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Terminal cretaceous environmental events.

C B Officer, C L Drake

    Science (New York, N.Y.)
    |March 8, 1985
    PubMed
    Summary
    This summary is machine-generated.

    The geologic record shows iridium was deposited over thousands of years, not instantaneously. Evidence suggests volcanic activity, not an asteroid impact, caused these terminal Cretaceous environmental events.

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    Area of Science:

    • Geochemistry
    • Paleontology
    • Volcanology

    Background:

    • The terminal Cretaceous period is marked by significant environmental changes.
    • The origin of iridium and associated elements found in the geologic record has been debated.
    • Distinguishing between impact events and volcanic activity is crucial for understanding past extinctions.

    Purpose of the Study:

    • To analyze the depositional timeframe of iridium and associated elements.
    • To determine the origin of these elements (mantle vs. meteoritic).
    • To evaluate the likelihood of an asteroid impact versus volcanic events as the cause of terminal Cretaceous environmental changes.

    Main Methods:

    • Geologic record analysis
    • Elemental deposition analysis

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  • Chronological dating of geologic strata
  • Main Results:

    • Iridium and associated elements were deposited over a period of 10,000 to 100,000 years.
    • Geologic evidence supports a mantle origin for these elements.
    • The findings align with a scenario of intense volcanic activity, not a single asteroid impact.

    Conclusions:

    • The deposition of iridium and associated elements was not instantaneous.
    • Volcanic activity is favored as the source of these elements.
    • A series of volcanic events, rather than an asteroid impact, likely caused the terminal Cretaceous environmental changes.