Evolutionary history of life: Wikis

Advertisements
  
  

Note: Many of our articles have direct quotes from sources you can cite, within the Wikipedia article! This article doesn't yet, but we're working on it! See more info or our list of citable articles.

Encyclopedia

From Wikipedia, the free encyclopedia

Part of the Biology series on
Evolution
Image of the tree of life showing genome size.
Mechanisms and processes

Adaptation
Genetic drift
Gene flow
Mutation
Natural selection
Speciation

Research and history

Introduction
Evidence
Evolutionary history of life
History
Modern synthesis
Social effect
Theory and fact
Objections / Controversy

Evolutionary biology fields

Cladistics
Ecological genetics
Evolutionary development
Evolutionary psychology
Human evolution
Molecular evolution
Phylogenetics
Population genetics

Biology portal ·  

The evolutionary history of life on Earth traces the processes by which living and fossil organisms evolved. It stretches from the origin of life on Earth, thought to be over 3,500 million years ago, to the present day. The similarities between all present day organisms indicate the presence of a common ancestor from which all known species have diverged through the process of evolution.[1]

Microbial mats of coexisting bacteria and archaea were the dominant form of life in the early Archean and many of the major steps in early evolution are thought to have taken place within them.[2] The evolution of oxygenic photosynthesis, around 3,500 million years ago, eventually led to the oxygenation of the atmosphere, beginning around 2,400 million years ago.[3] While eukaryotic cells may have been present earlier, their evolution accelerated when they began to use oxygen in their metabolism. The earliest evidence of complex eukaryotes with organelles, dates from 1,850 million years ago. Later, around 1,700 million years ago, multicellular organisms began to appear, with differentiated cells performing specialised functions.[4]

The earliest land plants date back to around 450 million years ago,[5] though evidence suggests that algal scum formed on the land as early as 1,200 million years ago. Land plants were so successful that they are thought to have contributed to the late Devonian extinction event.[6] Invertebrate animals appear during the Vendian period,[7] while vertebrates originated about 525 million years ago during the Cambrian explosion.[8]

During the Permian period, synapsids, including the ancestors of mammals, dominated the land,[9] but the Permian–Triassic extinction event 251 million years ago came close to wiping out all complex life.[10] During the recovery from this catastrophe, archosaurs became the most abundant land vertebrates, displacing therapsids in the mid-Triassic.[11] One archosaur group, the dinosaurs, dominated the Jurassic and Cretaceous periods,[12] while the ancestors of mammals survived only as small insectivores.[13] After the Cretaceous–Tertiary extinction event 65 million years ago killed off the non-avian dinosaurs[14] mammals increased rapidly in size and diversity.[15] Such mass extinctions may have accelerated evolution by providing opportunities for new groups of organisms to diversify.[16]

Fossil evidence indicates that flowering plants appeared and rapidly diversified in the Early Cretaceous, between 130 million years ago and 90 million years ago, probably helped by coevolution with pollinating insects. Flowering plants and marine phytoplankton are still the dominant producers of organic matter. Social insects appeared around the same time as flowering plants. Although they occupy only small parts of the insect "family tree", they now form over half the total mass of insects. Humans evolved from a lineage of upright-walking apes whose earliest fossils date from over 6 million years ago. Although early members of this lineage had chimp-sized brains, there are signs of a steady increase in brain size after about 3 million years ago.

Contents

Earliest history of Earth

History of Earth and its life
-4500 —
-4000 —
-3500 —
-3000 —
-2500 —
-2000 —
-1500 —
-1000 —
-500 —
0 —
Impact formed Moon
? Cool surface, oceans, atmosphere
? Earliest evidence of life
Oxygenation of atmosphere
Earliest multicellular organism
Earliest known fungi
Earliest known cnidarians
Earliest land invertebrates and plants
Earliest land vertebrates
Earliest known dinosaur
Extinction of non-avian dinosaurs
Scale:
Millions of years

The oldest meteorite fragments found on Earth are about 4,540 million years old, and this has convinced scientists that the whole Solar system, including Earth, formed around that time.[17] About 40 million years later a planetoid struck the Earth, throwing into orbit the material that formed the Moon.[18]

Until recently the oldest rocks found on Earth were about 3,800 million years old,[17] and this led scientists to believe for decades that Earth's surface was molten until then. Hence they named this part of Earth's history the Hadean eon, whose name means "hellish".[19] However analysis of zircons formed 4,400 to 4,000 million years ago indicates that Earth's crust solidified about 100 million years after the planet's formation and that Earth quickly acquired oceans and an atmosphere, which may have been capable of supporting life.[20]

Evidence from the Moon indicates that from 4,000 to 3,800 million years ago it suffered a Late Heavy Bombardment by debris that was left over from the formation of the Solar system, and Earth, having stronger gravity, should have experienced an even heavier bombardment.[19][21] While there is no direct evidence of conditions on Earth 4,000 to 3,800 million years ago, there is no reason to think that the Earth was not also affected by this late heavy bombardment.[22] This event may well have stripped away any previous atmosphere and oceans; in this case gases and water from comet impacts may have contributed to their replacement, although volcanic outgassing on Earth would have contributed at least half.[23]

Earliest evidence for life on Earth

The earliest identified organisms were minute and relatively featureless, so their fossils look like small rods, which are very difficult to tell apart from structures which form through physical processes. The oldest undisputed evidence of life on Earth, interpreted as fossilized bacteria, dates to 3,000 million years ago.[24] Other finds in rocks dated to about 3,500 million years ago have been interpreted as bacteria,[25] and geochemical evidence seemed to show the presence of life 3,800 million years ago.[26] However these analyses were closely scrutinized, and non-biological processes were found which could produce all of the "signatures of life" that had been reported.[27][28] While this does not prove that the structures found had a non-biological origin, they cannot be taken as clear evidence for the presence of life. Currently, the oldest unchallenged evidence for life is geochemical signatures from rocks deposited 3,400 million years ago,[24][29] although there has been little time for these recent reports (2006) to be examined by critics.

Origins of life on Earth

Euryarchaeota Nanoarchaeota Crenarchaeota Protozoa Algae Plantae Slime molds Animal Fungus Gram-positive bacteria Chlamydiae Chloroflexi Actinobacteria Planctomycetes Spirochaetes Fusobacteria Cyanobacteria Thermophiles Acidobacteria Proteobacteria
Evolutionary tree showing the divergence of modern species from their common ancestor in the center.[30] The three domains are colored, with bacteria blue, archaea green, and eukaryotes red.

Biochemists reason that all living organisms on Earth must share a single last universal ancestor, because it would be virtually impossible that two or more separate lineages could have independently developed the many complex biochemical mechanisms shared by all living organisms.[31][32] However the earliest organisms for which fossil evidence is available are bacteria, which are far too complex to have arisen directly from non-living materials.[33] The lack of fossil or geochemical evidence for earlier types of organism has left plenty of scope for hypotheses, which fall into two main groups: that life arose spontaneously on Earth, and that it was "seeded" from elsewhere in the universe.[34]

Advertisements

Life "seeded" from elsewhere

The idea that life Earth was "seeded" from elsewhere in the universe dates back at least to the fifth century BC.[35] In the twentieth century it was proposed by the physical chemist Svante Arrhenius,[36] by the astronomers Fred Hoyle and Chandra Wickramasinghe,[37] and by molecular biologist Francis Crick and chemist Leslie Orgel.[38] There are three main versions of the "seeded from elsewhere" hypothesis: from elsewhere in our Solar system via fragments knocked into space by a large meteor impact, in which case the only credible source is Mars;[39] by alien visitors, possibly as a result of accidental contamination by micro-organisms that they brought with them;[38] and from outside the Solar system but by natural means.[36][39] Experiments suggest that some micro-organisms can survive the shock of being catapulted into space and some can survive exposure to radiation for several days, but there is no proof that they can survive in space for much longer periods.[39] Scientists are divided over the likelihood of life arising independently on Mars,[40] or on other planets in our galaxy.[39]

Independent emergence on Earth

Life on earth is based on carbon and water. Carbon provides stable frameworks for complex chemicals and can be easily extracted from the environment, especially from carbon dioxide. The only other element with similar chemical properties, silicon, forms much less stable structures and, because most of its compounds are solids, would be more difficult for organisms to extract. Water is an excellent solvent and has two other useful properties: the fact that ice floats enables aquatic organisms to survive beneath it in winter; and its molecules have electrically negative and positive ends, which enables it to form a wider range of compounds than other solvents can. Other good solvents, such as ammonia, are liquid only at such low temperatures that chemical reactions may be too slow to sustain life, and lack water's other advantages.[41] Organisms based on alternative biochemistry may however be possible on other planets.[42]

Research on how life might have emerged unaided from non-living chemicals focuses on three possible starting points: self-replication, an organism's ability to produce offspring that are very similar to itself; metabolism, its ability to feed and repair itself; and external cell membranes, which allow food to enter and waste products to leave, but exclude unwanted substances.[43] Research on abiogenesis still has a long way to go, since theoretical and empirical approaches are only beginning to make contact with each other.[44][45]

Replication first: RNA world

The replicator in virtually all known life is deoxyribonucleic acid. DNA's structure and replication systems are far more complex than those of the original replicator.[33]

Even the simplest members of the three modern domains of life use DNA to record their "recipes" and a complex array of RNA and protein molecules to "read" these instructions and use them for growth, maintenance and self-replication. This system is far too complex to have emerged directly from non-living materials.[33] The discovery that some RNA molecules can catalyze both their own replication and the construction of proteins led to the hypothesis of earlier life-forms based entirely on RNA.[46] These ribozymes could have formed an RNA world in which there were individuals but no species, as mutations and horizontal gene transfers would have meant that the offspring in each generation were quite likely to have different genomes from those that their parents started with.[47] RNA would later have been replaced by DNA, which is more stable and therefore can build longer genomes, expanding the range of capabilities a single organism can have.[47][48][49] Ribozymes remain as the main components of ribosomes, modern cells' "protein factories".[50]

Although short self-replicating RNA molecules have been artificially produced in laboratories,[51] doubts have been raised about where natural non-biological synthesis of RNA is possible.[52] The earliest "ribozymes" may have been formed of simpler nucleic acids such as PNA, TNA or GNA, which would have been replaced later by RNA.[53][54]

In 2003 it was proposed that porous metal sulfide precipitates would assist RNA synthesis at about 100 °C (212 °F) and ocean-bottom pressures near hydrothermal vents. In this hypothesis lipid membranes would be the last major cell components to appear and until then the proto-cells would be confined to the pores.[55]

Metabolism first: Iron-sulfur world

A series of experiments starting in 1997 showed that early stages in the formation of proteins from inorganic materials including carbon monoxide and hydrogen sulfide could be achieved by using iron sulfide and nickel sulfide as catalysts. Most of the steps required temperatures of about 100 °C (212 °F) and moderate pressures, although one stage required 250 °C (482 °F) and a pressure equivalent to that found under 7 kilometres (4.3 mi) of rock. Hence it was suggested that self-sustaining synthesis of proteins could have occurred near hydrothermal vents.[56]

Membranes first: Lipid world

    = water-attracting heads of lipid molecules

    = water-repellent tails

Cross-section through a liposome.

It has been suggested that double-walled "bubbles" of lipids like those that form the external membranes of cells may have been an essential first step.[57] Experiments that simulated the conditions of the early Earth have reported the formation of lipids, and these can spontaneously form liposomes, double-walled "bubbles", and then reproduce themselves. Although they are not intrinsically information-carriers as nucleic acids are, they would be subject to natural selection for longevity and reproduction. Nucleic acids such as RNA might then have formed more easily within the liposomes than they would have outside.[58]

The clay theory

RNA is complex and there are doubts about whether it can be produced non-biologically in the wild.[52] Some clays, notably montmorillonite, have properties that make them plausible accelerators for the emergence of an RNA world: they grow by self-replication of their crystalline pattern; they are subject to an analog of natural selection, as the clay "species" that grows fastest in a particular environment rapidly becomes dominant; and they can catalyze the formation of RNA molecules.[59] Although this idea has not become the scientific consensus, it still has active supporters.[60]

Research in 2003 reported that montmorillonite could also accelerate the conversion of fatty acids into "bubbles", and that the "bubbles" could encapsulate RNA attached to the clay. These "bubbles" can then grow by absorbing additional lipids and then divide. The formation of the earliest cells may have been aided by similar processes.[61]

A similar hypothesis presents self-replicating iron-rich clays as the progenitors of nucleotides, lipids and amino acids.[62]

Environmental and evolutionary impact of microbial mats

Modern stromatolites in Shark Bay, Western Australia.

Microbial mats are multi-layered, multi-species colonies of bacteria and other organisms that are generally only a few millimeters thick, but still contain a wide range of chemical environments, each of which favors a different set of micro-organisms.[63] To some extent each mat forms its own food chain, as the by-products of each group of micro-organisms generally serve as "food" for adjacent groups.[64]

Stromatolites are stubby pillars built as microbes in mats slowly migrate upwards to avoid being smothered by sediment deposited on them by water.[63] There has been vigorous debate about the validity of alleged fossils from before 3,000 million years ago,[65] with critics arguing that so-called stromatolites could have been formed by non-biological processes.[27] In 2006 another find of stromatolites was reported from the same part of Australia as previous ones, in rocks dated to 3,500 million years ago.[66]

In modern underwater mats the top layer often consists of photosynthesizing cyanobacteria which create an oxygen-rich environment, while the bottom layer is oxygen-free and often dominated by hydrogen sulfide emitted by the organisms living there.[64] It is estimated that the appearance of oxygenic photosynthesis by bacteria in mats increased biological productivity by a factor of between 100 and 1,000. The reducing agent used by oxygenic photosynthesis is water, which is much more plentiful than the geologically-produced reducing agents required by the earlier non-oxygenic photosynthesis.[67] From this point onwards life itself produced significantly more of the resources it needed than did geochemical processes.[68] Oxygen is toxic to organisms that are not adapted to it, but greatly increases the metabolic efficiency of oxygen-adapted organisms.[69][70]

Oxygen became a significant component of Earth's atmosphere about 2,400 million years ago.[71] Although eukaryotes may have been present much earlier,[72][73] the oxygenation of the atmosphere was a prerequisite for the evolution of the most complex eukaryotic cells, from which all multicellular organisms are built.[74] The boundary between oxygen-rich and oxygen-free layers in microbial mats would have moved upwards when photosynthesis shut down overnight, and then downwards as it resumed on the next day. This would have created selection pressure for organisms in this intermediate zone to acquire the ability to tolerate and then to use oxygen, possibly via endosymbiosis, where one organism lives inside another and both of them benefit from their association.[2]

Cyanobacteria have the most complete biochemical "toolkits" of all the mat-forming organisms. Hence they are the most self-sufficient of the mat organisms and were well-adapted to strike out on their own both as floating mats and as the first of the phytoplankton, providing the basis of most marine food chains.[2]

Diversification of eukaryotes

Eukaryotes may have been present long before the oxygenation of the atmosphere,[72] but most modern eukaryotes require oxygen, which their mitochondria use to fuel the production of ATP, the internal energy supply of all known cells.[74] In the 1970s it was proposed and, after much debate, widely accepted that eukaryotes emerged as a result of a sequence of endosymbioses between "procaryotes". For example: a predatory micro-organism invaded a large procaryote, probably an archaean, but the attack was neutralized, and the attacker took up residence and evolved into the first of the mitochondria; one of these chimeras later tried to swallow a photosynthesizing cyanobacterium, but the victim survived inside the attacker and the new combination became the ancestor of plants; and so on. After each endosymbiosis began, the partners would have eliminated unproductive duplication of genetic functions by re-arranging their genomes, a process which sometimes involved transfer of genes between them.[77][78][79] Another hypothesis proposes that mitochondria were originally sulfur- or hydrogen-metabolising endosymbionts, and became oxygen-consumers later.[80] On the other hand mitochondria might have been part of eukaryotes' original equipment.[81]

There is a debate about when eukaryotes first appeared: the presence of steranes in Australian shales may indicate that eukaryotes were present 2,700 million years ago;[73] however an analysis in 2008 concluded that these chemicals infiltrated the rocks less than 2,200 million years ago and prove nothing about the origins of eukaryotes.[82] Fossils of the alga Grypania have been reported in 1,850 million-year-old rocks (originally dated to 2,100 million years ago but later revised[83]), and indicates that eukaryotes with organelles had already evolved.[84] A diverse collection of fossil algae were found in rocks dated between 1,500 million years ago and 1,400 million years ago.[85] The earliest known fossils of fungi date from 1,430 million years ago.[86]

Multicellular organisms and sexual reproduction

Multicellularity

A slime mold solves a maze. The mold (yellow) explored and filled the maze (left). When the researchers placed sugar (red) at two separate points, the mold concentrated most of its mass there and left only the most efficient connection between the two points (right).[87]

The simplest definitions of "multicellular", for example "having multiple cells", could include colonial cyanobacteria like Nostoc. Even a professional biologist's definition such as "having the same genome but different types of cell" would still include some genera of the green alga Volvox, which have cells that specialize in reproduction.[88] Multicellularity evolved independently in organisms as diverse as sponges and other animals, fungi, plants, brown algae, cyanobacteria, slime moulds and myxobacteria.[83][89] For the sake of brevity this article focuses on the organisms that show the greatest specialization of cells and variety of cell types, although this approach to the evolution of complexity could be regarded as "rather anthropocentric".[90]

The initial advantages of multicellularity may have included: increased resistance to predators, many of which attacked by engulfing; the ability to resist currents by attaching to a firm surface; the ability to reach upwards to filter-feed or to obtain sunlight for photosynthesis;[91] the ability to create an internal environment that gives protection against the external one;[90] and even the opportunity for a group of cells to behave "intelligently" by sharing information.[87] These features would also have provided opportunities for other organisms to diversify, by creating more varied environments than flat microbial mats could.[91]

Multicellularity with differentiated cells is beneficial to the organism as a whole but disadvantageous from the point of view of individual cells, most of which lose the opportunity to reproduce themselves. In an asexual multicellular organism, rogue cells which retain the ability to reproduce may take over and reduce the organism to a mass of undifferentiated cells. Sexual reproduction eliminates such rogue cells from the next generation and therefore appears to be a prerequisite for complex multicellularity.[91]

The available evidence indicates that eukaryotes evolved much earlier but remained inconspicuous until a rapid diversification around 1,000 million years ago. The only respect in which eukaryotes clearly surpass bacteria and archaea is their capacity for variety of forms, and sexual reproduction enabled eukaryotes to exploit that advantage by producing organisms with multiple cells that differed in form and function.[91]

Evolution of sexual reproduction

The defining characteristic of sexual reproduction is recombination, in which each of the offspring receives 50% of its genetic inheritance from each of the parents.[92] Bacteria also exchange DNA by bacterial conjugation, the benefits of which include resistance to antibiotics and other toxins, and the ability to utilize new metabolites.[93] However conjugation is not a means of reproduction, and is not limited to members of the same species – there are cases where bacteria transfer DNA to plants and animals.[94]

The disadvantages of sexual reproduction are well-known: the genetic reshuffle of recombination may break up favorable combinations of genes; and since males do not directly increase the number of offspring in the next generation, an asexual population can out-breed and displace in as little as 50 generations a sexual population that is equal in every other respect.[92] Nevertheless the great majority of animals, plants, fungi and protists reproduce sexually. There is strong evidence that sexual reproduction arose early in the history of eukaryotes and that the genes controlling it have changed very little since then.[95] How sexual reproduction evolved and survived is an unsolved puzzle.[96]

The Red Queen Hypothesis suggests that sexual reproduction provides protection against parasites, because it is easier for parasites to evolve means of overcoming the defenses of genetically identical clones than those of sexual species that present moving targets, and there is some experimental evidence for this. However there is still doubt about whether it would explain the survival of sexual species if multiple similar clone species were present, as one of the clones may survive the attacks of parasites for long enough to out-breed the sexual species.[92]

The Mutation Deterministic Hypothesis assumes that each organism has more than one harmful mutation and the combined effects of these mutations are more harmful than the sum of the harm done by each individual mutation. If so, sexual recombination of genes will reduce the harm done that bad mutations do to offspring and at the same time eliminate some bad mutations from the gene pool by isolating them in individuals that perish quickly because they have an above-average number of bad mutations. However the evidence suggests that the MDH's assumptions are shaky, because many species have on average less than one harmful mutation per individual and no species that has been investigated shows evidence of synergy between harmful mutations.[92]

The random nature of recombination causes the relative abundance of alternative traits to vary from one generation to another. This genetic drift is insufficient on its own to make sexual reproduction advantageous, but a combination of genetic drift and natural selection may be sufficient. When chance produces combinations of good traits, natural selection gives a large advantage to lineages in which these traits become genetically linked. On the other hand the benefits of good traits are neutralized if they appear along with bad traits. Sexual recombination gives good traits the opportunities to become linked with other good traits, and mathematical models suggest this may be more than enough to offset the disadvantages of sexual reproduction.[96] Other combinations of hypotheses that are inadequate on their own are also being examined.[92]

Fossil evidence for multicellularity and sexual reproduction

Horodyskia may have been an early metazoan,[83] or a colonial foraminiferan[97]

The earliest known fossil organism that is clearly multicellular, Qingshania,[note 1] dated to 1,700 million years ago, appears to consist of virtually identical cells. A red alga called Bangiomorpha, dated at 1,200 million years ago, is the earliest known organism which has differentiated, specialized cells, and is also the oldest known sexually-reproducing organism.[91] The 1,430 million-year-old fossils interpreted as fungi appear to have been multicellular with differentiated cells.[86] The "string of beads" organism Horodyskia, found in rocks dated from 1,500 million years ago to 900 million years ago, may have been an early metazoan;[83] however it has also been interpreted as a colonial foraminiferan.[97]

Emergence of animals

Animals are multicellular eukaryotes,[note 2] and are distinguished from plants, algae, and fungi by lacking cell walls.[99] All animals are motile,[100] if only at certain life stages. All animals except sponges have bodies differentiated into separate tissues, including muscles, which move parts of the animal by contracting, and nerve tissue, which transmits and processes signals.[101]

The earliest widely-accepted animal fossils are rather modern-looking cnidarians (the group that includes jellyfish, sea anemones and hydras), possibly from around 580 million years ago, although fossils from the Doushantuo Formation can only be dated approximately. Their presence implies that the cnidarian and bilaterian lineages had already diverged.[102]

The Ediacara biota, which flourished for the last 40 million years before the start of the Cambrian,[103] were the first animals more than a very few centimeters long. Many were flat and had a "quilted" appearance, and seemed so strange that there was a proposal to classify them as a separate kingdom, Vendozoa.[104] Others, however, been interpreted as early molluscs (Kimberella[105][106]), echinoderms (Arkarua[107]), and arthropods (Spriggina,[108] Parvancorina[109]). There is still debate about the classification of these specimens, mainly because the diagnostic features which allow taxonomists to classify more recent organisms, such as similarities to living organisms, are generally absent in the Ediacarans. However there seems little doubt that Kimberella was at least a triploblastic bilaterian animal, in other words significantly more complex than cnidarians.[110]

The small shelly fauna are a very mixed collection of fossils found between the Late Ediacaran and Mid Cambrian periods. The earliest, Cloudina, shows signs of successful defense against predation and may indicate the start of an evolutionary arms race. Some tiny Early Cambrian shells almost certainly belonged to molluscs, while the owners of some "armor plates", Halkieria and Microdictyon, were eventually identified when more complete specimens were found in Cambrian lagerstätten that preserved soft-bodied animals.[111]

Opabinia made the largest single contribution to modern interest in the Cambrian explosion.[112]

In the 1970s there was already a debate about whether the emergence of the modern phyla was "explosive" or gradual but hidden by the shortage of Pre-Cambrian animal fossils.[111] A re-analysis of fossils from the Burgess Shale lagerstätte increased interest in the issue when it revealed animals, such as Opabinia, which did not fit into any known phylum. At the time these were interpreted as evidence that the modern phyla had evolved very rapidly in the "Cambrian explosion" and that the Burgess Shale's "weird wonders" showed that the Early Cambrian was a uniquely experimental period of animal evolution.[113] Later discoveries of similar animals and the development of new theoretical approaches led to the conclusion that many of the "weird wonders" were evolutionary "aunts" or "cousins" of modern groups[114] – for example that Opabinia was a member of the lobopods, a group which includes the ancestors of the arthropods, and that it may have been closely related to the modern tardigrades.[115] Nevertheless there is still much debate about whether the Cambrian explosion was really explosive and, if so, how and why it happened and why it appears unique in the history of animals.[116]

Acanthodians were among the earliest vertebrates with jaws[117]

Most of the animals at the heart of the Cambrian explosion debate are protostomes, one of the two main groups of complex animals. One deuterostome group, the echinoderms, many of which have hard calcite "shells", are fairly common from the Early Cambrian small shelly fauna onwards.[111] Other deuterostome groups are soft-bodied, and most of the significant Cambrian deuterostome fossils come from the Chengjiang fauna, a lagerstätte in China.[118] The Chengjiang fossils Haikouichthys and Myllokunmingia appear to be true vertebrates,[119] and Haikouichthys had distinct vertebrae, which may have been slightly mineralized.[120] Vertebrates with jaws, such as the Acanthodians, first appeared in the Late Ordovician.[121]

Colonization of land

Adaptation to life on land is a major challenge: all land organisms need to avoid drying-out and all those above microscopic size have to resist gravity; respiration and gas exchange systems have to change; reproductive systems cannot depend on water to carry eggs and sperm towards each other.[122][123] Although the earliest good evidence of land plants and animals dates back to the Ordovician period (488 to 444 million years ago), modern land ecosystems only appeared in the late Devonian, about 385 to 359 million years ago.[124]

Evolution of soil

Before the colonization of land, soil, a combination of mineral particles and decomposed organic matter, did not exist. Land surfaces would have been either bare rock or unstable sand produced by weathering. Water and any nutrients in it would have drained away very quickly.[124]

Lichens growing on concrete

Films of cyanobacteria, which are not plants but use the same photosynthesis mechanisms, have been found in modern deserts, and only in areas that are unsuitable for vascular plants. This suggests that microbial mats may have been the first organisms to colonize dry land, possibly in the Precambrian. Mat-forming cyanobacteria could have gradually evolved resistance to desiccation as they spread from the seas to tidal zones and then to land.[124] Lichens, which are symbiotic combinations of a fungus (almost always an ascomycete) and one or more photosynthesizers (green algae or cyanobacteria),[125] are also important colonizers of lifeless environments,[124] and their ability to break down rocks contributes to soil formation in situations where plants cannot survive.[125] The earliest known ascomycete fossils date from 423 to 419 million years ago in the Silurian.[124]

Soil formation would have been very slow until the appearance of burrowing animals, which mix the mineral and organic components of soil and whose feces are a major source of the organic components.[124] Burrows have been found in Ordovician sediments, and are attributed to annelids ("worms") or arthropods.[124][126]

Plants and the Late Devonian wood crisis

Reconstruction of Cooksonia, a vascular plant from the Silurian.
Fossilized trees from the Mid-Devonian Gilboa fossil forest.

In aquatic algae, almost all cells are capable of photosynthesies and are nearly independent. Life on land required plants to become internally more complex and specialized: photosynthesis was most efficient at the top; roots were required in order to extract water from the ground; the parts in between became supports and transport systems for water and nutrients.[122][127]

Spores of land plants, possibly rather like liverworts, have been found in Mid Ordovician rocks dated to about 476 million years ago. In Mid Silurian rocks 430 million years ago there are fossils of actual plants including clubmosses such as Baragwanathia; most were under 10 centimetres (3.9 in) high, and some appear closely related to vascular plants, the group that includes trees.[127]

By the Late Devonian 370 million years ago, trees such as Archaeopteris were so abundant that they changed river systems from mostly braided to mostly meandering, because their roots bound the soil firmly.[128] In fact they caused a "Late Devonian wood crisis",[129] because:

  • They removed more carbon dioxide from the atmosphere, reducing the greenhouse effect and thus causing an ice age in the Carboniferous period.[130] In later ecosystems the carbon dioxide "locked up" in wood is returned to the atmosphere by decomposition of dead wood. However the earliest fossil evidence of fungi that can decompose wood also comes from the Late Devonian.[131]
  • The increasing depth of plants' roots led to more washing of nutrients into rivers and seas by rain. This caused algal blooms whose high consumption of oxygen caused anoxic events in deeper waters, increasing the extinction rate among deep-water animals.[130]

Land invertebrates

Animals had to change their feeding and excretory systems, and most land animals developed internal fertilization of their eggs. The difference in refractive index between water and air required changes in their eyes. On the other hand in some ways movement and breathing became easier, and the better transmission of high-frequency sounds in air encouraged the development of hearing.[123]

Some trace fossils from the Cambrian-Ordovician boundary about 490 million years ago are interpreted as the tracks of large amphibious arthropods on coastal sand dunes, and may have been made by euthycarcinoids,[132] which are thought to be evolutionary "aunts" of myriapods.[133] Other trace fossils from the Late Ordovician a little over 445 million years ago probably represent land invertebrates, and there is clear evidence of numerous arthropods on coasts and alluvial plains shortly before the Silurian-Devonian boundary, about 415 million years ago, including signs that some arthropods ate plants.[134] Arthropods were well pre-adapted to colonise land, because their existing jointed exoskeletons provided protection against desiccation, support against gravity and a means of locomotion that was not dependent on water.[135]

The fossil record of other major invertebrate groups on land is poor: none at all for non-parasitic flatworms, nematodes or nemerteans; some parasitic nematodes have been fossilized in amber; annelid worm fossils are known from the Carboniferous, but they may still have been aquatic animals; the earliest fossils of gastropods on land date from the Late Carboniferous, and this group may have had to wait until leaf litter became abundant enough to provide the moist conditions they need.[123]

The earliest confirmed fossils of flying insects date from the Late Carboniferous, but it is thought that insects developed the ability to fly in the Early Carboniferous or even Late Devonian. This gave them a wider range of ecological niches for feeding and breeding, and a means of escape from predators and from unfavorable changes in the environment.[136] About 99% of modern insect species fly or are descendants of flying species.[137]

Land vertebrates

Acanthostega changed views about the early evolution of tetrapods[138]

Tetrapods, vertebrates with four limbs, evolved from other rhipidistians over a relatively short timespan during the Late Devonian, between 370 million years ago and 360 million years ago.[140] From the 1950s to the early 1980s it was thought that tetrapods evolved from fish that had already acquired the ability to crawl on land, possibly in order to go from a pool that was drying out to one that was deeper. However in 1987 nearly-complete fossils of Acanthostega from about 363 million years ago showed that this Late Devonian transitional animal had legs and both lungs and gills, but could never have survived on land: its limbs and its wrist and ankle joints were too weak to bear its weight; its ribs were too short to prevent its lungs from being squeezed flat by its weight; its fish-like tail fin would have been damaged by dragging on the ground. The current hypothesis is that Acanthostega, which was about 1 metre (3.3 ft) long, was a wholly aquatic predator that hunted in shallow water. Its skeleton differed from that of most fish, in ways that enabled it to raise its head to breathe air while its body remained submerged, including: its jaws show modifications that would have enabled it to gulp air; the bones at the back of its skull are locked together, providing strong attachment points for muscles that raised its head; the head is not joined to the shoulder girdle and it has a distinct neck.[138]

The Devonian proliferation of land plants may help to explain why air-breathing would have been an advantage: leaves falling into streams and rivers would have encouraged the growth of aquatic vegetation; this would have attracted grazing invertebrates and small fish that preyed on them; they would have been attractive prey but the environment was unsuitable for the big marine predatory fish; air-breathing would have been necessary because these waters would have been short of oxygen, since warm water holds less dissolved oxygen than cooler marine water and since the decomposition of vegetation would have used some of the oxygen.[138]

Later discoveries revealed earlier transitional forms between Acanthostega and completely fish-like animals.[141] Unfortunately there is then a gap of about 30 million years between the fossils of ancestral tetrapods and Mid Carboniferous fossils of vertebrates that look well-adapted for life on land. Some of these look like early relatives of modern amphibians, most of which need to keep their skins moist and to lay their eggs in water, while others are accepted as early relatives of the amniotes, whose water-proof skins and eggs enable them to live and breed far from water.[139]

Dinosaurs, birds and mammals

Amniotes
Synapsids

Early synapsids (extinct)


Pelycosaurs

Extinct pelycosaurs


Therapsids

Extinct therapsids


Mammaliformes
   

Extinct mammaliformes


   

Mammals






Sauropsids


Anapsids; whether turtles belong here is debated[142]


   

Captorhinidae and Protorothyrididae


Diapsids

Araeoscelidia (extinct)


   
   

Squamata (lizards and snakes)


Archosaurs

Extinct archosaurs



Crocodilians


   

Pterosaurs (extinct)


Dinosaurs

Theropods
   

Extinct
theropods


   

Birds




Sauropods
(extinct)



   

Ornithischians (extinct)











Possible family tree of dinosaurs, birds and mammals[143][144]

Amniotes, whose eggs can survive in dry environments, probably evolved in the Late Carboniferous period, between 330 million years ago and 314 million years ago. The earliest fossils of the two surviving amniote groups, synapsids and sauropsids, date from around 313 million years ago.[143][144] The synapsid pelycosaurs and their descendants the therapsids are the most common land vertebrates in the best-known Permian fossil beds, between 229 million years ago and 251 million years ago. However at the time these were all in temperate zones at middle latitudes, and there is evidence that hotter, drier environments nearer the Equator were dominated by sauropsids and amphibians.[145]

The Permian-Triassic extinction wiped out almost all land vertebrates,[146] as well as the great majority of other life.[147] During the slow recovery from this catastrophe, estimated to be 30M years,[148] a previously obscure sauropsid group became the most abundant and diverse terrestrial vertebrates: a few fossils of archosauriformes ("shaped like archosaurs") have been found in Late Permian rocks,[149] but by the Mid Triassic archosaurs were the dominant land vertebrates. Dinosaurs distinguished themselves from other archosaurs in the Late Triassic, and became the dominant land vertebrates of the Jurassic and Cretaceous periods, between 199 million years ago and 65 million years ago.[150]

During the Late Jurassic, birds evolved from small, predatory theropod dinosaurs.[151] The first birds inherited teeth and long, bony tails from their dinosaur ancestors,[151] but some developed horny, toothless beaks by the very Late Jurassic[152] and short pygostyle tails by the Early Cretaceous.[153]

While the archosaurs and dinosaurs were becoming more dominant in the Triassic, the mammaliform successors of the therapsids could only survive as small, mainly nocturnal insectivores. This apparent set-back may actually have promoted the evolution of mammals, for example nocturnal life may have accelerated the development of endothermy ("warm-bloodedness") and hair or fur.[154] By 195 million years ago in the Early Jurassic there were animals that were very nearly mammals.[155] Unfortunately there is a gap in the fossil record throughout the Mid Jurassic.[156] However fossil teeth discovered in Madagascar indicate that true mammals existed at least 167 million years ago.[157] After dominating land vertebrate niches for about 150 million years, the dinosaurs perished 65 million years ago in the Cretaceous–Tertiary extinction along with many other groups of organisms.[158] Mammals throughout the time of the dinosaurs had been restricted to a narrow range of taxa, sizes and shapes, but increased rapidly in size and diversity after the extinction,[159][160] with bats taking to the air within 13 million years,[161] and cetaceans to the sea within 15 million years.[162]

Flowering plants

Gymnosperms




Gnetales
(gymnosperm)



Welwitschia
(gymnosperm)




Ephedra
(gymnosperm)




Bennettitales



Angiosperms
(flowering plants)




One possible family tree of flowering plants.[163]
Gymnosperms

Angiosperms
(flowering plants)






Cycads
(gymnosperm)



Bennettitales




Gingko





Gnetales
(gymnosperm)



Conifers
(gymnosperm)





Another possible family tree.[164]

The 250,000 to 400,000 species of flowering plants outnumber all other ground plants combined, and are the dominant vegetation in most terrestrial ecosystems. There is fossil evidence that flowering plants diversified rapidly in the Early Cretaceous, between 130 million years ago and 90 million years ago,[163][164] and that their rise was associated with that of pollinating insects.[164] Among modern flowering plants Magnolias are thought to be close to the common ancestor of the group.[163] However paleontologists have not succeeded in identifying the earliest stages in the evolution of flowering plants.[163][164]

Social insects

The social insects are remarkable because the great majority of individuals in each colony are sterile. This appears contrary to basic concepts of evolution such as natural selection and the selfish gene. In fact there are very few eusocial insect species: only 15 out of approximately 2,600 living families of insects contain eusocial species, and it seems that eusociality has evolved independently only 12 times among arthropods, although some eusocial lineages have diversified into several families. Nevertheless social insects have been spectacularly successful; for example although ants and termites account for only about 2% of known insect species, they form over 50% of the total mass of insects. Their ability to control a territory appears to be the foundation of their success.[165]

These termite mounds have survived a bush fire.

The sacrifice of breeding opportunities by most individuals has long been explained as a consequence of these species' unusual haplodiploid method of sex determination, which has the paradoxical consequence that two sterile worker daughters of the same queen share more genes with each other than they would with their offspring if they could breed.[166] However Wilson and Hölldobler argue that this explanation is faulty: for example, it is based on kin selection, but there is no evidence of nepotism in colonies that have multiple queens. Instead, they write, eusociality evolves only in species that are under strong pressure from predators and competitors, but in environments where it is possible to build "fortresses"; after colonies have established this security, they gain other advantages though co-operative foraging. In support of this explanation they cite the appearance of eusociality in bathyergid mole rats,[165] which are not haplodiploid.[167]

The earliest fossils of insects have been found in Early Devonian rocks from about 400 million years ago, which preserve only a few varieties of flightless insect. The Mazon Creek lagerstätten from the Late Carboniferous, about 300 million years ago, include about 200 species, some gigantic by modern standards, and indicate that insects had occupied their main modern ecological niches as herbivores, detritivores and insectivores. Social termites and ants first appear in the Early Cretaceous, and advanced social bees have been found in Late Cretaceous rocks but did not become abundant until the Mid Cenozoic.[168]

Humans

Modern humans evolved from a lineage of upright-walking apes that has been traced back over 6 million years ago to Sahelanthropus.[169] The first known stone tools were made about 2.5 million years ago, apparently by Australopithecus garhi, and were found near animal bones that bear scratches made by these tools.[170] The earliest hominines had chimp-sized brains, but there has been a fourfold increase in the last 3 million years; a statistical analysis suggests that hominine brain sizes depend almost completely on the date of the fossils, while the species to which they are assigned has only slight influence.[171] There is a long-running debate about whether modern humans evolved all over the world simultaneously from existing advanced hominines or are descendants of a single small population in Africa, which then migrated all over the world less than 200,000 years ago and replaced previous hominine species.[172] There is also debate about whether anatomically-modern humans had an intellectual, cultural and technological "Great Leap Forward" under 100,000 years ago and, if so, whether this was due to neurological changes that are not visible in fossils.[173]

Mass extinctions

Cambrian Ordovician Silurian Devonian Carboniferous Permian Triassic Jurassic Cretaceous Paleogene Neogene
Millions of years ago
Cambrian Ordovician Silurian Devonian Carboniferous Permian Triassic Jurassic Cretaceous Paleogene Neogene
Apparent extinction intensity, i.e. the fraction of genera going extinct at any given time, as reconstructed from the fossil record. (Graph not meant to include recent epoch of Holocene extinction event)

Life on earth has suffered occasional mass extinctions at least since 542 million years ago. Although they are disasters at the time, mass extinctions have sometimes accelerated the evolution of life on earth. When dominance of particular ecological niches passes from one group of organisms to another, it is rarely because the new dominant group is "superior" to the old and usually because an extinction event eliminates the old dominant group and makes way for the new one.[174][175]

The fossil record appears to show that the gaps between mass extinctions are becoming longer and the average and background rates of extinction are decreasing. Both of these phenomena could be explained in one or more ways:[176]

  • The oceans may have become more hospitable to life over the last 500 million years and less vulnerable to mass extinctions: dissolved oxygen became more widespread and penetrated to greater depths; the development of life on land reduced the run-off of nutrients and hence the risk of eutrophication and anoxic events; and marine ecosystems became more diversified so that food chains were less likely to be disrupted.[177][178]
  • Reasonably complete fossils are very rare, most extinct organisms are represented only by partial fossils, and complete fossils are rarest in the oldest rocks. So paleontologists have mistakenly assigned parts of the same organism to different genera which were often defined solely to accommodate these finds – the story of Anomalocaris is an example of this. The risk of this mistake is higher for older fossils because these are often unlike parts of any living organism. Many of the "superfluous" genera are represented by fragments which are not found again and the "superfluous" genera appear to become extinct very quickly.[176]
All genera
"Well-defined" genera
Trend line
"Big Five" mass extinctions
Other mass extinctions
Million years ago
Thousands of genera
Phanerozoic biodiversity as shown by the fossil record

Biodiversity in the fossil record, which is

"the number of distinct genera alive at any given time; that is, those whose first occurrence predates and whose last occurrence postdates that time"[179]

shows a different trend: a fairly swift rise from 542 to 400 million years ago; a slight decline from 400 to 200 million years ago, in which the devastating Permian–Triassic extinction event is an important factor; and a swift rise from 200 million years ago to the present.[179]

The present

Oxygenic photosynthesis accounts for virtually all of the production of organic matter from non-organic ingredients. Production is split about evenly between land and marine plants, and phytoplankton are the dominant marine producers.[180]

The processes that drive evolution are still operating. Well-known examples include the changes in coloration of the peppered moth over the last 200 years and the more recent appearance of pathogens that are resistant to antibiotics.[181][182] There is even evidence that humans are still evolving, and possibly at an accelerating rate over the last 40,000 years.[183]

See also

Footnotes

  1. ^ Name given as in Butterfield's paper "Bangiomorpha pubescens ..." (2000). A fossil fish, also from China, has also been named Qingshania. The name of one of these will have to change.
  2. ^ Myxozoa were thought to be an exception, but are now thought to be heavily modified members of the Cnidaria: Jímenez-Guri, E., Philippe, H., Okamura, B. and Holland, P. W. H. (July 2007). "Buddenbrockia is a cnidarian worm". Science 317 (116): 116–118. doi:10.1126/science.1142024. PMID 17615357. http://www.sciencemag.org/cgi/content/abstract/317/5834/116. Retrieved 2008-09-03. 

References

  1. ^ Futuyma, Douglas J. (2005). Evolution. Sunderland, Massachusetts: Sinuer Associates, Inc. ISBN 0-87893-187-2. 
  2. ^ a b c Nisbet, E.G., and Fowler, C.M.R. (December 7 1999). "Archaean metabolic evolution of microbial mats". Proceedings of the Royal Society: Biology 266 (1436): 2375. doi:10.1098/rspb.1999.0934.  - abstract with link to free full content (PDF)
  3. ^ Anbar, A.; Duan, Y.; Lyons, T.; Arnold, G.; Kendall, B.; Creaser, R.; Kaufman, A.; Gordon, G. et al. (2007). "A whiff of oxygen before the great oxidation event?". Science (New York, N.Y.) 317 (5846): 1903–1906. doi:10.1126/science.1140325. PMID 17901330.  edit
  4. ^ Bonner, J.T. (1998) The origins of multicellularity. Integr. Biol. 1, 27–36
  5. ^ "The oldest fossils reveal evolution of non-vascular plants by the middle to late Ordovician Period (~450-440 m.y.a.) on the basis of fossil spores" Transition of plants to land
  6. ^ Algeo, T.J. (1998). "Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events". Philosophical Transactions of the Royal Society B: Biological Sciences 353 (1365): 113–130. doi:10.1098/rstb.1998.0195. 
  7. ^ "Metazoa: Fossil Record". http://www.ucmp.berkeley.edu/phyla/metazoafr.html. 
  8. ^ Shu et al. (November 4, 1999). "Lower Cambrian vertebrates from south China". Nature 402: 42–46. doi:10.1038/46965. 
  9. ^ Hoyt, Donald F. (1997). "Synapsid Reptiles". http://www.csupomona.edu/~dfhoyt/classes/zoo138/SYNAPSID.HTML. 
  10. ^ Barry, Patrick L. (January 28, 2002). "The Great Dying". Science@NASA. Science and Technology Directorate, Marshall Space Flight Center, NASA. http://science.nasa.gov/headlines/y2002/28jan_extinction.htm. Retrieved March 26, 2009. 
  11. ^ Tanner LH, Lucas SG & Chapman MG (2004). "Assessing the record and causes of Late Triassic extinctions" (PDF). Earth-Science Reviews 65 (1-2): 103-139. doi:10.1016/S0012-8252(03)00082-5. http://nmnaturalhistory.org/pdf_files/TJB.pdf. Retrieved 2007-10-22. 
  12. ^ Benton, M.J. (2004). Vertebrate Paleontology. Blackwell Publishers. xii-452. ISBN 0-632-05614-2. 
  13. ^ "Amniota - Palaeos". http://www.palaeos.org/Amniota. 
  14. ^ Fastovsky DE, Sheehan PM (2005). "The extinction of the dinosaurs in North America". GSA Today 15 (3): 4–10. doi:10.1130/1052-5173(2005)015<4:TEOTDI>2.0.CO;2. http://www.gsajournals.org/perlserv/?request=get-document&doi=10.1130%2F1052-5173%282005%29015%3C4%3ATEOTDI%3E2.0.CO%3B2. Retrieved 2007-05-18. 
  15. ^ "Dinosaur Extinction Spurred Rise of Modern Mammals". News.nationalgeographic.com. http://news.nationalgeographic.com/news/2007/06/070620-mammals-dinos.html. Retrieved 2009-03-08. 
  16. ^ Van Valkenburgh, B. (1999). "Major patterns in the history of carnivorous mammals". Annual Review of Earth and Planetary Sciences 26: 463–493. doi:10.1146/annurev.earth.27.1.463. http://arjournals.annualreviews.org/doi/abs/10.1146/annurev.earth.27.1.463. 
  17. ^ a b
  18. ^ Galimov, E.M. and Krivtsov, A.M. (December 2005). "Origin of the Earth-Moon System". J. Earth Syst. Sci. 114 (6): 593–600. doi:10.1007/BF02715942.  [1]
  19. ^ a b Cohen, B.A., Swindle, T.D. and Kring, D.A. (December 2000). "Support for the Lunar Cataclysm Hypothesis from Lunar Meteorite Impact Melt Ages". Science 290 (5497): 1754–1756. doi:10.1126/science.290.5497.1754. PMID 11099411. http://www.sciencemag.org/cgi/content/abstract/290/5497/1754. Retrieved 2008-08-31. 
  20. ^
  21. ^ Britt, R.R. (2002-07-24). "Evidence for Ancient Bombardment of Earth". Space.com. http://www.space.com/scienceastronomy/planetearth/earth_bombarded_020724.html. Retrieved 2006-04-15. 
  22. ^ Valley, J.W., Peck, W.H., King, E.M. and Wilde, S.A. (April 2002). "A cool early Earth" (PDF). Geology 30 (4): 351–354. doi:10.1130/0091-7613(2002)030<0351:ACEE>2.0.CO;2. http://www.geology.wisc.edu/zircon/Valley2002Cool_Early_Earth.pdf. Retrieved 2008-09-13. 
  23. ^ Dauphas, N., Robert, F. and Marty, B. (December 2000). "The Late Asteroidal and Cometary Bombardment of Earth as Recorded in Water Deuterium to Protium Ratio". Icarus 148 (2): 508–512. doi:10.1006/icar.2000.6489. 
  24. ^ a b Brasier, M., McLoughlin, N., Green, O. and Wacey, D. (June 2006). "A fresh look at the fossil evidence for early Archaean cellular life" (PDF). Philosophical Transactions of the Royal Society: Biology 361 (1470): 887–902. doi:10.1098/rstb.2006.1835. http://physwww.mcmaster.ca/~higgsp/3D03/BrasierArchaeanFossils.pdf. Retrieved 2008-08-30. 
  25. ^
  26. ^ Mojzsis, S.J., Arrhenius, G., McKeegan, K.D., Harrison, T.M., Nutman, A.P. and Friend, C.R.L. (November 1996). "Evidence for life on Earth before 3,800 million years ago". Nature 384: 55–59. doi:10.1038/384055a0. http://www.nature.com/nature/journal/v384/n6604/abs/384055a0.html. Retrieved 2008-08-30. 
  27. ^ a b Grotzinger, J.P. and Rothman, D.H. (1996). "An abiotic model for stomatolite morphogenesis". Nature 383: 423–425. doi:10. 1038/383423a0. 
  28. ^
  29. ^ Schopf, J. (2006). "Fossil evidence of Archaean life". Philosophical Transactions of the Royal Society of London: B Biological Sciences 361 (1470): 869–85. doi:10.1098/rstb.2006.1834. PMID 16754604. 
  30. ^ Ciccarelli, F.D., Doerks, T., von Mering, C., Creevey, C.J., et al (2006). "Toward automatic reconstruction of a highly resolved tree of life". Science 311 (5765): 1283–7. doi:10.1126/science.1123061. PMID 16513982. 
  31. ^ Mason, S.F. (1984). "Origins of biomolecular handedness". Nature 311 (5981): 19–23. doi:10.1038/311019a0. PMID 6472461. 
  32. ^ Orgel, L.E. (October 1994). "The origin of life on the earth" (PDF). Scientific American 271 (4): 76–83. http://courses.washington.edu/biol354/The%20Origin%20of%20Life%20on%20Earth.pdf. Retrieved 2008-08-30.  Also available as a web page
  33. ^ a b c Cowen, R. (2000). History of Life (3rd ed.). Blackwell Science. p. 6. ISBN 0632044446. 
  34. ^ Villarreal LP, Witzany G (October 2009). "Viruses are essential agents within the roots and stem of the tree of life". J. Theor. Biol.. doi:10.1016/j.jtbi.2009.10.014. PMID 19833132. 
  35. ^ O'Leary, M.R. (2008). Anaxagoras and the Origin of Panspermia Theory. iUniverse, Inc.. ISBN 0595495966. 
  36. ^ a b Arrhenius, S. (1903). "The Propagation of Life in Space". Die Umschau volume=7.  Reprinted in Goldsmith, D.,, ed. The Quest for Extraterrestrial Life. University Science Books. ISBN 0198557043. 
  37. ^ Hoyle, F. and Wickramasinghe, C. (1979). "On the Nature of Interstellar Grains". Astrophysics and Space Science 66: 77–90. doi:10.1007/BF00648361. 
  38. ^ a b Crick, F (1973). "Directed Panspermia". Icarus 19: 341–348. doi:10.1016/0019-1035(73)90110-3. 
  39. ^ a b c d Warmflash, D. and Weiss, B. (November 2005). "Did Life Come From Another World?". Scientific American: 64–71. http://www.sciam.com/article.cfm?articleID=00073A97-5745-1359-94FF83414B7F0000&pageNumber=1&catID=2. Retrieved 2008-09-02. 
  40. ^ Ker, Than (August 2007). "Claim of Martian Life Called 'Bogus'". space.com. http://www.space.com/news/070823_mars_life.html. Retrieved 2008-09-02. 
  41. ^ Bennett, J. O. (2008). "What is life?". Beyond UFOs: The Search for Extraterrestrial Life and Its Astonishing Implications for Our Future. Princeton University Press. pp. 82–85. ISBN 0691135495. http://books.google.co.uk/books?id=lEQKnip7St4C&pg=PA84&dq=life+earth+carbon+water&lr=#PPA85,M1. Retrieved 2009-01-11. 
  42. ^ Schulze-Makuch, D., Irwin, L. N. (April 2006). "The prospect of alien life in exotic forms on other worlds". Naturwissenschaften 93 (4): 155–72. doi:10.1007/s00114-005-0078-6. PMID 16525788. 
  43. ^ Peretó, J. (2005). "Controversies on the origin of life" (PDF). Int. Microbiol. 8 (1): 23–31. PMID 15906258. http://www.im.microbios.org/0801/0801023.pdf. Retrieved 2007-10-07. 
  44. ^ Szathmáry, E. (February 2005). "Life: In search of the simplest cell". Nature 433: 469–470. doi:10.1038/433469a. http://www.nature.com/nature/journal/v433/n7025/full/433469a.html. Retrieved 2008-09-01. 
  45. ^ Luisi, P. L., Ferri, F. and Stano, P. (2006). "Approaches to semi-synthetic minimal cells: a review". Naturwissenschaften 93 (1): 1–13. doi:10.1007/s00114-005-0056-z. PMID 16292523. 
  46. ^ Joyce, G.F. (2002). "The antiquity of RNA-based evolution". Nature 418 (6894): 214–21. doi:10.1038/418214a. PMID 12110897. 
  47. ^ a b Hoenigsberg, H. (December 2003)). "Evolution without speciation but with selection: LUCA, the Last Universal Common Ancestor in Gilbert’s RNA world". Genetic and Molecular Research 2 (4): 366–375. PMID 15011140. http://www.funpecrp.com.br/gmr/year2003/vol4-2/gmr0070_full_text.htm. Retrieved 2008-08-30. (also available as PDF)
  48. ^ Trevors, J. T. and Abel, D. L. (2004). "Chance and necessity do not explain the origin of life". Cell Biol. Int. 28 (11): 729–39. doi:10.1016/j.cellbi.2004.06.006. PMID 15563395. 
  49. ^ Forterre, P., Benachenhou-Lahfa, N., Confalonieri, F., Duguet, M., Elie, C. and Labedan, B. (1992). "The nature of the last universal ancestor and the root of the tree of life, still open questions". BioSystems 28 (1-3): 15–32. doi:10.1016/0303-2647(92)90004-I. PMID 1337989. 
  50. ^ Cech, T.R. (August 2000). "The ribosome is a ribozyme". Science 289 (5481): 878–9. doi:10.1126/science.289.5481.878. PMID 10960319. http://www.sciencemag.org/cgi/content/short/289/5481/878. Retrieved 2008-09-01. 
  51. ^ Johnston, W. K. et al (2001). "RNA-Catalyzed RNA Polymerization: Accurate and General RNA-Templated Primer Extension". Science 292 (5520): 1319–1325. doi:10.1126/science.1060786. PMID 11358999. 
  52. ^ a b
  53. ^ Orgel, L. (November 2000). "Origin of life. A simpler nucleic acid". Science (journal) 290 (5495): 1306–7. PMID 11185405. 
  54. ^ Nelson, K.E., Levy, M., and Miller, S.L. (April 2000). "Peptide nucleic acids rather than RNA may have been the first genetic molecule". Proc. Natl. Acad. Sci. U.S.A. 97 (8): 3868–71. doi:10.1073/pnas.97.8.3868. PMID 10760258. PMC 18108. http://www.pnas.org/cgi/pmidlookup?view=long&pmid=10760258. 
  55. ^ Martin, W. and Russell, M.J. (2003). "On the origins of cells: a hypothesis for the evolutionary transitions from abiotic geochemistry to chemoautotrophic prokaryotes, and from prokaryotes to nucleated cells". Philosophical Transactions of the Royal Society: Biological 358: 59–85. doi:10.1098/rstb.2002.1183. PMID 12594918. 
  56. ^ Wächtershäuser, G. (August 2000). "Origin of life. Life as we don't know it". Science (journal) 289 (5483): 1307–8. PMID 10979855. 
  57. ^ Trevors, J.T. and Psenner, R. (2001). "From self-assembly of life to present-day bacteria: a possible role for nanocells". FEMS Microbiol. Rev. 25 (5): 573–82. doi:10.1111/j.1574-6976.2001.tb00592.x. PMID 11742692. 
  58. ^ Segré, D., Ben-Eli, D., Deamer, D. and Lancet, D. (February-April 2001). "The Lipid World" (PDF). Origins of Life and Evolution of Biospheres 2001 31 (1-2): 119–45. doi:10.1023/A:1006746807104. PMID 11296516. http://ool.weizmann.ac.il/Segre_Lipid_World.pdf. Retrieved 2008-09-01. 
  59. ^ Cairns-Smith, A.G. (1968), "An approach to a blueprint for a primitive organism", in Waddington, C,H., Towards a Theoretical Biology, 1, Edinburgh University Press, pp. 57–66 
  60. ^ Ferris, J.P. (June 1999). "Prebiotic Synthesis on Minerals: Bridging the Prebiotic and RNA Worlds". Biological Bulletin. Evolution: A Molecular Point of View 196 (3): 311–314. doi:10.2307/1542957. http://www.jstor.org/pss/1542957. Retrieved 2008-09-01. 
  61. ^ Hanczyc, M.M., Fujikawa, S.M. and Szostak, Jack W. (October 2003). "Experimental Models of Primitive Cellular Compartments: Encapsulation, Growth, and Division". Science 302 (5645): 618–622. doi:10.1126/science.1089904. PMID 14576428. http://www.sciencemag.org/cgi/content/abstract/302/5645/618. Retrieved 2008-09-01. 
  62. ^ Hartman, H. (October 1998). "Photosynthesis and the Origin of Life". Origins of Life and Evolution of Biospheres 28 (4–6): 512–521. http://www.springerlink.com/content/t1n325268n01217k/. Retrieved 2008-09-01. 
  63. ^ a b Krumbein, W.E., Brehm, U., Gerdes, G., Gorbushina, A.A., Levit, G. and Palinska, K.A. (2003), "Biofilm, Biodictyon, Biomat Microbialites, Oolites, Stromatolites, Geophysiology, Global Mechanism, Parahistology", in Krumbein, W.E., Paterson, D.M., and Zavarzin, G.A. (PDF), Fossil and Recent Biofilms: A Natural History of Life on Earth, Kluwer Academic, pp. 1–28, ISBN 1402015976, http://134.106.242.33/krumbein/htdocs/Archive/397/Krumbein_397.pdf, retrieved 2008-07-09 
  64. ^ a b Risatti, J. B., Capman, W. C. and Stahl, D. A. (October 11, 1994). "Community structure of a microbial mat: the phylogenetic dimension" (PDF). Proceedings of the National Academy of Sciences 91 (21): 10173–10177. doi:10.1073/pnas.91.21.10173. PMID 7937858. http://www.pnas.org/content/91/21/10173.full.pdf. Retrieved 2008-07-09. 
  65. ^ (the editor) (June 2006)). "Editor's Summary: Biodiversity rocks". Nature 441. http://www.nature.com/nature/journal/v441/n7094/edsumm/e060608-01.html. Retrieved 2009-01-10. 
  66. ^ Allwood, A. C., Walter, M. R., Kamber, B. S., Marshall, C. P. and Burch, I. W. (June 2006)). "Stromatolite reef from the Early Archaean era of Australia". Nature 441: 714–718. doi:10.1038/nature04764. http://www.nature.com/nature/journal/v441/n7094/abs/nature04764.html. Retrieved 2008-08-31. 
  67. ^ Blankenship, R.E. (1 January 2001). "Molecular evidence for the evolution of photosynthesis". Trends in Plant Science 6 (1): 4–6. doi:10.1038/35085554. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6TD1-424KK4J-3&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=6f38f9f1d29b24fc90d0145837338b9e. Retrieved 2008-07-14. 
  68. ^ Hoehler, T.M., Bebout, B.M. and Des Marais, D.J. (19 July 2001). "The role of microbial mats in the production of reduced gases on the early Earth". Nature 412: 324–327. doi:10.1038/35085554. http://www.nature.com/nature/journal/v412/n6844/full/412324a0.html. Retrieved 2008-07-14. 
  69. ^ Abele, D. (7 November 2002). "Toxic oxygen: The radical life-giver". Nature 420 (27): 27. doi:10.1038/420027a. http://www.nature.com/nature/journal/v420/n6911/full/420027a.html. Retrieved 2008-07-14. 
  70. ^ "Introduction to Aerobic Respiration". University of California, Davis. http://trc.ucdavis.edu/biosci10v/bis10v/week3/06aerobicrespirintro.html. Retrieved 2008-07-14. 
  71. ^ Goldblatt, C., Lenton, T.M. and Watson, A.J. (2006). "The Great Oxidation at ~2.4 Ga as a bistability in atmospheric oxygen due to UV shielding by ozone" (PDF). Geophysical Research Abstracts 8 (00770). http://www.cosis.net/abstracts/EGU06/00770/EGU06-J-00770.pdf. Retrieved 2008-09-01. 
  72. ^ a b Glansdorff, N., Xu, Y. and Labedan, B. (2008). "The Last Universal Common Ancestor: emergence, constitution and genetic legacy of an elusive forerunner". Biology Direct 3 (29): 29. doi:10.1186/1745-6150-3-29. 
  73. ^ a b Brocks, J. J., Logan, G. A., Buick, R. and Summons, R. E. (1999). "Archaean molecular fossils and the rise of eukaryotes". Science 285: 1033–1036. doi:10.1126/science.285.5430.1033. PMID 10446042. http://www.sciencemag.org/cgi/content/abstract/285/5430/1033. Retrieved 2008-09-02. 
  74. ^ a b Hedges, S. B., Blair, J. E., Venturi, M. L. and Shoe, J. L (January 2004). "A molecular timescale of eukaryote evolution and the rise of complex multicellular life". BMC Evolutionary Biology 4 (2): 2. doi:10.1186/1471-2148-4-2. http://www.biomedcentral.com/1471-2148/4/2/abstract/. Retrieved 2008-07-14. 
  75. ^ Burki, F., Shalchian-Tabrizi, K., Minge, M., Skjæveland, Å., Nikolaev, S. I. et al. (2007). "Phylogenomics Reshuffles the Eukaryotic Supergroups". PLoS ONE 2 (8): e790. doi:10.1371/journal.pone.0000790. 
  76. ^ Parfrey, L. W., Barbero, E., Lasser, E., Dunthorn, M., Bhattacharya, D., Patterson, D.J. and Katz, L.A. (December 2006). "Evaluating Support for the Current Classification of Eukaryotic Diversity". PLoS Genetics 2 (12): e220. doi:10.1371/journal.pgen.0020220. PMID 17194223. 
  77. ^ Margulis, L. (1981). Symbiosis in cell evolution. San Francisco: W.H. Freeman. ISBN 0716712563. 
  78. ^ Vellai, T. and Vida, G. (1999). "The origin of eukaryotes; the difference between eukaryotic and prokaryotic cells". Proceedings of the Royal Society: Biology 266: 1571–1577. doi:10.1098/rspb.1999.0817. 
  79. ^ Selosse, M-A., Abert, B., and Godelle, B. (2001). "Reducing the genome size of organelles favours gene transfer to the nucleus". Trends in ecology & evolution 16 (3): 135–141. doi:10.1016/S0169-5347(00)02084-X. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VJ1-429XTFM-H&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_version=1&_urlVersion=0&_userid=10&md5=8370ca16bcde45bfa1c050068a2d6e19. Retrieved 2008-09-02. 
  80. ^ Pisani, D., Cotton, J.A. and McInerney, J.O. (2007). "Supertrees disentangle the chimerical origin of eukaryotic genomes". Mol Biol Evol. 24 (8): 1752–60. doi:10.1093/molbev/msm095. PMID 17504772. 
  81. ^ Gray, M.W., Burger, G., and Lang, B.F. (1999). "Mitochondrial evolution". Science 283 (5407): 1476–1481. doi:10.1126/science.283.5407.1476. PMID 10066161. http://www.sciencemag.org/cgi/content/abstract/283/5407/1476. Retrieved 2008-09-02. 
  82. ^ Rasmussen, B., Fletcher, I.R., Brocks, J.R. and Kilburn, M.R. (October 2008). "Reassessing the first appearance of eukaryotes and cyanobacteria". Nature 455: 1101–1104. doi:10.1038/nature07381. 
  83. ^ a b c d Fedonkin, M. A. (March 2003). "The origin of the Metazoa in the light of the Proterozoic fossil record" (PDF). Paleontological Research 7 (1): 9–41. doi:10.2517/prpsj.7.9. http://www.vend.paleo.ru/pub/Fedonkin_2003.pdf. Retrieved 2008-09-02. 
  84. ^ Han, T.M. and Runnegar, B. (July 1992). "Megascopic eukaryotic algae from the 2.1-billion-year-old negaunee iron-formation, Michigan". Science 257 (5067): 232–235. doi:10.1126/science.1631544. PMID 1631544. http://www.sciencemag.org/cgi/content/abstract/257/5067/232. Retrieved 2008-09-02. 
  85. ^ Javaux, E. J., Knoll, A. H. and Walter, M. R. (September 2004). "TEM evidence for eukaryotic diversity in mid-Proterozoic oceans". Geobiology 2 (3): 121–132. doi:10.1111/j.1472-4677.2004.00027.x. http://www3.interscience.wiley.com/journal/118814335/abstract. Retrieved 2008-09-02. 
  86. ^ a b Butterfield, N. J. (2005). "Probable Proterozoic fungi". Paleobiology 31 (1): 165–182. doi:10.1666/0094-8373(2005)031<0165:PPF>2.0.CO;2. http://paleobiol.geoscienceworld.org/cgi/content/abstract/31/1/165. Retrieved 2008-09-02. 
  87. ^ a b Nakagaki, T., Yamada, H. and Tóth, Á. (September 2000). "Intelligence: Maze-solving by an amoeboid organism". Nature 407: 470. doi:10.1038/35035159. http://www.nature.com/nature/journal/v407/n6803/abs/407470a0.html. Retrieved 2008-09-03. 
  88. ^ Bell, G. and Mooers, A.O. (1968). "Size and complexity among multicellular organisms". Biological Journal of the Linnean Society 60 (3): 345–363. doi:10.1111/j.1095-8312.1997.tb01500.x. http://www3.interscience.wiley.com/journal/119168103/abstract. Retrieved 2008-09-03. 
  89. ^ Kaiser, D. (2001). "Building a multicellular organism". Annual Review of Genetics 35: 103–123. doi:10.1146/annurev.genet.35.102401.090145. PMID 11700279. 
  90. ^ a b Bonner, J. T. (January 1999). "The Origins of Multicellularity". Integrative Biology 1 (1): 27–36. doi:10.1002/(SICI)1520-6602(1998)1:1<27::AID-INBI4>3.0.CO;2-6. http://doi.wiley.com/10.1002/(SICI)1520-6602(1998)1:1%3C27::AID-INBI4%3E3.0.CO;2-6. Retrieved 2008-09-03. 
  91. ^ a b c d e Butterfield, N. J. (September 2000). "Bangiomorpha pubescens n. gen., n. sp.: implications for the evolution of sex, multicellularity, and the Mesoproterozoic/Neoproterozoic radiation of eukaryotes". Paleobiology 26 (3): 386–404. doi:10.1666/0094-8373(2000)026<0386:BPNGNS>2.0.CO;2. http://paleobiol.geoscienceworld.org/cgi/content/abstract/26/3/386. Retrieved 2008-09-02. 
  92. ^ a b c d e Jokela, J. (2001), "Sex: Advantage", Encyclopedia of Life Sciences, John Wiley & Sons, Ltd., doi:10.1038/npg.els.0001716 
  93. ^ Holmes, R.K. and Jobling, M.G. (1996), "Genetics: Exchange of Genetic Information", in Baron, S., Baron's Medical Microbiology (4th ed.), Galveston: University of Texas Medical Branch, ISBN 0-9631172-1-1, http://www.ncbi.nlm.nih.gov/books/bv.fcgi?highlight=conjugation&rid=mmed.section.468, retrieved 2008-09-02 
  94. ^ Christie, P. J. (April 2001). "Type IV secretion: intercellular transfer of macromolecules by systems ancestrally related to conjugation machines". Molecular Microbiology 40 (22): 294–305. doi:10.1046/j.1365-2958.2001.02302.x. http://lib.bioinfo.pl/meid:10183. Retrieved 2008-09-02. 
  95. ^ Ramesh, M. A., Malik, S-B. and Logsdon, J. M. Jr. (January 2005). "A phylogenomic inventory of meiotic genes; evidence for sex in Giardia and an early eukaryotic origin of meiosis" (PDF). Current Biology 15 (2): 185–91. doi:10.1016/j.cub.2005.01.003. http://euplotes.biology.uiowa.edu/web/jmlpubls/rml05.pdf. Retrieved 2008-12-22. 
  96. ^ a b Otto, S. P., and Gerstein, A. C. (2006). "Why have sex? The population genetics of sex and recombination". Biochemical Society Transactions 34: 519–522. doi:10.1042/BST0340519. http://www.biochemsoctrans.org/bst/034/0519/bst0340519.htm. Retrieved 2008-12-22. 
  97. ^ a b Dong, L., Xiao, S., Shen, B. and Zhou, C. (January 2008). "Silicified Horodyskia and Palaeopascichnus from upper Ediacaran cherts in South China: tentative phylogenetic interpretation and implications for evolutionary stasis". Journal of the Geological Society 165: 367–378. doi:10.1144/0016-76492007-074. http://findarticles.com/p/articles/mi_qa3721/is_200801/ai_n24394476/pg_1?tag=artBody;col1. Retrieved 2008-09-02. 
  98. ^ Gaidos, E., Dubuc, T., Dunford, M., McAndrew, P., Padilla-gamiño, J., Studer, B., Weersing, K. and Stanley, S. (2007). "The Precambrian emergence of animal life: a geobiological perspective" (PDF). Geobiology 5: 351. doi:10.1111/j.1472-4669.2007.00125.x. http://www.soest.hawaii.edu/GG/FACULTY/GAIDOS/geobiology2007.pdf. Retrieved 2008-09-03. 
  99. ^ Davidson, M.W.. "Animal Cell Structure". Florida State University. http://micro.magnet.fsu.edu/cells/animalcell.html. Retrieved 2008-09-03. 
  100. ^ Saupe, S.G. "Concepts of Biology". College of St. Benedict / St. John's University. http://employees.csbsju.edu/SSAUPE/biol116/Zoology/digestion.htm. Retrieved 2008-09-03. 
  101. ^ Hinde, R. T. (1998). "The Cnidaria and Ctenophora". in Anderson, D.T.,. Invertebrate Zoology. Oxford University Press. pp. 28–57. ISBN 0195513681. 
  102. ^ Chen, J.-Y., Oliveri, P., Gao, F., Dornbos, S.Q., Li, C-W., Bottjer, D.J. and Davidson, E.H. (August 2002). "Precambrian Animal Life: Probable Developmental and Adult Cnidarian Forms from Southwest China" (PDF). Developmental Biology 248 (1): 182–196. doi:10.1006/dbio.2002.0714. http://www.uwm.edu/~sdornbos/PDF's/Chen%20et%20al.%202002.pdf. Retrieved 2008-09-03. 
  103. ^ Grazhdankin, D. (2004). "Patterns of distribution in the Ediacaran biotas: facies versus biogeography and evolution". Paleobiology 30: 203. doi:10.1666/0094-8373(2004)030<0203:PODITE>2.0.CO;2. ISSN 0094–8373. 
  104. ^ Seilacher, A. (1992). "Vendobionta and Psammocorallia: lost constructions of Precambrian evolution" (abstract). Journal of the Geological Society, London 149 (4): 607–613. doi:10.1144/gsjgs.149.4.0607. ISSN 0016–7649. http://jgs.lyellcollection.org/cgi/content/abstract/149/4/607. Retrieved 2007-06-21. 
  105. ^ Martin, M.W.; Grazhdankin, D. V., Bowring, S. A., Evans, D. A. D., Fedonkin, M. A. and Kirschvink, J. L. (2000-05-05). "Age of Neoproterozoic Bilaterian Body and Trace Fossils, White Sea, Russia: Implications for Metazoan Evolution" (abstract). Science 288 (5467): 841. doi:10.1126/science.288.5467.841. PMID 10797002. http://www.scienceonline.org/cgi/content/abstract/288/5467/841. Retrieved 2008-07-03. 
  106. ^ Fedonkin, M. A. and Waggoner, B. (1997). "The late Precambrian fossil Kimberella is a mollusc-like bilaterian organism" (abstract). Nature 388: 868–871. doi:10.1038/42242. http://www.nature.com/nature/journal/v388/n6645/abs/388868a0.html. Retrieved 2008-07-03. 
  107. ^ Mooi, R. and Bruno, D. (1999). "Evolution within a bizarre phylum: Homologies of the first echinoderms" (PDF). American Zoologist 38: 965–974. http://icb.oxfordjournals.org/cgi/reprint/38/6/965.pdf. Retrieved 2007-11-24. 
  108. ^ McMenamin, M. A. S (2003). "Spriggina is a trilobitoid ecdysozoan" (abstract). Abstracts with Programs (Geological Society of America) 35 (6): 105. http://gsa.confex.com/gsa/2003AM/finalprogram/abstract_62056.htm. Retrieved 2007-11-24. 
  109. ^ Lin, J. P.; Gon, S.M.; Gehling, J.G.; Babcock, L.E.; Zhao, Y.L.; Zhang, X.L.; Hu, S.X.; Yuan, J.L.; Yu, M.Y.; Peng, J. (2006). "A Parvancorina-like arthropod from the Cambrian of South China". Historical Biology 18 (1): 33–45. doi:10.1080/08912960500508689.  edit
  110. ^ Butterfield, N. J. (2006). "Hooking some stem-group "worms": fossil lophotrochozoans in the Burgess Shale". Bioessays 28 (12): 1161–6. doi:10.1002/bies.20507. 
  111. ^ a b c Bengtson, S. (2004), Early skeletal fossils, in Lipps, J.H., and Waggoner, B.M., "Neoproterozoic - Cambrian Biological Revolutions" (PDF), Palentological Society Papers 10: 67–78, http://www.cosmonova.org/download/18.4e32c81078a8d9249800021554/Bengtson2004ESF.pdf, retrieved 2008-07-18 
  112. ^ Gould, S. J. (1989). Wonderful Life. Hutchinson Radius. pp. 124–136 and many others. ISBN 0091742714. 
  113. ^ Gould, S. J. (1989). Wonderful Life: The Burgess Shale and the Nature of History. W.W. Norton & Company. ISBN 039330700X. 
  114. ^ Budd, G. E. (2003). "The Cambrian Fossil Record and the Origin of the Phyla" (Free full text). Integrative and Comparative Biology 43 (1): 157–165. doi:10.1093/icb/43.1.157. http://intl-icb.oxfordjournals.org/cgi/content/abstract/43/1/157. Retrieved 2008-07-15. 
  115. ^ Budd, G. E. (1996). "The morphology of Opabinia regalis and the reconstruction of the arthropod stem-group". Lethaia 29 (1): 1–14. doi:10.1111/j.1502-3931.1996.tb01831.x. 
  116. ^ Marshall, C. R. (2006). "Explaining the Cambrian “Explosion” of Animals". Annu. Rev. Earth Planet. Sci. 34: 355–384. doi:10.1146/annurev.earth.33.031504.103001. http://arjournals.annualreviews.org/doi/abs/10.1146/annurev.earth.33.031504.103001?journalCode=earth. Retrieved 2007-11-06. 
  117. ^ Janvier, P. (2001), "Vertebrata (Vertebrates)", Encyclopedia of Life Sciences, Wiley InterScience, doi:10.1038/npg.els.0001531 
  118. ^ Conway Morris, S. (August 2, 2003). "Once we were worms". New Scientist 179 (2406): 34. http://cas.bellarmine.edu/tietjen/Evolution/once_we_were_worms.htm. Retrieved 2008-09-05. 
  119. ^ Shu, D-G., Luo, H-L., Conway Morris, S., Zhang, X-L., Hu, S-X., Chen, L., J. Han, J., Zhu, M., Li, Y. and Chen, L-Z. (November 1999). "Lower Cambrian vertebrates from south China" (PDF). Nature 402: 42–46. doi:10.1038/46965. http://www.bios.niu.edu/davis/bios458/Shu1.pdf. Retrieved 2008-09-05. 
  120. ^ Shu, D.-G., Conway Morris, S., Han, J., Zhang, Z.-F., Yasui, K., Janvier, P., Chen, L., Zhang, X.-L., Liu, J.-N., Li, Y. and Liu, H.-Q. (January 2003). "Head and backbone of the Early Cambrian vertebrate Haikouichthys". Nature 421: 526–529. doi:10.1038/nature01264. http://www.nature.com/nature/journal/v421/n6922/abs/nature01264.html. Retrieved 2008-09-05. 
  121. ^ Sansom I. J., Smith, M. M. and Smith, M. P. (2001), "The Ordovician radiation of vertebrates", in Ahlberg, P.E., Major Events in Early Vertebrate Evolution, Taylor and Francis, pp. 156–171, ISBN 0-415-23370-4 
  122. ^ a b Cowen, R. (2000). History of Life (3rd ed.). Blackwell Science. pp. 120–122. ISBN 0632044446. 
  123. ^ a b c Selden, P. A. (2001), ""Terrestrialization of Animals"", in Briggs, D.E.G., and Crowther, P.R., Palaeobiology II: A Synthesis, Blackwell, pp. 71–74, ISBN 0632051493, http://books.google.co.uk/books?id=AHsrhGOTRM4C&pg=PA71&lpg=PA71&dq=%22Terrestrialization+of+Animals%22+selden&source=web&ots=ImrDW71qDp&sig=JptdVx34SMIjKamHXDnEpKSE78s&hl=en&sa=X&oi=book_result&resnum=1&ct=result#PPA74,M1, retrieved 2008-09-05 
  124. ^ a b c d e f g Shear, W.A. (2000), "The Early Develpoment of Terrestrial Ecosystems", in Gee, H., Shaking the Tree: Readings from Nature in the History of Life, University of Chicago Press, pp. 169–184, ISBN 0226284964, http://books.google.co.uk/books?hl=en&lr=&id=ZJe_Dmdbm-QC&oi=fnd&pg=PA233&dq=evolution+flowering+plant+angiosperm&ots=abVpqx_cP8&sig=z1HvmrRLdJP9oPkN0bffbAyriEI#PPA233,M1, retrieved 2008-09-09 
  125. ^ a b Hawksworth, D.L. (2001), "Lichens", Encyclopedia of Life Sciences, John Wiley & Sons, Ltd., doi:10.1038/npg.els.0000368 
  126. ^ Retallack, G.J.; Feakes, C.R. (1987). "Trace Fossil Evidence for Late Ordovician Animals on Land". Science 235 (4784): 61–63. doi:10.1126/science.235.4784.61. 
  127. ^ a b Kenrick, P. and Crane, P. R. (September 1997). "The origin and early evolution of plants on land" (PDF). Nature 389: 33. doi:10.1038/37918. http://botit.botany.wisc.edu/courses/botany_940/06EvidEvol/papers/KendrickCrane1997.pdf. Retrieved 2008-09-05. 
  128. ^ Scheckler, S. E. (2001), ""Afforestation – the First Forests"", in Briggs, D.E.G., and Crowther, P.R., Palaeobiology II: A Synthesis, Blackwell, pp. 67–70, ISBN 0632051493, http://books.google.co.uk/books?id=AHsrhGOTRM4C&pg=PA69&lpg=PA69&dq=devonian+meandering+plants+trees&source=web&ots=ImrDW61pBt&sig=RsDgJXv-NNu6Rxk_yFpb5espyLY&hl=en&sa=X&oi=book_result&resnum=3&ct=result, retrieved 2008-09-05 
  129. ^ The phrase "Late Devonian wood crisis" is used at "Palaeos – Tetrapoda: Acanthostega". PALAEOS: The Trace of Life on Earth. http://www.palaeos.com/Vertebrates/Units/150Tetrapoda/150.150.html. Retrieved 2008-09-05. 
  130. ^ a b Algeo, T. J. and Scheckler, S. E. (1998). "Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events". Philosophical Transactions of the Royal Society: Biology 353: 113–130. doi:10.1098/rstb.1998.0195. 
  131. ^ Taylor T. N. and Osborn J. M. (1996). "The importance of fungi in shaping the paleoecosystem". Review of Paleobotany and Palynology 90: 249–262. doi:10.1016/0034-6667(95)00086-0. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V6W-454YDFK-7&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=9d5d008d99d044684e947ad74b05514d. Retrieved 2008-09-05. 
  132. ^ MacNaughton, R. B., Cole, J. M., Dalrymple, R. W., Braddy, S. J., Briggs, D. E. G. and Lukie, T. D. (May 2002). "First steps on land: Arthropod trackways in Cambrian-Ordovician eolian sandstone, southeastern Ontario, Canada". Geology 30 (5): 391–394. doi:10.1130/0091-7613(2002)030<0391:FSOLAT>2.0.CO;2. http://geology.geoscienceworld.org/cgi/content/abstract/30/5/391. Retrieved 2008-09-05. 
  133. ^ Vaccari, N. E., Edgecombe, G. D. and Escudero, C. (2004). "Cambrian origins and affinities of an enigmatic fossil group of arthropods". Nature 430: 554–557. doi:10.1038/nature02705. 
  134. ^ Buatois, L. A., Mangano, M. G., Genise, J. F. and Taylor, T. N. (June 1998). "The ichnologic record of the continental invertebrate invasion; evolutionary trends in environmental expansion, ecospace utilization, and behavioral complexity". PALAIOS 13 (3): 217–240. doi:10.2307/3515447. http://palaios.sepmonline.org/cgi/content/abstract/13/3/217. Retrieved 2008-09-05. 
  135. ^ Cowen, R. (2000). History of Life (3rd ed.). Blackwell Science. p. 126. ISBN 0632044446. 
  136. ^ Grimaldi, D. and Engel, M. (2005). "Insects Take to the Skies". Evolution of the Insects. Cambridge University Press. pp. 155–160. ISBN 0521821495. http://books.google.co.uk/books?id=Ql6Jl6wKb88C&dq=%22Evolution+of+the+Insects%22+grimaldi&printsec=frontcover&source=bn&hl=en&sa=X&oi=book_result&resnum=4&ct=result#PPA160,M1. Retrieved 2009-01-11. 
  137. ^ Grimaldi, D. and Engel, M. (2005). "Diversity of evolution". Evolution of the Insects. Cambridge University Press. p. 12. ISBN 0521821495. http://books.google.co.uk/books?id=Ql6Jl6wKb88C&dq=%22Evolution+of+the+Insects%22+grimaldi&printsec=frontcover&source=bn&hl=en&sa=X&oi=book_result&resnum=4&ct=result#PPA160,M1. Retrieved 2009-01-11. 
  138. ^ a b c Clack, J. A. (November, 2005). "Getting a Leg Up on Land". Scientific American. http://www.sciam.com/article.cfm?id=getting-a-leg-up-on-land. Retrieved 2008-09-06. 
  139. ^ a b Ahlberg, P. E. and Milner, A. R. (April 1994). "The Origin and Early Diversification of Tetrapods". Nature 368: 507–514. doi:10.1038/368507a0. http://www.nature.com/nature/journal/v368/n6471/abs/368507a0.html. Retrieved 2008-09-06. 
  140. ^ Gordon, M. S., Graham, J. B. and Wang, T. (September/October 2004). "Revisiting the Vertebrate Invasion of the Land". Physiological and Biochemical Zoology 77 (5): 697–699. doi:10.1086/425182. 
  141. ^ Daeschler, E. B., Shubin, N. H. and Jenkins, F. A. (April 2006). "A Devonian tetrapod-like fish and the evolution of the tetrapod body plan" (PDF). Nature 440: 757–763. doi:10.1038/nature04639. http://www.com.univ-mrs.fr/~boudouresque/Publications_DOM_2006_2007/Daeschler_et_al_2006_Nature.pdf. Retrieved 2008-09-06. 
  142. ^ Debraga, M. and Rieppel, O. (July 1997). "Reptile phylogeny and the interrelationships of turtles". Zoological Journal of the Linnean Society 120 (3): 281–354. doi:10.1111/j.1096-3642.1997.tb01280.x. http://www3.interscience.wiley.com/journal/119830935/abstract. Retrieved 2008-09-07. 
  143. ^ a b Benton M. J. and Donoghue, P. C. J. (2007). "Paleontological Evidence to Date the Tree of Life". Molecular Biology and Evolution 24 (1): 26–53. doi:10.1093/molbev/msl150. PMID 17047029. http://mbe.oxfordjournals.org/cgi/content/full/24/1/26. Retrieved 2008-09-07. 
  144. ^ a b Benton, M. J. (May 1990). "Phylogeny of the Major Tetrapod Groups: Morphological Data and Divergence Dates". Journal of Molecular Evolution 30 (5): 409–424. doi:10.1007/BF02101113. http://www.springerlink.com/content/k152294003652458/. Retrieved 2008-09-07. 
  145. ^ Sidor, C. A., O'Keefe, F. R., Damiani, R., Steyer, J. S., Smith, R. M. H., Larsson, H. C. E., Sereno, P. C., Ide, O., and Maga, A. (April 2005). "Permian tetrapods from the Sahara show climate-controlled endemism in Pangaea". Nature 434: 886–889. doi:10.1038/nature03393. http://www.nature.com/nature/journal/v434/n7035/full/nature03393.html. Retrieved 2008-09-08. 
  146. ^ Smith, R. and Botha, J. (September-October 2005). "The recovery of terrestrial vertebrate diversity in the South African Karoo Basin after the end-Permian extinction". Comptes Rendus Palevol 4: 623–636. doi:10.1016/j.crpv.2005.07.005. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6X1G-4GYH7VN-1&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_version=1&_urlVersion=0&_userid=10&md5=add24b0622f2aff0b41e7c42a3160fa7. Retrieved 2008-09-08. 
  147. ^ Benton, M. J. (2005). When Life Nearly Died: The Greatest Mass Extinction of All Time. Thames & Hudson. ISBN 978-0500285732. 
  148. ^ Sahney, S. and Benton, M.J. (2008). "Recovery from the most profound mass extinction of all time" (PDF). Proceedings of the Royal Society: Biological 275: 759. doi:10.1098/rspb.2007.1370. http://journals.royalsociety.org/content/qq5un1810k7605h5/fulltext.pdf. 
  149. ^ Gauthier, J., Cannatella, D. C., de Queiroz, K., Kluge, A. G. and Rowe, T. (1989), "Tetrapod Phylogeny", in B. Fernholm, B., Bremer K., and Jörnvall, H. (PDF), The Hierarchy of Life, Elsevier Science, p. 345, http://si-pddr.si.edu/dspace/bitstream/10088/4689/1/VZ_1989GauthieretalHierLife.pdf, retrieved 2008-09-08 
  150. ^ Benton, M. J. (March 1983), "Dinosaur Success in the Triassic: a Noncompetitive Ecological Model" (PDF), Quarterly Review of Biology 58 (1), http://palaeo.gly.bris.ac.uk/Benton/reprints/1983success.pdf, retrieved 2008-09-08 
  151. ^ a b Padian, K. (2004). "Basal Avialae". in Weishampel, David B.; Dodson, Peter; & Osmólska, Halszka (eds.). The Dinosauria (Second ed.). Berkeley: University of California Press. pp. 210–231. ISBN 0-520-24209-2. 
  152. ^ Hou, L., Zhou, Z., Martin, L. D. and Feduccia, A. (October 2002). "A beaked bird from the Jurassic of China". Nature 377: 616–618. doi:10.1038/377616a0. http://www.nature.com/nature/journal/v377/n6550/abs/377616a0.html. Retrieved 2008-09-08. 
  153. ^ Clarke, J. A., Zhou, Z. and Zhang, F. (2006). "Insight into the evolution of avian flight from a new clade of Early Cretaceous ornithurines from China and the morphology of Yixianornis grabaui". Journal of Anatomy 208 (3): 287–308. doi:10.1111/j.1469-7580.2006.00534.x. http://www3.interscience.wiley.com/journal/118559634/abstract?CRETRY=1&SRETRY=0. Retrieved 2008-09-08. 
  154. ^ Ruben, J. A. and Jones, T. D. (2000). "Selective Factors Associated with the Origin of Fur and Feathers". American Zoologist 40 (4): 585–596. doi:10.1093/icb/40.4.585. http://icb.oxfordjournals.org/cgi/content/full/40/4/585. 
  155. ^ Luo, Z-X., Crompton, A. W. and Sun, A-L. (May 2001). "A New Mammaliaform from the Early Jurassic and Evolution of Mammalian Characteristics". Science 292 (5521): 1535–1540. doi:10.1126/science.1058476. PMID 11375489. http://www.sciencemag.org/cgi/content/full/292/5521/1535. Retrieved 2008-09-08. 
  156. ^ Cifelli, R.L. (November 2001). "Early mammalian radiations". Journal of Paleontology 75: 1214. doi:10.1666/0022-3360(2001)075<1214:EMR>2.0.CO;2. http://findarticles.com/p/articles/mi_qa3790/is_200111/ai_n8958762/pg_6. 
  157. ^ Flynn, J. J., Parrish, J. M. Rakotosamimanana, B., Simpson, W. F. and Wyss, A.R. (September 1999). "A Middle Jurassic mammal from Madagascar". Nature 401: 57–60. doi:10.1038/43420. http://www.nature.com/nature/journal/v401/n6748/abs/401057a0.html. Retrieved 2008-09-08. 
  158. ^ MacLeod, N., Rawson, P. F., Forey, P. L., Banner. F. T., Boudagher-Fadel, M. K., Bown, P. R., Burnett, J. A., Chambers, P., Culver, S., Evans, S. E., Jeffery, C., Kaminski, M. A., Lord, A. R., Milner, A. C., Milner, A. R., Morris, N., Owen, E., Rosen, B. R., ,Smith, A. B., Taylor, P. D., Urquhart, E. and Young, J. R. (1997). "The Cretaceous–Tertiary biotic transition". Journal of the Geological Society 154 (2): 265–292. doi:10.1144/gsjgs.154.2.0265. http://findarticles.com/p/articles/mi_qa3721/is_199703/ai_n8738406/print. 
  159. ^ Alroy, J. (March 1999). "The fossil record of North American mammals: evidence for a Paleocene evolutionary radiation". Systematic biology 48 (1): 107–18. doi:10.1080/106351599260472. PMID 12078635. 
  160. ^ Archibald, J. D. and Deutschman, D. H. (June 2001). "Quantitative Analysis of the Timing of the Origin and Diversification of Extant Placental Orders". Journal of Mammalian Evolution 8 (2): 107–124. doi:10.1023/A:1011317930838. http://www.ingentaconnect.com/content/klu/jomm/2001/00000008/00000002/00342277. Retrieved 2008-09-24. 
  161. ^ Simmons, N. B., Seymour, K. L., Habersetzer, J. and Gunnell, G. F. (February 2008). "Primitive Early Eocene bat from Wyoming and the evolution of flight and echolocation". Nature 451: 818–821. doi:10.1038/nature06549. 
  162. ^ Thewissen, J. G. M., Madar, S. I. and Hussain, S. T. (1996). "Ambulocetus natans, an Eocene cetacean (Mammalia) from Pakistan". Courier Forschungsinstitut Senckenberg 191: 1–86. ISBN 978-3-510-61084-6. 
  163. ^ a b c d Crane, P. R., Friis, E. M. and Pedersen, K. R. (2000), "The Origin and Early Diversification of Angiosperms", in Gee, H., Shaking the Tree: Readings from Nature in the History of Life, University of Chicago Press, pp. 233–250, ISBN 0226284964, http://books.google.co.uk/books?hl=en&lr=&id=ZJe_Dmdbm-QC&oi=fnd&pg=PA233&dq=evolution+flowering+plant+angiosperm&ots=abVpqx_cP8&sig=z1HvmrRLdJP9oPkN0bffbAyriEI#PPA233,M1, retrieved 2008-09-09 
  164. ^ a b c d Crepet, W. L. (November 2000). "Progress in understanding angiosperm history, success, and relationships: Darwin’s abominably "perplexing phenomenon"". Proceedings of the National Academy of Sciences 97 (24): 12939–12941. doi:10.1073/pnas.97.24.12939. PMID 11087846. http://www.pnas.org/content/97/24/12939.full.pdf+html. Retrieved 2008-09-09. 
  165. ^ a b Wilson, E. O. and Hölldobler, B. (September 2005). "Eusociality: Origin and consequences". Proceedings of the National Academy of Sciences 102 (38): 13367–13371. doi:10.1073/pnas.0505858102. PMID 16157878. http://www.pnas.org/content/102/38/13367.full.pdf+html. Retrieved 2008-09-07. 
  166. ^ Hughes, W. O. H., Oldroyd, B. P., Beekman, M. and Ratnieks, F. L. W. (2008-05-30). "Ancestral Monogamy Shows Kin Selection Is Key to the Evolution of Eusociality" (html). Science (American Association for the Advancement of Science) 320 (5880): 1213–1216. doi:10.1126/science.1156108. PMID 18511689. http://www.sciencemag.org/cgi/content/abstract/320/5880/1213. Retrieved 2008-08-04. 
  167. ^ Lovegrove, B. G. (January 1991). "The evolution of eusociality in molerats (Bathyergidae): a question of risks, numbers, and costs". Behavioral Ecology and Sociobiology 28 (1): 37–45. doi:10.1007/BF00172137. http://www.springerlink.com/content/k4n52v522l816125/. Retrieved 2008-09-07. 
  168. ^ Labandeira, C. and Eble, G. J. (2000), "The Fossil Record of Insect Diversity and Disparity", in Anderson, J., Thackeray, F., van Wyk, B., and de Wit, M. (PDF), Gondwana Alive: Biodiversity and the Evolving Biosphere, Witwatersrand University Press, http://www.santafe.edu/research/publications/workingpapers/00-08-044.pdf, retrieved 2008-09-07 
  169. ^ Brunet, M., Guy, F., Pilbeam, D., Mackaye, H. T. et al (July 2002). "A new hominid from the Upper Miocene of Chad, Central Africa". Nature 418: 145–151. doi:10.1038/nature00879. http://www.nature.com/nature/journal/v418/n6894/abs/nature00879.html. Retrieved 2008-09-09. 
  170. ^ de Heinzelin, J., Clark, J. D., White, T. et al (April 1999). "Environment and Behavior of 2.5-Million-Year-Old Bouri Hominids". Science 284 (5414): 625–629. doi:10.1126/science.284.5414.625. PMID 10213682. http://www.sciencemag.org/cgi/content/full/sci;284/5414/625. Retrieved 2008-09-09. 
  171. ^ De Miguel, C. and Henneberg, M. (2001). "Variation in hominid brain size: How much is due to method?". HOMO - Journal of Comparative Human Biology 52 (1): 3–58. doi:10.1078/0018-442X-00019. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B7GW4-4DPCHXC-2&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_version=1&_urlVersion=0&_userid=10&md5=aef79dbca1f189c885cfe9f36636b131. Retrieved 2008-09-09. 
  172. ^ Leakey, Richard (1994). The Origin of Humankind. Science Masters Series. New York, NY: Basic Books. pp. 87–89. ISBN 0465053130. 
  173. ^ Mellars, Paul (2006). "Why did modern human populations disperse from Africa ca. 60,000 years ago?". Proceedings of the National Academy of Sciences 103: 9381. doi:10.1073/pnas.0510792103. PMID 16772383. http://www.pnas.org/cgi/reprint/0510792103v1. 
  174. ^ Benton, M. J. (2004). "6. Reptiles Of The Triassic". Vertebrate Palaeontology (3rd ed.). Blackwell. ISBN 978-0-632-05637-8. http://www.blackwellpublishing.com/book.asp?ref=0632056371. 
  175. ^ Van Valkenburgh, B. (1999). "Major patterns in the history of xarnivorous mammals". Annual Review of Earth and Planetary Sciences 26: 463–493. doi:10.1146/annurev.earth.27.1.463. http://arjournals.annualreviews.org/doi/abs/10.1146/annurev.earth.27.1.463. 
  176. ^ a b MacLeod, N. (2001-01-06). "Extinction!". http://www.firstscience.com/home/articles/earth/extinction-page-2-1_1258.html. Retrieved 2008-09-11. 
  177. ^ Martin, R. E. (1995). "Cyclic and secular variation in microfossil biomineralization: clues to the biogeochemical evolution of Phanerozoic oceans". Global and Planetary Change 11 (1): 1. doi:10.1016/0921-8181(94)00011-2. 
  178. ^ Martin, R.E. (1996). "Secular increase in nutrient levels through the Phanerozoic: Implications for productivity, biomass, and diversity of the marine biosphere". PALAIOS 11: 209–219. doi:10.2307/3515230. 
  179. ^ a b Rohde, R. A. and Muller, R. A. (March 2005). "Cycles in fossil diversity" (PDF). Nature 434: 208–210. doi:10.1038/nature03339. http://muller.lbl.gov/papers/Rohde-Muller-Nature.pdf. Retrieved 2008-09-22. 
  180. ^ Field, C. B., Behrenfeld, M. J., Randerson, J. T. and Falkowski, P. (July 1998). "Primary Production of the Biosphere: Integrating Terrestrial and Oceanic Components". Science 281 (5374): 237–240. doi:10.1126/science.281.5374.237. http://www.sciencemag.org/cgi/content/full/sci;281/5374/237. Retrieved 2008-09-13. 
  181. ^ Grant, B. S., and Wiseman, L. L. (2002). "Recent History of Melanism in American Peppered Moths". Journal of Heredity 93 (2): 86–90. doi:10.1093/jhered/93.2.86. ISSN 1465-7333. PMID 12140267. http://jhered.oxfordjournals.org/cgi/content/abstract/93/2/86. Retrieved 2008-09-11. 
  182. ^ Levin, B. R., Perrot, V. and Walker, N. (March 1, 2000). "Compensatory Mutations, Antibiotic Resistance and the Population Genetics of Adaptive Evolution in Bacteria". Genetics 154 (3): 985–997. PMID 10757748. http://www.genetics.org/cgi/content/abstract/154/3/985. Retrieved 2008-09-11. 
  183. ^ Hawks, J., Wang, E. T., Cochran, G. M., Harpending, H. C. and Moyzis, R. K. (December 2007). "Recent acceleration of human adaptive evolution". Proceedings of the National Academy of Sciences 104 (52): 20753–20758. doi:10.1073/pnas.0707650104. PMID 18087044. http://www.pnas.org/content/104/52/20753.full. Retrieved 2008-09-11. 

Further reading

External links

General information

History of evolutionary thought


Advertisements






Got something to say? Make a comment.
Your name
Your email address
Message