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Information Journal Paper

Title

THE CAUSE OF BIOMASS EXTINCTION AT THE FRASNIAN-FAMENNIAN BOUNDARY, THE KERMAN PROVINCE SOUTHEASTERN, CENTRAL IRAN

Pages

  45-49

Abstract

 About 35 samples were collected from lower and upper parts of the proposed Frasnian-Famennian boundary in three sections of Upper Devonian marine sediments of the Kerman province. The biostratigraphical and geochemical studies indicate that about 45% extinction of brachiopods probably caused by the Frasnian-Famennian bioevents, which is slightly higher than thr rate of Devonian- Carboniferous extinction elsewhere. The results of isotopic carbon and oxygen isotope analysis (δ 13C%0 VPDB and δ 10O %VPDB) show a sudden decrease at the proposed Frasnian-Famennian extinction boundary which is followed by positive values above this horizon. The negative excursion may indicate a biomass extinction due to either a meteorite impact or decay of organic matter. The isotopic variations are correlated with those of faunal changes and their extinctions in the area.

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  • Cite

    APA: Copy

    DASTANPOUR, M., & AFTABI, A.. (2002). THE CAUSE OF BIOMASS EXTINCTION AT THE FRASNIAN-FAMENNIAN BOUNDARY, THE KERMAN PROVINCE SOUTHEASTERN, CENTRAL IRAN. JOURNAL OF SCIENCES ISLAMIC REPUBLIC OF IRAN, 13(1), 45-49. SID. https://sid.ir/paper/542271/en

    Vancouver: Copy

    DASTANPOUR M., AFTABI A.. THE CAUSE OF BIOMASS EXTINCTION AT THE FRASNIAN-FAMENNIAN BOUNDARY, THE KERMAN PROVINCE SOUTHEASTERN, CENTRAL IRAN. JOURNAL OF SCIENCES ISLAMIC REPUBLIC OF IRAN[Internet]. 2002;13(1):45-49. Available from: https://sid.ir/paper/542271/en

    IEEE: Copy

    M. DASTANPOUR, and A. AFTABI, “THE CAUSE OF BIOMASS EXTINCTION AT THE FRASNIAN-FAMENNIAN BOUNDARY, THE KERMAN PROVINCE SOUTHEASTERN, CENTRAL IRAN,” JOURNAL OF SCIENCES ISLAMIC REPUBLIC OF IRAN, vol. 13, no. 1, pp. 45–49, 2002, [Online]. Available: https://sid.ir/paper/542271/en

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