Research Updates

Updatetime: 2018-02-13

 

  ↑ Late Cretaceous ostracod fauna from the Shenjiatun Section (Songliao Basin, Northeast China): Biostratigraphic and Palaeoecological implications. (WANG Yaqiong et al., 2017.Cretaceous Research)  

 

 

  ↑ Clam shrimp genus Ordosestheria from the Lower Cretaceous Dalazi Formation in Jilin Province, north-eastern China. (TENG Xiao, LI Gang, 2017.Cretaceous Research) 

    

 

  ↑ Brachiopod faunas after the end Ordovician mass extinction from South China: Testing ecological change through a major taxonomic crisis. (HUANG Bing et al., 2017.Journal of Asian Earth Sciences) 

     

 

  ↑ SEM morphological study of clam shrimp Diestheria (spinicaudatan) of the Jehol Biota of China. (LI Yuling et al., 2017.Sci. Rep.Niigata Univ.(Geology)) 

    

 

  ↑ Middle–Late Ordovician chitinozoans from the Yichang area, South China, and their macroevolutionary and palaeobiogeographical implications.  (LIANG Yan et al., 2017.Review of Palaeobotany and Palynology)   

 

 

  ↑ Acanthomorphic acritarchs of the Doushantuo Formation from an upper slope section in northwestern Hunan Province, South China, with implications for early–middle Ediacaran biostratigraphy. (OUYANG Qing et al., 2017.Precambrian Research). 

 

 

  ↑ Microfacies analysis of the Lower-Middle Ordovician succession at Xiangshuidong, southwestern Hubei Province, and the drowning and shelf-ramp transition of a carbonate platform in the Yangtze region. (LUAN Xiaocong et al., 2017.Palaeogeography, Palaeoclimatology, Palaeoecology) 

    

 

  ↑ Llandovery (Silurian) conodont provincialism: An update based on quantitative analysis. (CHEN Zhongyang et al., 2017. Palaeogeography, Palaeoclimatology, Palaeoecology)  

 

 

  ↑ Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation. (ZHANG Junpeng et al., 2017.Scientific Reports) 

    

 

  ↑ Integrated conodont biostratigraphy and carbon isotope chemostratigraphy in the Lower–Middle Ordovician of southern Sweden reveals a complete record of the MDICE. (WU Rongchang et al., 2017.Geological Magazine) 

    

 

  ↑ Nuclei and nucleoli in embryo-like fossils from the Ediacaran Weng’an Biota. (YIN Zongjun et al., 2017.Precambrian Research)  

    

 

  ↑ Astronomical tuning and magnetostratigraphy of the Upper Triassic Xujiahe Formation of South China and Newark Supergroup of North America: Implications for the Late Triassic time scale. (LI Mingsong, et al., 2017.Earth and Planetary Science Letters)  

    

 

  ↑ New Early Cretaceous clam shrimps (Spinicaudata) from uppermost Bouhedma Formation of northern Chotts range, southern Tunisia: Taxonomy, stratigraphy and palaeoenvironmental implications. (LI Gang et al., 2017.Cretaceous Research) 

    

 

  ↑ Discovery of Late Devonian plants from the southern Yellow Sea borehole of China and its palaeogeographical implications. (GUO Xingwei, XU Honghe* et al., 2017.Palaeogeography, Palaeoclimatology, Palaeoecology) 

 

 

  ↑ Graptolite diversification during the Floian and Dapingian (Early-Middle Ordovician): A case study from the Ningkuo Formation of Hunan Province, China. (LI Lixia et al., 2017.Palaeoworld)  

 

 

  ↑ Tremadocian (Early Ordovician) chitinozoan biostratigraphy of South China: An update. (LIANG Yan et al., 2017.Review of Palaeobotany and Palynology) 

    

  

  ↑ Stromatolites in Middle Ordovician carbonate–evaporite sequences and their carbon and sulfur isotopes stratigraphy, Ordos Basin, northwestern China. (MENG Fanwei et al., 2017.Carbonates and Evaporites) 

 

 

  ↑ Post-glacial Foraminifera of the incised Yangtze paleo-valley and paleoenvironmental implications. (KE Xue, LI Baohua* et al., 2017.Journal of Paleontology) 

 

  

  ↑ Late Triassic ecosystem variations inferred by palynological records from Hechuan, southern Sichuan Basin, China. (LI Liqin et al., 2017.Geological Magazine) 

 

 

  ↑ Orthrozanclus elongata n. sp. and the significance of sclerite-covered taxa for early trochozoan evolution. (ZHAO Fangchen et al., 2017.Scientific Reports) 

    

 

  ↑ The Yudomski Event and subsequent decline: New evidence from δ34S data of lower and middle Cambrian evaporites in the Tarim Basin, western China. (MENG Fanwei et al., 2017.Carbonates and Evaporites) 

.....CONTENTS OF PALAEONEWS NO.6.....


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