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Encyclopedia of Evolution.pdf - Online Reading Center

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chapter 10. On the imperfection <strong>of</strong> the geological record<br />

I have already explained why it is that we do not today see<br />

numerous intermediate forms between species: Natural selection<br />

favors the forms that are most distinct from the parents,<br />

and from one another, in a group <strong>of</strong> newly evolving varieties.<br />

Now I will explain why these innumerable intermediate forms<br />

seem to be absent from the fossil record as well. “… this, perhaps,<br />

is the most obvious and serious objection which can be<br />

urged against [my] theory.”<br />

The geological record is highly imperfect; indeed, it<br />

could hardly be otherwise. We know that different breeds <strong>of</strong><br />

pigeon were bred from a single ancestral species; yet there is<br />

very little if any record <strong>of</strong> this in the fossils.<br />

Go look for yourself, along a shoreline, and see the erosion<br />

that is there taking place, and think about how slowly<br />

and irregularly erosion is occurring there, to be deposited in<br />

the shallow oceans nearby. Yet this erosion has occurred,<br />

in the past, enough to produce a total <strong>of</strong> almost 14 miles <strong>of</strong><br />

depth in geological deposits, and these 14 miles represent<br />

only the period <strong>of</strong> time in which deposition was occurring,<br />

during times <strong>of</strong> the subsidence <strong>of</strong> the crust; at least half <strong>of</strong> the<br />

time, the crust was rising, causing erosion instead <strong>of</strong> subsidence.<br />

After all, if you have deposition in one location, you<br />

must have erosion somewhere else. You will not find all 14<br />

miles in any one location; this figure is calculated by adding<br />

up the deposits in one location that correspond to those <strong>of</strong><br />

another location [a procedure developed by earlier geologists;<br />

see Smith, William].<br />

During my journeys I saw, in one location, a mass <strong>of</strong><br />

conglomerate rock more than 10,000 feet thick. This rock<br />

was formed <strong>of</strong> rounded pebbles imbedded in metamorphic<br />

rock that had been transformed by heat; this conglomerate<br />

rock, therefore, was formed from earlier rocks. How old the<br />

Earth must be! Just how long is a million years? Some pr<strong>of</strong>essors<br />

have demonstrated this to their students by making a<br />

mark, one-tenth <strong>of</strong> an inch in diameter, on a strip <strong>of</strong> paper<br />

83 feet 4 inches long; the mark represents a century, the strip<br />

<strong>of</strong> paper a million years! Yet the Earth has existed many millions<br />

<strong>of</strong> years.<br />

Here are just some <strong>of</strong> the reasons that the geological<br />

strata are imperfect as a record <strong>of</strong> past life on Earth:<br />

1. Only a few places on the Earth have been thoroughly<br />

explored by geologists.<br />

2. The only organisms that are preserved as fossils are those<br />

that die:<br />

• during periods <strong>of</strong> deposition. Those that die during<br />

periods <strong>of</strong> erosion are unlikely to get covered with sediments<br />

and preserved.<br />

• at a time and place where deposition is occurring rapidly<br />

enough to bury them before they decompose. In most<br />

parts <strong>of</strong> the ocean, sediments are not accumulating; this<br />

is why most <strong>of</strong> the ocean is blue.<br />

• underwater, or where they can be transported to a riverbed,<br />

delta, or continental shelf.<br />

3. The very times when species are more likely to become<br />

extinct than to evolve new forms—the times when the<br />

appendix 429<br />

crust is subsiding, and terrestrial regions are being flooded<br />

and plunged into dark depths—are the very times when<br />

fossils are most likely to form; conversely, the times when<br />

species are most likely to evolve—the times when the crust<br />

is rising, and new terrestrial surfaces (as well as intertidal<br />

and subtidal surfaces) are being formed—are the times<br />

when fossils are least likely to form.<br />

Therefore if a species, or whole group, evolved under<br />

conditions when fossils were not forming, and were then fossilized,<br />

they would appear in the fossil record as if they were<br />

specially created. While positive evidence is trustworthy—we<br />

can trust a fossil when we find it—negative evidence (the<br />

absence <strong>of</strong> fossils) tells us nothing worthwhile. [This is one<br />

<strong>of</strong> the assertions most vigorously debated regarding punctuated<br />

equilibria.]<br />

While this may explain why the geological record, on a<br />

worldwide scale, does not preserve evidence <strong>of</strong> innumerable<br />

transitional forms, it does not explain why innumerable transitional<br />

forms are not preserved within any one formation. In<br />

particular, some species seem to appear suddenly in the fossil<br />

record, without predecessors leading up to it, even when there<br />

has been no interruption <strong>of</strong> deposition. The appearance <strong>of</strong> a<br />

species in the fossil record is much more likely to be the result<br />

<strong>of</strong> immigration from a different region, where it had already<br />

evolved, than <strong>of</strong> its sudden origin in that location. In some<br />

cases a species seems to disappear, then reappear, then disappear,<br />

then reappear; this is not because it re-evolved several<br />

times, but because it vanished, then migrated back in from<br />

another area, several times. Even within any one formation,<br />

deposition may not have been uninterrupted; each formation<br />

probably represents a whole series <strong>of</strong> switches between erosion<br />

and deposition.<br />

A more serious problem is what appears to be the<br />

sudden appearance <strong>of</strong> a great variety <strong>of</strong> multicellular lifeforms<br />

at the beginning <strong>of</strong> the Cambrian period (see Cambrian<br />

explosion). My theory, if true, should explain the<br />

origin <strong>of</strong> all these forms, gradually, from a common ancestor;<br />

therefore the world must have swarmed with creatures<br />

even before this time. There is even a good question<br />

as to whether the Earth has existed long enough for the<br />

diversity <strong>of</strong> forms seen in the Cambrian deposits to have<br />

evolved, if William Thomson’s calculations are correct. [It<br />

turned out that they were not; see Kelvin, Lord.] I can<br />

give no satisfactory explanation for the absence <strong>of</strong> fossils<br />

in Precambrian rocks. The presence <strong>of</strong> organic matter in<br />

these deposits indicates that life existed throughout that<br />

time, a fact also demonstrated by the fossil <strong>of</strong> Eozoon. [It<br />

turned out that Eozoon was not a fossil; however, numerous<br />

unicellular fossils, and a few multicellular ones, have<br />

been found in Precambrian deposits since Darwin’s time.<br />

Darwin was right that life, albeit primarily single-celled,<br />

existed throughout that time.] The case must at present<br />

remain inexplicable; and it may be truly urged as a valid<br />

argument against the views here entertained. [The discovery<br />

<strong>of</strong> the slightly more ancient Ediacaran organisms has<br />

not helped to, even now, solve the problem <strong>of</strong> the relatively<br />

rapid origin <strong>of</strong> multicellular life.]

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