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《Journal of Stratigraphy》 1992-01
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Recent advance in the research of the strata near the Jurassic-Cretaceous boundary in eastern Heilongjiang

Sun Ge, Zheng Shao-lin, Sun Xue-kun, He Cheng-quan, Piao Tai-yuan, Shang Yu-ke, Zhang Chuan-bo, Yu Zi-ye and Zhao Yan-hua  
The finding of the new marine beds with Valanginian-Hauterivian dinoflagellates intercalated in the lower Chengzihe Formation and the new discovery of the earliest angio-sperm megafossils from the upper part of the formation, made recently by the authors, have shown the geological age of the Chengzihe Formation as early-middle Early Cretaceous, approximately corresponding to Berriasian (Ryazanian)-Hauterivian(or to early Barremian). The biozones represented by Buchia of the Donganzhen Formation are revised by the authorsas following: B,-B. pacifica (L. Valanginian), B3-B. volgensis-B. cf. okensis-B. cf.subokensis-B. unschensis (Ryazanian-E. Valanginian), B2-B. fischeriana-B. unschensis (L.Volgian), B,-B. russiensis-B. fischeriana (M. Volgian). The J-K. boundary (i. e. betweenthe B2 and B3) is redefined as that lower for 4.9m than before and with the first occurrence of B. cf. subokensis as the lowest Lower Cretaceous (i. e. the Upper Subformation of Donganzhen Fm). The geological ages of the "Shihebei Fm", Dongrong Fm and the Longzaogou Group are also discussed.
【Fund】: 中国科学院院长基金
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