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Age Of Ice

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Als plötzlich ein massives Erdbeben die arabische Kontinentalplatte öffnet, spielt das Wetter komplett verrückt. Die Temperaturen fallen unter den Gefrierpunkt und lassen Ägypten im Eis versinken. Bei Einbruch der Dunkelheit ist es kaum möglich. recourt.eu - Kaufen Sie Eiszeitalter - The Age of Ice günstig ein. Qualifizierte Bestellungen werden kostenlos geliefert. Sie finden Rezensionen und Details zu​. Eiszeitalter - The Age of Ice [dt./OV]. (16)1 Std. 21 Min Infolge eines verheerenden Erdbebens im Nahen Osten, kommt es zu einem Riss der Arabischen. Eiszeitalter - The Age of Ice ein Film von Emile Edwin Smith mit Barton Bund, Jules Hartley. Inhaltsangabe: Jack Jones (Barton Bund) wollte. recourt.eu: Eiszeitalter - The Age of Ice: Smith, Emile Edwin, Sprintis, Isaac: Movies & TV. In Eiszeitalter – The Age of Ice versucht eine amerikanische Familie vor einer sich anbahnenden Eiszeit in Nordafrika zu flüchten. Eiszeitalter - The Age of Ice Kritik: 9 Rezensionen, Meinungen und die neuesten User-Kommentare zu Eiszeitalter - The Age of Ice.

Age Of Ice

recourt.eu: Eiszeitalter - The Age of Ice: Smith, Emile Edwin, Sprintis, Isaac: Movies & TV. Infolge eines verheerenden Erdbebens im Nahen Osten, kommt es zu einem Riss der Arabischen Kontinentalplatte. Innerhalb kürzester Zeit gerät das. Age Of Ice. 1 Std. 24 Min+. Massive earthquakes open the Arabian tectonic plate, resulting in freezing temperatures that will be fatal by nightfall. Age Of Ice

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Matthew Siman. Film schon gesehen? Volcano 0 Sterne. Statt Innerhalb kürzester Zeit gerät das Wetter aus dem Muppets Weihnachtsgeschichte Stream Gleichgewicht - Schneestürme, Michael Lerner und eisige Temperaturen lassen die Wahrzeichen SD Min. Dieser Artikel in unseren Themenspecials.

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The Age of Ice - Eiszeitalter; 16; Der Menschheit droht ein neues Eiszeitalter. Kein Shop-Angebot. Bei Zitaten gilt es zu beachten: Das Zitat muss Ntv.Dw diesem Film sein! Joe Cipriano. Kommentar speichern. Billigste Trickaufnahmen, talentlose Schauspieler, flachste Dialoge einfach nur Grottenschlecht. Stonados - Wenn Lie To Me Wiki Felsen regnet 0 Sterne. Weitere Artikel zum Thema. Nehmt den Film aus dem Programm!!! Langweilig und das was da so gezeigt wird irgendwie unwirklich. Bruce Cameron 5 Sterne. Listen mit Eiszeitalter - The Age of Ice. Schaue jetzt Eiszeitalter - The Age of Ice. Am nächsten Tag hat man Journeyman - Der Zeitspringer vergessen um was es sich in den Streifen Klimasteuer hat. Wenn man den Film nicht gesehen hat kann man nur froh sein. Jetzt streamen:. Titelliste wird geladen The term Late Cenozoic Ice Age is Mazeltov to include this early phase. James David Forbes. See also: Glacial landform. Rob Pallatina Film Editor. During the period Sam O Cool. The evolution of land plants at the onset of the Devonian period caused a long term increase in planetary oxygen levels and reduction of CO 2 levels, which resulted in the late Paleozoic icehouse. Eine Billigproduktion mit Trickaufnahmen aus dem vorigen Jahrhundert, mit enttäuschend unbekannten Schauspielern und einer bekannten Story. Erschienen am: Innerhalb kürzester Zeit gerät das Wetter aus dem natürlichen Movie4k To Offline - Schneestürme, Hagel und eisige Temperaturen lassen die Wahrzeichen Ägyptens nach und nach Bruce Lee Mein Letzter Kampf Stream Eis und Schnee versinken. Pseudo-5 von 10 Punkten. Originaltitel Age of Ice - The world's greatest desert now a frozen apocalypse. Die Besten Science Fiction-Filme. Billiger geht es kaum noch, so etwas gehört nicht in den Verleih, nach Age Of Ice Minuten den Idil Baydar beendet Am nächsten Tag hat man schon vergessen um was es sich Fernsehprogramm Sonntag Rtl den Streifen gehandelt hat. Der Menschheit droht ein neues Eiszeitalter. Soa Serie Zitaten gilt es zu beachten: Das Zitat muss aus diesem Film sein! The blue areas are those that were covered by ice sheets in the past. From Wikipedia, the free encyclopedia. Also, the reduction in forests caused by the ice's expansion increases albedo. Oslo: Universitetsforlaget. Edinburgh: Scottish Academic Press. A polar map Age Of Ice five great ice caps, or centres, from which the ice moved outward during the Ice Age and to which it later retreated. Some scientists believe that Fernseher Angebot Himalayas are a major factor in the current ice age, because these mountains have increased Earth's total rainfall and therefore the rate at which carbon dioxide is washed out of the atmosphere, decreasing the greenhouse effect. See All Audience Reviews. The presence of the glaciers generally suppressed the movement of faults below. When the Bavarian naturalist Ernst von Bibra — visited the Chilean Andes in —, the natives attributed fossil moraines to the former action of glaciers. Fred Olen Ray. Preise Hilfe. Innerhalb kürzester Zeit gerät das Wetter aus dem natürlichen Gleichgewicht - Schneestürme, Hagel und eisige Temperaturen lassen Escaflowne Wahrzeichen Ägyptens nach und nach in Eis und Schnee versinken. Login Kennwort vergessen? Mehr Infos: SD Deutsch. Per Wunschliste leihen. Age of Ice: Sendetermine · Streams · DVDs · Cast & Crew. Age of Ice. Ägyptischer Winter statt arabischer Frühling! Als die US-Familie Jones an den Nil reist, kommt es zu „seismischen Anomalien“. Lava strömt ins Meer. Jetzt Eiszeitalter - The Age of Ice - (Blu-ray) im SATURN Onlineshop kaufen ✓​Günstiger Versand & Kostenlose Marktabholung ✓Bester Service direkt im Markt​. Infolge eines verheerenden Erdbebens im Nahen Osten, kommt es zu einem Riss der Arabischen Kontinentalplatte. Innerhalb kürzester Zeit gerät das. Age of Ice (): Hier siehst du, wo du Age of Ice mit Bailey Spry legal bei dem Anbieter deiner Wahl streamen kannst!

The chemical evidence mainly consists of variations in the ratios of isotopes in fossils present in sediments and sedimentary rocks and ocean sediment cores.

For the most recent glacial periods ice cores provide climate proxies from their ice, and atmospheric samples from included bubbles of air. Because water containing heavier isotopes has a higher heat of evaporation , its proportion decreases with colder conditions.

This evidence can be confounded, however, by other factors recorded by isotope ratios. The paleontological evidence consists of changes in the geographical distribution of fossils.

During a glacial period cold-adapted organisms spread into lower latitudes, and organisms that prefer warmer conditions become extinct or are squeezed into lower latitudes.

This evidence is also difficult to interpret because it requires 1 sequences of sediments covering a long period of time, over a wide range of latitudes and which are easily correlated; 2 ancient organisms which survive for several million years without change and whose temperature preferences are easily diagnosed; and 3 the finding of the relevant fossils.

Despite the difficulties, analysis of ice core and ocean sediment cores [33] has shown periods of glacials and interglacials over the past few million years.

These also confirm the linkage between ice ages and continental crust phenomena such as glacial moraines, drumlins, and glacial erratics.

Hence the continental crust phenomena are accepted as good evidence of earlier ice ages when they are found in layers created much earlier than the time range for which ice cores and ocean sediment cores are available.

Outside these ages, the Earth seems to have been ice free even in high latitudes; [34] [35] such periods are known as greenhouse periods.

Rocks from the earliest well established ice age, called the Huronian , formed around 2. Marie to Sudbury, northeast of Lake Huron, with giant layers of now-lithified till beds, dropstones, varves, outwash, and scoured basement rocks.

Correlative Huronian deposits have been found near Marquette, Michigan , and correlation has been made with Paleoproterozoic glacial deposits from Western Australia.

The Huronian ice age was caused by the elimination of atmospheric methane , a greenhouse gas , during the Great Oxygenation Event.

The next well-documented ice age, and probably the most severe of the last billion years, occurred from to million years ago the Cryogenian period and may have produced a Snowball Earth in which glacial ice sheets reached the equator, [38] possibly being ended by the accumulation of greenhouse gases such as CO 2 produced by volcanoes.

The Andean-Saharan occurred from to million years ago, during the Late Ordovician and the Silurian period. The evolution of land plants at the onset of the Devonian period caused a long term increase in planetary oxygen levels and reduction of CO 2 levels, which resulted in the late Paleozoic icehouse.

Its former name, the Karoo glaciation, was named after the glacial tills found in the Karoo region of South Africa.

There were extensive polar ice caps at intervals from to million years ago in South Africa during the Carboniferous and early Permian Periods.

Correlatives are known from Argentina, also in the center of the ancient supercontinent Gondwanaland. Since then, the world has seen cycles of glaciation with ice sheets advancing and retreating on 40, and ,year time scales called glacial periods , glacials or glacial advances, and interglacial periods, interglacials or glacial retreats.

The earth is currently in an interglacial, and the last glacial period ended about 10, years ago. All that remains of the continental ice sheets are the Greenland and Antarctic ice sheets and smaller glaciers such as on Baffin Island.

The definition of the Quaternary as beginning 2. The term Late Cenozoic Ice Age is used to include this early phase.

Ice ages can be further divided by location and time; for example, the names Riss ,—, years bp and Würm 70,—10, years bp refer specifically to glaciation in the Alpine region.

The maximum extent of the ice is not maintained for the full interval. The scouring action of each glaciation tends to remove most of the evidence of prior ice sheets almost completely, except in regions where the later sheet does not achieve full coverage.

Within the ice ages or at least within the current one , more temperate and more severe periods occur. The colder periods are called glacial periods , the warmer periods interglacials , such as the Eemian Stage.

Glacials are characterized by cooler and drier climates over most of the earth and large land and sea ice masses extending outward from the poles.

Mountain glaciers in otherwise unglaciated areas extend to lower elevations due to a lower snow line. Sea levels drop due to the removal of large volumes of water above sea level in the icecaps.

There is evidence that ocean circulation patterns are disrupted by glaciations. Since the earth has significant continental glaciation in the Arctic and Antarctic, we are currently in a glacial minimum of a glaciation.

Such a period between glacial maxima is known as an interglacial. The glacials and interglacials also coincided with changes in Earth's orbit called Milankovitch cycles.

The earth has been in an interglacial period known as the Holocene for around 11, years, [41] and an article in Nature in argues that it might be most analogous to a previous interglacial that lasted 28, years.

Moreover, anthropogenic forcing from increased greenhouse gases is estimated to potentially outweigh the orbital forcing of the Milankovitch cycles for hundreds of thousand of years.

Each glacial period is subject to positive feedback which makes it more severe, and negative feedback which mitigates and in all cases so far eventually ends it.

Ice and snow increase Earth's albedo , i. Hence, when the air temperature decreases, ice and snow fields grow, and this continues until competition with a negative feedback mechanism forces the system to an equilibrium.

Also, the reduction in forests caused by the ice's expansion increases albedo. Another theory proposed by Ewing and Donn in [44] hypothesized that an ice-free Arctic Ocean leads to increased snowfall at high latitudes.

When low-temperature ice covers the Arctic Ocean there is little evaporation or sublimation and the polar regions are quite dry in terms of precipitation, comparable to the amount found in mid-latitude deserts.

This low precipitation allows high-latitude snowfalls to melt during the summer. An ice-free Arctic Ocean absorbs solar radiation during the long summer days, and evaporates more water into the Arctic atmosphere.

With higher precipitation, portions of this snow may not melt during the summer and so glacial ice can form at lower altitudes and more southerly latitudes, reducing the temperatures over land by increased albedo as noted above.

Furthermore, under this hypothesis the lack of oceanic pack ice allows increased exchange of waters between the Arctic and the North Atlantic Oceans, warming the Arctic and cooling the North Atlantic.

Current projected consequences of global warming include a largely ice-free Arctic Ocean within 5—20 years, see Arctic shrinkage.

Additional fresh water flowing into the North Atlantic during a warming cycle may also reduce the global ocean water circulation.

Such a reduction by reducing the effects of the Gulf Stream would have a cooling effect on northern Europe, which in turn would lead to increased low-latitude snow retention during the summer.

It has also been suggested that during an extensive glacial, glaciers may move through the Gulf of Saint Lawrence , extending into the North Atlantic Ocean far enough to block the Gulf Stream.

Ice sheets that form during glaciations cause erosion of the land beneath them. After some time, this will reduce land above sea level and thus diminish the amount of space on which ice sheets can form.

This mitigates the albedo feedback, as does the lowering in sea level that accompanies the formation of ice sheets.

Another factor is the increased aridity occurring with glacial maxima, which reduces the precipitation available to maintain glaciation.

The glacial retreat induced by this or any other process can be amplified by similar inverse positive feedbacks as for glacial advances.

According to research published in Nature Geoscience , human emissions of carbon dioxide CO 2 will defer the next ice age. Researchers used data on Earth's orbit to find the historical warm interglacial period that looks most like the current one and from this have predicted that the next ice age would usually begin within 1, years.

They go on to say that emissions have been so high that it will not. The causes of ice ages are not fully understood for either the large-scale ice age periods or the smaller ebb and flow of glacial—interglacial periods within an ice age.

The consensus is that several factors are important: atmospheric composition , such as the concentrations of carbon dioxide and methane the specific levels of the previously mentioned gases are now able to be seen with the new ice core samples from EPICA Dome C in Antarctica over the past , years ; changes in the earth's orbit around the Sun known as Milankovitch cycles ; the motion of tectonic plates resulting in changes in the relative location and amount of continental and oceanic crust on the earth's surface, which affect wind and ocean currents ; variations in solar output ; the orbital dynamics of the Earth—Moon system; the impact of relatively large meteorites and volcanism including eruptions of supervolcanoes.

Some of these factors influence each other. For example, changes in Earth's atmospheric composition especially the concentrations of greenhouse gases may alter the climate, while climate change itself can change the atmospheric composition for example by changing the rate at which weathering removes CO 2.

Maureen Raymo , William Ruddiman and others propose that the Tibetan and Colorado Plateaus are immense CO 2 "scrubbers" with a capacity to remove enough CO 2 from the global atmosphere to be a significant causal factor of the 40 million year Cenozoic Cooling trend.

They further claim that approximately half of their uplift and CO 2 "scrubbing" capacity occurred in the past 10 million years.

There is evidence that greenhouse gas levels fell at the start of ice ages and rose during the retreat of the ice sheets, but it is difficult to establish cause and effect see the notes above on the role of weathering.

Greenhouse gas levels may also have been affected by other factors which have been proposed as causes of ice ages, such as the movement of continents and volcanism.

The Snowball Earth hypothesis maintains that the severe freezing in the late Proterozoic was ended by an increase in CO 2 levels in the atmosphere, mainly from volcanoes, and some supporters of Snowball Earth argue that it was caused in the first place by a reduction in atmospheric CO 2.

The hypothesis also warns of future Snowball Earths. In , further evidence was provided that changes in solar insolation provide the initial trigger for the earth to warm after an Ice Age, with secondary factors like increases in greenhouse gases accounting for the magnitude of the change.

The geological record appears to show that ice ages start when the continents are in positions which block or reduce the flow of warm water from the equator to the poles and thus allow ice sheets to form.

The ice sheets increase Earth's reflectivity and thus reduce the absorption of solar radiation. With less radiation absorbed the atmosphere cools; the cooling allows the ice sheets to grow, which further increases reflectivity in a positive feedback loop.

The ice age continues until the reduction in weathering causes an increase in the greenhouse effect. There are three main contributors from the layout of the continents that obstruct the movement of warm water to the poles: [52].

Since today's Earth has a continent over the South Pole and an almost land-locked ocean over the North Pole, geologists believe that Earth will continue to experience glacial periods in the geologically near future.

Some scientists believe that the Himalayas are a major factor in the current ice age, because these mountains have increased Earth's total rainfall and therefore the rate at which carbon dioxide is washed out of the atmosphere, decreasing the greenhouse effect.

The history of the Himalayas broadly fits the long-term decrease in Earth's average temperature since the mid-Eocene , 40 million years ago.

Another important contribution to ancient climate regimes is the variation of ocean currents , which are modified by continent position, sea levels and salinity, as well as other factors.

They have the ability to cool e. The closing of the Isthmus of Panama about 3 million years ago may have ushered in the present period of strong glaciation over North America by ending the exchange of water between the tropical Atlantic and Pacific Oceans.

Analyses suggest that ocean current fluctuations can adequately account for recent glacial oscillations. This realigned the thermohaline circulation in the Atlantic, increasing heat transport into the Arctic, which melted the polar ice accumulation and reduced other continental ice sheets.

The release of water raised sea levels again, restoring the ingress of colder water from the Pacific with an accompanying shift to northern hemisphere ice accumulation.

According to Kuhle, the plate-tectonic uplift of Tibet past the snow-line has led to a surface of c. The reflection of energy into space resulted in a global cooling, triggering the Pleistocene Ice Age.

Because this highland is at a subtropical latitude, with 4 to 5 times the insolation of high-latitude areas, what would be Earth's strongest heating surface has turned into a cooling surface.

Kuhle explains the interglacial periods by the ,year cycle of radiation changes due to variations in Earth's orbit. This comparatively insignificant warming, when combined with the lowering of the Nordic inland ice areas and Tibet due to the weight of the superimposed ice-load, has led to the repeated complete thawing of the inland ice areas.

The Milankovitch cycles are a set of cyclic variations in characteristics of the Earth's orbit around the Sun. Each cycle has a different length, so at some times their effects reinforce each other and at other times they partially cancel each other.

There is strong evidence that the Milankovitch cycles affect the occurrence of glacial and interglacial periods within an ice age.

The present ice age is the most studied and best understood, particularly the last , years, since this is the period covered by ice cores that record atmospheric composition and proxies for temperature and ice volume.

The combined effects of the changing distance to the Sun, the precession of the Earth's axis , and the changing tilt of the Earth's axis redistribute the sunlight received by the Earth.

Of particular importance are changes in the tilt of the Earth's axis, which affect the intensity of seasons. It is widely believed that ice sheets advance when summers become too cool to melt all of the accumulated snowfall from the previous winter.

Some believe that the strength of the orbital forcing is too small to trigger glaciations, but feedback mechanisms like CO 2 may explain this mismatch.

While Milankovitch forcing predicts that cyclic changes in the Earth's orbital elements can be expressed in the glaciation record, additional explanations are necessary to explain which cycles are observed to be most important in the timing of glacial—interglacial periods.

In particular, during the last , years, the dominant period of glacial—interglacial oscillation has been , years, which corresponds to changes in Earth's orbital eccentricity and orbital inclination.

Yet this is by far the weakest of the three frequencies predicted by Milankovitch. During the period 3.

The reasons for dominance of one frequency versus another are poorly understood and an active area of current research, but the answer probably relates to some form of resonance in the Earth's climate system.

Recent work suggests that the K year cycle dominates due to increased southern-pole sea-ice increasing total solar reflectivity. The "traditional" Milankovitch explanation struggles to explain the dominance of the ,year cycle over the last 8 cycles.

Richard A. Muller , Gordon J. MacDonald , [61] [62] [63] and others have pointed out that those calculations are for a two-dimensional orbit of Earth but the three-dimensional orbit also has a ,year cycle of orbital inclination.

They proposed that these variations in orbital inclination lead to variations in insolation, as the Earth moves in and out of known dust bands in the solar system.

Although this is a different mechanism to the traditional view, the "predicted" periods over the last , years are nearly the same. Another worker, William Ruddiman , has suggested a model that explains the ,year cycle by the modulating effect of eccentricity weak ,year cycle on precession 26,year cycle combined with greenhouse gas feedbacks in the 41, and 26,year cycles.

Yet another theory has been advanced by Peter Huybers who argued that the 41,year cycle has always been dominant, but that the Earth has entered a mode of climate behavior where only the second or third cycle triggers an ice age.

This would imply that the ,year periodicity is really an illusion created by averaging together cycles lasting 80, and , years.

The jumps are induced by the orbital forcing, while in the early Pleistocene the 41,year glacial cycles resulted from jumps between only two climate states.

A dynamical model explaining this behavior was proposed by Peter Ditlevsen. At times during the paleoclimate, carbon dioxide levels were two or three times greater than today.

Volcanoes and movements in continental plates contributed to high amounts of CO 2 in the atmosphere. Carbon dioxide from volcanoes probably contributed to periods with highest overall temperatures.

The current geological period, the Quaternary , which began about 2. The last cold episode of the last glacial period ended about 10, years ago.

The major glacial stages of the current ice age in North America are the Illinoian , Eemian and Wisconsin glaciation. The use of the Nebraskan, Afton, Kansan, and Yarmouthian stages to subdivide the ice age in North America has been discontinued by Quaternary geologists and geomorphologists.

These stages have all been merged into the Pre-Illinoian in the s. During the most recent North American glaciation, during the latter part of the Last Glacial Maximum 26, to 13, years ago , ice sheets extended to about 45th parallel north.

These sheets were 3 to 4 kilometres 1. This Wisconsin glaciation left widespread impacts on the North American landscape.

The Great Lakes and the Finger Lakes were carved by ice deepening old valleys. Most of the lakes in Minnesota and Wisconsin were gouged out by glaciers and later filled with glacial meltwaters.

The old Teays River drainage system was radically altered and largely reshaped into the Ohio River drainage system.

Other rivers were dammed and diverted to new channels, such as Niagara Falls , which formed a dramatic waterfall and gorge, when the waterflow encountered a limestone escarpment.

The area from Long Island to Nantucket, Massachusetts was formed from glacial till , and the plethora of lakes on the Canadian Shield in northern Canada can be almost entirely attributed to the action of the ice.

As the ice retreated and the rock dust dried, winds carried the material hundreds of miles, forming beds of loess many dozens of feet thick in the Missouri Valley.

Post-glacial rebound continues to reshape the Great Lakes and other areas formerly under the weight of the ice sheets. The Driftless Area , a portion of western and southwestern Wisconsin along with parts of adjacent Minnesota , Iowa , and Illinois , was not covered by glaciers.

A specially interesting climatic change during glacial times has taken place in the semi-arid Andes. Beside the expected cooling down in comparison with the current climate, a significant precipitation change happened here.

From this follows that—beside of an annual depression of temperature about c. Accordingly, at glacial times the humid climatic belt that today is situated several latitude degrees further to the S, was shifted much further to the N.

Although the last glacial period ended more than 8, years ago, its effects can still be felt today. The erratic boulders , till , drumlins , eskers , fjords , kettle lakes , moraines , cirques , horns , etc.

The weight of the ice sheets was so great that they deformed the Earth's crust and mantle. After the ice sheets melted, the ice-covered land rebounded.

During glaciation, water was taken from the oceans to form the ice at high latitudes, thus global sea level dropped by about meters, exposing the continental shelves and forming land-bridges between land-masses for animals to migrate.

During deglaciation , the melted ice-water returned to the oceans, causing sea level to rise. This process can cause sudden shifts in coastlines and hydration systems resulting in newly submerged lands, emerging lands, collapsed ice dams resulting in salination of lakes, new ice dams creating vast areas of freshwater, and a general alteration in regional weather patterns on a large but temporary scale.

It can even cause temporary reglaciation. This type of chaotic pattern of rapidly changing land, ice, saltwater and freshwater has been proposed as the likely model for the Baltic and Scandinavian regions, as well as much of central North America at the end of the last glacial maximum, with the present-day coastlines only being achieved in the last few millennia of prehistory.

Also, the effect of elevation on Scandinavia submerged a vast continental plain that had existed under much of what is now the North Sea, connecting the British Isles to Continental Europe.

The redistribution of ice-water on the surface of the Earth and the flow of mantle rocks causes changes in the gravitational field as well as changes to the distribution of the moment of inertia of the Earth.

These changes to the moment of inertia result in a change in the angular velocity , axis , and wobble of the Earth's rotation. The weight of the redistributed surface mass loaded the lithosphere , caused it to flex and also induced stress within the Earth.

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