In a recent report published in National Science Review, a Chinese team of scientists highlights the discovery of well-preserved blue-stain fungal hyphae within a Jurassic fossil wood from northeastern China, which pushes back the earliest known fossil record of this fungal group by approximately 80 million years. The new finding provides crucial fossil evidence for studying the origin and early evolution of blue-stain fungi and offers fresh insights into understanding the ecological relationships between the blue-stain fungi, plants, and insects during the Jurassic period.Blue-stain fungi constitute a distinctive group of wood-colonizing fungi which lack the ability to decompose wood lignocellulose, yet are capable of causing significant wood discoloration. Though these fungi are generally nonfatal to their hosts, they often accelerate tree mortality when associated with wood-boring insects.Molecular phylogenetic analyses suggest that blue-stain fungi should be an old fungal group, which might originate during the Late Paleozoic or early Mesozoic. However, hardly anything is known about the geological occurrences of blue-stain fungi.Not until 2022, the first credible fossil record of blue-stain fungi was reported from the Cretaceous in South Africa with an age of approximately 80 million years.This research team was led by Prof. Ning Tian from Shenyang Normal University (SNU) and Prof. Yongdong Wang from Nanjing Institute of Geology and Palaenology, CAS (NIGPAS), and was jointly studied by Prof. Zikun Jiang from the Chinese Academy of Geological Sciences in Beijing as well as other scholars from SNU. They foundwell-preserved fossil fungal hyphae preserved within a Jurassic petrified wood from northeastern China, dated 160 million years ago. Microscopic examination reveals thefossil hyphae are dark in colour, which is indicative of pigmentation, a hallmark of contemporary blue-stain fungi which results in the discoloration of woods. Of interest, when penetrating the wood cell wall, the hyphae commonly form a very specialized structure called “penetration peg”. That is to say when pushing through the wood's cell walls, the hyphae commonly slim down in size, making it easier to pierce through the tough barrier. The discovery of the penetration peg enables the team to ensure that the fossil fungus that they found belongs to the blue-stain fungi. Unlike wood-decay fungi, which degrade wood cell walls through enzymatic secretion, the blue-stain fungi lack the enzymatic capacity to decompose wood structures. Instead, their hyphae mechanically breach wood cell walls via the penetration pegs.The finding of Jurassic blue-stain fungi from China pushes back the earliest known fossil record of this fungal group by approximately 80 million years, providing crucial fossil evidence for further understanding the origin and early evolution of blue-stain fungi.Additionally, it offers fresh insights into understanding the ecological relationships between the blue-stain fungi, plants, and insects during the Jurassic period. The bark beetle subfamily Scolytinae is considered as one of the major spore dispersal agents for extant blue-stain. However, both molecular biological and fossil evidence proposed that the origin time of Scolytinae dates back no earlier than the Early Cretaceous. Given the Jurassic age of present fossil fungus, it is hypothesized that its spore dispersal vector was not Scolytinae but rather other wood-colonizing insects prevalent during that period.This study was funded by the National Natural Science Foundation of China and the Liaoning Revitalization Talents Program.Article information:Tian Ning*, Wang Yongdong*, Li Fangyu, Jiang Zikun, Tan Xiao, 2025. Blue-stain fungus from the Jurassic provides new insights into early evolution and ecological interactions. National Science Review, 12(6): nwaf160. https://doi.org/10.1093/nsr/nwaf160.Figure 1 Anatomical details of the fungus-bearing wood Xenoxylon phyllocladoides Gothan from the Jurassic of western Liaoning, NE China(a) Transverse section, a insect-boring hole. (b, c) Transverse section, distinct growth rings with collapsed early wood. (d-e) Radial section, uniseriate distant bordered pits. (f, g) Radial section, window-like cross-field pits. Bars: (a) 500 μm; (b) 200 μm; (c) 100 μm; (d-g) 50 μm.Figure 2. Blue-stain fungus in wood tissues of Xenoxylon phyllocladoides Gothan from the Jurassic of western Liaoning Province, NE China.(a–c) Hyphae with septa (white arrow heads). (d) Hyphae growing in the cross-field zone. (e, h) Hyphae penetrating tracheid walls with appressorium-like structures and distinct hyphal pegs (white arrow heads). (f) Colonization of ray parenchyma cells by hyphae. (g, i–j, l) Hyphae horizontally penetrating the tracheid walls with appressorium-like structures. (k) Hyphae colonizing in the tracheid lumen, and passing through the bordered pits. (m–o) Slender hyphae within tracheid lumen with chlamydosporelike structures (white arrow heads).Bars: (a–d, f–n) 50 μm; (e) 25 μm.<!--!doctype-->
Exploring macroevolutionary patterns and processes using fossil records is vital to understanding how developmental drivers and ecological pressures shape biodiversity. Size is one of the most conspicuous organismal traits and serves as a crucial factor in determining how organisms interact with their environment, making patterns of animal body size evolution a focus of macroevolutionary research. Nevertheless, the macroevolutionary patterns of body size across numerous major metazoan clades and their constraining mechanisms remain enigmatic.
Recently, Dr. SUN Zhixin, supervised by Professors ZHAO Fangchen and ZHU Maoyan from the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS), collaborated with Dr. ZENG Han (NIGPAS) and Pro. Douglas H. Erwin from the Santa Fe Institute to conduct a comprehensive study on body size evolution in trilobites, a highly representative group of fossil invertebrates. This research was published in Science Advances on May 2th, 2025.A recent study shows that marine oxygen levels were crucial to the evolution of Early Paleozoic trilobite body size, suggesting that oxygen may have influenced the evolution of other animals’ body size as well.The research, involving a comprehensive analysis of body size evolution in trilobites—a highly representative group of fossil invertebrates—was led by Prof. ZHAO Fangchen and Prof. ZHU Maoyan from the Nanjing Institute of Geology and Palaeontology of the Chinese Academy of Sciences. Results were published in Science Advances.Patterns of animal body size evolution have long been a focus of scientific research, with different theories attempting to explain it. For example, Cope’s Rule holds that animal species tend to evolve to become larger over time. In contrast, Bergmann’s Rule states that in warm-blooded animals, like mammals and birds, species living in colder climates tend to be larger than those living in warmer climates. Both of these theories were developed in the 19th century.Recently, some studies have emphasized the role of oxygen in animal body size evolution, but many of these studies are based on fossil vertebrates. Among invertebrates, research on body size evolution has been limited to a few groups, such as brachiopods and insects.The Early Paleozoic is an ideal period for testing the relative importance of oxygen levels and other environmental mechanisms on body size, due to environmental fluctuations in marine oxygen levels, marine chemistry, and temperature during this epoch.Trilobites have been a central focus of macroevolutionary studies—i.e., those involving large-scale changes in life forms rather than individual species—due to their long geological history, diverse ecological adaptations, and abundant fossil record. With adult body sizes ranging from ~2 mm (Acanthopleurella stipulae) to more than 700 mm (Isotelus rex or Ogyginus forteyi), they are an ideal clade for testing the evolutionary dynamics of body size. Additionally, few comprehensive assessments have been done on the evolution of body size in giant trilobites, despite long-standing interest in them.To explore the macroevolutionary potential of trilobites, the researchers compiled an extensive dataset of body size for Cambrian and Ordovician forms, covering 1,091 genera and representing over 90% of trilobite families during this period. They examined the role of marine oxygen and temperature in determining evolutionary trends in trilobite size. Their results highlight the long-term impact of marine oxygen levels on the evolution of trilobite body size, further confirming the significant role oxygen played in shaping the evolutionary dynamics of early metazoans.The dataset shows that the body size patterns of trilobites during the Cambrian and Ordovician periods can be divided into six phases (I-VI), with body size changes concentrated in five brief events: in early Age 4 (ca. 514 Ma), the late Wuliuan (ca. 506.5 Ma), the Guzhangian (ca. 500.5 Ma), the late Tremadocian (ca. 480 Ma), and the late Katian (ca. 450 Ma).The size differences across the six phases are significant—they are not the result of sample size differences across intervals. Major size changes occurred in each major geographic region, particularly during Age 4, the Guzhangian, and the middle Tremadocian, suggesting that global patterns mirrored regional trends. Collectively, these results imply that changes in trilobite body size were more likely to be influenced by global rather than regional factors.To investigate whether the episodic changes in body size obscure an underlying directional pattern, the researchers identified trends in average body size across the 24 most diverse trilobite families. Most well-sampled trilobite families showed no significant size changes through time, ruling out Cope's Rule at the family level. Moreover, the researchers reconstructed and plotted ancestral body size onto family-level phylogeny, fitting five different models of continuous trait macroevolution.The results indicate that most trilobite families were near the average size, with some clades independently evolving to larger or smaller sizes during different ages. However, none of the results support an overall trend in body size evolution. Overall, these analyses reveal no preferential direction in trilobite body size during the Cambrian and Ordovician periods that would support Cope’s Rule.In contrast, trilobite size was strikingly correlated with fluctuations in marine redox (i.e., marine oxygen levels), especially during the well-known anoxic events of this interval. For example, reductions in trilobite size during the early Cambrian Age 4, the Guzhangian, and the late Katian correspond with the Sinsk, SPICE, and HOAE anoxic events. The miniaturization phases after Sinsk and SPICE (phases II and V) also coincided with sustained marine anoxia. Furthermore, the end of the persistent Black Shale Anoxic Event (BSAE) in the late Tremadocian may have triggered the most pronounced increase in trilobite size.From the late Tremadocian, trilobite size remained stable for nearly 30 Myr (phase V), coinciding with the expansion of marine oxygenation. In contrast, although global cooling may have triggered the extraordinary Great Ordovician Biodiversity Event (GOBE), estimates of early Paleozoic temperature changes show little correlation with trilobite body size. In short, trilobite body size changes during the Cambrian and Ordovician periods correspond closely with marine redox fluctuations.It is reasonable to assume that marine redox influenced, if not directly controlled, trilobite body size changes across the world since larger bodies need more oxygen and smaller bodies need less. All in all, this study strongly supports a model in which oxygen levels constrained body size evolution in trilobites—whose size evolution, along with that of other marine metazoans, has not been understood as well as that of terrestrial clades.Furthermore, the study provides independent support for the hypothesis that oxygen was an important driver of early animal evolution more generally and may have influenced the body size evolution of other clades as well.This research was supported by the National Key Research and Development Program of China and the National Natural Science Foundation of China.Fig.1: Tempo and mode in the body size evolution of Cambrian-Ordovician trilobites. Changes in maximum size (red) and mean size (blue) for each time slice, with lines and shading representing the mean value and 95% confidence intervals. Discrete episodes of body size change are marked by red arrows, and these events demarcate six distinct phases.Fig. 2: Body size evolution of Cambrian-Ordovician trilobites in Laurentia (B), East Gondwana (C), West Gondwana (D), Baltica and Avalonia (E). Three episodes of change in body size during Cambrian Age 4, the Guzhangian and middle Tremadocian are marked 1, 2 and 3.Fig. 3: Phylogenetic based family-level body size evolution in Cambrian-Ordovician trilobites. (A) Ancestral state reconstruction of body size. (B) Evolutionary traitgram of trilobite body size. (C) Model-fitting results expressed as Akaike weights for five different evolutionary models.Fig. 4: Cambrian and Ordovician trilobite body size (A) and their correlation to the inferred oxygen levels (B) and temperature (C). (B) Ocean redox conditions and widespread anoxic intervals, showing strong links between trilobite body size and marine redox changes, blue and purple indicate oxic and anoxic states, respectively. (C) Temperature curves are based on bulk-rock (purple line) and skeletal material (gray line) δ18O datasets.
A research team from the Nanjing Institute of Geology and Palaeontology of the Chinese Academy of Sciences has identified a fossil acanthocephalan, Juracanthocephalus, from the 160-million-year-old Daohugou Biota in Inner Mongolia, China. This finding was published in Nature.A research team from the Nanjing Institute of Geology and Palaeontology of the Chinese Academy of Sciences has identified a fossil acanthocephalan, Juracanthocephalus, from the 160-million-year-old Daohugou Biota in Inner Mongolia, China. This finding was published in Nature.Acanthocephalans, commonly known as thorny-headed or spiny-headed worms, are a group of endoparasitic worms found in both marine and terrestrial ecosystems. These medically significant parasites infect a wide range of hosts, including humans, pigs, dogs, cats, and fish. Acanthocephalans are characterized by their worm-like body shape and a retractable proboscis armed with rows of recurved (i.e., backward-facing) hooks for anchoring to the digestive tracts of their hosts. Historically classified as a distinct animal phylum, their highly specialized body plan has led to ongoing debates regarding their phylogenetic position.Morphological studies have proposed various hypotheses linking acanthocephalans to Platyhelminthes (flatworms), Priapulida (penis worms), or Rotifera (wheel animals). However, molecular phylogenetic analyses strongly suggest that acanthocephalans are a highly specialized subgroup within Rotifera. Despite this, the morphological disparity between endoparasitic acanthocephalans and free-living rotifers remains striking.Furthermore, the fossil record of acanthocephalans is exceptionally sparse due to their soft bodies—which were less likely to fossilize than harder ones—and concealed habitats. Until now, the only known fossil evidence consisted of four putative acanthocephalan eggs discovered in the coprolites of a Late Cretaceous crocodyliform. Due to the lack of body fossils, the origin and early evolution of acanthocephalans thus remain poorly understood.Using scanning electron microscopy (SEM) and energy-dispersive spectroscopy (EDS), the research team conducted a detailed anatomical analysis of Juracanthocephalus and updated the morphological matrix of worm-like animals to support a comprehensive phylogenetic analysis.The results indicate that Juracanthocephalus represents a transitional form between free-living, jawed rotifers and jawless, endoparasitic acanthocephalans, bridging an evolutionary gap. This finding provides the first direct fossil evidence to help resolve the long-standing mystery of acanthocephalan origins.Juracanthocephalus has a fusiform body divided into a proboscis, neck, and trunk. The proboscis is equipped with strongly sclerotized, slightly curved hooks, while the ventral surface of the trunk features 38 lines of transverse, setaceous combs—a trait comparable to modern acanthocephalans. A possible alimentary tract is preserved in the proboscis, though no clear gut is visible in the trunk. The terminal end of the fossil displays a structure resembling the bursa of male acanthocephalans.Notably, Juracanthocephalus has a jaw apparatus composed of clustered, tooth-like units arranged in converging paired rows, with the jaws increasing in size posteriorly. This structure closely resembles that found in Gnathifera, a group that includes Gnathostomulida, Micrognathozoa, and Syndermata (which encompasses Rotifera and Acanthocephala).To determine the phylogenetic position of Juracanthocephalus, the research team compiled an updated morphological matrix incorporating both extant and extinct worm-like animals. The analysis identifies Juracanthocephalus as a stem-group acanthocephalan, sister to all extant acanthocephalans. This finding aligns with molecular phylogenetic analyses, which place acanthocephalans within Rotifera (including Monogononta, Bdelloidea, and Seisonidea).However, the precise placement of acanthocephalans within Rotifera remains contentious, with six competing hypotheses arising from molecular and morphological studies. When Juracanthocephalus is excluded from the morphological matrix, the results support Seisonidea as the sister group to all other Rotifera, consistent with previous morphological analyses but conflicting with molecular data.Conversely, incorporating Juracanthocephalus into the matrix positions Seisonidea as the sister group to Juracanthocephalus and all extant acanthocephalans, reconciling morphological and molecular phylogenetic analyses.The discovery of Juracanthocephalus provides a crucial reference for understanding the evolutionary innovations and body plan of acanthocephalans. Its hooked proboscis and large body size suggest that it was an endoparasite during the Jurassic period. Furthermore, this fossil implies that acanthocephalans may have originated in terrestrial environments and diverged from Rotifera no later than the Middle Jurassic.This study underscores the importance of transitional fossils in elucidating radical morphological changes in animal body plans. While molecular phylogenetics has revolutionized our understanding of evolutionary relationships, Juracanthocephalus highlights the indispensable role of fossil evidence in reconstructing the history of life.The research was supported by the National Natural Science Foundation of China, the IUGS “Deep-time Digital Earth” Big Science Program, and the Jiangsu Innovation Support Plan for International Science and Technology Cooperation Programme.Figure 1: Juracanthocephalus (a, overall view; b, artistic reconstruction) and the comparison with extant Acanthocephala (c). Scale bars, 2.0 mm (a, b), 0.5 mm (c).Figure 2: The backscatter scanning electron (BSE) image (a), overlay image of several elements concentrations (b) and elemental maps of carbon from energy-dispersive X-ray spectroscopy (c) of Juracanthocephalus. Scale bar, 2.0 mm.Figure 3: Simplified cladogram of Gnathifera showing Juracanthocephalus in red color.Figure 4: Phylogenetic tree from 50% majority rule bootstrap consensus tree of parsimony analysis. When Juracanthocephalus is included in the matrix, the results recover Seisonidea as the sister group to Juracanthocephalus + all extant acanthocephalans (a); when Juracanthocephalus is excluded from the morphological matrix, the results support the Seisonidea as the sister group of all other Rotifera (b).
International scientists have uncovered the oldest known phosphatic stromatoporoid sponge, dating back approximately 480 million years to the Early Ordovician, in South China.Stromatoporoid sponges were key reef builders during the Palaeozoic era, playing a crucial role in constructing biological frameworks—similar to the role of modern corals. They were especially important during the middle Paleozoic era (from the late Middle Ordovician to Devonian), a time marked by a major transition from microbial-dominated to skeletal-dominated reef ecosystems. Previously, stromatoporoid reefs were thought to have emerged suddenly in the late Darriwilian period (around 460 million years ago), leading to questions about their origins and early evolutionary history.Recently, an international research team led by scientists from the Nanjing Institute of Geology and Palaeontology of the Chinese Academy of Sciences discovered an exceptionally preserved phosphatic stromatoporoid sponge from the Early Ordovician, dating back about 480 million years, in Yuan’an, Yichang, South China.This newly identified stromatoporoid, Lophiostroma leizunia, not only extends the fossil record of stromatoporoid reefs by about 20 million years but also provides valuable insights into the early biomineralization strategies of ancient animals.South China is renowned for its exceptional fossil preservation and its diverse Early Paleozoic marine ecosystems. Researchers have extensively studied <!-- “Researchers have extensively studied” would be good. Thank you! -->the Ordovician strata in this region, documenting the early diversification of marine life during the Great Ordovician Biodiversification Event (GOBE)—a critical period marked by dramatic increases in marine biodiversity.Lophiostroma leizunia is unique among all known sponges for constructing its skeleton using fluorapatite, a phosphate mineral. This finding establishes the phylum Porifera (sponges) as the first animal group known to utilize all three principal biominerals: silica, calcium carbonate, and calcium phosphate. This distinctive skeletal composition suggests that early sponges had the genetic capacity to employ diverse biomineralization strategies.Fossil evidence indicates that Lophiostroma leizunia formed complex reef structures and played a crucial role in framework construction, binding together other reef components, including calcimicrobes, lithistid sponges, Calathium, and echinoderms. These reef ecosystems exhibit remarkable ecological complexity—comparable to those found in later reef systems.This study was supported by the National Natural Science Foundation of China, the National Research Foundationof Korea, and the Korea Polar Research Institute project.This study enhances our understanding of early reef ecosystems and the evolution of biomineralization across the animal kingdom, providing new insights into how environmental factors influenced biological evolution during this critical period in Earth’s history.Figure 1. Thin section photographs of Lophiostroma leizuniaFigure 2. Mineralogical and micro-scaled features of Lophiostroma leizuniaFigure 3. Stromatoporoid-echinoderm reef type
The Cambrian explosion, which occurred from the late Ediacaran to the early Cambrian, stands as one of the most pivotal evolutionary events in Earth’s history. Across the Ediacaran-Cambrian boundary (ECB), the once-thriving Ediacara-type biota vanished, while metazoans forged a Phanerozoic-type ecosystem within approximately 18 million years (539–521 Ma). Our previous understanding of this critical evolutionary transition relied on relatively continuous records of small shelly fossils from shallow-water carbonates and phosphatic deposits, alongside Ediacara-type macrofossils and trace fossils mainly preserved in siliciclastic rocks. However, the widely developed sedimentary discontinuities near the ECB in shallow-water settings hindered a comprehensive understanding of the biological processes during this turning point.Recently, the research team led by Prof. Maoyan Zhu from the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS), proposed that chert deposits across the ECB offer a new window into this biological revolution. The study, with Dr. Cui Luo as the first author, was published online on March 10, 2025, in Geology.Cherts, being able to exquisitely preserve non-mineralized organisms and their anatomical details, have been exceptional taphonomic windows since the Archean. The Ediacaran-Cambrian cherts of South China have been investigated by Chinese paleontologists since the 1990s, with dozens of microalgal genera recognized. Built on this basis, the team examined cherts from eight ECB sections across South China and delineated two distinct fossil assemblages through integrated paleontological and carbon isotope stratigraphic analyses.The terminal Ediacaran fossil assemblage (550–539 Ma) is dominated by enigmatic string- and strap-like forms of uncertain affinity, with Horodyskia (bead-like strings) and Nenoxites (crescent-segmented strings) being particularly common. These fossils are preserved primarily as clay-mineral casts, differing from the carbonaceous or permineralized preservation typical of other chert Lagerstätten. In contrast, early Cambrian cherts (539–521 Ma) reveal a highly diverse assemblage with finely preserved anatomical details, encompassing acritarchs, algal microfossils, mineralized animal skeletons, and carbonaceous fossils of uncertain affinity. A large acanthomorphic acritarch from the Luxishao section echoes forms from the early Ediacaran, suggesting that some ancient taxa may have persisted into the Cambrian. Sponge spicules in cherts extend below the nadir of the basal Cambrian carbon isotope excursion (BACE), indicating that biomineralization in sponges, like that of small shelly fossils such as Anabarites, originated prior to the Cambrian. Especially noteworthy are the complex carbonaceous filmy fossils unique to the Cambrian assemblage, which are distinct from algal remains and absent in Precambrian cherts. These fossils, potentially representing animal cuticles, indicate an innovation in soft-tissue structures among multicellular eukaryotes at the dawn of the Cambrian.These findings align with prior insights from other taphonomic windows, confirming a rapid biospheric shift near the ECB; a few Ediacaran forms persisted into the Cambrian, while Cambrian-specific skeletal fossils extend below the BACE nadir. This consistency reinforces previous conclusions while highlighting the potential of chert fossil records as a new window for exploring ECB biological changes. The broad distribution of cherts across varying water depths and their capability of preserving delicate non-mineralized tissues could provide good complements to the skeletal fossil data from shallow-water settings. As such, this avenue of research merits heightened attention in future studies.The study also shows that representative members of both assemblages are widespread across the Yangtze craton, from west to east (Yunnan to Anhui) and from proximal shelf to distal upper slope facies. However, vertical overlap between the two assemblages is rare, with only one prior report noting their co-occurrence. Future investigations are required to test whether these assemblage differences stem from taphonomic bias or sedimentary hiatus.This study was supported by the National Key Research and Development Program and the National Natural Science Foundation of China. Numerous team members offered help in the extensive fieldwork. Dr. Soo-Yeun Ahn contributed significantly to the material collection during her postdoctoral project.Fig. 1 Investigated sections and their distribution in the Terreneuvian lithofacies paleogeographical map.Fig. 2 The contrasting characteristics between the terminal Ediacaran (A–F) and the early Cambrian fossil assemblages (G–O).Fig. 3 Some of the carbonaceous filmy fossils in the Cambrian cherts.Fig. 4 (A) Temporal distribution of chert Lagerstätten and other taphonomic windows across the Ediacaran-Cambrian transition, along with representative fossils in each window. (B) Spatial distribution of fossils in cherts across the Ediacaran-Cambrian transition.<!--!doctype-->
Amber, known as nature’s “time capsule,” provides a unique window into Earth’s history and the evolution of life. It not only preserves the morphology of ancient organisms but also records environmental information from prehistoric times, making it a crucial medium for paleontological research. Currently, the oldest known amber containing biological inclusions comes from the Triassic strata of Italy, while all other amber with biological inclusions dates to the Cretaceous or later, such as Cretaceous Burmese amber, Eocene Fushun amber, and Miocene Dominican amber. Jurassic amber has long remained a gap in research.Recently, a research team led by Professor Dany Azar from the Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, discovered a precious Jurassic insect fossil in amber from the Late Jurassic (Kimmeridgian) in Aintourine, northern Lebanon. This discovery not only fills the gap in the Mesozoic amber fossil record but also provides important clues for studying insect evolutionary history. The fossil, named Jankotejacoccus libanogloria, is the earliest known Jurassic amber insect inclusion, revealing that male characteristics of scale insects appeared in the early stages of evolution.Lebanon is renowned in paleontology for its rich amber deposits. Under the leadership of Dany Azar, researchers have identified over 500 amber outcrops from the Early Cretaceous in Lebanon, 31 of which contain biological inclusions, along with 19 outcrops from the Late Jurassic. This period is crucial in the study of terrestrial ecosystem evolution, as it marks the emergence of angiosperms and the co-evolutionary relationship between plants and pollinating insects.The newly discovered Jankotejacoccus libanogloria is a herbivorous adult male scale insect, significantly different from all other scale insects, and has been classified into a new family. The fossil reveals that male characteristics of scale insects, including morphological and behavioral transformations, appeared early in their evolution. The Late Jurassic primitive male scale insect fossils are morphologically related to modern groups and coexisted with the dominant gymnosperms of the time. Associated marine fossils and zircon analysis support its age as Kimmeridgian.The Aintourine amber is proven to originate from the gymnosperm family Cheirolepidiaceae. The semi-angular morphology of the sediment-amber boundary suggests that the low viscosity of the resin may have contributed to the rarity of biological preservation in such amber, although other factors (e.g., resin flow or taphonomic processes) may also have played a role. Associated plant materials in the amber include Protopodocarpoxylon, Brachyphyllum, Classostrobus, and Classopolis pollen from the Cheirolepidiaceae. The paleoenvironment has been reconstructed as a forested temporary swamp habitat, with tall araucarias, ginkgoes, shrub ferns, tree ferns, and aquatic ferns. The amber is typically transparent, containing fungal spores, minerals, and organic debris (charcoal, leaves, wood, and fungi). There is no evidence of long-distance transport or redeposition, suggesting the depositional environment was near the amber-producing trees. However, whether these trees dominated the forest remains uncertain, as they may have coexisted with other species.This discovery not only provides new insights into the origins of amber forest ecosystems but also paves the way for further research on evolution and biodiversity. Future studies on Lebanese amber deposits and findings are expected to enhance our understanding of the early development of modern ecosystems and offer more insights into the biodiversity and terrestrial evolution of the mid-Mesozoic.This research was supported by the Chinese Academy of Sciences Hundred Talents Program (Category A).Article Information:Peter Vršanský*, Hemen Sendi, Júlia Kotulová, Jacek Szwedo, Martina Havelcová, Helena Palková, Lucia Vršanská, Jakub Sakala, L'ubica Puškelová, Marián Golej, Adrian Biroň, Daniel Peyrot, Donald Quicke, Didier Néraudeau, Pavel Uher, Sibelle Maksoud, Dany Azar*, 2025. Jurassic Park approached: a coccid from Kimmeridgian cheirolepidiacean Aintourine Lebanese amber. National Science Review, Volume 12: nwae200, https://doi.org/10.1093/nsr/nwae200Reconstruction of the Jurassic amber ecosystem in Aintourine, northern Lebanon (Image by: Júlia Káčerová).Jurassic amber forest of Aintourine and fossil evidence from the perspective of dinosaurs (Image by: Júlia Káčerová).Male scale insect Jankotejacoccus libanogloria from Jurassic amber in Lebanon.<!--!doctype-->
Since 2019, Dr. Peng Huiping from the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, under the guidance of his supervisor Prof. Feng Liu, has collaborated with Prof. Mingli Wan from the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Prof. Wan Yang from Missouri University of Science and Technology, and Prof. Jun Liu from the Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, to conduct detailed research on palynomorphs from the well-dated South Taodonggou section exposed on the western margin of the Turpan-Hami Basin in Xinjiang, China. This research provides new fossil evidence for understanding the evolution of terrestrial vegetation in the Turpan-Hami Basin during the end-Permian mass extinction, with findings recently published in Science Advances.A new study reveals that a region in China’s Turpan-Hami Basin served as a refugium, or “Life oasis” for terrestrial plants during the end-Permian mass extinction, the most severe biological crisis since the Cambrian period.The research, published in Science Advances, challenges the widely held view that terrestrial ecosystems suffered the same catastrophic losses as marine environments during this period.The discovery, led by Prof. LIU Feng from the Nanjing Institute of Geology and Palaeontology (NIGPAS) of the Chinese Academy of Sciences, provides the first conclusive fossil evidence of a terrestrial plant community that remained largely undisturbed throughout the extinction event, allowing for continuous evolution and rapid ecological recovery afterward.The team’s findings suggest that some land areas were shielded from the worst effects of the extinction, creating pockets of resilience that played a crucial role in the rebound of life on Earth.The end-Permian mass extinction, which occurred approximately 252 million years ago, wiped out over 80% of marine species, and its impact on land has long been debated. One prevailing theory suggests that volcanic eruptions in Siberia triggered widespread terrestrial devastation through wildfires, acid rain, and toxic gases. Evidence for this includes the successive extinction of characteristic Gigantopteris flora in South China and typical Glossopteris flora across Gondwanaland around the end-Permian mass extinction.However, the opposing camp argues that these catastrophic effects were limited by latitude and atmospheric circulation. Some fossil discoveries even suggest that certain Mesozoic plants existed before the extinction event, pointing to uninterrupted evolution.The South Taodonggou section in Xinjiang offers a unique perspective. Detailed analysis of fossil pollen and spores, along with precise dating methods from a Bayesian age model developed by Professor YANG Wan of the Missouri University of Science and Technology, have revealed a continuous record of riparian fern fields and coniferous forests thriving from 160,000 years before the extinction began until 160,000 years after it ended.“The presence of intact tree trunks and fern stems further confirms that these microfossils represent local vegetation, not transported remnants,” said Professor WAN Mingli from NIGPAS.Although some plant species disappeared locally, the researchers found that the overall extinction rate of spore and pollen species in the South Taodonggou section was possibly only about 21%—far lower than the marine extinction rate during the same period. This conclusion was based on the discovery of many “missing” species in Early Triassic strata elsewhere, indicating temporary migration rather than permanent extinction.This stable vegetation base was crucial for the rapid recovery of the local ecosystem. Fossil evidence shows that within just 75,000 years after the extinction ended, the area supported diverse tetrapods, including herbivorous Lystrosaurus and carnivorous chroniosuchians, demonstrating a quick return to a complex food web. This discovery contrasts with the previous understanding that ecosystem recovery after the end-Permian extinction took over a million years. The new evidence suggests local ecological diversity in this area recovered more than ten times faster than in other regions.The researchers cited the region’s stable, semi-humid climate as crucial to its biological resilience. According to analysis of paleosol matrices, the region consistently received about 1000 mm of rainfall per year during this time. Due to its consistent precipitation, South Taodonggou offered more abundant vegetation and a more habitable environment than other regions following the end-Permian mass extinction, providing vital support for migrating animals.Despite its proximity to the volcanic activity that triggered the end-Permian extinction, the Turpan-Hami Basin provided a safe haven for terrestrial life, demonstrating that even seemingly dangerous locations can harbor crucial biodiversity.“This suggests that local climate and geographic factors can create surprising pockets of resilience, offering hope for conservation efforts in the face of global environmental change,” said Professor LIU Feng from NIGPAS.In light of current concerns about a potential sixth mass extinction driven by human activity, the discovery of this “Life oasis” highlights the importance of identifying and protecting such natural refugia.This work was supported by the National Natural Science Foundation of China, the National Key R&D Program of China, the Second Tibetan Plateau Scientific Expedition and Research Program and the US National Science Foundation.<!--!doctype-->
Located at the northeastern margin of the Qinghai-Xizang (Tibetan) Plateau, the Qaidam Basin serves as a key region for studying Mesozoic terrestrial ecosystem evolution and exploration of fossil energy resources.Since the 1950s, abundant paleobotanical and palynological findings have been accumulated from the Lower-Middle Jurassic in this region. However, as a crucial proxy of paleobotanical research, fossil woods have rarely been documented in the Jurassic strata of the Qaidam Basin, and the systematic studies remain insufficient. This knowledge gap has hindered comprehensive analysis of Mesozoic paleovegetation evolution and climatic and environmental changes in the area.Recently, a Sino-German joint research team on paleobotany, led by Professor Wang Yongdong from the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS), Dr. Xie Aowei from Senckenberg Research Institute, Germany (SRI), and Prof. Tian Ning from the College of Paleontology of Shenyang Normal University (CPSNU) discovered a new type of exceptionally well-preserved fossil wood material in the Early Jurassic strata dating back about 186 million years ago on the northeastern margin of the Qaidam Basin. They carried out systematic anatomical studies, confirmed its taxonomic attributes and revealed its significance for paleobiogeography and paleoclimate research.Anatomical studies have shown that fossil exhibits araucarian radial tracheid pits, each cross-field usually bearing 1–2 podocarpoid pits, taxodioid pits or oopores, abundant septa in tracheids, and all ray cell walls thin and unpitted. These morphological features support its classification into the extinct conifer plant genus Metapodocarpoxylon Dupéron-Laudoueneix et Pons.Since 1985, the genus Metapodocarpoxylon has been establishedfor over 40 years. Previously records of this genus are restricted to the northern Gondwana during the Mesozoic, and their localities are documented in over 40 localities forming a distinctive latitudinal belt extending westwards from Lebanon to Peru in the Jurassic and Cretaceous sediments. The current discovery not only represents its first record in Laurasia but also expands its biogeographic range from northern Gondwana to Laurasia, defying conventional biogeographic boundaries. This report has broken through the traditional understanding of geographical distribution of Metapodocarpoxylon, and contributes to a deeper understanding of the migration and evolution patterns of this plants in the geological history.Fossil records shows that Metapodocarpoxylon mainly appeared from the Middle Jurassic to the Cretaceous period. This study reveals that the genus might have originated in Laurasia during the Early Jurassic and then migrated to the Gondwana region under the influence of climate change. The new fossil materials discovered in the Qaidam Basin have pushed the fossil record of this genus back from the previously known Middle Jurassic to the Early Jurassic (about 20 million years earlier).The fossil wood of Metapodocarpoxylon displays distinct growth rings, with abundant, well-formed earlywood and narrow latewood, as well as abrupt transitions between earlywood and latewood. This observation, along with previous interpretations based on macroflora, palynoflora and sedimentological data, suggests that a warm and humid climate condition with mild seasonality prevailed in the region during the Early Jurassic.Integrated analysis of palaeobotanical and sedimentological data further indicates that the Qaidam Basin experienced a warm-humid climate with mild seasonal precipitation disparities, providing optimal conditions for dense coniferous forests. This conclusion aligns with palaeobotanical and palynological evidence supporting a "conifer-dominated temperate humid climate," thereby furnishing critical evidence for reconstructing palaeovegetation and refining Early Jurassic climatic models in East Asia.This research has been published in the Cambridge University international journal Geological Magazine. Prof. Yongdong Wang from NIGPAS, Dr. Aowei Xie from SRI and Prof. Ning Tian CPSNU served as co-corresponding authors. The international collaborative team included Prof. Dr. Dieter Uhl (Senckenberg Research Institute), Dr. Min Xu, Dr. Yanbin Zhu, Dr. Li Zhang, Dr. Xiao Teng, and doctoral student Hongyu Chen from NIGPAS. This research received joint support from the National Natural Science Foundation of China, the Strategic Priority Research Programs (Category B) of Chinese Academy of Sciences, and the State Key Laboratory of Palaeobiology and Stratigraphy.Reference: Xie, A.*, Chen, H., Wang, Y.*, Tian, N.*, Xu, M., Zhu, Y., Zhang, L., Teng, X., Uhl, D. 2024. An exceptionally preserved conifer wood Metapodocarpoxylon from the Jurassic of northeastern Qinghai-Xizang (Tibetan) Plateau, and its palaeobiogeographic and palaeoclimatic significances. Geological Magazine, 162(e7): 1–10. https://doi.org/10.1017/S0016756824000451Fig. 1 Anatomical characters of Metapodocarpoxylon wood from the Lower Jurassic in the Qaidam Basin. (a–c), cross sections; (d–h), radial sections.Fig. 2 Anatomical characters of Metapodocarpoxylon wood from the Lower Jurassic in the Qaidam Basin. (a–d), radial sections; (e–i), tangential sections.Fig. 3 Palaeobiogeographic map showing the spatio-temporal distribution of Metapodocarpoxylon worldwide<!--!doctype-->
Marine strata of Cretaceous age are widely distributed and well exposed in the Gamba area of South Tibet. A pre-requisite for understanding the depositional and palaeoenvironmental processes, which formed these deposits, is a reliable stratigraphic framework. The strata of the Qiangdong section in the Gamba area yielded calcareous nannofossils which provide a powerful tool for establishing a detailed biostratigraphic subdivision. They also allow for a supra-regional correlation, ideally on a global scale.Recently, an international research team consisting of PhD student HAN Meiling, Prof. LI Gang from the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS), alongside Prof. Jörg Mutterlose from Ruhr University Bochum, Germany, and Prof. Ulrich Heimhofer from Leibniz University Hannover, Germany, conducted a systematic study on the mid-Cretaceous calcareous nannofossil biostratigraphy of the Qiangdong section in the Gamba area, southern Tibet. This study has been published in the international journal “Cretaceous Research”.A total of 76 species have been identified in the 159 m thick section, allowing for the recognition of seven bioevents (calcareous nannofossil zones UC0 to UC7) covering the upper Albian–lower Turonian interval. The first occurrences of the calcareous nannofossil marker species Corollithion kennedyi (base UC1a, 100.5 Ma) and Quadrum intermedium (base UC5c, 94.1 Ma) constrain the Albian/Cenomanian and Cenomanian/Turonian boundaries in the Qiangdong section.The dominance of Watznaueria barnesiae throughout the studied interval suggests that diversity and abundance of the assemblages were clearly driven by diagenesis. Interval 1 (0–11 m) is barren of calcareous nannofossils. Within Interval 2 (12–43 m), the coexistence of Biscutum constans, Zeugrhabdotus spp. and Nannoconus spp. indicates a deep nutricline. Interval 3 (44–122 m) shows a decrease of B. constans, Discorhabdus ignotus and Nannoconus spp. along with an increase in W. barnesiae, suggesting enhanced diagenesis. Interval 4 (123–159 m), dominated by W. barnesiae, indicates a diagenetically highly altered environment with limited species diversity. A significant negative correlation between species diversity and the relative abundance of W. barnesiae further supports the idea that strong diagenetic alteration affected the nannofossil assemblages.A regional comparison with findings from the Tingri area, about 150 km west of the studied section, enhances the precision of biostratigraphic correlations in South Tibet. In addition, moderate to poor nannofossil preservation suggests a diagenetic influence for both the Tingri and Gamba areas, highlighting the necessity of critically evaluating nannofossil preservation when interpreting nannofossil assemblages for reliable palaeoceanographic reconstructions. The temperature and nutrient indices obtained in this study deviate from those published in past studies. These findings emphasize that preservation and diagenetic influence need to be critically considered when interpreting nannofossil assemblages for palaeoenvironmental reconstructions.This research was supported by the National Natural Science Foundation of China.Reference: Han, M., Li, G.*, Heimhofer, U., Mutterlose, J., 2025. Late Albian–early Turonian calcareous nannofossils from southern Tibet—implications for preservation, biostratigraphy and palaeoecology. Cretaceous Research, 171:106101. https://doi.org/10.1016/j.cretres.2025.106101Figure 1.Structural diagram of the study area and the location of the sectionFigure 2. Lithology, CaCO3 content, relative abundances of selected nannofossil taxa, temperature (MTI) and nutrients (MNI) in the Qiangdong section. ACB = Albian/Cenomanian boundary, CTB = Cenomanian/Turonian boundary.
The western Thailand and the Baoshan area of western Yunnan, China, were both part of the Sibumasu Terrane during the Early Paleozoic, located at low-latitudes of the peri-Gondwana. In November 2019, the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS), and Mahasarakham University in Thailand signed a Memorandum of Understanding, initiating an in-depth collaboration in the field of geology and paleontology. Supported by this memorandum, the Early Paleozoic research team from NIGPAS conducted field investigations in Thailand in January 2020 and March 2023. Together with colleagues from Thailand, the team collected abundant conodont samples from the Ordovician and Silurian strata.Recently, Associate Professor Dr. CHEN Zhongyang, Dr. FANG Xiang, Assistant Professor Dr. LI Wenjie and other colleagues from the Early Paleozoic research team at NIGPAS, together with Professor Clive Burrett, Associate Professor Mongkol Udchachon, and Hathaithip Thassanapak from Mahasarakham University, Thailand, conducted analyses and systematic studies on these conodont samples. The significant findings, enriching the fossil records of Early Paleozoic conodonts in western Thailand and providing new insights into the paleobiological communities and paleogeographic environments. The research result was published in Journal of Palaeogeography and Palaeoworld.(1) New insights into Ordovician conodonts from the Ban Tha Kradan area in western ThailandNine genera and 11 species of conodonts were reported in the Ban Tha Kradan area of western Thailand for the first time. By the analysis of lithology and stratigraphic ages, the upper part of the Tha Manao Formation in the western Thailand was revised as the Pa Kae Formation. Based on conodonts and macrofossils, the Tha Manao Formation in western Thailand is assigned to the upper Floian to Darriwilian, and the conformably overlying Pa Kae Formation to the Sandbian to lower Katian.(2) First report of early Silurian conodont fauna in western ThailandFor the first time, the early Silurian conodonts were documented in western Thailand. Samples from the Kroeng Kravia Forest Park area revealed the upper Telychian Lower Pterospathodus amorphognathoides amorphognathoides Subzone. Analysis of microfacies and conodont fauna indicate that these fossils originated from a relatively deep marine environment. Furthermore, the conodont fauna is similar to that from Baoshan area of Yunnan Province and Langao area of Shaanxi Province in West China and resembles that from similar depositional environments in Australia, Laurentia, and peri-Gondwana, suggesting good connections among these regions by ocean currents.This series of studies was supported by the National Key Research and Development Program of China, the Second Tibetan Plateau Scientific Expedition and Research Program, the Strategic Priority Research Program of the Chinese Academy of Sciences, the National Natural Science Foundation of China, the Chinese Academy of Geological Sciences, and the Mahasarakham University.Reference:Chen, Z.Y., Li, W.J., Fang, X., Li, C., Burrett, C., Udchachon, M., Zhang, Y.D., 2024. Ordovician conodonts from the Ban Tha Kradan area, western Thailand. Palaeoworld, 33(3), 546-558. https://doi.org/10.1016/j.palwor.2022.12.004Chen, Z.Y., Thassanapak, H., Li, W.J., Wu, X.J., Udchachon, M., Fang, X., Burrett, C., 2025. First documentation of early Silurian conodonts from western Thailand and its geological implications. Journal of Palaeogeography, 14(1): 157-171. https://doi.org/10.1016/j.jop.2024.08.010Fig. 1. Ordovician conodonts from the Tha Manao Formation, Ban Tha Kradan area, western ThailandFig. 2. Silurian conodonts from the Kroeng Kravia Forest Park area, western ThailandFig. 3. Correlation of the stratigraphical successions of the Floian to Katian between the Sibumasu Terrane and the Upper Yangtze Platform of South ChinaFig. 4. Distribution of the upper Telychian conodont faunas containing Pterospathodus pennatus procerus, Panderodus langkawiensis, and Dapsilodus spp.
