The fossil record of ‘early’ tetrapods: evidence of a major evolutionary
transition?
by Paul Garner
Summary
According to evolutionary theory, the origin of tetrapods from a fish-like ancestor
during the Devonian Period was one of the major events in the history of life on
earth. The ‘drying pond’ hypothesis was proposed to explain the selection
pressures behind the transition. According to this hypothesis, the tetrapods evolved
as fishes became progressively better adapted to terrestrial conditions during prolonged
episodes of drought. Recently, however, the assumption that feet and legs evolved
to facilitate life on the land has been called into question. The ‘earliest’
known tetrapods with feet and legs are now thought to have been aquatic animals;
evolutionists therefore argue that feet and legs evolved in a shallow water environment
and were only later co-opted for use on the land. This paper reviews the radical
changes in thinking about the fish-tetrapod transition that have taken place in
the evolutionary community. It also considers the chimeromorphic nature of Devonian
tetrapods and fishes, and offers some critical comments on the evolutionary interpretation
of their fossil record.
Evolutionists believe that tetrapods—i.e. vertebrates with four limbs—were
the first animals to move on to the land, having evolved from a fish ancestor during
the Devonian period (conventionally 408 to 360 million years ago). The fossil record
of Devonian tetrapods is often presented as compelling evidence of this major evolutionary
transition.1 Science writer
Carl Zimmer has written a popular book, At the Water’s Edge,2 which purports to show how life
came ashore (i.e. how fish evolved into tetrapods) and then went back to the sea
(i.e. how land mammals gave rise to the whales). A more technical presentation was
written recently by Jenny Clack, Reader in Vertebrate Palaeontology and Senior Assistant
Curator of the University Museum of Zoology, Cambridge. Entitled Gaining Ground:
The Origin and Evolution of Tetrapods,3
it begins with these words:
‘About 370 million years ago, something strange and significant happened on
Earth. That time, part of an interval of Earth’s history called the Devonian
Period by scientists such as geologists and paleontologists, is known popularly
as the Age of Fishes. After about 200 million years of earlier evolution, the vertebrates—animals
with backbones—had produced an explosion of fishlike animals that lived in
the lakes, rivers, lagoons, and estuaries of the time. The strange thing that happened
during the later parts of the Devonian period is that some of these fishlike animals
evolved limbs with digits—fingers and toes. Over the ensuing 350 million years
or so, these so-called tetrapods gradually evolved from their aquatic ancestry into
walking terrestrial vertebrates, and these have dominated the land since their own
explosive radiation allowed them to colonize and exploit the land and its opportunities.
The tetrapods, with their limbs, fingers, and toes, include humans, so this distant
Devonian event is profoundly significant for humans as well as for the planet.’4
Indeed, according to the cladistic framework that now dominates evolutionary systematics,
humans are not simply descended from fish—they are fish!
Clack states:
‘Although humans do not usually think of themselves as fishes, they nonetheless
share several fundamental characters that unite them inextricably with their relatives
among the fishes … Tetrapods did not evolve from sarcopterygians
[lobe-finned fishes]; they are sarcopterygians, just as one would not say
that humans evolved from mammals; they are mammals.’5
In this paper I will critically examine the fossil record of ‘early’
tetrapods and discuss the way in which older evolutionary views of their origin
have been overturned in the last two decades. I will also consider the mosaic distribution
of characters that we observe in Devonian tetrapods and fishes, the problems that
it poses for evolutionary theory, and how it might be understood in a creationist
framework.
The ‘drying pond’ hypothesis
Many evolutionary scenarios have been proposed to explain the origin of tetrapods.
Most of them were developed to answer the question, ‘Why did fish leave the
water and come onto the land?’ The early theories usually focused on the environmental
setting and selection pressures behind the transition. Tetrapods were thought to
have evolved during the Devonian, a period associated in many parts of the world
with sediments stained red by iron oxide. Classic red beds, such as the Siluro-Devonian
rocks of Europe (the Old Red Sandstone) and their North American equivalents (the
Catskill and Escuminac formations), have often been interpreted as the product of
hot, semi-desert environments with seasonal wetness. This led many to speculate
that an increasingly arid climate was a major influence on the evolution of air-breathing
vertebrates. A classic paper by Barrell6
set the scene for much future discussion. He argued that the first tetrapods arose
‘under the compulsion of seasonal dryness’.7 Under such conditions, it was suggested, the air-bladder
of certain fishes became progressively better adapted as an organ of respiration
and the gills atrophied. The development of a new system of breathing allowed fishes
to survive the drought conditions by moving between bodies of water. Those fishes
with more limb-like appendages were better able to make the journey and this ultimately
led to the evolution of limbs with digits. This became known as ‘the drying
pond hypothesis’ and was popularized by the great vertebrate palaeontologist
Alfred Sherwood Romer.8

Figure 1. Reconstruction of Ichthyostega, showing skull, vertebral
column, and limbs, and its hind limb based on a specimen collected in 1987. Note
the seven digits on the hind limb (from Clack).15
|
‘Early’ tetrapods from East Greenland
When Romer was popularizing the ‘drying pond’ idea, the earliest known
tetrapods were Ichthyostega and Acanthostega from the Upper Devonian
of East Greenland. Ichthyostega was first described by Säve-Söderbergh9 and then by Jarvik in
a series of papers and a monograph.10–12 Although
the anatomy of Ichthyostega is known in considerable detail, its body proportions
are uncertain because the fossil material comes from more than one individual. Ichthyostega
is about one metre long with a broad, flat head, short, barrel-shaped body, stocky
legs, large pelvic and pectoral girdles, and a rib cage with broad, overlapping
ribs (Figure 1). It is very evidently a tetrapod, with limbs rather than fins. Nevertheless,
Ichthyostega has some fish-like characteristics, including a lateral line
system and a tail with bony fin rays. Early reconstructions portrayed Ichthyostega
as a semi-aquatic creature but most later ones depicted it as a predominantly terrestrial
animal (e.g. Jarvik13).
As recently as 1988, a major vertebrate palaeontology text described Ichthyostega
as a fairly typical land animal with the usual complement of five digits on the
hind limb.14 The second
Devonian tetrapod from East Greenland was Acanthostega.9,10 For many years this animal was known only from two
partial skull roofs, but these were enough to mark it out as different from Ichthyostega.
The search for evolutionary ancestors
Evolutionists sought the ancestry of the tetrapods among the lobe-finned fishes.
Although the lobe-fins are dominant in the fossil fish faunas of the Palaeozoic
(conventionally 590 to 248 million years ago), they are represented today by only
four surviving genera (the coelacanth Latimeria and three genera of lungfish).
In 1892, Cope and others argued that tetrapods had evolved from the crossopterygians,
the group of lobe-fins that includes the coelacanths.16 Various crossopterygians were proposed as the ‘model
ancestor’, including Sauripteris17,18
and Osteolepis.19
However, most attention settled upon Eusthenopteron, from Escuminac Bay
in Quebec, Canada. This is the fish that was commonly illustrated, in popular books
on fossils, as hauling itself up onto Devonian riverbanks (e.g. Owen20).
Nevertheless, there was evidently a substantial discontinuity in the fossil record
between terrestrial vertebrates like Ichthyostega and their presumed ancestors.
This was reflected in creationist treatments of the problem21 and acknowledged by evolutionists, such as Carroll22 who wrote:
‘We have not found any fossils that are intermediate between such clearly
terrestrial animals and the strictly aquatic rhipidistians described in the previous
chapter.’
|
Taxon
|
Stratigraphic unit
|
Age
|
Location
|
Material
|
Reference(s)
|
|
Pederpes
|
Ballagan Fm
|
Tournaisian
|
Scotland
|
Skull, almost complete articulated skeleton
|
23
|
|
Sinostega
|
Zhongning Fm
|
Famennian
|
Ningxia Hui, China
|
Incomplete left mandible
|
24
|
|
Tulerpeton
|
Khovanshchina Beds
|
Famennian
|
Tula Region, Russia
|
Fore and hind limbs, partial pectoral and pelvic girdles,
skull fragments
|
25–28
|
|
Ventastega
|
Ketleri Fm
|
Famennian
|
Latvia
|
Skull fragments, girdle fragments
|
29
|
|
Acanthostega
|
Britta Dal Fm
|
Famennian
|
East Greenland
|
Skulls, articulated skeletons
|
9,10,30–36,44,50
|
|
Ichthyostega
|
Aina Dal Fm Britta Dal Fm
|
Famennian
|
East Greenland
|
Skulls, skeletal elements, some articulated
|
9–12,44
|
|
Hynerpeton
|
Catskill Fm
|
Famennian
|
Pennsylvania, USA
|
Pectoral girdle, skull fragments
|
37,38
|
|
Densignathus
|
Catskill Fm
|
Famennian
|
Pennsylvania, USA
|
Lower jaw
|
38
|
|
Metaxygnathus
|
Cloghnan Shale
|
Famennian
|
New South Wales, Australia
|
Lower jaw
|
39
|
|
Elginerpeton
|
Scat Craig Beds
|
Frasnian
|
Scotland
|
Ilia, limb bones, skull and pectoral girdle fragments
|
40–42
|
|
Obruchevichthys
|
Ogre Beds
|
Frasnian
|
Latvia
|
Lower jaw fragments
|
40
|
|
Livoniana
|
Gauja Fm
|
Givetian
|
Latvia
|
Lower jaw fragments
|
43
|
Table 1. ‘Early’ tetrapods and so-called ‘near
tetrapods’. Most are represented by single specimens; Acanthostega
is unique in that it represents a stratigraphic range. Givetian is a subdivision
of the Middle Devonian, Frasnian and Famennian are subdivisions of the Upper Devonian,
and Tournaisian is a subdivision of the Lower Carboniferous.
Aquatic tetrapods challenge the ‘drying pond’ hypothesis
Since 1990 our knowledge of ‘early’ tetrapods has been greatly expanded,
with many new taxa being described. Fossil material is now known from Scotland,
Greenland, Latvia, the USA, Australia, Russia, and China (Table 1).23–43
Furthermore, our understanding of the Greenland tetrapods has been revolutionized
by the discovery of new material. As a consequence, a major re-evaluation of tetrapod
origins has taken place, and almost every aspect of the ‘drying pond’
hypothesis has had to be discarded.

Figure 2. Acanthostega in a swimming posture (from Clack).46
|
The fatal blow to the ‘drying pond’ hypothesis has been the realization
that the Devonian tetrapods were predominantly aquatic in habit. New ichthyostegid
material, including a well-preserved and articulated hind limb, collected by an
expedition to East Greenland in 1987, revealed that Ichthyostega was polydactylous,
with seven digits on the hind limb (Figure 1).44 This
was a very surprising discovery because pentadactyly had been assumed to be the
normal condition in ‘early’ tetrapods. Furthermore, the flattened bones
and inflexible ankle of the hind limb suggests that it was more like the paddle
of an elephant seal than the leg of a terrestrial animal.45 It appears that the earliest reconstruction of Ichthyostega
as a creature at home in the water was more accurate than later ones portraying
it on land.
Acanthostega is also much more completely known as a result of material
collected by the 1987 expedition, including the first postcranial remains.47,48
It was a smaller animal than Ichthyostega and its teeth suggest that it
had a different diet. Several articulated specimens were found in a single lens
of rock, interpreted as a possible flash flood deposit.49 The remarkable preservation meant that some delicate
structures, not often preserved in fossil tetrapods, are known in Acanthostega.
The gill skeleton was fish-like50
and it has been suggested that Acanthostega had internal gills somewhat
similar to those of the Australian lungfish (Neoceratodus). Acanthostega
had a tail with fin rays, even larger than that of Ichthyostega (Figure
2). The fin rays also extended further beneath the tail, in similar fashion to those
of a lungfish, suggesting that Acanthostega was a thoroughly aquatic creature.
This conclusion is supported by the morphology of the fore and hind limbs which
are difficult to interpret as load-bearing structures; rather, they appear to be
designed for swimming. As with Ichthyostega, perhaps the most extraordinary
feature was the number of digits. An articulated fore limb revealed eight digits
in a paddle-like arrangement (Figure 3). Clack51 speculates that they may have been enclosed in some
kind of webbing.

Figure 3. The left forelimb of Acanthostega, showing the eight
digits (from Clack).52
|
Most evolutionists had assumed that the origin of limbs with digits was synonymous
with the vertebrate invasion of the land. This led to the popular ‘conquest
of the land’ idea, typified by artistic reconstructions and museum displays
of fish crawling out of Devonian pools. However, the latest thinking about the aquatic
or semi-aquatic nature of the Devonian tetrapods has led modern-day evolutionists
to reject this assumption. They now argue that the key tetrapod characters evolved
for a shallow-water existence and were only later co-opted for terrestrial use.
The new generation of Darwinists dismisses the ‘drying pond’ hypothesis
as untestable story-telling, and increasingly relies on cladistics as an alternative
framework for understanding the transition. The cladistic approach to the fish-tetrapod
transition focuses on determining the sequence of acquisition of key tetrapod characteristics,
from which inferences are drawn about the nature of the transition.53 We should recognize, however,
that the cladistic methodology is inherently Darwinian and assumes from the outset
the continuity of life. By its very nature, cladistics is insensitive to the discontinuities
which creationists believe characterize living things.54
Other problems with the ‘drying pond’ hypothesis
The drying pond hypothesis has other problems.55 For instance, it is recognized that red beds are not
necessarily indicators of arid climates:
‘The red bed problem has been extremely controversial, with marked differences
of opinion, possibly due to the fact that the term “red bed” is a catchall
for many sedimentary types produced under different conditions, the only common
feature of them being the red color.’56
Modern red beds develop in the oxidizing conditions of the low latitude tropics
(e.g. the Amazon Basin). Such environments are characterized by monsoonal rainfall,
not arid conditions. Another problem is that, even if the red beds were laid down
under conditions of semi-aridity, evolutionists cannot assume that the tetrapods
arose in such environments, for the simple reason that many Devonian sediments are
not red beds. Some are interpreted as river, lake, or near-shore sediments rich
in organic matter, suggesting nearby forests.57
Furthermore, a survey of modern fishes that leave the water to spend time on land58 affords no support
for the ‘drying pond’ hypothesis. There is no association between those
that leave the water and those that possess digit-like fins. For example, eels undertake
long journeys overland but they have nothing that could be described as digit-like
appendages. Indeed, most of the fishes that possess digit-like structures are deep
water species or habitual bottom dwellers, such as the Sargassum frogfish.
New views on tetrapod ancestry
There have also been changes of opinion about which group of fishes is closest to
the ancestry of tetrapods. Eusthenopteron is no longer regarded as the
model ancestor. Depictions showing this fish emerging onto dry land owed more to
evolutionary presuppositions than evidence. Eusthenopteron was a rather
undistinguished fish with no obvious adaptations to terrestrial life; tetrapod-like
behaviour was attributed to it simply because there was no better candidate to fill
the role of tetrapod ancestor. The true lifestyle of Eusthenopteron seems
to have been that of a lurking aquatic predator, somewhat similar to the modern
pike (Esox).
Attention is now focused on the formerly more obscure lobe-finned fishes, Panderichthys
and Elpistostege. Until recently, these two genera were united in a family
called the panderichthyids, but evolutionists now believe that they are not uniquely
related to each other.59
Fossil material from Latvia and Canada shows that these fish were more tetrapod-like
than other lobe-fins. Indeed, based on a partial skull roof, Elpistostege
was originally described as a tetrapod.60
Although there has been dissent,61,62 these genera are increasingly
regarded by evolutionists as the closest known relatives of tetrapods.63–65 The latest work by Ahlberg et al.43 indicates that Elpistostege is even
more tetrapod-like than Panderichthys. These fish have crocodile-like skulls
with dorsally placed eyes, straight tails, and slightly flattened bodies without
dorsal or anal fins (see Figure 4). Like tetrapods, but unlike all other fishes,
they also have frontal bones in the skull roof. Like Eusthenopteron, they
seem designed for life as shallow-water predators.

Figure 4. Panderichthys, an Upper Devonian lobe-finned fish regarded
by evolutionists as close to the ancestor of tetrapods (from Clack).59
|
Chimeromorphs pose problems for evolutionary theory
Creationists and evolutionists have observed that many organisms, both fossil and
living, exhibit a mosaic distribution of character traits. Parker66 put it this way:
‘Each created kind is a unique combination of traits that are individually
shared with members of other groups.’
Stephen Jay Gould called such organisms ‘mosaic forms’ or ‘chimeras’67 while Kurt Wise68,69
calls them chimeromorphs. The duck-billed platypus (Ornithorhynchus anatinus),
for instance, has features of both mammals (hair, milk production) and reptiles
(egg-laying). Perhaps the best-known fossil example is Archaeopteryx, which
combines feathers with teeth and wing claws. In fact, a mosaic pattern of character
distribution is seen in many other fossil organisms. For instance, Woodmorappe70
recently drew attention to the chimeric nature of the pakicetids, a group of terrestrial
artiodactyls with a whale-like inner ear.
This observation seems to apply to the Devonian tetrapods and fishes considered
in this article. For example, Daeschler et al. noted that:
‘Devonian tetrapods show a mosaic of terrestrial and aquatic adaptations.’71
Some of the fishes possess tetrapod-like characters while the tetrapods have fish-like
features. Evolutionists interpret mosaic organisms like these as evolutionary intermediates
linking major groups. However, Wise72
makes an important point against this interpretation:
‘Although the entire organism is intermediate in structure, it’s the
combination of structures that is intermediate, not the nature of the structures
themselves. Each of these organisms appears to be a fully functional organism full
of fully functional structures.’
Evolutionary theory might lead us to expect examples of intermediate structures,
but there is nothing intermediate about, for example, the internal gills of Acanthostega,
its lateral line system, or its limbs. They are fully developed and highly complex.
What is unusual is their combination in a single organism. Intelligent design offers
an alternative understanding of this widespread pattern. The Devonian tetrapods
are thought to have lived a predatory lifestyle in weed-infested shallow water.
They were therefore equipped with characteristics appropriate to that habitat (e.g.
crocodile-like morphology with dorsally placed eyes, limbs and tails made for swimming,
internal gills, lateral line systems). Some of these features are also found in
fishes that shared their environment.
The mosaic pattern makes it difficult to identify organisms or groups of organisms
that possess the ‘right’ combination of characters to be considered
part of an evolutionary lineage. Consider the tetrapod-like lobe-fins Panderichthys
and Elpistostege. Despite their appearance, these fish have some unique
characters (such as the design of the vertebrae) that rule them out as tetrapod
ancestors. At best, evolutionists can only claim that they are a model
of the kind of fish that must have served as that ancestor. The same problem is
encountered with the Devonian tetrapods. For example, Ichthyostega is described
as ‘a very strange animal, and parts of it are like no other known tetrapod
or fish’.73 Similarly,
the shoulder girdles of the Devonian tetrapods ‘are not obviously halfway
in structure between those of fishes and those of later tetrapods but have some
unique and some unexpected features’.74 Another example is Livoniana, a so-called
‘near tetrapod’ known from two lower jaw fragments. It possesses a curious
mixture of fish-like and tetrapod-like characteristics, but it also has up to five
rows of teeth, a feature not seen either in the fishes from which it is thought
to be descended nor the tetrapods into which it is said to be evolving.75 That the mosaic distribution
of characters can cause great confusion is exemplified by the recent discovery of
Psarolepis, a fish from the Upper Silurian/Lower Devonian of China, which
combines characters found in placoderms, chondrichthyans, ray finned fishes, and
lobe-fins.76
Additional problems with ‘early’ tetrapod evolution
Another problem is that the fossil record imposes tight constraints on the timing
of the supposed transition. The earliest tetrapod fossils are found in late Frasnian
sediments, but their presumed ancestors are hardly much older. To exacerbate the
situation, the Frasnian ‘near tetrapods’ (Obruchevichthys,
Elginerpeton, Livoniana) are already morphologically diverse at
their first appearance.77
Thus Darwinists are compelled to postulate a rapid burst of evolution in which radical
changes must have taken place:
‘Panderichthys and Elpistostege flourished in the early
Frasnian and are some of the nearest relatives of tetrapods. But tetrapods appear
only about 5 to 10 million years later in the late Frasnian, by which time they
were widely distributed and had evolved into several groups, including the lineage
leading to the tetrapods of the Famennian. This suggests that the transition from
fish to tetrapod occurred rapidly within this restricted time span.’78
Second, key morphological transitions, such as the purported change from paired
fins to limbs with digits, remain undocumented by fossils. Where appendages are
known they are clearly either fish-like fins or digit-bearing limbs, not at some
transitional stage from one to the other. At one time it was claimed that the pectoral
fins of rhizodonts, a group of lobe-finned fish, were remarkably similar to tetrapod
limbs, but following the description of Gooloogongia from the Famennian
of New South Wales, Johanson and Ahlberg79
have urged that they not be used as a model for the origin of tetrapod limbs. Furthermore,
the pectoral fins of lobe-finned fish tend to be larger than the pelvic fins, whereas
the Devonian tetrapods were ‘rear-wheel drive’ animals with larger hind
limbs than fore limbs.80
None of the recent fossil discoveries shed any light on this supposed reconfiguration.
Third, there are functional challenges to Darwinian interpretations. For instance,
in fish the head, shoulder girdle, and circulatory systems constitute a single mechanical
unit. The shoulder girdle is firmly connected to the vertebral column and is an
anchor for the muscles involved in lateral undulation of the body, mouth opening,
heart contractions, and timing of the blood circulation through the gills.81 However, in amphibians the
head is not connected to the shoulder girdle, in order to allow effective terrestrial
feeding and locomotion. Evolutionists must suppose that the head became incrementally
detached from the shoulder girdle, in a step-wise fashion, with functional intermediates
at every stage. However, a satisfactory account of how this might have happened
has never been given.
Conclusion
Recent discoveries have undoubtedly advanced our knowledge of Devonian tetrapods
and future creationist discussions of tetrapod origins must take this into account.
It is no longer sufficient for creationists to contrast Eusthenopteron
with Ichthyostega and point to the large morphological gap between them.
We need to have more to say. Nevertheless, the presumed transition from fish to
tetrapods remains contentious. The data and their interpretation are a source of
lively debate and ongoing controversy:
‘In the not-too-distant past, there was almost no fossil material, and ideas
were based largely on informed guesswork. Speculation was intense, and as is often
the case, in inverse proportion to the amount of data. To be truthful, there is
still not much real data, so that speculation is still active, and whatever is concluded
today may be overturned by the discovery of a new fossil tomorrow. That in some
sense is to be hoped for, because only in that way can guesses be falsified and
tested as scientific hypotheses.’82
A robust rationale for concluding that the Upper Devonian tetrapods evolved from
a fish ancestor, or that they gave rise to Carboniferous tetrapod lineages, is lacking.
It is hoped that this paper may stimulate creationists to develop a fuller understanding
of these remarkable creatures and their ecological and geological context.83
Paul Garner has a B.Sc. (Hons)
in Geology and Biology and is a Fellow of the Geological Society of London. He works
full-time as a speaker and researcher with Biblical Creation Ministries in the UK.
He is also a Committee Member of the Biblical Creation Society, co-editor of the
BCS journal, Origins, and is on the Board of The Genesis Agendum, a charitable
company promoting church and public awareness of the substantial historical and
scientific evidence supporting the biblical record. Return to top.
Further reading
References
- Morton, G.R., Fish to amphibian transition, <home.entouch.net/dmd/transit.htm>,
27 June 2003. Return to text.
- Zimmer, C., At the Water’s Edge: Fish with Fingers, Whales
with Legs, and How Life Came Ashore but Then Went Back to Sea, Touchstone,
New York, 1998. Return to text.
- Clack, J.A., Gaining Ground: The Origin and Evolution of Tetrapods,
Indiana University Press, Bloomington, 2002. Return to text.
- Clack, Ref. 3, p. 1. Return to text.
- Clack, Ref. 3, pp. 17, 18. Return to text.
- Barrell, J., Influence of Silurian-Devonian climates on the rise
of air-breathing vertebrates, Bulletin of the Geological Society of America
27:387–436, 1916. Return to text.
- Barrell, Ref. 6, p. 390. Return to text.
- Romer, A.S., Man and the Vertebrates, Volume 1, Penguin,
Harmondsworth, pp. 48–49, 1954. Return to text.
- Säve-Söderbergh, G., Preliminary note on Devonian stegocephalians
from East Greenland, Meddelelser om Grønland 94:1–107,
1932. Return to text.
- Jarvik, E., On the fish-like tail in the ichthyostegid stegocephalians,
Meddelelser om Grønland 114:1–90, 1952. Return to text.
- Jarvik, E., Specializations in early vertebrates, Annales
Societe Royale Zoologique de Belgique 94:11–95, 1965.
Return to text.
- Jarvik, E., The Devonian tetrapod Ichthyostega, Fossils
and Strata 40:1–213, 1996. Return to text.
- Jarvik, E., Basic Structure and Evolution of Vertebrates,
Volumes 1 and 2, Academic Press, New York, 1980. Return to text.
- Carroll, R.L., Vertebrate Paleontology and Evolution,
W.H. Freeman and Company, New York, p. 164, 1988. Return to text.
- Clack, Ref. 3, p. 114. Return to text.
- Cope, E.D., On the phylogeny of the vertebrata, Proceedings
of the American Philosophical Society 30:278–281, 1892.
Return to text.
- Gregory, W.K., Present status of the problem of the origin of
the Tetrapoda, with special reference to the skull and paired limbs, Annals of the
New York Academy of Sciences 26:317–383, 1915.
Return to text.
- Gregory, W.K., Further observations on the pectoral girdle and
fin of Sauripterus taylori Hall, a crossopterygian fish from the Upper
Devonian of Pennsylvania, with special reference to the origin of the pentadactylate
extremities of Tetrapoda, Proceedings of the American Philosophical Society
75:673–690, 1935. Return to text.
- Watson, D.M.S., Croonian lecture—The evolution and origin
of the Amphibia, Philosophical Transactions of the Royal Society of London Series
B 214:189–257, 1926. Return to text.
- Owen, E., Prehistoric Animals: the Extraordinary Story of
Life Before Man, Octopus Books, London, p. 20, 1975. Return to text.
- Gish, D.T.,
Evolution: The Fossils Say No! Third edition, Creation-Life Publishers,
San Diego, pp. 78–83, 1979. Return to text.
- Carroll, Ref. 14, p. 158. Return to text.
- Clack, J.A., An early tetrapod from ‘Romer’s Gap’,
Nature 418:72–76, 2002. Return to text.
- Zhu, M., Ahlberg, P.E., Zhao, W. and Jia, L., First Devonian tetrapod
from Asia, Nature 420:760–761, 2002.
Return to text.
- Lebedev, O.A., The first record of a Devonian tetrapod in the
USSR, Doklady Akademii Nauk SSSR 278:1470–1473,
1984. Return to text.
- Lebedev, O.A., The first tetrapods: searchings and findings,
Priroda 11:26–36, 1985. Return to text.
- Lebedev, O.A. and Clack, J.A., Upper Devonian tetrapods from Andreyevka,
Tula region, Russia, Palaeontology 36:721–734, 1993.
Return to text.
- Lebedev, O.A. and Coates, M.I., The postcranial skeleton of the
Devonian tetrapod Tulerpeton curtum Lebedev, Zoological Journal of the
Linnean Society 114:307–348, 1995. Return
to text.
- Ahlberg, P.E., Lukševis, E. and Lebedev, O., The first
tetrapod finds from the Devonian (Upper Famennian) of Latvia, Philosophical Transactions
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review based on the Devonian genus Acanthostega, Transactions of the Royal
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Jarvik and the evolution of the otic region in tetrapods, Zoological Journal of
the Linnean Society 122:61–97, 1998. Return
to text.
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tetrapod clade, Nature 373:420–425, 1995.
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of Scat Craig, Morayshire, Scotland, Zoological Journal of the Linnean Society
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Today 4:407–409, 1988. Return to text.
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tetrapod palaeoecology in the light of new discoveries in East Greenland, Terra
Nova 2:131–137, 1990. Return to text.
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creation biosystematic method; in: Walsh, R.E. and Brooks, C.L. (Eds), Proceedings
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of panderichthyid fishes with comments on their relationship to tetrapods; in: Schultze,
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Creation: Facts of Life, Master Books, Green Forest, p. 118, 1994.
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major groups; in: Moreland, J.P. (Ed.), The Creation Hypothesis: Scientific Evidence
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understanding of transitional forms,
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nested or not? in: Walsh, R.E. (Ed.), Proceedings of the Fourth International Conference
on Creationism, Creation Science Fellowship, Pittsburgh, pp. 619–631,
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- Woodmorappe, J., Walking whales, nested
hierarchies, and chimeras: do they exist? Journal of Creation 16(1):111–119,
2002. Return to text.
- Daeschler et al., Ref. 37, p. 641. Return
to text.
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Livoniana—have they (finally!) found a missing link? Journal of Creation
16(1):4–6, 2002. Return to text.
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light on the origin of bony fishes, Nature 397:607–610,
1999. Return to text.
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from Australia, Nature 394:569–573, 1998.
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text.
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bar of the Spiny Dogfish (Squalas acanthias): implications for the evolutionary
history of the shoulder girdle of vertebrates, 43rd Annual Meeting of
the Palaeontological Association, Manchester, 19–22 December 1999;
<www.palass.org/index.html>, 4 April 2003. Click on ‘Abstracts’
then ‘Manchester 1999’. Return to text.
- Clack, Ref. 3, p. 3. Return to text.
- One approach to understanding the ‘early’ tetrapods
is outlined in a forthcoming paper: Garner, P., From Fins to Feet: Did Fish Evolve
into Tetrapods? The Genesis Agendum Occasional Paper 9, 2003. Available
from The Genesis Agendum, P.O.Box 5918, Leicester LE2 3XE, UK. Return
to text.
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