Deep ocean is no place to hide.Far below the waves, in the dark reaches of the sea, underwater gardens bloom wherever volcanic fluids seep from the seafloor. These hot, chemical-laden brines sustain an odd collection of microbes and animals, among them tube-shaped worms, giant clams, and blind shrimp. Because these hidden communities seem completely cut off from the rest of the world, some scientists think seafloor vents have sheltered ancient species that were wiped out in other parts of the globe long ago. A fossil discovery in Russia suggests otherwise. In the Jan. 9 Nature, a team of British and Russian scientists describes the petrified pet·ri·fy v. pet·ri·fied, pet·ri·fy·ing, pet·ri·fies v.tr. 1. To convert (wood or other organic matter) into a stony replica by petrifaction. 2. remnants of a vent community that thrived during Earth's Silurian period Silurian period (sĭl r`ēən, sī–) [from the Silures, ancient tribe of S Wales, where the period was first studied; named by the British geologist R. I. , which ran from 438 million to 410 million years ago. Found in the southern Ural mountains Ural MountainsMountain range, Russia and Kazakhstan. Generally held to constitute the boundary between Europe and Asia, the range extends north-south for some 1,550 mi (2,500 km) from just south of the Kara Sea to the Ural River; a southward spur extends into northwestern , this deposit contains the oldest and most diverse set of fossil vent creatures ever discovered, report Crispin T. S. Little of the Natural History Museum in London and his colleagues. Some denizens of the Silurian seafloor community are familiar, such as the large tubeworms seen at modern vents. Other members of the ancient oasis are unique, however. The Russian deposit includes fossilized fos·sil·ize v. fos·sil·ized, fos·sil·iz·ing, fos·sil·iz·es v.tr. 1. To convert into a fossil. 2. To make outmoded or inflexible with time; antiquate. v.intr. brachiopods-clamlike creatures that do not populate any known vents today. During the Silurian, brachiopods were abundant in the oceans, but they suffered severely during the mass extinction mass extinction, the extinction of a large percentage of the earth's species, opening ecological niches for other species to fill. There have been at least ten such events. at the end of the Permian period Permian period (pûr`mēən) [from Perm, Russia], sixth and last period of the Paleozoic era (see Geologic Timescale, table) from 250 to 290 million years ago. , 250 million years ago. Their absence from modern vents indicates that these ocean bottom communities have not served as protective refuges, contend Little and his colleagues. |
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r`ēən, sī–)
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