Posts Tagged ‘Fossil Evidence’

Genus Eustenopteron

Monday, February 27th, 2012


The Devonian period, some 350 million years ago, some of the crossopterygian fishes came out onto the land. It is very likely that these fishes were of a type represented by the genus Eustenopteron. In evolutionary terms, this was one of the boldest steps in history: a venturing of early vertebrates into a completely new environment to which they were only partially adapted. Once this step had been made, however, it was not long before these advanced, air-breathing fishes became transformed into primitive Amphibia.

From available fossil evidence it has been calculated that the earliest amphibians belonged to a group known as chthyostegids, creatures that had characteristics of both the crossopterygian fishes and the later, more advanced amphibians. A typical chthyostegid, a member of the genus Ichthyostega, had a skull about 15 cm (6 in) in lenght. Although similar in many respects to the skull of crossoptergian fish ancestor, there were certain important changes between that of the fish and that of the amphibian. In the fish, for example, the part of the skull in front of the eyes was comparatively short, while the portion behind the eyes was comparatively long. In Ichthyostega a paradoxical situation prevailed in which the portion of the skull behind the eyes was relatively shorter than that of the fishes and the portion in front relatively longer. In amphibians, the eyes tended to be oriented more toward the top of the skull than in the fishes. Although Ichthyostega had developed strong pectoral and pelvic girdles that carried completely developed limbs and feet, the fin rays of the fish tail were retained! From this early fish/amphibian we can follow the evolution of the later amphibians as they radiated into different lines.

In changing from a totally aquatic experience to a new terrestrial life, various problems had to be resolved. While a fish normally obtains its oxygen from water by means of gills, the early amphibians had to further develop and perfect the lungs that they had inherited from their crossopterygian ancestors, although in the larval stage (as is still the case with modern amphibians) they continued to respire by means of gills. Another problem that land-dwelling animals had to deal with was the possibility of desiccation or drying up.

 

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Reptiles

Saturday, December 25th, 2010


The history of reptiles, from their first appearance during the Carboniferous to the present, is traced on this chart. (Each white area represents a major order plotted according to when it first began to flower and how long it lasted.) In addition to the major groups, many short-lived offshoots developed. For reasons of space only two of them, represented by the marine forms Geosaurus  and Tylosaurus, have been included here. Solid bars on the chart indicate lines of descent which have been fairly well established by the fossil record. Broken bars are used where the fossil evidence is sketchy.

A striking aspect of reptile history is how, from the primitive cotylosaurs (here represented by Seymouria), these creatures radiated to occupy an enormous variety of niches on land, in the water, and in the air. One group of cotylosaurian descendants that played a profound role in the development of reptiles was the thecodonts, primitive archosaurs. Not only did they give rise to the Ornithischia  and Saurischia (popularly called dinosaurs), but also the Pterosauria (flying reptiles) and the Crocodilia. Thecodonts were even related to the ancestral birds. The mammals evolved from another group, the therapsids, shown at lower left.

Another curious fact of reptilian evolution revealed by this chart is the relative suddenness with which order after order disappeared toward the end of the Cretaceous, described as “the time of the great.”

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Dinosaur Family Tree

Saturday, December 5th, 2009


The evolutionary tree of dinosaurs contains a great deal of information. The horizontal axis represents time, and the vertical axis represents dinosaurian diversity. All the major families of dinosaurs are indicated with horizontal lines that record their known distribution in time, as based upon present fossil evidence. Future finds of dinosaur skeletons may extend the time ranges backwards or forwards in time.

There are two “fixed” time lines that do not seem to be breached, however. The dinosaurs arose from a single ancestor some 230 million years ago, in the Middle to Late Triassic, and it is unlikely that older dinosaur skeletons will be found. The second “fixed” time line corresponds to the extinction of the last dinosaurs 66 million years ago. Despite strenuous efforts to find post-Mesozoic dinosaur specimens, and many reports of supposed discoveries, no such remains have withstood close scrutiny. Most usually, post-mesozoic dinosaur bones have been reworked, that is, removed from the rock by natural erosion and redeposited in a younger sediment.

The most important aspect of this phylogenetic tree is the representation of the relationships between the different families. This is based on recent cladistic anlyses, carried out by a number of North American and European vertebrae paleontologists after 1985, and the pattern shown here is quite revolutionary in the sense that it is dramatically different from anything in popular books of this sort. It is also important because it shows a much higher degree of resolution than the earlier phylogenies; that is, the pattern of relationships is shown in a much more detailed way than was possible before.

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