HOME
        TheInfoList



The Silurian ( ) is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at million years ago (Mya), to the beginning of the Devonian Period, Mya. The Silurian is the shortest period of the Paleozoic Era. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out. A significant evolutionary milestone during the Silurian was the diversification of jawed fish and bony fish. Multi-cellular life also began to appear on land in the form of small, bryophyte-like and vascular plants that grew beside lakes, streams, and coastlines, and terrestrial arthropods are also first found on land during the Silurian. However, terrestrial life would not greatly diversify and affect the landscape until the Devonian.


History of study


The Silurian system was first identified by British geologist Roderick Murchison, who was examining fossil-bearing sedimentary rock strata in south Wales in the early 1830s. He named the sequences for a Celtic tribe of Wales, the Silures, inspired by his friend Adam Sedgwick, who had named the period of his study the Cambrian, from the Latin name for Wales. This naming does not indicate any correlation between the occurrence of the Silurian rocks and the land inhabited by the Silures (. Geologic map of Wales, Map of pre-Roman tribes of Wales). In 1835 the two men presented a joint paper, under the title ''On the Silurian and Cambrian Systems, Exhibiting the Order in which the Older Sedimentary Strata Succeed each other in England and Wales,'' which was the germ of the modern geological time scale. As it was first identified, the "Silurian" series when traced farther afield quickly came to overlap Sedgwick's "Cambrian" sequence, however, provoking furious disagreements that ended the friendship. Charles Lapworth resolved the conflict by defining a new Ordovician system including the contested beds. An alternative name for the Silurian was ''"Gotlandian"'' after the strata of the Baltic island of Gotland. The French geologist Joachim Barrande, building on Murchison's work, used the term ''Silurian'' in a more comprehensive sense than was justified by subsequent knowledge. He divided the Silurian rocks of Bohemia into eight stages. His interpretation was questioned in 1854 by Edward Forbes, and the later stages of Barrande; F, G and H have since been shown to be Devonian. Despite these modifications in the original groupings of the strata, it is recognized that Barrande established Bohemia as a classic ground for the study of the earliest Silurian fossils.

Subdivisions



Llandovery

The Llandovery Epoch lasted from mya, and is subdivided into three stages: the , lasting until , the , lasting to , and the . The epoch is named for the town of Llandovery in Carmarthenshire, Wales.

Wenlock

The Wenlock, which lasted from mya, is subdivided into the (to ) and ages. It is named after Wenlock Edge in Shropshire, England. During the Wenlock, the oldest-known tracheophytes of the genus ''Cooksonia'', appear. The complexity of slightly later Gondwana plants like ''Baragwanathia'', which resembled a modern clubmoss, indicates a much longer history for vascular plants, extending into the early Silurian or even Ordovician. The first terrestrial animals also appear in the Wenlock, represented by air-breathing millipedes from Scotland.

Ludlow

The Ludlow lasted from mya. It is named for the town of Ludlow in Shropshire, England. The Ludlow comprises the stage (lasting until ) and the stage (named for Ludford, also in Shropshire).


Přídolí


The Přídolí epoch, lasting from mya, is the final and shortest epoch of the Silurian. It is named after one locality at the ''Homolka a Přídolí'' nature reserve near the Prague suburb Slivenec in the Czech Republic. ''Přídolí'' is the old name of a cadastral field area.

Regional stages

In North America a different suite of regional stages is sometimes used: * Cayugan (upper Silurian – Ludlow) * Lockportian (middle Silurian: upper Wenlock) * Tonawandan (middle Silurian: lower Wenlock) * Ontarian (lower Silurian: upper Llandovery) * Alexandrian (lowest Silurian: lower Llandovery) In Estonia the following suite of regional stages is used: * Kaugatuma stage (upper Silurian: upper Přídolí) * Ohessaare stage (upper Silurian: lower Přídolí) * Kuressaare stage (upper Silurian: upper Ludlow) * Paadla stage (upper Silurian: lower Ludlow) * Rootsiküla stage (middle Silurian: upper Wenlock) * Jaagarahu stage (middle Silurian: middle Wenlock) * Jaani stage (middle Silurian: lower Wenlock) * Adavere stage (lower Silurian: upper Llandovery) * Raikküla stage (lower Silurian: middle Llandovery) * Juuru stage (lowest Silurian: lower Llandovery) In Lithuania the following suite of regional stages is used: * Minija stage (upper Silurian: upper Přídolí) * Jūra stage (upper Silurian: lower Přídolí) * Pagėgiai stage (upper Silurian: upper Ludlow) * Dubysa stage (upper Silurian: lower Ludlow) * Gėluva stage (middle Silurian: upper Wenlock) * Jaani-Jaagarahu stage (middle Silurian: lower Wenlock, western and central Lithuania) * Jaagarahu stage (middle Silurian: middle Wenlock, eastern Lithuania) * Jaani stage (middle Silurian: lower Wenlock, eastern Lithuania) * Adavere stage (lower Silurian: upper Llandovery) * Juuru-Raikküla stage (lowest Silurian: lower Llandovery)

Paleogeography

left|Ordovician-Silurian_boundary_on_[[Hovedøya,_[[Norway.html" style="text-decoration: none;"class="mw-redirect" title="Hovedøya.html" style="text-decoration: none;"class="mw-redirect" title="Ordovician-Silurian boundary on [[Hovedøya">Ordovician-Silurian boundary on [[Hovedøya, [[Norway">Hovedøya.html" style="text-decoration: none;"class="mw-redirect" title="Ordovician-Silurian boundary on [[Hovedøya">Ordovician-Silurian boundary on [[Hovedøya, [[Norway, showing brownish late Ordovician [[mudstone and later dark deep-water Silurian [[shale. The layers have been overturned by the [[Caledonian orogeny. With the [[supercontinent [[Gondwana covering the equator and much of the southern hemisphere, a large ocean occupied most of the northern half of the globe. The high sea levels of the Silurian and the relatively flat land (with few significant mountain belts) resulted in a number of island chains, and thus a rich diversity of environmental settings. During the Silurian, Gondwana continued a slow southward drift to high southern latitudes, but there is evidence that the Silurian icecaps were less extensive than those of the late-Ordovician glaciation. The southern continents remained united during this period. The melting of icecaps and glaciers contributed to a rise in sea level, recognizable from the fact that Silurian sediments overlie eroded Ordovician sediments, forming an unconformity. The continents of Avalonia, Baltica, and Laurentia drifted together near the equator, starting the formation of a second supercontinent known as Euramerica. When the proto-Europe collided with North America, the collision folded coastal sediments that had been accumulating since the Cambrian off the east coast of North America and the west coast of Europe. This event is the Caledonian orogeny, a spate of mountain building that stretched from New York State through conjoined Europe and Greenland to Norway. At the end of the Silurian, sea levels dropped again, leaving telltale basins of evaporites extending from Michigan to West Virginia, and the new mountain ranges were rapidly eroded. The Teays River, flowing into the shallow mid-continental sea, eroded Ordovician Period strata, forming deposits of Silurian strata in northern Ohio and Indiana. The vast ocean of Panthalassa covered most of the northern hemisphere. Other minor oceans include two phases of the Tethys, the Proto-Tethys and Paleo-Tethys, the Rheic Ocean, the Iapetus Ocean (a narrow seaway between Avalonia and Laurentia), and the newly formed Ural Ocean.

Climate and sea level

The Silurian period enjoyed relatively stable and warm temperatures, in contrast with the extreme glaciations of the Ordovician before it, and the extreme heat of the ensuing Devonian. Sea levels rose from their Hirnantian low throughout the first half of the Silurian; they subsequently fell throughout the rest of the period, although smaller scale patterns are superimposed on this general trend; fifteen high-stands (periods when sea levels were above the edge of the continental shelf) can be identified, and the highest Silurian sea level was probably around 140 m higher than the lowest level reached. During this period, the Earth entered a long, warm greenhouse phase, supported by high CO2 levels of 4500 ppm, and warm shallow seas covered much of the equatorial land masses. Early in the Silurian, glaciers retreated back into the South Pole until they almost disappeared in the middle of Silurian. The period witnessed a relative stabilization of the Earth's general climate, ending the previous pattern of erratic climatic fluctuations. Layers of broken shells (called coquina) provide strong evidence of a climate dominated by violent storms generated then as now by warm sea surfaces. Later in the Silurian, the climate cooled slightly, but closer to the Silurian-Devonian boundary, the climate became warmer.


Perturbations


The climate and carbon cycle appear to be rather unsettled during the Silurian, which had a higher concentration of isotopic excursions than any other period. The Ireviken event, Mulde event and Lau event each represent isotopic excursions following a minor mass extinction and associated with rapid sea-level change, in addition to the larger extinction at the end of the Silurian. Each one leaves a similar signature in the geological record, both geochemically and biologically; pelagic (free-swimming) organisms were particularly hard hit, as were brachiopods, corals and trilobites, and extinctions rarely occur in a rapid series of fast bursts.

Flora and fauna

The Silurian was the first period to see megafossils of extensive terrestrial biota, in the form of moss-like miniature forests along lakes and streams. However, the land fauna did not have a major impact on the Earth until it diversified in the Devonian. The first fossil records of vascular plants, that is, land plants with tissues that carry water and food, appeared in the second half of the Silurian period. The earliest-known representatives of this group are ''Cooksonia''. Most of the sediments containing ''Cooksonia'' are marine in nature. Preferred habitats were likely along rivers and streams. ''Baragwanathia'' appears to be almost as old, dating to the early Ludlow (420 million years) and has branching stems and needle-like leaves of 10–20 cm. The plant shows a high degree of development in relation to the age of its fossil remains. Fossils of this plant have been recorded in Australia, Canada and China. ''Eohostimella heathana'' is an early, probably terrestrial, "plant" known from compression fossils of early Silurian (Llandovery) age. The chemistry of its fossils is similar to that of fossilised vascular plants, rather than algae. The first bony fish, the Osteichthyes, appeared, represented by the Acanthodians covered with bony scales; fish reached considerable diversity and developed movable jaws, adapted from the supports of the front two or three gill arches. A diverse fauna of eurypterids (sea scorpions)—some of them several meters in length—prowled the shallow Silurian seas of North America; many of their fossils have been found in New York state. Leeches also made their appearance during the Silurian Period. Brachiopods, bryozoa, molluscs, hederelloids, tentaculitoids, crinoids and trilobites were abundant and diverse. Endobiotic symbionts were common in the corals and stromatoporoids. Reef abundance was patchy; sometimes fossils are frequent but at other points are virtually absent from the rock record. The earliest-known animals fully adapted to terrestrial conditions appear during the Mid-Silurian, including the millipede ''Pneumodesmus''. Some evidence also suggests the presence of predatory trigonotarbid arachnoids and myriapods in Late Silurian facies. Predatory invertebrates would indicate that simple food webs were in place that included non-predatory prey animals. Extrapolating back from Early Devonian biota, Andrew Jeram ''et al.'' in 1990 suggested a food web based on as-yet-undiscovered detritivores and grazers on micro-organisms. Image:Cooksonia.png|''Cooksonia'', the earliest vascular plant, middle Silurian File:Wrens Nest Fossils 2.jpg|Silurian sea bed fossils collected from Wren's Nest Nature Reserve, Dudley UK Image:Kaugatuma Bedding Plane Pridoli Estonia.jpg|Crinoid fragments in a Silurian (Pridoli) limestone (Saaremaa, Estonia) File:Wrens Nest Fossils 3.jpg|Silurian sea bed fossils collected from Wren's Nest Nature Reserve, Dudley UK Image:Silurianfishes ntm 1905 smit 1929.gif|Artist's impression of Silurian underwater fauna File:Eurypterus Paleoart.jpg|''Eurypterus'', a common Upper Silurian eurypterid File:Poraspis.jpg|''Poraspis'' File:Calymene celebra Raymond, 1916.jpg|Trilobites were still diverse and common in the Silurian. Fossils of ''Calymene celebra'' are extremely abundant in parts of central USA.

Notes



References

*Emiliani, Cesare. (1992). ''Planet Earth : Cosmology, Geology, & the Evolution of Life & the Environment''. Cambridge University Press. (Paperback Edition ) * Mikulic, DG, DEG Briggs, and J Kluessendorf. 1985. A new exceptionally preserved biota from the Lower Silurian of Wisconsin, USA. Philosophical Transactions of the Royal Society of London, 311B:75-86. * * Ogg, Jim; June, 2004, ''Overview of Global Boundary Stratotype Sections and Points (GSSP's)'' https://web.archive.org/web/20060716071827/http://www.stratigraphy.org/gssp.htm Original version accessed April 30, 2006, redirected to archive on May 6, 2015.

External links


Palaeos:
Silurian

The Silurian
Paleoportal: Silurian strata in U.S., state by state
*

{{Authority control Category:Geological periods