Impacts of groundwater dynamics around a macro-tidal river on agricultural soil salinity.

Estuaries are vulnerable to oceanic and atmospheric climate change. Much of the research investigating climate change impacts on estuaries is focused on saltwater intrusion within surface water due to drought and rising sea levels, with implications for ecosystems and humans. Groundwater and soil near estuaries may also be influenced, as estuary salinity and hydraulic head changes can impact soils and aquifers not previously at risk of salinization. This study was conducted to address knowledge gaps related to present and future groundwater salinity distribution in a groundwater system connected to a macro-tidal estuary. The studied estuary experiences a tidal bore due to its hydraulic connection to the Bay of Fundy in Nova Scotia, Canada. A parcel of agricultural land adjacent to the estuary was selected to assess the groundwater response to episodic fluctuations in estuary water levels and salinity. Groundwater monitoring and electromagnetic surveys were conducted to map soil and groundwater salinity patterns. A numerical model of groundwater flow and solute transport informed by field data was used to investigate how varying estuary salinity due to droughts and sea-level rise could impact groundwater salinity. Results showed that, in contrast to salt wedges observed along marine coasts, the saline groundwater existed as a plume immediately around the estuary. Model simulations showed that short-term droughts had an insignificant impact on the adjacent groundwater salinity. However, permanent increases in salinity caused by sea-level rise increased the plume volume by 86 %, or an additional ∼11 m horizontally and âˆ¼ 4.5 m vertically. Our results suggest that increased river salinity in this setting would not result in widespread salinization of porewater and agricultural soils, but more extensive salinization may be experienced in permeable aquifers or along more saline estuarine zones. Findings may inform land management decisions in regions exposed to increased salinity in the future.

Morphodynamics of a composite sand-cobble beach in response to extratropical cyclone Fiona and seasonal wave variability.

Climate change is driving higher coastal water levels, and models project accelerated future sea-level rise and coastal storm intensification. These dynamics paired with anthropogenic coastal alterations will drive drastic coastal change worldwide. Composite beaches with mixed sediment sizes warrant detailed study as these exhibit complex morphodynamics in response to changing hydrodynamics due to the distinct transport thresholds of different sediment types. This study uses a novel multi-method approach to investigate a composite sand-cobble beach in Atlantic Canada experiencing a shortening seasonal sand-covered period. Hydrodynamic forcing and associated beach changes were monitored over a focused eight-month period, while satellite-based visual imagery and reconstructed wave data were analyzed over longer periods. Results show that intra-annual wave energy changes drive sand dynamics, with reduced summer wave energy facilitating short-term deposition. Long-term positive trends were identified in late spring wave heights, which likely contribute to the shortening sand-covered period. Seasonal dynamics were overwhelmed by extratropical cyclone Fiona, which made landfall on September 24, 2022, generating significant wave heights up to 6.8 m in the bay, mobilizing sediment, and steepening cobble berms. A new index approach based on visual imagery facilitated the investigation of beach sand appearance/disappearance using the relative redness of sand compared to cobble. Finally, the UAV-based surveys yielded high-resolution orthomosaics and LiDAR-based elevation mapping, and highlighted pronounced longshore variability in erosion and deposition during Fiona. The beach mostly recovered to pre-storm conditions in <4 months, which indicates that proposed beach nourishment activities may only experience temporary success. The longer-term results showing a conversion of sand to cobble suggest that loss of sandy beach habitat is likely to increase, even without shoreline migration or coastal squeeze driven by sea-level rise.

Closing the gap between science and management of cold-water refuges in rivers and streams.

Human activities and climate change threaten coldwater organisms in freshwater ecosystems by causing rivers and streams to warm, increasing the intensity and frequency of warm temperature events, and reducing thermal heterogeneity. Cold-water refuges are discrete patches of relatively cool water that are used by coldwater organisms for thermal relief and short-term survival. Globally, cohesive management approaches are needed that consider interlinked physical, biological, and social factors of cold-water refuges. We review current understanding of cold-water refuges, identify gaps between science and management, and evaluate policies aimed at protecting thermally sensitive species. Existing policies include designating cold-water habitats, restricting fishing during warm periods, and implementing threshold temperature standards or guidelines. However, these policies are rare and uncoordinated across spatial scales and often do not consider input from Indigenous peoples. We propose that cold-water refuges be managed as distinct operational landscape units, which provide a social and ecological context that is relevant at the watershed scale. These operational landscape units provide the foundation for an integrated framework that links science and management by (1) mapping and characterizing cold-water refuges to prioritize management and conservation actions, (2) leveraging existing and new policies, (3) improving coordination across jurisdictions, and (4) implementing adaptive management practices across scales. Our findings show that while there are many opportunities for scientific advancement, the current state of the sciences is sufficient to inform policy and management. Our proposed framework provides a path forward for managing and protecting cold-water refuges using existing and new policies to protect coldwater organisms in the face of global change.

Impacts of repeated coastal flooding on soil and groundwater following managed dike realignment.

Coastal defense structures (e.g., dikes, seawalls) protect vulnerable communities along marine coastlines and estuaries from the physical and chemical influences of adjacent water bodies. These structures are susceptible to overtopping or breaching by tides and waves, with risks amplified by climate change-induced sea-level rise. Repeated inundation by saline water can contaminate freshwater resources and salinize soil, impacting land-use activities, including agricultural productivity. Managed ecosystem-based dike realignment and salt marsh restoration can provide alternatives to traditional coastal adaptation approaches. We assess the changes to soil salinity at a managed dike realignment project prior to the transformation from a diked terrestrial environment to an estuarine environment. Baseline data are compared to conditions following 8-10 months of intermittent flooding at spring tides. Results show that an increase in salinity occurred over the entire site in the shallow subsurface, with the most significant contamination occurring in low-lying areas. Bulk soil electrical conductivity (salinity proxy) measured from geophysical surveys increased from the previous freshwater condition of ∼300 µS/cm to over 6000 µS/cm following <20 flood events, while successive flooding resulted in increased soil moisture as infiltrated floodwater propagated to greater depths. Sediment deposition occurred at high rates, with up to 4 cm of sediment deposited per flood, converting much of the previously cultivated land into tidal mudflats. Deeper sediments and groundwater (i.e., >1.8 m depth) were not impacted over the time scale of this research. This study demonstrates that intermittent shallow flooding can rapidly increase moisture content and soil salinity in surficial sediments and, in turn, adversely impact conditions suitable for agricultural crop production. The realignment zone serves as an engineered analog of coastal flooding, presenting an opportunity to investigate how low-lying coastal environments may experience regular flooding in the future due to sea-level rise and intensifying coastal storms.

Impacts of permafrost thaw on streamflow recession in a discontinuous permafrost watershed of northeastern China.

Permafrost thaw due to climate change is altering terrestrial hydrological processes by increasing ground hydraulic conductivity and surface and subsurface hydrologic connectivity across the pan-Arctic. Understanding how runoff responds to changes in hydrologic processes and conditions induced by permafrost thaw is critical for water resources management in high-latitude and high-altitude regions. In this study, we analyzed streamflow recession characteristics for 1964-2016 for the Tahe watershed located at the southern margin of the permafrost region in Eurasia. Results reveal a link between streamflow recession and permafrost degradation as indicated by the statistical analyses of streamflow and the modeled ground warming and active layer thickening. The recession constant and the active layer temperatures at depths of 5, 40, 100, and 200 cm simulated by the backpropagation neural network model significantly increased during the study period from 1972 to 2020 due to intensified climate warming in northeastern China. The onset of seasonal active layer thaw was advanced by 10 days, and the modeled active layer thickness increased by 54 cm in this period. The average annual streamflow recession time increased by 11.5 days (+53 %) from the warming period (1972-1988) to the thawing period (1989-2016), with these periods determined from breakpoint analysis. These hydrologic changes arose from increased catchment storage and were correlated to increased active layer thickness and longer seasonal thawing periods. These results highlight that permafrost degradation can significantly extend the recession flow duration in a watershed underlain by discontinuous, sporadic, and isolated permafrost, and thereby alter flooding dynamics and water resources in the southern margin of the Eurasian permafrost region.

Shallow subsurface heat recycling is a sustainable global space heating alternative.

Despite the global interest in green energy alternatives, little attention has focused on the large-scale viability of recycling the ground heat accumulated due to urbanization, industrialization and climate change. Here we show this theoretical heat potential at a multi-continental scale by first leveraging datasets of groundwater temperature and lithology to assess the distribution of subsurface thermal pollution. We then evaluate subsurface heat recycling for three scenarios: a status quo scenario representing present-day accumulated heat, a recycled scenario with ground temperatures returned to background values, and a climate change scenario representing projected warming impacts. Our analyses reveal that over 50% of sites show recyclable underground heat pollution in the status quo, 25% of locations would be feasible for long-term heat recycling for the recycled scenario, and at least 83% for the climate change scenario. Results highlight that subsurface heat recycling warrants consideration in the move to a low-carbon economy in a warmer world.

Small atoll fresh groundwater lenses respond to a combination of natural climatic cycles and human modified geology.

Freshwater lenses underlying small ocean islands exhibit spatial variability and temporal fluctuations in volume, influencing ecologic management. For example, The Palmyra Atoll National Wildlife Refuge harbors one of the few surviving native stands of Pisonia grandis in the central Pacific Ocean, yet these trees face pressure from groundwater salinization, with little basic groundwater data to guide decision making. Adding to natural complexity, the geology of Palmyra was heavily altered by dredge and fill activities. Our study based at this atoll combines geophysical and hydrological field measurements from 2008 to 2019 with groundwater modeling to study the drivers of observed freshwater lens dynamics. Electromagnetic induction (EMI) field data were collected on the main atoll islands over repeat transects in 2008 following 'strong' La Niña conditions (wet) and in 2016 during 'very strong' El Niño conditions (dry). Shallow monitoring wells were installed adjacent to the geophysical transects in 2013 and screened within the fresh/saline groundwater transition zone. Temporal EMI and monitoring well data showed a strong contraction of the freshwater lens in response to El Niño conditions, and indicated a thicker lens toward the ocean side, an opposite spatial pattern to that observed for many other Pacific islands. On an outer islet where a stand of mature Pisonia trees exist, EMI surveys revealed only a thin (<3 m from land surface) layer of brackish groundwater during El Niño. Numerical groundwater simulations were performed for a range of permeability distributions and climate conditions at Palmyra. Results revealed that the observed atypical lens asymmetry is likely due to more efficient submarine groundwater discharge on the lagoon side as a result of lagoon dredging and filling with high-permeability material. Simulations also predict large decreases (40%) in freshwater lens volume during dry cycles and highlight threats to the Pisonia trees, yielding insight for atoll ecosystem management worldwide.

Inferring watershed hydraulics and cold-water habitat persistence using multi-year air and stream temperature signals.

Streams strongly influenced by groundwater discharge may serve as "climate refugia" for sensitive species in regions of increasingly marginal thermal conditions. The main goal of this study is to develop paired air and stream water annual temperature signal analysis techniques to elucidate the relative groundwater contribution to stream water and the effective groundwater flowpath depth. Groundwater discharge to streams attenuates surface water temperature signals, and this attenuation can be diagnostic of groundwater gaining systems. Additionally, discharge from shallow groundwater flowpaths can theoretically transfer lagged annual temperature signals from aquifer to stream water. Here we explore this concept using multi-year temperature records from 120 stream sites located across 18 mountain watersheds of Shenandoah National Park, VA, USA and a coastal watershed in Massachusetts, USA. Both areas constitute important cold-water habitat for native brook trout (Salvelinus fontinalis). Observed annual temperature signals indicate a dominance of shallow groundwater discharge to streams in the National Park, in contrast to the coastal watershed that has strong, apparently deeper, groundwater influence. The average phase lag from air to stream signals in Shenandoah National Park is 11 d; however, extended lags of approximately 1 month were observed in a subset of streams. In contrast, the coastal stream has pronounced attenuation of annual temperature signals without notable phase lag. To better understand these observed differences in signal characteristics, analytical and numerical models are used to quantify mixing of the annual temperature signals of surface and groundwater. Simulations using a total heat budget numerical model indicate groundwater-induced annual temperature signal phase lags are likely to show greater downstream propagation than the related signal amplitude attenuation. The measurement of multi-seasonal paired air and water temperatures offers great promise toward understanding catchment processes and informing current cold-water habitat management at ecologically-relevant scales.

Groundwater flow estimation using temperature-depth profiles in a complex environment and a changing climate.

Obtaining reliable estimates of vertical groundwater flows remains a challenge but is of critical importance to the management of groundwater resources. When large scale land clearing or groundwater extraction occurs, methods based on water table fluctuations or water chemistry are unreliable. As an alternative, a number of methods based on temperature-depth (T-z) profiles are available to provide vertical groundwater flow estimates from which recharge rates may be calculated. However, methods that invoke steady state assumptions have been shown to be inappropriate for sites that have experienced land surface warming. Analytical solutions that account for surface warming are available, but they typically include unrealistic or restrictive assumptions (e.g. no flow initial conditions or linear surface warming). Here, we use a new analytical solution and associated computer program (FAST) that provides flexible initial and boundary conditions to estimate fluxes using T-z profiles from the Willunga Super Science Site, a complex, but densely instrumented groundwater catchment in South Australia. T-z profiles from seven wells (ranging from high elevation to near sea level) were utilised, in addition to mean annual air temperatures at nearby weather stations to estimate boundary conditions, and thermal properties were estimated from down borehole geophysics. Temperature based flux estimates were 5 to 23mmy-1, which are similar to those estimated using chloride mass balance. This study illustrates that T-z profiles can be studied to estimate recharge in environments where more commonly applied methods fail.

Post-traumatic dissection of the internal carotid artery associated with ipsilateral facial nerve paralysis: diagnostic and forensic issues.

Traumatic internal carotid artery dissection may result from a direct blow to anterolateral aspect of the neck, or an extreme extension and rotation of the neck. Traumas involved are variable ranging from high speed motor vehicle accident to trivial traumas. The most frequent presentations of carotid artery dissection are stroke, Hörner syndrome, and paralysis of a cranial nerve. Time of ischemic signs onset is very variable too, diverging from immediate to several months delay. We report the case of a 60-year-old woman, who was assaulted by a young man. Immediately, she complained of headache and posterior cervical pain. Three months later she developed a left hemifacial paralysis. MRI and MRA showed a dissection of the left internal carotid artery. The causal relationship between the trauma and the carotid artery dissection as well as forensic issues are discussed.

Viability of primary term cytotrophoblast cell culture in normoxia and hypoxia.

Cytotrophoblast (CT) cells isolated and purified from term placenta are able to differentiate into syncytiotrophoblast cells. Previous reports suggested that hypoxia is an inhibitor of this differentiation and also increases apoptosis. As visual observations of our CT cell cultures indicated a better development in hypoxia than in normoxia (defined as 2.5 and 21% O(2), respectively), we decided to assess the effect of low oxygen tension on in vitro CT cell differentiation by measuring cell viability, apoptosis and CT cell fusion and differentiation. We observed a 45% decrease in cell viability 24 h after plating both in normoxia and in hypoxia but no difference between the two oxygen conditions. Cell viability remained stable during the 4-day culture. Apoptosis also did not increase in hypoxia. Apoptotic index and caspase activation were even lower in hypoxia than in normoxia at Day 1 and Day 4 of the culture. Finally, we observed a 5-fold and 6-fold increase in Syncytin-1 mRNA expression in normoxia and in hypoxia, respectively, indicating that hypoxia did not inhibit CT cell fusion. CT cells differentiated as well in hypoxia as an increase in inhibin α subunit mRNA was evidenced during the 4-day culture. This increase was even higher in hypoxia than in normoxia. In conclusion, hypoxia defined as 2.5% O(2) based on first trimester placental pO(2) did not decrease term primary CT cell viability and did not increase apoptosis. Moreover, it did not inhibit either CT cell fusion or differentiation.

Risks of non-lethal weapon use: case studies of three French victims of stinger grenades.

The development of non-lethal weapons started in the 1960s. In France, they have been used by the police for about 10 years. We relate the cases of three French women, victims of stinger grenades, non-lethal weapons recently adopted by the French law enforcement to distract and disperse crowds. The three victims presented serious injuries requiring emergency surgical care. One lost her eye. Based on these cases, we discuss the lethal character of these weapons and propose measures to be taken to prevent their dramatic consequences. Although the danger is obviously less than for firearms, stinger grenades are nonetheless potentially lethal and cause serious physical injuries.

Rupture of the left ventricle due to blunt trauma--a pediatric case study and literature review.

Tamponade due to rupture of the chambers of the heart, in particular the left ventricle, after blunt thoracic trauma is described only sparsely in the literature. Most cases involve multiple thoracic trauma following motor vehicle accidents. We present the case study of a five-year old victim of a household accident, in which two concrete basins apparently fell on him. He died rapidly, despite attempted resuscitation. The autopsy showed essentially a hemorrhagic extravasation of the diaphragm and mediastinum, hemopericardium, and massive damage to the apex of the left ventricle. Pathological exam confirmed the traumatic origin of the cardiac rupture, with no underlying pathology. We will discuss the mechanisms described in the literature that result in such lesions, the mechanism which we believe most probable in this case, and the importance of background information. In our case study, lack of specific information concerning the accident prevents a definitive conclusion of the exact mechanism that caused this massive trauma particularly due to the fact that the external examination couldn't find any lesion in favor of a thoracic or abdominal traumatism. To our knowledge, in context of a household accident, such an isolated lesion causing almost immediate death has not previously been described in the literature.

Chronic consumption of ethanol leads to substantial cell damage in cultured rat astrocytes in conditions promoting acetaldehyde accumulation.

AIMS: This study aimed at comparing the cerebral cytotoxicity of ethanol and its main metabolite acetaldehyde after acute or chronic exposures of rat astrocytes in primary culture. METHODS: Cytotoxicity was evaluated on the cell reduction of viability (MTT reduction test) and on the characterization of DNA damage by single cell gel electrophoresis (or comet assay). RESULTS: Changes in astrocyte survival and in DNA integrity only occurred when the astrocytes were chronically exposed to ethanol (20 mM; 3, 6 or 9 days). On the other hand, viability and DNA integrity were deeply affected by acute exposure to acetaldehyde. Both effects were dependent on the concentration of acetaldehyde. The cytotoxic effect of acetaldehyde was also indirectly evaluated after modifications of the normal ethanol metabolism by the use of different inducers or inhibitors. In presence of ethanol, the concomitant induction of catalase (i.e. by glucose oxidase) and inhibition of aldehyde dehydrogenase (i.e. by methylene blue) led to acetaldehyde accumulation within cells. It was followed by both a reduction in viability and a substantial increase in DNA strand breaks. CONCLUSIONS: These data were thus consistent with a possible predominant role of acetaldehyde during brain ethanol metabolism. On the other hand, the effects observed after AMT could also suggest a possible direct ethanol effect and a role for free radical attacks. These data were thus consistent with a possible predominant role of acetaldehyde during brain ethanol metabolism. On the other hand, the effects observed after AMT could also suggest a possible direct ethanol effect and a role for free radical attacks.

Ethanol can modify the effects of certain free radical-generating systems on astrocytes.

The central nervous system is vulnerable to oxidative stress, especially when a toxicant can modify the physiological balance between anti- and pro-oxidant mechanisms. Among brain cells, astrocytes seem less vulnerable than neurons, but their impairment can dramatically affect neurons because of their protective role toward neurons. Ethanol is able to stimulate the formation of reactive oxygen species and modify the activity of most of the antioxidant agents. However, ethanol can react with the OH* radical to form the alpha-hydroxyethyl radical, which is considered to be less toxic. Ethanol also can stimulate H2O2 degradation through catalase activation. This study, therefore, sought to determine whether ethanol affected the sensitivity of astrocytes exposed to various free radical-generating systems. The cellular impact of such exposure was assessed by assays exploring cytotoxicity (i.e., NR (neutral red) and MMT (3-(4,5-dimethylthiazol-2-yl)-2,5-diphenyltetiazolium bromide) reduction assays) and genotoxicity (comet assay) induced by these treatments. DNA alterations were evaluated by single-cell gel electrophoresis (comet assay), considered a precocious biomarker of intracellular alterations. After concomitant exposure to H2O2 and ethanol, the viability of astrocytes decreased significantly whereas the mean percentage of DNA in the tail increased,reflecting DNA damage (H2O2 was either directly added to the culture medium or endogenously produced from menadione). Ethanol also reduced the loss of viability and DNA alterations after exposure to OH* radicals produced by a Fenton system. The exposure to a xanthine/xanthine oxidase system had the same effect.

Impact of ethanol and acetaldehyde on DNA and cell viability of cultured neurones.

Ethanol consumption has long been associated with brain damage. However, the mechanism underlying this deleterious effect remains unclear. Among different hypotheses, acetaldehyde is regarded by certain authors as playing a major role in the expression of ethanol toxicity, but there are still some uncertainties about the exact nature of its implication. We therefore tried to characterize the profile of the alterations of neuronal viability and DNA integrity obtained after either a direct exposure to ethanol or to acetaldehyde. Ethanol at concentrations within the range of blood alcohol levels in intoxicated humans (< or = 100 mmol/L) induced DNA alterations without any apparent effect on cell viability. Acetaldehyde (< or = 1000 micromol/L) can also induce DNA alterations but with a different profile of the DNA cellular alterations. The comparison between the distributions of the comet tail DNA indicated that ethanol induced strong breaks (tail DNA > or = 60 a.u.) generation whereas acetaldehyde rather induced lower breaks (20 < or = tail DNA < or = 50 a.u.) formation but affecting a greater number of neurones. Acetaldehyde had thus a different genotoxic potential which may suggest a different mode of action or a different cellular target. Furthermore, when a single 100 mmol/L ethanol exposure did not lead to any loss of cell viability, the addition of an inhibitor of aldehyde dehydrogenase was followed by a significant loss in viability. In contrast, the inhibition of catalase, which suppresses acetaldehyde synthesis, led to no reduced viability in the same exposure conditions. ROS also reduced viability, but this was observed only after both cytochrome P450 stimulation and catalase inhibition. These combined results could suggest that acetaldehyde may play a significant role in the expression of ethanol toxicity in brain.

Acute exposure of cultured neurones to ethanol results in reversible DNA single-strand breaks; whereas chronic exposure causes loss of cell viability.

AIMS: Ethanol can create progressive neuropathological and functional alterations of neurones. However, the influence of exposure duration is still debated. It is difficult to specify the level of alcohol consumption leading to alcohol-induced brain damage. Moreover, the mechanism of toxicity is assumed to combine direct and metabolically induced effects, although numerous uncertainties remain. Finally, the genotoxic power of ethanol has not fully been investigated in the brain. In the experiment reported herein, primary cultures of neurones were exposed either chronically or acutely to doses of ethanol within the range of blood alcohol levels in intoxicated humans. The impact on the integrity of neurones was assessed by cytotoxicity tests and DNA alterations by single-cell gel electrophoresis (Comet assay) and flow cytometry. Chronic ethanol exposure, even at a low dose, was more harmful to neurones than acute exposure. Both significant reductions in cell viability and DNA alterations were observed in this condition. On the other hand, DNA repair capacities seemed to be preserved as long as the viability measured by specific tests was not affected. Instead, neurones entered a death cell process compatible with apoptosis.

[Not Available]. / Sévices à des enfants ou insensibilité congénitale à la douleur?

Congenital insensitivity to pain is a rare illness that can cause accidental external and internal injuries in children. When child abuse is suspected, the awareness of this illness can complicate any medicolegal interpretation of findings.Several components are needed to diagnose congenital insensitivity to pain: lack of sensitivity to pain since birth; involvement of the whole body; integrity of osteotendinous reflexes; and other sensitivity processes and negative paraclinical, including histological, examinations.This article describes the case of two siblings examined during an emergency legal procedure at the forensic medicine unit of the Grenobles University Hospital Centre in France. The medico-legal interpretation of facts and examinations must be conservative in case of legal complications and must follow an analysis of the child's and family's medicosocial problems since the child's birth. The family's socioeducational support and the communication of information on this illness should be a priority to avoid any misunderstanding and overrun in the child's management and monitoring.

Effects of chronic ethanol exposure on acetaldehyde and free radical production by astrocytes in culture.

In a previous study, the production of acetaldehyde and free radicals derived from ethanol was characterized in astrocytes in primary culture. In the present study, the effects of chronic exposure on the production of both compounds as well as on the main antioxidant system were compared with those of an acute exposure. This was done to better understand the different ways the brain reacts to these modes of exposure. Under these conditions, both a time-dependent increase in the accumulation of acetaldehyde and a decreased formation of the alpha-hydroxyethyl radical were shown. This was associated with increased activities of catalase, superoxide dismutase (SOD), and glutathione peroxidase (GPX) and with decreased glutathione (GSH) content. These effects, which counteract reactive oxygen species (ROS) formation by stimulating the main enzymes of the antioxidant system, were also associated with the reduced amount of radicals derived from ethanol. This could be a beneficial effect, but this was counter-balanced by the increased rate of acetaldehyde accumulation, whose high toxicity is well known. All these effects underline the crucial role played by catalase which, on one hand converts hydrogen peroxide to water and, on the other hand, ethanol to acetaldehyde.