Volume 62,Issue 4,2023 Table of Contents

  • Display Type:
  • Text List
  • Abstract List
  • 1  Keep the history spirit, foster further academic innovation, and create greater glory—commemorating the 70th anniversary of Acta Palaeontologica Sinica
    2023, 62(4):451-453. DOI: 10.19800/j.cnki.aps.2023102 CSTR:
    [Abstract](90) [HTML](0) [PDF 453.74 K](358)
    Abstract:
    Acta Palaeontologica Sinica (APS) has a history of 70 years since its inception in 1953. Over the past 70 years, several generations of palaeontologists on the editorial board of APS have made important contributions to promoting academic publications and exchange of ideas in paleontology. Since the beginning of the new century, APS has been continuing in its history spirit and foster to its academic integrity and innovation, and has implemented a series of innovative development measures. At the same time, the journal adheres to its Chinese characteristics and international perspectives, promoting the improvement of its academic connotation, and thriving toward the target of a high-quality journal. In particular, APS has been recently included in the internationally renowned Elsevier database Scopus. In the future, APS will continue its courage and persistence to innovate and make continuous efforts to elevate the journal to a higher level, and make new contributions to promoting palaeontological publications, the development of palaeontology, and academic exchanges in China.
    2  Opportunities and challenges for the development of geobiology
    XIE Shu-cheng LUO Gen-ming
    2023, 62(4):454-462. DOI: 10.19800/j.cnki.aps.2023025 CSTR:
    [Abstract](227) [HTML](0) [PDF 1.00 M](427)
    Abstract:
    At the present time, geobiology has attracted a great attention and faces both opportunities and challenges for its disciplinary development. The innovation of technology and methodology in modern days has led to the progressive shift in the study objects from macrofossils to microfossils and finally to geomicrobes and geoviruses. Meanwhile, the themes of geobiology have shifted from environmental impacts on biotic evolution to biotic impacts on paleoclimatic and paleoenvironmental changes and even on the deep processes, which enable us to decipher the fundamental issues related to the Earth’s habitability. The broadening of both the study objects and the disciplinary themes has greatly enhanced the support for societal services from the perspective of geobiology, including the supply of resources and energy, and the coordinated resilience to the crises in climate, environments, and biodiversity in modern days. However, the deep-going disciplinary development of geobiology awaits the innovation of more techniques and methods. It is further needed for geobiology to decipher not only the underlying dynamics of biotic evolution but also the biotic impacts on the deep processes including the plate movements and volcanisms, which in turn helps to evaluate whether the biosphere changed the directions or routines of the evolution of the habitable Earth, and to provide implication for coping with the crises of climate, environments, and biodiversity loss in modern days.
    3  New perspectives on Cambrian Explosion: construction of the first animal consumer-driven marine ecosystem on Earth
    ZHANG Zhi-fei LIANG Yue LIU Fan HU Ya-zhou YAO Jin-long SONG Bao-peng LUO Mei ZHANG Cai-bin WANG Jia-yue CHEN Yan-long GUO Jun-feng HUA Hong LI Guo-xiang
    2023, 62(4):463-515. DOI: 10.19800/j.cnki.aps.2023051 CSTR:
    [Abstract](855) [HTML](0) [PDF 70.33 M](750)
    Abstract:
    The Cambrian Explosion represents one of the most profound phases in the history of life, with nearsimultaneous emergence of most modern animal phyla, including all Bilateria. Since this time, the proliferation of animals across all ecospaces, including terrestrial environments, suggests that the Earth has become increasingly habitable for animal life. Along with the sudden appearance of essentially all the readily fossilized major animal groups, the Cambrian Explosion (540–510 Ma) also resulted in the first appearance of macro-consumers and complex trophic interactions, and established patterns of emergence and diversification that define the modern animal tree of life. Following the Cambrian, despite numerous major geological events and the migration of both plants and animals into the terrestrial realm, there is no apperance of new animal phyla. The Cambrian Explosion can therefore be considered a unique event in the history of life, representing both a key transition in global habitability and the starting point for animal consumer-driven marine ecosystems.
    Previous work by multiple research teams, from both China and abroad, has explored the Cambrian Explosion from many different perspectives, and has markedly increased our understanding of this major evolutionary event. Based on this work, combined with research progress on Precambrian biotas, this paper proposes three macroevolutionary phases in the evolution of early life. Each phase is defined by both organismal “hierarchical level” and geological settings, with the Cambrian Explosion representing the culmination of the three phases. These three phases are: molecular-level evolution during the origin of early continents, cellular-level evolution along with the supercontinent evolution of Nuna (Columbia) and Rodinia, and tissue-level evolution coupled with the early assembly and breakup of Pangea. At the earliest stages of Earth’s history, macro-level prokaryotes, derived from protocell-forming molecules, first formed (Molecular Phase). The first appearance of eukaryotic cells, derived from prokaryotes, represents the next milestone in biological evolution (Cellular Phase). The subsequent emergence of multicellular eukaryotes (metazoans) represents the third and final phase (Tissues Phase). Combined with the advent of multicellularity comes a revolution in body-plan organization, facilitated by the innovative capacity to develop specialized tissues. This includes the spontaneous development of mineralized epithelial exoskeletons and connective tissue endoskeletons.
    Based on these developments, a ‘Lego Blocks’ hypothesis for the Cambrian Explosion is proposed, driven by the initiation of the modern plate tectonic regime characterized by full-plate deep subductions and the associated changes in Earth’s multi-sphere interactions, and bio-litho-atmospheric cycles during Rodinia breakup and Gondwana assembly. During this period of geological disruptions, the diversity of marine niches expanded, resulting in both accelerated phylogenetic diversity and ecological expansion, as organisms developed both a wide range of specialized biological tissues and tissue arrangements to exploit the newly available vacant niche space. The failure of new animal phyla to emerge following the Cambrian Explosion can thus possibly be explained by both a maximization of potential organismal complexity and the relative stabilization of ecospaces. Following the breakup of the Neoproterozoic supercontinent Rodinia, major palaeogeographic changes during the Phanerozoic are limited to the opening and closing of the NeoPaleo-Tethys Ocean, neither of which created novel ecological niches not previously in existence.
    4  A brief discussion on paleontology research in the context of Big Data
    HUANG Bing
    2023, 62(4):516-530. DOI: 10.19800/j.cnki.aps.2023035 CSTR:
    [Abstract](124) [HTML](0) [PDF 598.60 K](603)
    Abstract:

    Over the past half-century, data-based research in paleontology has increasingly assumed a prominent role. It is widely acknowledged that contemporary scientific research has entered the era of Big Data. However, owing to the inherent characteristics of non-laboratory disciplines, the rate of production of paleontological data resources is limited, making it challenging to align with the fundamental characteristics associated with Big Data temporarily. Nevertheless, the era of Big Data and its associated concepts have clearly exerted a positive influence on paleontology. For instance, recent years have witnessed the diversification of data output in paleontology, along with the inherent complexity of mathematical methods and models, which are closely linked to this era. This article, primarily based on the author’s research background, offers a concise overview of the three key stages in the history of quantitative paleontological research. Simultaneously considering the commonalities among paleontological data, it categorizes paleontological data within the context of Big Data as structural, semi-structured, or non-structured, while also providing an introduction to fundamental research methodologies. Following a discussion of the similarities and differences between the two major research perspectives of quantitative paleontology and analytical paleobiology, the article emphasizes the advantages of analytical paleobiology’s research methodologies and statistical models over traditional statistical approaches. In recent years, paleontology has unmistakably displayed characteristics indicative of data-driven research. However, a model-driven research perspective may be necessary. The methodology combines top-down model design with bottom-up data collection and analysis could ensure the sustainability of paleontological data research. Furthermore, given that paleontology is not inherently a data-intensive discipline, its collaboration with data from other geoscientific fields, will in turn promote the interdisciplinary growth of paleontology. Finally, the latest developments in the field of statistics also warrant the attention of paleontologists. The selection of appropriate statistical models and the nuanced interpretation of data should account for the inherent complexity and potential multiple solutions within paleontological studies. Particular caution should be exercised when identifying causal relationships related to statistical significance.

    5  Patterns of vertebrate evolution influenced by the climatic and environmental effects of the Tibetan Plateau uplift
    DENG Tao HOU Su-kuan WU Fei-xiang WANG Shi-qi LI Zhi-heng
    2023, 62(4):531-545. DOI: 10.19800/j.cnki.aps.2023036 CSTR:
    [Abstract](151) [HTML](0) [PDF 1.56 M](475)
    Abstract:
    During the gradual formation of the Tibetan Plateau, the shaping of modern biodiversity in this region was greatly influenced by its uplift. At the same time, the origination of many endemic species and even the intercontinental spread of ancestors of modern widespread groups were also driven by this uplift. During the Mesozoic era, the area where the Tibetan Plateau is located today was covered with vast oceans. The Triassic marine sediments in the Himalayas yield vertebrate fossils such as ichthyosaurs and helicoprionid sharks. By the Jurassic and the Cretaceous, some areas in southeastern Xizang gradually transitioned from marine environment to freshwater lakes in the Qamdo Basin, similar to the coeval Sichuan Basin. Reptiles such as dinosaurs lived near the lakes. The collision between the Indian Plate and the Eurasian Plate in the early Cenozoic era gradually uplifted the Tibetan Plateau. At that time, there was a water system connecting the interior of the Tibetan region with the tropical regions of Southeast Asia, resulting in the flourishing of tropical and subtropical fish. With the significant increase in terrain elevation in this area, the environment became dry and cool, resulting in the extinction of fish acclimated to warm weather and their transformation into the unique snow carps of the Tibetan Plateau. The rapid rise of the Tibetan Plateau resulted in the strengthening of the monsoon climate, and the continuous aridification of the inland regions of Central Asia. The Miocene fauna in western China is mainly composed of drought tolerant grassland mammals, as well as coexisting drought tolerant birds and reptiles. The Tibetan Plateau finally reached its modern height during the Pliocene when its climate and environment had the characteristics of a cryosphere, and it became the initial evolutionary center of the Ice Age fauna. The global temperature dropped below today’s level for the first time at 2.6 Ma, and animals that have adapted to the freezing environment quickly spread to the surrounding areas of the Tibetan Plateau and more distant areas, becoming the foundation of modern animal diversity. The Tibetan Plateau has undergone complex and large-scale environmental changes during its geological history. A series of tectonic movements and geomorphological evolution have triggered and formed the climate pattern of the Tibetan Plateau and its surrounding areas and may have promoted the increased biodiversity in the region.
    6  Progress on the study of mummified fossil woods from the Cenozoic of South China
    HUANG Lu-liang Alexei Asafievich OSKOLSKI QUAN Cheng JIN Jian-hua
    2023, 62(4):546-566. DOI: 10.19800/j.cnki.aps.2023046 CSTR:
    [Abstract](134) [HTML](0) [PDF 22.44 M](395)
    Abstract:
    Although fossil woods are abundant in China, they are not as well-studied as fossil leaves. In addition, reports on these fossil woods are mainly focused on specimens from the north and southwest of China and are limited to their taxonomy. Studies on other aspects related to these fossil woods, such as their paleoclimatic and paleoecological implications are relatively rare. In most cases, these fossil woods are petrified or mineralized. Mummified fossil woods are very scarce. These mummified specimens have a unique and important value for the study of their taxonomy, phylogeny, and paleoclimate. Recently, a large number of mummified fossil woods were discovered and collected from the Cenozoic of South China, including the late Oligocene Yongning Formation of the Nanning Basin, and the Miocene Erzitang Formation of the Guiping Basin, Guangxi, and the Late Pleistocene sediments of the Maoming Basin, Guangdong. This paper summarizes the progress on the study of these mummified fossil woods, including the composition, paleovegetation, paleoclimate and paleoecology of the floras, as well as the phytogeographical history of Magnolia L., Syzygium Gaertn., and Liquidambar L. Based on the floristic composition of the flora, the growth rings and other anatomical characteristics of the woods, it was suggested that there is an evergreen (with a few deciduous) broad-leaved forest in a warm and humid subtropical seasonal climate during the late Oligocene in Nanning Basin of Guangxi; an evergreen-deciduous, broad-coniferous mixed forest in a warm and humid subtropical climate during the Miocene in the Guiping Basin, and an Guangxi; evergreen-deciduous and broad-coniferous mixed forest in a warm and humid subtropical to tropical monsoon climate in the Late Pleistocene of Maoming Basin, Guangdong. This report represents the first comprehensive study on the mummified fossil woods from low-latitude areas of China. The results, provide an important basis for the study of the evolution of the Cenozoic floras and their paleoenvironments.
    7  Overview of the Cretaceous macrofloras of Romania
    Mihai Emilian POPA
    2023, 62(4):567-574. DOI: 10.19800/j.cnki.aps.2023101 CSTR:
    [Abstract](55) [HTML](0) [PDF 2.81 M](389)
    Abstract:
    The Cretaceous macrofloras of Romania are mainly preserved as compressions in several basins of the South Carpathians (Ha?eg, Rusca Montan?, and Ruc?r basins), Transylvania (Transylvanian Basin) and Dobrogea (Babadag Basin), with insignificant occurrences in the East Carpathians. Preservation of the Romania Cretaceous flora is generally poor, as the plant compressions usually lack cuticles or in situ spores and pollen. The ages of these floras range from the Cenomanian up to the Maastrichtian, and their biodiversity encompasses pteridophytes (horsetails and ferns), gymnosperms (conifers) and angiosperms (monocotyledonates and dicotyledonates). From the palaeophytogeographic point of view, the Romanian Cretaceous floras belong to the European Province of the Eurasian Region, occurring along the northern frame of the Tethys realm. The only coal flora was discovered in the Rusca Montan? Basin, while the rest of the Romanian Cretaceous floras are allochthonous floras preserved in clastic sediments.
    8  The Matoniaceae ferns from the Mesozoic of China: fossil record, diversity variation and tempo-spatial distribution pattern
    HUANG Zhuan-li WANG Yong-dong XU Yuan-yuan LU Ning ZHANG Xiao-qing
    2023, 62(4):575-597. DOI: 10.19800/j.cnki.aps.2023010 CSTR:
    [Abstract](121) [HTML](0) [PDF 23.21 M](398)
    Abstract:
    Matoniaceae Presl 1847 is a family of leptosporangiate ferns represented by two extant genera, Matonia R. Brown 1829 and Phanerosorus Copeland 1909, both of which are restricted to the tropical-subtropical areas, such as the Malay Archipelago and Indonesia. Nine fossil genera of Matoniaceae have been reported from the Mesozoic strata of Eurasia, Americas, and Antarctica. Similar to their modern representatives, the presence of these fossil matoniaceous plants suggests tropical-subtropical climate conditions. Available reports indicate that there are 16 documented species in two genera of the Mesozoic of China, including 15 species of Phlebopteris and one species of Matonidium. Paleogeographically, six species of Phlebopteris are distributed in the Southern Floristic Province during the Late Triassic. During the Early Jurassic, Phlebopteris reached its highest level of diversity with 10 species widely distributed in both the Southern and Northern Floristic Provinces; Of the 10 species, eight are newly emerged. During the Middle Jurassic and the Early Cretaceous, the diversity of the genus Phlebopteris is significantly decreased, with only three species reported from Xinjiang, Gansu and Hubei Provinces. Whereas the records of Matonidium are limited, with only one species reported from the Early Cretaceous of Heilongjiang Province. The change of diversity level and tempo-spatial distribution pattern of these matoniaceous ferns from China are suggested to be linked to paleoclimatic variations during the Mesozoic.
    9  A new genus and species of Procercopidae (Insecta: Hemiptera) from the Lower Jurassic Sangonghe Formation of NW China
    ZHANG Qian-qi CHEN Jun WANG Bo ZHANG Hai-chun
    2023, 62(4):598-604. DOI: 10.19800/j.cnki.aps.2023032 CSTR:
    [Abstract](135) [HTML](0) [PDF 1.38 M](395)
    Abstract:
    A new extinct procercopid (Hemiptera) genus and species, Magnicercopis pingi Zhang, Chen et Zhang, gen. et sp. nov., is established based on a tegmen specimen collected from the Lower Jurassic Sangonghe Formation near Urumqi, northern Xinjiang, NW China. The new genus is unique in having three MP terminals, the presence of crossvein im, and forking level of MP basal to that of CuA. A detailed comparison of venation is made between this new taxon and other Jurassic procercopids from China, especially its closest relative, Longucercopis xinjiangensis Zhang, Chen et Zhang, 2022. This finding not only increases the diversity of the Procercopidae but also provides some tegmen information for this family.

    Current Issue


    Volume , No.

    Table of Contents

    Archive

    Volume

    Issue

    Most Read

    Most Cited

    Most Downloaded



    WeChat

    Mobile website