You
could not possibly understand my bizarre desire to seek out a
fish halfway round the world, without first knowing something
about the protagonists in this fish saga. Let me begin with the
fish.
Compress
the four and a half billion year history of our planet into a
single year--as Carl Sagan was so fond of doing. You will find
that humankind and human civilization comprise only the last few
minutes and seconds of December 31st. For the first seven months
of the year, from January through July, the planet percolated
with the ingredients of life. By August, single celled bacteria
and algae were the first standard bearers of evolution. Two months
later, on the first of November, sea worms and jellyfish appeared,
soon accompanied by sponges, mollusks and shellfish.
Not
until the 18th of November, did the first jawless fishes, resembling
today's lamprey eels, squirm in tepid waters. By the 22nd, some
had developed true skeletal backbones and jaws. A few of these,
including the coelacanths, could waddle along the bottom on fleshy
lobbed fins. That was four hundred and ten million years ago,
at the beginning of an epoch in earth's history scientists call
the Devonian- The Age of Fishes.
Some
scientists believe that at that time, when the earth's land surface
consisted of two super continents--Pangea in the northern hemisphere
and Gondwana in the southern--all you would ever be was crammed
into the genes of a foot-long fresh water lobe-finned inhabitant
of lakes and rivers called Eusthenopteron. This leg-finned, air-breathing
fish is often credited with making the transition to land, becoming
extinct as a species in the process, as it gave rise to the first
amphibians 360 million years ago. One scientist has suggested
that Eusthenopteron became a land-walker not because he had a
yen for terra firma, but rather because he needed to crawl from
one river puddle to another during dry seasons. I think of this
prosaic account of our terrestrial origins whenever my motorcycle
won't start. At bottom, everything comes down to getting about.

The
early coelacanth was similar in appearance and size to Eusthenopteron,
but with enough differences to belong to a separate family. While
Eusthenopteron apparently did his transforming, Natural Selection
never really worked on the coelacanth again. Its incredible survival
down to the present furnishes a deja vu of the genetic past of
all terrestrial tetrapods, ourselves included. It is the retarded
relative of whom one might say "There but for the grace of
God go I."
In hindsight, coelacanths seem like primitive antiques. But not so when they first appeared as small freshwater, inshore predators. They were very racy models, at the apex of evolutionary design. The backbone formed a fluid-filled, cartilaginous tube, which provided a firm yet flexible support for muscles. The sucking maws of jawless predecessors had transformed, through a modification of one of the gill arches, into hinged, rigid structures with teeth on the bottom ridge and upper palate--true jaws. The brain, though still tiny, was encased in a hardened skull, which hinged in the middle to increase the gape of the mouth while feeding. The eyes were well developed with reflecting cells called tapita to enhance night vision. The chambered heart pumped blood in prototype to our own. Two indentations in the snout led into a peculiar cavity, a rostral organ-- perhaps acting as an electro-receptor. Along the sides, a pressure sensitive lateral line was well developed to sense the proximity of other fishes and objects- useful in maneuvering and locating prey. Two back or dorsal fins and one protruding beneath the nape of the tail were complimented by paired lobed pectoral and pelvic fins. These contained in their trunks the bones which in the coelacanth's cousin, Eusthenopteron, later evolved into arms and legs. The scales were thick, and lined with serrated rows of hardened toothpick-point denticles. Perhaps most distinctive of all was the trilobated tail with its extra trunk and fin protruding from the middle. It was this feature that made fossil coelacanths so easily recognizable and helped clinch the case for the first living specimen to be identified.
Early
coelacanths were common in freshwater lakes and rivers throughout
much of the world and their fossils have been found from Greenland
to Madagascar. Two hundred and fifty million years ago, when amphibians
were first slithering about the river banks, coelacanths spawned
marine forms that grew larger than their fresh water cousins.
This
entire period was once called "The Age of Fishes," as
they are so predominant in the fossil record of the era. Marine
coelacanths shared these Paleozoic waters with other predators,
including early sharks--quite different in appearance from today's
descendants. Armored fishes, called Placoderms, whose heads and
upper torsos were sheathed in horny plates, moved by undulating
both their bodies and their stretched out, lopsided wisps of tails.
Most placoderms were small, but some deep ocean varieties stretched
over eight feet.
Ratfishes
nibbled the upper layers of the seabed's dead and dying. Squids
and cuttlefishes jetted tail first through the water. Sixteen
foot sea scorpions and thirty foot nautiloids, ancestors of today's
pearly nautilus, snatched at smaller fishes, who fed in turn on
crabs, clams, urchins, chunks of corals, and ubiquitous bivalved
brachiopods. Segmented trilobites roiled the bottom, feeding on
particles of decay. Coral polyps and sponges built reefs along
craggy rock outcrops. Tube worms unfurled fans to filter plankton
drifting in the current.
Most
of these animals are long gone, casualties of the mass waves of
extinction that have swept the planet over the eons. Others have
left descendants in almost unrecognizably different forms. From
Eusthenopteron came the amphibians, and from them the reptiles,
among whom dinosaurs came to dominate the terrestrial landscape
for 150 million years.
By
the time, two hundred and fifteen million years ago, when dinosaurs
were taking over on land, there were as many as thirty species
of coelacanths. Their fossils are strewn across North America,
Europe, Greenland, and particularly Madagascar. One hundred million
years later there were fewer than ten species. By then the two
mega continents, Pangea and Gondwana, were splitting up, sending
the new continental land masses on their tectonic drift across
the oceans. The dinosaurs came to an end 65 million years ago,
in one of the greatest mass extinctions of all time. During this
late Cretaceous extinction, over ninety percent of the earth's
fauna, including the dinosaurs, disappeared forever. In the terms
of our cosmic calendar analogy, this was at the end of November.
All that would be of human evolution and cultural history was
still a month away.
During
the 18th and 19th centuries A.D., a rage of plant and animal classifying
consumed naturalists. Animals, living and extinct, were sorted
out into kingdom, phylum, class, order, family, genus, and species.
Subheadings were added whenever there was a doubt. Coelacanths
were just one of dozens of kinds of fossil fishes identified,
described and classified. They had no privileged status. The first
fossil coelacanth to be described and named was a specimen found
near Newcastle in England. The work was done by the famous zoologist
Louis Agassiz, in 1836. He combined Greek words for "space"
and "spine," coming up with "coelacanthus,"
to name the fish after its hollow dorsal fin spines. (Ironically,
given the present evolutionary significance of this fish, Agassiz
would become a leading opponent of Darwin's Theory of Evolution!)
The "youngest" coelacanth fossil species to emerge,
a 2 foot fish called Macropona, is one hundred million years old.
In fact, no fossil coelacanths have been found in rocks younger
than the sixty-five million year old Cretaceous sediments which
sandwiched the last of the dinosaurs bones. The coelacanths seemed
just as extinct.
But were they?