Micropaleontological observations on the Lower Cretaceous iron ore-related formations of the Mecsek Mts. (Upper Valanginian–Lower Hauterivian, South Hungary)

The Late Valanginian–Early Hauterivian iron ore deposit and related formations at Zengővárkony (Mecsek Mts., South Hungary) provided a relatively rich microfauna of foraminifera, crustacean microcoprolites, and sponge spicules. Benthic foraminifera are recognized in decreasing abundance: Glomospira cf. gordialis (Jones and Parker 1860), Lenticulina sp., Spirillina sp., Nodosaria sp., Epistomina sp., and Trocholina sp. A Hedbergella sp. indicates the presence of planktonic foraminifera around the ore deposit. Besides this microfauna, sponge spicules (diactine-type criccorhabds and anactine-type rhax forms) are first recorded from this environment. Rock-forming quantities of various ichnospecies of crustacean microcoprolites are recorded. Favreina hexaochetarius, Palaxius tetraochetarius, and Palaxius decaochetarius isp. provided statistically evaluated quantities in thin sections, which point to a complete crustacean ichnofauna from juveniles to adults. Four different microfossil assemblages are recognized from the Apátvarasd Limestone Fm: (a) Glomospira-dominated foraminifer assemblage, (b) diverse crustacean microcoprolite assemblage dominated by Palaxius, (c) monotypic Favreina assemblage, and (d) diverse sponge-dominated assemblage. These assemblages are similar to that of the Recent Aegean Sea hydrothermal field communities. The remains of an undetermined crinoid from dissolved rock sample may indicate a vivid sea-bottom environment

A Linear-Time Branching-Time Spectrum for Behavioral Specification Theories

We propose behavioral specification theories for most equivalences in the linear-time--branching-time spectrum. Almost all previous work on specification theories focuses on bisimilarity, but there is a clear interest in specification theories for other preorders and equivalences. We show that specification theories for preorders cannot exist and develop a general scheme which allows us to define behavioral specification theories, based on disjunctive modal transition systems, for most equivalences in the linear-time--branching-time spectrum

Systématique, phylogénie et homéomorphie des Engonoceratidae HYATT, 1900 (Ammonoidea, Crétacé) et révision de Engonoceras duboisi LATIL, 1989

Les Enganoceratidae apparaissent à l'Albien basal (ou peut-être dès l'Aptien terminal) dans les séries de plates-formes carbonatées de la marge sud de la province méditerranéenne du domaine téthysien. Leur efficacité évolutive leur permet de coloniser rapidement l'ensemble du domaine téthysien et même au delà comme le montre la présence de groupes endémiques dans le Bassin Péruvien et dans la mer intérieure occidentale des États-Unis. Plus tard, le groupe élargira encore plus son aire de distribution en envahissant certaines régions du domaine boréal (mer de Mowry, Canada). Les Enganoceratidae semblent avoir eu un mode de vie nectoplanctonique, épipélagique et sténohalin au sein de mers chaudes peu à très peu profondes (rivages, lagons), dont la fréquence a favorisé leur évolution. Ce groupe, dont l'origine est obscure, est bien individualisé. Il comprend neuf genres et une centaine d'espèces. Leur apparition semble avoir été provoquée par la crise anoxique OAE 1b et leur rapide expansion favorisée par l'extension progressive des mers chaudes et épicontinentales qui accompagne la montée des eaux du milieu du Crétacé. Le déclin des Enganoceratidae semble lié à l'accélération de la montée des mers qui caractérise la fin du Cénomanien, sans doute par modification substantielle de leurs habitats peu profonds. Ce groupe est considéré comme un colonisateur efficace et un bon indicateur de milieux de faible profondeur en ambiance transgressive. À partir de nouvelles études stratigraphiques et structurales, il est proposé une révision de l'espèce Engonoceras duboisi qui doit être rattachée au genre Parengonoceras. Par ailleurs, il est mis en évidence que le fait de présenter des sutures simplifiées de type Cératite et une coquille lancéolée à oxycône comprimé est symptomatique d'ammonites adaptées à des milieux marins peu profonds. Ce modèle est, en effet, répété trois fois au long de l'évolution des Ammonoïdes mésozoïques.The Engonoceratidae may well have originated on the shallow marine carbonate platforms of the southern margin of the Mediterranean Province of the Tethyan Realm during the earliest Albian (?latest Aptian). In the entire Tethyan Realm and beyond adaptive radiation of the group was rapid and successful during the early Albian as indicated by endemic centres in the Peruvian Basin and the Western Interior Sea (USA). Later the group successfully enlarged its distribution, and invaded some provinces (Mowry Sea, Canada) of the Boreal Realm. The mode of life of engonoceratids seems to have been nektoplanktonic, epipelagic, and stenohaline, restricted to shallow water and platform or in some cases extremely shallow (littoral and lagoonal) facies which may have helped their radiation. The group is distinctive and consists of nine genera and up to a hundred species, although its origin is still obscure. Their appearance may have been triggered by the oceanic anoxic event (OAE 1b) and their rapid rise may have been helped by their shallow water mode of life and the global mid-Cretaceous warming and rise in sea level. The fall of the engonoceratids coincides with the end-Cenomanian rapid transgression, which may have changed their shallow water habitats. Today the group is considered to have been a successful colonizer, a reliable stratigraphical indicator for shallow marine environments and a pioneer taxon for recognition of transgressive phases. Based on new material and sutural analysis, Engonoceras duboisi is revised and assigned to Parengonoceras. A set of features consisting of a simplified ceratitid suture, lanceolate and compressed oxycone shell together comprising a shallow marine ecotype is pointed out as a successful and repeated morphotype among Mesozoic Ammonoidea, for it was repeated three times during ammonoid evolution

A unique Valanginian paleoenvironment at an iron ore deposit near Zengővárkony (Mecsek Mts, South Hungary), and a possible genetic model

Abstract The spatially restricted Early Valanginian iron ore (limonite) and manganese deposit at Zengõvárkony (Mecsek Mts, southern Hungary) contains a rich, strongly limonitized, remarkably large-sized (specimens are 30–70% larger than those at their type localities) brachiopod-dominated (mainly Lacunosella and Nucleata) megafauna and a diverse crustacean microfauna, which indicates a shallow, nutrient-rich environment possibly linked to an uplifted block, and/or a hydrothermal vent

Description of the Characteristic Soil Profiles and Indication of the Degree of Sheet Erosion in Verpelét

In the administrative area of Verpelét settlement, we excavated 22 soil profiles in July and August of 2014 to show what soil types build up the area, as well as the extent of soil erosion in each profile. The description of the soil profiles was carried out based on the methods of the FAO (2006) and Novák’s Soil Practicality (2013). In the study area, we found chernozem brown forest soils (Chernozems), alluvial meadow soils (Fluvisols), humous sandy soils (Arenosols), humous alluvial soils (Fluvisols), meadow chernozem soils (Chernozems), Ramann brown forest soils (Cambisols), and brown forest soils with clay illuviation (Luvisols). We examined the sheet erosion in the vicinity of Verpelét using three methods: (1) GIS method considering slope category values, (2) examining the geomorphological character of the environment around the soil profiles, and (3) determining the sheet erosion within the specific soil profiles using the methods of Kerényi (1991) and Kerényi and Martonné Erdős (1994). The first method did not indicate any erosion-prone areas in the Verpelét vicinity; however, we were able to detect greater soil erosion in the excavated soil profiles. Using the second method, 32% of the excavated soil profiles were strongly eroded, 36% were moderately eroded, 4.5% were weakly eroded, and 27.5% showed accumulation conditions. However, our third method, which focused on specific soil profiles, indicated that 32% of the excavated soil profiles were strongly eroded, 63.5% were moderately eroded, and only 4.5% were weakly eroded. The question arises as to what causes this significant difference between the various methods, and where the significant sheet erosion in the examined profiles in Verpelét actually originates from. In order to investigate this question, we examined the 1st, 2nd, 3rd Military Survey Maps, the topographic map from 1990, the CLC18 satellite imagery and the 2023 version of Google Earth. The previously forested areas on these maps were already characterized by extensive arable land, and later by arable and vineyard areas. Today, Verpelét has become predominantly an actively cultivated agricultural landscape. Therefore, the significant sheet erosion can be attributed to the spread of inappropriate land use methods and significant anthropogenic impacts (β-euhemerobic level)

Associations between data-driven lifestyle profiles and cognitive function in the AusDiab study

Background: Mounting evidence highlights the importance of combined modifiable lifestyle factors in reducing risk of cognitive decline and dementia. Several a priori additive scoring approaches have been established; however, limited research has employed advanced data-driven approaches to explore this association. This study aimed to examine the association between data-driven lifestyle profiles and cognitive function in community-dwelling Australian adults. Methods: A cross-sectional study of 4561 Australian adults (55.3% female, mean age 60.9 ± 11.3 years) was conducted. Questionnaires were used to collect self-reported data on diet, physical activity, sedentary time, smoking status, and alcohol consumption. Cognitive testing was undertaken to assess memory, processing speed, and vocabulary and verbal knowledge. Latent Profile Analysis (LPA) was conducted to identify subgroups characterised by similar patterns of lifestyle behaviours. The resultant subgroups, or profiles, were then used to further explore associations with cognitive function using linear regression models and an automatic Bolck, Croon & Hagenaars (BCH) approach. Results: Three profiles were identified: (1) “Inactive, poor diet” (76.3%); (2) “Moderate activity, non-smokers” (18.7%); and (3) “Highly active, unhealthy drinkers” (5.0%). Profile 2 “Moderate activity, non-smokers” exhibited better processing speed than Profile 1 “Inactive, poor diet”. There was also some evidence to suggest Profile 3 “Highly active, unhealthy drinkers” exhibited poorer vocabulary and verbal knowledge compared to Profile 1 and poorer processing speed and memory scores compared to Profile 2. Conclusion: In this population of community-dwelling Australian adults, a sub-group characterised by moderate activity levels and higher rates of non-smoking had better cognitive function compared to two other identified sub-groups. This study demonstrates how LPA can be used to highlight sub-groups of a population that may be at increased risk of dementia and benefit most from lifestyle-based multidomain intervention strategies

Associations of dietary intake on biological markers of inflammation in children and adolescents: A systematic review

Background: In children and adolescents, chronic low-grade inflammation has been implicated in the pathogenesis of co- and multi-morbid conditions to mental health disorders. Diet quality is a potential mechanism of action that can exacerbate or ameliorate low-grade inflammation; however, the exact way dietary intake can regulate the immune response in children and adolescents is still to be fully understood. Methods: Studies that measured dietary intake (patterns of diet, indices, food groups, nutrients) and any inflammatory biomarkers in children and adolescents aged 2 to19 years and published until November 2020 were included in this systematic review, and were selected in line with PRISMA guidelines through the following databases: Academic Search Complete, CINAHL, Global Health, Medline COMPLETE andWeb of Science-Core Collection. A total of 53 articles were identified. Results: Results show that adequate adherence to healthful dietary patterns such as the Mediterranean diet, or food groups such as vegetables and fruit, or macro/micro nutrients such as fibre or vitamin C and E, are associated with decreased levels of pro-inflammatory biomarkers, mainly c-reactive protein (CRP), interleukin-6 (IL-6) and tumour necrosis factor-alpha (TNF-α), whereas adherence to aWestern dietary pattern, as well as intake of food groups such as added sugars, macro-nutrients such as saturated fatty acids or ultra-processed foods, is associated with higher levels of the same pro-inflammatory biomarkers. Conclusions: This is the first systematic review examining dietary intake and biological markers of inflammation in both children and adolescents. A good quality diet, high in vegetable and fruit intake, wholegrains, fibre and healthy fats ameliorates low-grade inflammation, and therefore represents a promising therapeutic approach, as well as an important element for disease prevention in both children and adolescents.A.B. and C.M.P. are funded by the UK Medical Research Council (grants MR/L014815/1, MR/J002739/1and MR/N029488/1), the European Commission Horizon 2020 (grant SC1-BHC-01- 2019) and the National Institute for Health Research (NIHR) Biomedical Research Centre at South London and Maudsley NHS Foundation Trust and King’s College London; they have also received research funding from Johnson and Johnson for research on depression and inflammation, but this paper is independent from this funding. In addition, C.M.P. is funded by the Wellcome Trust strategy award to the Neuroimmunology of Mood Disorders and Alzheimer’s Disease (NIMA) Consortium (104025), which is also funded by Janssen, GlaxoSmithKline, Lundbeck and Pfizer, but, again, this paper is independent from this funding