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The Ordovician Period, the second period of the Paleozoic Era, took place from 488 to 444 million years ago. During those 44 million years, the landmasses of earth were devoid of life except for hardy lichens, tiny algae, and a few lowly non-vascular plants. The oceans, however, teemed with diverse marine invertebrates and primitive vertebrates. The ecosystems of these great shallow seas seem familiar–with colorful intermeshed filter feeders, grazing herbivores, and swift deadly predators. And yet the creatures are so alien as to make Ordovician reconstructions almost resemble another planet. All of the creatures of a modern coral reef are replaced by strange analogs: the dominant filter feeder were not corals but weird sponge-like animals—the archaeocyathids. The grazers were conodonts and trilobites. The predators were primitive sharks, huge scorpion-like eurypterids, and above all, the nautiloids–for the Ordovician was a time when cephalopods ruled the earth.
Clever mollusks with multiple tentacles, eyes, and a method of jet propulsion, cephalopods had evolved in the Late Cambrian from a snail-like ancestor. Their taxonomy exploded in complexity during the Ordovician period. They also left the shallow continental shelves to range across the pelagic ocean and to descend into the benthic depths. The cephalopods of the Ordovician period were the nautiloids, animals which manipulated a bubble of air within a chambered shell to move up and down the water column. They could grab prey with their many tentacles or retreat into their calcium-based shell. The family quickly exploded in complexity. To quote palaeos.com:
At least ten different orders flourished at this time, all but one appearing for the first time during the early or middle part of the Ordovician. This astonishing diversity included straight, curved, loosely coiled, and tightly coiled shelled types, and even one group (the Ascocerids) that in order to become lighter and more streamlined lost the a large part of their shell altogether. These intelligent carnivorous molluscs replaced the Cambrian Anomalocarids as the dominant life form and top predator of the world’s ocean. The biggest, such as the endocerids, attained huge size; with shells of up to 10 meters in length they were the largest animal that, up until that time, had ever lived.
Some paleontologists have expressed doubts about this magnificent ten meter endocerid shell. But, even so, it is worth remembering that this measurement did not include the tentacles and the head of the creature. These giant orthocones must have been formidable predators, living on nautiloids, eurypterids, and jawless fish. The great monsters are believed to have had weak eyes (and could probably be avoided by staying shell-side of the behemoths). However an even bigger problem faced the tentacled masters of that world.
During Ordovician times, the land masses that are now South America, Africa, Madagascar, Antarctica, India, South Asia, and Australia were all joined together as a supercontinent, Gondwanaland. Over tens of millions of years Gondwanaland gradually drifted into the Southern Polar regions of the globe. This resulted in heavy glaciation, which in turn caused rapid deep freezes and sudden interglacial warm periods—in other words, an ice age. This great ice age caused the depth of the ocean to fluctuate wildly which brought a crashing end to the Ordovician and its dominant cephalopods. The mass extinction which ended the Ordovician period was the second worst in the history of the planet (eclipsed only by the mass extinction at the end of the Permian period). More than 60% of marine invertebrates went extinct (including whole families of mollusks). This was but one set back for cephalopods. The family has burgeoned and then crashed many times, but it marked the end of their time as apex predator.