Carbon-14 in Diamonds:The UCI Data

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    Graphite Versus

    Phanerozoic Carbon

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    0.1

    0.2

    0.3

    0.4

    0.5

    0.6

    0.7

    0.8

    Graphite

    Range

    Mass Spec C

    Coal

    Petroleum

    Foraminifera

    Wood

    Other

    Upper C. L.Lower C. L.

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    The RATE Group

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    Eocene

    (40 Ma)

    Cretaceous

    (100 Ma)

    Pennsylvanian

    (350 Ma)

    TX ND MT UT UT AZ KY PA PA IL

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    Other data

    0

    0.1

    0.2

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    0.5

    0.6

    0.7

    0.8

    Graphite

    Range

    Mass Spec C

    Coal

    Petroleum

    Foraminifera

    Wood

    Other

    Upper C. L.Lower C. L.

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    The UCI Diamond Data

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    Graphite

    Range

    Mass Spec C

    Diamonds

    Upper C. L.

    Lower C. L.

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    The UCI Diamond Data

    0

    0.020.04

    0.06

    0.08

    0.1

    0.12

    0.14

    0.16

    0.18

    0.2

    Graphite

    Range

    Mass Spec C

    Diamonds

    Upper C. L.

    Lower C. L.

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    The UCI Diamond Data

    0

    0.01

    0.02

    0.03

    0.04

    0.05

    0.06

    0.07

    Graphite

    Diamonds

    Upper C. L.

    Lower C. L.

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    The UCI Diamond Data

    in Chronological Order

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    0.01

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    0.07

    Graphite

    Diamonds

    Upper C. L.

    Lower C. L.

    UCIAMS-15442?

    UCIAMS-14440?

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    Implications of

    The UCI Diamond Data

    The data argue that some diamonds have

    very low 14C concentrations

    They are consistent with the hypothesis thatcontamination contributes to observed

    background

    They argue that there are differences of

    carbon-14 concentrations in diamonds.

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    Implications of

    The UCI Diamond Data

    Diamond 9639 is 9.35 standard deviations from

    the mean of Diamond 12674-12679

    That is not the proper test

    Grubbs testing gives G1=2.195895th percentile is 1.938 for 7 samples (0.0115)

    99th percentile is 2.097 (0.0092)

    100th percentile is 2.2678

    Grubbs testing on Diamond 9640 gives 2.182

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    Authors Comments

    At this time, it is not clear to us what factorsmight be involved in the greater variability in theapparent 14C concentrations exhibited in

    individual diamonds (Section B) as opposed tosplits from a single natural diamond (Section A).Possible factors suggested to us are greatervariability in the orientation of the crystal faciesand microfractures in individual diamonds.

    Note the absence of the possibility of differencesin actual 14C content due to residual activity.

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    Summary

    The data indicate that there is residualcarbon in at least some diamonds

    This indication is getting stronger with time

    Residual carbon requires a short ageIt destroys the standard geological timescale

    Long-agers are unlikely to concede this fact

    If I have to argue, I prefer that the datasupport my argument

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    The End

    Now its Erv Taylors turn