Misplaced Pages

Doswelliidae

Article snapshot taken from Wikipedia with creative commons attribution-sharealike license. Give it a read and then ask your questions in the chat. We can research this topic together.
#418581

97-636: Doswelliidae is an extinct family of carnivorous archosauriform reptiles that lived in North America and Europe during the Middle to Late Triassic period. Long represented solely by the heavily-armored reptile Doswellia , the family's composition has expanded since 2011, although two supposed South American doswelliids ( Archeopelta and Tarjadia ) were later redescribed as erpetosuchids . Doswelliids were not true archosaurs , but they were close relatives and some studies have considered them among

194-438: A food chain who lose their prey. "Species coextinction is a manifestation of one of the interconnectednesses of organisms in complex ecosystems ... While coextinction may not be the most important cause of species extinctions, it is certainly an insidious one." Coextinction is especially common when a keystone species goes extinct. Models suggest that coextinction is the most common form of biodiversity loss . There may be

291-480: A monospecific family of basal archosauriforms represented by Doswellia kaltenbachi from the Late Triassic of North America. However, a 2011 cladistic analysis by Desojo, Ezcurra, & Schultz recovered the newly named Brazilian genus Archeopelta as well as the enigmatic Argentinian archosauriform Tarjadia as close relatives of Doswellia, within a monophyletic Doswelliidae. These authors defined

388-657: A nautilus to the Royal Society that was more than two feet in diameter, and morphologically distinct from any known living species. Hooke theorized that this was simply because the species lived in the deep ocean and no one had discovered them yet. While he contended that it was possible a species could be "lost", he thought this highly unlikely. Similarly, in 1695, Sir Thomas Molyneux published an account of enormous antlers found in Ireland that did not belong to any extant taxa in that area. Molyneux reasoned that they came from

485-415: A species or a population is the variety of genetic information in its living members. A large gene pool (extensive genetic diversity ) is associated with robust populations that can survive bouts of intense selection . Meanwhile, low genetic diversity (see inbreeding and population bottlenecks ) reduces the range of adaptions possible. Replacing native with alien genes narrows genetic diversity within

582-436: A viable population for species preservation and possible future reintroduction to the wild, through use of carefully planned breeding programs . The extinction of one species' wild population can have knock-on effects, causing further extinctions. These are also called "chains of extinction". This is especially common with extinction of keystone species . A 2018 study indicated that the sixth mass extinction started in

679-474: A Lazarus species when extant individuals were described in 2019. Attenborough's long-beaked echidna ( Zaglossus attenboroughi ) is an example of a Lazarus species from Papua New Guinea that had last been sighted in 1962 and believed to be possibly extinct, until it was recorded again in November 2023. Some species currently thought to be extinct have had continued speculation that they may still exist, and in

776-495: A cascade of coextinction across the trophic levels . Such effects are most severe in mutualistic and parasitic relationships. An example of coextinction is the Haast's eagle and the moa : the Haast's eagle was a predator that became extinct because its food source became extinct. The moa were several species of flightless birds that were a food source for the Haast's eagle. Extinction as

873-429: A common ancestor with modern horses. Pseudoextinction is much easier to demonstrate for larger taxonomic groups. A Lazarus taxon or Lazarus species refers to instances where a species or taxon was thought to be extinct, but was later rediscovered. It can also refer to instances where large gaps in the fossil record of a taxon result in fossils reappearing much later, although the taxon may have ultimately become extinct at

970-399: A fact that was accepted by most scientists. The primary debate focused on whether this turnover caused by extinction was gradual or abrupt in nature. Cuvier understood extinction to be the result of cataclysmic events that wipe out huge numbers of species, as opposed to the gradual decline of a species over time. His catastrophic view of the nature of extinction garnered him many opponents in

1067-611: A frog-like hopper by one study. They had long bodies and tails, and their front legs were shorter than their hind legs. Unlike in some other groups of archosauriforms, doswelliids retain teeth on the pterygoid , on the roof of the mouth. Although Vancleavea had a short and deep skull, most doswelliids had slender and elongated snouts, similar to other members of Proterochampsia . Advanced doswelliids possessed dorsal ribs which splay outwards (rather than downwards), making their bodies wide and low. Doswelliids were armored with multiple rows of bony scutes ( osteoderms ) on their backs. With

SECTION 10

#1733093414419

1164-708: A higher risk of extinction and die out faster than less sexually dimorphic species, the least sexually dimorphic species surviving for millions of years while the most sexually dimorphic species die out within mere thousands of years. Earlier studies based on counting the number of currently living species in modern taxa have shown a higher number of species in more sexually dimorphic taxa which have been interpreted as higher survival in taxa with more sexual selection, but such studies of modern species only measure indirect effects of extinction and are subject to error sources such as dying and doomed taxa speciating more due to splitting of habitat ranges into more small isolated groups during

1261-405: A large range, a lack of individuals of both sexes (in sexually reproducing species), or other reasons. Pinpointing the extinction (or pseudoextinction ) of a species requires a clear definition of that species . If it is to be declared extinct, the species in question must be uniquely distinguishable from any ancestor or daughter species, and from any other closely related species. Extinction of

1358-592: A later point. The coelacanth , a fish related to lungfish and tetrapods , is an example of a Lazarus taxon that was known only from the fossil record and was considered to have been extinct since the end of the Cretaceous Period . In 1938, however, a living specimen was found off the Chalumna River (now Tyolomnqa) on the east coast of South Africa. Calliostoma bullatum , a species of deepwater sea snail originally described from fossils in 1844 proved to be

1455-479: A long, slender rod bent at a 90-degree angle. Also like Doswellia , the "corner" of the bend has a rough ridge at the front. Nevertheless, the ribs of Jaxtasuchus did not extend outwards to the same extent as those of Doswellia . Caudal (tail) vertebrae were also elongated. Jaxtasuchus was covered with armor plates known as osteoderms . The osteoderms lay on the body in four longitudinal rows: two inner rows of paramedian osteoderms (i.e. ones which were adjacent to

1552-587: A mathematical model that falls in all positions. By contrast, conservation biology uses the extinction vortex model to classify extinctions by cause. When concerns about human extinction have been raised, for example in Sir Martin Rees ' 2003 book Our Final Hour , those concerns lie with the effects of climate change or technological disaster. Human-driven extinction started as humans migrated out of Africa more than 60,000 years ago. Currently, environmental groups and some governments are concerned with

1649-456: A natural part of the evolutionary process. Only recently have extinctions been recorded and scientists have become alarmed at the current high rate of extinctions . Most species that become extinct are never scientifically documented. Some scientists estimate that up to half of presently existing plant and animal species may become extinct by 2100. A 2018 report indicated that the phylogenetic diversity of 300 mammalian species erased during

1746-441: A new mega-predator or by transporting animals and plants from one part of the world to another. Such introductions have been occurring for thousands of years, sometimes intentionally (e.g. livestock released by sailors on islands as a future source of food) and sometimes accidentally (e.g. rats escaping from boats). In most cases, the introductions are unsuccessful, but when an invasive alien species does become established,

1843-610: A population a higher chance in the short term of surviving an adverse change in conditions. Effects that cause or reward a loss in genetic diversity can increase the chances of extinction of a species. Population bottlenecks can dramatically reduce genetic diversity by severely limiting the number of reproducing individuals and make inbreeding more frequent. Extinction sometimes results for species evolved to specific ecologies that are subjected to genetic pollution —i.e., uncontrolled hybridization , introgression and genetic swamping that lead to homogenization or out-competition from

1940-407: A race of animals to become extinct. A series of fossils were discovered in the late 17th century that appeared unlike any living species. As a result, the scientific community embarked on a voyage of creative rationalization, seeking to understand what had happened to these species within a framework that did not account for total extinction. In October 1686, Robert Hooke presented an impression of

2037-502: A reduction in agricultural productivity. Furthermore, increased erosion contributes to poorer water quality by elevating the levels of sediment and pollutants in rivers and streams. Habitat degradation through toxicity can kill off a species very rapidly, by killing all living members through contamination or sterilizing them. It can also occur over longer periods at lower toxicity levels by affecting life span, reproductive capacity, or competitiveness. Habitat degradation can also take

SECTION 20

#1733093414419

2134-486: A result of climate change has been confirmed by fossil studies. Particularly, the extinction of amphibians during the Carboniferous Rainforest Collapse , 305 million years ago. A 2003 review across 14 biodiversity research centers predicted that, because of climate change, 15–37% of land species would be "committed to extinction" by 2050. The ecologically rich areas that would potentially suffer

2231-479: A species (or replacement by a daughter species) plays a key role in the punctuated equilibrium hypothesis of Stephen Jay Gould and Niles Eldredge . In ecology , extinction is sometimes used informally to refer to local extinction , in which a species ceases to exist in the chosen area of study, despite still existing elsewhere. Local extinctions may be made good by the reintroduction of individuals of that species taken from other locations; wolf reintroduction

2328-439: A species may come suddenly when an otherwise healthy species is wiped out completely, as when toxic pollution renders its entire habitat unliveable; or may occur gradually over thousands or millions of years, such as when a species gradually loses out in competition for food to better adapted competitors. Extinction may occur a long time after the events that set it in motion, a phenomenon known as extinction debt . Assessing

2425-404: A species or group of species. "Just as each species is unique", write Beverly and Stephen C. Stearns , "so is each extinction ... the causes for each are varied—some subtle and complex, others obvious and simple". Most simply, any species that cannot survive and reproduce in its environment and cannot move to a new environment where it can do so, dies out and becomes extinct. Extinction of

2522-518: A subsequent report, IPBES listed unsustainable fishing, hunting and logging as being some of the primary drivers of the global extinction crisis. In June 2019, one million species of plants and animals were at risk of extinction. At least 571 plant species have been lost since 1750, but likely many more. The main cause of the extinctions is the destruction of natural habitats by human activities, such as cutting down forests and converting land into fields for farming. A dagger symbol (†) placed next to

2619-562: Is a mostly complete skeleton missing the head and neck, which was found at the Schumann quarry of Eschenau (part of Vellberg ). Another specimen from the same quarry, SMNS 91083, preserves an incomplete skull and neck. A third specimen from the quarry, SMNS 90500, preserves a forelimb, osteoderms, and a femur (thigh bone). Other more fragmentary specimens include vertebrae and osteoderms recovered from various other quarries and strata unearthed during highway construction. At some sites Jaxtasuchus

2716-517: Is also evidence to suggest that this event was preceded by another mass extinction, known as Olson's Extinction . The Cretaceous–Paleogene extinction event (K–Pg) occurred 66 million years ago, at the end of the Cretaceous period; it is best known for having wiped out non-avian dinosaurs , among many other species. According to a 1998 survey of 400 biologists conducted by New York 's American Museum of Natural History , nearly 70% believed that

2813-444: Is an example of this. Species that are not globally extinct are termed extant . Those species that are extant, yet are threatened with extinction, are referred to as threatened or endangered species . Currently, an important aspect of extinction is human attempts to preserve critically endangered species. These are reflected by the creation of the conservation status "extinct in the wild" (EW) . Species listed under this status by

2910-585: Is difficult to demonstrate unless one has a strong chain of evidence linking a living species to members of a pre-existing species. For example, it is sometimes claimed that the extinct Hyracotherium , which was an early horse that shares a common ancestor with the modern horse , is pseudoextinct, rather than extinct, because there are several extant species of Equus , including zebra and donkey ; however, as fossil species typically leave no genetic material behind, one cannot say whether Hyracotherium evolved into more modern horse species or merely evolved from

3007-417: Is estimated as 100 to 1,000 times "background" rates (the average extinction rates in the evolutionary time scale of planet Earth), faster than at any other time in human history, while future rates are likely 10,000 times higher. However, some groups are going extinct much faster. Biologists Paul R. Ehrlich and Stuart Pimm , among others, contend that human population growth and overconsumption are

Doswelliidae - Misplaced Pages Continue

3104-569: Is known from a jaw fragment and several teeth, and Batrachotomus kupferzellensis , a large pseudosuchian archosaur that is known from several skeletons. Jaxtasuchus is the most abundant archosauriform reptile in the Lower Keuper. Its remains have been uncovered in six fossil localities: Limestone quarries at Rielingshausen, Zwingelhausen, and Vellberg (which has two quarries: Schumann and Ummenhofen), as well as roadcuts at Kupferzell and Wolpertshausen . The holotype specimen, SMNS 91352,

3201-513: Is known only by its osteoderms. Jaxtasuchus is named after Jagst , a tributary of the Neckar river in the region where fossils were found. The type species J. salomoni is named after Hans Michael Salomon, who discovered the holotype specimen and donated it to the Staatliches Museum für Naturkunde Stuttgart where it is now housed. The maxilla was long and low, with 15 tooth sockets. It

3298-459: Is the angular , which has a concave upper edge that may have formed the base of a mandibular fenestra (a hole in the jaw common to most archosauriforms but absent in Doswellia ). The cervical (neck) vertebrae of Jaxtasuchus were characteristically longer than they were high, increasing in size towards the base of the neck. The neural spines were low and rectangular, but were slightly taller at

3395-592: Is the destruction of ocean floors by bottom trawling . Diminished resources or introduction of new competitor species also often accompany habitat degradation. Global warming has allowed some species to expand their range, bringing competition to other species that previously occupied that area. Sometimes these new competitors are predators and directly affect prey species, while at other times they may merely outcompete vulnerable species for limited resources. Vital resources including water and food can also be limited during habitat degradation, leading to extinction. In

3492-525: Is the most important determinant of genus extinction at background rates but becomes increasingly irrelevant as mass extinction arises. Limited geographic range is a cause both of small population size and of greater vulnerability to local environmental catastrophes. Extinction rates can be affected not just by population size, but by any factor that affects evolvability , including balancing selection , cryptic genetic variation , phenotypic plasticity , and robustness . A diverse or deep gene pool gives

3589-457: Is the termination of a taxon by the death of its last member . A taxon may become functionally extinct before the death of its last member if it loses the capacity to reproduce and recover. Because a species' potential range may be very large, determining this moment is difficult, and is usually done retrospectively. This difficulty leads to phenomena such as Lazarus taxa , where a species presumed extinct abruptly "reappears" (typically in

3686-474: The International Union for Conservation of Nature (IUCN) are not known to have any living specimens in the wild and are maintained only in zoos or other artificial environments. Some of these species are functionally extinct, as they are no longer part of their natural habitat and it is unlikely the species will ever be restored to the wild. When possible, modern zoological institutions try to maintain

3783-477: The Late Pleistocene could take up to 5 to 7 million years to restore mammal diversity to what it was before the human era. Extinction of a parent species where daughter species or subspecies are still extant is called pseudoextinction or phyletic extinction. Effectively, the old taxon vanishes, transformed ( anagenesis ) into a successor, or split into more than one ( cladogenesis ). Pseudoextinction

3880-619: The fossil record ) after a period of apparent absence. More than 99% of all species that ever lived on Earth , amounting to over five billion species, are estimated to have died out. It is estimated that there are currently around 8.7 million species of eukaryotes globally, and possibly many times more if microorganisms , such as bacteria , are included. Notable extinct animal species include non-avian dinosaurs , saber-toothed cats , dodos , mammoths , ground sloths , thylacines , trilobites , golden toads , and passenger pigeons . Through evolution , species arise through

3977-441: The postorbital . Its structure is similar to that of most diapsid reptiles, indicating that Jaxtasuchus likely retained a lower temporal fenestra like other diapsids. This contrasts with Doswellia , which has a smaller and stouter postorbital bone and a lower temporal fenestra which has been completely closed up, giving it a euryapsid skull. Braincase bones have also been preserved in one specimen. The occipital condyle , which

Doswelliidae - Misplaced Pages Continue

4074-410: The slender-billed curlew ( Numenius tenuirostris ), not seen since 2007. As long as species have been evolving, species have been going extinct. It is estimated that over 99.9% of all species that ever lived are extinct. The average lifespan of a species is 1–10 million years, although this varies widely between taxa. A variety of causes can contribute directly or indirectly to the extinction of

4171-484: The strata of the Paris basin. They saw alternating saltwater and freshwater deposits, as well as patterns of the appearance and disappearance of fossils throughout the record. From these patterns, Cuvier inferred historic cycles of catastrophic flooding, extinction, and repopulation of the earth with new species. Cuvier's fossil evidence showed that very different life forms existed in the past than those that exist today,

4268-619: The 20 biodiversity goals laid out by the Aichi Biodiversity Targets in 2010, only 6 were "partially achieved" by the deadline of 2020. The report warned that biodiversity will continue to decline if the status quo is not changed, in particular the "currently unsustainable patterns of production and consumption, population growth and technological developments". In a 2021 report published in the journal Frontiers in Conservation Science , some top scientists asserted that even if

4365-451: The Aichi Biodiversity Targets set for 2020 had been achieved, it would not have resulted in a significant mitigation of biodiversity loss. They added that failure of the global community to reach these targets is hardly surprising given that biodiversity loss is "nowhere close to the top of any country's priorities, trailing far behind other concerns such as employment, healthcare, economic growth, or currency stability." For much of history,

4462-605: The Earth is currently in the early stages of a human-caused mass extinction, known as the Holocene extinction . In that survey, the same proportion of respondents agreed with the prediction that up to 20% of all living populations could become extinct within 30 years (by 2028). A 2014 special edition of Science declared there is widespread consensus on the issue of human-driven mass species extinctions. A 2020 study published in PNAS stated that

4559-570: The North American moose and that the animal had once been common on the British Isles . Rather than suggest that this indicated the possibility of species going extinct, he argued that although organisms could become locally extinct, they could never be entirely lost and would continue to exist in some unknown region of the globe. The antlers were later confirmed to be from the extinct deer Megaloceros . Hooke and Molyneux's line of thinking

4656-518: The Paris basin, could be formed by a slow rise and fall of sea levels . The concept of extinction was integral to Charles Darwin 's On the Origin of Species , with less fit lineages disappearing over time. For Darwin, extinction was a constant side effect of competition . Because of the wide reach of On the Origin of Species , it was widely accepted that extinction occurred gradually and evenly (a concept now referred to as background extinction ). It

4753-619: The United States government, to force the removal of Native Americans , many of whom relied on the bison for food. Jaxtasuchus salomoni Jaxtasuchus is an extinct genus of armored doswelliid archosauriform reptile known from the Middle Triassic ( Ladinian stage) of the Erfurt Formation in Germany . The type species , Jaxtasuchus salomoni , was named in 2013 on

4850-429: The accumulation of slightly deleterious mutations , then a population will go extinct. Smaller populations have fewer beneficial mutations entering the population each generation, slowing adaptation. It is also easier for slightly deleterious mutations to fix in small populations; the resulting positive feedback loop between small population size and low fitness can cause mutational meltdown . Limited geographic range

4947-423: The base of the neck. The dorsal ( torso ) vertebrae, on the other hand, had wide neural spines with a roughly textured upper surface. This rough texturing signified where the vertebrae attached to the overlying osteoderms. The dorsal vertebrae were also longer than they were high, and some (but not all) had keels on their lower surface. Much like Doswellia , the ribs of Jaxtasuchus had an unusual shape, that being

SECTION 50

#1733093414419

5044-670: The basis of several incomplete skeletons and other isolated remains. Like other doswelliids, members of the genus were heavily armored, with four longitudinal rows of bony plates called osteoderms covering the body. Jaxtasuchus is the first doswelliid known from Europe and is most closely related to Doswellia from the Late Triassic of the eastern United States. However, it was not as specialized as Doswellia , retaining several generalized archosauriform characteristics and having less armor. Jaxtasuchus fossils have been found in aquatic mudstones alongside fossils of temnospondyl amphibians, crustaceans, and mollusks, suggesting that Jaxtasuchus

5141-631: The closest large monophyletic clade to Archosauria , with only the Chinese archosauriform Yonghesuchus nested closer to archosaurs. However, a phylogenetic analysis by Ezcurra (2016) recovered Doswelliidae alongside the family Proterochampsidae within the clade Proterochampsia , which was found to be the sister taxon of Archosauria . The unusual aquatic archosauriform Vancleavea was also referred to Doswelliidae in this analysis. Subsequently, Ezcurra et al. (2017) excluded Archeopelta and Tarjadia from Doswelliidae, considering them to be archosaurs of

5238-600: The consequences can be catastrophic. Invasive alien species can affect native species directly by eating them, competing with them, and introducing pathogens or parasites that sicken or kill them; or indirectly by destroying or degrading their habitat. Human populations may themselves act as invasive predators. According to the "overkill hypothesis", the swift extinction of the megafauna in areas such as Australia (40,000 years before present), North and South America (12,000 years before present), Madagascar , Hawaii (AD 300–1000), and New Zealand (AD 1300–1500), resulted from

5335-418: The contemporary extinction crisis "may be the most serious environmental threat to the persistence of civilization, because it is irreversible." Biologist E. O. Wilson estimated in 2002 that if current rates of human destruction of the biosphere continue, one-half of all plant and animal species of life on earth will be extinct in 100 years. More significantly, the current rate of global species extinctions

5432-471: The deliberate destruction of some species, such as dangerous viruses , and the total destruction of other problematic species has been suggested. Other species were deliberately driven to extinction, or nearly so, due to poaching or because they were "undesirable", or to push for other human agendas. One example was the near extinction of the American bison , which was nearly wiped out by mass hunts sanctioned by

5529-403: The endangered wild water buffalo is most threatened with extinction by genetic pollution from the abundant domestic water buffalo ). Such extinctions are not always apparent from morphological (non-genetic) observations. Some degree of gene flow is a normal evolutionary process; nevertheless, hybridization (with or without introgression) threatens rare species' existence. The gene pool of

5626-575: The event of rediscovery would be considered Lazarus species. Examples include the thylacine , or Tasmanian tiger ( Thylacinus cynocephalus ), the last known example of which died in Hobart Zoo in Tasmania in 1936; the Japanese wolf ( Canis lupus hodophilax ), last sighted over 100 years ago; the American ivory-billed woodpecker ( Campephilus principalis ), with the last universally accepted sighting in 1944; and

5723-399: The exception of Vancleavea , which had many different forms of smooth osteoderms, doswelliid osteoderms were characteristically covered by deep, circular pits. There is also a smooth area (an anterior articular lamina) on the front edge of each osteoderm where the preceding osteoderm overlaps. This combination of osteoderm features is also present in erpetosuchids and some aetosaurs , although

5820-443: The extinction crisis. According to the International Union for Conservation of Nature (IUCN), 784 extinctions have been recorded since the year 1500, the arbitrary date selected to define "recent" extinctions, up to the year 2004; with many more likely to have gone unnoticed. Several species have also been listed as extinct since 2004. If adaptation increasing population fitness is slower than environmental degradation plus

5917-475: The extinction of species caused by humanity, and they try to prevent further extinctions through a variety of conservation programs. Humans can cause extinction of a species through overharvesting , pollution , habitat destruction , introduction of invasive species (such as new predators and food competitors ), overhunting, and other influences. Explosive, unsustainable human population growth and increasing per capita consumption are essential drivers of

SECTION 60

#1733093414419

6014-874: The family Erpetosuchidae instead. Litorosuchus , an aquatic archosauriform which is considered a close relative of Vancleavea , may also be a doswelliid if Vancleavea is a member of the family. The following cladogram is after Ezcurra (2016): Dorosuchus neoetus Euparkeria capensis ( Euparkeriidae ) Dongusuchus efremovi Yarasuchus deccanensis Avemetatarsalia Phytosauria The rest of Pseudosuchia (incl. Koilamasuchus ) Vancleavea campi Archeopelta arborensis Tarjadia ruthae Doswellia kaltenbachi Jaxtasuchus salomoni Proterochampsa barrionuevoi Proterochampsa nodosa Cerritosaurus binsfeldi Tropidosuchus romeri Pseudochampsa ischigualastensis Gualosuchus reigi Chanaresuchus bonapartei Rhadinosuchus gracilis Extinction Extinction

6111-434: The family as the most inclusive clade containing all archosauromorphs more closely related to Doswellia kaltenbachi than to Proterochampsa barrionuevoi , Erythrosuchus africanus , Caiman latirostris , (the broad-snouted caiman) or Passer domesticus (the house sparrow). Within the next few years, several other genera of archosauriforms were classified as Dosweliids. A second New Mexican species of Doswellia

6208-533: The field of zoology , and biology in general, and has also become an area of concern outside the scientific community. A number of organizations, such as the Worldwide Fund for Nature , have been created with the goal of preserving species from extinction. Governments have attempted, through enacting laws, to avoid habitat destruction, agricultural over-harvesting, and pollution . While many human-caused extinctions have been accidental, humans have also engaged in

6305-437: The flexed paramedian osteoderms, Jaxtasuchus likely had a more tall and narrow torso than Doswellia , which possessed six medial rows of osteoderms before flexure started to occur. Despite the heavy armor of the torso, the limb bones of Jaxtasuchus were fairly small and slender, with the hindlimbs longer than the forelimbs. The bones of the forelimb were slender and unspecialized, similar to those of Euparkeria rather than

6402-435: The form of a physical destruction of niche habitats. The widespread destruction of tropical rainforests and replacement with open pastureland is widely cited as an example of this; elimination of the dense forest eliminated the infrastructure needed by many species to survive. For example, a fern that depends on dense shade for protection from direct sunlight can no longer survive without forest to shelter it. Another example

6499-580: The habitat retreat of taxa approaching extinction. Possible causes of the higher extinction risk in species with more sexual selection shown by the comprehensive fossil studies that rule out such error sources include expensive sexually selected ornaments having negative effects on the ability to survive natural selection , as well as sexual selection removing a diversity of genes that under current ecological conditions are neutral for natural selection but some of which may be important for surviving climate change. There have been at least five mass extinctions in

6596-660: The heaviest losses include the Cape Floristic Region and the Caribbean Basin . These areas might see a doubling of present carbon dioxide levels and rising temperatures that could eliminate 56,000 plant and 3,700 animal species. Climate change has also been found to be a factor in habitat loss and desertification . Studies of fossils following species from the time they evolved to their extinction show that species with high sexual dimorphism , especially characteristics in males that are used to compete for mating, are at

6693-401: The hip were wider than they were long. At the base of the tail, the square-shaped paramedian osteoderms gradually lose their texture while the lateral osteoderms keep theirs. Further down the tail, the paramedian osteoderms become longer and finely pitted, while the lateral osteoderms shrink into triangular structures and then disappear. Small, keeled osteoderms were present on the limbs. Based on

6790-447: The history of life on earth, and four in the last 350 million years in which many species have disappeared in a relatively short period of geological time. A massive eruptive event that released large quantities of tephra particles into the atmosphere is considered to be one likely cause of the " Permian–Triassic extinction event " about 250 million years ago, which is estimated to have killed 90% of species then existing. There

6887-475: The human era since the Late Pleistocene would require 5 to 7 million years to recover. According to the 2019 Global Assessment Report on Biodiversity and Ecosystem Services by IPBES , the biomass of wild mammals has fallen by 82%, natural ecosystems have lost about half their area and a million species are at risk of extinction—all largely as a result of human actions. Twenty-five percent of plant and animal species are threatened with extinction. In

6984-431: The introduced ( or hybrid ) species. Endemic populations can face such extinctions when new populations are imported or selectively bred by people, or when habitat modification brings previously isolated species into contact. Extinction is likeliest for rare species coming into contact with more abundant ones; interbreeding can swamp the rarer gene pool and create hybrids, depleting the purebred gene pool (for example,

7081-505: The lateral ones, and had a higher prominence. The osteoderms at the level of the axis vertebra (second cervical) were trapezoidal, while those at the third cervical were broad. The rest of the cervicals had elongated and rectangular osteoderms, with the paramedians being twice as long as they were wide and the lateral osteoderms being three times as long. The dorsal osteoderms were flexed, rather than perfectly flat, and were slightly longer than wide. However, dorsal osteoderms directly in front of

7178-485: The main drivers of the modern extinction crisis. In January 2020, the UN's Convention on Biological Diversity drafted a plan to mitigate the contemporary extinction crisis by establishing a deadline of 2030 to protect 30% of the Earth's land and oceans and reduce pollution by 50%, with the goal of allowing for the restoration of ecosystems by 2050. The 2020 United Nations ' Global Biodiversity Outlook report stated that of

7275-414: The midline of the body) and a single row on each side placed lateral to these paramedian rows. Most of the osteoderms were roughly textured by a radiating web of ridges and pits, although they also had a flat, smooth front edge which was thinner than the rest of the plate. The middle of each osteoderm plate had a mound-like prominence covered with small pits. The paramedian osteoderms were generally wider than

7372-421: The modern understanding of extinction as the end of a species was incompatible with the prevailing worldview. Prior to the 19th century, much of Western society adhered to the belief that the world was created by God and as such was complete and perfect. This concept reached its heyday in the 1700s with the peak popularity of a theological concept called the great chain of being , in which all life on earth, from

7469-487: The most derived non-archosaurian archosauriforms. They may have also been related to the Proterochampsidae , a South American family of crocodile-like archosauriforms. Doswelliids are believed to be semiaquatic carnivores similar to crocodilians in appearance, as evidenced by their short legs and eyes and nostrils which are set high on the head, though the putative member Scleromochlus has been interpreted as

7566-490: The name of a species or other taxon normally indicates its status as extinct. Examples of species and subspecies that are extinct include: A species is extinct when the last existing member dies. Extinction therefore becomes a certainty when there are no surviving individuals that can reproduce and create a new generation. A species may become functionally extinct when only a handful of individuals survive, which cannot reproduce due to poor health, age, sparse distribution over

7663-469: The natural course of events, species become extinct for a number of reasons, including but not limited to: extinction of a necessary host, prey or pollinator, interspecific competition , inability to deal with evolving diseases and changing environmental conditions (particularly sudden changes) which can act to introduce novel predators, or to remove prey. Recently in geological time, humans have become an additional cause of extinction of some species, either as

7760-410: The newly emerging school of uniformitarianism . Jean-Baptiste Lamarck , a gradualist and colleague of Cuvier, saw the fossils of different life forms as evidence of the mutable character of species. While Lamarck did not deny the possibility of extinction, he believed that it was exceptional and rare and that most of the change in species over time was due to gradual change. Unlike Cuvier, Lamarck

7857-399: The original population, thereby increasing the chance of extinction. Habitat degradation is currently the main anthropogenic cause of species extinctions. The main cause of habitat degradation worldwide is agriculture, with urban sprawl , logging, mining, and some fishing practices close behind. The degradation of a species' habitat may alter the fitness landscape to such an extent that

7954-466: The osteoderms of the latter group differ in the arrangement of the pits and the fact that the anterior articular lamina is formed by a raised bar. Doswellia had at least ten rows of osteoderms, creating a flattened carapace-like armor plate on its back. Jaxtasuchus had lighter armor, with only four rows. The family was originally named by R. E. Weems in 1980 and was placed in its own suborder , Doswelliina . The Doswelliidae has long been considered

8051-702: The process of speciation —where new varieties of organisms arise and thrive when they are able to find and exploit an ecological niche —and species become extinct when they are no longer able to survive in changing conditions or against superior competition . The relationship between animals and their ecological niches has been firmly established. A typical species becomes extinct within 10 million years of its first appearance, although some species, called living fossils , survive with little to no morphological change for hundreds of millions of years. Mass extinctions are relatively rare events; however, isolated extinctions of species and clades are quite common, and are

8148-410: The relative importance of genetic factors compared to environmental ones as the causes of extinction has been compared to the debate on nature and nurture . The question of whether more extinctions in the fossil record have been caused by evolution or by competition or by predation or by disease or by catastrophe is a subject of discussion; Mark Newman, the author of Modeling Extinction , argues for

8245-968: The robust structures of Erythrosuchus . The metacarpals were long and slender, but the hand was not complete enough to come to specific conclusions on its structure. The hindlimbs were also typical of generalized early archosauriforms, and the femur (thigh bone) had an apparent fourth trochanter . The metatarsals were also similar to those of Euparkeria . Cladogram after Schoch & Sues, 2013: Mesosuchus Prolacerta Proterosuchus Erythrosuchus Euparkeria Turfanosuchus Avemetatarsalia Pseudosuchia Chanaresuchus Vancleavea Tarjadia Archeopelta Doswellia Jaxtasuchus Fossils of Jaxtasuchus in Vellberg come from mudstones that were most likely deposited in brackish-water lakes or marshes. Because its fossils are common, they were probably not swept into aquatic environments from terrestrial areas. Jaxtasuchus

8342-460: The species is no longer able to survive and becomes extinct. This may occur by direct effects, such as the environment becoming toxic , or indirectly, by limiting a species' ability to compete effectively for diminished resources or against new competitor species. Habitat destruction, particularly the removal of vegetation that stabilizes soil, enhances erosion and diminishes nutrient availability in terrestrial ecosystems. This degradation can lead to

8439-430: The sudden introduction of human beings to environments full of animals that had never seen them before and were therefore completely unadapted to their predation techniques. Coextinction refers to the loss of a species due to the extinction of another; for example, the extinction of parasitic insects following the loss of their hosts. Coextinction can also occur when a species loses its pollinator , or to predators in

8536-412: The tiniest microorganism to God, is linked in a continuous chain. The extinction of a species was impossible under this model, as it would create gaps or missing links in the chain and destroy the natural order. Thomas Jefferson was a firm supporter of the great chain of being and an opponent of extinction, famously denying the extinction of the woolly mammoth on the grounds that nature never allows

8633-555: The total extinction of the dodo and the extirpation of indigenous horses to the British Isles. He similarly argued against mass extinctions , believing that any extinction must be a gradual process. Lyell also showed that Cuvier's original interpretation of the Parisian strata was incorrect. Instead of the catastrophic floods inferred by Cuvier, Lyell demonstrated that patterns of saltwater and freshwater deposits , like those seen in

8730-577: The wider scientific community of his theory. Cuvier was a well-regarded geologist, lauded for his ability to reconstruct the anatomy of an unknown species from a few fragments of bone. His primary evidence for extinction came from mammoth skulls found in the Paris basin . Cuvier recognized them as distinct from any known living species of elephant, and argued that it was highly unlikely such an enormous animal would go undiscovered. In 1812, Cuvier, along with Alexandre Brongniart and Geoffroy Saint-Hilaire , mapped

8827-493: Was covered with irregular pits and had an incision at its rear edge, likely representing the antorbital fenestra . Fragments of premaxilla and nasal bones were also preserved, with a similar texturing to the maxilla. The teeth were sharp and slightly curved. They were oval shaped in cross-section, and uniquely lacked serrations while also having pronounced longitudinal ridges along their labial and lingual (cheek- and tongue-facing) sides. A three-pronged bone has been identified as

8924-566: Was described in 2012; however, this species was subsequently transferred to the separate doswelliid genus Rugarhynchos . Two additional dosweliids were named in 2013: Jaxtasuchus salomoni based on several skeletons found in the Ladinian -age Lower Keuper of Germany, and Ankylosuchus chinlegroupensis based on fragments of four vertebrae, parts of the skull and of a limb bone from the early Carnian Colorado City Formation . Desojo, Ezcurra, & Schultz (2011)'s analysis placed Doswellidae as

9021-483: Was difficult to disprove. When parts of the world had not been thoroughly examined and charted, scientists could not rule out that animals found only in the fossil record were not simply "hiding" in unexplored regions of the Earth. Georges Cuvier is credited with establishing the modern conception of extinction in a 1796 lecture to the French Institute , though he would spend most of his career trying to convince

9118-409: Was formed by the basioccipital bone, projected from the rest of the skull (in contrast with Archeopelta ), and the paired exoccipital bones which lied upon it did not contact each other (similar to other doswelliids). While Doswellia had a pronounced peg-like extension on the rear surface of the supraoccipital bone , Jaxtasuchus only had a vertical ridge. The only preserved bone of the lower jaw

9215-430: Was not until 1982, when David Raup and Jack Sepkoski published their seminal paper on mass extinctions, that Cuvier was vindicated and catastrophic extinction was accepted as an important mechanism . The current understanding of extinction is a synthesis of the cataclysmic extinction events proposed by Cuvier, and the background extinction events proposed by Lyell and Darwin. Extinction is an important research topic in

9312-557: Was semiaquatic like modern crocodilians . Fossils of Jaxtasuchus have been found in the Lower Keuper of southern Germany, which dates back to the end of the Middle Triassic. The osteoderms of Jaxtasuchus were originally interpreted as the dermal bones of temnospondyl amphibians and later as the plates of aetosaur reptiles. The only other archosauriforms currently known from the Lower Keuper are Zanclodon laevis , which

9409-571: Was skeptical that catastrophic events of a scale large enough to cause total extinction were possible. In his geological history of the earth titled Hydrogeologie, Lamarck instead argued that the surface of the earth was shaped by gradual erosion and deposition by water, and that species changed over time in response to the changing environment. Charles Lyell , a noted geologist and founder of uniformitarianism , believed that past processes should be understood using present day processes. Like Lamarck, Lyell acknowledged that extinction could occur, noting

#418581