Issue 6,1988 Table of Contents

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  • 1  FRESH-WATER MOLLUSCAN FAUNA ACROSS JURASSICCRETACEOUS BOUNDARY IN SOUTHEAST JILIN
    Zhu Guoxin Zhou Yuzhang
    1988(6):717-717. DOI: 10.19800/j.cnki.aps.1988.06.013 CSTR:
    [Abstract](9) [HTML](0) [PDF 140.68 K](198)
    Abstract:

    Southeast Jilin includes Tonghua, Hunjiang, Liuhe, Jiaohe, etc, with the Sankeyushu section in the Sanyuanpu Basin taken as the type locality and the sequence described as follows: K2 Sankeyushu Formation: neutral volcanic rock

    2  STUDY ON STROMATOLITIC DECLINE EVENT IN TERMINAL PRECAMBRIAN
    Cao Ruiji
    1988(6):747-747. DOI: 10.19800/j.cnki.aps.1988.06.014 CSTR:
    [Abstract](16) [HTML](0) [PDF 145.08 K](225)
    Abstract:
    In Precambrian, stromatolites, especially columnar stromatolites, underwent a marked evolutionary process from beginning of development through extensive flourish to rapid decline. The present paper makes a discussion on the exact data and cause of the stromatolitic decline in an attempt to reveal the evolution of biosphere and change of ecological environments in the terminal Precambrian according to a study of the stromatolitic decline event.
    3  SOME ORDOVICIAN GONIOCERATIDS OF NORTH CHINA
    Li Xuesen
    1988(6):776-776. DOI: 10.19800/j.cnki.aps.1988.06.015 CSTR:
    [Abstract](7) [HTML](0) [PDF 106.56 K](208)
    Abstract:
    The cephalopods described in the present paper were mainly collected from the Badou Formation in the Zhangqiu district of central Shandong and the Fengfeng Formation in the Fengfeng city of southern Hebei by the writer and his colleagues in 1982-1983. They consist of 3 genera and 11 species, including 1 new genus and 9 new species. This paper also discusses previous reports on the Gonioceras from China and the contrast of the Badou Formation with the Fengfeng Formation as well as ecology, migration, origin and evolution of gonioceratids.

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