s 4 s
Bursts of Evolution
The Cambrian
Explosion
Earth
was born 4.6 billion years ago. Life on
earth was born about a billion years later – sometime between 3.85 and 3.5
billion years ago. For the next three
billion years, life on earth was comprised of simple microscopic critters. Complex life emerged toward the end of the
story – after 88.5% of earth's history had already passed. But once it got here, complex life wasted no
time diversifying into an impressive array of different forms. During a comparatively short period of time
called the Cambrian Explosion, which occurred about 530 million years ago,
complex life underwent a dramatic increase in evolutionary diversification that
has never been equaled before or since.
As Wicander and Monroe put it,
The basic body plans for all
animals were apparently established by the end of the Cambrian Explosion, and
only minor modifications have occurred since then.[1]
Carroll
states that all the major body plans (phyla) came into existence within 5
million years, from 530 to 525 million years ago, and that,
There is
no evidence for the gradual evolution of the major features by which the
individual phyla or classes are characterized.[2]
Gould expounds,
Even our strongest opponents
admit that in less than twenty million years, from the inception of the Cambrian
Explosion to the deposition of the Burgess Shale, marine invertebrate life
reached a fully modern range – and that more than 500 million years of
subsequent evolution has not at all enlarged the scope of basic anatomical
variety.[3]
Schulze-Makuch and Irwin add,
Most of the extant higher order
taxa of plants and animals were fixed at that (Cambrian) time and have remained
essentially unchanged to the present.[4]
The
Cambrian Explosion records the first truly diverse ecological system in the
history of the planet. Among the life
forms present were the first mollusks, including gastropods and bivalves; and
also the brachiopods with their shells; the arthropods with their segmented
bodies and hard exoskeletons, including the trilobites; the trilobites'
cousins, the chelicerates, which had the basic framework of their descendents
the scorpions and spiders, complete with antennae, long stinger tails, and legs near their mouth; and their cousins, the
crustaceans, some of which looked similar to crabs and lobsters even back then;
the echinoderms, which were the ancestors of the starfish; the cnidarians,
which were primitive precursors to jelly fish and corals; sponges; comb
jellies; sea anemones; sea cucumbers; velvet worms; carnivorous worms; and segmented
worms. All of these extremely diverse
body plans were present during the Cambrian Explosion.
The
Cambrian Explosion also saw the first species of the phylum chordata, which
gave rise to that most illustrious critter known as Homo sapiens. One such
distant relative of ours, Haikouella, had
a rather large brain, which has caused some to suppose that intelligent life is
common in the universe and may arise more quickly in the natural course of
evolution than previously thought.[5] These animals had most of the guts modern
chordates now have, including a heart, arteries, gills, a spinal chord, large
muscles, and teeth.[6]
The
ancestors to these chordates were the annelid worms. Yet annelid worms first appear in the
Cambrian too, thus compounding the amount of evolution which must have occurred
in the Cambrian. Moreover, the genealogy
breaks off at the annelids, with no ancestor in the fossil record known before
it. Dzik writes,
There is no evidence for the
presence of annelids in the Precambrian and recent findings of extraordinarily
preserved segmented Ediacaran (Precambrian) metazoans show that their anatomy
is different from annelids.[7]
This means there were two quick
jumps; one from some unknown ancestor to annelids, and another from annelids to
chordates – back to back quantum leaps in a short period of time.
There
were even more body plans which quickly went extinct. Often called evolutionary
"experiments," these strange creatures don't even have any known
relatives – no parent species, no descendant species, and nothing similar in
the fossil record. At least 20 such
"dead end" phyla emerged in the Cambrian only to quickly suffer
extinction.[8]
The
Cambrian Explosion was the most remarkable event in the history of life,
because so many completely different creatures evolved so quickly, without
evidence for gradual change over long periods of time.
The
Cambrian Explosion flies in the face of Natura
non facit saltum. The sudden
emergence of so many entirely different body plans defies the expectation that
evolution should happen gradually. Some
believe that the Cambrian was too short a time to account for the amount of
evolution in the fossil record, and so they look for a way to rationalize how
complex life could have been evolving before the Cambrian. However, the fossil evidence for ancestors of
Cambrian forms is weak, so they imagine that small soft bodied forms were
evolving before the Cambrian, before hard exoskeletons and shells were
prevalent. Because the fossil record
preserves hard parts better than soft body tissue, they say that the fossil
record before the Cambrian is simply incomplete. However, even though soft body tissue is
rare, it is occasionally preserved, and the fossil record for soft body tissue
indicates that there was an increase in the diversity of soft body tissue as
well as in hard body tissue during the Cambrian. Many more burrows of soft bodied animals are
found in the Cambrian than in previous time frames.[9]
The Molecular Clock and the Cambrian Explosion
The
molecular clock is a way to estimate how many millions of years ago two or more
lineages diverged. It does this by
measuring differences between two or more species' DNA. It is often calibrated to data points in the
fossil record, and assumes that mutation rates are predictable and/or
relatively constant. If mutation rates
were higher during certain times in earth's history, then the molecular clock
will record a greater degree of difference between the DNA of the two lineages,
and will therefore overstate the age of their most recent common ancestor. This is exactly what happens.
Across
a very large number of lineages, the molecular clock tells us that lineages
diverged much earlier than the fossil record allows. That is, the estimated time of divergence as
predicted by DNA comparative differences is significantly earlier than the age
of the first fossils that confirm the divergence.
According
to the fossils, the Cambrian Explosion was completed, start to finish, in about
10 million years or less. But the
molecular data indicates that the divergences between Cambrian lineages must
have taken place at least 100 million years beforehand, if not more; otherwise,
there would not have been enough time for genetic mutation to accomplish such a
great amount of diversity.[10] There are only two possibilities to explain
this: Either the mutation rate increased
about ten-fold during the Cambrian Explosion, or there was no Cambrian
Explosion. Levinton et al indicated this
as follows:
The divergence in animal phyla
was neither Cambrian nor explosive… The only obvious way to escape these
conclusions is to argue that the rate of molecular evolution was greater during
the Cambrian Explosion than in subsequent times.[11]
What could cause such a sudden
increase in molecular evolution?
Levinton
et al suggested that the ancestors of the Cambrian biota were so small that we
don't see them in the fossil record. Yet
they also acknowledged that this is problematic in light of the fact that the
most recent common ancestor of protostomes and deuterostomes must have had a
circulatory system, which is the prerequisite for large size.[12] Thus, the lack of large-sized Cambrian-like
animals before the Cambrian confirms the reality of the Cambrian Explosion.
Apparent
increases in the rate of mutation are not confined only to the Cambrian
Explosion. The phenomenon remains a
fixture across many ages and many lineages.
Molecular evidence suggests that modern birds first diversified 90 million
years ago; however, the fossil evidence cannot support their diversification
until about 30 million years later.
Moreover, even genetic studies of the molecular data itself indicate
that the divergences were not staggered or gradual, but rather were explosive,
as Poe and Chubb concluded, "Neoaves (i.e. – modern birds) differentiated
so rapidly that the radiation might be considered essentially
simultaneous."[13]
Likewise,
molecular data places the most recent common ancestor of rodents and primates at
110 million years ago, but neither order emerged with their distinct features
until 55 million years ago, just half the time predicted.[14]
In
a third example, molecular evidence suggests snakes arose 125 million years
ago,[15]
but the fossil record does not produce indisputable snakes until 20 million
years later.[16]
The
same kind of phenomena has been observed when the molecular clock for flowering
plants in calculated. Numerous specimens
of flowering plants appear as a well-represented lineage in the fossil record
starting 132 million years ago, and become diversified by 125 million years
ago. However, molecular evidence based
on strict constancy in the mutation rate indicates that they should have
appeared much earlier – perhaps back as much as 450 million years ago. From the perspective of the fossil record,
this is absurd, because plants did not even exist 450 million years ago. Yet that is what the DNA evidence tells us. Even when the fossil record is used to
calibrate molecular clocks, the results still indicate a date for the first
flowering plants which is much older than the fossil record can
substantiate. More than a few molecular
studies have been done, all but one yielding a range of dates for the first
flowering plants which predate their earliest fossils. Often, the date suggested by molecular data
predates the earliest fossils by dozens and in some cases even hundreds of
millions of years.[17] [18]
Such
large gaps between the molecular data and the fossil evidence suggest that
accelerations in the mutation rate occur near the base of lineages.
What
could cause an acceleration in the mutation rate of plants? There was no great ecological calamity 132
million years ago that could explain a change in the mutation rate. The climate during this time was stable and
hospitably warm. We lack a natural
explanation.
Brochu
et al summarized the various deficiencies in the molecular clock, saying,
The more we look at fossils,
molecules, or algorithms, the stronger the disparity seems to grow… (Either) we
assume… imperfections in the fossil record… Or, we assume that the fossil
record closely approximates the origination times of these orders and that the molecular clocks are being misled by
mysterious simultaneous speedups of evolutionary rate (emphasis added).[19]
The only rational basis on which
to deny that these magical mystery "speedups of evolutionary rate"
have happened is to deny the accuracy of the fossil record.
Hox
Genes and the Cambrian Explosion
Shortly
before the Cambrian, the first arguably genuine members of the phylum cnidaria
appeared. These were the likely
ancestors of corals and jellyfish.
Genetically, the cnidarians have only two hox genes, and at that time,
the cnidarians were the most complex life form on the planet. By the end of the Cambrian, the number of hox
genes in the most complex life forms had apparently increased somewhere in the
vicinity of about twenty-fold.[20] Hox genes code for variable proteins, and are
responsible for the diversity we observe across the various life forms. The magnitude of this rapid and exponential
multiplication of hox genes during the Cambrian has no parallel in evolutionary
history.
The
genetic history of the Cambrian can be reconstructed as follows: A lineage diverged from the cnidarians,
called the bilaterians, which became the common ancestor of all clams, worms,
insects, reptiles, humans, and virtually every other animal that comes to mind
except sponges. This primordial common
ancestor of most every animal had 7 hox genes.[21] Thereafter, the bilaterians diverged into
protostomes and deuterostomes – the former including all insects, crustaceans,
brachiopods, worms, mollusks, etc; and the latter including starfish, humans,
birds, reptiles, fish, etc. These
quickly diversified, adding as many as 7 more hox genes, depending on the
lineage.[22] The common ancestor of the vertebrates then
underwent a four-fold duplication, forming four hox complexes, each complex
having multiple genes. This must have
happened extremely early in vertebrate history, for even the jawless lampreys
participated in this event – indicating it happened even before jaws
evolved. Today, all tetrapods, including
all amphibians, reptiles, birds, and mammals, have 39 hox genes spread across
these four hox complexes[23] –
which indicates that this must have occurred prior to their divergence about
360 million years ago. Since then, the
only large scale duplication of hox complexes to occur has been that of the
teleost fish.[24]
The
implications are stunning. Prior to the
Cambrian, we have no clear fossil record confirming the divergence of the
bilaterians from the cnidarians. This
means that the greatest number of hox genes any life form had achieved was
still just two, since the cnidarians have just two. Moreover, the emergence of the vertebrates
occurred in the Cambrian, and the vertebrates had an exponentially larger
number of hox genes. Hence, it appears
likely that the number of hox genes in the most advanced life forms jumped from
2 to approximately 39 or so during the Cambrian or shortly thereafter – a
remarkable increase in the number of hox genes for such a short period of
time. What is more, in over 360 million
years since the first fish climbed out on land and grew legs, the number of hox
genes in the tetrapods has remained constant at 39 – for all frogs, lizards,
birds, and humans. To be sure, within
each gene, a tremendous amount of evolution has occurred since then. Yet the number of hox genes has not changed
for tetrapods since the mid Paleozoic.
Why
did the number of hox genes increase so dramatically in the early
Paleozoic? And why, with the exception
of the teleost fish, have they remained stable since then? What prompted such a sudden blossom of life
in the Cambrian? Why did so much
evolutionary change, diversification, and progress take place in such a short
time? The Cambrian Explosion, both in
terms of fossil evidence and in terms of genetic evidence, remains the most
confounding enigma in all evolutionary science.
The Carnian Explosion
If
the Cambrian Explosion was the greatest blossoming of new life forms the world
has ever seen, then the Triassic would be the second greatest such
explosion. Ward states that the
"Triassic Explosion," saw, "the largest number of new body plans
seen since the Cambrian."[25]
The height of the Triassic explosion was the Carnian age. Lasting from 228 to
216.5 million years ago, the Carnian saw more new body plans emerge among the
vertebrates than in any other age. Not
only did the dinosaurs first emerge during this time, so did many other new
forms. The first lizards were found in
the Tiki Formation of the Carnian.[26] The first pterosaurs, that is, the flying
reptiles who dominated the skies during the time of the dinosaurs, also most
likely evolved around the Carnian-Norian boundary. We might also possibly add turtles to this
list, as the first turtle might be as old as 220 million years, which would
make it Carnian in age.[27]
The
earliest true mammals also made their debut in the Carnian. The mammal Tikitherium accomplished the evolution of the mammalian molar tooth
during this time. According to Datta, Tikitherium's molar tooth "stands
apart as a distinctly different entity" from those of seemingly related
species, and is "the earliest mammalian representative possessing this
advanced dental specialization."[28] Other more primitive mammal teeth from the
Carnian fill a morphological gap or "missing link" between the
cynodont reptiles and the true mammals,[29]
indicating that the Carnian is the dividing line between true mammals and the
mammal-like reptiles from which they evolved.
The split between mammal and reptile had been a long time in
coming. From the early synapsids and
pelycosaurs to the later therapsids and cynodonts, the evolution of reptiles
into mammals is one of the more gradually evolving lineages the fossil record
can provide. The dinosaurs also have a
traceable lineage to more primitive reptiles called archosaurs. Hence, we know they evolved. They did not spontaneously emerge; rather,
the Carnian saw an acceleration in the amount of evolution across many types of
vertebrates.
Both
the mammals and the dinosaurs each accomplished something unique in the Carnian
– something that would propel them to become the dominant forms of life on the
planet from then on. In the mammals'
case, it was the innovation of the molar tooth, which gives mammals an
advantage in chewing grass and herbs. In
dinosaurs, it was the innovation of erect posture made possible by direct
support of the body by the legs, which permitted them to run faster and grow
larger than any animal before them.
There
was nothing environmentally spectacular about the Carnian period that could
have catalyzed this burst of evolution.
There was no radical change in climate nor was there a mass extinction
event. There was no apparent reason for
why animals may have been forced to adapt and thereby become such new and
different forms. The Carnian landscape
was determined by the supercontinent Pangaea, which was all continents joined
together in one giant land mass. Pangaea
in the Carnian was the same hot and dry desert of a supercontinent it had been
for tens of millions of years before.
There was no great geographic or climate change in the Carnian that
could have caused such a large number of new forms to evolve then more than at
other times.
The Eocene Explosion
The
dinosaurs became extinct 65.5 million years ago, clearing the way for the age
of mammals. But for the first 10 or 12
million years after the dinosaurs were gone, mammals did precious little with
the opportunity. Most of them remained
small and non-diverse. Moreover, the
same marsupials and multituberculates which had lived under the feet of the
dinosaurs before the extinction came back to rule the planet after the
dinosaurs were gone. Mammals did not
change that much after the dinosaurs were gone.
Wolves and wildcats were still a long time in the future. Instead, the biggest carnivores of those
times were silly looking ostrich-type flightless birds that looked more like
Sesame Street's Big Bird than any real carnivore. In essence, the birds were awkwardly evolving
back toward being dinosaurs to fill the niche left empty by the dinosaurs. But for the 10 million years or so during
which flightless birds were evolving back toward dinosaurs, they never got much
beyond the appearance of a gorilla-sized turkey.
One
would think that if ever in the history of the planet there was an opportunity
for a lineage to undergo a massive degree of adaption and speciation, it would
have been the opportunity afforded the mammals and birds immediately after the
dinosaurs went extinct, because the competition was eliminated. But such was not the case.
The
major breakthrough for mammals did not come with the death of the
dinosaurs. Rather, it came about 10
million years later. About 55 million
years ago, "there was an explosion in mammalian variety." The distinct lineages of monkey-like
primates, elephants, rodents, full-fledged bats, whales, horses, and the
primitive ancestors of cattle and pigs all made their debut at that time.[30]
Why
did all these important lineages suddenly evolve their unique traits 55 million
years ago? According to molecular data,
which estimates divergence times based on calibration to the amount of
divergence in the fossil record, they should have diverged much earlier, toward
the middle of the time of the dinosaurs.
Yet the fossil record marks their sudden origins about 10 million years
after the dinosaurs became extinct. This
discrepancy between molecular data and the fossil record could be explained if
there was a 100-fold increase in DNA mutations that lasted over a period of
500,000 years.[31] What could cause such a drastic increase in
mutations? Whatever the cause, one fact
is undeniable – the diversification of the mammals in the early Eocene is
separated in time from the extinction of the dinosaurs by a substantial space
of at least 10 million years, and therefore the greatest diversification of the
mammals was not a direct result of the dinosaurs becoming extinct. Rather, there was another unseen force at
play which seems to have dramatically increased mutation rates for a relatively
short period of time, about 55 million years ago.
The
heart of the question is, what
accelerates the mutation rate?
[1] Wicander, Reed; Monroe, James S. Historical Geology: Evolution of Earth and Life Through Time, 4th Ed. 2004, Brooks/Cole – Thomson Learning, Belmont, CA, p 218
[2] Carroll, Robert L. Patterns and Processes of Vertebrate Evolution. 1997, Cambridge University Press, Cambridge, UK, p 3, 344
[3] Gould, in Morris, Simon Conway; Gould, Stephen Jay. Showdown on the Burgess Shale. 1998, Natural History Magazine, 107 (10), p 48-55.
[4] Schulze-Makuch, Dirk; Irwin, Louis N. Life in the Universe: Expectations and Constraints. 2004, Springer-Verlag, Berlin & Heidelberg, Germany, p 36
[5] Heeren, Fredric J. Was the First Craniate on the Road to Cognition? A Modern Craniate's Perspective. 2003, Evolution and Cognition, Vol 9, No 2, p 141
[6] Chen, Jun-Yuan; Huang, Di-Ying; Li, Chia-Wei. An Early Cambrian Craniate-like Chordate. 1999, Nature 402, p 518
[7] Dzik, Jerzy. Anatomy and Relationships of the Early Cambrian Worm Myoscolex. 2004, The Norwegian Academy of Science and Letters, Zoologica Scripta 33, p 57-69
[8] Gould, Stephen Jay; Andrews, Peter; Barber, John; Benton, Michael; Collins, Marianne; Janis, Christine; Kish, Ely; Morishima, Akio; Sepkoski, J John Jr; Stringer, Christopher; Tibbles, Jean-Paul; Cox, Steve. The Book of Life: An Illustrated History of the Evolution of Life on Earth. 2001, W W Norton & Co, New York, NY, p 54
[9] Gould, Stephen Jay; Andrews, Peter; Barber, John; Benton, Michael; Collins, Marianne; Janis, Christine; Kish, Ely; Morishima, Akio; Sepkoski, J John Jr; Stringer, Christopher; Tibbles, Jean-Paul; Cox, Steve. The Book of Life: An Illustrated History of the Evolution of Life on Earth. 2001, W W Norton & Co, New York, NY, p 52-53
[10] Levinton, Jeffrey; Dubb, Lindsey; Wray, Gregory A. Simulations of Evolutionary Radiations and Their Application to Understanding the Probability of a Cambrian Explosion. 2004, Journal of Paleontology 78(1), p 31-38
[11] Levinton; et al. ibid. p 31, 34
[12] Levinton; et al. ibid. p 37
[13] Poe, Steven; Chubb, Alison L. Birds in a Bush: Five Genes Indicate Explosive Evolution of Avian Orders. 2004, Evolution 58(2), p 404-415
[14] Van Tuinen, Marcel; Hedges, S Blair. The Effect of External and Internal Fossil Calibrations on the Avian Evolutionary Timescale. 2004, Journal of Paleontology 78(1), p 45-50
[15] Wiens, John J; Brandley; Matthew C, Reeder, Tod W. Why Does a Trait Evolve Multiple Times within a Clade? Repeated Evolution of Snakelike Body Form in Squamate Reptiles. 2006, Evolution 60(1), p 135-136
[16] Rage, J C; Escuillie, F. The Cenomanian: Stage of Hindlimbed Snakes. 2003, Camets de Geologie, Maintenon, Article 2003/01 (CG2003_A01_JCR-FE), p 1-11
[17] Bell, Charles D; Soltis, Douglas E; Soltis, Pamela S. The Age of the Angiosperms: A Molecular Timescale without a Clock. 2005, Evolution 59(6), p 1245-1258
[18] Magallon, Susana A; Sanderson, Michael J. Angiosperm Divergence Times: The Effect of Genes, Codon Positions, and Time Constraints. 2005, Evolution 59(8), p 1653-1670
[19] Brochu, Christopher A; Sumrall, Colin D; Theodor, Jessica M. When Clocks (and Communities) Collide: Estimating Divergence Time from Molecules and the Fossil Record. 2004, Journal of Paleontology 78(1), p 1, 4
[20] Carroll, Sean B; Grenier, Jennifer K; Weatherbee, Scott D. From DNA to Diversity: Molecular Genetics and the Evolution of Animal Design, 2nd Ed. 2005, Blackwell Publishing, Malden, MA, p 114-120
[21] Carroll, Sean B et al. ibid, p 116
[22] Carroll, Sean B et al. ibid, p 116
[23] Carroll, Sean B et al. ibid, p 117, 120
[24] Carroll, Sean B et al. ibid, p 117, 120
[25] Ward, Peter D. Out of Thin Air: Dinosaurs, Birds, and Earth's Ancient Atmosphere. 2006, Joseph Henry Press, Washington, DC, p 159
[26] Datta, P M; Ray, Sanghamitra. Earliest Lizard from the Late Triassic (Carnian) of India. 2006, Journal of Vertebrate Paleontology 26(4), p 795-800
[27] Gaffney, Eugene S. The Comparative Osteology of the Triassic Turtle Proganochelys. 1990, Bulletin of the American Museum of Natural History 194.
[28] Datta, P M. Earliest Mammal with Transversely Expanded Upper Molar from the Late Triassic (Carnian) Tiki Formation, South Rewa Gondwana Basin, India. 2005, Journal of Vertebrate Paleontology 25(1), p 200-207
[29] Lucas, Spencer G; Heckert, Andrew B; Harris, Jerald D; Seegis, Dieter; Wild, Rupert. Mammal-like Tooth from the Upper Triassic of Germany. 2001, Journal of Vertebrate Paleontology 21(2), p 397-399
[30] Haines, Tim; Chambers, Paul. The Complete Guide to Prehistoric Life. 2006, Firefly Books, Buffalo, NY, p 146
[31] Hebert, Paul D N; Remigio, Elpidio A; Colbourne, John K; Taylor, Derek J; Wilson, Christopher C. Accelerated Molecular Evolution in Halophilic Crustaceans. 2002, Evolution 56(5), p 920