125-399: Seisonacea (for order) Seisonidae is a family of rotifers , found on the gills of Nebalia , a marine crustacean . Peculiar among rotifers, males and females are both present and equal in size. Males and females are similar with paired gonads . It is considered to have diverged from the other rotifers early on, and in one treatment is placed in a separate class Seisonoidea . They have
250-428: A Neo-Latin word meaning ' wheel -bearer' due to the corona around the mouth that in concerted sequential motion resembles a wheel (although the organ does not actually rotate). Rotifers have bilateral symmetry and a variety of different shapes. The body of a rotifer is divided into a head, trunk, and foot, and is typically somewhat cylindrical. There is a well-developed cuticle , which may be thick and rigid, giving
375-454: A climate change feedback . The emissions from thawing permafrost will have a sufficient impact on the climate to impact global carbon budgets . It is difficult to accurately predict how much greenhouse gases the permafrost releases because of the different thaw processes are still uncertain. There is widespread agreement that the emissions will be smaller than human-caused emissions and not large enough to result in runaway warming . Instead,
500-628: A penis . The gonopore is homologous to the cloaca of females, but in most species has no connection to the vestigial digestive system, which lacks an anus . In the genus Asplanchna also the females lacks an anus, but have kept the cloacal opening for excretion and the release of eggs. The phylum Rotifera encloses three classes that reproduce by three different mechanisms: Seisonidea only reproduce sexually; Bdelloidea reproduce exclusively by asexual parthenogenesis; Monogononta reproduce alternating these two mechanisms ("cyclical parthenogenesis" or "heterogony"). Parthenogenesis (amictic phase) dominates
625-407: A 2022 review concluded that every 1 °C (1.8 °F) of global warming would cause 0.04 °C (0.072 °F) and 0.11 °C (0.20 °F) from abrupt thaw by the year 2100 and 2300. Around 4 °C (7.2 °F) of global warming, abrupt (around 50 years) and widespread collapse of permafrost areas could occur, resulting in an additional warming of 0.2–0.4 °C (0.36–0.72 °F). As
750-547: A bdelloid rotifer, Adineta vaga , was reported to be around 244 Mb. The genomes of Monogononts seem to be significantly smaller than those of Bdelloids. In Monogononta the nuclear DNA content (2C) in eight different species of four different genera ranged almost fourfold, from 0.12 to 0.46 pg. Haploid "1C" genome sizes in Brachionus species range at least from 0.056 to 0.416 pg. Permafrost Permafrost (from perma- ' permanent ' and frost )
875-399: A characteristic chewing pharynx (called the mastax ), sometimes via a ciliated tube, and sometimes directly. The pharynx has a powerful muscular wall and contains tiny, calcified, jaw-like structures called trophi , which are the only fossilizable parts of a rotifer. The shape of the trophi varies between different species, depending partly on the nature of their diet. In suspension feeders,
1000-544: A climate where the mean annual soil surface temperature is between −5 and 0 °C (23 and 32 °F). In the moist-wintered areas mentioned before, there may not even be discontinuous permafrost down to −2 °C (28 °F). Discontinuous permafrost is often further divided into extensive discontinuous permafrost, where permafrost covers between 50 and 90 percent of the landscape and is usually found in areas with mean annual temperatures between −2 and −4 °C (28 and 25 °F), and sporadic permafrost, where permafrost cover
1125-440: A few hours. Bdelloids can survive the dry state for long periods, with the longest well-documented dormancy being nine years. Rotifers can also undergo other forms of cryptobiosis, notably cryobiosis which results from decreased temperatures. In 2021, researchers collected samples from remote Arctic locations containing rotifers which when thawed revealed living specimens around 24,000 years old. While in other anhydrobionts, such as
1250-524: A fifth of both the industrial and the polluted sites (1000 and 2200–4800) are expected to start thawing in the future even if the warming does not increase from its 2020 levels. Only about 3% more sites would start thawing between now and 2050 under the climate change scenario consistent with the Paris Agreement goals, RCP2.6 , but by 2100, about 1100 more industrial facilities and 3500 to 5200 contaminated sites are expected to start thawing even then. Under
1375-541: A further $ 1.32 billion. In particular, fewer than 20% of railways would be at high risk by 2100 under 1.5 °C (2.7 °F), yet this increases to 60% at 2 °C (3.6 °F), while under SSP5-8.5, this level of risk is met by mid-century. For much of the 20th century, it was believed that permafrost would "indefinitely" preserve anything buried there, and this made deep permafrost areas popular locations for hazardous waste disposal. In places like Canada's Prudhoe Bay oil field, procedures were developed documenting
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#17330845181411500-455: A large and elongate body with reduced corona. Their muscular system is similar to that of other rotifers: they have longitudinal muscles as well as open annular muscles. Being attached for most of their life, they are semi-sessile, but are capable of detaching and crawl short distances if required. Feeding has never been observed directly, but the stomach in Seison nebaliae contained bacteria, while
1625-537: A larger clade called Syndermata . In June 2021, biologists reported the restoration of bdelloid rotifers after being frozen for 24,000 years in the Siberian permafrost . Early purported fossils of rotifers have been suggested in Devonian and Permian fossil beds. John Harris first described the rotifers (in particular a bdelloid rotifer ) in 1696 as "an animal like a large maggot which could contract itself into
1750-633: A major climate tipping point in what was known as a clathrate gun hypothesis , but are now no longer believed to play any role in projected climate change. At the Last Glacial Maximum , continuous permafrost covered a much greater area than it does today, covering all of ice-free Europe south to about Szeged (southeastern Hungary ) and the Sea of Azov (then dry land) and East Asia south to present-day Changchun and Abashiri . In North America, only an extremely narrow belt of permafrost existed south of
1875-524: A major foodsource and with many species also contributing to the decomposition of soil organic matter. Most species of the rotifers are cosmopolitan , but there are also some endemic species, like Cephalodella vittata to Lake Baikal . Recent barcoding evidence, however, suggests that some 'cosmopolitan' species, such as Brachionus plicatilis , B. calyciflorus , Lecane bulla , among others, are actually species complexes . In some recent treatments, rotifers are placed with acanthocephalans in
2000-416: A mean annual temperature of −2 °C (28.4 °F) or below. In the coldest regions, the depth of continuous permafrost can exceed 1,400 m (4,600 ft). It typically exists beneath the so-called active layer , which freezes and thaws annually, and so can support plant growth, as the roots can only take hold in the soil that's thawed. Active layer thickness is measured during its maximum extent at
2125-531: A minimum thickness of at least 2 m and a short diameter of at least 10 m. First recorded North American observations of this phenomenon were by European scientists at Canning River (Alaska) in 1919. Russian literature provides an earlier date of 1735 and 1739 during the Great North Expedition by P. Lassinius and Khariton Laptev , respectively. Russian investigators including I.A. Lopatin, B. Khegbomov, S. Taber and G. Beskow had also formulated
2250-543: A permafrost zone or region. This is because only slightly more than half of this area is defined as a continuous permafrost zone, where 90%–100% of the land is underlain by permafrost. Around 20% is instead defined as discontinuous permafrost, where the coverage is between 50% and 90%. Finally, the remaining <30% of permafrost regions consists of areas with 10%–50% coverage, which are defined as sporadic permafrost zones, and some areas that have isolated patches of permafrost covering 10% or less of their area. Most of this area
2375-445: A recessive allele. Resting eggs enclose an embryo encysted in a three-layered shell that protects it from external stressors. They are able to remain dormant for several decades and can resist adverse periods (e.g., pond desiccation or presence of antagonists). When favourable conditions return and after an obligatory period of diapause which varies among species, resting eggs hatch releasing diploid amictic females that enter into
2500-400: A series of tube-like secretions with a highly filamentous framework. This is highly suggestive of a glycosaminoglycan structure- proteins with negatively charged polysaccharide chains forming proteoglycan molecules. These molecules are standard in vertebrate and invertebrate gelatins such as mucus . Despite recent advancements in understanding RCO organ and secretion ultrastructure,
2625-404: A short intestine that terminates in a cloaca on the posterior dorsal surface of the animal. Up to seven salivary glands are present in some species, emptying to the mouth in front of the oesophagus, while the stomach is associated with two gastric glands that produce digestive enzymes . A pair of protonephridia open into a bladder that drains into the cloaca. These organs expel water from
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#17330845181412750-436: A spherical figure and then stretch itself out again; the end of its tail appeared with a forceps like that of an earwig ". In 1702, Antonie van Leeuwenhoek gave a detailed description of Rotifer vulgaris and subsequently described Melicerta ringens and other species. He was also the first to publish observations of the revivification of certain species after drying. Other forms were described by other observers, but it
2875-500: A substance that probably represents hemolymph of the Nebalia host was found in the stomach of Paraseison annulatus . The latter prefer to settle beneath the carapace on the gills of the host's legs, and the former is usually found on the host's carapase, trunk or legs. Their host often lives in tidal puddles with decomposing algae for a limited period of time, with oxygen content so low it sometimes reaches anoxia, which doesn't seem to bother
3000-605: A year. In 2006, the cost of adapting Inuvialuit homes to permafrost thaw was estimated at $ 208/m if they were built at pile foundations, and $ 1,000/m if they didn't. At the time, the average area of a residential building in the territory was around 100 m . Thaw-induced damage is also unlikely to be covered by home insurance , and to address this reality, territorial government currently funds Contributing Assistance for Repairs and Enhancements (CARE) and Securing Assistance for Emergencies (SAFE) programs, which provide long- and short-term forgivable loans to help homeowners adapt. It
3125-517: Is soil or underwater sediment which continuously remains below 0 °C (32 °F) for two years or more: the oldest permafrost had been continuously frozen for around 700,000 years. Whilst the shallowest permafrost has a vertical extent of below a meter (3 ft), the deepest is greater than 1,500 m (4,900 ft). Similarly, the area of individual permafrost zones may be limited to narrow mountain summits or extend across vast Arctic regions. The ground beneath glaciers and ice sheets
3250-534: Is already considered "warm" permafrost, making it particularly unstable. Qinghai–Tibet Plateau has a population of over 10 million people – double the population of permafrost regions in the Arctic – and over 1 million m of buildings are located in its permafrost area, as well as 2,631 km of power lines , and 580 km of railways. There are also 9,389 km of roads, and around 30% are already sustaining damage from permafrost thaw. Estimates suggest that under
3375-655: Is also located in high mountain regions, with the Tibetan Plateau being a prominent example. Only a minority of permafrost exists in the Southern Hemisphere , where it is consigned to mountain slopes like in the Andes of Patagonia , the Southern Alps of New Zealand, or the highest mountains of Antarctica . Permafrost contains large amounts of dead biomass that have accumulated throughout millennia without having had
3500-473: Is also possible for subsurface alpine permafrost to be covered by warmer, vegetation-supporting soil. Alpine permafrost is particularly difficult to study, and systematic research efforts did not begin until the 1970s. Consequently, there remain uncertainties about its geography. As recently as 2009, permafrost had been discovered in a new area – Africa's highest peak, Mount Kilimanjaro (4,700 m (15,400 ft) above sea level and approximately 3° south of
3625-419: Is associated with a wide range of issues, and International Permafrost Association (IPA) exists to help address them. It convenes International Permafrost Conferences and maintains Global Terrestrial Network for Permafrost , which undertakes special projects such as preparing databases, maps, bibliographies, and glossaries, and coordinates international field programmes and networks. As recent warming deepens
3750-444: Is because carbon can be released through either aerobic or anaerobic respiration , which results in carbon dioxide (CO 2 ) or methane (CH 4 ) emissions, respectively. While methane lasts less than 12 years in the atmosphere, its global warming potential is around 80 times larger than that of CO 2 over a 20-year period and about 28 times larger over a 100-year period. While only a small fraction of permafrost carbon will enter
3875-429: Is decreasing as well; as of 2019, ~97% of permafrost under Arctic ice shelves is becoming warmer and thinner. Based on high agreement across model projections, fundamental process understanding, and paleoclimate evidence, it is virtually certain that permafrost extent and volume will continue to shrink as the global climate warms, with the extent of the losses determined by the magnitude of warming. Permafrost thaw
Seisonidae - Misplaced Pages Continue
4000-429: Is different and found on a different chromosome excluding the possibility of homozygous sexual reproduction . Rotifers eat particulate organic detritus, dead bacteria, algae, and protozoans. They eat particles up to 10 micrometres in size. Like crustaceans , rotifers contribute to nutrient recycling. For this reason, they are used in fish tanks to help clean the water, to prevent clouds of waste matter. Rotifers affect
4125-497: Is difficult because the heat of the building (or pipeline ) can spread to the soil, thawing it. As ice content turns to water, the ground's ability to provide structural support is weakened, until the building is destabilized. For instance, during the construction of the Trans-Siberian Railway , a steam engine factory complex built in 1901 began to crumble within a month of operations for these reasons. Additionally, there
4250-620: Is expected that cumulative greenhouse gas emissions from permafrost thaw will be smaller than the cumulative anthropogenic emissions, yet still substantial on a global scale, with some experts comparing them to emissions caused by deforestation . The IPCC Sixth Assessment Report estimates that carbon dioxide and methane released from permafrost could amount to the equivalent of 14–175 billion tonnes of carbon dioxide per 1 °C (1.8 °F) of warming. For comparison, by 2019, annual anthropogenic emissions of carbon dioxide alone stood around 40 billion tonnes. A major review published in
4375-420: Is expected to be lost "over decades and centuries". The exact amount of carbon that will be released due to warming in a given permafrost area depends on depth of thaw, carbon content within the thawed soil, physical changes to the environment, and microbial and vegetation activity in the soil. Notably, estimates of carbon release alone do not fully represent the impact of permafrost thaw on climate change. This
4500-435: Is expected to thaw, affecting all their inhabitants (currently 3.3 million people). Consequently, a wide range of infrastructure in permafrost areas is threatened by the thaw. By 2050, it's estimated that nearly 70% of global infrastructure located in the permafrost areas would be at high risk of permafrost thaw, including 30–50% of "critical" infrastructure. The associated costs could reach tens of billions of dollars by
4625-489: Is found in Siberia, northern Canada, Alaska and Greenland. Beneath the active layer annual temperature swings of permafrost become smaller with depth. The greatest depth of permafrost occurs right before the point where geothermal heat maintains a temperature above freezing. Above that bottom limit there may be permafrost with a consistent annual temperature—"isothermal permafrost". Permafrost typically forms in any climate where
4750-427: Is further modified, with the upper band splitting into two rotating wheels, raised up on a pedestal projecting from the upper surface of the head. The trunk forms the major part of the body, and encloses most of the internal organs. The foot projects from the rear of the trunk, and is usually much narrower, giving the appearance of a tail. The cuticle over the foot often forms rings, making it appear segmented, although
4875-517: Is generated by radioactive decay of unstable isotopes and flows to the surface by conduction at a rate of ~47 terawatts (TW). Away from tectonic plate boundaries, this is equivalent to an average heat flow of 25–30 °C/km (124–139 °F/mi) near the surface. When the ice content of a permafrost exceeds 250 percent (ice to dry soil by mass) it is classified as massive ice. Massive ice bodies can range in composition, in every conceivable gradation from icy mud to pure ice. Massive icy beds have
5000-478: Is internal. The male either inserts his penis into the female's cloaca or uses it to penetrate her skin, injecting the sperm into the body cavity. The egg secretes a shell, and is attached either to the substratum, nearby plants, or the female's own body. A few species, such as members of the Rotaria , are ovoviviparous , retaining the eggs inside their body until they hatch. Most species hatch as miniature versions of
5125-561: Is less than 50 percent of the landscape and typically occurs at mean annual temperatures between 0 and −2 °C (32 and 28 °F). In soil science, the sporadic permafrost zone is abbreviated SPZ and the extensive discontinuous permafrost zone DPZ . Exceptions occur in un-glaciated Siberia and Alaska where the present depth of permafrost is a relic of climatic conditions during glacial ages where winters were up to 11 °C (20 °F) colder than those of today. At mean annual soil surface temperatures below −5 °C (23 °F)
Seisonidae - Misplaced Pages Continue
5250-462: Is no groundwater available in an area underlain with permafrost. Any substantial settlement or installation needs to make some alternative arrangement to obtain water. A common solution is placing foundations on wood piles , a technique pioneered by Soviet engineer Mikhail Kim in Norilsk. However, warming-induced change of friction on the piles can still cause movement through creep , even as
5375-509: Is not usually defined as permafrost, so on land, permafrost is generally located beneath a so-called active layer of soil which freezes and thaws depending on the season. Around 15% of the Northern Hemisphere or 11% of the global surface is underlain by permafrost, covering a total area of around 18 million km (6.9 million sq mi). This includes large areas of Alaska , Canada , Greenland , and Siberia . It
5500-454: Is possible that in the future, mandatory relocation would instead take place as the cheaper option. However, it would effectively tear the local Inuit away from their ancestral homelands. Right now, their average personal income is only half that of the median NWT resident, meaning that adaptation costs are already disproportionate for them. By 2022, up to 80% of buildings in some Northern Russia cities had already experienced damage. By 2050,
5625-516: Is related to the tundra. Alpine permafrost also occurred in the Drakensberg during glacial maxima above about 3,000 metres (9,840 ft). Permafrost extends to a base depth where geothermal heat from the Earth and the mean annual temperature at the surface achieve an equilibrium temperature of 0 °C (32 °F). This base depth of permafrost can vary wildly – it is less than a meter (3 ft) in
5750-595: Is subdivided into intrusive, injection and segregational ice. The latter is the dominant type, formed after crystallizational differentiation in wet sediments , which occurs when water migrates to the freezing front under the influence of van der Waals forces . This is a slow process, which primarily occurs in silts with salinity less than 20% of seawater : silt sediments with higher salinity and clay sediments instead have water movement prior to ice formation dominated by rheological processes. Consequently, it takes between 1 and 1000 years to form intrasedimental ice in
5875-586: Is the Monogononta, with about 1,500 species, followed by the Bdelloidea, with about 350 species. There are only two known genera with three species of Seisonidea. The Acanthocephala , previously considered to be a separate phylum, have been demonstrated to be modified rotifers. The exact relationship to other members of the phylum has not yet been resolved. One possibility is that the Acanthocephala are closer to
6000-433: Is the ongoing "greening" of the Arctic. As climate change warms the air and the soil, the region becomes more hospitable to plants, including larger shrubs and trees which could not survive there before. Thus, the Arctic is losing more and more of its tundra biomes, yet it gains more plants, which proceed to absorb more carbon. Some of the emissions caused by permafrost thaw will be offset by this increased plant growth, but
6125-525: Is unknown. Notable sites with known ancient ice deposits include Yenisei River valley in Siberia , Russia as well as Banks and Bylot Island in Canada's Nunavut and Northwest Territories . Some of the buried ice sheet remnants are known to host thermokarst lakes . Intrasedimental or constitutional ice has been widely observed and studied across Canada. It forms when subterranean waters freeze in place, and
6250-459: The Mongolian Plateau are the only areas where the average active layer is deeper than 600 centimetres (20 ft), with the record of 10 metres (33 ft). The border between active layer and permafrost itself is sometimes called permafrost table. Around 15% of Northern Hemisphere land that is not completely covered by ice is directly underlain by permafrost; 22% is defined as part of
6375-694: The Northern and Southern Hemisphere are cold enough to support perennially frozen ground: some of the best-known examples include the Canadian Rockies , the European Alps , Himalaya and the Tien Shan . In general, it has been found that extensive alpine permafrost requires mean annual air temperature of −3 °C (27 °F), though this can vary depending on local topography , and some mountain areas are known to support permafrost at −1 °C (30 °F). It
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#17330845181416500-460: The Pleistocene . Base depth is affected by the underlying geology, and particularly by thermal conductivity , which is lower for permafrost in soil than in bedrock . Lower conductivity leaves permafrost less affected by the geothermal gradient , which is the rate of increasing temperature with respect to increasing depth in the Earth's interior. It occurs as the Earth's internal thermal energy
6625-419: The anterior end of the gland where they undergo homotypic fusion to create larger granules with numerous "mesh-like" contents. These contents gradually fuse into tubular secretions that accumulate in the reservoir, awaiting secretion. Cross-striated longitudinal muscles form a partial sleeve around the reservoir and may function to squeeze the secretions through the gland's duct that often penetrates through
6750-724: The brine shrimp , this desiccation tolerance is thought to be linked to the production of trehalose , a non-reducing disaccharide ( sugar ), bdelloids apparently cannot synthesise trehalose. In bdelloids, a major cause of the resistance to desiccation, as well as resistance to ionizing radiation, is a highly efficient mechanism for repairing the DNA double-strand breaks induced by these agents. This repair mechanism likely involves mitotic recombination between homologous DNA regions. Rotifers fall prey to many animals, such as copepods , fish (e.g. herring , salmon ), bryozoa , comb jellies , jellyfish , starfish , and tardigrades . The genome size of
6875-418: The cloaca . Males do not usually have a functional digestive system, and are therefore short-lived, often being sexually fertile at birth. They have a single testicle and sperm duct , associated with a pair of glandular structures referred to as prostates (unrelated to the vertebrate prostate ). The sperm duct opens into a gonopore at the posterior end of the animal, which is usually modified to form
7000-504: The continental shelves of the polar regions. These areas formed during the last Ice Age , when a larger portion of Earth's water was bound up in ice sheets on land and when sea levels were low. As the ice sheets melted to again become seawater during the Holocene glacial retreat , coastal permafrost became submerged shelves under relatively warm and salty boundary conditions, compared to surface permafrost. Since then, these conditions led to
7125-403: The equator ). In 2014, a collection of regional estimates of alpine permafrost extent had established a global extent of 3,560,000 km (1,370,000 sq mi). Yet, by 2014, alpine permafrost in the Andes has not been fully mapped, although its extent has been modeled to assess the amount of water bound up in these areas. Subsea permafrost occurs beneath the seabed and exists in
7250-408: The ice sheet at about the latitude of New Jersey through southern Iowa and northern Missouri , but permafrost was more extensive in the drier western regions where it extended to the southern border of Idaho and Oregon . In the Southern Hemisphere , there is some evidence for former permafrost from this period in central Otago and Argentine Patagonia , but was probably discontinuous, and
7375-573: The pressure melting point throughout, may have liquid water at the interface with the ground and are therefore free of underlying permafrost. "Fossil" cold anomalies in the geothermal gradient in areas where deep permafrost developed during the Pleistocene persist down to several hundred metres. This is evident from temperature measurements in boreholes in North America and Europe. The below-ground temperature varies less from season to season than
7500-527: The southern hemisphere , most of the equivalent line would fall within the Southern Ocean if there were land there. Most of the Antarctic continent is overlain by glaciers, under which much of the terrain is subject to basal melting . The exposed land of Antarctica is substantially underlain with permafrost, some of which is subject to warming and thawing along the coastline. A range of elevations in both
7625-454: The "appropriate" way to inject waste beneath the permafrost. This means that as of 2023, there are ~4500 industrial facilities in the Arctic permafrost areas which either actively process or store hazardous chemicals. Additionally, there are between 13,000 and 20,000 sites which have been heavily contaminated, 70% of them in Russia, and their pollution is currently trapped in the permafrost. About
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#17330845181417750-415: The 1990s. Between 2000 and 2018, the average active layer thickness had increased from ~127 centimetres (4.17 ft) to ~145 centimetres (4.76 ft), at an average annual rate of ~0.65 centimetres (0.26 in). In Yukon , the zone of continuous permafrost might have moved 100 kilometres (62 mi) poleward since 1899, but accurate records only go back 30 years. The extent of subsea permafrost
7875-452: The Bdelloidea and Monogononta than to the Seisonidea; the corresponding names and relationships are shown in the cladogram below. Seisonida Bdelloidea Monogononta Acanthocephala The Rotifera, strictly speaking, are confined to the Bdelloidea and the Monogononta. Rotifera, Acanthocephala and Seisonida make up a clade called Syndermata. The word rotifer is derived from
8000-899: The Seisonidae. Two genera with total four species belong to Seisonidae: This rotifer -related article is a stub . You can help Misplaced Pages by expanding it . Rotifer The rotifers ( / ˈ r oʊ t ɪ f ər z / , from Latin rota 'wheel' and -fer 'bearing'), sometimes called wheel animals or wheel animalcules , make up a phylum ( Rotifera / r oʊ ˈ t ɪ f ər ə / ) of microscopic and near-microscopic pseudocoelomate animals . They were first described by Rev. John Harris in 1696, and other forms were described by Antonie van Leeuwenhoek in 1703. Most rotifers are around 0.1–0.5 mm (0.0039–0.0197 in) long (although their size can range from 50 μm (0.0020 in) to over 2 mm (0.079 in)), and are common in freshwater environments throughout
8125-496: The United States, while under the scenario of high global warming and worst-case permafrost feedback response, they would approach year 2019 emissions of China. Fewer studies have attempted to describe the impact directly in terms of warming. A 2018 paper estimated that if global warming was limited to 2 °C (3.6 °F), gradual permafrost thaw would add around 0.09 °C (0.16 °F) to global temperatures by 2100, while
8250-412: The active layer subject to permafrost thaw, this exposes formerly stored carbon to biogenic processes which facilitate its entrance into the atmosphere as carbon dioxide and methane . Because carbon emissions from permafrost thaw contribute to the same warming which facilitates the thaw, it is a well-known example of a positive climate change feedback . Permafrost thaw is sometimes included as one of
8375-480: The adult. Sessile species, however, are born as free-swimming larvae , which closely resemble the adults of related free-swimming species. Females grow rapidly, reaching their adult size within a few days, while males typically do not grow in size at all. The life span of monogonont females varies from two days to about three weeks. ' Ancient asexuals': Bdelloid rotifers are assumed to have reproduced without sex for many millions of years. Males are absent within
8500-443: The air temperature, with mean annual temperatures tending to increase with depth due to the geothermal crustal gradient. Thus, if the mean annual air temperature is only slightly below 0 °C (32 °F), permafrost will form only in spots that are sheltered (usually with a northern or southern aspect , in the north and south hemispheres respectively) creating discontinuous permafrost. Usually, permafrost will remain discontinuous in
8625-403: The animal a box-like shape, or flexible, giving the animal a worm-like shape; such rotifers are respectively called loricate and illoricate . Rigid cuticles are often composed of multiple plates, and may bear spines, ridges, or other ornamentation. Their cuticle is nonchitinous and is formed from sclerotized proteins. The two most distinctive features of rotifers (in females of all species) are
8750-567: The annual permafrost emissions are likely comparable with global emissions from deforestation , or to annual emissions of large countries such as Russia , the United States or China . Apart from its climate impact, permafrost thaw brings more risks. Formerly frozen ground often contains enough ice that when it thaws, hydraulic saturation is suddenly exceeded, so the ground shifts substantially and may even collapse outright. Many buildings and other infrastructure were built on permafrost when it
8875-429: The areas where it is shallowest, yet reaches 1,493 m (4,898 ft) in the northern Lena and Yana River basins in Siberia . Calculations indicate that the formation time of permafrost greatly slows past the first several metres. For instance, over half a million years was required to form the deep permafrost underlying Prudhoe Bay, Alaska , a time period extending over several glacial and interglacial cycles of
9000-429: The asexual phase of the life cycle. Bdelloid rotifer females cannot produce resting eggs, but many can survive prolonged periods of adverse conditions after desiccation . This facility is termed anhydrobiosis , and organisms with these capabilities are termed anhydrobionts. Under drought conditions, bdelloid rotifers contract into an inert form and lose almost all body water; when rehydrated they resume activity within
9125-511: The atmosphere as methane, those emissions will cause 40-70% of the total warming caused by permafrost thaw during the 21st century. Much of the uncertainty about the eventual extent of permafrost methane emissions is caused by the difficulty of accounting for the recently discovered abrupt thaw processes, which often increase the fraction of methane emitted over carbon dioxide in comparison to the usual gradual thaw processes. Another factor which complicates projections of permafrost carbon emissions
9250-554: The atmosphere, as well as the transfer of carbon between land and water as methane, dissolved organic carbon , dissolved inorganic carbon , particulate inorganic carbon and particulate organic carbon . Most of the bacteria and fungi found in permafrost cannot be cultured in the laboratory, but the identity of the microorganisms can be revealed by DNA -based techniques. For instance, analysis of 16S rRNA genes from late Pleistocene permafrost samples in eastern Siberia 's Kolyma Lowland revealed eight phylotypes , which belonged to
9375-482: The body, helping to maintain osmotic balance . The coronal cilia pull the animal, when unattached, through the water. Like many other microscopic animals, adult rotifers frequently exhibit eutely —they have a fixed number of cells within a species, usually on the order of 1,000. Bdelloid rotifer genomes contain two or more divergent copies of each gene , suggesting a long-term asexual evolutionary history. For example, four copies of hsp82 are found. Each
9500-582: The brain, this organ usually consists of one or more glands and a sac or reservoir. The sac drains into a duct before opening through pores on the uppermost part of the head. Current data shows a wide diversity in structure and potential function. In some species it is reduced or may even be absent completely. Benthic species have larger RCO's than planktonic species. Despite this diversity, positional correspondence of RCOs strongly suggests homology . A 2023 study using transmission electron microscopy and confocal laser scanning microscopy has illuminated
9625-421: The bristles of the corona are sensitive to touch, and there are also a pair of tiny sensory pits lined by cilia in the head region. Despite over 100 years of research, rotifer anatomy still has many poorly understood components. One of the more mysterious organs in rotifers is the "retrocerebral organ" (RCO), which still remains very enigmatic in its morphology, function, development, and evolution. Lying close to
9750-423: The cerebral ganglion. Much like the organ itself, the precise function and biochemical makeup of the secretions is still unknown. The small size of rotifers and small volume of the secretions makes isolation immensely difficult. The secretions have some similarities to the hydrogel secretions that form gelatinous housings in some rotifer species. Ultrastructure analysis of T. similis secretions showed them to be
9875-409: The chance to fully decompose and release their carbon , making tundra soil a carbon sink . As global warming heats the ecosystem, frozen soil thaws and becomes warm enough for decomposition to start anew, accelerating the permafrost carbon cycle . Depending on conditions at the time of thaw, decomposition can release either carbon dioxide or methane , and these greenhouse gas emissions act as
10000-421: The coast of Tuktoyaktuk in western Arctic Canada , where the remains of Laurentide Ice Sheet are located. Buried surface ice may derive from snow, frozen lake or sea ice , aufeis (stranded river ice) and even buried glacial ice from the former Pleistocene ice sheets. The latter hold enormous value for paleoglaciological research, yet even as of 2022, the total extent and volume of such buried ancient ice
10125-424: The corona include alteration of the cilia into bristles or large tufts, and either expansion or loss of the ciliated band around the head. In genera such as Collotheca , the corona is modified to form a funnel surrounding the mouth. In many species, such as those in the genus Testudinella , the cilia around the mouth have disappeared, leaving just two small circular bands on the head. In the bdelloids , this plan
10250-704: The damage to buildings ($ 2.8 billion), but there's also damage to roads ($ 700 million), railroads ($ 620 million), airports ($ 360 million) and pipelines ($ 170 million). Similar estimates were done for RCP4.5, a less intense scenario which leads to around 2.5 °C (4.5 °F) by 2100, a level of warming similar to the current projections. In that case, total damages from permafrost thaw are reduced to $ 3 billion, while damages to roads and railroads are lessened by approximately two-thirds (from $ 700 and $ 620 million to $ 190 and $ 220 million) and damages to pipelines are reduced more than ten-fold, from $ 170 million to $ 16 million. Unlike
10375-480: The damage to residential infrastructure may reach $ 15 billion, while total public infrastructure damages could amount to 132 billion. This includes oil and gas extraction facilities, of which 45% are believed to be at risk. Outside of the Arctic, Qinghai–Tibet Plateau (sometimes known as "the Third Pole"), also has an extensive permafrost area. It is warming at twice the global average rate, and 40% of it
10500-586: The discontinuous zone. Observed warming was up to 3 °C (5.4 °F) in parts of Northern Alaska (early 1980s to mid-2000s) and up to 2 °C (3.6 °F) in parts of the Russian European North (1970–2020). This warming inevitably causes permafrost to thaw: active layer thickness has increased in the European and Russian Arctic across the 21st century and at high elevation areas in Europe and Asia since
10625-416: The end of summer: as of 2018, the average thickness in the Northern Hemisphere is ~145 centimetres (4.76 ft), but there are significant regional differences. Northeastern Siberia , Alaska and Greenland have the most solid permafrost with the lowest extent of active layer (less than 50 centimetres (1.6 ft) on average, and sometimes only 30 centimetres (0.98 ft)), while southern Norway and
10750-459: The environment as the warming progresses. Lastly, concerns have been raised about the potential for pathogenic microorganisms surviving the thaw and contributing to future pandemics . However, this is considered unlikely, and a scientific review on the subject describes the risks as "generally low". Permafrost is soil , rock or sediment that is frozen for more than two consecutive years. In practice, this means that permafrost occurs at
10875-475: The exact function of the organ is still ultimately unclear. The leading hypotheses are that the RCO secretes a mucus-like substance that aids in benthic locomotion, adhesion, and/or reproduction (i.e., attachment of eggs to a substrate), although more research is needed to explore function and evaluate the homology between species. The coronal cilia create a current that sweeps food into the mouth. The mouth opens into
11000-431: The exact proportion is uncertain. It is considered very unlikely that this greening could offset all of the emissions from permafrost thaw during the 21st century, and even less likely that it could continue to keep pace with those emissions after the 21st century. Further, climate change also increases the risk of wildfires in the Arctic, which can substantially accelerate emissions of permafrost carbon. Altogether, it
11125-438: The fine structure of this organ further. The study, the first of its kind, investigated the RCO in one species, Trichocerca similis . It was determined to be a syncytial organ , composed of a posterior glandular region, an expansive reservoir, and an anterior duct . The glandular portion has an active cytoplasm with paired nuclei , abundant rough ER , ribosomes , Golgi , and mitochondria . Secretion granules accumulate at
11250-469: The formation of frozen debris lobes (FDLs), which are defined as "slow-moving landslides composed of soil, rocks, trees, and ice". This is a notable issue in the Alaska 's southern Brooks Range , where some FDLs measured over 100 m (110 yd) in width, 20 m (22 yd) in height, and 1,000 m (1,100 yd) in length by 2012. As of December 2021, there were 43 frozen debris lobes identified in
11375-425: The gradual and ongoing decline of subsea permafrost extent. Nevertheless, its presence remains an important consideration for the "design, construction, and operation of coastal facilities, structures founded on the seabed, artificial islands , sub-sea pipelines , and wells drilled for exploration and production". Subsea permafrost can also overlay deposits of methane clathrate , which were once speculated to be
11500-411: The influence of aspect can never be sufficient to thaw permafrost and a zone of continuous permafrost (abbreviated to CPZ ) forms. A line of continuous permafrost in the Northern Hemisphere represents the most southern border where land is covered by continuous permafrost or glacial ice. The line of continuous permafrost varies around the world northward or southward due to regional climatic changes. In
11625-430: The internal structure is uniform. Many rotifers can retract the foot partially or wholly into the trunk. The foot ends in from one to four toes, which, in sessile and crawling species, contain adhesive glands to attach the animal to the substratum. In many free-swimming species, the foot as a whole is reduced in size, and may even be absent. Rotifers have a small cerebral ganglion, effectively its brain, located just above
11750-502: The major tipping points in the climate system due to the exhibition of local thresholds and its effective irreversibility. However, while there are self-perpetuating processes that apply on the local or regional scale, it is debated as to whether it meets the strict definition of a global tipping point as in aggregate permafrost thaw is gradual with warming. In the northern circumpolar region, permafrost contains organic matter equivalent to 1400–1650 billion tons of pure carbon, which
11875-439: The mastax, from which a number of nerves extend throughout the body. The number of nerves varies among species, although the nervous system usually has a simple layout. The nervous system comprises about 25% of the roughly 1,000 cells in a rotifer. Rotifers typically possess one or two pairs of short antennae and up to five eyes. The eyes are simple in structure, sometimes with just a single photoreceptor cell . In addition,
12000-574: The mean annual air temperature is lower than the freezing point of water. Exceptions are found in humid boreal forests , such as in Northern Scandinavia and the North-Eastern part of European Russia west of the Urals , where snow acts as an insulating blanket. Glaciated areas may also be exceptions. Since all glaciers are warmed at their base by geothermal heat, temperate glaciers , which are near
12125-591: The monogonont life cycle, promoting fast population growth and colonization. In this phase males are absent and amictic females produce diploid eggs by mitosis which develop parthenogenetically into females that are clones of their mothers. Some amictic females can generate mictic females that will produce haploid eggs by meiosis. Mixis (meiosis) is induced by different types of stimulus depending on species. Haploid eggs develop into haploid dwarf males if they are not fertilized and into diploid "resting eggs" (or "diapausing eggs") if they are fertilized by males. Fertilization
12250-403: The original theories for ice inclusion in freezing soils. While there are four categories of ice in permafrost – pore ice, ice wedges (also known as vein ice), buried surface ice and intrasedimental (sometimes also called constitutional ) ice – only the last two tend to be large enough to qualify as massive ground ice. These two types usually occur separately, but may be found together, like on
12375-525: The other costs stemming from climate change in Alaska, such as damages from increased precipitation and flooding, climate change adaptation is not a viable way to reduce damages from permafrost thaw, as it would cost more than the damage incurred under either scenario. In Canada, Northwest Territories have a population of only 45,000 people in 33 communities, yet permafrost thaw is expected to cost them $ 1.3 billion over 75 years, or around $ 51 million
12500-514: The other hands, disturbance of formerly hard soil increases drainage of water reservoirs in northern wetlands . This can dry them out and compromise the survival of plants and animals used to the wetland ecosystem. In high mountains, much of the structural stability can be attributed to glaciers and permafrost. As climate warms, permafrost thaws, decreasing slope stability and increasing stress through buildup of pore-water pressure, which may ultimately lead to slope failure and rockfalls . Over
12625-691: The past century, an increasing number of alpine rock slope failure events in mountain ranges around the world have been recorded, and some have been attributed to permafrost thaw induced by climate change. The 1987 Val Pola landslide that killed 22 people in the Italian Alps is considered one such example. In 2002, massive rock and ice falls (up to 11.8 million m ), earthquakes (up to 3.9 Richter ), floods (up to 7.8 million m water), and rapid rock-ice flow to long distances (up to 7.5 km at 60 m/s) were attributed to slope instability in high mountain permafrost. Permafrost thaw can also result in
12750-491: The phyla Actinomycetota and Pseudomonadota . "Muot-da-Barba-Peider", an alpine permafrost site in eastern Switzerland, was found to host a diverse microbial community in 2016. Prominent bacteria groups included phylum Acidobacteriota , Actinomycetota , AD3, Bacteroidota , Chloroflexota , Gemmatimonadota , OD1, Nitrospirota , Planctomycetota , Pseudomonadota , and Verrucomicrobiota , in addition to eukaryotic fungi like Ascomycota , Basidiomycota , and Zygomycota . In
12875-515: The pipeline from sinking and the Qingzang railway in Tibet employs a variety of methods to keep the ground cool, both in areas with frost-susceptible soil . Permafrost may necessitate special enclosures for buried utilities, called " utilidors ". Globally, permafrost warmed by about 0.3 °C (0.54 °F) between 2007 and 2016, with stronger warming observed in the continuous permafrost zone relative to
13000-412: The presence of corona on the head, a structure ciliated in all genera except Cupelopagis and presence of mastax. In the more primitive species, the corona forms a simple ring of cilia around the mouth from which an additional band of cilia stretches over the back of the head. In the great majority of rotifers, however, this has evolved into a more complex structure. Modifications to the basic plan of
13125-595: The presence of permafrost. Black spruce tolerates limited rooting zones, and dominates flora where permafrost is extensive. Likewise, animal species which live in dens and burrows have their habitat constrained by the permafrost, and these constraints also have a secondary impact on interactions between species within the ecosystem . While permafrost soil is frozen, it is not completely inhospitable to microorganisms , though their numbers can vary widely, typically from 1 to 1000 million per gram of soil. The permafrost carbon cycle (Arctic Carbon Cycle) deals with
13250-534: The presently living species, scientists observed a variety of adaptations for sub-zero conditions, including reduced and anaerobic metabolic processes. There are only two large cities in the world built in areas of continuous permafrost (where the frozen soil forms an unbroken, below-zero sheet) and both are in Russia – Norilsk in Krasnoyarsk Krai and Yakutsk in the Sakha Republic . Building on permafrost
13375-427: The scenario most similar to today, SSP2-4.5 , around 60% of the current infrastructure would be at high risk by 2090 and simply maintaining it would cost $ 6.31 billion, with adaptation reducing these costs by 20.9% at most. Holding the global warming to 2 °C (3.6 °F) would reduce these costs to $ 5.65 billion, and fulfilling the optimistic Paris Agreement target of 1.5 °C (2.7 °F) would save
13500-419: The second half of the century. Reducing greenhouse gas emissions in line with the Paris Agreement is projected to stabilize the risk after mid-century; otherwise, it'll continue to worsen. In Alaska alone, damages to infrastructure by the end of the century would amount to $ 4.6 billion (at 2015 dollar value) if RCP8.5 , the high-emission climate change scenario , were realized. Over half stems from
13625-408: The size of the male. In parthenogenetic species, males may be present only at certain times of the year, or absent altogether. The female reproductive system consists of one or two ovaries , each with a vitellarium gland that supplies the eggs with yolk . Together, each ovary and vitellarium form a single syncitial structure in the anterior part of the animal, opening through an oviduct into
13750-623: The soil remains frozen. The Melnikov Permafrost Institute in Yakutsk found that pile foundations should extend down to 15 metres (49 ft) to avoid the risk of buildings sinking. At this depth the temperature does not change with the seasons, remaining at about −5 °C (23 °F). Two other approaches are building on an extensive gravel pad (usually 1–2 m (3 ft 3 in – 6 ft 7 in) thick); or using anhydrous ammonia heat pipes . The Trans-Alaska Pipeline System uses heat pipes built into vertical supports to prevent
13875-668: The southern Brooks Range, where they could potentially threaten both the Trans Alaska Pipeline System (TAPS) corridor and the Dalton Highway , which is the main transport link between the Interior Alaska and the Alaska North Slope . As of 2021, there are 1162 settlements located directly atop the Arctic permafrost, which host an estimated 5 million people. By 2050, permafrost layer below 42% of these settlements
14000-413: The species composition of algae in ecosystems through their choice in grazing. Rotifers may compete with cladocera and copepods for planktonic food sources. Rotifers are dioecious and reproduce sexually or parthenogenetically . They are sexually dimorphic , with the females always being larger than the males. In some species, this is relatively mild, but in others the female may be up to ten times
14125-696: The species, and females reproduce only by parthenogenesis . However, a new study provided evidence for interindividual genetic exchange and recombination in Adineta vaga , a species previously thought to be anciently asexual. Recent transitions: Loss of sexual reproduction can be inherited in a simple Mendelian fashion in the monogonont rotifer Brachionus calyciflorus : This species can normally switch between sexual and asexual reproduction (cyclical parthenogenesis), but occasionally gives rise to purely asexual lineages (obligate parthenogens). These lineages are unable to reproduce sexually due to being homozygous for
14250-470: The surface. However, only a fraction of this stored carbon is expected to enter the atmosphere. In general, the volume of permafrost in the upper 3 m of ground is expected to decrease by about 25% per 1 °C (1.8 °F) of global warming, yet even under the RCP8.5 scenario associated with over 4 °C (7.2 °F) of global warming by the end of the 21st century, about 5% to 15% of permafrost carbon
14375-537: The surrounding ground begins to jut outward at a slope. This can eventually result in the formation of large-scale land forms around this core of permafrost, such as palsas – long (15–150 m (49–492 ft)), wide (10–30 m (33–98 ft)) yet shallow (<1–6 m (3 ft 3 in – 19 ft 8 in) tall) peat mounds – and the even larger pingos , which can be 3–70 m (10–230 ft) high and 30–1,000 m (98–3,281 ft) in diameter . Only plants with shallow roots can survive in
14500-859: The top 2.5 meters of clay sediments, yet it takes between 10 and 10,000 years for peat sediments and between 1,000 and 1,000,000 years for silt sediments. Permafrost processes such as thermal contraction generating cracks which eventually become ice wedges and solifluction – gradual movement of soil down the slope as it repeatedly freezes and thaws – often lead to the formation of ground polygons, rings, steps and other forms of patterned ground found in arctic, periglacial and alpine areas. In ice-rich permafrost areas, melting of ground ice initiates thermokarst landforms such as thermokarst lakes , thaw slumps, thermal-erosion gullies, and active layer detachments. Notably, unusually deep permafrost in Arctic moorlands and bogs often attracts meltwater in warmer seasons, which pools and freezes to form ice lenses , and
14625-435: The transfer of carbon from permafrost soils to terrestrial vegetation and microbes, to the atmosphere, back to vegetation, and finally back to permafrost soils through burial and sedimentation due to cryogenic processes. Some of this carbon is transferred to the ocean and other portions of the globe through the global carbon cycle. The cycle includes the exchange of carbon dioxide and methane between terrestrial components and
14750-431: The trophi are covered in grinding ridges, while in more actively carnivorous species, they may be shaped like forceps to help bite into prey. In some ectoparasitic rotifers, the mastax is adapted to grip onto the host, although, in others, the foot performs this function instead. Behind the mastax lies an oesophagus , which opens into a stomach where most of the digestion and absorption occurs. The stomach opens into
14875-424: The very high emission scenario RCP8.5, 46% of industrial and contaminated sites would start thawing by 2050, and virtually all of them would be affected by the thaw by 2100. Organochlorines and other persistent organic pollutants are of a particular concern, due to their potential to repeatedly reach local communities after their re-release through biomagnification in fish. At worst, future generations born in
15000-444: The water drains or evaporates, soil structure weakens and sometimes becomes viscous until it regains strength with decreasing moisture content. One visible sign of permafrost degradation is the random displacement of trees from their vertical orientation in permafrost areas. Global warming has been increasing permafrost slope disturbances and sediment supplies to fluvial systems, resulting in exceptional increases in river sediment. On
15125-417: The world with a few saltwater species. Some rotifers are free swimming and truly planktonic , others move by inchworming along a substrate, and some are sessile , living inside tubes or gelatinous holdfasts that are attached to a substrate. About 25 species are colonial (e.g., Sinantherina semibullata ), either sessile or planktonic. Rotifers are an important part of the freshwater zooplankton , being
15250-469: The year 2022 concluded that if the goal of preventing 2 °C (3.6 °F) of warming was realized, then the average annual permafrost emissions throughout the 21st century would be equivalent to the year 2019 annual emissions of Russia. Under RCP4.5, a scenario considered close to the current trajectory and where the warming stays slightly below 3 °C (5.4 °F), annual permafrost emissions would be comparable to year 2019 emissions of Western Europe or
15375-519: Was built up over thousands of years. This amount equals almost half of all organic material in all soils , and it is about twice the carbon content of the atmosphere , or around four times larger than the human emissions of carbon between the start of the Industrial Revolution and 2011. Further, most of this carbon (~1,035 billion tons) is stored in what is defined as the near-surface permafrost, no deeper than 3 metres (9.8 ft) below
15500-444: Was frozen and stable, and so are vulnerable to collapse if it thaws. Estimates suggest nearly 70% of such infrastructure is at risk by 2050, and that the associated costs could rise to tens of billions of dollars in the second half of the century. Furthermore, between 13,000 and 20,000 sites contaminated with toxic waste are present in the permafrost, as well as the natural mercury deposits, which are all liable to leak and pollute
15625-438: Was not until the publication of Christian Gottfried Ehrenberg 's Die Infusionsthierchen als vollkommene Organismen in 1838 that the rotifers were recognized as being multicellular animals. About 2,200 species of rotifers have been described. Their taxonomy is currently in a state of flux. One treatment places them in the phylum Rotifera, with three classes: Seisonidea , Bdelloidea and Monogononta . The largest group
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