on the effect of foil compliance on its self-propulsion performance, mimicking natural propulsion mechanisms, with the foil free to move in the horizontal direction. We find that with certain compliance, the foil may experience a velocity crisis, meaning that its propulsive capability is completely lost. This phenomenon is caused by the loss of beat speed when the foil’s passive deformation is out of phase with the pitching motion. By contrast, the two motions can be in phase at proper compliance, leading to an increased beat speed. This will significantly enhance propulsive velocity up to $33\,\%$ compared with the rigid case. The results demonstrate the feasibility of compliance tuning to circumvent the velocity crisis and improve the propulsive speed, which are helpful in the design of micro aerial robots using biomimetic membranes.
This Element supports Gwich'in, Iñupiat, and all Alaska Natives' collective continuance and reparative justice from the perspective of a settler in the traditional territories of lower Tanana Dene Peoples. It stands with Alaska Natives' recovering and safe-keeping: kinships obstructed by settler-colonialism; ontologies and languages inseparable from land-relations and incommensurable with English-language perspectives; and epistemologies not beholden to any colonialist standard. These rights and responsibilities clash with Leopoldian conservation narratives still shaping mind-sets and institutions that eliminate Indigenous Peoples by telling bad history and by presuming entitlements to lands and norm-making authority. It models an interlocking method and methodology – surfacing white supremacist settler-colonialist assumptions and structures of Leopoldian conservation narratives – that may be adapted to critique other problematic legacies. It offers a pra xis of anti-colonialist, anti-racist, liberatory environmental-narrative critical-assessment centering Indigenous experts and values, including consent, diplomacy, and intergenerational respect needed for stable coalitions-making for climate and environmental justice.
Xandarellida is a clade of artiopodan euarthropods known exclusively from the early Cambrian (Series 2, Stage 3) Chengjiang biota of South China, apart from the possible inclusion of Phytophilaspis Ivantsov, 1999 from the early Cambrian Sinsk Biota of Siberia. A rare euarthropod taxon represented by four specimens from the Emu Bay Shale (Cambrian Series 2, Stage 4) of Kangaroo Island, South Australia, represents the first record of Xandarellida from East Gondwana. A new monotypic genus, Austroxandarella n. gen., is based on A.poikar n. sp., being most readily distinguished by its elongate pygidium. Close affinities to Xandarella Hou et al., 1991 are suggested by a thorax of 10 tergites, with progressive elongation of the posterior three tergites relative to the seven anterior tergites of subequal length—this elongation representing the dorsoventral decoupling of biramous appendage pairs and tergites shared by all xandarellids. Discovery of an Australian xandarellid adds more support for biogeographic affinities between East Gondwana and South China in the early Cambrian.
The objective of this chapter is to more fully explore how urban environmental change takes place. The role and significance of economic development and normative planning efforts are explored. These conditions further help refine understanding of how different drivers and social and economic forces influence how cities both create and respond to the environmental crises and how transitions are manifested. Several different narratives of urban transitions are defined. These include urban transitions as sequence, collapse, advance, futures, and just sustainability. An integrated framework that links the different elements of urban environmental transitions is presented and discussed. The framework includes four steps – stress, crisis, transition, and transformation – with coupled components and elements such as drivers, spheres of action, and process and product outcomes. A review of the application areas and specific cases are presented as an introduction to the next section of the book.
Gamero-Castaño and colleagues have reported that a large number of calculated shapes for electrified cone jets collapse into a nearly universal geometry when scaled with a characteristic length $R_G$ previously introduced by Gañán-Calvo et al. (J. Aerosol Sci., vol. 25, 1994, pp. 1121–1142). The theoretical reasons for that unexpected success were, however, unclear. Recently, Pérez-Lorenzo & Fernández de la Mora (J. Fluid Mech., vol. 931, 2022, A4) have noted that a slightly different length scale $L_j$ is suggested by the asymptotic jet structure inferred by Gañán-Calvo (Phys. Rev. Lett., vol. 79, 1997, pp. 217–220) from energy conservation and the hypothesis that the asymptotic electric field is that given by Taylor’s static model. This article aims to identify which of these two scales best collapses calculated cone-jet structures, and whether there is an alternative superior one. The characteristic lengths are tested against a large set of numerical solutions of a cone-jet model. The effectiveness of each scaling is determined through analyses based on the standard deviation of the numerical solutions. Despite the slight difference between $R_G$ and $L_j$, this analysis clearly identifies $L_j$ as the most accurate scaling for all cone-jet parameters tested. Differentiating between both scales would not have been possible with experimental measurements, but requires the use of high-fidelity numerical solutions. Surprisingly, the success of $L_j$ is not limited to the jet region, but extends to the cone and the neck. These findings provide a slightly superior scaling enjoying a considerably firmer theoretical basis.
Daily life in cities is often about balance and compromise. Urban densities facilitate things being in close proximity and provide convenience for residents, but they also create an opportunity for traffic congestion and increased social and environmental inequity, and the possibility of lower-density suburban sprawl. To promote urban sustainability, a careful balance of economic development, ecology, and equity is required. In this chapter, four examples of urban sustainability crises and the dramatic response to them are examined. The cases include Miami, US; Oslo, Norway; St. Georges, Grenada; and Shenzhen, China. In each situation, the sustainability crisis emerges from a deeply set awareness of diminishing environmental quality of life and a feeling that the residents’ sense of place is under threat. The drivers of this threat are deeply embedded in social and economic factors. In each city, the policy switch to enhanced sustainability results from an aggressive, multi-scalar effort to alter and redirect the pattern of urban spatial development.
A pressing need exists to understand how, when, and why to adjust and build upon urban environmental policies that can influence a city’s capacity to foster and enact climate adaptation and mitigation. The objective of this book has been to define what we can learn from past urban environmental crises and resulting policy transitions that might be applicable to understand how climate change will manifest as crises in cities and what can be done to help accelerate urban climate action. In this chapter, we more directly turn our attention to learning what the book’s case studies reveal about these objectives. The case studies illustrate how existing urban environmental practices can be adjusted and enhanced to better grapple with the challenges of climate change. The analysis provides the groundwork for a set of innovative recommendations on how to perceive the urban climate crisis and how to consider new urban climate change policies. A key overall conclusion is that we should do all we can to learn from previous urban environmental crises as they will continue to inform us moving into the future.