Kalangi Rodrigo, Nicola Nannini, Vittorio Facincani
et al.
This study presents a zooarchaeological and taphonomic analysis of the previously unstudied component of the Mousterian faunal assemblage from Unit A9 at Grotta di Fumane (northeastern Italy), offering refined insights into Neanderthal subsistence behaviour during Marine Isotope Stage 3. Building on the previously published analysis of the principal portion of the assemblage, the new data reaffirm a subsistence strategy focused on selective transport and intensive on-site processing of high-utility carcass components. The ungulate assemblage—dominated by <i>Cervus elaphus</i> and <i>Capreolus capreolus</i>, with additional contributions from <i>Rupicapra rupicapra</i> and <i>Capra ibex</i>—is characterised by the dominance of hindlimb elements, moderate cranial representation, and a pronounced scarcity of axial remains. These patterns indicate that carcass reduction commenced at kill sites, where low-yield trunk segments were removed, while high-nutritional-value limb portions were preferentially transported to the cave for secondary processing. Taphonomic indicators, including abundant cut marks, percussion notches, and extensive bone fragmentation, demonstrate systematic defleshing, marrow extraction, and possible grease rendering within the cave, activities that were spatially associated with combustion features. Occasional cranial transport suggests targeted acquisition of high-fat tissues such as brains and tongue, behaviour consistent with cold-climate optimisation strategies documented in both ethnographic and experimental contexts. Collectively, the evidence indicates that Unit A9 served as a residential locus embedded within a logistically organised mobility system, where carcass processing, resource exploitation, and lithic activities were closely integrated. These findings reinforce the broader picture of late Neanderthals as adaptable and behaviourally sophisticated foragers capable of strategic planning and efficient exploitation of ungulate prey within the dynamic environments of northern Italy.
ARTAI A. SANTOS, ANTONIO HERNÁNDEZ-ORÚE, ENRIQUE PEÑALVER
et al.
We describe Aspidothorax hispanicus sp. nov. from Gzhelian, Pennsylvanian strata of León, Spain, representing the first
occurrence of Aspidothoracidae in the Iberian Peninsula. This discovery expands the paleogeographical range of the
family, previously known only from the Russian Federation and France. The new insect is preserved in close association
with foliar remains of medullosan (Alethopteris zeilleri) and callistophytalean (Pseudomariopteris cordato-ovata) seed
ferns whose environmental preferences suggest that the new insect species inhabited humid tropical forests. The fossil
leaves bear six types of damage, probably produced by insects, belonging to three functional feeding groups: margin
feeding, hole feeding, and piercing and sucking. This diversity of interactions highlights varied feeding strategies, includ
ing chewing, piercing and sucking behaviors, evidencing a more complex range of herbivory in the area than previously
known. The stylet mouthparts of Megasecoptera make these insects strong candidates for producing the piercing and
sucking damage on the associated plants. The presence of dark patches and spots on the fossil wing, probably represents
a camouflage strategy against predators, such as Palaeodictyoptera and other active hunters. The dark wing apex might
also reflect the presence of sexual dimorphism or courtship behavior. This new assemblage of insects, in addition to
plants and plant-insect interactions, contributes to a broader paleoecological understanding of the Carboniferous forests
of the La Magdalena Coalfield.
Understanding the past dynamics of vegetation in response to climate change is crucial for predicting future ecological outcomes. This study has two primary objectives: (1) to reconstruct the vegetation history of the coastal region around Lake Lilaste in Central Latvia during the Holocene and (2) to assess the impacts of climate change on forest composition through the analysis of pollen data and radiocarbon dating. The results indicate that dominant tree species, particularly pine (<i>Pinus</i>), have shown remarkable resilience despite significant climate fluctuations. Pine’s adaptation to the sandy, mineral-poor soils surrounding the lake likely underpins its sustained dominance, while the influence of climate change on overall tree biomass is more notable. Our results suggest that vegetation may be more susceptible to future climate variability, yet the region’s geological and soil conditions continue to favor pine, birch (<i>Betula</i>), and alder (<i>Alnus</i>) populations. While human activities have influenced the region during the last millennia, their impact has been more pronounced in areas further from the lake. This study underlines the importance of long-term forest dynamics and emphasizes that the soil and geological and geographical setting must be considered for climate change assessments.
SOL A. CAVASIN, IGNACIO A. CERDA, SEBASTIÁN APESTEGUÍA
Sphenodontians are a group of vertebrates with a vast taxonomic diversity and worldwide distribution of their fossils.
Although they have been the subject of many studies on their phylogeny and morphology, those focused on their paleobiology
are still scarce. We present here the osteohistology of eleven postcranial elements corresponding to a single
specimen of Priosphenodon avelasi, an eilenodontine sphenodontian from Cenomanian–Turonian rocks of Río Negro
(Argentina). The bone samples described here share a parallel-fibered type of matrix. The degree of vascularization
varies in all the samples, but none of them present a significant density of primary vascular canals. Lines of arrested
growth were observed in all appendicular elements, being better preserved in the humerus, radius and fibula. Extrinsic
fibers were observed only in reduced regions of the cortex of the ulna and in one of the phalanges. The primary bone
tissue suggests that the specimen had a relatively low growth rate with alternation between slow and accelerated stages.
The latter could explain why this taxon reached the largest sizes of all known sphenodontians.
Abstract Ophiuroids, also known as brittle stars, are an important component of modern marine benthos, yet their fossil record is still poorly understood. Here, we describe new finds of ophiuroids from the upper Sinemurian (Lower Jurassic) of Asturias, north-west Spain. The material consists of several articulated specimens that show all relevant anatomical details to allow for an exhaustive description of a new species, Arenorbis santameraensis sp. nov., which adds a Jurassic member to the genus Arenorbis previously known exclusively from the Middle Triassic of central Europe. We demonstrate that Arenorbis has characters that are typically found in the suborder Ophiodermatina. The new Jurassic record of Arenorbis shows remarkable parallels with its Middle Triassic equivalents in terms of sedimentological and taphonomic context, suggesting niche conservatism in this genus. In contrast to its wide geographical distribution during the Middle Triassic, the new species is currently only known from a restricted area, which suggests that it represents a Jurassic relict of a formerly widespread Triassic lineage. ZooBank LSID: urn:lsid:zoobank.org:pub:D253BD9D-53C3-44BA-884B-15BA1F7876D3
Sedimentation is a leading global problem that affects the environment and dams by reducing the live storage capacity of reservoirs and the life expectance of dams. Hence, prioritizing watersheds according to the risk of soil loss is crucial for extending the useful life of dams and reservoirs. The objectives of this study were to assess sediment flow in the Genale Dawa-3 reservoir, identify subbasins that are prone to soil erosion, and evaluate the impact of different management practices on minimizing sediment yields by using the Soil and Water Assessment Tool (SWAT) model. The SWAT model was calibrated and validated by observed streamflow and sediment data based on the SUFI-2 algorithm by SWAT-CUP, and its performance was assessed. The model simulated the average annual sediment yield; the input to the reservoir was 16.83 ton/ha/yr for the period of 1990–2015. From a total of 31 subbasins, 12 were categorized from high to very severe (11–60 ton/ha/yr) sediment-yielding subbasins and selected for sediment management. The simulated scenarios showed that the average annual sediment reductions at critical erosion hot spots in subbasins after the application of filter strips, soil/stone bund, terracing, and contour farming were 35.03%, 66.54%, 80.88%, and 53.11%, respectively. Therefore, this study concluded that reducing sediment yield by implementing terracing in critical areas at risk of soil erosion was more effective than other soil conservation measures. Overall, this research can help planners and decision-makers to implement appropriate soil conservation measures in the most erosive subwatersheds in order to extend the useful life of the Genale Dawa-3 hydropower dam and reservoir.
Differential fertility preferences for men and women may provide insights into human sexual conflict. We explore whether pairbonded couples have different preferences for future offspring, which socioecological factors are associated with these preferences, and who achieves their desired fertility over time. We utilise the Indonesia Family Life Survey (IFLS), a longitudinal survey which collected data from 1993 to 2015, to compare desired future fertility for 9655 couples and follow couples who had divergent preferences. The majority of couples (64.8%) want the same number of future offspring. In 20.7% of couples, husbands want more future offspring than their wives, while the reverse occurs in 14.5% of couples. Living in villages with the husband's or the wife's parent(s) is associated with having divergent preferences for future offspring, where there is a higher likelihood that women prefer more offspring than their husbands. When examining fertility outcomes, women, particularly those who marry at older ages, are more likely to achieve their desired preference. Contrary to previous research, we do not find that living near one's natal kin or having increased autonomy increases an individual's likelihood of achieving desired fertility outcomes.
Elena A. Jagt-Yazykova, Martin Košťák, John W. M. Jagt
Abstract A newly collected specimen of the enigmatic coleoid genus Longibelus is recorded from lower Turonian strata along the River Shadrinka in Sakhalin (Russian Far East). To date, this is the first record of Late Cretaceous coleoid cephalopods from the island and, in fact, from the entire Pacific coast of the Russian Federation. Lithological characteristics, coupled with published geochemical analyses (δ13C and Corg content), suggest the habitat of this coleoid taxon to have been the middle to outer (i.e. distal) shelf. Its provenance from the stratigraphical level that is known as the Scaphites Event, characterised by a mass occurrence of Scaphites and Yesoites, may be indicative of occasional or marginal overlap in ranges, rather than life in similar habitats. On the basis of lithological features and in view of the extremely rare occurrence of Longibelus in rich ammonite assemblages with clear ecological/bathymetric preferences, the natural habitat of Longibelus may have comprised neritic to mesopelagic zones over distal shelves and slopes.
Live streaming conferences increase the participation of a diverse audience, help defray travel costs and overcome problems related to travel restrictions. In this article, we lay out tips for implementing live-streaming in scientific meetings. We also cover legal, ethical, and technical aspects implicated with live-streaming scientific talks. To write this article, we leveraged knowledge from our experience in organizing the symposium “Deciphering the Denisovans,” presented at the 88th Annual Meeting of the American Association of Physical Anthropology (AAPA) in Cleveland, OH, in 2019, as well as literature on the topic.
Jannatul Maowa Malitha, Md. Ariful Islam, Saima Islam
et al.
Abstract Background Early onset of menarche is one of the most important factors for breast cancer and other associated health hazards. The aim of this study was to investigate the early age at menarche and its associated factors in school girls (age, 10–12 years) in Rajshahi District, Bangladesh. Methods Data was collected from Rajshahi District, Bangladesh, using multistage random sampling. Independent sample t test and binary logistic regression model were used in this study. A total number of 386 school girls aged 10–12 years were considered as a sample for this study. Results This study revealed that more than 48% girls already attained menarche within the age of 12 years, among them 25.6%, 41.0%, and 58.3% girls experienced menarche at the age of 10, 11, and 12 years, respectively. It was observed that the menarcheal girls were significantly taller (p < 0.01) and heavier (p < 0.01) than non-menarcheal girls. The menarcheal girls’ mothers were heavier (p < 0.01), shorter (p < 0.01), had more BMI (p < 0.01), reached menarche (p < 0.05) earlier than non-menarcheal girls’ mothers. Menarcheal girls had less number of siblings (p < 0.01) and lower order of birth (p < 0.05) than non-menarcheal girls. After controlling the effect of other factors, multiple logistic regression model demonstrated that obese girls were more likely to attain menarche than under- [AOR = 0.279, CI 95% 0.075–0.986; p < 0.05] and normal [AOR = 0.248, CI 95% 0.082–0.755; p < 0.05] weight girls. Urban school girls had more chance to get menarche than rural school girls at same age (AOR = 0.012, 95% CI 0.003–0.047; p < 0.01). Conclusions Therefore, modern lifestyle changes may have the important factors for early age at menarche of the studied girls in Bangladesh.
Susanna Kümmell, Fernando Abdala, Judyth Sassoon
et al.
To date there is little information on carpal bone homology in late Palaeozoic and Mesozoic Synapsida. Crucial to the understanding of homology in synapsid carpal elements is the fact that different nomenclatures are used for the carpals of non-mammaliamorph Synapsida (Gegenbauer’s canonical nomenclature) and Mammaliaformes (mammalian nomenclature). The homologies of the carpals of non-mammaliamorph synapsids and mammals were established early last century and have not been reviewed since then. Here we provide a detailed study of the carpal bones of synapsids ranging in age from the early Permian to Late Cretaceous. The mammaliamorph lunate, previously considered the homologue of the intermedium of non-mammaliamorph synapsids, is interpreted here as homologous to their lateral centrale. We interpret the single mammaliamorph centrale as a homologue of the medial centrale of non-mammaliamorph synapsids. In some synapsid specimens, we found that one or two centralia are fused to the radiale (e.g., the gorgonopsian Arctognathus and tritylodontid Bienotheroides), supporting a digging habit. A third centrale is present in the therocephalian Theriognathus, very likely an abnormal duplication. An additional medial bone in a biarmosuchian was interpreted as a prepollex/ sesamoid. A cartilaginous prepollex/sesamoid may also have been present in several non-mammaliamorph synapsids, which have an open space proximal to distal carpal I. Distal carpal V is completely lost in dicynodonts and it is mainly fused to distal carpal IV in the adult stage of most other therapsid groups, but showed a delayed development in most non-mammaliamorph cynodonts. In mammaliamorphs, distal carpal V is not present. Our observations provide an updated revision of synapsid carpal homologies, mainly on the basis of position and anatomical contacts and also taking into account the results of embryological studies.
C. Stephan, Jodi M. Caple, Pierre Guyomarc’h
et al.
Abstract Facial imaging is a term used to describe methods that use facial images to assist or facilitate human identification. This pertains to two craniofacial identification procedures that use skulls and faces—facial approximation and photographic superimposition—as well as face-only methods for age progression/regression, the construction of facial graphics from eyewitness memory (including composites and artistic sketches), facial depiction, face mapping and newly emerging methods of molecular photofitting. Given the breadth of these facial imaging techniques, it is not surprising that a broad array of subject-matter experts participate in and/or contribute to the formulation and implementation of these methods (including forensic odontologists, forensic artists, police officers, electrical engineers, anatomists, geneticists, medical image specialists, psychologists, computer graphic programmers and software developers). As they are concerned with the physical characteristics of humans, each of these facial imaging areas also falls in the domain of physical anthropology, although not all of them have been traditionally regarded as such. This too offers useful opportunities to adapt established methods in one domain to others more traditionally held to be disciplines within physical anthropology (e.g. facial approximation, craniofacial superimposition and face photo-comparison). It is important to note that most facial imaging methods are not currently used for identification but serve to assist authorities in narrowing or directing investigations such that other, more potent, methods of identification can be used (e.g. DNA). Few, if any, facial imaging approaches can be considered honed end-stage scientific methods, with major opportunities for physical anthropologists to make meaningful contributions. Some facial imaging methods have considerably stronger scientific underpinnings than others (e.g. facial approximation versus face mapping), some currently lie entirely within the artistic sphere (facial depiction), and yet others are so aspirational that realistic capacity to obtain their aims has strongly been questioned despite highly advanced technical approaches (molecular photofitting). All this makes for a broad-ranging, dynamic and energetic field that is in a constant state of flux. This manuscript provides a theoretical snapshot of the purposes of these methods, the state of science as it pertains to them, and their latest research developments.
The family Cantharidae is a worldwide distributed group of flattened and soft-bodied beetles displaying aposematic
colouration. These beetles, commonly known as soldier beetles, have an extensive fossil record dating back to the
Lower Cretaceous. The majority of fossil material, referred to Cantharidae, is known from amber inclusions. In
this paper we describe and illustrate a new soldier beetle Kuskaella macroptera gen. et sp. nov. from the Baltic amber. It is characterised by pronotum of the male parallel-sided in basal third and abruptly narrowed towards apex, and
of the female gradually and steadily narrowing from the basal margin to the apex; globular head; unequal maxillary
palpomeres with the last segment elongated-globular and pointed; long elytra slightly surpassing the last abdominal
segment. This finding is the first described species of both sexes preserved in a single amber piece.
Kristian G. Jakobsen, Glenn A. Brock, Arne T. Nielsen
A bivalve-dominated molluscan fauna is described from the Darriwilian (Middle Ordovician) Stairway Sandstone, Amadeus Basin, central Australia. The fauna comprises 16 species of bivalves and rostroconchs plus six gastropod species which are treated under open nomenclature. Two new bivalves, Sthenodonta paenesymmetrica sp. nov. and Modiolopsis pojetai sp. nov., are described. The relatively low-diverse molluscan fauna constitutes around 62% of the total benthic macrofauna. Approximately 75% of the molluscs comprise bivalves, especially nuculoids, which were biogeographically restricted to low latitudes during the Ordovician. The molluscan assemblage displays a very high degree of endemism at species level, though the bivalve Sthenodonta eastii also occurs in the Georgina Basin farther to the northeast. This indicates a possible marine connective seaway between the Georgina and Amadeus basins during the Darriwilian. Nuculites, Cyrtodonta, and Modiolopsis are cosmopolitan and previously reported from North China, Avalonia, and Southern Gondwana.
Eugenio Sanz, Antonio Arcos, Carlos Pascual
et al.
This paper reports the use of FEA (Finite Element Analysis) to model dinosaur tracks. Satisfactory reproductions of sauropod ichnites were simulated using 3D numerical models of the elasto-plastic behaviour of soils. Though the modelling was done of ichnites in situ at the Miraflores I tracksite (Soria, Spain), the methodology could be applied to other tracksites to improve their ichnological interpretation and better understand how the type and state of the trodden sediment at the moment the track is created is a fundamental determinant of the morphology of the ichnite. The results obtained explain why the initial and commonly adopted hypothesis—that soft sediments become progressively more rigid and resistant at depth—is not appropriate at this tracksite. We explain why it is essential to consider a more rigid superficial layer (caused by desiccation) overlying a softer layer that is extruded to form a displacement rim. Adult sauropods left trackways behind them. These tracks could be filled up with water due to phreatic level was close to the ground surface. The simulation provides us with a means to explain the differences between similar tracks (of different depths; with or without displacement rims) in the various stratigraphic layers of the tracksite and to explain why temporary and variable conditions of humidity lead to these differences in the tracks. The simulations also demonstrate that track depth alone is insufficient to differentiate true tracks from undertracks and that other discrimination criteria need to be taken into account. The scarcity of baby sauropod tracks is explained because they are shallow and easily eroded.
Sonia Colantonio, Claudio F. Kuffer, Vicente Fuster
Una forma de estimar la consanguinidad y parentesco en poblaciones históricas es la isonimia. Este trabajo analiza la distribución de apellidos en la población blanca de la ciudad de Córdoba con datos extraídos de censos de 1795, 1813 y 1832. Se estiman indicadores de consanguinidad y parentesco por isonimia en los tres años mencionados, considerando por un lado la población adulta y por otro los matrimonios identificados. Se calculan, asimismo, indicadores de migración a partir de la distribución neutral de los apellidos. A pesar de la alta endogamia para el grupo blanco referida en los trabajos históricos, los resultados indican una escasa consanguinidad y un comportamiento marcadamente aleatorio de los apellidos en los tres casos, con valores muy similares de parentesco intrapoblacional, tanto para adultos como para casados. Se observa que los mayores valores de migración son para 1795, decreciendo en los otros censos probablemente como consecuencia de un balance entre la inmigración y procesos de emigración. Los hombres manifiestan siempre mayor movilidad geográfica; dentro de cada sexo es más acentuada entre los individuos casados.