I recently skimmed through Adrian Lister’s book
Darwin’s Fossils: The Collection that
Shaped the Theory of Evolution (Smithsonian Books, 2018). I am not aware
that any previous book has gone through all of the specimens that Darwin
collected while traveling around the world on H.M.S. Beagle in 1832-1835. Nearly every science-literate person
has heard about the finches Darwin saw on the Galápagos
Islands, and how these observations eventually led him to think of natural
selection. But what about the fossils that he collected and sent back to
England?
Previous authors such as Niles Eldredge have
noted that Darwin’s fossils included the bones of numerous large extinct
mammals from South America, and that it was from this that Darwin concluded
what could be called the succession of forms. That is, in the past, the kinds
of fossilized mammals lived in the same locations that they are currently
found. Glyptodonts (giant armadillos) lived in South America; armadillos lived
there today. Giant llamas lived there in the past; llamas live there today.
Giant sloths lived there in the past; sloths live there today. Darwin
concluded, and scientists widely agreed, that when species become extinct, they
are succeeded by similar species in the same location. Today, we can hardly
force ourselves to avoid saying that modern species live in the same places
that their ancestors lived. But
“ancestors” means “evolutionary ancestors” and this is the very thing that
Darwin eventually concluded from his observations. But he had to gather the
evidence first.
Darwin collected a lot of other fossils as
well. He collected petrified wood. He found a petrified forest in Patagonia. He
noted that the bases of the trunks were inclined away from the Andes, and so
were the sedimentary layers in the rocks, which implied that the Andes had been
pushed up out of the Earth since those sedimentary layers had been formed. He
also found a few carbonized leaves such as those that can today be found near
Clarkia, Idaho, about which I wrote in 2014.
Darwin also found fossilized seashells far
above the high tide line, some of them even high in the Andes. The conclusion
that was obvious to him, as to us, is that land that was once below the sea has
risen. But Darwin was not satisfied with drawing the obvious conclusion. He
wanted to eliminate other possible explanations, and to do so before his
critics might attempt it in print. Suppose, for example, that the fossilized
seashells above high tide were not actually fossils, but were modern middens?
That is, what if fishermen hauled seashells up onto land (which they did in
fact do) and that what Darwin was seeing was just a pile of leftover shells?
Darwin observed midden heaps that were produced by fishermen, and found that
the shells were in piles, while the putative fossil shells were individually
spaced out, not in piles. In fact, when Darwin asked local fishermen if the
putative fossils could have put the shells there, they laughed at the idea.
Darwin suspected that the fossil seashells far
above high tide were not deposited in the places where they had lived but had
been dead at the time the waves deposited them on an ancient beach. He needed
evidence for this. He saw that some of the shells had dead barnacles on the
inner surface, which means the shells had been dead for a while before being
buried in sediments. If Darwin had not looked for this evidence, he might not
later have been able to distinguish fossil shells from an ancient seashore vs.
fossil shells from an ancient shell bed.
Darwin also thought that earthquakes caused the
successive stepwise uplift of land in South America. But he wanted evidence for
this. He got it. In 1835, he witnessed a severe earthquake in Concepción on the Pacific
coast of Chile. This one earthquake lifted the land surface at least eight
feet. Such earthquakes happen about every century; these earthquakes could
easily have produced the Andes. If Darwin had not seen one of these earthquakes
for himself, he would have had to depend on second-hand accounts. In fact, an
earthquake at least as strong as the 1835 quake, in almost exactly the same
place, occurred in 2010.
My point is that while he was on his voyage,
Darwin was not just collecting fossils but testing scientific hypotheses about
them while he was there rather than
wishing he had done so when he got back home. Until I looked through Lister’s
book, I had not known this.
Lister’s book also told the story of Darwin’s
discovery that coral atolls formed as volcanoes subsided in the ocean floor.
This would explain not only their roughly circular shape but also why the
atolls were not perfectly circular, like volcanoes, and why they were much
larger than volcanoes. The new corals built their reefs on top of old reefs,
each new reef being in a slightly different location from the old reef. (A
delightful story: When prominent geologist Charles Lyell read Darwin’s theory
of coral reefs, he danced around with wild contortions. I’d always thought
Lyell was kind of a stick-in-the-mud but I was wrong.) Darwin could not
actually prove that there were volcanoes at the bases of coral atolls, however.
This was first done in 1952 when geologists drilled a hole down into a coral
reef, piercing through thousands of feet of coral limestone, until they hit
volcanic rock.
I would not recommend buying this book, unless
you are a paleontologist, because it is heavy reading for the rest of us. But
it is well illustrated and taught me some new things that, even though I have
read dozens of books about Darwin, I’d never known. Get it from your library.
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