This study presents a series of new radiocarbon dates and the first stable carbon and nitrogen isotope measurements of C3 cereal grains from Roman Iron Age (1–400 AD) archaeobotanical assemblages in Lithuania, southeastern Baltic region. These data are complemented by stable isotope measurements of faunal remains to assess local environmental conditions and evaluate human impact on the landscape through agricultural practices. The δ15N and δ13C values indicate that agriculture during this period relied heavily on intensive manuring and cultivation in open, well-irrigated landscapes. The results also reveal diverse cultivation strategies across sites, with isotopic differences between rye and barley suggesting the possible use of an infield–outfield cultivation system. Radiocarbon dates indicate that these agricultural innovations may have started as early as the 1st to mid-2nd century AD with the introduction of rye, however the evidence points to a gradual and uneven adoption rather than a rapid uniform shift.

The James Ross Basin, situated in the northwestern portion of the Antarctic Peninsula, holds one of the most complete sedimentary records of the Cretaceous, and hosts exceptionally well-preserved and diverse fossil assemblages, particularly notable for high southern latitudes. The Santa Marta Formation (Santonian–Campanian) harbors a rich decapod crustacean fauna, including Anomura, Astacidea, Achelata, Brachyura, and Glypheidea. Among brachyuran crabs, only four families have been described on James Ross Island: Homolodromiidae, Necrocarcinidae, Prosopidae, and Raninidae. This work focuses on a brachyuran from the Marambio Group, a part of the Santa Marta Formation. The material presented here was collected during the 41st Brazilian Antarctic Operation by researchers of the PALEOANTAR project. The site consists of a sequence of intercalated volcanic sandstones, siltstones, and tuffs, interpreted as a set of volcanoclastic deposits formed in a deltaic environment. The specimen described here with a well-preserved ventral surface, Sabellidromites santamarta new species, is assigned to the Dynomenidae based on uropods as calcified dorsal plates, a reduced, obliquely subdorsal fifth pereopod (fourth pereopod not reduced), and characteristics of the dorsal carapace. The occurrence of Sabellidromites santamarta n. sp. in the Santonian–Campanian of Antarctica suggests biogeographic exchanges of the dynomenid fauna between the Northern and Southern hemispheres during the Late Cretaceous.

UUID: http://zoobank.org/5c53c84a-af78-432f-ba1a-795008a3db70

Microbial O2 production via oxygenic photosynthesis was vital in oxygenating the Earth’s surface environment during the Great Oxygenation Event (GOE) ca. 2.5 to 2.3 billion years ago. However, geochemical, paleontological and genomic data suggest the emergence of oxygenic photosynthesis precedes the GOE by at least 500 million years. This demonstrates that the first appearance of microbial O2 in the environment cannot explain the timing of atmospheric oxygenation. Instead, the GOE was facilitated by Earth’s geodynamic evolution, expanding cyanobacterial habitats and the changing redox state of the mantle, decreasing the abundance of reduced surface rocks, volcanic gases and aqueous solutes. These trends ultimately resulted in magnified O2 production rates and diminished O2 consumption rates. Thus, the GOE can be understood as a misbalance between O2 sources and sinks. One of the most critical O2 sinks on modern Earth is microbial O2 consumption via aerobic respiration, and accumulating evidence suggests its emergence well before the GOE. However, the role of aerobic microorganisms as an O2 sink delaying the GOE remains poorly explored. Here, we review the redox evolution of Earth’s mantle and surface environments, as well as the Archean evolution of aerobic microbial metabolisms. Oxygenic photosynthesis released O2 to the environment, but the secular oxidation of the solid Earth was critical in allowing O2 accumulation. Aerobic respiration expanded in response to the GOE, but our survey suggests it could have been a critical O2 sink even earlier. Hence, aerobic respiration can be seen as geobiological feedback to changes in the Earth system from deep in the mantle up to the surface. However, the timing and rate of O2 consumption by aerobic respiration before the GOE remain poorly constrained. We conclude by highlighting open questions and future research directions to understand the role of the aerobic O2 sink in delaying the GOE.

In recent years, the increasing accumulation of radiocarbon dating data in Jomon research has progressed, creating a foundation for more detailed chronological estimates of the Jomon period’s high-resolution typo-chronology. However, there remains a gap between relative chronologies based on typology and radiocarbon data. A key issue arises from discrepancies between the concept of keishiki (“type” in Japanese) as a time unit of relative chronology, defined based on production period, and the radiocarbon dates, which reflect various events that occurred to the pottery after its production. To overcome the gap, this study introduced a new Bayesian chronological model, the one-sided sequential model, which sequentially orders only the start boundaries of each typological group. When this model was applied to a case study from the Middle Jomon period in the Kanto region, it estimated more reasonable date ranges for each phase of the typo-chronology than the contiguous model. Additionally, the resulting estimated duration of each pottery type was shorter during periods of higher estimated populations and longer during periods of lower estimated populations, providing new insights into the temporal aspects of Jomon society While Bayesian chronological modeling is not prevalent in Jomon research, appropriate models make it possible to make chronological estimates consistent with the high-resolution Jomon chronology, which is considered to approach a generational scale. Such attempts enable detailed clarification of various social and cultural changes. The temporality of the past thus revealed provides a new approach to a deeper understanding of Jomon society.

Positive human–wildlife coexistence, especially in contexts of rewilding and the reintroduction of large carnivores, partially depends on communication between stakeholders. The media, and in particular local journalism, can play a crucial role in determining people’s knowledge of and attitudes towards wildlife. In this article, we analyse the online coverage of bears produced by the most widely circulated local newspaper in Trentino (Italy), where bears have been reintroduced thanks to a rewilding project funded by the European Union. Employing quantitative and qualitative content analysis of 375 articles, we look into the main features of the media coverage of bears over one year (2024). We find that articles tend to focus on controversial and uncommon events, such as culls and interactions. The most prevalent sources of quotations in the articles are politicians and activists, while experts, local residents, and individuals in the farming sector are less often quoted. The majority of articles are framed through the lens of the socio-political struggle generated by bear presence. Micro-dynamics of the online media coverage include high polarisation, fragmentation of narratives, and the marginalisation of relevant stakeholders (i.e., local communities, experts, European institutions).

Punctuated equilibria (PE) was presented 50 years ago as an alternative to the widespread assumption that most evolution proceeds by gradual phyletic change within lineages. Unfortunately, PE has been widely misunderstood, misrepresented, and unfairly dismissed since this first publication. We argue that much of this misunderstanding centers around a misinterpretation of the meaning of “mode” in evolution, and its significance, properly understood, for how we understand macroevolutionary processes. PE proposed that most morphospecies do not show significant anagenetic trends through their stratigraphic ranges, and that most new morphospecies that are recognized arise via cladogenesis. To the degree that this is true, most exploration of disparity space must be associated with cladogenesis.

We surveyed a sample of the recent paleontological literature to assess the frequency with which new morphospecies appear in the fossil record via anagenesis versus cladogenesis using a persistence of ancestor criterion and found the overwhelmingly dominant mode of species origin to be cladogenesis. This is a valuable but underutilized approach to this problem, which could be exploited with more studies of species-level phylogenies of fossil taxa. Combined with the conclusions of other studies that stasis or nondirectional change is common, this finding of the dominance of cladogenesis affirms that PE is very much alive and of substantial significance for understanding macroevolutionary patterns.

The cycling of carbon in riverine systems is a critical component of global carbon cycle research. However, the sources and performances of riverine carbon in the Qinling Mountains, a pivotal hydrological nexus in China, remain poorly understood. This study investigates the seasonal variations of dissolved organic carbon (DOC) concentration in the Tianyu River within the Qinling Mountains. By utilizing a combination of carbon isotopic signatures (Δ14C-δ13C) and the stepped-combustion method, we examined the sources of DOC and the contribution ratio of each end-member. Our findings reveal that: (1) the concentrations and dual carbon isotope ratios of DOC in the Tianyu River are influenced by regional climatic factors, exhibiting distinct seasonal patterns; (2) the 14C age of DOC in the Tianyu River is comparatively older than the global average for rivers but younger than that of China’s three major rivers (the Yellow, Yangtze, and Pearl Rivers); and (3) the DOC mainly comes from exogenous sources, with a proportion of about 85.8%–88.4%. Vegetation and riverine sediments are identified as primary contributors. These findings suggest that exemplary ecological preservation exists within the Qinling region while operating within an efficient carbon cycling system. This investigation provides initial insights into how regional climatic conditions influence riverine carbon cycles and enhances our understanding of biogeochemical processes related to carbon.

The site of Stublina, first excavated in 1956 by Milutin Garašanin of the Institute of Archaeology and Radoslav Galović of the National Museum Belgrade is located at the southeast outskirts of the Supska village near the town of Ćurpija, in Central Serbia. Its location on the edge of the flood plain of the Central Balkans’ major waterway, the Velika Morava River, places it on a major corridor extending south to north, linking southern Europe and the Aegean with the Pannonian plains in the north. Based on material finds, the site predominantly belongs to the Late Neolithic and is attributable to the so-called Vinča culture complex; however, sporadic finds of Early Neolithic Starčevo type pottery and Late Medieval burials were also reported. The results of the excavation were published in a single monograph in 1979, containing information on roughly half of the excavated area. However, radiocarbon dating was never performed on the site. The site of Stublina, containing evidence for the life span of the so-called Vinča culture complex in the Velika Morava River basin, one of the most important corridors during the entire Neolithic period of Southeast Europe, is a valuable chronological beacon based on its vast material record of pottery fragments, traditionally used to construct relative chronological sequences in the past. In this paper, we present the results of contextual radiocarbon dating using Bayesian chronological modeling with 28 new AMS 14C radiocarbon dates, selected from the material archive located in the depos of the National Museum of Serbia in Belgrade. The samples were chosen from stratigraphically well-defined contexts published in the 1979 Garašanin and Garašanin volume on Supska. These contexts provide secure chronological order of layers and features, representing the entire life span of the site in the Late Neolithic period. Our results provide strong validation for archival records originating from old archaeological excavations and breathe new life into their potential for contemporary archaeological research, using techniques and methods unavailable at the time of their creation.