How well do paleontologists know fossil distributions?
by Michael Oard
It is unfortunate but true. Similar fossils can be given different names when found
in strata of different supposed ages. This practice masks the true range of the
fossil within the geological time scale. In a recent example, even though the fossils
were almost identical, they were assigned to different species. Such practices multiply
the number of names, confuse our knowledge of fossil distribution, and hide the
fact that the geological column may well be compromised.
It would be great if we could know the actual three-dimensional distribution of
the fossils in the earth. This would go a long way towards understanding their deposition
during the Flood. Usually all that is available is a fossil sample along a cliff,
ravine or some other cut into a particular formation.
One might think that good extrapolations have been made from these limited, two-dimensional
outcrops and that the fossil content in the remainder of the formation is well understood.
But some surprises would be in store if we could actually know the distribution
of all the fossils in the formation. The more the sedimentary rocks of the earth
are examined, the more the fossil ranges are expanded—especially downward.
One such surprise occurred on Vancouver Island, British Columbia, Canada, when a
sponge of Upper Triassic ‘age’ (the standard geological time scale is
used for communication purposes only) was discovered in a carbonate formation.1 It was named Nucha? vancouverensis
sp. nov. Now, the formation where the sponge was found is considered
a standard reference for the North American Triassic because of its ammonoid index
fossils. Surprisingly, the sponge is nearly identical to one previously found only
in the Middle Cambrian of western New South Wales, Australia, named Nucha naucum.2
In spite of the obvious similarity, because the Vancouver Island specimen was not
exactly the same as its Australian counterpart, a question mark was placed
after its genus name and it was given a different species name. Still, the researcher
who reported the find, George Stanley, believes the similarities are striking enough
to put the fossil in the same genus.
The Vancouver Island fossil is used to support some very large geological ideas—that
an exotic terrane3 (the Wrangellia
terrane) was plastered onto the western side of the North America plate from an
unknown, tropical-ocean locality. The problem is that the two fossils are located
on opposite sides of Pangaea, the hypothetical, huge ancient landmass of the Paleozoic.
Their respective oceans were supposedly separated by thousands of kilometres of
continent.
Because it was previously only known from Australia, Nucha is considered
a Tethyan taxon from the Paleozoic tropics.4
So the two fossils, although very similar in appearance, are separated greatly in
space and time.
Stanley downplays the significance of the separation in time: ‘The absence
of Nucha between Middle Cambrian and Late Triassic time is somewhat of
a conundrum.’5 The reason for
this nonchalant attitude toward a fossil not found during a supposed 300 million-year
period and separated spatially by a considerable distance is, I believe, because
this case is not isolated.
In fact, Stanley mentions several examples and refers to other authors who know
of a number of other examples. These seeming anomalies are referred to as ‘holdover
taxa’, ‘refugia species’, or even ‘Lazarus taxa’.
Of course, if a representative of the fossil is found alive today, it is called
a ‘living fossil’. The importance of such holdover taxa to paleontologists
is stated by Stanley:
‘Of great interest to paleontologists and evolutionary biologists alike is
the occurrence of relict or holdover faunas, also known as Lazarus taxa. These taxa,
mostly at family, genus, and species levels, appear to leapfrog large intervals
of geologic time, including the recovery phases following mass extinctions. They
seem to elude our most concerted sampling efforts, failing to be accounted for over
considerable intervals of time.’2
What lessons do such holdover taxa have for creationists? First, they show that
geologists and paleontologists do not know the three-dimensional distribution of
fossils, although they may have reasonable estimates in isolated formations. There
have been and will always be surprises. Fossils seem to be constantly extending
their geological time ranges. We should be sceptical of statements to the effect
that a particular fossil is an index fossil that is restricted to, say, the Cambrian
‘period’, or the Permian ‘period’, etc.
Second, such holdover taxa make it hard to believe that the alleged millions of
years between the fossil occurrences are real. Where was the organism living all
those millions of years? Why is there no fossil record of its existence throughout
all that time? In this particular example, paleontologists may eventually find fossils
of this sponge between the ‘Middle Cambrian’ and the ‘Upper Triassic’.
Even so, the fossils would still be very scarce between these two ‘periods’
and a few finds would not alter the obvious conclusion that the time gap is illusory.
Third, a fossil can be assigned to a different species because it is found at a
supposed different geologic time, obscuring the true range of the taxon within the
geological time scale. In the case of Nucha, the difference between the
Vancouver Island sponge and the Australian sponge was slight, but the former fossil
was given a different species name with a question mark after the genus name.
Similar practices with other taxan contribute to the multiplication of names and
a more limited distribution of taxa. Thus, the true range of any organism is likely
broader than one is led to believe by the examination of its taxonomy.
Since much variability is present within any given organism and hence its fossils,
paleontologists often do not know where to draw the line in their classification
schemes. Different names for nearly identical fossils are probably common. This
tendency to give different names to similar fossils found in formations with supposedly
different ages, even to placing them in different superfamilies, has been demonstrated
by Tammy Tosk for the microfossils called foraminifers.6
John Woodmorappe
found that much of the stratigraphic order in the ammonoids is due to time-stratigraphic
concepts and taxonomic manipulations.7
This is particularly serious because particular types of foraminifera and ammonoids
are used as index fossils for dating formations.
Geologists do not know the three-dimensional distribution of fossils in the rocks,
and tend to invent different names for similar fossils, just because they are found
in strata of supposedly different ages.8
This does not engender confidence in the geological column they construct, or in
the fossil-dating scheme on which it is based.
Acknowledgement
I thank Peter Klevberg for reviewing the manuscript and for providing input into
this issue.
References and notes
- Stanley, G.D., Jr, A Triassic sponge from Vancouver Island: possible
holdover from the Cambrian, Canadian Journal of Earth Sciences 35:1037–1043,
1998. Return to text.
- Picket, J. and Jell, P.A., Middle Cambrian Sphinctozoa (Porifera)
from New South Wales, Memoirs of the Association of Australian Palaeontologists
1:85–92, 1982. Return to text.
- A terrane is a fault-bounded geologic entity distinctively different
from its adjoining neighbour. Return to text.
- Stanley, Ref. 1, p. 1037. The Tethys Sea is a hypothetical, Palaeozoic
sea on the east coast of Pangaea, located in the tropics between Laurasia in the
north and Gondwana in the south. Return to text.
- Stanley, Ref. 1, p. 1042. Return to text.
- Tosk, T., Foraminifers in the fossil record: implications for an
ecological zonation model, Origins 15(1):8–18, 1988.
Return to text.
-
Woodmorappe, J., The cephalopods in the creation and the universal deluge: in:
Studies in Flood Geology, 2nd edition, Institute for Creation Research,
El Cajon, CA, pp. 177–197, 1999. Return to text.
- Dietz, R.S. and Holden, J.C., The Breakup of Pangaea, Scientific
American, 1970; Quoted in: Press, F. and Siever, R., Earth, 4th ed.,
W.H. Freeman and Co., New York, p. 518, 1986. Return to text.
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