254 research outputs found
Life in a warm deep sea: routine activity and burst swimming performance of the shrimp Acanthephyra eximia in the abyssal Mediterranean
Measurements of routine swimming speed, "tail-flip'' escape responses, and oxygen consumptions were made of the deep-sea shrimp Acanthephyra eximia using autonomous landers in the Rhodos Basin at depths of up to 4,400 m and temperatures of 13 - 14.5 degrees C. Routine swimming speeds at 4,200 m averaged 0.18 m s(-1) or 3.09 body lengths s(-1), approximately double those of functionally similar oceanic scavengers. During escape responses peak accelerations of 23 m s(-2) or 630.6 body lengths s(-2) were recorded, with animals reaching speeds of 1.61 m s(-1) or 34.8 body lengths s(-2). When compared to shallow-water decapods at similar temperatures these values are low for a lightly calcified shrimp such as A. eximia despite a maximum muscle mass specific power output of 90.0 W kg(-1). A preliminary oxygen consumption measurement indicated similar rates to those of oceanic crustacean scavengers and shallower-living Mediterranean crustaceans once size and temperature had been taken into account. These animals appear to have high routine swimming speeds but low burst muscle performances. This suite of traits can be accounted for by high competition for limited resources in the eastern Mediterranean, but low selective pressure for burst swimming due to reductions in predator pressure
Respiratory epithelial adenomatoid hamartoma in a child with nasal polyposis. Case report
Benign and malignant formations of the nose and paranasal sinuses in the early stages of development are asymptomatic or manifest minor nonspecific signs, and therefore often remain unrecognized. Hamartoma is a tumor-like formation of a dysembriological nature, consisting of excessive tissues peculiar to the affected organ. Due to the rarity of the occurrence of hamartomas of the sinonasal region, especially in pediatric practice, their diagnosis may present certain difficulties, since they can mimic other formations, such as nasal polyps or inverted papilloma, may occur as an isolated formation in the nasal cavity, or in combination with chronic rhinosinusitis, nasal polyposis, allergic rhinosinusitis. Aim – to report a rare clinical case in pediatric practice of respiratory epithelial adenomatoid hamartoma associated with allergic rhinosinusitis and polyposis, display the relationship between the occurrence of respiratory epithelial adenomatoid hamartoma and chronic inflammation of the nasal cavity and paranasal sinuses, to carry out differential diagnosis with other exophytic aggressive lesions of the nasal cavity, combine and summarize available data on sinonasal hamartomas. The article describes a clinical case of respiratory epithelial adenomatoid hamartoma in a 17-year-old child with a previous 4-year follow-up with nasal cavity polyposis and a history of repeated polypotomy. The results of endoscopy and computed tomography of the nasal cavity and paranasal sinuses, the results of surgical intervention, as well as the conclusions of a histological examination of the tumor removed from the patient are presented. The authors analyzed the domestic and foreign literature, on the basis of which they presented a differential series of sinonasal hamartomas. Respiratory epithelial adenomatoid hamartoma is a rare pathological formation of the sinonasal region, which manifests itself as an isolated polypoid mass in the nasal cavity or as an accidental surgical finding in patients with chronic sinusitis. The association with nasal polyps supports the hypothesis that inflammation may be one of the inducing factors. Respiratory epithelial adenomatoid hamartoma, although rare, should be considered in the differential diagnosis of exophytic lesions of the nasal cavity. The tactics of treatment involves endoscopic removal of the formation within healthy tissues, which provides good long-term results, relapses are extremely rare
The efficiency of tear substitute therapy at dysfunction tear basic secretion
Purpose: to evaluate the efficiency and tolerance of drops replacing tear with hyaluronic acid 0.15% (Hylabak, thea, France) for the treatment of tear film diseases, in particular blepharoconjunctival form of dry eye syndrome.Methods: 32 patients (range 38 to 72 years) with blepharoconjunctival form of dry eye syndrome were treated lubricant Hylabak 2-4 times a day during 7-30 days.Results: After treatment was detected the elimination of complaints in 30 of 32 people, increasing the stability of the tear film (increasing values of the samples Norn test from 7.3 ±0.5 to 10.1±0.6 seconds), as well as normalization of Schirmer test (from 8.8±0.4 to 15.2±0.5 mm).Conclusion: the study was showed high efficacy of lubricant Hylabak and subjective tolerability at blepharoconjunctival form of dry eye syndrome
Climate warming, marine protected areas and the ocean-scale integrity of coral reef ecosystems
Coral reefs have emerged as one of the ecosystems most vulnerable to climate variation and change. While the contribution
of a warming climate to the loss of live coral cover has been well documented across large spatial and temporal scales, the
associated effects on fish have not. Here, we respond to recent and repeated calls to assess the importance of local
management in conserving coral reefs in the context of global climate change. Such information is important, as coral reef
fish assemblages are the most species dense vertebrate communities on earth, contributing critical ecosystem functions
and providing crucial ecosystem services to human societies in tropical countries. Our assessment of the impacts of the
1998 mass bleaching event on coral cover, reef structural complexity, and reef associated fishes spans 7 countries, 66 sites
and 26 degrees of latitude in the Indian Ocean. Using Bayesian meta-analysis we show that changes in the size structure,
diversity and trophic composition of the reef fish community have followed coral declines. Although the ocean scale
integrity of these coral reef ecosystems has been lost, it is positive to see the effects are spatially variable at multiple scales,
with impacts and vulnerability affected by geography but not management regime. Existing no-take marine protected areas
still support high biomass of fish, however they had no positive affect on the ecosystem response to large-scale disturbance.
This suggests a need for future conservation and management efforts to identify and protect regional refugia, which should
be integrated into existing management frameworks and combined with policies to improve system-wide resilience to
climate variation and change
Improvement of Protective Oxide Layers Formed by Highfrequency Plasma Electrolytic Oxidation on Mg-RE Alloy with LPSO-Phase
Received: 17.04.23. Revised: 17.05.23. Accepted: 23.05.23. Available online: 29.05.23.PEO of Mg-RE (LPSO) alloy allows improving its corrosion behaviour and surface mechanical properties.Increase of pulse frequency under PEO allows decreasing the porosity and heterogeneity of the oxide layers.The best corrosion resistance and adhesive strength demonstrate the oxide layer obtained in aluminate electrolyte under high-frequency PEO.Oxide layers on Mg97Y2Zn1 magnesium alloy with strengthening LPSO-phase were formed by plasma electrolytic oxidation (PEO) in bipolar mode with frequency variation of forming current pulses (50 and 500 Hz) and addition of sodium aluminate or sodium silicate to alkali phosphate fluoride electrolyte. Microstructure, chemical and phase composition, corrosion and mechanical properties of the oxide layers formed were investigated. With increasing current frequency for both electrolytes, an increase in homogeneity of the oxide layers structure and a decrease in their porosity and fracturing at constant thickness were recorded. The oxide layers formed at 500 Hz even with some decrease in hardness have better adhesive strength and 2 orders of magnitude higher short-term corrosion resistance values. PEO of Mg-alloy with LPSO-phase in the electrolyte with addition of sodium aluminate in combination with increased pulse frequency (500 Hz) allows forming the best-quality uniform oxide layer with high hardness, adhesive strength and corrosion resistance properties. The use of electrolyte with addition of sodium silicate reduced the adhesive strength by 1.5 times and brought down the long-term corrosion resistance of oxide layers by an order of magnitude, as compared with the electrolyte with sodium aluminate. The reason for a significant improvement in the complex of protective properties of the oxide layers with an increase in the current pulse frequency is supposed to be a decrease in the power and duration of individual microarc discharges with simultaneous increase in their number per unit oxidized area.Financial support is provided by the Russian Science Foundation (grant No. 20-79-10262), https://rscf.ru/project/20-79-10262/
Improvement of protective oxide layers formed by high-frequency plasma electrolytic oxidation on Mg-RE alloy with LPSO-phase
Oxide layers on Mg97Y2Zn1 magnesium alloy with strengthening LPSO-phase were formed by plasma electrolytic oxidation (PEO) in bipolar mode with frequency variation of forming current pulses (50 and 500 Hz) and addition of sodium aluminate or sodium silicate to alkali phosphate fluoride electrolyte. Microstructure, chemical and phase composition, corrosion and mechanical properties of the oxide layers formed were investigated. With increasing current frequency for both electrolytes, an increase in homogeneity of the oxide layers structure and a decrease in their porosity and fracturing at constant thickness were recorded. The oxide layers formed at 500 Hz even with some decrease in hardness have better adhesive strength and 2 orders of magnitude higher short-term corrosion resistance values. PEO of Mg-alloy with LPSO-phase in the electrolyte with addition of sodium aluminate in combination with increased pulse frequency (500 Hz) allows forming the best-quality uniform oxide layer with high hardness, adhesive strength and corrosion resistance properties. The use of electrolyte with addition of sodium silicate reduced the adhesive strength by 1.5 times and brought down the long-term corrosion resistance of oxide layers by an order of magnitude, as compared with the electrolyte with sodium aluminate. The reason for a significant improvement in the complex of protective properties of the oxide layers with an increase in the current pulse frequency is supposed to be a decrease in the power and duration of individual microarc discharges with simultaneous increase in their number per unit oxidized area
The Medicine Tree: Unsettling palaeoecological perceptions of past environments and human activity
In this paper, we consider palaeoecological approaches to past landscapes and reflect upon how these are relevant to archaeological themes concerning concepts of environmental change and the role of past and present human communities in these processes. In particular, we highlight the importance of local context in the perception and understanding of landscape. Utilising a case study from Nepal, we look to ‘unsettle’ a conventional palaeoecological interpretation of a pollen record, originally constructed on western ecological principles, and instead draw on an interpretative perspective rooted in local Buddhist ecological knowledge, or a ‘folk taxonomy’, known as ‘The Medicine Tree’. We discuss how the interpretations of patterns and processes of vegetation change from a pollen record are not necessarily absolute. In particular, we outline how the palaeoecological frame of enquiry and reference is rooted in an essentially Eurocentric, Western scientific paradigm, which, in turn, shapes how we perceive and conceive of past landscapes and the role of ‘anthropogenic impact’ on vegetation. The aim of this is not to suggest that scientific approaches to the ‘reconstruction’ of past landscapes are necessarily invalid, but to illustrate how ‘empirical’ scientific methods and interpretations in archaeological science are contingent upon specific social and cultural frames of reference. We discuss the broader relevance of this, such as how we interpret past human activity and perception of landscape change, the ways in which we might look to mobilise research in the context of contemporary problems, issues concerning ‘degraded landscapes’ and how we incorporate local and archaeological perspectives with palaeoecology within an interconnected and iterative process
Contrasting responses to climate change at Himalayan treelines revealed by population demographics of two dominant species
Alpine treelines are expected to shift upward due to recent climate change. However, interpretation of changes in montane systems has been problematic because effects of climate change are frequently confounded with those of land use changes. The eastern Himalaya, particularly Langtang National Park, Central Nepal, has been relatively undisturbed for centuries and thus presents an opportunity for studying climate change impacts on alpine treeline uncontaminated by potential confounding factors.
We studied two dominant species, Abies spectabilis (AS) and Rhododendron campanulatum (RC), above and below the treeline on two mountains. We constructed 13 transects, each spanning up to 400 m in elevation, in which we recorded height and state (dead or alive) of all trees, as well as slope, aspect, canopy density, and measures of anthropogenic and animal disturbance.
All size classes of RC plants had lower mortality above treeline than below it, and young RC plants (<2 m tall) were at higher density above treeline than below. AS shows little evidence of a position change from the historic treeline, with a sudden extreme drop in density above treeline compared to below. Recruitment, as measured by size–class distribution, was greater above treeline than below for both species but AS is confined to ~25 m above treeline whereas RC is luxuriantly growing up to 200 m above treeline.
Synthesis. Evidence suggests that the elevational limits of RC have shifted upward both because (a) young plants above treeline benefited from facilitation of recruitment by surrounding vegetation, allowing upward expansion of recruitment, and (b) temperature amelioration to mature plants increased adult survival. We predict that the current pure stand of RC growing above treeline will be colonized by AS that will, in turn, outshade and eventually relegate RC to be a minor component of the community, as is the current situation below the treeline
Palynological evidence for environmental and climatic change in the lower Guadiana valley, Portugal, during the last 13 000 years
Pollen analysis of a 48 m AMS radiocarbon-dated sediment sequence from the Guadiana estuary provides the first record of Lateglacial and Holocene vegetation history in the Algarve province of Portugal. This paper focuses on the record of terrestrial pollen taxa, which document a series of forest expansions and declines during the period 13 000 cal. BP to 1600 cal. BP and provide insights into climate evolution in southwestern Iberia. The main vegetation phases identified in the Guadiana valley are (1) Lateglacial interstadial (Allerød) forest with Quercus and Pinus under a temperate, moist, continental climate;
(2) a Younger Dryas forest decline (Quercus) and expansion of pinewoods, xeric scrub and open ground habitats (with Juniperus, Artemisia, Ephedra distachya type, Centaurea scabiosa type) under arid and cold conditions; (3) an early Holocene forest/scrub/open-ground vegetation mosaic developing under a warm, dry and continental climate; (4) a maximum of Quercus forest and thermomediterranean evergreen taxa (Olea, Phillyrea, Pistacia) reflecting a warm, moist oceanic climate between c. 9000 cal. BP and c. 5000 cal. BP; and (5) the expansion of shrublands with Cistaceae and Ericaceae under a drier climatic regime and increasing anthropogenic activity since c. 5000 cal. BP. Holocene episodes of maximum climatic aridity are identified in the record of xerophytic taxa (Juniperus, Artemisia, Ephedra distachya type) centred around 10 200 cal. BP, 7800 cal. BP, 4800 cal. BP, 3100 cal. BP and 1700 cal. BP. Regional comparisons suggest a correlation of arid phases across southern Iberia and northwest Africa, which can be related to abrupt North Atlantic coolings (Bond events).Research Council studentship for WJF (NERC/S/A/2001/06109), with the support of Trinity College and the Department of Geography, University of Cambridg
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