Origins 10(2):93-95 (1983).
GENERAL SCIENCE NOTE
The steady spontaneous transmutation of a radioactive isotope into a
stable daughter isotope provides a means for determining the length of time the
accumulation of daughter atoms has been maintained in association with its parent
source — the radioisotope age of the mineral that contains the parent and daughter
atoms. It is reasonable to expect that a radioisotope age for a mineral formation should
specify the length of time that formation has been in existence, and also the minimum age
of any fossils that may be associated with it. On this basis a quantitative geologic time
scale has been developed (Harlan et al. 1964, 1971).
To be suitable for geologic time scale calibration a radioisotope age
must meet three requirements: chemical isolation, stratigraphic control, and biological
control. To meet the requirement of chemical isolation there must be no indication that
either radioactive parent atoms or daughter type atoms have been transferred into or out
of the mineral during the indicated time period. Diffusion due to heat, and solution or
deposition due to contact with water can violate the chemical isolation requirement.
Stratigraphic control requires that the mineral sample come from a clearly defined
geologic formation which has an expected age range that is consistent with the
radioisotope age of the sample. For example, a radioisotope age of either 100 million
years (m.y.) or 3000 m.y. would not be accepted as the "true" real time age of a
rock obtained from a geologic formation that is unquestioningly of Cambrian
classification, regardless of how precise and accurate the isotope determinations may be.
To be desirable as a calibration of the phanerozoic time scale, a radioisotope age should
also meet standards of biological control, i.e., it should relate to a mineral sample that
is associated with the proper index fossils for the age in question. While biological
control and stratigraphic control are interrelated, applying each explicitly makes a more
stringent requirement. The reader who is interested in the stance of the professional
literature on these criteria should consult W. B. Harland et al. (1964), George V. Cohee
et al. (1978), and Giles S. Odin (1982).
Lack of chemical isolation generally (but not always) has been expected
to produce radioisotope ages that are most likely to be younger than the correct real time
age, particularly when the daughter isotope is highly mobile, as is the case for the inert
gas (argon) produced by the radioactive decay of potassium. Radioisotope ages that are
younger than what would be expected on the basis of stratigraphic control and biological
control are usually accounted for as evidence that chemical isolation has not been
maintained.
Radioisotope ages that are older than allowable on the basis of
stratigraphic or biological control are explained as due to retention of daughter isotopes
from a state in which the mineral components existed previous to the association in which
they are now found. Brooks et al. (1976) list 22 examples of rubidium-strontium (Rb-Sr)
ages ranging from 70 million to 3300 m.y. which are stratigraphically constrained to
represent volcanic activity within the last 65 m.y. (late Flood and/or post-Flood volcanic
activity, according to conservative Biblical creationist interpretations of geology). Five
continents are represented in this set of examples. Othman et al. (1984) have recently
reported an extensive study of 32 typical worldwide granulite samples that have geologic
age assignments ranging from 20 to 3100 m.y., yet have samarium-neodymium (Sm-Nd)
radioisotope ages that in most cases are greater than the geologic ages and range from 851
to 3744 m.y. Rb-Sr ages for this sample set range from 596 to 3650 m.y. Allègre and
Rousseau (1984) report Sm-Nd ages ranging from 1870 to 3780 m.y. for a set of seven
Australian shale samples that have geologic age assignments ranging from 200 to greater
than 3300 m.y.
In contrast with the earlier perception that potassium-argon (K-Ar)
ages for glauconites are probably less than the formation age, it has now been established
that K-Ar ages for a glauconite should be considered suspect as too old, due to possible
incorporation of radiogenic argon along with potassium at the time of glauconite formation
(Odin and Dodson 1982). Volcanics associated with organic material that can be dated by
radioactive carbon generally have a K-Ar age much greater than that given by radiocarbon
for the eruption (Stapor and Tanner 1973). A prime example is the 485,000 K-Ar age for
volcanics from a Mt. Rangitoto eruption which destroyed trees less than 300 C-14 years old
(McDougall et al. 1969).
The brief review reported in this article should make it apparent that
while techniques for the determination of radioisotope age are precise and accurate, the
interpretation of a radioisotope age in terms of real time is subjective and will reflect
the biases of the interpreter. For illustration, consider the 12.3 to 519 m.y. K-Ar ages
obtained for glauconitized coprolites from the Gulf of Guinea (see Odin and Dodson 1982,
p. 286). A 12.3 million year age for a mineral presumed to have formed 500 m.y. ago could
be explained as the consequence of argon loss caused by heating in a recent portion of the
presumed 500 m.y. existence of the specimen. The 12.3 m.y. age also could be explained on
the basis of radiogenic argon incorporation together with potassium in a crystallization
that occurred only 4000 years ago. And the 12.3 m.y. could be considered to be a
"correct" indication of the time this glauconite has been in existence (Odin and
Dodson only presume that these coprolites formed "less than 100,000 years ago").
Each of these interpretations is equally valid scientifically until measured against
definitive evidence to the contrary. One's theoretical biases will determine what he
allows as definitive evidence, and how he treats this evidence. Returning to the title for
this review, it can be said that the real time interpretation of a radioisotope age for a
rock is no more solid than the theoretical perspective of the interpreter.
REFERENCES
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