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Author Topic: Origin of Mankind  (Read 137 times)
Description: From mammal-like reptiles: a process of over 70 million years
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« on: September 07, 2007, 11:31:40 AM »

Space pile-up 'condemned dinos'



How mammals got their big break

A colossal collision in space 160 million years ago set the dinosaurs on the path to extinction, a study claims.

An asteroid pile-up sent debris swirling around the Solar System, including a chunk that later smashed into Earth wiping out the great beasts.

Other fragments crashed into the Moon, Venus and Mars, gouging out some of their most dominant impact craters, a US-Czech research team believes.

Its study, based on computer modelling, is reported in the journal Nature.

Nature 449, 48-53 (6 September 2007) | doi:10.1038/nature06070
An asteroid breakup 160 Myr ago as the probable source of the K/T impactor

William F. Bottke1, David Vokrouhlick�1,2  &  David Nesvorn�1

   1. Southwest Research Institute, 1050 Walnut St, Suite 300, Boulder, Colorado 80302, USA
   2. Institute of Astronomy, Charles University, V Holes caronovic caronk�ch 2, 18000 Prague 8, Czech Republic

Correspondence to: William F. Bottke1 Correspondence and requests for materials should be addressed to W.F.B. (Email: ).
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Abstract

The terrestrial and lunar cratering rate is often assumed to have been nearly constant over the past 3 Gyr. Different lines of evidence, however, suggest that the impact flux from kilometre-sized bodies increased by at least a factor of two over the long-term average during the past approx100 Myr. Here we argue that this apparent surge was triggered by the catastrophic disruption of the parent body of the asteroid Baptistina, which we infer was a approx170-km-diameter body (carbonaceous-chondrite-like) that broke up Unfortunately we are unable to provide accessible alternative text for this. If you require assistance to access this image, or to obtain a text description, please contact Myr ago in the inner main asteroid belt. Fragments produced by the collision were slowly delivered by dynamical processes to orbits where they could strike the terrestrial planets. We find that this asteroid shower is the most likely source (>90 per cent probability) of the Chicxulub impactor that produced the Cretaceous/Tertiary (K/T) mass extinction event 65 Myr ago.

Southwest Research Institute (SwRI) News
New research reveals a large asteroid breakup to be the likely source of the impactor that caused a mass extinction event on Earth 65 million years ago

Boulder, Colo. � Sept. 6, 2007 � The impactor believed to have wiped out the dinosaurs and other life forms on Earth some 65 million years ago has been traced back to a breakup event in the main asteroid belt. A joint U.S.-Czech team from Southwest Research Institute (SwRI) and Charles University in Prague suggests that the parent object of asteroid (298) Baptistina disrupted when it was hit by another large asteroid, creating numerous large fragments that would later create the Chicxulub crater on the Yucatan Peninsula as well as the prominent Tycho crater found on the Moon.

The team of researchers, including Dr. William Bottke (SwRI), Dr. David Vokrouhlicky (Charles University, Prague) and Dr. David Nesvorny (SwRI), combined observations with several different numerical simulations to investigate the Baptistina disruption event and its aftermath. A particular focus of their work was how Baptistina fragments affected the Earth and Moon.

At approximately 170 kilometers in diameter and having characteristics similar to carbonaceous chondrite meteorites, the Baptistina parent body resided in the innermost region of the asteroid belt when it was hit by another asteroid estimated to be 60 kilometers in diameter. This catastrophic impact produced what is now known as the Baptistina asteroid family, a cluster of asteroid fragments with similar orbits. According to the team's modeling work, this family originally included approximately 300 bodies larger than 10 kilometers and 140,000 bodies larger than 1 kilometer.

Once created, the newly formed fragments� orbits began to slowly evolve due to thermal forces produced when they absorbed sunlight and re-radiated the energy away as heat. According to Bottke, "By carefully modeling these effects and the distance traveled by different-sized fragments from the location of the original collision, we determined that the Baptistina breakup took place 160 million years ago, give or take 20 million years."

The gradual spreading of the family caused many fragments to drift into a nearby "dynamical superhighway" where they could escape the main asteroid belt and be delivered to orbits that cross Earth�s path. The team's computations suggest that about 20 percent of the surviving multi-kilometer-sized fragments in the Baptistina family were lost in this fashion, with about 2 percent of those objects going on to strike the Earth, a pronounced increase in the number of large asteroids striking Earth.

Support for these conclusions comes from the impact history of the Earth and Moon, both of which show evidence of a two-fold increase in the formation rate of large craters over the last 100 to 150 million years. As described by Nesvorny, "The Baptistina bombardment produced a prolonged surge in the impact flux that peaked roughly 100 million years ago. This matches up pretty well with what is known about the impact record."

Bottke adds, "We are in the tail end of this shower now. Our simulations suggest that about 20 percent of the present-day, near-Earth asteroid population can be traced back to the Baptistina family."

The team then investigated the origins of the 180 kilometer diameter Chicxulub crater, which has been strongly linked to the extinction of the dinosaurs 65 million years ago. Studies of sediment samples and a meteorite from this time period indicate that the Chicxulub impactor had a carbonaceous chondrite composition much like the well-known primitive meteorite Murchison. This composition is enough to rule out many potential impactors but not those from the Baptistina family. Using this information in their simulations, the team found a 90 percent probability that the object that formed the Chicxulub crater was a refugee from the Baptistina family.

These simulations also showed there was a 70 percent probability that the lunar crater Tycho, an 85 kilometer crater that formed 108 million years ago, was also produced by a large Baptistina fragment. Tycho is notable for its large size, young age and its prominent rays that extend as far as 1,500 kilometers across the Moon. Vokrouhlicky says, "The probability is smaller than in the case of the Chicxulub crater because nothing is yet known about the nature of the Tycho impactor."

This study demonstrates that the collisional and dynamical evolution of the main asteroid belt may have significant implications for understanding the geological and biological history of Earth.

As Bottke says, "It is likely that more breakup events in the asteroid belt are connected in some fashion to events on the Earth, Moon and other planets. The hunt is on!"

The article, "An asteroid breakup 160 Myr ago as the probable source of the K/T impactor," was published in the Sept. 6 issue of Nature.

The NASA Origins of Solar Systems, Planetary Geology and Geophysics, and Near-Earth Objects Observations programs funded Bottke's and Nesvorny's research; Vokrouhlicky was funded by the Grant Agency of the Czech Republic.

Editors: Images to accompany this story are available at http://www.swri.org/press/2007/asteroid.htm.

For more information contact Maria Martinez at (210) 522-3305, Communications Department, Southwest Research Institute, PO Drawer 28510, San Antonio, TX 78228-0510.
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« Reply #1 on: September 07, 2007, 11:45:52 AM »


Side-by-side of Shuttle Radar Topography Mission data (top) and Landsat data (bottom), Yucatan Peninsula, Mexico

Chicxulub Crater

Chicxulub Crater (IPA: /tʃikʃu'lub/) (cheek-shoo-LOOB) is an ancient impact crater buried underneath the Yucat�n Peninsula, with its center located approximately underneath the town of Chicxulub, Yucat�n, Mexico.

Investigations suggest that this impact structure is dated from the late Cretaceous Period, about 65 million years ago. Thus the meteorite associated with the crater is implicated in causing the extinction of the dinosaurs as suggested by the K-T boundary.

Impact specifics

The meteorite's estimated size was about 10 km (6 mi) in diameter, releasing an estimated 500 zettajoules (5.0�1023 joules) of energy, approximately 100 teratons of TNT (1014 tons),[1] on impact. By contrast, the most powerful man-made explosive device ever detonated, the Tsar Bomba or Emperor Bomb, had a yield of only 50 megatons, which would make this impact 2,000,000 times more powerful.

The impact would have caused some of the largest megatsunamis in Earth's history. These would have spread in all directions, hitting the Caribbean island of Cuba especially hard. A cloud of dust, ash and steam would spread itself from the crater. The pieces of the meteorite would have rained all over Earth, igniting global wildfires. The shock waves would have continued hundreds of kilometers into the planet, causing global earthquakes and volcanic eruptions. The emission of dust and particles covered the entire surface of the earth for several years, possibly a decade, creating a harsh environment. (Pope, et al., 1997)

Extinction of the dinosaurs

This timing is in good agreement with the theory postulated by the late physicist Luis Alvarez and his son, geologist Walter Alvarez, for the extinction of the dinosaurs. The Alvarezes, at the time both faculty members at the University of California, Berkeley, postulated that the extinction of the dinosaurs, roughly contemporaneous with the K-T boundary, could have been caused by the impact of just such a large meteorite. This theory is now widely, though not universally, accepted by the scientific community.[2]

The main evidence is a widespread, thin layer of clay present in this geological boundary across the world. In the late 1970s, the Alvarezes and colleagues reported[3] that it contained an abnormally high concentration of iridium � 6 parts per billion by weight or more compared to 0.4[4] for the Earth's crust as a whole. Meteorites can contain around 470 parts per billion[5] of this element. It was hypothesised that the iridium was spread into the atmosphere when the meteorite was vapourised and settled across the Earth's surface amongst other material thrown up by the impact, producing the relatively iridium-rich layer of clay.[6]

Discovery

Clues in Haitian rock

In early 1990, Alan R. Hildebrand, a graduate student at the University of Arizona, visited a small mountain village named Beloc in Haiti. He was investigating certain K-T deposits that include thick, jumbled deposits of coarse rock fragments, which were apparently scoured up from one location and deposited elsewhere by a kilometers-high tsunami that most likely resulted from an Earth impact. Such deposits occur in many locations but seem to be concentrated in the Caribbean Basin.

Hildebrand found a greenish brown coloured clay with an excess of iridium and containing shocked quartz grains and small beads of weathered glass that appeared to be tektites. He and his faculty adviser, William V. Boynton, published the results of the research in the scientific press[7], suggesting that the deposits were the result of an Earth impact and that the impact could not have been more than 1,000 kilometers (620 mi) away.

No crater was known to exist in the Caribbean basin. However Hildebrand and Boynton also reported their findings to an international geological conference, sparking substantial interest. Evidence pointed to possible crater sites off the north coast of Colombia or near the western tip of Cuba. Then Carlos Byars, a reporter for the Houston Chronicle, contacted Hildebrand and told him that a geophysicist named Glen Penfield had discovered what might be the impact crater in 1978, buried under the northern Yucat�n Peninsula.



Discovery of "arc"

In that year, Penfield had been working for Petroleos Mexicanos (PEMEX, the Mexican state-owned oil company) as a staff member for an airborne magnetic survey of the Yucat�n Peninsula. When Penfield examined the survey data, he found a huge underground "arc", with its ends pointing south, in the Caribbean off the Yucatan that was inconsistent with the region's geology.

Penfield then obtained a gravity map of the Yucatan that had been made in the 1960s. He found another arc, but this one was on the Yucatan itself, and its ends pointed north. He matched up the two maps and found that the two arcs joined up in a circle, 180 kilometers (112 miles) wide, with its center at the village of Puerto Chicxulub.

Although PEMEX would not allow him to release specific data, the company did allow him and PEMEX official Antonio Camargo to present their results at a geological conference in 1981. The conference was under-attended in that year, ironically because most geologists were attending a workshop on Earth impacts, and their report attracted very little attention, though it did get back to Byars.

Penfield knew that PEMEX had drilled exploratory wells in the region in 1951. One of the wells had bored into a thick layer of andesite about 1.3 kilometers (4,200 ft) down. Such a structure could have resulted from the intense heat and pressures of an Earth impact, but at the time of the borings it had been written off as a "volcanic dome", even though such a feature was out of place in the geology of the region.

Correlation of data

After Hildebrand got in touch with Penfield, the two men were able to locate two separate samples from the wells drilled by PEMEX in 1951. Analysis of the samples clearly showed shock-metamorphic materials. Studies by other geologists of the debris found in Haiti at Beloc also showed it to be clearly the result of an impact.


SIR-C data of Yucatan impact crater site

Satellite surveys

In 1996, a team of California researchers, including Kevin O. Pope, Adriana Ocampo, and Charles Duller, conducted a survey of satellite images of the region. They found that there was a ring of sinkholes centered on Puerto Chicxulub that matched the ring Penfield had found in his data. The sinkholes were likely caused by subsidence of the crater's wall. (Pope, et al., 1996)

Further studies have reinforced the consensus. Indeed, some evidence has accumulated that the actual crater is 300 kilometers (186 miles) wide, and the 180 kilometer ring is just an inner wall. (Sharpton & Marin, 1997)

Multiple impact theory

In recent years, several other craters of around the same age as Chicxulub have been discovered, all between latitudes 20�N and 70�N. Examples include the Silverpit crater in the United Kingdom, and the Boltysh crater in Ukraine, both much smaller than Chicxulub but likely to have been caused by objects many tens of metres across striking the Earth. This has led to the hypothesis that the Chicxulub impact may have been only one of several impacts that happened all at the same time. Another possible crater thought to have been formed at the same time is the Shiva crater, though the structure's status as a crater is contested.

The collision of Comet Shoemaker-Levy 9 with Jupiter in 1994 proved that gravitational interactions can fragment a comet, giving rise to many impacts over a period of a few days if the comet should collide with a planet. Comets frequently undergo gravitational interactions with the gas giants, and similar disruptions and collisions are very likely to have occurred in the past. This scenario may have occurred on Earth 65 million years ago.

In late 2006, Ken MacLeod, a geology professor from the University of Missouri�Columbia, completed an analysis of sediment below the ocean's surface bolstering the single-impact theory. MacLeod conducted his analysis approximately 4,500 kilometers (2,800 mi) from the Chicxulub Crater to control for possible changes in soil composition at the impact site while still close enough to be affected by the impact. The analysis revealed there was only one layer of impact debris in the sediment, indicating only one impact. Reuters quoted Multiple Impact proponent Gerta Keller as saying, "Unfortunately, these claims are rather hyper-inflated and do not withstand close examination."[8]

Possible origin of asteroid

On September 5, 2007 a report was issued that stated a possible origin of the asteroid that caused the Chicxulub Crater formation. A possible asteroid collision event, believed to have occurred 160 million years ago in the asteroid belt, that also resulted in the formation of the asteroid known as 298 Baptistina, might have sent the "Chicxulub asteroid" on a path which eventually reached the Earth, from a collision that broke up a much larger body believed to be about 170 km (105 miles) across, with the impacting body being of a possible 60 km (37 miles) across size.[1]

References

   1.  Bralower, Timothy J.; Charles K. Paull and R. Mark Leckie (1998). "The Cretaceous-Tertiary boundary cocktail: Chicxulub impact triggers margin collapse and extensive sediment gravity flows".
   2.  The Chicxlub debate, Princeton University website
   3.  W., Alvarez; L.W. Alvarez, F. Asaro, and H.V. Michel (1979). "Anomalous iridium levels at the Cretaceous/Tertiary boundary at Gubbio, Italy: Negative results of tests for a supernova origin". Christensen, W.K., and Birkelund, T. Cretaceous/Tertiary Boundary Events Symposium: 69, volume 2.
   4.  webelements.com, Geological abundance of iridium
   5.  QIV.inc periodic table
   6.  Asteroid Rained Glass Over Entire Earth, Scientists Say, National Geographic News, 15 May 2005
   7.  Chicxulub Crater; a possible Cretaceous/Tertiary boundary impact crater on the Yucatan Peninsula, Mexico, from Google Scholar
   8.  http://www.cnn.com/2006/TECH/space/12/01/asteroid.dinosaurs.reut/index.html

    * Pope KO, Baines KH, Ocampo AC, Ivanov BA (1997). "Energy, volatile production, and climatic effects of the Chicxulub Cretaceous/Tertiary impact". Journal of Geophysical Research 102 (E9): 21645-64. PMID 11541145.
    * Pope KO, Ocampo AC, Kinsland GL, Smith R (1996). "Surface expression of the Chicxulub crater". Geology 24 (6): 527-30. PMID 11539331.
    * Rojas-Consuegra, R., M. A. Iturralde-Vinent, C. D�az-Otero y D. Garc�a-Delgado (2005). "Significaci�n paleogeogr�fica de la brecha basal del L�mite K/T en Loma Dos Hermanas (Loma del Capiro), en Santa Clara, provincia de Villa Clara. I Convenci�n Cubana de Ciencias de la Tierra.". GEOCIENCIAS 8 (6): 1-9. ISBN 959-7117-03-7.
    * Sharpton VL, Marin LE (1997). "The Cretaceous-Tertiary impact crater and the cosmic projectile that produced it". Annals of the New York Academy of Sciences 822: 353-80. PMID 11543120.
    * Single Massive Asteroid Wiped Out Dinosaurs Reuters, December 1, 2006
    * The Chixulub Debate
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« Reply #2 on: September 07, 2007, 11:51:26 AM »


The skull is just 12 millimetres long

Fossil hints at mammal evolution

A team of scientists from China and the United States has described a tiny fossil creature that could be one of the ancestors of modern mammals.

The shrew-like animal would have run under the feet of dinosaurs at the start of the Jurassic period, nearly 195 million years ago.

The fossil was found in Yunnan province in China and has been given the name Hadrocodium wui, meaning Fullhead.

Full is a relative term; the animal weighed only about two grams - the same as the smallest land mammal living today. Its skull was just 12mm long

It probably ate the same sorts of things as today's shrews, said lead researcher Dr Zhe-Xi Luo of the Carnegie Museum of Natural History.

Fossil record

He told the BBC: "This was an insectivore It has very fragile teeth, and limited by its very tiny size, it was only capable of eating small insects, small worms, and not much of anything else."

But the animal had, for its size, a significantly bigger brain than the more primitive mammals already known from the early Jurassic.

Writing in the journal Science, Dr Luo and his colleagues say they are particularly excited by the creature's middle ear bones, which are separated from the lower jaw, a key evolutionary difference between mammals and reptiles.

The discovery of this important feature in Hadrocodium wui pushes back by another 40 million years its first appearance in the fossil record.

The researchers argue that an expanding brain in an evolving creature could force the ear bones to move apart.


The anatomy of the cranium in Hadrocodium wui suggests the animal used its newfound brain power for hearing and smelling; both areas of the brain are well-developed.

When it scurried about, the Earth's domination by dinosaurs still had many millions of years to run.

The ancestral mammals had yet to diverge into the present-day groups - placentals, like humans, horses and whales; marsupials, like kangaroos; and monotremes, such as the duck-billed platypus.

Dr Luo said: "Hadrocodium could be our distant cousin, an early mammal that existed alongside the ancestor of living mammals.

"Or it could be our great-great grand uncle, closely related to living mammals but not in our direct lineage.

"Or Hadrocodium could be the direct ancestor of living mammals. The fossil evidence can't distinguish between these three possibilities. But we are satisfied to know that Hadrocodium is the sister taxon (closest known relative) to all living mammals," said Dr Luo.
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« Reply #3 on: September 07, 2007, 11:54:33 AM »


Pangea

Mammal Evolution

All modern mammals evolved from a group of reptiles that lived more than 200 million years ago. Over time these reptiles developed the various adaptations that define mammals today: the skull and jaw bones were rearranged, they developed different types of teeth, they brought the limbs underneath the body rather than sprawling out to the sides, and they developed a diaphragm and palate to help them breathe efficiently and eat at the same time. At some point during their development, the mammals also started to regulate their own body temperature through internal heat production and started to feed their young with milk. Since these are features which don't fossilise it is impossible to say when these changes occurred.

the world of mesozoic mammals The world of these early mammals was very different from the world today. There was only one continent on Earth, and the climate was much warmer. The other animals around at the time were the first dinosaurs, and many other reptilian groups. Invertebrates had been around for a very long time and were very diverse, as were the fish. There were no flowers, but plenty of non-flowering plants.

The first mammals were small, and probably nocturnal since their internal heat production allowed them to stay active even when the temperatures dropped at night. They used their sense of smell to find prey and each other.

By about 100 million years ago there were several types of mammal. We are familiar with the monotremes, marsupials and placentals of today, but there were also other kinds, such as multituberculates, which are now extinct. The world was changing, though. The one mass of land began to break up, and the separating continents took with them living cargoes of animals.



The first split was a north-south divide. North America and Eurasia broke away from South America, Africa, Australia and Antarctica. Then Africa broke away from the Southern continent, and India too went adrift. Placental mammals were divided and started to develop in four different ways.

elephants are Afrotheres In Africa, a group developed known as the Afrotheres. Today these are represented by the elephants, the sea cows, the elephant shrews, the golden moles, the tenrecs and the aardvark. In South America, a group known as the Xenarthrans developed, today represented by the anteaters, sloths and armadillos. Across North America and Eurasia lived the Laurasiatherians, a large group containing the carnivores, hoofed animals, whales, bats and other animals. Also in the north lived the fourth group known as the Euarchontaglires: the rodents and primates.

The marsupials were not confined to the Southern hemisphere as they are today. Opossums lived in Europe and North America and even invaded Africa when it finally came into contact with Europe around 30 million years ago. The monotremes have a much poorer fossil record, and so it is not known how diverse and widespread they might once have been.

rodents spread across the globe Having split apart, the continents eventually started to collide with each other, and their different groups of mammals started to mix. First Africa collided with Europe. Primates, hoofed animals and carnivores flooded in, while elephants and other Afrotheres spread north. Then South America and North America touched, allowing Xenarthrans like the giant ground sloths and armadillos to move north, whilst hoofed animals and carnivores moved into South America.
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« Reply #4 on: September 07, 2007, 01:19:19 PM »

The evolution of mammals from synapsids (mammal-like reptiles) was a gradual process which took approximately 70 million years, from the mid-Permian to the mid-Jurassic, and by the mid-Triassic there were many species that looked like mammals.

From the point of view of cladistics, mammals are the only surviving synapsids.


Restoration of Thrinaxodon, a member of the cynodont group which includes the ancestors of mammals

Here is a very simplified "family tree" - the text below describes some of the uncertainties and areas of debate.

--Tetrapods--------------------------------------------------
      |
      +-- Amphibians ---------------------------------------
      |
      `--Amniotes-----
             |
             +--Sauropsids------------------------------------
             |
             `--Synapsids------
                    |
                    `--Pelycosaurs----
                           |
                           `--Therapsids-----
                                  |
                                  `--Mammals------------------

Therapsids

Therapsids

Therapsids descended from pelycosaurs in the middle Permian and took over their position as the dominant land vertebrates. They differ from pelycosaurs in several features of the skull and jaws, including: larger temporal fenestrae; incisors which are equal in size.[7]

The therapsids went through a series of stages, beginning with animals which were very like their pelycosaur ancestors and ending with some which could easily be mistaken for mammals:

    * gradual development of a bony secondary palate.[8] Most books and articles interpret this as a prequisite for the evolution of mammals' high metabolic rate, because it enabled these animals to eat and breathe at the same time. But some scientists point out that some modern ectotherms use a fleshy secondary palate to separate the mouth from the airway, and that a bony palate provides a surface on which the tongue can manipulate food, facilitating chewing rather than breathing.[9] The interpretation of the bony secondary palate as an aid to chewing also suggests the development of a faster metabolism, since chewing makes it possible to digest food more quickly. In mammals the palate is formed by two specific bones, but various Permian therapsids had other combinations of bones in the right places to function as a palate.
    * the dentary gradually becomes the main bone of the lower jaw.
    * progress towards an erect limb posture, which would increase the animals' stamina by avoiding Carrier's constraint. But this process was erratic - for example: all herbivorous therapsids retained sprawling limbs (some late forms may have had semi-erect hind limbs); Permian carnivorous therapsids had sprawling forelimbs, and some late Permian ones also had semi-sprawling hindlimbs. In fact modern monotremes still have semi-sprawling limbs.
    * in the Triassic, progress towards the mammalian jaw and middle ear.
    * there is plausible evidence of hair in Triassic therapsids, but none for Permian therapsids.
    * some scientists have argued that some Triassic therapsids show signs of lactation.

Therapsid family tree

(simplified from [10]; only those which are most relevant to the evolution of mammals are described below)

Therapsids
  |
  +--Biarmosuchia
  |
  `--+--Dinocephalia
     |
     +--Neotherapsida
          |
          +--Anomodonts
          |      |
          |      `--Dicynodonts
          |
          `--+--Theriodontia
                    |
                    +--Gorgonopsia
                    |
                    `--+--Therocephalia
                       |
                       `--Cynodontia
                              .
                              . . . (Mammals, eventually)

Only the dicynodonts, therocephalians and cynodonts survived into the Triassic.

Triassic takeover

The catastrophic Permian-Triassic mass extinction killed off about 70 percent of terrestrial vertebrate species, and the majority of land plants. As a result:[14]

    * Ecosystems and food chains collapsed, and the recovery took about 6 million years.
    * The survivors had re-start the struggle for dominance of their former ecological niches - even the cynodonts, which had seemed on the way to dominance at the end of the Permian.

But the cynodonts lost out to a previously obscure group of sauropsids, the archosaurs (which include the ancestors of crocodilians, dinosaurs and birds). This reversal of fortunes is often called the "Triassic takeover". Several explanations have been offered for it, but the most likely is that the early Triassic was predominantly arid and therefore archosaurs' superior water conservation gave them a decisive advantage (all known sauropsids have glandless skins and excrete uric acid, which requires less water to keep it sufficiently liquid than the urea which mammals excrete and presumably therapsids excreted).[15] The Triassic takeover was gradual - in the earliest part of the Triassic cynodonts were the main predators and lystrosaurs were the main herbivores, but by the mid-Triassic archosaurs dominated all the large carnivore and herbivore niches.

But the Triassic takeover may have been a vital factor in the evolution of cynodonts into mammals. The cynodonts' descendants were only able to survive as small, mainly nocturnal insectivores.[16] As a result:

    * The therapsid trend towards differentiated teeth with precise occlusion accelerated, because of the need to hold captured arthropods and crush their exoskeletons.
    * Nocturnal life required advances in thermal insulation and temperature regulation to enable the ancestors of mammals to be active in the cool of the night.
    * Acute senses of hearing and smell became vital.
          o This accelerated the development of the mammalian middle ear, and therefore of the mammalian jaw since bones which had been part of the jaw joint became part of the middle ear.
          o The increase in the size of the olfactory and auditory lobes of the brain increased brain weight as a total percentage of body weight. Brain tissue requires a disproportionate amount of energy.[17][18] The need for more food to support the enlarged brains increased the pressures for improvements in insulation, temperature regulation and feeding.
    * As a side-effect, sight became slightly less important, and this is reflected in the fact that most mammals have poor color vision, including the "lower primates" such as lemurs.[19]

From cynodonts to true mammals

Many uncertainties

While the Triassic takeover probably accelerated the evolution of mammals, it made life more difficult for paleontologists because good fossils of the nearly-mammals are extremely rare, mainly because they were mostly smaller than rats:

    * They were largely restricted to environments which are less likely to provide good fossils. The best terrestrial environments for fossilization are floodplains, where seasonal floods quickly cover dead animals in a protective layer of silt which is later compressed into sedimentary rock. But floodplains are dominated by medium to large animals, and the Triassic therapsids and near-mammals could not compete with archosaurs in the medium to large size range.
    * Their delicate bones were vulnerable to being destroyed before they could be fossilized - by scavengers (including fungi and bacteria) and by being trodden on.
    * Small fossils are harder to spot and more vulnerable to being destroyed by weathering and other natural stresses before they are discovered.

In fact it was said as recently as the the 1980s that all the Mesozoic fossils of mammals and near-mammals could be contained in a few shoeboxes - and they were mostly teeth, which are the most durable of all bones.[20]

As a result:

    * In many cases it is difficult to assign a Mesozoic mammal or near-mammal fossil to a genus.
    * All the available fossils of a genus seldom add up to a complete skeleton, and hence it is difficult to decide which genera are most like each other and therefore most likely to be closely-related. In other words, it becomes very difficult to classify them by means of cladistics, which is the most reliable and least subjective method currently available.

So the evolution of mammals in the Mesozoic is full of uncertainties, although there is no room for doubt that true mammals did first appear in the Mesozoic.

Mammals or mammaliformes?

One result of these uncertainties has been a change in the paleontologists' definition of "mammal". For a long time a fossil was considered a mammal if it met the jaw-ear criterion (the jaw joint consists only of the squamosal and dentary; and the articular and the quadrate bones have become the middle ear's malleus and incus). But more recently paleontologists have usually defined "mammal" as the last common ancestor of monotremes, marsupials and placentals and all of its descendants. So they had to define another clade mammaliformes to accommodate all the animals which are more mammal-like than cynodonts but less closely related to monotremes, marsupials and placentals.[21] Although this now appears to be the majority approach, some paleontologists have resisted it because: it simply moves most of the problems into the new clade without solving them; the clade mammaliformes includes some animals with "mammalian" jaw joints and some with "reptilian" (articular-to-quadrate) jaw joints; and the newer definition of "mammal" and "mammaliformes" depend on last common ancestors of both groups which have not yet been found.[22] Despite these objections, this article follows the majority approach and treats most of the cynodonts' Mesozoic descendants as mammaliformes.

Family tree - cynodonts to mammals

(based on Mammaliformes - Palaeos)

--Cynodonts
    |
    `--Mammaliformes
         |
         +--Allotheria
         |    |
         |    `--Multituberculates
         |
         `--+--Morganucodontidae
            |
            `--+--Docodonta
               |
               `--+--Hadrocodium
                  |
                  `--Symmetrodonta
                       |
                       |--Kuehneotheriidae
                       |
                       `--Mammals

The earliest true mammals

This part of the story introduces new complications, since true mammals are the only group which still has living members:

    * One has to distinguish between extinct groups and those which have living representatives.
    * One often feels compelled to try to explain the evolution of features which do not appear in fossils. This endeavor often involves Molecular phylogenetics, a technique which has become popular since the mid-1980s but is still often controversial because of its assumptions, especially about the reliability of the molecular clock.

Family tree of early true mammals

(based on Mammalia: Overview - Palaeos; X marks extinct groups)

--Mammals
    |
    +--Australosphenida
    |    |
    |    +--Ausktribosphenidae X
    |    |
    |    `--Monotremes
    |
    `--+--Triconodonta X
       |
       `--+--Spalacotheroidea X
          |
          `--Cladotheria
               |
               |--Dryolestoidea X
               |
               `--Theria
                    |
                    +--Metatheria
                    |
                    `--Eutheria

Evolution of major groups of living mammals

There are currently vigorous debates between traditional paleontologists ("fossil-hunters") and molecular phylogeneticists about how and when the true mammals diversified, especially the placentals. Generally the traditional paelontologists date the appearance of a particular group by the earliest known fossil whose features make it likely to be a member of that group, while the molecular phylogeneticists suggest that each lineage diverged earlier (usually in the Cretaceous) and that the earliest members of each group were anatomically very similar to early members of other groups and differed only in their genes. These debates extend to the definition of and relationships between the major groups of placentals - the controversy about Afrotheria is a good example.

Fossil-based family tree of placental mammals

Here is a very simplified version of a typical family tree based on fossils, based on Cladogram of Mammalia - Palaeos. Paleontologists agree about most of it, especially the major groups, but still have some debates about the details.

For the sake of brevity and simplicity the diagram omits some extinct groups in order to focus on the ancestry of well-known modern groups of placentals - X marks extinct groups. The diagram also shows:

    * the age of the oldest known fossils in many groups, since one of the major debates between traditional paleontologists and molecular phylogeneticists is about when various groups first became distinct.
    * well-known modern members of most groups.

--Eutheria
    |
    +--Xenarthra (Paleocene)
    |  (armadillos, anteaters, sloths)
    |
    `--+--Pholidota (early Eocene)
       |  (pangolins)
       |
       `--Epitheria (late Cretaceous)
          |
          |--(some extinct groups) X
          |
          `--+--Insectivora (late Cretaceous)
             |  (hedgehogs, shrews, moles, tenrecs)
             |
             `--+--+--Anagalida
                |  |  |
                |  |  +--Zalambdalestidae X (late Cretaceous)
                |  |  |
                |  |  `--+--Macroscelidea (late Eocene)
                |  |     |  (elephant shrews)
                |  |     |
                |  |     `--+--Anagaloidea X
                |  |        |
                |  |        `--Glires (early Paleocene)
                |  |             |
                |  |             +--Lagomorpha (Eocene)
                |  |             |  (rabbits, hares, pikas)
                |  |             |
                |  |             `--Rodentia (late Paleocene)
                |  |                (mice & rats, squirrels,
                |  |                 porcupines)
                |  |           
                |  `--Archonta
                |       |
                |       |--+--Scandentia (mid [Eocene])
                |       |  |  (tree shrews)
                |       |  |
                |       |  `--Primatomorpha
                |       |       |
                |       |       +--Plesiadapiformes X
                |       |       |
                |       |       `--Primates (early Paleocene)
                |       |          (tarsiers, lemurs, monkeys,
                |       |            apes, humans)
                |       |
                |       `--+--Dermoptera (late Eocene)
                |          |  (colugos)
                |          |
                |          `--Chiroptera (late Paleocene)
                |             (bats)
                |
                `--+--Ferae (early Paleocene)
                   |  (cats, dogs, bears, seals)
                   |
                   `--Ungulatomorpha (late Cretaceous)
                        |
                        +--Eparctocyona (late Cretaceous)
                        |  |
                        |  +--(some extinct groups) X
                        |  |
                        |  `--+--Arctostylopida X (late Paleocene)
                        |     |
                        |     `--+--Mesonychia X (mid Paleocene)
                        |        | (predators / scavengers,
                        |        |  but not closely related
                        |        |  to modern carnivores)
                        |        |
                        |        `--Cetartiodactyla
                        |           |
                        |           +--Cetacea (early Eocene)
                        |           |  (whales, dolphins, porpoises)
                        |           |
                        |           `--Artiodactyla (early Eocene)
                        |              (even-toed ungulates:
                        |               pigs, hippos, camels,
                        |               giraffes,  cattle, deer)
                        |
                        `--Altungulata
                             |
                             +--Hilalia X
                             |
                             `--+--+--Perissodactyla (late Paleocene)
                                |  |    (odd-toed ungulates:
                                |  |     horses, rhinos, tapirs)
                                |  |
                                |  `--Tubulidentata (early Miocene)
                                |     (aardvarks)
                                |
                                `--Paenungulata ("not quite ungulates")
                                     |
                                     +--Hyracoidea (early Eocene)
                                     |  (hyraxes)
                                     |
                                     `--+--Sirenia (early Eocene)
                                        |  (manatees, dugongs)
                                        |
                                        `--Proboscidea (early Eocene)
                                           (elephants)

This family tree contains some surprises and puzzles. For example:

    * The closest living relatives of cetaceans (whales, dolphins, porpoises) are artiodactyls, hoofed animals which are almost all pure vegetarians.
    * Bats are fairly close relatives of primates.
    * The closest living relatives of elephants are the aquatic sirenians, while their next relatives are hyraxes, which look more like well-fed guinea pigs.
    * There is little correspondence between the structure of the family (what was descended from what) and the dates of the earliest fossils of each group. For example the earliest fossils of perissodactyls (the living members of which are horses, rhinos and tapirs) date from the late Paleocene but the earliest fossils of their "sister group" the Tubulidentata date from the early Miocene, nearly 50M years later. Paleontologists are fairly confidents about the family relationships, which are based on cladistic analyses, and believe that fossils of the ancestors of modern aardvarks have simply not been found yet.

Family tree of placental mammals according to molecular phylogenetics

Molecular phylogenetics uses features of organisms's genes to work out family trees in much the same way as paleontologists do with fossils - if two organisms' genes / fossil features are more similar to each other than to those of a third organism, the two organisms are more closely related to each other than to the third.

Molecular phylogeneticists have proposed a family tree which is very different from the one with which paleontologists are familiar. Like paleontologists, molecular phylogeneticists have different ideas about various details, but here is a typical family tree according to molecular phylogenetics:[49][50] Note that the diagram shown here omits extinct groups, as one cannot extract DNA from fossils.

--Eutheria
   |
   +--Atlantogenata ("born round the Atlantic ocean")
   |    |
   |    +--Xenarthra (armadillos, anteaters, sloths)
   |    |
   |    `--Afrotheria
   |       |
   |       +--Afroinsectiphilia
   |       |   (golden moles, tenrecs, otter shrews)
   |       |
   |       +--Pseudungulata ("false ungulates")
   |       |    |
   |       |    +--Macroscelidea (elephant shrews)
   |       |    |
   |       |    `--Tubulidentata (aardvarks)
   |       |
   |       `--Paenungulata ("not quite ungulates")
   |            |
   |            +--Hyracoidea (hyraxes)
   |            |
   |            +--Proboscidea (elephants)
   |            |
   |            `--Sirenia (manatees, dugongs)
   |
   `--Boreoeutheria ("northern true / placental mammals")
        |
        +--Laurasiatheria
        |    |
        |    +--Erinaceomorpha (hedgehogs, gymnures)
        |    |
        |    +--Soricomorpha (moles, shrews, solenodons)
        |    |
        |    +--Cetartiodactyla
        |    |  (cetaceans and even-toed ungulates)
        |    |
        |    `--Pegasoferae
        |         |
        |         +--Pholidota (pangolins)
        |         |
        |         +--Chiroptera (bats)
        |         |
        |         +--Carnivora (cats, dogs, bears, seals)
        |         |
        |         `--Perissodactyla (horses, rhinos, tapirs).
        |
        `--Euarchontoglires
             |
             +--Glires
             |    |
             |    +--Lagomorpha
             |    |  (rabbits, hares, pikas)
             |    |
             |    `--Rodentia (late Paleocene)
             |        (mice & rats, squirrels, porcupines)
             |           
             `--Euarchonta
                  |
                  |--Scandentia (tree shrews)
                  |
                  |--Dermoptera (colugos)
                  |
                  `--Primates
                     (tarsiers, lemurs, monkeys, apes, humans)

The most significant of the many differences between this family tree and the one familiar to paleontologists are:

    * The top-level division is between Atlantogenata and Boreoeutheria, instead of between Xenarthra and the rest. But some Molecular phylogeneticists have proposed a 3-way top-level split between Xenarthra, Afrotheria and Boreoeutheria.
    * Afrotheria contains several groups which are only distantly related according to the paleontologists' version: Afroinsectiphilia ("African insectivores"), Tubulidentata (aardvarks, which paleontologists regard as much closer to odd-toed ungulates than to other members of Afrotheria), Macroscelidea (elephant shrews, usually regarded as close to rabbits and rodents). The only members of Afrotheria which paleontologists would regard as closely related are Hyracoidea (hyraxes), Proboscidea (elephants) and Sirenia (manatees, dugongs).
    * Insectivores are split into 3 groups: one is part of Afrotheria and the other two are distinct sub-groups within Boreoeutheria.
    * Bats are closer to Carnivora and odd-toed ungulates than to primates and Dermoptera (colugos).
    * Perissodactyla (odd-toed ungulates) are closer to Carnivora and bats than to Artiodactyla (even-toed ungulates).

The grouping together of the Afrotheria has some geological justification. All surviving members of the Afrotheria live in South America or (mainly) Africa. As Pangaea broke up Africa and South America separated from the other continents less than 150M years ago, and from each other between 100M and 80M years ago.[51][52] The earliest known eutherian mammal is Eomaia, from about 125M years ago. So it would not be surprising if the earliest eutherian immigrants into Africa and South America were isolated there and radiated into all the available ecological niches.

Nevertheless these proposals have been controversial. Paleontologists naturally insist that fossil evidence must take priority over deductions form DNA samples. More surprisingly, these new family trees have been criticised by other molecular phylogeneticists, sometimes quite harshly: [53]

    * Mitochondrial DNA's mutation rate in mammals varies from region to region - some parts hardly ever change and some change extremely quickly and even show large variations between individuals within the same species.[54][55]
    * Mammalian mitochondrial DNA mutates so fast that it causes a problem called "saturation", where random noise drowns out any information that may be present. If a particular piece of mitochondrial DNA mutates randomly every few million years, it will have changed several times in the 60 to 75M years since the major groups of placental mammals diverged.[56]

Evolution of mammalian features

Jaws and middle ears

Hadrocodium, whose fossils date from the early Jurassic, provides the first clear evidence of fully mammalian jaw joints and middle ears. Curiously it is usually classified as a member of the mammaliformes rather than a as a true mammal.

Milk production (lactation)

It has been suggested that lactation's original function was to keep eggs moist. Much of the argument is based on monotremes (egg-laying mammals):[59][60][61]

    * Monotemes do not have nipples but secrete milk from a hairy patch on their bellies.
    * During incubation, monotremes' eggs are covered in sticky substance whose origin is not known. Before the eggs are laid, their shells have only three layers. Afterwards a fourth layer appears, and its composition is different from that of the original three. The sticky substance and the fourth layer may be produced by the mammary glands.
    * If so, that may explain why the patches from which monotremes secrete milk are hairy - it is easier to spread moisture and other substances over the egg from a broad, hairy area than from a small, bare nipple.

Hair and fur

The first clear evidence of hair or fur is in fossils of Castorocauda, from 164M years ago in the mid Jurassic.

From 1955 onwards some scientists have interpreted the foramina (passages) in the maxillae (upper jaws) and premaxillae (small bones in front of the maxillae) of cynodonts as channels which supplied blood vessels and nerves to vibrissae (whiskers), and suggested that this was evidence of hair or fur.[62][63] But foramina do not necessarily show that an animal had vibrissae - for example the modern lizard Tupinambis has foramina which are almost identical to those found in the non-mammalian cynodont Thrinaxodon.[64][65]

Erect limbs

The evolution of erect limbs in mammals is incomplete - living and fossil monotremes have sprawling limbs. In fact some scientists think that the parasagittal (non-sprawling) limb posture is a synapomorphy (distinguishing characteristic) of the Boreosphenida, a group which contains the Theria and therefore includes the last common ancestor of modern marsupial and placentals - and therefore that all earlier mammals had sprawling limbs.[66]

Sinodelphys (the earliest known marsupial) and Eomaia (the earliest known eutherian) lived about 125M years ago, so erect limbs must have evolved before then.

Warm-bloodedness

"Warm-bloodedness" is a complex and rather ambiguous term, because it includes some or all of:

    * Endothermy, i.e. the ability to generate heat internally rather than via behaviors such as basking or muscular activity.
    * Homeothermy, i.e. maintaining a fairly constant body temperature.
    * Tachymetabolism, i.e. maintaining a high metabolic rate, particularly when at rest. This requires a fairly high and stable body temperature, since: biochemical processes run about half as fast if an animal's temperature drops by 10�C; most enzymes have an optimum operating temperature and their efficiency drops rapidly outside the preferred range.

Since we can't know much about the internal mechanisms of extinct creatures, most discussion focuses on homeothermy and tachymetabolism.

Modern monotremes have a lower body temperature and more variable metabolic rate than marsupials and placentals.[67] So the main question is when a monotreme-like metabolism evolved in mammals. The evidence found so far suggests Triassic cynodonts may have had fairly high metabolic rates, but is not conclusive.

[Respiratory turbinates

Modern mammals have respiratory turbinates, convoluted structures of thin bone in the nasal cavity. These are lined with mucous membranes which warm and moisten inhaled air and extract heat and moisture from exhaled air. An animal with respiratory turbinates can maintain a high rate of breathing without the danger of drying its lungs out, and therefore may have a fast metabolism. Unfortunately these bones are very delicate and therefore have not yet been found in fossils. But rudimentary ridges like those which support respiratory turbinates have been found in Triassic therapsids such as Thrinaxodon and Diademodon, which suggests that they may have had fairly high metabolic rates. [68] [69][70]

Bony secondary palate

Mammals have a secondary bony palate which separates the respiratory passage from the mouth, allowing them to eat and breathe at the same time. Secondary bony palates have been found in the more advanced cynodonts and have been used as evidence of high metabolic rates.[71][72] [73] But some cold-blooded vertebrates have secondary bony palates (crocodilians and some lizards), while birds, which are warm-blooded, do not have them.[74]

Diaphragm

A muscular diaphragm helps mammals to breathe, especially during strenuous activity. For a diaphragm to be work, the ribs must not restrict the abdomen, so that expansion of the chest can be compensated for by reduction in the volume of the abdomen and vice versa. The advanced cynodonts have very very mammal-like rib cages, with greatly reduced lumbar ribs. This suggests that these animals had diaphragms, were capable of strenuous activity for fairly long periods and therefore had high metabolic rates.[75][76] On the other hand these mammal-like rib cages may have evolved to increase agility.[77] But the movement of even advanced therapsids was "like a wheelbarrow", with the hindlimbs providing all the thrust while the forelimbs only steered the animal, in other words advanced therapsids were not as agile as either modern mammals or the early dinosaurs.[78] So the idea that the main function of these mammal-like rib cages was to increase agility is doubtful.

Limb posture

The therapsids had sprawling forelimbs and semi-erect hindlimbs.[79][80] This suggests that Carrier's constraint would have made it rather difficult for them to move and breathe at the same time, but not as difficult as it is for animals such as lizards which have completely sprawling limbs.[81] But cynodonts (advanced therapsids) had costal plates which stiffened the rib cage and therefore may have reduced sideways flexing of the trunk while moving, which would have made it a little easier for them to breathe while moving .[82] These facts suggest that advanced therapsids were significantly less active than modern mammals of similar size and therefore may have had slower metabolisms.

Insulation (hair and fur)

Insulation is the "cheapest" way to maintain a fairly constant body temperature. So possession of hair of fur would be good evidence of homeothermy, but would not be such strong evidence of a high metabolic rate.[83] [84]

We have already seen that: the first clear evidence of hair or fur is in fossils of Castorocauda, from 164M years ago in the mid Jurassic; arguments that advanced therapsids had hair are unconvincing

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  19. Travis, J (October 2003). "Visionary research: scientists delve into the evolution of color vision in primates". Science News 164 (15).
  20. Cifelli, R.L. (November 2001). "Early mammalian radiations". Journal of Paleontology.
  21. Mammaliformes - Palaeos.
  22. Cifelli, R.L. (November 2001). "Early mammalian radiations". Journal of Paleontology.
  23. Mammaliformes - Palaeos.
  24. Morganucodontids & Docodonts - Palaeos.
  25. Jurassic "Beaver" Found; Rewrites History of Mammals.
  26. Symmetrodonta - Palaeos.
  27. Mammalia - Palaeos.
  28. Mammalia - Palaeos.
  29. Appendicular Skeleton.
  30. Mammalia: Spalacotheroidea & Cladotheria - Palaeos.
  31. Appendicular Skeleton.
  32. Metatheria - Palaeos.
  33. Szalay, F.S. & B.A. Trofimov (1996), "The Mongolian Late Cretaceous Asiatherium, and the early phylogeny and paleobiogeography of Metatheria", Journal of Vertebrate Paleontology 16 (3): 474-509
  34. Oldest Marsupial Fossil Found in China. National Geographic News (December 15, 2003).
  35. Didelphimorphia - Palaeos.
  36. Family Peramelidae (bandicoots and echymiperas).
  37. Species is as species does... Part II.
  38. Marsupials.
  39. Novacek, M.J.; G.W. Rougier & J.R. Wible et al. (1997), "Epipubic bones in eutherian mammals from the late Cretaceous of Mongolia", Nature 389 (6650): 440-441
  40. Eomaia scansoria: discovery of oldest known placental mammal.
  41. Fox, D (1999), "Why we don't lay eggs", New Scientist
  42. Eutheria - Palaeos.
  43. Jurassic "Beaver" Found; Rewrites History of Mammals.
  44. Mammaliformes - Palaeos.
  45. Luo, Z.-X., Wible, J.R. (2005). "A Late Jurassic Digging Mammal and Early Mammal Diversification". Science 308: 103-107..
  46. Meng, J., Hu, Y., Wang, Y., Wang, X., Li, C. (Dec 2006). "A Mesozoic gliding mammal from northeastern China". Nature 444 (7121): 889-893.
  47. Li, J., Wang, Y., Wang, Y., Li, C. (2000). "A new family of primitive mammal from the Mesozoic of western Liaoning, China". Chinese Science Bulletin 46 (9): 782-785.  abstract, in English
  48. Hu, Y., Meng, J., Wang, Y., Li, C. (2005). "Large Mesozoic mammals fed on young dinosaurs". Nature 433: 149-152.
  49. Murphy, W.J., Eizirik, E., Springer, M.S et al (14 December 2001). "Resolution of the Early Placental Mammal Radiation Using Bayesian Phylogenetics". Science 294 (5550): 2348-2351. doi:10.1126/science.1067179.
  50. Kriegs, J.O., Churakov, G., Kiefmann, M., et al (2006). "Retroposed Elements as Archives for the Evolutionary History of Placental Mammals". PLoS Biol 4 (4): e91. doi:10.1371/journal.pbio.0040091.  (pdf version)
  51. Historical perspective (the Dynamic Earth, USGS)
  52. Cretaceous map
  53. Insectivora Overviw - Palaeos
  54. Springer, M.S. (1996). "Secondary Structure and patterns of evolution among mammalian mitochondrial 12S rRNA molecules". J. Mol. Evol. 43: 357-373.
  55. Springer, M.S. (1995). "Compensatory substitutions and the evolution of the mitochondrial 12S rRNA gene in mammals". Mol. Biol. Evol. 12: 1138-1150.
  56. Li, W-H (1997). Molecular Evolution. Sinauer Associates.
  57. Bininda-Emonds, O.R.P. (2007). "The delayed rise of present-day mammals". Nature (446): 507-511.
  58. Dinosaur Extinction Spurred Rise of Modern Mammals
  59. Oftedal, O.T. (2002). "The mammary gland and its origin during synapsid evolution". Journal of Mammary Gland Biology and Neoplasia 7 (3): 225-252.
  60. Oftedal, O.T. (2002). "The origin of lactation as a water source for parchment-shelled eggs=Journal of Mammary Gland Biology and Neoplasia" 7 (3): 253-266.
  61. Lactating on Eggs
  62. Brink, A.S. (1955). "A study on the skeleton of Diademodon". Palaeontologia Africana 3: 3-39.
  63. Kemp, T.S. (1982). Mammal-like reptiles and the origin of mammals. London: Academic Press, 363.
  64. Bennett, A. F. and Ruben, J. A. (1986) "The metabolic and thermoregulatory status of therapsids"; pp. 207-218 in N. Hotton III, P. D. MacLean, J. J. Roth and E. C. Roth (eds), "The ecology and biology of mammal-like reptiles", Smithsonian Institution Press, Washington.
  65. Estes, R. (1961). "Cranial anatomy of the cynodont reptile Thrinaxodon liorhinus". Bulletin of the Museum of Comparative Zoology: 165-180.
  66. Kielan−Jaworowska, Z. (2006). "Limb posture in early mammals: Sprawling or parasagittal". Acta Palaeontologica Polonica 51 (3): 10237-10239.
  67. Paul, G.S. (1988). Predatory Dinosaurs of the World. New York: Simon and Schuster, 464.
  68. Hillenius, W.H. (1992). "The evolution of nasal turbinates and mammalian endothermy". Paleobiology 18 (1): 17-29.
  69. Ruben, J. (1995). "The evolution of endothermy in mammals and birds: from physiology to fossils". Annual Review of Physiology 57: 69-95.
  70. Brink, A.S. (1955). "A study on the skeleton of Diademodon". Palaeontologia Africana 3: 3-39.
  71. Brink, A.S. (1955). "A study on the skeleton of Diademodon". Palaeontologia Africana 3: 3-39.
  72. Kemp, T.S. (1982). Mammal-like reptiles and the origin of mammals. London: Academic Press, 363.
  73. McNab, B.K. (1978). "The evolution of endothermy in the phylogeny of mammals". American Naturalist 112: 1-21.
  74. Bennett, A. F. and Ruben, J. A. (1986) "The metabolic and thermoregulatory status of therapsids"; pp. 207-218 in N. Hotton III, P. D. MacLean, J. J. Roth and E. C. Roth (eds), "The ecology and biology of mammal-like reptiles", Smithsonian Institution Press, Washington.
  75. Brink, A.S. (1955). "A study on the skeleton of Diademodon". Palaeontologia Africana 3: 3-39.
  76. Kemp, T.S. (1982). Mammal-like reptiles and the origin of mammals. London: Academic Press, 363.
  77. Bennett, A. F. and Ruben, J. A. (1986) "The metabolic and thermoregulatory status of therapsids"; pp. 207-218 in N. Hotton III, P. D. MacLean, J. J. Roth and E. C. Roth (eds), "The ecology and biology of mammal-like reptiles", Smithsonian Institution Press, Washington.
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  80. Kemp, T.S. (1982). Mammal-like reptiles and the origin of mammals. London: Academic Press, 363.
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  84. Withers, P.C. (1992). Comparative Animal Physiology. Fort Worth: Saunders College, 949.
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« Reply #5 on: September 07, 2007, 01:31:58 PM »


An artist's impression of the now extinct species Homo neanderthalensis

Human evolution

Human evolution is the part of biological evolution concerning the emergence of humans as a distinct species. It is the subject of a broad scientific inquiry that seeks to understand and describe how this change and development occurred. The study of human evolution encompasses many scientific disciplines, most notably physical anthropology, linguistics and genetics. The term "human", in the context of human evolution, refers to the genus Homo, but studies of human evolution usually include other hominins, such as the australopithecines.

Hominin species distributed through time



Before Homo

The evolutionary history of the primates can be traced back for some 85 million years, as one of the oldest of all surviving placental mammal groups. Most paleontologists consider that primates share a common ancestor with the bats, another extremely ancient lineage, and that this ancestor probably lived during the late Cretaceous together with the last dinosaurs. The oldest known primates come from North America, but they were widespread in Eurasia and Africa as well, during the tropical conditions of the Paleocene and Eocene.

With the beginning of modern climates, marked by the formation of the first Antarctic ice in the early Oligocene around 40 million years ago, primates went extinct everywhere but Africa and southern Asia. Fossil evidence found in Germany 20 years ago was determined to be about 16.5 million years old, some 1.5 million years older than similar species from East Africa.[6] It suggests that the great ape and human lineage first appeared in Eurasia and not Africa.

The discoveries suggest that the early ancestors of the hominids (the family of great apes and humans) migrated to Eurasia from Africa about 17 million years ago, just before these two continents were cut off from each other by an expansion of the Mediterranean Sea. Begun says that the great apes flourished in Eurasia and that their lineage leading to the African apes and humans�Dryopithecus�migrated south from Europe or Western Asia into Africa. The surviving tropical population, which is seen most completely in the upper Eocene and lowermost Oligocene fossil beds of the Fayum depression southwest of Cairo, gave rise to all living primates�lemurs of Madagascar, lorises of Southeast Asia, galagos or "bush babies" of Africa, and the anthropoids; platyrrhines or New World monkeys, and catarrhines or Old World monkeys and the great apes and humans.

The earliest known catarrhine is Kamoyapithecus from uppermost Oligocene at Eragaleit in the northern Kenya rift valley, dated to 24 Ma (millions of years before present). Its ancestry is generally thought to be close to such genera as Aegyptopithecus, Propliopithecus, and Parapithecus from the Fayum, at around 35 mya. There are no fossils from the intervening 11 million years. No near ancestor to South American platyrrhines, whose fossil record begins at around 30 mya, can be identified among the North African fossil species, and possibly lies in other forms that lived in West Africa that were caught up in the still-mysterious transatlantic sweepstakes that sent primates, rodents, boa constrictors, and cichlid fishes from Africa to South America sometime in the Oligocene.

In the early Miocene, after 22 mya, many kinds of arboreally adapted primitive catarrhines from East Africa suggest a long history of prior diversification. Because the fossils at 20 mya include fragments attributed to Victoriapithecus, the earliest cercopithecoid, the other forms are (by default) grouped as hominoids, without clear evidence as to which are closest to living apes and humans. Among the presently recognized genera in this group, which ranges up to 13 mya, we find Proconsul, Rangwapithecus, Dendropithecus, Limnopithecus, Nacholapithecus, Equatorius, Nyanzapithecus, Afropithecus, Heliopithecus, and Kenyapithecus, all from East Africa. The presence of other generalized non-cercopithecids of middle Miocene age from sites far distant�Otavipithecus from cave deposits in Namibia, and Pierolapithecus and Dryopithecus from France, Spain and Austria�is evidence of a wide diversity of forms across Africa and the Mediterranean basin during the relatively warm and equable climatic regimes of the early and middle Miocene.

The youngest of the Miocene hominoids, Oreopithecus, is from 9 mya coal beds in Italy.

Molecular evidence indicates that the lineage of gibbons (family Hylobatidae) became distinct between 18 and 12 Ma, and that of orangutans (subfamily Ponginae) at about 12 Ma; we have no fossils that clearly document the ancestry of gibbons, which may have originated in a so far unknown South East Asian hominid population, but fossil proto-orangutans may be represented by Ramapithecus from India and Griphopithecus from Turkey, dated to around 10 Ma.

Molecular evidence further suggests that between 8 and 4 mya, first the gorillas, and then the chimpanzee (genus Pan) split off from the line leading to the humans; human DNA is 98.4 percent identical to the DNA of chimpanzees. We have no fossil record, however, of either group of African great apes, possibly because bones do not fossilize in rain forest environments.

Hominines, however, seem to have been one of the mammal groups (as well as antelopes, hyenas, dogs, pigs, elephants, and horses) that adapted to the open grasslands as soon as this biome appeared, due to increasingly seasonal climates, about 8 mya, and their fossils are relatively well known. The earliest are Sahelanthropus tchadensis (7�6 mya) and Orrorin tugenensis (6 mya), followed by:

    * Ardipithecus (5.5�4.4 mya), with species Ar. kadabba and Ar. ramidus;
    * Australopithecus (4�2 mya), with species Au. anamensis, Au. afarensis, Au. africanus, Au. bahrelghazali, and Au. garhi;
    * Kenyanthropus (3-2.7 mya), with species Kenyanthropus platyops
    * Paranthropus (3�1.2 mya), with species P. aethiopicus, P. boisei, and P. robustus;
    * Homo (2 mya�present), with species Homo habilis, Homo rudolfensis, Homo ergaster, Homo georgicus erectus, Homo antecessor, Homo cepranensis, Homo erectus, Homo heidelbergensis, Homo rhodesiensis, Homo sapien neanderthalensis, Homo sapien idaltu, Homo sapien archaic, Homo floresiensis

The genus Homo

The word homo is Latin for "human", chosen originally by Carolus Linnaeus in his classification system. It is often translated as "man", although this can lead to confusion, given that the English word "man" can be generic like homo, but can also specifically refer to males. Latin for "man" in the gender-specific sense is vir, cognate with "virile" and "werewolf". The word "human" is from humanus, the adjectival form of homo.

In modern taxonomy, Homo sapiens is the only extant species of its genus, Homo. Likewise, the ongoing study of the origins of Homo sapiens often demonstrates that there were other Homo species, all of which are now extinct. While some of these other species might have been ancestors of H. sapiens, many were likely our "cousins", having speciated away from our ancestral line.[7] There is not yet a consensus as to which of these groups should count as separate species and which as subspecies of another species. In some cases this is due to the paucity of fossils, in other cases it is due to the slight differences used to classify species in the Homo genus. The Sahara pump theory provides an explanation of the early variation in the genus Homo.

Use of tools

Using tools is not only a sign of intelligence, it also may have acted as a stimulus for human evolution. Over the past 3 or 2 million years, human brain size has increased threefold. A brain needs a lot of energy: the brain of a modern human consumes about 20 Watts (400 kilocalories per day); this is one fifth of total human energy consumption. Early hominoids, like apes, were essentially plant eaters (fruit, leaves, roots), their diet only occasionally supplemented by meat (often from scavenging). However, plant food in general yields considerably less energy and nutritive value than meat. Therefore, being able to hunt for large animals, which was only possible by using tools such as spears, made it possible for humans to sustain larger and more complex brains, which in turn allowed them to develop yet more intelligent and efficient tools.

Precisely when early man started to use tools is difficult to determine, because the more primitive these tools are (for example, sharp-edged stones) the more difficult it is to decide whether they are natural objects or human artifacts. There is some evidence that the australopithecines (4 mya) may have used broken bones as tools, but this is debated.

Stone tools

Stone tools are first attested around 2.6 million years ago, when H. habilis in Eastern Africa used so-called pebble tools, choppers made out of round pebbles that had been split by simple strikes.[25] This marks the beginning of the Paleolithic, or Old Stone Age; its end is taken to be the end of the last Ice Age, around 10,000 years ago. The Paleolithic is subdivided into the Lower Paleolithic (Early Stone Age, ending around 350,000�300,000 years ago), the Middle Paleolithic (Middle Stone Age, until 50,000�30,000 years ago), and the Upper Paleolithic.

The period from 700,000�300,000 years ago is also known as the Acheulean, when H. ergaster (or erectus) made large stone hand-axes out of flint and quartzite, at first quite rough (Early Acheulian), later "retouched" by additional, more subtle strikes at the sides of the flakes. After 350,000 BP (Before Present) the more refined so-called Levallois technique was developed. It consisted of a series of consecutive strikes, by which scrapers, slicers ("racloirs"), needles, and flattened needles were made.[25] This speed-up of cultural change seems connected with the arrival of modern humans, homo sapiens. As human culture advanced, different populations of humans began to create novelty in existing technologies. Artifacts such as fish hooks, buttons and bone needles begin to show signs of variation among different population of humans, something that had not been seen in human cultures prior to 50,000 BP. Typically, neanderthalensis populations are found with technology similar to other contemporary neanderthalensis populations.

Theoretically, modern human behavior is taken to include four ingredient capabilities: abstract thinking (concepts free from specific examples), planning (taking steps to achieve a farther goal), innovation (finding new solutions), and symbolic behaviour (such as images, or rituals). Among concrete examples of modern human behaviour, anthropologists include specialization of tools, use of jewelry and images (such as cave drawings), organization of living space, rituals (for example, burials with grave gifts), specialized hunting techniques, exploration of less hospitable geographical areas, and barter trade networks. Debate continues whether there was indeed a "revolution" leading to modern man ("the big bang of human consciousness"), or a more gradual evolution.[26]

Notable human evolution researchers

    * James Burnett, Lord Monboddo, most famous today as a founder of modern comparative historical linguistics
    * Henry McHenry, specializes in studies of human evolution, the origins of bipedality, and paleoanthropology
    * Svante P��bo, a biologist specializing in evolutionary genetics
    * Jeffrey H. Schwartz, an American physical anthropologist and professor of biological anthropology
    * Erik Trinkaus, a prominent paleoanthropologist and expert on Neanderthal biology and human evolution
    * Milford H. Wolpoff, a paleoanthropologist
    * Charles Darwin, an English naturalist who documented considerable evidence that species originate through evolutionary change
    * J. B. S. Haldane, a British geneticist and evolutionary biologist
    * Leonard Shlain, a surgeon and author of three books
    * Richard Dawkins, a British ethologist, evolutionary biologist who has promoted a gene-centered view of evolution.
    * Sir Alister Hardy, a British zoologist, who first hypothesised the aquatic ape theory of human evolution.
    * Louis Leakey
    * Richard Leakey


Species list

This list will conduct in chronological order, following genus.

    * Sahelanthropus
          o Sahelanthropus tchadensis
    * Orrorin
          o Orrorin tugenensis
    * Ardipithecus
          o Ardipithecus kadabba
          o Ardipithecus ramidus
    * Australopithecus
          o Australopithecus anamensis
          o Australopithecus afarensis
          o Australopithecus bahrelghazali
          o Australopithecus africanus
          o Australopithecus garhi
    * Paranthropus
          o Paranthropus aethiopicus
          o Paranthropus boisei
          o Paranthropus robustus
    * Kenyanthropus
          o Kenyanthropus platyops
    * Homo
          o Homo habilis
          o Homo rudolfensis
          o Homo ergaster
          o Homo georgicus
          o Homo erectus
          o Homo cepranensis
          o Homo antecessor
          o Homo heidelbergensis
          o Homo rhodesiensis
          o Homo neanderthalensis
          o Homo sapiens idaltu
          o Homo sapiens (Cro-magnon)
          o Homo sapiens sapiens
          o Homo floresiensis

Additional notes

    * The validity of evolution and the origins of humanity have often been a subject of great political and religious controversy within the non-scientific community (see Creation-evolution controversy and Hybrid-origin).
    * The classification of humans and their relatives has changed considerably over time (see History of hominoid taxonomy).
    * Speculation about the future evolution of humans is often explored in science fiction as continued speciation of humans as they fill various ecological niches (see Adaptive radiation and Co-evolution), as well as deliberate self-modification (see Participant evolution).
    * Currently, scientists have estimated that humans branched off from their common ancestor with chimpanzees about 5�7 mya.

References

   1. Darwin, Charles (1861). On the Origin of Species, 3rd, John Murray, 488.
   2. Dart RA (1925). "The Man-Ape of South Africa". Nature 115: 195-199.
   3. Wood B (1996). "Human evolution". Bioessays 18 (12): 945-54. DOI:10.1002/bies.950181204. PMID 8976151.
   4. Wood B (1992). "Origin and evolution of the genus Homo". Nature 355 (6363): 783-90. DOI:10.1038/355783a0. PMID 1538759.
   5. Cela-Conde CJ, Ayala FJ (2003). "Genera of the human lineage". Proc. Natl. Acad. Sci. U.S.A. 100 (13): 7684-9. DOI:10.1073/pnas.0832372100. PMID 12794185.
   6. Kordos L, Begun DR (2001). "Primates from Rudab�nya: allocation of specimens to individuals, sex and age categories". J. Hum. Evol. 40 (1): 17-39. DOI:10.1006/jhev.2000.0437. PMID 11139358.
   7. Strait DS, Grine FE, Moniz MA (1997). "A reappraisal of early hominid phylogeny". J. Hum. Evol. 32 (1): 17-82. DOI:10.1006/jhev.1996.0097. PMID 9034954.
   8. Wood B (1999). "'Homo rudolfensis' Alexeev, 1986-fact or phantom?". J. Hum. Evol. 36 (1): 115-8. DOI:10.1006/jhev.1998.0246. PMID 9924136.
   9. Gabounia L. de Lumley M. Vekua A. Lordkipanidze D. de Lumley H. (2002). "Discovery of a new hominid at Dmanisi (Transcaucasia, Georgia)". Comptes Rendus Palevol, 1 (4): 243-53. DOI:10.1016/S1631-0683(02)00032-5.
  10. Lordkipanidze D, Vekua A, Ferring R, et al (2006). "A fourth hominin skull from Dmanisi, Georgia". The anatomical record. Part A, Discoveries in molecular, cellular, and evolutionary biology 288 (11): 1146-57. DOI:10.1002/ar.a.20379. PMID 17031841.
  11. Turner W (1895). "On M. Dubois' Description of Remains recently found in Java, named by him Pithecanthropus erectus: With Remarks on so-called Transitional Forms between Apes and Man". Journal of anatomy and physiology 29 (Pt 3): 424-45. PMID 17232143.
  12. Spoor F, Wood B, Zonneveld F (1994). "Implications of early hominid labyrinthine morphology for evolution of human bipedal locomotion". Nature 369 (6482): 645-8. DOI:10.1038/369645a0. PMID 8208290.
  13. Manzi G, Mallegni F, Ascenzi A (2001). "A cranium for the earliest Europeans: phylogenetic position of the hominid from Ceprano, Italy". Proc. Natl. Acad. Sci. U.S.A. 98 (17): 10011-6. DOI:10.1073/pnas.151259998. PMID 11504953.
14. Berm�dez de Castro JM, Arsuaga JL, Carbonell E, Rosas A, Mart�nez I, Mosquera M (1997). "A hominid  from the lower Pleistocene of Atapuerca, Spain: possible ancestor to Neandertals and modern humans". Science 276 (5317): 1392-5. PMID 9162001.
15. Czarnetzki A, Jakob T, Pusch CM (2003). "Palaeopathological and variant conditions of the Homo heidelbergensis type specimen (Mauer, Germany)". J. Hum. Evol. 44 (4): 479-95. PMID 12727464.
16. Harvati K (2003). "The Neanderthal taxonomic position: models of intra- and inter-specific craniofacial variation". J. Hum. Evol. 44 (1): 107-32. PMID 12604307.
17. Krings M, Stone A, Schmitz RW, Krainitzki H, Stoneking M, P��bo S (1997). "Neandertal DNA sequences and the origin of modern humans". Cell 90 (1): 19-30. PMID 9230299.
18. Serre D, Langaney A, Chech M, et al (2004). "No evidence of Neandertal mtDNA contribution to early modern humans". PLoS Biol. 2 (3): E57. DOI:10.1371/journal.pbio.0020057. PMID 15024415.
19. Guti�rrez G, S�nchez D, Mar�n A (2002). "A reanalysis of the ancient mitochondrial DNA sequences recovered from Neandertal bones". Mol. Biol. Evol. 19 (8): 1359-66. PMID 12140248.
20. Hebsgaard MB, Wiuf C, Gilbert MT, Glenner H, Willerslev E (2007). "Evaluating Neanderthal genetics and phylogeny". J. Mol. Evol. 64 (1): 50-60. DOI:10.1007/s00239-006-0017-y. PMID 17146600.
21. Indiana University (March 27, 2006). Scientists discover hominid cranium in Ethiopia. Press release. Retrieved on 2006-11-26.
22. Brown P, Sutikna T, Morwood MJ, et al (2004). "A new small-bodied hominin from the Late Pleistocene of Flores, Indonesia". Nature 431 (7012): 1055-61. DOI:10.1038/nature02999. PMID 15514638.
23. Argue D, Donlon D, Groves C, Wright R (2006). "Homo floresiensis: microcephalic, pygmoid, Australopithecus, or Homo?". J. Hum. Evol. 51 (4): 360-74. DOI:10.1016/j.jhevol.2006.04.013. PMID 16919706.
24. a b Martin RD, Maclarnon AM, Phillips JL, Dobyns WB (2006). "Flores hominid: new species or microcephalic dwarf?". The anatomical record. Part A, Discoveries in molecular, cellular, and evolutionary biology 288 (11): 1123-45. DOI:10.1002/ar.a.20389. PMID 17031806.
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« Reply #6 on: October 27, 2007, 04:28:58 PM »



Neanderthals 'were flame-haired'
By Paul Rincon
Science reporter, Murcia, Spain

Some Neanderthals were probably redheads, a DNA study has shown.

Writing in Science journal, a team of researchers extracted DNA from remains of two Neanderthals and retrieved part of an important gene called MC1R.

In modern people, a change - or mutation - in this gene causes red hair, but, until now, no one knew what hair colour our extinct relatives had.

By analysing a version of the gene in Neanderthals, scientists found that they also have sported fiery locks.

"We found a variant of MC1R in Neanderthals which is not present in modern humans, but which causes an effect on the hair similar to that seen in modern redheads," said lead author Carles Lalueza-Fox, assistant professor in genetics at the University of Barcelona.

Science 26 October 2007:
Vol. 318. no. 5850, pp. 546 - 547
DOI: 10.1126/science.318.5850.546
Ancient DNA Reveals Neandertals With Red Hair, Fair Complexions

Elizabeth Culotta

A pigmentation gene from the bones of two Neandertals, reported online this week in Science (www.sciencemag.org/cgi/content/abstract/1147417), indicates that at least some Neandertals had pale skin and red hair, similar to some of the Homo sapiens who today inhabit their European homeland.

REPORTS
A Melanocortin 1 Receptor Allele Suggests Varying Pigmentation Among Neanderthals
    Carles Lalueza-Fox, Holger R�mpler, David Caramelli, Claudia St�ubert, Giulio Catalano, David Hughes, Nadin Rohland, Elena Pilli, Laura Longo, Silvana Condemi, Marco de la Rasilla, Javier Fortea, Antonio Rosas, Mark Stoneking, Torsten Sch�neberg, Jaume Bertranpetit, and Michael Hofreiter (25 October 2007)

Submitted on July 5, 2007
Accepted on October 12, 2007

A Melanocortin 1 Receptor Allele Suggests Varying Pigmentation Among Neanderthals
Carles Lalueza-Fox 1+*, Holger R�mpler 2+, David Caramelli 3, Claudia St�ubert 4, Giulio Catalano 5, David Hughes 6, Nadin Rohland 6, Elena Pilli 3, Laura Longo 7, Silvana Condemi 8, Marco de la Rasilla 9, Javier Fortea 9, Antonio Rosas 10, Mark Stoneking 6, Torsten Sch�neberg 4, Jaume Bertranpetit 11, Michael Hofreiter 6*

1 Departament de Biologia Animal, Universitat de Barcelona, Spain.
2 Molecular Biochemistry, Medical Faculty, University of Leipzig, Leipzig, Germany.; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA.
3 Laboratorio di Antropologia, Universit� di Firenze, Italy.
4 Molecular Biochemistry, Medical Faculty, University of Leipzig, Leipzig, Germany.
5 Laboratorio di Antropologia, Universit� di Firenze, Italy.; Unitat de Biologia Evolutiva, Universitat Pompeu Fabra, Barcelona, Spain.
6 Department of Evolutionary Genetics, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany.
7 Dipartimento di Scienze Ambientali, Universit� di Siena, Siena, Italy.
8 Unit� d'Anthropologie, CNRS, UMR 6578, Marseille, France.
9 �rea de Prehistoria, Universidad de Oviedo, Spain.
10 Departamento de Paleobiolog�a, Museo Nacional de Ciencias Naturales, CSIC, Madrid, Spain.
11 Unitat de Biologia Evolutiva, Universitat Pompeu Fabra, Barcelona, Spain.

* To whom correspondence should be addressed.
Carles Lalueza-Fox , E-mail:
Michael Hofreiter , E-mail:

+These authors contributed equally to this work.

The melanocortin 1 receptor (MC1R) regulates pigmentation in humans and other vertebrates. Variants of MC1R with reduced function are associated with pale skin color and red hair in humans primarily of European origin. We amplified and sequenced a fragment of the MC1R gene (mc1r) from two Neanderthal remains. Both specimens have a mutation not found in ~3,700 modern humans. Functional analyses show that this variant reduces MC1R activity to a level that alters hair and/or skin pigmentation in humans. The impaired activity of this variant suggests that Neanderthals varied in pigmentation levels, potentially to the scale observed in modern humans. Our data suggest that inactive MC1R variants evolved independently in both modern humans and Neanderthals.
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