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    Schimper then assumed that there must have been global times of obliteration "Verödungszeiten" with a cold climate and frozen water.

    Schimper, de Charpentier and possibly Venetz convinced Agassiz that there had been a time of glaciation.

    They mainly drew upon the preceding works of Venetz, de Charpentier and on their own fieldwork. Agassiz appears to have been already familiar with Bernhardi's paper at that time.

    The audience was very critical and some opposed to the new theory because it contradicted the established opinions on climatic history. Most contemporary scientists thought that the Earth had been gradually cooling down since its birth as a molten globe.

    In order to overcome this rejection, Agassiz embarked on geological fieldwork. De Charpentier felt that Agassiz should have given him precedence as it was he who had introduced Agassiz to in-depth glacial research.

    All together, it took several decades until the ice age theory was fully accepted by scientists. This happened on an international scale in the second half of the s following the work of James Croll , including the publication of Climate and Time, in Their Geological Relations in , which provided a credible explanation for the causes of ice ages.

    Geological evidence for ice ages comes in various forms, including rock scouring and scratching, glacial moraines , drumlins , valley cutting, and the deposition of till or tillites and glacial erratics.

    Successive glaciations tend to distort and erase the geological evidence, making it difficult to interpret. Furthermore, this evidence was difficult to date exactly; early theories assumed that the glacials were short compared to the long interglacials.

    The advent of sediment and ice cores revealed the true situation: It took some time for the current theory to be worked out.

    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 [30] 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. 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, [34] 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 Karoo Ice Age.

    It is named after the glacial tills found in the Karoo region of South Africa, where evidence for this ice age was first clearly identified.

    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, [37] 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 might outweigh orbital forcing for as long as intensive use of fossil fuels continues.

    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 [41] 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: 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.

    There is considerable evidence that over the very recent period of the last — years, the sharp increases in human activity, especially the burning of fossil fuels , has caused the parallel sharp and accelerating increase in atmospheric greenhouse gases which trap the sun's heat.

    The consensus theory of the scientific community is that the resulting greenhouse effect is a principal cause of the increase in global warming which has occurred over the same period, and a chief contributor to the accelerated melting of the remaining glaciers and polar ice.

    A investigation finds that dinosaurs released methane through digestion in a similar amount to humanity's current methane release, which "could have been a key factor" to the very warm climate million years ago.

    William Ruddiman has proposed the early anthropocene hypothesis, according to which the anthropocene era, as some people call the most recent period in the earth's history when the activities of the human species first began to have a significant global impact on the earth's climate and ecosystems, did not begin in the 18th century with the advent of the Industrial Era, but dates back to 8, years ago, due to intense farming activities of our early agrarian ancestors.

    It was at that time that atmospheric greenhouse gas concentrations stopped following the periodic pattern of the Milankovitch cycles.

    In his overdue-glaciation hypothesis Ruddiman states that an incipient glacial would probably have begun several thousand years ago, but the arrival of that scheduled glacial was forestalled by the activities of early farmers.

    At a meeting of the American Geophysical Union December 17, , scientists detailed evidence in support of the controversial idea that the introduction of large-scale rice agriculture in Asia, coupled with extensive deforestation in Europe began to alter world climate by pumping significant amounts of greenhouse gases into the atmosphere over the last 1, years.

    In turn, a warmer atmosphere heated the oceans making them much less efficient storehouses of carbon dioxide and reinforcing global warming, possibly forestalling the onset of a new glacial age.

    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: 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.

    Muller , Gordon J. MacDonald , [59] [60] [61] 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.

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