Radioactive ‘dating’ in conflict!
Fossil wood in ‘ancient’ lava flow yields radiocarbon
by Andrew Snelling
When miners were sinking a ventilation shaft for the new Crinum Coal Mine in Central
Queensland in 1993 (see map below) they unearthed a rare find. After digging through
the thin surface sands and clays, followed by basalt, 21 metres (almost 69 feet)
down they found pieces of wood entombed in the bottom basalt flow.1 Below the basalt were layers of claystone, siltstone,
and sandstone with interbedded coal seams.2
Fossil wood in ‘ancient’ basalt
wood was in three states—ash, charred, and intact.1
Those on-site at the time speculated that there had been two distinct trees, partly
standing, still organic in nature, and thus not petrified. The imprint of a leaf
was also discovered within the basalt, which was also regarded as remarkable, remembering
that the enclosing rock was once molten lava erupted at 1000–1200°C (about
1800–2200°F).
So how could these tree trunks have survived being engulfed by molten lava? At approximately
four metres (13 feet) thick, the basalt flow is relatively thin,1,3 and thus
cooling would have been rapid (perhaps days, but a few weeks at most4). This is verified by the observed internal structure
of the basalt flow.1,5 Since the tree trunks were engulfed at the bottom
of the flow, cooling may have been immediate, with any water present in the wood
aiding extremely rapid encapsulation and thus preservation.
The local geological context makes the basalt flow approximately ‘30 million
years old’,1,3
in keeping with other basalt flows in the region all regarded as of Tertiary age
(in the conventional terminology). Since the tree trunks were entombed in the basalt
lava, the wood is thus supposedly at least 30 million years old. Also, what looked
like the tree roots were found in the siltstone below the basalt,3
suggesting the trees when alive were rooted into the siltstone and thus growing
on a land surface that was then covered by basalt lava. This siltstone belongs to
the Permian German Creek coal measures, conventionally believed to be around 255
million years old.6
Collection of samples
Small fragments of some of the wood samples were kindly sent to us, and a subsequent
mine visit took place in late August 1994.7
The pieces of wood recovered by the miners were examined and photographed, as too
was the leaf imprint, but access to the ventilation shaft was not possible, nor
were samples of the enclosing basalt available, having long been dumped with all
the other rubble and waste rock. However, an exploratory hole had been drilled close
to where the shaft was eventually dug. In the relevant drill core, at the bottom
of the lowermost basalt flow, pieces of fossil wood still containing organic carbon
were present encased in the basalt, right at the boundary of the basalt flow with
the siltstone below. This drill core was subsequently sent to us once permission
was granted by the mining company.7
After visiting the mine site, nearby outcrops of the same basalt flows were investigated
and sampled. This was to make sure we at least had some samples of the basalt, just
in case permission to have the drill core wasn’t forthcoming.
Charred fossil wood.
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Intact fossil wood.
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Basalt with holes from former gas bubbles.
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Fossil tree with roots in siltstone.
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Laboratory work
Tiny portions of the same piece of fossil wood encased in the basalt in the drill
core were sent for radiocarbon (14C) analyses to two reputable laboratories—Geochron
Laboratories in Cambridge, Boston (USA), and the Antares Mass Spectrometry laboratory
at the Australian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights
near Sydney (Australia). Neither laboratory was told exactly where the samples came
from to ensure that there would be no resultant bias. Both laboratories use the
more sensitive accelerator mass spectrometry (AMS) technique for radiocarbon analyses,
Geochron being a commercial laboratory and Antares being a major research laboratory.
Also, tiny fragments of the initial wood samples provided to us, from the pieces
of wood that had been found during sinking of the ventilation shaft, were sent off
for radiocarbon analyses—one set of different fragments to each laboratory.
Pieces of the basalt samples from the outcrop and the drill core were also sent
to analytical laboratories, for major, minor, and trace element analyses to establish
the character of these rocks, but mainly for radioactive ‘dating’ analyses.
Potassium-argon (K-Ar) ‘dating’ was performed on the two outcrop samples
by the AMDEL laboratory in Adelaide (Australia), while one of the two outcrop samples
and two drill core samples, one being in contact with the fossil wood, were ‘dated’
by Geochron Laboratories.
Results
The radiocarbon (14C) results are listed in
Table 1.8 It
is immediately evident that there was detectable radiocarbon in all wood samples,
so that the laboratories’ staff had neither hesitation nor difficulties in
calculating 14C ‘ages’. When subsequently questioned regarding
the limits of the analytical method for the radiocarbon and any possibility of contamination,
staff at both laboratories (Ph.D. scientists) were readily insistent that the results,
with one exception,9 were within the
detection limits and therefore provided quotable finite ‘ages’!8
Furthermore, they pointed to the almost identical δ13C results
(last column in Table 1), consistent with the carbon being organic carbon from wood,
and indicating no possibility of contamination. So the results in Table 1 are staunchly
defended by the laboratories as valid, indicating an ‘age’ of perhaps
44,000–45,500 years for the wood encased in the basalt retrieved from the
drill core.
In stark contrast to the ‘age’ of the wood are the potassium-argon (K-AR)
‘ages’ of the basalt (see Table
2).8 It is readily apparent that there are
significant variations in the results, as evident in the calculated ‘ages’
of the outcrop 2 sample provided by each laboratory. The problem of obtaining consistently
‘acceptable’ K-AR ‘ages’ is also highlighted by the observation
that both outcrop and both drill core samples probably represent the same basalt
flow in each respective location (hence the calculated average ‘ages’
in the last column of Table 2).10
The staff of both laboratories (again Ph.D. scientists) defended their analytical
results,8,11
and did not hesitate to affirm that these basalt samples are, according to their
radioactive K-AR ‘dating’, around 45 million years old.
|
Sample
|
Lab |
Lab code |
14C ‘age’ (BP) years |
δ13CPDB15 |
|
Wood in Drill Core
|
Geochron
ANSTO
|
GX-20798-AMS
OZB472
|
>35,620
44,700±950
|
-25.7‰
-25.78‰
|
|
Other Wood
|
Geochron |
GX-20087-AMS |
29,544±759 |
-25.1‰ |
|
Other Wood |
ANSTO |
OZB473 |
37,800±3,450 |
-26.16‰ |
|
Conclusions
While the quality and accuracy of the analytical work undertaken by all the laboratories
involved is unquestionably respected, all the calculated ‘ages’ are
mere interpretations based on unproven assumptions about constancy of radioactive
decay rates, and on the geochemical behaviour of these elements (and their isotopes)
in the unobservable past. To young-earth creationists the geological context of
these fossil wood fragments in the basalt lava flow clearly indicates that these
represent post-Flood trees overwhelmed by a post-Flood volcanic eruption nearby,
and thus both the fossil wood and the basalt are less than 4,500 years old.12
Nevertheless, within the conventional (uniformitarian) framework of interpretation,
a clear-cut conflict can be seen between these two radioactive ‘dating’
methods. Normally fossil wood found in such an ‘ancient’ basalt would
not be radiocarbon ‘dated’, because the wood would be considered far
too old for any radiocarbon to be left in it.13
Yet here these radioactive ‘dating’ methods are again demonstrated to
be unreliable and clearly useless at determining the true age of the wood and basalt.14 Therefore, any published results
from these ‘dating’ methods should not be seen as casting any doubts
whatsoever on the reliability of the biblical chronology so carefully provided for
us by the (always present) Creator Himself.
|
Basalt sample |
Lab |
Lab code |
K-Ar ‘age’ (million years) |
Average K-Ar ‘age’ (million years) |
|
Outcrop 1
|
AMDEL
|
G878300G/95
|
44.9 ±1.1
|
|
|
Outcrop 2
|
AMDEL
Geochron
|
G878300G/95
R-11800
|
47.9 ±1.6
39.1 ±1.5 |
|
Drill Core
|
Geochron
|
R-11798
|
58.3 ±2.0
|
47.5±10.8 |
|
Drill Core Enclosing Wood
|
Geochron
|
R-11799
|
36.7 ±1.2
|
|
Table 2: Potassium-argon (K-AR) ‘dates’ on basalt samples.
Return to text.
|
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References and notes
- ‘Rare find unearthed at Crinum’, BHP Australia
Coal Newsline, p. 1, December 1993–January 1994. Return to
text.
- Copies of the relevant geological cross-section and drill-hole
data were kindly supplied by the Crinum Mine Project staff. Return to
text.
- Letter dated 27 April 1994 from Greg B. Chalmers, the Chief Project
Engineer at the time for the Crinum Mine Project. Return to text.
- A.A. Snelling, The formation and cooling of dykes,
Journal of Creation 5(1):81-90, 1991. Return
to text.
- An upper section filled with vesicles (spherical holes left by
gas bubbles), a coarse-grained middle section, and a hard, dense, fine-grained bottom
section—indicative of rapid cooling from bottom up and top down simultaneously.
Return to text.
- Falkner, ‘Sedimentological studies in the German Creek coal
measures and their relevance to longwall mining’, New Developments in Coal
Geology (A Symposium), J.W. Beetson (ed.), Coal Geology Group (Geological
Society of Australia), pp. 143–148, 1993. Return to text.
- Greg B. Chalmers, then Chief Project Engineer, and BHP Australia
Coal Pty Ltd, operators of the Crinum Mine, are thanked for allowing our visit to
the mine and the photographing of their fossil wood and leaf specimens, and for
providing pieces of their fossil wood samples and the several metres of drill core
that were so crucial to this investigation. Return to text.
- Original copies of all the official laboratory analytical and ‘dating’
reports, and the correspondence with staff of the laboratories, have been kept on
file. Return to text.
- The one exception was due to the small quantity of carbon extracted
from the sample, but when repeated by the other lab, a finite ‘age’
was obtained. Return to text.
- However, other analytical results provide evidence that the outcrop
does probably represent a younger, though closely related, basalt flow to that sampled
in the drill core. Return to text.
- They did suggest the possibility of some variable contamination
of the samples with atmospheric argon, but definitely not contamination introduced
by their laboratory procedures. Return to text.
- It needs to be remembered that during the Flood and immediate
post-Flood periods the earth’s stronger, but fluctuating, magnetic field affected
the incoming cosmic ray influx, resulting thus in a lower radiocarbon production
rate and therefore radiocarbon ‘ages’ much greater than the true ages.
Return to text.
- The results of this investigation confirm that it is likely radiocarbon
may also be detected in other fossil woods found at even deeper levels in the so-called
geological column, even if the fossil wood was from pre-Flood trees buried during
the Flood. Further investigations are in progress. Return to text.
- A fuller report with all technical and analytical details, including
the results from other radioactive ‘dating’
methods and the attempted identification of the fossil wood, was later published,
Latest Technical Journal (vol. 14 no. 2) rebuts skeptics, 2000. Return
to text.
- δ13CPDB denotes the measured difference
of the ratio of 13C/12C (both stable isotopes) in the sample
compared to the PDB (Pee Dee Belemnite) standard—a fossil belemnite from the
Cretaceous Pee Dee Formation in South Carolina, USA. The units used are parts per
thousand, written as ‰ or per mil (compared with parts per hundred, written
as % or per cent). Organic carbon from the different varieties of life gives different
characteristic δ13CPDB values. Return to
text.
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