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Comma shrimp, or cumaceans, are diverse benthic crustaceans, yet they are one of the groups with the poorest fossil record, hindering our understanding of the evolution of the group in deep time. Here, we describe a new species of fossil comma shrimp, Makrokylindrus itoi sp. nov., from the Plio‐Pleistocene of Japan. The singular fossil is exceptionally preserved, including details of the carapace, cuticle, and some appendages, and it represents the first known fossil of the family Diastylidae and only the fourth fossil crown group cumacean known to date. We suggest that the scarce and sparsely known fossil record of cumaceans likely reflects a lack of recognition due to their small size and unfamiliar anatomy, making fossil cumaceans easy to misidentify, be confused with crustacean larvae of unknown affinities, or be interpreted as fragments of other crustaceans (taxonomic bias), rather than a lack of fossilization potential (taphonomic bias). [ABSTRACT FROM AUTHOR]

Langebaanweg is a Mio‐Pliocene locality located on the West Coast of South Africa. It is renowned for its rich diversity of both terrestrial and marine vertebrate fossils. Several carnivorans have been identified from this site, amongst which is the recently described jackal‐like canid, Eucyon khoikhoi. One of the skeletons assigned to E. khoikhoi exhibits anatomical deformities on several bones of the skeleton. Here, we use multiple methodologies (anatomical descriptions, CT scanning and histology) to investigate the bony overgrowths or exostoses evident in the radius, and we compare these findings with those of a radius from a healthy individual of the same species from Langebaanweg. Our results show that anatomical observations are important for first level observation of the pathology, but that micro‐CT scanning permits a more precise assessment of how the pathology affected the internal organization of the bone, both periosteally and endosteally. This methodology permitted us to diagnose the tumors as benign rather than cancerous. Our observations of calcified cartilage in the histological thin sections in the region of the exostosis allowed us to further diagnose the exostosis as an osteochondroma. This study has demonstrated the usefulness of applying multiple techniques to characterize and diagnose pathological bony growths in a fossil canivoran. We have also demonstrated the usefulness of histological studies in permitting a more refined diagnosis of the exostosis as an osteochondroma. [ABSTRACT FROM AUTHOR]

Dinomyidae is a South American group of caviomorph rodents with a single extant species (Dinomys branickii), but with a rich fossil record including medium-sized to giant species, which reached its peak diversity during the Late Miocene. The dinomyids from the Cerro Azul Formation (late Middle Miocene to Early Pliocene) have been studied in detail from localities in La Pampa Province, Argentina. In this contribution, dinomyids from Chasicoan Stage/Age (Late Miocene) levels of the Cerro Azul Formation at Arroyo Chasicó locality (Buenos Aires Province, Argentina) are revised, including previously published material and unpublished ones. We confirm the presence of Tetrastylus sp. Diaphoromys gamayensis, and define two new taxa, Bondesiomys chasiquensis gen. et sp. nov. and Gyriabrus sokka sp. nov. The diversity of dinomyids from the Cerro Azul Formation at Arroyo Chasicó is higher than other Chasicoan faunas at the same latitude, identified in localities of La Pampa Province, since in Cerro Patagua there are not Dinomyidae records and in Cerro la Bota Tetrastylus sp. and Dinomyidae indet. were the only recorded taxa. [ABSTRACT FROM AUTHOR]

A fungal palynomorph corresponding to the fossil-species Lirasporis intergranifer R. Potonié & S.C.D. Sah, from the Middle Miocene lignite mine in Tomisławice (central Poland), is considered as the new combination Cancellidium intergraniferum (R. Potonié & S.C.D. Sah) G. Worobiec & E. Worobiec, comb. nov. The fossil-genus Lirasporis is treated as a synonym of the modern genus Cancellidium Tubaki. Cancellidium intergraniferum from the Miocene of Poland represents the first fossil record of Cancellidium outside Asia, the first record of this genus from Europe, and the northernmost known fossil occurrence of Cancellidium. Living representatives of Cancellidium seem to prefer warm and humid climates and, being aero-aquatic hyphomycetes, are usually associated with decaying woody remains in aquatic environments. A similar ecology is suggested for the fossil C. intergraniferum, which could be a reliable fungal non-pollen palynomorph proxy for palaeoclimatic and palaeoenvironmental reconstructions. [ABSTRACT FROM AUTHOR]

The predation-driven Mesozoic marine revolution (MMR) is believed to have induced a dramatic change in the bathymetric distribution of many shallow marine invertebrates since the late Mesozoic. For instance, stalked crinoids – isocrinids (Isocrinida) have undergone a striking decline in shallow-sea environments and today they are restricted to deep-sea settings (below 100 m depth). However, the timing and synchronicity of this shift are a matter of debate. A delayed onset of MMR and/or shifts to a retrograde, low-predation community structure during the Paleogene in the Southern Ocean were invoked. In particular, recent data from the Southern Hemisphere suggest that the environmental restriction of isocrinids to the deep-sea settings may have occurred at the end of the Eocene around Antarctica and Australia, and later in the early Miocene in New Zealand. Here, we report the anomalous occurrence of the isocrinids in shallow nearshore marine facies from the middle Miocene of Poland (Northern Hemisphere, Central Paratethys). Thus, globally, this is the youngest record of shallow-sea stalked crinoids. This finding suggests that some relict stalked crinoids may have been able to live in the shallow-water environments by the middle Miocene, and further confirms that the depth restriction of isocrinids to offshore environments was not synchronous on a global scale. [ABSTRACT FROM AUTHOR]

New fossil remains of Rhinocerotidae, dated from the early Late Miocene, were discovered from the lowermost part of the Irrawaddy Formation in the Tebingan area, Magway Region, central Myanmar. The Tebingan rhinoceros fossils, consisting of isolated teeth, maxillae, and mandibles, are assigned to three taxa: Brachypotherium perimense defined by a constricted protocone, a well-developed parastyle and broad upper teeth, to 'Brachypotherium' fatehjangense with a flat ectoloph, crochet, and the absence of tubercle at the entrance of the median valley. Other specimens were assigned to Rhinoceros sp. due to having a developed parastyle, crochet and a strong anterior cingulum and the absence of a constricted protocone and ante-crochet. The evolutionary history of Rhinocerotidae is poorly known in Southeast Asia, and few rhinoceros' species have been identified from the Irrawaddy Formation. The newly identified Rhinoceros specimens from the early Late Miocene Tebingan area are the oldest fossil records for Rhinoceros in Southeast Asia. The Tebingan mammal fauna is similar to the Nagri and Dhok Pathan faunas of the lower/middle Siwaliks of the Indian subcontinent, indicating the faunal exchange between these two regions in the late Neogene. [ABSTRACT FROM AUTHOR]

The Late Miocene vertebrate fauna from the Entre Ríos Province, Argentina, comes from two units: the marine Paraná Formation and the Lower Member of Ituzaingó Formation (LMIF). This latter includes a lower conglomerate set, with fine quartz gravel, and clay and chalcedony clasts, and fossil remains, traditionally known as ‘Mesopotamiense’ or ‘Conglomerado osífero’. We present new fossil vertebrate remains from the LMIF at the Puerto Víboras locality (Hernandarias, Entre Ríos Province) including Leptodactylus sp. (Amphibia, Anura), Crocodylia indet. Caimaninae indet. and Paranasuchus gasparinae (Alligatoridae), Chelidae indet. (Testudines, Pleurodira), Chelonoidis sp. (Testudines, Cryptodira), Plohophorus paranensis (Cingulata, Glyptodontidae), and Macraucheniinae indet. (Macraucheniidae, Litopterna). The record of Leptodactylus sp. represents the oldest record of the genus and the first amphibian record for the Neogene of the Entre Ríos Province. The material described herein and assigned to Chelonoidis sp. allows to confirm for the first time the presence of a testudinid in the Late Miocene of the Entre Ríos Province. [ABSTRACT FROM AUTHOR]

The Indo-West Pacific is home to a diverse array of modern fish species, and the study of their fossils can provide valuable insights into the origins and evolution of this biodiversity. This report presents rare remains of five individuals of acropomatiform fish, including a semi-articulated skeleton, recovered from the Upper Kueichulin Formation (Lower Pliocene) in northern Taiwan. The fossils are preserved in the form of nodules discovered at the locality known for abundant marine crustaceans and echinoderms. These specimens can be assigned to the family Stereolepididae, based on morphology of the opercle with the presence of two spines, a preopercle characterized by serrations on the posterior margin and denticulations on the ventral margin, and a distinctive skull architecture. Differences in skull morphology distinguish these specimens from other species within the genus and thus are described as Stereolepis arcanum n. sp. Significantly, the species represents the oldest known record of the family globally and stands as the second known fossil representative. This discovery not only enhances our understanding of the palaeobiodiversity of fish fauna in the Indo-West Pacific during the Neogene, but also highlights the importance of further research efforts in this area. [ABSTRACT FROM AUTHOR]

Otters, subfamily Lutrinae (Mustelidae), are predators that thrive in aquatic environments, and have a semiaquatic to fully aquatic lifestyle. While modern otters are found across the globe, their fossil history is limited, primarily documented by fragmented dentognathic remains. In this work, we report on and describe new dental remains of a medium-sized Lutrinae from the Late Miocene of Baccinello and Casteani (Tuscany), improving the poor fossil record of the subfamily in Europe. Tyrrhenolutra helbingi Hürzeler, 1987 is a poorly known species, described on some dental remains from the Baccinello mines and a few other localities. Considering its peculiar morphology, it has often been overlooked in the scientific literature. Description of the material stored at the Naturhistorisches Museum, Basel and Museo di Geologia e Paleontologia dell’Università di Firenze offers new insights on the intraspecific variability and dental morphology of this taxon. The comparative study of these findings highlights several morphological and biometrical similarities between T. helbingi and Paludolutra maremmana Hürzeler, 1987, which allow us to redefine these taxa as Tyrrhenolutra maremmana nov. comb. We carried out a total-evidence cladistic analysis seeking support for morphometric and morphological similarities between T. “helbingi” and “P.” maremmana. The resulting parsimony analyses support the synonymy, excluding a close relationship of T. maremmana with Paludolutra of Italy and Spain, as previously thought. Furthermore, we confirm a long-forgotten hypothesis identifying Limnonyx Crusafont Pairó, 1950 as the possible continental ancestor of Tyrrhenolutra. [ABSTRACT FROM AUTHOR]

Very few remains of elapid snakes are known from the Iberian Peninsula, but these include a probable endemic extinct species of cobra, Naja iberica from the Late Miocene. We here describe isolated cobra vertebrae from several Middle–Late Miocene localities in the Vallès‐Penedès Basin (Catalonia, Spain). All of these fossils are herein referred to an indeterminate species of the genus Naja. These remains are the first conclusive evidence that cobras were present in Iberia before the Messinian Salinity Crisis, and that they persisted there throughout the Miocene (and ultimately until the Pliocene). Recently, a phylogeny of extinct Naja based on cranial and vertebral morphology recognized N. iberica as a distinct lineage separate from the Central European one, represented mainly by Naja romani. However, due to taxonomic uncertainties, it is still unclear whether Iberian cobras were all part of a single lineage or whether several Naja lineages inhabited the Iberian Peninsula. They went extinct in Iberia before the end of the Pliocene. In the Vallès‐Penedès Basin, cobras were living in a mosaic environment, surviving through different phases characterized by different environmental features. [ABSTRACT FROM AUTHOR]

Abstract The predation-driven Mesozoic marine revolution (MMR) is believed to have induced a dramatic change in the bathymetric distribution of many shallow marine invertebrates since the late Mesozoic. For instance, stalked crinoids – isocrinids (Isocrinida) have undergone a striking decline in shallow-sea environments and today they are restricted to deep-sea settings (below 100 m depth). However, the timing and synchronicity of this shift are a matter of debate. A delayed onset of MMR and/or shifts to a retrograde, low-predation community structure during the Paleogene in the Southern Ocean were invoked. In particular, recent data from the Southern Hemisphere suggest that the environmental restriction of isocrinids to the deep-sea settings may have occurred at the end of the Eocene around Antarctica and Australia, and later in the early Miocene in New Zealand. Here, we report the anomalous occurrence of the isocrinids in shallow nearshore marine facies from the middle Miocene of Poland (Northern Hemisphere, Central Paratethys). Thus, globally, this is the youngest record of shallow-sea stalked crinoids. This finding suggests that some relict stalked crinoids may have been able to live in the shallow-water environments by the middle Miocene, and further confirms that the depth restriction of isocrinids to offshore environments was not synchronous on a global scale.

Abstract The Terminal Fusarium Clade (TFC) is a group in the Nectriaceae family with agricultural and clinical relevance. In recent years, various phylogenies have been presented in the literature, showing disagreement in the topologies, but only a few studies have conducted analyses on the divergence time scale of the group. Therefore, the evolutionary history of this group is still being determined. This study aimed to understand the evolutionary history of the TFC from a phylogenomic perspective. To achieve this objective, we performed a phylogenomic analysis using the available genomes in GenBank and ran eight different pipelines. We presented a new robust topology of the TFC that differs at some nodes from previous studies. These new relationships allowed us to formulate new hypotheses about the evolutionary history of the TFC. We also inferred new divergence time estimates, which differ from those of previous studies due to topology discordances and taxon sampling. The results suggested an important diversification process in the Neogene period, likely associated with the diversification and predominance of terrestrial ecosystems by angiosperms. In conclusion, we presented a robust time-scale phylogeny that allowed us to formulate new hypotheses regarding the evolutionary history of the TFC.

Abstract In this contribution, we investigate two sparassodonts from the Sarmiento Formation (Colhuehuapian Age; Early Miocene) recovered at the Patagonian locality of Sacanana, Chubut Province, Argentina. The first specimen (MACN-Pv CH1911), identified as Sipalocyon externus, is an almost complete cranium with upper dentition. The second specimen (MACN-Pv CH40), referred to Borhyaena macrodonta, consists of a fragmentary rostral portion of the face with associated m3–m4. The cranium of S. externus was studied through µCT-scanning to investigate its internal anatomy and infer paleoecological aspects of olfaction and hearing. In general, the endocranial anatomy and encephalization quotient are like those of other metatherians. We report the presence of an accessory transverse diploic sinus that has not previously been described in marsupials. Elements of the nasal cavity (e.g., turbinals, ossified nasal septum, cribriform plate) of S. externus exhibit features that are widespread among marsupials. Sense of olfaction, as evaluated from the cribriform plate and the 3D models of the olfactory bulbs, appears to have grossly resembled that of the domestic cat, a well-researched therian proxy. The dimensions of the tympanic membrane, as estimated from the preserved ectotympanic, suggest that the optimal hearing frequency of S. externus would have been similar to that of extant carnivorous marsupials. In sum, our study suggests that S. externus was a typical small-bodied (2–3 kg) hypercarnivorous metatherian that primarily relied on vision to hunt its prey, complemented by other sensory capabilities (olfaction and hearing), in a similar manner to small felids.

The Terminal Fusarium Clade (TFC) is a group in the Nectriaceae family with agricultural and clinical relevance. In recent years, various phylogenies have been presented in the literature, showing disagreement in the topologies, but only a few studies have conducted analyses on the divergence time scale of the group. Therefore, the evolutionary history of this group is still being determined. This study aimed to understand the evolutionary history of the TFC from a phylogenomic perspective. To achieve this objective, we performed a phylogenomic analysis using the available genomes in GenBank and ran eight different pipelines. We presented a new robust topology of the TFC that differs at some nodes from previous studies. These new relationships allowed us to formulate new hypotheses about the evolutionary history of the TFC. We also inferred new divergence time estimates, which differ from those of previous studies due to topology discordances and taxon sampling. The results suggested an important diversification process in the Neogene period, likely associated with the diversification and predominance of terrestrial ecosystems by angiosperms. In conclusion, we presented a robust time-scale phylogeny that allowed us to formulate new hypotheses regarding the evolutionary history of the TFC. [ABSTRACT FROM AUTHOR]

• First record of Miocene large-sized vertebrate coprolites from the western India. • Geochemical analyses confirm phosphatic character of ichnofossils. • Biotic inclusions confirm omnivorous diet of the chelonian producer. • Overall data suggest coprolites were deposited in coastal marine settings. In this paper, we provide the first data on large (cm-sized) coprolites (represented by three morphotypes) comprising a rare occurrence of eight specimens from a total of three vertebrate-bearing horizons identified within the Early Miocene (Aquitanian) Khari Nadi Formation and Middle Miocene (Burdigalian-Langhian) Chassra Formation, Kutch Basin, western India. The geochemical data confirm the phosphatic character of the investigated ichnofossils. The dominance of partly digested bone matter and presence of plant remains in all the three coprolite morphotypes reflects the omnivorous diet of the producers, which were most likely chelonians. The occurrence of an inclusion (in a coprolite specimen recorded in this study) showcasing an ultrastructure similar to mammalian dental enamel is a rarity in Neogene coprolite records. Additional biotic inclusions observed in the investigated coprolites include ostracods (assigned to genera Paractinocythereis, Hermanites, and Propontocypris); large planispiral benthic foraminifera including the genus Quinqueloculina ; uniserial and biserial benthic foraminifera belonging to genus Textularia ; marine calcareous algae genus Actinoporella ; chrysophytes (resting spores or cysts of planktonic algae); sponge spicules (represented by the morphotypes Acanthoxea and Strongyle); freshwater diatom genus Aulacoseira ; unidentified fungal remains; and phytoliths. Taken together, the biotic and abiotic (e.g., pyrite) inclusions, geochemical data and associated microbiota suggest that these ichnofossils were deposited in a dominantly coastal marine (intertidal) setting linked to a lacustrine/palustrine environment. [ABSTRACT FROM AUTHOR]

Aim: The response of South American seasonally dry tropical forest (SDTF) and savanna species to the Quaternary climate changes is still poorly understood. Here we use multi‐model inference approach to compare the phylogeography and demographic history of five trumpet tree species (also known as pau‐d'arco) and draw general biogeographical patterns: Handroanthus impetiginosus, H. ochraceus, H. serratifolius, Tabebuia aurea and T. roseoalba. Location: Amazonia, Atlantic Forest, Cerrado and Caatinga ecoregions, South America and Brazil. Taxa: Bignoniaceae, Tabebuia Alliance, trees. Methods: We compiled genetic data, occurrence records and ecological niche modelling (ENM) from published articles. We used coalescent modelling to test patterns of co‐divergence, and analysed niche breadth and overlap and spatial patterns in genetic diversity using quantile regressions. Results: Species showed concordant lineage divergence times in the Pleistocene. Lineage diversification and phylogeographical patterns are more related to species niche breadth than to biome (savanna or SDTF). Differences in genetic diversity among species matches the expected for the demographic scenarios obtained with coalescent simulations and ENMs: species with wider range expansion during the Last Glacial Maximum had higher diversity than species with range retraction or multiple refugia. Main Conclusions: Diversification burst in the Pliocene, and major diversification of lineages during the Pleistocene seems to be a general pattern in SDTF and savannas in the South America. The high number of haplotypes at the Central Brazil, corresponding to the Cerrado ecoregion, highlights the importance of Protected Areas for SDTFs and savannas, highly threatened biomes in Brazil. [ABSTRACT FROM AUTHOR]

Eolian sediments are extensively distributed across the Earth's surface, and their formation is intricately linked to climate change, tectonic activity, and topographic features. Consequently, the investigation of eolian sediments bears great geological significance. The northwest region of China is renowned for hosting the most extensive and thickest Late Miocene–Pliocene red clay deposits globally. Nonetheless, scholars have yet to reach a consensus regarding the precise formation processes of these red clays. The identification of the source region of the red clays is crucial for comprehending their formation mechanism. The correlation of zircon U-Pb age spectra is a frequently utilized method for determining the provenance of eolian sediments. In this study, we compared the previously published zircon U-Pb ages (n = 12,918) of the Late Miocene–Pliocene red clays in the Ordos Plateau with those from the potential provenance regions (n = 24,280). The analysis, supported by the tectonic and climatic background of the region, revealed that the Late Miocene–Pliocene red clay in the Ordos Plateau originates predominantly from the Yellow and Wei rivers, with a minor contribution from the weathering of bedrock in the western North China Craton. The transport of these detrital materials by the East Asian winter monsoon is impeded by the presence of the Qinling and Taihang Shan, resulting in their deposition on the flat surface of the Ordos Plateau. This development of red clay is consistent with the proximal accumulation model, illustrating how the hydrosphere, atmosphere, and lithosphere interacted to shape the red clay deposits during the Late Miocene and Pliocene periods in the Ordos Plateau. [ABSTRACT FROM AUTHOR]

Chalicotheres are enigmatic perissodactyls that had large claws instead of hooves. The present study concerns the material of Chalicotheriidae from the Late Miocene hominid locality of Hammerschmiede in Germany. The HAM 5 fossil site (11.62 Ma) consists of six isolated dental and postcranial chalicothere elements. Based on the morphology and dimensions of the dentition, the material can be assigned to the chalicotheriine Anisodon sp. This genus is the most common representative of Chalicotheriidae in Central Europe during the Middle Miocene but becomes much rarer during the Late Miocene. The HAM 4 fossil site (11.44 Ma) has yielded a patella belonging to a schizotheriine and a skull fragment that could possibly also belong to a schizotheriine. Thus, the schizotheriine and the chalicotheriine occur in different horizons in Hammerschmiede. Both taxa probably had a rather similar diet but different locomotion, and their disparate occurrences are most plausibly associated with environmental differences among the two fossiliferous levels. [ABSTRACT FROM AUTHOR]

The correct selection of the value of p is a complex and iterative procedure that requires experience in the interpretation of the obtained interpolated maps. Inverse Distance Weighting is a method applied to the porosities of the K and L hydrocarbon reservoirs discovered in the Neogene (Lower Pontian) subsurface sandstones in northern Croatia (Pannonian Basin System). They represent small and large data samples. Also, a standard statistical analysis of the data was made, followed by a qualitative–quantitative analysis of the maps, based on the selection of different values for the power distance exponent (p-value) for the K and L reservoir maps. According to the qualitative analysis, for a small data set, the p-value could be set at 1 or 2, giving the optimal result, while for a large data set, a p value of 3 or 4 could be applied. For quantitative analysis, in the case of a small data set, p = 2 is recommended, resulting in a root mean square error value of 0.03458, a mean absolute error of 0.02013 and a median absolute deviation of 0.00546. In contrast, a p-value of 3 or 4 is selected as appropriate for a large data set, with root mean square errors of 0.02435 and 0.02437, mean square errors of 0.01582 and 0.01509 and median absolute deviations 0.00896 and 0.00444. Eventually for a small data set, it is recommended to use a p-value of 2, and for a large data set, a p-value of 3 or 4. [ABSTRACT FROM AUTHOR]

In this contribution, we investigate two sparassodonts from the Sarmiento Formation (Colhuehuapian Age; Early Miocene) recovered at the Patagonian locality of Sacanana, Chubut Province, Argentina. The first specimen (MACN-Pv CH1911), identified as Sipalocyon externus, is an almost complete cranium with upper dentition. The second specimen (MACN-Pv CH40), referred to Borhyaena macrodonta, consists of a fragmentary rostral portion of the face with associated m3–m4. The cranium of S. externus was studied through µCT-scanning to investigate its internal anatomy and infer paleoecological aspects of olfaction and hearing. In general, the endocranial anatomy and encephalization quotient are like those of other metatherians. We report the presence of an accessory transverse diploic sinus that has not previously been described in marsupials. Elements of the nasal cavity (e.g., turbinals, ossified nasal septum, cribriform plate) of S. externus exhibit features that are widespread among marsupials. Sense of olfaction, as evaluated from the cribriform plate and the 3D models of the olfactory bulbs, appears to have grossly resembled that of the domestic cat, a well-researched therian proxy. The dimensions of the tympanic membrane, as estimated from the preserved ectotympanic, suggest that the optimal hearing frequency of S. externus would have been similar to that of extant carnivorous marsupials. In sum, our study suggests that S. externus was a typical small-bodied (2–3 kg) hypercarnivorous metatherian that primarily relied on vision to hunt its prey, complemented by other sensory capabilities (olfaction and hearing), in a similar manner to small felids. [ABSTRACT FROM AUTHOR]

The diagenetic evolution of sandstone is very complicated under the conditions of high temperatures and pressures in deep-water, deep-buried regimes, which have great influence on reservoir quality. This study investigates the typical reservoir target of Neogene deep-water, submarine-fan sandstones under high-temperature, high-pressure regimes in the Qiongdongnan Basin, South China Sea. Utilizing a thin section, scanning electron microscope (SEM), mineral geochemistry combined with burial history evolution, complex diagenetic events, and main controlling factors of the sandstone in the Neogene Meishan Formation were determined. The results show that the evolution of sandstone reservoirs is initially controlled by depositional framework compositions and subsequently modified by eogenetic and mesogenetic alterations during progressive burial. Eogenetic alterations mainly include the following: (1) mechanical compaction; (2) dissolution of feldspar; (3) low-Fe calcite cementation. Mesogenetic events were identified as the following: (1) dissolution of feldspar; (2) ferroan calcite and ankerite formation; (3) precipitation of quartz and clay mineral. Mechanical compaction is greatly influenced by the original depositional framework composition, and sandstone samples enriched in high contents of detrital clay matrix always experienced extensive mechanical compaction. Different phases of carbonate cement during different diagenetic regimes lead to continuous destruction on reservoir porosity. The dissolution of unstable feldspar minerals during eogenetic and mesogenetic environments leads to the development of secondary porosities and would enhance the quality of the reservoir. Overpressure formation is pervasively developed owing to early disequilibrium compaction and subsequent natural gas charging. Only well-sorted sandstones with low contents of detrital clay matrix could resist early mechanical compaction, lead to ample residual original porosities, and then undergo extensive mineral dissolution to generate sufficient secondary porosities. Subsequently, these porosities would be effectively protected by overpressure formation. Poor-sorted sandstones with high contents of detrital clay matrix would experience strong mechanical compaction and extensive destruction of original porosities. Thus, these sandstones are difficult to have significant dissolution and are unable to be effectively protected by overpressure formation. Therefore, the interplay between the original framework composition and the corresponding diagenetic pathways coupled with overpressure formation would result in strong reservoir heterogeneity for the deep-buried sandstones during progressive burial. [ABSTRACT FROM AUTHOR]

The remarkable uplift of the Tibetan Plateau in the Neogene had great impacts on the climate and environment of East Asia and even the world. Therefore, establishment of the Neogene stratigraphic framework of the Tibetan Plateau is of great significance to research in various fields of geosciences. Based on marine sediments, the international chronostratigraphic system of the Neogene is divided into six stages in the Miocene and two stages in the Pliocene. Since the beginning of the Cenozoic, the share of terrestrial strata on continents has increased rapidly. By the Neogene, it had far exceeded that of marine strata, and almost all deposits on the Tibetan Plateau and its surrounding areas were terrestrial strata. In China, the Miocene includes five stages and the Pliocene includes two stages. Except for the Tunggurian of the Miocene, which has a lower boundary at 15 Ma, the other stages have the same paleomagnetic definitions and time intervals as the corresponding international marine stages. Mammalian fossils play a very important role in the division and correlation of Cenozoic terrestrial strata, and rodent, carnivore, proboscidean, perissodactyl and artiodactyl fossils are especially important in Neogene terrestrial biostratigraphy. There are many basins with well-exposed strata and abundant mammalian fossils in the Tibetan Plateau. The lower boundary stratotype sections of the Neogene Xiejian and Bahean stages are located respectively in the Xining and Linxia basins, and there are precise paleomagnetic dates in coordination with mammalian fossils. The lower boundary stratotypes of other stages can also be effectively determined in the Tibetan Plateau. Many first appearing mammalian genera in East Asia also appeared in the Tibetan Plateau and its surrounding areas, especially in the Linxia Basin on the northeast margin and in the Siwaliks on the southwest margin. Among them, Prodeinotherium first appeared at the bottom of the Miocene in the Siwaliks, and the earliest Hipparion of the Old World first appeared at the bottom of the Bahean Stage in the Linxia Basin. Carbon and oxygen isotope analysis of enamel and paleosols of Cenozoic sediments and mammal fossils in the Tibetan Plateau and its surrounding areas have been used to reconstruct the climate, environment and vegetation development characteristics, and revealed that these changes were not only related to global change, but also had regional features. Evidence of the Late Miocene C4 plant expansion event based on carbon isotope changes comes from the southern margin of the Tibetan Plateau, but in sharp contrast, δ13C indicates that there was still no clear or significant C4 plant signal on the northern margin of the Tibetan Plateau until the end of the Neogene. The δ18O analysis shows that there were several major climate change events in the Cenozoic, especially in the Late Miocene at about 7 Ma, when positive drift of δ18O indicates that the northern and southern sides of the Tibetan Plateau were changing to drier environments. The strong uplift of the Tibetan Plateau in the Late Miocene strengthened the thermal contrast between sea and land, which strengthened monsoon circulation and led to the expansion of C4 vegetation in South Asia. However, the East Asian summer monsoon, which can bring atmospheric precipitation and a climate suitable for C4 plants to northern China, was not enough to affect the northern Tibetan Plateau. The Tibetan Plateau on the whole rose to an altitude of about 3000 m in the Miocene, becoming a barrier to mammalian migration; it reached its modern altitude of more than 4000 m in the Pliocene, thus forming a cryosphere environment, which led to the emergence of ancestral types of the Ice Age fauna. [ABSTRACT FROM AUTHOR]

Fossil concentrations are a conspicuous feature of the Monte León Formation (Lower Miocene), providing the opportunity to carry out combined sedimentological and paleontological studies that allow elucidating the processes involved in its genesis and contributing to the knowledge of the depositional paleoenvironment. With these objectives, the stratigraphic, sedimentological, and paleontological features of fossil concentrations containing turritelline gastropods were analyzed in rocks exposed at Restinga Norte (Santa Cruz Province). Four representative samples were extracted, and the taphonomic features of recovered turritelline specimens were analyzed in the laboratory. The textural analysis of the sediments that make up the matrix of the concentrations and the adjacent beds was also carried out. The results allowed them to be classified as "turritelline-dominated assemblages" constituting mixed biogenic-sedimentologic concentrations, with characteristics given by the behavior of the turritellines and their final reworking within the habitat. The abundance of turritellines and the diversity of bryozoans as sclerobionts suggest a habitat of nutrient-rich marine waters, probably associated with upwelling. The good preservation and the high percentage of empty shells—together with the characteristics of the sediment—suggest that their accumulation on the bottom was favored by a low-energy environment. These shells would have been oriented by a unidirectional current that promoted —favored also by a high sedimentary supply—their rapid burial and preservation. The results established that the turritelline-dominated assemblages were formed in a shallow marine shelf in the transition between the retrogradational and progradational facies of the transgressive-regressive cycle proposed for the Monte León Formation in the study area. Las concentraciones fósiles son un rasgo conspicuo de la Formación Monte León (Mioceno Inferior), proveyendo la oportunidad de realizar estudios sedimentológicos y paleontológicos combinados que permitan dilucidar los procesos involucrados en su génesis y contribuir al conocimiento del paleoambiente depositacional. Con estos objetivos, se analizaron los rasgos estratigráficos, sedimentológicos y paleoecológicos de concentraciones fósiles con gasterópodos Turritellinae, presentes en Restinga Norte (provincia de Santa Cruz). Se extrajeron cuatro muestras representativas y se analizaron en laboratorio los rasgos tafonómicos de los especímenes de turritélidos recuperados. Adicionalmente, se realizó el análisis textural de los sedimentos que conforman la matriz de las concentraciones y de los niveles adyacentes. Los resultados permitieron clasificarlas como ensambles dominados por gasterópodos Turritellinae ("turritelline-dominated assemblages"), constituyendo concentraciones mixtas biogénico-sedimentológicas, con características dadas por el comportamiento de los turritélidos y su retrabajo final dentro del hábitat. La abundancia de turritélidos junto con la diversidad de briozoos como esclerobiontes sugieren un hábitat de aguas marinas ricas en nutrientes, probablemente asociado a surgencia de aguas profundas. La buena preservación y el alto porcentaje de conchillas vacías, junto con las características del sedimento sugieren que su acumulación sobre el fondo fue promovida en un ambiente de baja energía. Éstas habrían sido orientadas por una corriente unidireccional promoviendo, en conjunto con un alto aporte sedimentario, su enterramiento rápido y preservación. Los resultados obtenidos sugieren que los ensambles se formaron en una plataforma marina somera, en la transición entre las facies retrogradantes y progradantes del ciclo transgresivo-regresivo propuesto para la Formación Monte León en el área de estudio. [ABSTRACT FROM AUTHOR]

Abstract Otoliths are common and diverse in the Neogene of tropical America. Following previous studies of Neogene tropical American otoliths of the lanternfishes (Myctophidae), marine catfishes (Ariidae), croakers (Sciaenidae), and cusk-eels (Ophidiiformes), we describe here the otoliths of the gobies (Gobiidae). The Gobiidae represent the richest marine fish family, with more than 2000 species worldwide and about 250 in America. In the fossil record too they are the species richest family in the Neogene of tropical America. We have investigated otoliths sampled from Ecuador, Pacific and Atlantic Panama, Atlantic Costa Rica, Dominican Republic, Venezuela, and Trinidad, ranging in age from late Early Miocene (late Burdigalian) to late Early Pleistocene (Calabrian). Most of the studied material originates from the collection expeditions of the Panama Paleontology Project (PPP). Our study represents the first comprehensive record of fossil gobies from America, and we recognize 107 species, of which 51 are new to science, 35 are in open nomenclature, and 19 represent species that also live in the region today. Previously, only two fossil otolith-based goby species have been described from the Neogene of tropical America. The dominant gobies in the fossil record of the region are from the Gobiosomatini, particularly of genera living over soft bottoms or in deeper water such as Bollmannia, Microgobius, Antilligobius, and Palatogobius. Another purpose of our study is to provide a first comprehensive account of otoliths of the extant Gobiidae of America, which we consider necessary for an adequate identification and interpretation of the Neogene otoliths. We studied otoliths of 130 extant American gobiid species and figured 106 of them for comparison. We also present a morphological analysis and characterization of the extant otoliths as a basis for the identification of fossil otoliths. Problems that commonly arise with the identification of fossil otoliths and specifically of fossil goby otoliths are addressed and discussed. A comparison of the history of the Gobiidae in tropical America reveals a high percentage of shared species between the Pacific and the Atlantic basins during the Late Miocene (Tortonian and Messinian) from at least 11 to 6 Ma. A recording gap on the Pacific side across the Pliocene allows a comparison again only in the late Early Pleistocene (Calabrian, 1.8 to 0.78 Ma), which shows a complete lack of shared species. These observations support the effective closure of the former Central American Seaway and emersion of the Isthmus of Panama in the intervening time. Groups that today only exist in the East Pacific were also identified in the Miocene and Pliocene of the West Atlantic, and there is also at least one instance of a genus now restricted to the West Atlantic having occurred in the East Pacific as late as the Pleistocene. The evolution of gobies in tropical America and the implications thereof are extensively discussed. Furthermore, observations of fossil gobies in the region are discussed in respect to paleoenvironmental indications and paleobiogeographic aspects.

The history of the Paratethys and its inhabiting organisms was profoundly influenced by its connections with the Global Ocean. As the sea‐straits linking Paratethys with the ocean expanded, they integrated the Paratethys with the global ocean, causing its water level to mirror the global eustatic fluctuations. These intervals of increased ocean connectivity existed during most part of the Oligocene–Early Miocene, in the Early Badenian–Tarkhanian, and in the Late Badenian–Konkian, when also fostered favourable environments for marine life to flourish in the Paratethys. When the marine connections became unstable and the sea‐straits closed (e.g., in the second half of Rupelian–Solenovian time, late Ottnangian–Kozakhurian, middle Badenian–Karaganian and from the onset of the Sarmatian up to the Pliocene), transformed into vast lacustrine waterbodies where water levels and salinities were controlled by the balance between river runoff and precipitation versus evaporation. Excess of water led to the basin expansion and brackish conditions, while deficits caused contraction and fragmentation. This resulted in hypersaline basins and lagoons co‐existing with freshwater lakes, creating diverse environments and faunas that hindered effective biostratigraphic correlations. These fluctuations caused the decline of the marine biota, leaving behind only euribiontic organisms capable of enduring drastic shifts in salinity, ion composition, and oxygen levels. Over time, these survivors diversified and gave rise to endemic faunal communities adapted to the brackish environments. The history of the faunistic and phytoplankton composition of the Carpathian part of the basin (Central Paratethys) became noticeably different from the Euxine‐Caspian ones from the beginning of the Neogene, which led to different stratigraphic schemes of these parts of the Paratethys. In recent decades, our focus has centred on refining our understanding of the Eastern Paratethys paleogeography. While the periods of high base levels in the Eastern Paratethys are well‐documented, the significant base‐level drops during isolation phases have often been overlooked. This was primarily because, until recently, there were no effective methods for reconstructing the paleogeography and geo ‐ chronology of Paratethys during these episodes of base‐level drops. However, with the advancements in seismic stratigraphy and the utilization of integrated magneto‐bio‐stratigraphy, we now possess the means to explore the scale and spatial distribution of paleogeographic changes, particularly during the substantial basin reductions in partial desiccation periods. Large regressions (during second part of the Rupelian, terminal Tarkhanian, and Sarmatian in the Eastern Paratethys and during early Pliocene in the Caspian basin) erode parts of sedimentary layers, forming surfaces of inconsistency between geological bodies accumulated before and after the sea‐level drop, which can be traced on seismic profiles as erosion boundaries. By deciphering such surfaces and the depth of river incisions flowing into the basin, it is now possible to reconstruct the relief picture resulting from these erosions and quantify the depth of baselevel drops in the Paratethys during the largest regressions.

Vladimir Laskarev (1868–1954) Russian and Serbian geologist strongly influenced geological literature by introducing a scientific term Paratethys for the series of intercontinental water basins separated from the Mediterranean Sea and the World Ocean by the Alpine orogeny. Laskarev’s scientific activity in the Russian Empire (1890‐s – 1919) was based in the University of Odessa. As an active university professor Vladimir Laskarev contributed to the geological mapping of the western provinces of Imperial Russia and to regional Neogene geology and paleontology of the Odessa and Bessarabian regions. Several of Laskarev’s students became well‐known geologists and paleontologists during the Soviet era. Vladimir Laskarev’s contribution to geological studies in Serbia between 1920–1953 is extremely important. During his life in Belgrade, he published twice as many papers on various aspects of Neogene and Quaternary geology and paleontology. His most important contribution is certainly the official introduction of the term Paratethys into geological science. The steady spread of this term in scientific literature began in the early 1940‐s and reached its peak in 1970–1980‐s during international Neogene correlation and mapping projects.

Otoliths are common and diverse in the Neogene of tropical America. Following previous studies of Neogene tropical American otoliths of the lanternfishes (Myctophidae), marine catfishes (Ariidae), croakers (Sciaenidae), and cusk-eels (Ophidiiformes), we describe here the otoliths of the gobies (Gobiidae). The Gobiidae represent the richest marine fish family, with more than 2000 species worldwide and about 250 in America. In the fossil record too they are the species richest family in the Neogene of tropical America. We have investigated otoliths sampled from Ecuador, Pacific and Atlantic Panama, Atlantic Costa Rica, Dominican Republic, Venezuela, and Trinidad, ranging in age from late Early Miocene (late Burdigalian) to late Early Pleistocene (Calabrian). Most of the studied material originates from the collection expeditions of the Panama Paleontology Project (PPP). Our study represents the first comprehensive record of fossil gobies from America, and we recognize 107 species, of which 51 are new to science, 35 are in open nomenclature, and 19 represent species that also live in the region today. Previously, only two fossil otolith-based goby species have been described from the Neogene of tropical America. The dominant gobies in the fossil record of the region are from the Gobiosomatini, particularly of genera living over soft bottoms or in deeper water such as Bollmannia, Microgobius, Antilligobius, and Palatogobius. Another purpose of our study is to provide a first comprehensive account of otoliths of the extant Gobiidae of America, which we consider necessary for an adequate identification and interpretation of the Neogene otoliths. We studied otoliths of 130 extant American gobiid species and figured 106 of them for comparison. We also present a morphological analysis and characterization of the extant otoliths as a basis for the identification of fossil otoliths. Problems that commonly arise with the identification of fossil otoliths and specifically of fossil goby otoliths are addressed and discussed. A comparison of the history of the Gobiidae in tropical America reveals a high percentage of shared species between the Pacific and the Atlantic basins during the Late Miocene (Tortonian and Messinian) from at least 11 to 6 Ma. A recording gap on the Pacific side across the Pliocene allows a comparison again only in the late Early Pleistocene (Calabrian, 1.8 to 0.78 Ma), which shows a complete lack of shared species. These observations support the effective closure of the former Central American Seaway and emersion of the Isthmus of Panama in the intervening time. Groups that today only exist in the East Pacific were also identified in the Miocene and Pliocene of the West Atlantic, and there is also at least one instance of a genus now restricted to the West Atlantic having occurred in the East Pacific as late as the Pleistocene. The evolution of gobies in tropical America and the implications thereof are extensively discussed. Furthermore, observations of fossil gobies in the region are discussed in respect to paleoenvironmental indications and paleobiogeographic aspects. [ABSTRACT FROM AUTHOR]

Premise of research. The genus Carya is a classic example of the eastern North American–eastern Asian disjunct distribution, but its biogeographic history is not well understood because many species present in the Cenozoic of Europe have ambiguous relationships to extant species. Methodogy. The morphology and anatomy of fossil nuts of C. ventricosa (Sternberg ex Brongniart) Unger from the Miocene of Salzhausen, Germany, of eight extant Carya species, and of four extant Juglans species were investigated using micro–computed tomography scanning. Carpological characteristics were analyzed using VG Studio for comparison. The morphological characters of 25 other Carya fruit fossils known from the literature were studied for comparison. Pivotal results. The peripheral course of the placental bundles within the primary septum of C. ventricosa confirms its identity to the genus Carya and distinguishes it from Juglans and from other genera of the Juglandaceae. Detailed comparison of carpological morphology and anatomy indicates that C. ventricosa is readily distinguished from extant North American species and more closely resembles the East Asian tropical C. poilanei ; both have a prominent low-density layer and/or prominent lacunae in the nutshell and contrast with other species in lacking a sharply defined pair of internal longitudinal ribs. The well-developed secondary septum in C. poilanei differs from the weakly developed, nearly absent secondary septum in C. ventricosa. The cuneate base of the locule distinguishes C. ventricosa from all extant species. Conclusions. Carya poilanei is the closest extant species to C. ventricosa. Europe might have been a key center of Cenozoic diversification and served as the ancestral area of the extant East Asian Carya lineages. [ABSTRACT FROM AUTHOR]

United Nations protection programmes under the UNESCO’s Global Geopark initiatives have resulted in the establishment and recognition of 195 Global Geoparks in 48 countries to sustainably protect Geoheritage. Given an inclusive approach with local communities and the geoscientific communities as stakeholders, the UNESCO Global Geopark concept has gained popularity in India. Further, India provides a diverse range of geoheritage in terms of rock records from the Precambrian to the Holocene. The Kachchh region (western India) has tremendous scope to be conserved under the UNESCO Geopark programme as it sustains many plausible geosites. Of the numerous geosites within Kachchh, the “Palasava” locale holds geoheritage potential as it exposes ~ 14 million-year-old Chassra Formation sedimentary succession that is well-known to yield vertebrate (including marine and terrestrial mammals) fossils. These fossils hold significance in the context of origin and diversification of middle Miocene vertebrates (including mammals), Neogene biochronology of Kutch, palaeobiogeographic scenarios involving various vertebrate groups, and related aspects. In a geotourism context, the Palasava locale presents picturesque views being located between the Wagad Highland and the Little Rann of Kutch. In addition to local religious and cultural features, the Kachchh (= Kutch) region is globally well-recognized for the “Wild Ass Sanctuary” and the “Rann Utsav”– “Festival of the Rann.” Owing to its unique Geoheritage and geotourism potential, we herein, propose Palasava locale as a “geosite” within the “Kachchh Geopark” to protect and conserve this geologically significant locale, to enhance sustainable geotourism in the region for the economic benefit of the local population and for the public to cherish. [ABSTRACT FROM AUTHOR]

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There are now many examples in the fossil record of shark bite marks preserved on biogenic materials including coprolites, ammonoids, sea star ossicles, an echinoid, and bone and calcified cartilage. These exceptional fossils document evidence of exploratory behavior, active predation, and/or scavenging. However, only a small subset report on the presence of shark teeth embedded in fossilized bone or cartilage. Although a few shark tooth-marked seal bones are known from the fossil record, no direct evidence of predation or scavenging in the form of a shark tooth embedded in a fossil seal bone has yet been documented. Herein, we describe the first shark tooth embedded in a seal (Phocidae Gray, 1821) bone, a calcaneum (CMM-V-6964), that was surface collected in Mosaic's South Fort Meade Mine, Hardee County, Fort Meade, Florida, United States. The isolated bone originated from within the Bone Valley Member of the Peace River Formation (Hawthorn Group). The partial tooth is identified as having come from an Early Pliocene great white shark, Carcharodon carcharias (Linnaeus, 1758). This discovery also represents the first C. carcharias tooth ever found embedded in a fossil bone. The embedded tooth may have come about as a result of active predation or scavenging. The extant macropredatory sharks, Carcharodon carcharias (great white shark), Notorynchus cepedianus (Péron, 1807) (sevengill shark), Somniosus microcephalus (Bloch & Schneider, 1801) (the Greenland shark), and Somniosus antarcticus Whitley, 1939 (sleeper shark), are known to actively prey upon seals (Pinnipedia Illiger, 1811). If this peculiar fossil association resulted from active predation, the seal did not survive the encounter because there is no evidence of healing in the area around the embedded shark tooth. [ABSTRACT FROM AUTHOR]

To date, the phocid fossil record from the Western Atlantic includes representatives of the subfamilies Monachinae and Phocinae. New partial postcranial bones (humerus, innominate) of true seals from the Meherrin River, Murfreesboro, Hertford County, North Carolina, U.S.A. are morphologically examined in detail. The newly discovered postcranial bones are compared to representatives of other pinnipeds (Phocidae, Otariidae, and Odobenidae) and to representatives from other phocid subfamilies (Cystophorinae, Devinophocinae, Monachinae, and Phocinae). Detailed morphological analyses demonstrate characteristics that are known to be phocid-specific, such as: the humeral deltoid crest extending to half its length, becoming thinner towards the distal portion; short and flattened femur, with a diaphysis that is broader at its distal end; and absence of femoral lesser trochanter. Taxonomic assessment identified the humerus as Phocanella pumila (Subfamily Phocinae), and the three innominate bones (Subfamily Monachinae): Homiphoca capensis, Sarcodectes magnus, and a newly discovered genus and species Seronectes meherrinensis. In the same collection, a fossil femur from the Chesapeake Group, St. Marys Formation, Maryland-Virginia is identified as Homiphoca capensis (Subfamily Phocinae). This study further confirms the likely presence of adaptively diverse phocids from either the subfamily Monachinae or Phocinae in the same locality during the Miocene time. [ABSTRACT FROM AUTHOR]

This study documents palynomorph assemblages from the Oligocene through the Early Miocene, across the significant Warm-house to Cool-house transition, using a subsurface section from the AG-5 well, north Western Desert of Egypt. Although the Paleogene and Neogene strata occupied a large area of the land, little about vegetation and ecosystem processes that shaped the climate and biodiversity during this time window is known. Here, based on a comprehensive palynological analysis of the Oligocene to Early Miocene Dabaa and Moghra formations encountered in the AG-5 well, we show that the studied area was characterized by a humid tropical to subtropical climate during the Oligocene-Miocene time interval. The obtained results provide clear evidence of the poorly known Paleogene-Neogene ecosystem in North Africa. In terms of palynostratigraphical framework, three palynozones covering the late Oligocene-Early Miocene interval are recognized. Moreover, the recovered palynomorphs inferred a deposition of the Dabaa Formation under a normal marine, inner shelf to littoral environment. However, for the basal part of the Moghra Formation, a deposition in an offshore marine environment, outer shelf (high sea level, 100–200 m depth) is assumed, whereas a deposition in shallow coastal lagoons, estuary, or delta environment (low sea level) is presumed for its uppermost part. [ABSTRACT FROM AUTHOR]

We present new interpretations and mapping that define the distribution, extent, and sediment thickness of 25 primarily offshore sedimentary basins within New Zealand’s Exclusive Economic Zone (EEZ) and Extended Continental Shelf (ECS). These basins cover ∼1.64 million km2 of the ∼5.8 million km2 (∼28%) of New Zealand’s offshore territory. The sedimentary basins formed in different tectonic settings. Most initially formed during the mid- to Late Cretaceous in either a rift-related setting during Gondwana break-up, or within or atop the paleo Gondwana subduction margin. Others formed due to the onset of mid-Paleogene sea-floor spreading, or are related to Neogene–Quaternary subsidence driven by subduction processes. Slight to significant late Paleogene to Quaternary tectonic overprints are pervasive in basins located within the Hikurangi subduction margin’s deformation zone. Knowledge of the distribution and extent of these basins was refined during the multi-year ‘Atlas of Petroleum Prospectivity’ research programme, which builds upon many decades of previous research. New digital structure, isochore, and paleogeographic maps, along with annotated seismic reflection profiles, have been developed where data coverage has allowed, using a consistent set of age-equivalent seismic horizons tied to the New Zealand Geological Timescale. Maximum total sediment thickness of ∼11 km occurs in Taranaki Basin. [ABSTRACT FROM AUTHOR]

Lamiinae (Cerambycidae, Coleoptera) is a striking subfamily due to its members' economic importance and role in the forest ecosystem. Morphological diversity, worldwide distribution and species richness complicate its already intricate phylogenetic relationships. We implemented Maximum Likelihood (ML) and time-scaled Bayesian Inference (BI) analyses to the species from East of Marmara Basin, Türkiye, from the tribes Acanthocinini, Acanthoderini, Agapanthiini, Batocerini, Dorcadionini, Lamiini, Mesosini, Monochamini, Phytoeciini, Phrynetini, Pogonocherini (including Exocentrini) and Saperdini using partial mitochondrial cytochrome c oxidase-I (COI) and 16S rRNA and nuclear 28S rRNA gene regions (2257 base pair alignment length) and Neighbor-Joining (NJ) and ML analysis to the global COI gene region dataset (658 bp). The most recent common ancestor (MRCA) of Lamiinae members included in the analyses was dated ~ 127 million years ago (Mya) in the Cretaceous. The MRCA of Dorcadionini, Lamiini and Monochamini was younger than the common ancestors of the other close tribes. There was a concurrence between resolutions of ML and BI on the affiliations of Dorcadionini and Monochamini to Lamiini and the proximity of Batocerini to Lamiini, Acanthocinini to Acanthoderini, Phrynetini to Pogonocherini, and Phytoeciini to Saperdini. The COI-based NJ and ML gene trees suggest that the closest relatives of most of the sampled Lamiinae species from the East of Marmara Basin were the European conspecifics or congeners. Our results support Dorcadionini and Monochamini as synonyms of Lamiini; and Phytoeciini of Saperdini. Also, they suggest that the emergence of the living tribes included in this study was during the Paleogene, and their intrageneric diversifications occurred during the Cenozoic, mostly the Neogene. [ABSTRACT FROM AUTHOR]

Western Anatolia is one of the fastest-extending continental regions. The approximately N-S extension, in three phases, generated grabens of various ages and trends. The first phase occurred during the late Oligocene-Early Miocene and caused the exhumation of the high‐grade metamorphic rocks in the footwall of the low‐angle detachment fault(s). This phase caused the NNE trending grabens, particularly in the northern areas. The second phase happened in the Late Miocene. The initial rise of the central horst (the Bozdağ Horst) bounded by the detachment faults corresponds to this extension. The third phase generated the dominant morphotectonic entities of western Anatolia, the E-W trending normal faults, and the associated grabens in Quaternary. Western Anatolia began rotating counter-clockwise since the westerly escape of the Anatolian Plate reached the region and caused the generation of the NE-NW trending conjugated strike-slip faults and the consequent grabens along the coastal areas in the Holocene. [ABSTRACT FROM AUTHOR]

[Display omitted] • We determined UMVC eruption ages and developed a petrogenetic model for MVC. • Oceanic island basalt-type alkaline magmatic genesis and evolution were explored. • Early decarbonation processes in Precambrian subduction zones are implicated. • Carbon-rich marine sediments impact eastern China's alkaline basalts. The chemical composition of eastern North China Craton (NCC)'s alkaline basaltes likely influenced by subducting Pacific Plate. Nonetheless, the influence of these processes on the western craton remains uncertain due to the lack of geochemical evidence. The recent discovery of Ulanqab maar volcanic cluster (UMVC) in the western NCC has become significant research windows. However, their petrogenesis and magmatic processes remain poorly understood. In the present study, 40Ar/39Ar, whole rock and mineral geochemistry, and Sr–Nd–Mg isotope data for the UMVC in the western NCC are reported. These data reveal that the UMVC was formed during the Neogene (7.60 ± 0.04 Ma), diverging from Quaternary basalts or as part of the Hannuoba basalts (eastern Ulanqab). The UMVC rocks, featuring typical oceanic island basalts traits with moderate (87Sr/86Sr)i values (0.70487–0.70524) and ε Nd (t) values from −4.95 to + 0.82, likely originated from an enriched EMI-type mantle source during the mid-Proterozoic. This involved mixing melts from 30 to 50 % partial melting of garnet lherzolite and 5–15 % partial melting of garnet pyroxenite in a deep magma chamber. Crystallization of clinopyroxene and garnet in this chamber created high-Ti alkaline lavas, with limited presence in erupted lavas due to sluggish magma ascent in the profound lithospheric mantle. In shallower lithospheric mantle regions, interactions between alkaline magma and orthopyroxenite improved transport kinetics, enabling clinopyroxene and olivine crystallization under lower pressure. These magmas integrated mafic crystal mushes from accumulation chambers. The study also identified a low Mg isotope composition (δ26Mg = − 0.56 ‰ to − 0.42 ‰) in samples, suggesting a hybrid source influenced by early decarbonation in Precambrian subduction zones. This finding indicates the incorporation of Mg-rich carbonate minerals from marine sediments into the magma source, contributing to the observed variations in eastern China's alkaline basalts. [ABSTRACT FROM AUTHOR]

Contrasting with their current ranges in the Antarctic and subantarctic zones, the fossil record reveals that phocids (true and elephant seals) inhabited widespread subtropical regions across the Southern Hemisphere in the geologic past. At least four extinct phocid taxa have been described from Miocene and Pliocene fossiliferous levels in Chile and Peru, constituting two of the taxonomically richest phocid assemblages known. Still, some Chilean remains morphologically differ from those recovered from Peru, suggesting an unprecedented phocid diversity. We examined phocid mandibular remains from the Bahía Inglesa Formation in northern Chile. We identified the occurrence of the long-snouted seal Acrophoca longirostris, a morphologically distinguishable and undescribed form of Acrophoca, and Hadrokirus martini, an extinct phocid with a robust feeding morphology, constituting the first record of this taxon outside Peru. We also recognised four other indeterminate phocids with considerable morphological differences from contemporaneous taxa. Moreover, one of these specimens uniquely combines morphological attributes distinct from all known extant and extinct phocids, likely corresponding to a new taxon. These reports significantly increase the taxonomic and morphological diversities of fossil seals from the eastern South Pacific and emphasise the substantial transformations of phocid assemblages over geologic time. [ABSTRACT FROM AUTHOR]

The sedimentary basins in the Continental Rift of Southeastern Brazil (CRSB) provide an opportunity for ichnological analyses due to its well-known facies relationships and paleoenvironmental interpretations. This study reports invertebrate trace fossils from the Neogene fluvial deposits (Floriano Formation) and applies integrated ichnological and facies analyses to reconstruct the environmental conditions recorded in this lithostratigraphic unit. Fieldworks revealed a rich ichnofauna in the Floriano Formation, whose facies associations have been interpreted as indicative of meandering river environments. Four sedimentary facies were identified, including bioturbated sandstone, horizontally stratified sandstone, laminated sandstone, and mudstone. Six ichnogenera were identified, Arenicolites, Beaconites, Camborygma, Palaeophycus, Skolithos, and Taenidium. Those ichnogenera occur as Skolithos, Taenidium, and Beaconites ichnocoenoses. The Skolithos ichnocoenosis is primarily represented within sand bar deposits, indicating arthropod colonization in abandoned channels. The Taenidium ichnocoenosis, which is observed within mudstone layers and presents Camborygma burrows, suggests transitional environments between aquatic and subaerial conditions, locally with high water table levels. The Beaconites ichnocoenosis indicates changes in substrate consistency associated with progressive desiccation and extended exposure time. Therefore, the identified ichnocoenoses, combined with the analysis of physical sedimentary structures, suggest generally humid conditions during colonization by invertebrates of the meandering river deposits of the Floriano Formation. [ABSTRACT FROM AUTHOR]

Otters, subfamily Lutrinae (Mustelidae), are predators that thrive in aquatic environments, and have a semiaquatic to fully aquatic lifestyle. While modern otters are found across the globe, their fossil history is limited, primarily documented by fragmented dentognathic remains. In this work, we report on and describe new dental remains of a medium-sized Lutrinae from the Late Miocene of Baccinello and Casteani (Tuscany), improving the poor fossil record of the subfamily in Europe. Tyrrhenolutra helbingi Hürzeler, 1987 is a poorly known species, described on some dental remains from the Baccinello mines and a few other localities. Considering its peculiar morphology, it has often been overlooked in the scientific literature. Description of the material stored at the Naturhistorisches Museum, Basel and Museo di Geologia e Paleontologia dell’Università di Firenze offers new insights on the intraspecific variability and dental morphology of this taxon. The comparative study of these findings highlights several morphological and biometrical similarities between T. helbingi and Paludolutra maremmana Hürzeler, 1987, which allow us to redefine these taxa as Tyrrhenolutra maremmana nov. comb. We carried out a total-evidence cladistic analysis seeking support for morphometric and morphological similarities between T. “helbingi” and “P.” maremmana. The resulting parsimony analyses support the synonymy, excluding a close relationship of T. maremmana with Paludolutra of Italy and Spain, as previously thought. Furthermore, we confirm a long-forgotten hypothesis identifying Limnonyx Crusafont Pairó, 1950 as the possible continental ancestor of Tyrrhenolutra.

Abstract The sedimentary basins in the Continental Rift of Southeastern Brazil (CRSB) provide an opportunity for ichnological analyses due to its well-known facies relationships and paleoenvironmental interpretations. This study reports invertebrate trace fossils from the Neogene fluvial deposits (Floriano Formation) and applies integrated ichnological and facies analyses to reconstruct the environmental conditions recorded in this lithostratigraphic unit. Fieldworks revealed a rich ichnofauna in the Floriano Formation, whose facies associations have been interpreted as indicative of meandering river environments. Four sedimentary facies were identified, including bioturbated sandstone, horizontally stratified sandstone, laminated sandstone, and mudstone. Six ichnogenera were identified, Arenicolites, Beaconites, Camborygma, Palaeophycus, Skolithos, and Taenidium. Those ichnogenera occur as Skolithos, Taenidium, and Beaconites ichnocoenoses. The Skolithos ichnocoenosis is primarily represented within sand bar deposits, indicating arthropod colonization in abandoned channels. The Taenidium ichnocoenosis, which is observed within mudstone layers and presents Camborygma burrows, suggests transitional environments between aquatic and subaerial conditions, locally with high water table levels. The Beaconites ichnocoenosis indicates changes in substrate consistency associated with progressive desiccation and extended exposure time. Therefore, the identified ichnocoenoses, combined with the analysis of physical sedimentary structures, suggest generally humid conditions during colonization by invertebrates of the meandering river deposits of the Floriano Formation.

The Miocene deposits of the Carpathian Foreland yielded marine vertebrate remains in numerous fossil localities. Various authors have described a fauna composed of pinnipeds, sea birds, turtles, bony fish, and cetaceans. This fauna is characteristic to the Paratethys epicontinental sea. The family Cetotheriidae appears to have included most baleen whale taxa that lived in the Eastern Paratethys in general, and in the Dacian Basin in particular, during the Miocene. In the Dacian Basin, several Miocene cetotheriid occurrences have been mentioned so far, yet remain scarce. The aim of this work is to describe previously unpublished cetotheriid remains housed at the Museum of Oltenia Craiova and to provide an updated distribution of the cetotheriid fossil localities from the Dacian Basin. [ABSTRACT FROM AUTHOR]

The present study focuses on calcareous nannofossil biostratigraphy of the last 23 Myr in the Mediterranean region and is intended as a review paper in which an updated zonation is presented. This includes the improvements in biostratigraphic classification achieved in the last decades. The proposed biozonal scheme incorporates the biochronologic data derived from the integration of biostratigraphically useful events with radiometric datings, magnetostratigraphy and astronomically tuned cyclostratigraphy. This biochronology directly derives by previous compilations and includes improved data and ages derived from recent studies based on high resolution quantitative analysis of nannofossil assemblages. The presented zonal scheme consists of 21 biozones and 35 subzones spanning the last 23 Myr, named according to the well-established code-system MNN (Mediterranean Nannofossil Neogene) for the Miocene and Pliocene time interval and MNQ (Mediterranean Nannofossil Quaternary) for the Pleistocene and Holocene. In addition, a revision of the nannofossil biostratigraphy at the Oligocene/Miocene transition is given, with the introduction of Zone MNP26 (Mediterranean Nannofossil Paleogene), as a result of the different age assigned to the Oligocene/Miocene chronostratigraphic boundary. This zonation provides a significant bio-chronostratigraphic resolution of about 0.5 Myr, corresponding to a degree of precision functional for dating sedimentary successions and, therefore, useful for geological studies (e.g. geological mapping, temporal scanning of geological phasis). The biostratigraphic resolution can be furtherly improved through integration with the analogous scheme recently established for planktonic foraminifers. [ABSTRACT FROM AUTHOR]

The results of a taxonomic and morphological revision of Mionetta natator (Milne-Edwards, 1867) from the lower Miocene of Western and Central Europe are presented. It is shown that the collections of small ducks from the Saint-Gérand-le-Puy localities (France) do indeed contain a small species of the genus Mionetta, which is here described as Mionetta defossa sp. nov. However, Mionetta natator represents a separate taxon, and is here assigned to the genus Caerulonettion gen. nov., showing morphological similarities with extant Malacorhynchus and fossil Mioquerquedula spp. The first small ducks from the lower Miocene of Kazakhstan are also described (Aral Formation, the Agyspe and Altynshokysu localities; Akzhar Formation, the Golubye Peski locality), tentatively attributed to Mionetta defossa and Mionetta sp. The diversity and relationships of small ducks of the Early and Middle Miocene of Eurasia are discussed. [ABSTRACT FROM AUTHOR]

Although Pliocene temperature and pCO2 are similar to those predicted in the IPPC RCP4.5 scenario, the distribution of coral reefs in the center of maximum coral diversity, the Coral Triangle, during this period has not been explored. We discovered a significantly lower occurrence of reefs during the Pliocene, which we refer to as the Pliocene Reef Gap, but this decrease was not associated with a drop in coral genus richness. While some of the multiple local causes that drove this decline, such as sea level rise, are analogs to drivers of Anthropocene reef decline, neither warming nor increasing pCO2 are among them. [ABSTRACT FROM AUTHOR]

The genus Castanea, divided into seven extant species of trees worldwide, includes the American chestnut, C. dentata. This once common North American tree has been nearly eliminated from the landscape due to the appearance of chestnut blight early in the Twentieth Century. Castanea has a long history as a component of palynological assemblages, though megafossil paleobotanical remains are quite rare. The distributions of what are believed to be Castanea pollen as they have been derived from coastal plain and near-shore sediments dating back to the Neogene of the coastal plain of the southeastern US are discussed. The abundances of Castanea pollen in microfossil preparations are carefully considered relative to the concept of 'pollen sum' and while it appears that the trees were quite abundant as components of coastal woodlands during the Neogene, the actual number of pollen we found in samples is quite low. American chestnut trees continued to be important into the late Pleistocene and through the time when humans first occupied both coastal and inland areas of the southeastern US. [ABSTRACT FROM AUTHOR]

Recently collected carnivoran specimens from the Siwalik Group of Pakistan are described and discussed. These specimens add to our knowledge of the previously known taxa while also adding to our biogeographic, stratigraphic, and temporal knowledge of the carnivorans from the Siwaliks. At least eight distinct taxa are identified, and although most specimens are fragmentary, some hyaenid specimens are identified further (e.g. Lycyaena and Ictitherium). We identify and describe the first herpestid fossils from the Chinji Formation, the first hyaenid (Lycyaena cf. L. dubia) from the Tatrot Formation, and the first definitive occurrence of Ictitherium (Ictitherium cf. I. viverrinum) from the Dhok Pathan Formation. We report the first occurrences of several taxa from various sites in the Siwaliks of Pakistan, including the first reports of any carnivorans from Dhok Milan, Kohtehra, and Lawa. Individual sites show a wide range of carnivoran biodiversity, however larger scale trends are more discernible when comparing those between formations in the Siwaliks. Several taxa disappear over time from the carnivoran fauna of the Siwaliks, starting with barbourofelines, and continuing with amphicyonids (and non-carnivoran hyaenodontids). Felids and mustelids are the most diverse carnivorans in the Siwaliks, while caniforms become more prevalent through time. [ABSTRACT FROM AUTHOR]