Until it can answer these questions the debate over
evolution will not end.
The concept of self-organization can answer these questions
since creation and speciation are the result of....internal
processes, not...natural selection, which serves merely
to fine-tune what has already been crated.
On the Origins of New Forms of Life
6.5: Gould and Eldredge
The battle between the gradualists and the saltationists, which is
further discussed below, continued until the 1940s, when a strong
intellectual shift occurred. Gradualism then became the ascendant
perspective among biologists. But in the early 1970s paleontologists
Stephen Jay Gould and Niles Eldredge raised the flag of saltation once
again.1 Their 1972 article caused an evolutionary uproar that has not
subsided to this day. As had many of their saltationist colleagues in
years gone by, they emphasized that a wide variety of fossil types 1)
arise suddenly and 2) are static thereafter. Gould (1980a: 182) later
expressed the problem succinctly:
The history of most fossil species includes two features particularly
inconsistent with gradualism:
(1) Stasis. Most species exhibit no directional change during their
tenure on earth. They appear in the fossil record looking much the same
as when they disappear; morphological change is usually limited and
directionless.
(2) Sudden appearance. In any local area, a species does not arise
gradually by the steady transformation of its ancestors; it appears all
at once and 'fully formed.'
Fossil Trilobites
Fossil Trilobites (Cambrian)
For years Eldredge had sifted through fossils trying to document
examples of slow, steady directional change. Instead he found that “once
species appear in the fossil record, they tend not to change very much
at all. Species remain imperturbably, implacably resistant to change as
a matter of course — often for millions of years.”2 For example, over an
eight-million-year period, the only detectable alteration in one of the
trilobites Eldredge had been studying was a slight change in the
structure of its compound eyes, the number of lens-rows dropped from
eighteen to seventeen.3 Eldredge (1995: 68) asserts paleontologists have
hesitated to emphasize the observed pattern of stasis in the fossil
record because it is inconsistent with neo-Darwinian theory:
For the most part it has been paleontological reluctance to cross swords
with Darwinian tradition that accounts for the failure to inject the
empirical reality of stasis into the evolutionary picture.
But exacting studies like Eldredge’s really serve only to emphasize the
existence of a phenomenon that most people could infer on the basis of
ordinary experience. Look at any guide to the identification of fossils.
Each of the listed types must be relatively stable — otherwise the
pictures and descriptions provided by the guide would be useless. For
each type, a guide specifies a particular time range during which that
form existed. Outside that range, the type in question is not known to
exist. Each type remains identifiable by its description and/or picture
over the entire period of its existence, from its first appearance to
extinction.
That is, each has a characteristic set of traits retained largely
unchanged. Each such form appears in the fossil record at a certain
lowermost stratum with its peculiar set of traits that remains stable up
to the time of the form's extinction. This is the typical pattern seen
in fossils.
Many types of organisms existing today have persisted unaltered for vast
ages. This fact has long been known. Even Huxley, Darwin's most ardent
supporter, was aware of it. In the Origin's year of publication (1859)
he gave a lecture entitled On the Persistent Types of Animal Life. In it
he noted that
certain well marked forms of living beings have existed through enormous
epochs, surviving not only the changes of physical conditions, but
persisting comparatively unaltered, while other forms of life have
appeared and disappeared. Such forms may be termed “persistent types” of
life; and examples of them are abundant enough in both the animal and
the vegetable worlds.
Among plants, for instance, ferns, club mosses, and Coniferæ, some of
them apparently generically identical with those now living, are met
with as far back as the Carboniferous epoch [which ended nearly 300
million years ago]; the cone of the oolitic [i.e., 135–152 million years
ago4] Arancaria is hardly distinguishable from that of existing species;
a species of Pinus has been discovered in the Purbecks [which date to
about 144 million years ago5], and a walnut (Juglans) in the cretaceous
rocks [the Cretaceous Period ended about 65 million years ago]. All
these are types of vegetable structure, abounding at the present day;
and surely it is a most remarkable fact to find them persisting with so
little change through such vast epochs. Every subkingdom of animals
yields instances of the same kind."6
The cassowary (Casuarius casuarius), the second-largest extant bird, is
known from 24-million-year-old deposits.7 Fossil insects, preserved in
amber for long eons of time are often indistinguishable from living
ones.8 In an article describing his experience examining ancient insects
in Harvard's Museum of Comparative Zoology, Paul Zahl (1978: 237) makes
the following comment on fifty-million-year-old amber-preserved
specimens in the museum's collection:
In each was a fly, ant, grasshopper, beetle, or spider, all perfectly
lifelike as though some magic wand had cast the spell of frozen sleep
upon them. [They looked] singularly like the fly, ant, grasshopper,
beetle, or spider in my own garden. Had evolution overlooked such genera
during the intervening fifty thousand millennia?
Many of the crocodilians (alligators, crocodiles, caimans, gharials)
have apparently persisted without change for some 200 million years
(2000 times the “lifetime” of Homo sapiens). Stokes (1982: 510) states
that the inarticulate brachiopod Lingula anatina “appeared first in the
Cambrian and has persisted without change through a life history of
innumerable generations spread over at least 500 million years.” Extant
animals such as the horseshoe crab once dodged the tread of dinosaurs.9
The Dawn Redwood (Metasequoia glyptostropoides) was once known only from
fossils. This tree, dating back to at least the Upper Cretaceous (about
70 million years ago), was discovered alive in China in 1941. Modern
specimens are nearly identical to the ancient fossils.10 Unchanged from
the time of the dinosaurs, it is now popular with landscapers here in
the United States.
Schindewolf (1993: 190) notes that in the ideally preserved remains of
220-million-year-old (Triassic) triopsid crustaceans from the Keuper
formation in Franconian region of southwest Germany,
Every detail of the structure of the body and its most delicate
appendages can be made out — the eyes, the antennae, the mandibles, with
their serrated masticatory surfaces, the maxillae, with their rows of
fine bristles, the filmy swimmerets (exopodites and endopodites) set
with bristles, the brood chamber filled with eggs, and much more. As a
consequence, a very detailed comparison with the Recent species Triops
cancriformis could be made, and the author stresses that even the most
minor characters were identical.
Romer (1966: 129) says Homoeosaurus, a contemporary of early dinosaurs
(Jurassic Period), “appears to have been almost identical in structure”
with a modern lizard, the tuatara (Sphenodon punctatus), now confined to
islands off the coast of New Zealand. The fossils of the modern
ocean-dwelling mollusc Neopilina galatheae (see image right) can be
found alongside extinct 350-million-year-old trilobites.11 The ostracod
Sylthere vonhachi is known from the Upper Ordovician (i.e., prior to 490
mya) and still exists today.12
How do these various forms of life persist so long without change? The
cases cited are glaring. But the typical organism in the fossil record
shows the very same pattern on a more modest time scale. The only
difference is that, in the usual case, a fossil form exists unchanged
for millions, rather than hundreds of millions, of years. Neo-Darwinian
theory would say this stability is imposed by functional restrictions on
form dictated by the environment. But are environmental constraints
really so demanding? Over such long time periods, it seems radical
changes in the environment must have occurred. Is it plausible that the
environment, especially an environment altered greatly with time, should
be able rigidly to control and stabilize the form of every part of an
organism?
As Bowler (1989: 337) notes, by the 1970s many paleontologists had
become dissatisfied with gradualistic explanations of evolution
because many of the classic examples of gradual change had not withstood
the test of modern techniques. If there were no genuine cases of
gradualism in the record, then the argument for treating all cases of
sudden change as the result of imperfect [fossil] evidence was
undermined. It might be better to reexamine the evidence in a new light,
putting aside the traditional Darwinian assumption of gradualism and
opting instead for a model of evolution that would allow for the sudden
appearance of new forms as indicated by the fossil record.
The abruptness of the paleontological data is still clearly at odds with
gradualistic explanations of evolution, just as it was in Cuvier's day.
As Winsor (1979: 112) notes
Even species that resemble one another in all but the most trivial
details are seen to maintain their particular distinctness generation
after generation, often for millions of years. It takes a very
determined and sympathetic searcher to find any transformations in
nature comparable to the appearance of domestic breeds, and such forms
are not regarded as species.
If anyone, could be described as a “very determined and sympathetic
searcher,” it was Ernst Mayr. He, too, admits saltation is the typical
pattern: Although he maintains that a “certain proportion” of fossil
forms undergo gradual change into subsequent forms,13 “far more
frequently,” he says, “the extant species are supplemented by — or the
extinct species are replaced by — new species that turn up in the fossil
record. In the classical literature this sudden introduction of new
species was usually ascribed to instantaneous saltations.”14 As Gould
(1980a: 189) puts it, “All paleontologists know that the fossil record
contains precious little in the way of intermediate forms.”
http://www.macroevolution.net/stephen-jay-gould.html