Cover for The Outline of Science, Volume 1

Project Gutenberg #20417

The Outline of Science, Volume 1

J. Arthur Thomson

1922

Thomson's broad popular-science survey of astronomy, biology, and Earth science, prepared section by section from Project Gutenberg HTML.

Project Gutenberg #20417 Public domain in the United States Cover source Local typographic cover created for MojiMori from public-domain source metadata

Section 71 of 226

The Era of Ancient Life (Pal ozoic)

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The Cambrian period was the time of the establishment of the chief stocks of backboneless animals such as sponges, jellyfishes, worms, sea-cucumbers, lamp-shells, trilobites, crustaceans, and molluscs. There is something very eloquent in the broad fact that the peopling of the seas had definitely begun some thirty million years ago, for Professor H. F. Osborn points out that in the Cambrian period there was already a colonisation of the shore of the sea, the open sea, and the deep waters. The Ordovician period was marked by abundant representation of the once very successful class of Trilobites—jointed-footed, antenna-bearing, segmented marine animals, with numerous appendages and a covering of chitin. They died away entirely with the end of the Pal ozoic era. Also very notable was the abundance of predatory cuttlefishes, the bullies of the ancient seas. But it was in this period that the first backboned animals made their appearancean epoch-making step in evolution. In other words, true fishes were evolveddestined in the course of ages to replace the cuttlefishes (which are mere molluscs) in dominating the seas.[Pg 92] RECENT TIMES Human civilisation. {PLEISTOCENE OR GLACIAL TIME Last great Ice Age. CENOZOIC ERA {MIOCENE AND PLIOCENE TIMES Emergence of Man. {EOCENE AND OLIGOCENE TIMES Rise of higher mammals. {CRETACEOUS PERIOD Rise of primitive mammals, flowering plants, and higher insects. MESOZOIC ERA {JURASSIC PERIOD Rise of birds and flying reptiles. {TRIASSIC PERIOD Rise of dinosaur reptiles. {PERMIAN PERIOD Rise of reptiles. {CARBONIFEROUS PERIOD Rise of insects. PAL OZOIC ERA {DEVONIAN PERIOD First amphibians. {SILURIAN PERIOD Land animals began. {ORDOVICIAN PERIOD First fishes. {CAMBRIAN PERIOD Peopling of the sea. PROTEROZOIC AGES Many of the Backboneless stocks began. ARCH OZOIC AGES Living creatures began to be upon the earth. {Making of continents and ocean-basins. FORMATIVE TIMES {Beginnings of atmosphere and hydrosphere. {Cooling of the earth. {Establishment of the solar system. In the Silurian period in which the peopling of the seas went on apace, there was the first known attempt at colonising the dry land. For in Silurian rocks there are fossil scorpions, and that implies ability to breathe dry airby means of internal surfaces, in this case known as lungbooks. It was also towards the end of the Silurian, when a period of great aridity set in, that fishes appeared related to our mud-fishes or double-breathers (Dipnoi), which have lungs as well as gills. This, again, meant utilising dry air, just as the present-day mud-fishes do when the water disappears from the pools in hot weather. The lung-fishes or mud-fishes of to-day are but three in number, one in Queensland, one in South America, and one in Africa, but they are extremely[Pg 93] interesting "living fossils," binding the class of fishes to that of amphibians. It is highly probable that the first invasion of the dry land should be put to the credit of some adventurous worms, but the second great invasion was certainly due to air-breathing Arthropods, like the pioneer scorpion we mentioned. PICTORIAL REPRESENTATION OF THE SUCCESSIVE STRATA OF THE EARTH'S CRUST, WITH SUGGESTIONS OF CHARACTERISTIC FOSSILS E.g. Fish and Trilobite in the Devonian (red), a large Amphibian in the Carboniferous (blue), Reptiles in Permian (light red), the first Mammal in the Triassic (blue), the first Bird in the Jurassic (yellow), Giant Reptiles in the Cretaceous (white), then follow the Tertiary strata with progressive mammals, and Quaternary at the top with man and mammoth. The Devonian period, including that of the Old Red Sandstone, was one of the most significant periods in the earth's history. For it was the time of the establishment of flowering plants upon the earth and of terrestrial backboned animals. One would like to have been the discoverer of the Devonian foot-print of Thinopus, the first known Amphibian foot-print—an eloquent vestige of the third great invasion of the dry land. It was probably from a stock of Devonian lung-fishes that the first Amphibians sprang, but it was not till the next period that they came to their own. While they were still feeling their way, there was a remarkable exuberance of shark-like and heavily armoured fishes in the Devonian seas.

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