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学者姓名：张欣松
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新疆西准噶尔北部谢米斯台山—沙尔布尔提山地区是中亚造山带的重要组成部分.志留纪普里道利世—早泥盆世期间,该地区沉积了一套由海相复理石到陆棚碳酸盐岩转变的盆地充填序列,其沉积体系的时空展布、岩相变化以及物源分析可为重建西准噶尔北部古地理格局以及古亚洲洋演化提供证据.本文对沙尔布尔提山地区的芒克鲁Ⅱ剖面进行了详细的岩相分析、砂岩碎屑统计、主、微量元素分析,来探讨沉积盆地的演化过程、构造背景和物源属性.芒克鲁Ⅱ剖面出露乌吐布拉克组与曼格尔组,剖面由底到顶依次出现盆地—斜坡背景层沉积、盆地浊积岩、陆棚边缘的异重流扇、陆棚、浅水颗粒滩的相序列,表现为向上变浅的盆地充填序列.沉积物以砂岩、砾岩和生物碎屑颗粒灰岩为主.砂岩成分以长石、岩屑为主,成分变异指数ICV=1.37,值大于 1,指示了碎屑岩成熟度低.砂岩样品富集大离子亲石元素(LILEs),亏损高场强元素(HFSEs),轻稀土与重稀土元素比值(LREEs/HREEs)在 2.89～7.41,均值 6.15.物源判别及构造判别图解综合显示其物源主要来自长英质火山岩及安山岩的混合源区,物源区以大陆岛弧与大洋岛弧环境为主.研究表明,谢米斯台山-沙尔布尔提山岛弧火山岩可能为盆地充填过程提供了丰富的物源,盆地浊积岩向陆棚异重岩沉积的转变不仅代表了盆地充填的暂时性终止,也有可能代表了沙尔布尔提山地区在这一时期的俯冲碰撞活动基本结束.
Keyword ：
复理石 复理石 岛弧 岛弧 岩相 岩相 志留纪普里道利世—早泥盆世 志留纪普里道利世—早泥盆世 物源 物源 西准噶尔 西准噶尔
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| GB/T 7714 | 杜伟东 , 张欣松 , 尹家一 et al. 西准噶尔沙尔布尔提山地区志留纪普里道利世—早泥盆世盆地充填序列及其沉积大地构造意义 [J]. | 沉积与特提斯地质 , 2025 , 45 (1) : 48-68 . |
| MLA | 杜伟东 et al. "西准噶尔沙尔布尔提山地区志留纪普里道利世—早泥盆世盆地充填序列及其沉积大地构造意义" . | 沉积与特提斯地质 45 . 1 (2025) : 48-68 . |
| APA | 杜伟东 , 张欣松 , 尹家一 , 纵瑞文 . 西准噶尔沙尔布尔提山地区志留纪普里道利世—早泥盆世盆地充填序列及其沉积大地构造意义 . | 沉积与特提斯地质 , 2025 , 45 (1) , 48-68 . |
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The Upper Devonian Hongguleleng Formation is a significant stratigraphic unit near the Frasnian/Famennian and Devonian/Carboniferous boundaries of the Kazakhstan Paleoplate. However, its age is still under debate. A new palynostratigraphic analysis was conducted at the Gennaren section to provide a more accurate biostratigraphic assignment. In this study, we identified 43 species belonging to 26 spore genera, including those in open nomenclature. Despite the poor preservation of the palynofloras, the spore taxa were categorized into two assemblages. Assemblage I is established at the lower part of the lower member of the Hongguleleng Formation, containing Cornispora varicornata, cf. Auroraspora pseudocrista, and Cyrtospora cristifera. Assemblage II is from the upper part of the lower member of the Hongguleleng Formation, including Grandispora cornuta, Grandispora famennensis var. famennensis, Grandispora cf. famennensis var. minutus, Grandispora microseta, and Rugospora radiata. These assemblages are compared with the Western European DV Oppel Zone (lower-middle Famennian), and the GF to VCo Oppel zones. The assemblages are equivalent to the conodont crepida–rhomboidea and marginifera to Lower trachytera zones (middle-upper Famennian). © 2024
Keyword ：
Devonian/Carboniferous boundary Devonian/Carboniferous boundary Famennian Famennian Hongguleleng Formation Hongguleleng Formation Palynostratigraphy Palynostratigraphy Western Junggar Western Junggar
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| GB/T 7714 | Shen, Z. , Steemans, P. , Pereira, Z. et al. Palynological assemblages from Hongguleleng Formation of Western Junggar, Northwest China and their correlation with conodont zonation [J]. | Palaeoworld , 2024 , 33 (6) : 1580-1593 . |
| MLA | Shen, Z. et al. "Palynological assemblages from Hongguleleng Formation of Western Junggar, Northwest China and their correlation with conodont zonation" . | Palaeoworld 33 . 6 (2024) : 1580-1593 . |
| APA | Shen, Z. , Steemans, P. , Pereira, Z. , Zong, R.-W. , Zhang, X.-S. , Ma, K.-Y. et al. Palynological assemblages from Hongguleleng Formation of Western Junggar, Northwest China and their correlation with conodont zonation . | Palaeoworld , 2024 , 33 (6) , 1580-1593 . |
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Sediments from land are primarily transported into basins through hyperpycnal flow, which plays a significant role in the process of basin filling. Various models of hyperpycnites have been proposed. This study examines a Silurian-Devonian basin-fill sequence in NW China to validate existing models and presents a visually compelling case demonstrating the process of basin filling through flood-dominated river discharge. The Utubulak Member of the Kekexiongkuduke Formation can be subdivided into three parts, representing basin floor, slope and shelf environments, collectively representing a regressive basin fill sequence. The lower part consists of flood-related turbidites contain or encompass material of terrestrial and marine origin, their sustained and pulsed velocity structures are similar to river discharge. These turbidites may result from basinal hyperpycnal flow or retrogressive failures of the shelf-edge (hyperpycnal) delta. The middle (slope deposits) contains bi-graded hyperpycnite bed interpreted commonly attributed to deposition by river floods exhibiting the classical waxing-waning configuration. Additionally, fine-grained deposits resulting from river-generated, dilute hyperpycnal or hypopycnal plumes are observed interbedded with the basin turbidites or slope background deposits. In the upper part, the presence of thick-bedded sandstones indicates that sustained hyperpycnal flow can transport sands to the shelf-edge/shelf, facilitating deep-water sand delivery. The vertical distribution of the various flood-related facies in basin floor, slope and shelf strata emphasize the complexity of hyperpycnites in different settings, and particularly highlighting challenges associated with their recognition in basin deposits. The investigated succession accumulated in an island-arc setting which provided a favorable condition for a river-fed turbidite system to develop. The narrow shelf facilitated transport of sediments by hyperpycnal flows directly into the basin, while erosion of high mountains promoted a high sediment supply for hyperpycnal flow. And a river-fed turbidite system commonly developed during the late stages of basin filling.
Keyword ：
Basin-fill Basin-fill Flood-related turbidite Flood-related turbidite Hyperpycnite Hyperpycnite Island-arc Island-arc Silurian-Devonian Silurian-Devonian Sustained turbidity current Sustained turbidity current Western Junggar Western Junggar
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| GB/T 7714 | Zhang, Xinsong , Du, Weidong , Zong, Ruiwen et al. River-fed basin-fill and hyperpycnites in an island-arc setting: The Silurian-Devonian - Devonian Kekexiongkuduke Formation from Western Junggar, China [J]. | MARINE AND PETROLEUM GEOLOGY , 2024 , 168 . |
| MLA | Zhang, Xinsong et al. "River-fed basin-fill and hyperpycnites in an island-arc setting: The Silurian-Devonian - Devonian Kekexiongkuduke Formation from Western Junggar, China" . | MARINE AND PETROLEUM GEOLOGY 168 (2024) . |
| APA | Zhang, Xinsong , Du, Weidong , Zong, Ruiwen , Yin, Jiayi . River-fed basin-fill and hyperpycnites in an island-arc setting: The Silurian-Devonian - Devonian Kekexiongkuduke Formation from Western Junggar, China . | MARINE AND PETROLEUM GEOLOGY , 2024 , 168 . |
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华南中—上泥盆统碳酸盐岩高度发育,但却缺乏系统碳酸盐岩微相研究。广西都安四红山剖面和宜州拉利剖面的中—上泥盆统连续发育,是华南泥盆系重要的参考剖面。中—晚泥盆世,四红山剖面为斜坡—盆地相,而拉利剖面为台地—盆地相。本文重建了这两条剖面中—上泥盆统牙形石生物地层,在此基础上结合碳酸盐岩微相沉积学研究,恢复了它们同时期沉积环境演变过程,为不同地层单元的区域对比提供了可靠依据。在吉维特期和弗拉期FZ1～FZ4期,四红山剖面主要为分水岭组硅质灰岩及“榴江组”钙质泥岩,拉利剖面主要为老爷坟组礁灰岩。而在弗拉期牙形石带FZ5～FZ8期间,两条剖面均因海侵事件造成台地淹没形成五指山组,主要特征为大化石稀少的微晶/瘤状/泥质条带灰岩,本次海侵可以与全球Middlesex事件相对应。此外中—晚泥盆世一系列生物环境事件,如F-F事件可通过牙形类的种群更替得以识别。
Keyword ：
吉维特阶 吉维特阶 广西 广西 弗拉阶 弗拉阶 沉积微相 沉积微相 泥盆纪 泥盆纪 牙形类 牙形类
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| GB/T 7714 | 安晏庆 , 张欣松 , 杜伟东 . 广西中—晚泥盆世拉利和四红山剖面的碳酸盐岩微相和牙形石生物地层格架 [J]. | 地层学杂志 , 2024 , 48 (02) : 147-171 . |
| MLA | 安晏庆 et al. "广西中—晚泥盆世拉利和四红山剖面的碳酸盐岩微相和牙形石生物地层格架" . | 地层学杂志 48 . 02 (2024) : 147-171 . |
| APA | 安晏庆 , 张欣松 , 杜伟东 . 广西中—晚泥盆世拉利和四红山剖面的碳酸盐岩微相和牙形石生物地层格架 . | 地层学杂志 , 2024 , 48 (02) , 147-171 . |
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The Silurian-Devonian Boundary (SDB) was the first Global Stratotype Section and Point (GSSP) to be established. Extensive and well-preserved SDB strata are found in Western Europe and North America. Territory of China is composed of multiple plates and terranes, which were located in the equatorial and low-latitude regions of the northern hemisphere during the late Silurian to the Early Devonian. Due to the Kwangsian Orogeny, continuous Silurian-Devonian sequences are absent in the main parts of North China, Yangtze, and Tarim cratons in China. Accordingly, continuous stratal sections across the SDB have only been sporadically reported from the orogenic belts and southwestern margin of South China. The lack of continuous carbonate sediments during the Silurian-Devonian and scarcity of fossil markers obtained has long time limited for complex research on the SDB in China. However, the discovery of the conodont Caudicriodus woschmidti in several regions, and the widespread presence of encrinurid trilobites and crinoids, have allowed recognition of the SDB in China. Abundant volcanic material near the SDB facilitates high-precision chronological studies. Apart from the global delta 13C positive excursion and Icriodus Event above the SDB, most other events are only evident in certain regions or even in a single section. Therefore, there is an urgent need for more data and evidence from other areas and plates. This work summarizes research on the SDB in China from various tectonic settings, tectonic plates, and from different facies and regions, and provides a brief review of the research history, current state of art, achievements in study of the SDB in China, and outlines prospects for future research.
Keyword ：
Biostratigraphy Biostratigraphy Central Asian Orogenic Belt Central Asian Orogenic Belt China China Conodont Conodont Silurian-Devonian Boundary (SDB) Silurian-Devonian Boundary (SDB) Trilobite Trilobite
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| GB/T 7714 | Yin, Jiayi , Slavik, Ladislav , Wang, Zhihong et al. The Silurian-Devonian Boundary of China: Review and perspectives [J]. | EARTH-SCIENCE REVIEWS , 2024 , 254 . |
| MLA | Yin, Jiayi et al. "The Silurian-Devonian Boundary of China: Review and perspectives" . | EARTH-SCIENCE REVIEWS 254 (2024) . |
| APA | Yin, Jiayi , Slavik, Ladislav , Wang, Zhihong , Shen, Zhen , Zhang, Xinsong , Liu, Yilong et al. The Silurian-Devonian Boundary of China: Review and perspectives . | EARTH-SCIENCE REVIEWS , 2024 , 254 . |
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The Upper Devonian Hongguleleng Formation is a significant stratigraphic unit near the Frasnian/Famennian and Devonian/Carboniferous boundaries of the Kazakhstan Paleoplate. However, its age is still under debate. A new palynostratigraphic analysis was conducted at the Gennaren section to provide a more accurate biostratigraphic assignment. In this study, we identified 43 species belonging to 26 spore genera, including those in open nomenclature. Despite the poor preservation of the palynofloras, the spore taxa were categorized into two assemblages. Assemblage I is established at the lower part of the lower member of the Hongguleleng Formation, containing Cornispora varicornata, cf. Auroraspora pseudocrista, and Cyrtospora cristifera. Assemblage II is from the upper part of the lower member of the Hongguleleng Formation, including Grandispora cornuta, Grandispora famennensis var. famennensis, Grandispora cf. famennensis var. minutus, Grandispora microseta, and Rugospora radiata. These assemblages are compared with the Western European DV Oppel Zone (lower-middle Famennian), and the GF to VCo Oppel zones. The assemblages are equivalent to the conodont crepida-rhom- boidea and marginifera to Lower trachytera zones (middle-upper Famennian). (c) 2024 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights are reserved, including those for text and data mining, AI training, and similar technologies.
Keyword ：
Devonian/Carboniferous boundary Devonian/Carboniferous boundary Famennian Famennian Hongguleleng Formation Hongguleleng Formation Palynostratigraphy Palynostratigraphy Western Junggar Western Junggar
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| GB/T 7714 | Shen, Zhen , Steemans, Philippe , Pereira, Zelia et al. Palynological assemblages from Hongguleleng Formation of Western Junggar, Northwest China and their correlation with conodont zonation [J]. | PALAEOWORLD , 2024 , 33 (6) : 1580-1593 . |
| MLA | Shen, Zhen et al. "Palynological assemblages from Hongguleleng Formation of Western Junggar, Northwest China and their correlation with conodont zonation" . | PALAEOWORLD 33 . 6 (2024) : 1580-1593 . |
| APA | Shen, Zhen , Steemans, Philippe , Pereira, Zelia , Zong, Rui-Wen , Zhang, Xin-Song , Ma, Kun-Yuan et al. Palynological assemblages from Hongguleleng Formation of Western Junggar, Northwest China and their correlation with conodont zonation . | PALAEOWORLD , 2024 , 33 (6) , 1580-1593 . |
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<正>华南泥盆纪碳酸盐岩地层广泛发育,沉积厚度大,分布范围广,满足油气成藏条件是有利成藏区带。近二十年来,牙形石生物地层的建立为不同区域层序地层划分提供了可靠年代地层格架。但近十年来华南碳酸盐岩沉积研究主要聚焦于个别关键事件如弗拉期和法门期之交绝灭事件,导致目前华南中-晚泥盆世碳酸盐岩斜坡-盆地长周期的沉积环境演变尚不明确,其碳酸盐岩生产过程缺乏牙形石生物地层带来的时间地层格架控制,尤其是五指山组这一广为人知的浮游相碳酸盐岩的下界不明确,此前研究主要是上世纪八十至九十年代的成果,需要更新。
Keyword ：
地层控制 地层控制 晚泥盆世 晚泥盆世 海平面变化 海平面变化 牙形石 牙形石 碳酸盐岩微相 碳酸盐岩微相
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| GB/T 7714 | 安晏庆 , 张欣松 , 杜伟东 . 广西中-晚泥盆世在牙形石生物年代地层控制下的碳酸盐岩微相及海平面变化 [C] //第十七届全国古地理学及沉积学学术会议摘要集——专题4 沉积作用与岩相古地理 . 2023 . |
| MLA | 安晏庆 et al. "广西中-晚泥盆世在牙形石生物年代地层控制下的碳酸盐岩微相及海平面变化" 第十七届全国古地理学及沉积学学术会议摘要集——专题4 沉积作用与岩相古地理 . (2023) . |
| APA | 安晏庆 , 张欣松 , 杜伟东 . 广西中-晚泥盆世在牙形石生物年代地层控制下的碳酸盐岩微相及海平面变化 第十七届全国古地理学及沉积学学术会议摘要集——专题4 沉积作用与岩相古地理 . (2023) . |
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The Ediacaran glaciation has garnered considerable attention for its potential biological impact because it witnesses the birth of complex animals. Many researchers question whether large-scale regional or even global glaciations, represent critical barriers to the evolution of macroscopic animals. So how did complex animals survive during a major glaciation? One possible explanation is the existence of isolated shallower refugia or icefree oases. However, the sedimentary evolution of such ice-free oases and how they could support the survival of complex life forms are not yet fully understood. This study focuses on the inter-diamictite black sediments in the Ediacaran Talisayi Formation of NW China (Yili block), which may represent a habitable ice-free oasis during the Gaskiers glaciation. The sedimentary facies and geochemical analyses indicate that these deposits were formed in oxygenated and photic shallow glacier lake environments with highly developed microbial mat substrates, it was formed during a short-lived partial deglaciation with enhanced weathering. And diverse organic-wall microfossils were found within the inter-diamictite black sediments. Furthermore, based on the growth habits of modern microbial algal mats, a paleontological clock can be established to estimate the duration of partial deglaciation, which may have lasted only for thousands of years. The ice-free oasis formed during this period could potentially harbor complex ecosystems, providing valuable ecological and temporal windows for the evolution of complex animals.
Keyword ：
Ediacaran Ediacaran Gaskiers glaciation Gaskiers glaciation Ice free oasis Ice free oasis Microbial mat Microbial mat Partial deglaciation Partial deglaciation
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| GB/T 7714 | Zhang, Xinsong , An, Yanqing , Chen, Yarui et al. Microbial mat, organic-wall microfossils and geochemistry of the Ediacaran inter-diamictite black sediments in NW China: A short-lived habitable benthic, oxic and photic "ice-free oases" [J]. | PRECAMBRIAN RESEARCH , 2023 , 401 . |
| MLA | Zhang, Xinsong et al. "Microbial mat, organic-wall microfossils and geochemistry of the Ediacaran inter-diamictite black sediments in NW China: A short-lived habitable benthic, oxic and photic "ice-free oases"" . | PRECAMBRIAN RESEARCH 401 (2023) . |
| APA | Zhang, Xinsong , An, Yanqing , Chen, Yarui , Du, Weidong , Wang, Liyuan . Microbial mat, organic-wall microfossils and geochemistry of the Ediacaran inter-diamictite black sediments in NW China: A short-lived habitable benthic, oxic and photic "ice-free oases" . | PRECAMBRIAN RESEARCH , 2023 , 401 . |
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One of the five great mass extinctions of the Phanerozoic is the Frasnian-Famennian (F-F) mass extinction, for which the causes have not yet been identified. In this study, cyclostratigraphic analysis of two F-F transition sections was carried out in South China: the Yangdi section, a marine slope facies, and the Lali section, a marine basin facies. Paleoclimate proxy data collected at high resolution along these sections include magnetic susceptibility and X-ray fluorescence geochemistry (Ca and Fe concentrations). Time series analysis and modeling of the proxy data reveal that frequencies comparable to those of the Earth's long and short orbital eccentricity, obliquity, and precession index characterize the two successions. Metronomic 405-kyr long orbital eccentricity cycles identified along the two sections were used to construct a floating astronomical time scale across the F-F transition, revealing that 1000 kyr separates the Lower and Upper Kellwasser horizons (LKH and UKH), and similar to 1600 kyr separates the maximum values of the LKH and UKH delta C-13 excursions. The estimated duration of the UKH is 150 kyr, during which the first, second, and third extinctions of the F-F biotic crisis lasted 120 kyr, 20 kyr, and 10 kyr, respectively. Sedimentary noise models of the magnetic susceptibility and Ca concentration time series indicate that changes in sedimentary noise correspond to sea level variations. Modeling suggests that the long orbital eccentricity cycles controlled sea surface temperatures, and that third-order eustatic changes were forced by the combined orbital eccentricity and obliquity variations. Finally, we propose an "astronomical climate change" model as a defining mechanism of the F-F biotic crisis.
Keyword ：
Cyclostratigraphy Cyclostratigraphy F-F mass extinction F-F mass extinction Kellwasser events Kellwasser events Orbital forcing Orbital forcing Sea level changes Sea level changes
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| GB/T 7714 | Ma, Kunyuan , Hinnov, Linda , Zhang, Xinsong et al. Astronomical climate changes trigger Late Devonian bio- and environmental events in South China [J]. | GLOBAL AND PLANETARY CHANGE , 2022 , 215 . |
| MLA | Ma, Kunyuan et al. "Astronomical climate changes trigger Late Devonian bio- and environmental events in South China" . | GLOBAL AND PLANETARY CHANGE 215 (2022) . |
| APA | Ma, Kunyuan , Hinnov, Linda , Zhang, Xinsong , Gong, Yiming . Astronomical climate changes trigger Late Devonian bio- and environmental events in South China . | GLOBAL AND PLANETARY CHANGE , 2022 , 215 . |
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The Hongguleleng Formation, the highest and most important Devonian marine carbonate horizon in western Junggar, contains an endemic shallow-water Icriodus-Polygnathus conodont fauna with rare palmatolepids and other genera. The conodont faunas from the Bulongguoer and the Wulankeshun sections are similar, with high abundance (about 40%) of endemic taxa (13 taxa), indicating isolation of the Junggar Basin during early Famennian. Non-endemic species in the faunas suggest that the Lower Member of the Hongguleleng Formation is assignable to the Pa. rhomboidea Zone to the Pa. marginifera marginifera Zone of early Famennian, not including the Frasnian-Famennian boundary. The Upper Member may be of late Famennian-early Tournaisian in age on the basis of our preliminary faunal analysis. (c) 2021 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
Keyword ：
Conodont Conodont Famennian Famennian Hongguleleng Formation Hongguleleng Formation Upper Devonian Upper Devonian western Junggar western Junggar
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| GB/T 7714 | Zhang, Xin-Song , Over, D. Jeffrey , Gong, Yi-Ming . Famennian conodonts from the Hongguleleng Formation at the Bulongguoer stratotype section, western Junggar, Northwest China [J]. | PALAEOWORLD , 2021 , 30 (4) : 677-688 . |
| MLA | Zhang, Xin-Song et al. "Famennian conodonts from the Hongguleleng Formation at the Bulongguoer stratotype section, western Junggar, Northwest China" . | PALAEOWORLD 30 . 4 (2021) : 677-688 . |
| APA | Zhang, Xin-Song , Over, D. Jeffrey , Gong, Yi-Ming . Famennian conodonts from the Hongguleleng Formation at the Bulongguoer stratotype section, western Junggar, Northwest China . | PALAEOWORLD , 2021 , 30 (4) , 677-688 . |
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