Carboniferous Period 359.2–299 million years ago PreЄ Є O S D C P T J K Pg N
Mean atmospheric O2 content over period duration	ca. 32.5 Vol %[1] (163 % of modern level)
Mean atmospheric CO2 content over period duration	ca. 800 ppm[2] (3 times pre-industrial level)
Mean surface temperature over period duration	ca. 14 °C[3] (0 °C above modern level)
Sea level (above present day)	Falling from 120m to present day level throughout Mississippian, then rising steadily to about 80m at end of period[4]
Key events in the Carboniferous view • discuss • edit -360 — – -355 — – -350 — – -345 — – -340 — – -335 — – -330 — – -325 — – -320 — – -315 — – -310 — – -305 — – -300 — – -295 — Permian Devonian Tournaisian Visean Serpukhovian Bashkirian Moscovian Kasimovian Gzhelian           C a r b o n i f e r o u s M i s s i s s i p p i a n P e n n - i a n  Palæozoic An approximate timescale of key Carboniferous events. Axis scale: millions of years ago.

The Carboniferous is a geologic period and system that extends from the end of the Devonian Period, about 359.2 ± 2.5 Mya (million years ago), to the beginning of the Permian Period, about 299.0 ± 0.8 Mya (ICS, 2004^[5]). The name 'Carboniferous', which means "coal-bearing" and derives from the Latin words carbo (coal) and ferre (to carry), was coined by geologists, William Conybeare and William Phillips in 1822. Based on a study of the British rock succession, it was the first of the modern 'system' names to be employed, and reflects the fact that many coal beds were formed globally during this time.^[6] The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian.^[7]

Terrestrial life was well established by the Carboniferous period. Amphibians were the dominant land vertebrates, of which one branch would eventually evolve into reptiles, the first fully terrestrial vertebrates. Arthropods were also very common, and many (such as Meganeura), were much larger than those of today. Vast swathes of forest covered the land, which would eventually be laid down and become the coal beds characteristic of the Carboniferous system. A minor marine and terrestrial extinction event occurred in the middle of the period, caused by a change in climate.^[8] The latter half of the period experienced glaciations, low sea level, and mountain building.

Subdivisions[link]

In the USA the Carboniferous is usually broken into Mississippian (earlier) and Pennsylvanian (later) Periods. The Mississippian is about twice as long as the Pennsylvanian, but due to the large thickness of coal bearing deposits with Pennsylvanian ages in Europe and North America, the two subperiods were long thought to have been more or less equal.^[9] The faunal stages from youngest to oldest, together with some of their subdivisions, are:

Late Pennsylvanian: Gzhelian (most recent)

• Noginskian / Virgilian (part)

Late Pennsylvanian: Kasimovian

• Klazminskian
• Dorogomilovksian / Virgilian (part)
• Chamovnicheskian / Cantabrian / Missourian
• Krevyakinskian / Cantabrian / Missourian

Middle Pennsylvanian: Moscovian

• Myachkovskian / Bolsovian / Desmoinesian
• Podolskian / Desmoinesian
• Kashirskian / Atokan
• Vereiskian / Bolsovian / Atokan

Early Pennsylvanian: Bashkirian / Morrowan

• Melekesskian / Duckmantian
• Cheremshanskian / Langsettian
• Yeadonian
• Marsdenian
• Kinderscoutian

Late Mississippian: Serpukhovian

• Alportian
• Chokierian / Chesterian / Elvirian
• Arnsbergian / Elvirian
• Pendleian

Middle Mississippian: Visean

• Brigantian / St Genevieve / Gasperian / Chesterian
• Asbian / Meramecian
• Holkerian / Salem
• Arundian / Warsaw / Meramecian
• Chadian / Keokuk / Osagean (part) / Osage (part)

Early Mississippian: Tournaisian (oldest)

• Ivorian / (part) / Osage (part)
• Hastarian / Kinderhookian / Chouteau

Paleogeography[link]

A global drop in sea level at the end of the Devonian reversed early in the Carboniferous; this created the widespread epicontinental seas and carbonate deposition of the Mississippian.^[10] There was also a drop in south polar temperatures; southern Gondwanaland was glaciated throughout the period, though it is uncertain if the ice sheets were a holdover from the Devonian or not.^[10] These conditions apparently had little effect in the deep tropics, where lush coal swamps flourished within 30 degrees of the northernmost glaciers.^[10]

A mid-Carboniferous drop in sea level precipitated a major marine extinction, one that hit crinoids and ammonites especially hard.^[10] This sea level drop and the associated unconformity in North America separate the Mississippian subperiod from the Pennsylvanian subperiod.^[10] This happened about 318 million years ago, at the onset of the Permo-Carboniferous Glaciation.^{[citation needed]}

The Carboniferous was a time of active mountain-building, as the supercontinent Pangaea came together. The southern continents remained tied together in the supercontinent Gondwana, which collided with North America–Europe (Laurussia) along the present line of eastern North America. This continental collision resulted in the Hercynian orogeny in Europe, and the Alleghenian orogeny in North America; it also extended the newly-uplifted Appalachians southwestward as the Ouachita Mountains.^[10] In the same time frame, much of present eastern Eurasian plate welded itself to Europe along the line of the Ural mountains. Most of the Mesozoic supercontinent of Pangea was now assembled, although North China (which would collide in the Latest Carboniferous), and South China continents were still separated from Laurasia. The Late Carboniferous Pangaea was shaped like an "O."

There were two major oceans in the Carboniferous—Panthalassa and Paleo-Tethys, which was inside the "O" in the Carboniferous Pangaea. Other minor oceans were shrinking and eventually closed - Rheic Ocean (closed by the assembly of South and North America), the small, shallow Ural Ocean (which was closed by the collision of Baltica and Siberia continents, creating the Ural Mountains) and Proto-Tethys Ocean (closed by North China collision with Siberia/Kazakhstania).

Climate[link]

The early part of the Carboniferous was mostly warm; in the later part of the Carboniferous, the climate cooled. Glaciations in Gondwana, triggered by Gondwana's southward movement, continued into the Permian and because of the lack of clear markers and breaks, the deposits of this glacial period are often referred to as Permo-Carboniferous in age.

The cooling and drying of the climate led to the Carboniferous Rainforest Collapse (CRC). Tropical rainforests fragmented and then were eventually devastated by climate change.^[8]

Rocks and coal[link]

Lower Carboniferous marble in Big Cottonwood Canyon, Wasatch Mountains, Utah.

Carboniferous rocks in Europe and eastern North America largely consist of a repeated sequence of limestone, sandstone, shale and coal beds.^[11] In North America, the early Carboniferous is largely marine limestone, which accounts for the division of the Carboniferous into two periods in North American schemes. The Carboniferous coal beds provided much of the fuel for power generation during the Industrial Revolution and are still of great economic importance.

The large coal deposits of the Carboniferous primarily owe their existence to two factors. The first of these is the appearance of bark-bearing trees (and in particular the evolution of the bark fiber lignin). The second is the lower sea levels that occurred during the Carboniferous as compared to the Devonian period. This allowed for the development of extensive lowland swamps and forests in North America and Europe. Some^[who?] hypothesize that large quantities of wood were buried during this period because animals and decomposing bacteria had not yet evolved that could effectively digest the new lignin. Those early plants made extensive use of lignin. They had bark to wood ratios of 8 to 1, and even as high as 20 to 1. This compares to modern values less than 1 to 4. This bark, which must have been used as support as well as protection, probably had 38% to 58% lignin. Lignin is insoluble, too large to pass through cell walls, too heterogeneous for specific enzymes, and toxic, so that few organisms other than Basidiomycetes fungi can degrade it. It can not be oxidized in an atmosphere of less than 5% oxygen. It can linger in soil for thousands of years and inhibits decay of other substances.^[12] Probably the reason for its high percentages is protection from insect herbivory in a world containing very effective insect herbivores, but nothing remotely as effective as modern insectivores and probably many fewer poisons than currently. In any case coal measures could easily have made thick deposits on well drained soils as well as swamps. The extensive burial of biologically-produced carbon led to a buildup of surplus oxygen in the atmosphere; estimates place the peak oxygen content as high as 35%, compared to 21% today.[1] This oxygen level probably increased wildfire activity, as well as resulted in insect and amphibian gigantism--creatures whose size is constrained by respiratory systems that are limited in their ability to diffuse oxygen.

In eastern North America, marine beds are more common in the older part of the period than the later part and are almost entirely absent by the late Carboniferous. More diverse geology existed elsewhere, of course. Marine life is especially rich in crinoids and other echinoderms. Brachiopods were abundant. Trilobites became quite uncommon. On land, large and diverse plant populations existed. Land vertebrates included large amphibians.

Life[link]

Plants[link]

Etching depicting some of the most significant plants of the Carboniferous.

Early Carboniferous land plants, some of which were preserved in coal balls, were very similar to those of the preceding Late Devonian, but new groups also appeared at this time.

The main Early Carboniferous plants were the Equisetales (horse-tails), Sphenophyllales (vine-like plants), Lycopodiales (club mosses), Lepidodendrales (scale trees), Filicales (ferns), Medullosales (informally included in the "seed ferns", an artificial assemblage of a number of early gymnosperm groups) and the Cordaitales. These continued to dominate throughout the period, but during late Carboniferous, several other groups, Cycadophyta (cycads), the Callistophytales (another group of "seed ferns"), and the Voltziales (related to and sometimes included under the conifers), appeared.

The Carboniferous lycophytes of the order Lepidodendrales, which are cousins (but not ancestors) of the tiny club-moss of today, were huge trees with trunks 30 meters high and up to 1.5 meters in diameter. These included Lepidodendron (with its fruit cone called Lepidostrobus), Halonia, Lepidophloios and Sigillaria. The roots of several of these forms are known as Stigmaria. The Cladoxylopsids were large trees, that were ancestors of ferns, first arising in the Carboniferous.^[13]

The fronds of some Carboniferous ferns are almost identical with those of living species. Probably many species were epiphytic. Fossil ferns and "seed ferns" include Pecopteris, Cyclopteris, Neuropteris, Alethopteris, and Sphenopteris; Megaphyton and Caulopteris were tree ferns.

The Equisetales included the common giant form Calamites, with a trunk diameter of 30 to 60 cm (24 in) and a height of up to 20 m (66 ft). Sphenophyllum was a slender climbing plant with whorls of leaves, which was probably related both to the calamites and the lycopods.

Cordaites, a tall plant (6 to over 30 meters) with strap-like leaves, was related to the cycads and conifers; the catkin-like inflorescence, which bore yew-like berries, is called Cardiocarpus. These plants were thought to live in swamps and mangroves. True coniferous trees (Walchia, of the order Voltziales) appear later in the Carboniferous, and preferred higher drier ground.

Marine invertebrates[link]

In the oceans the most important marine invertebrate groups are the Foraminifera, corals, Bryozoa, Ostracoda, brachiopods, ammonoids, hederelloids, microconchids and echinoderms (especially crinoids). For the first time foraminifera take a prominent part in the marine faunas. The large spindle-shaped genus Fusulina and its relatives were abundant in what is now Russia, China, Japan, North America; other important genera include Valvulina, Endothyra, Archaediscus, and Saccammina (the latter common in Britain and Belgium). Some Carboniferous genera are still extant.

The microscopic shells of radiolarians are found in cherts of this age in the Culm of Devon and Cornwall, and in Russia, Germany and elsewhere. Sponges are known from spicules and anchor ropes, and include various forms such as the Calcispongea Cotyliscus and Girtycoelia, the demosponge Chaetetes, and the genus of unusual colonial glass sponges Titusvillia.

Both reef-building and solitary corals diversify and flourish; these include both rugose (for example, Canina, Corwenia, Neozaphrentis), heterocorals, and tabulate (for example, Chladochonus, Michelinia) forms. Conularids were well represented by Conularia

Bryozoa are abundant in some regions; the fenestellids including Fenestella, Polypora, and Archimedes, so named because it is in the shape of an Archimedean screw. Brachiopods are also abundant; they include productids, some of which (for example, Gigantoproductus) reached very large (for brachiopods) size and had very thick shells, while others like Chonetes were more conservative in form. Athyridids, spiriferids, rhynchonellids, and terebratulids are also very common. Inarticulate forms include Discina and Crania. Some species and genera had a very wide distribution with only minor variations.

Annelids such as Serpulites are common fossils in some horizons. Among the mollusca, the bivalves continue to increase in numbers and importance. Typical genera include Aviculopecten, Posidonomya, Nucula, Carbonicola, Edmondia, and Modiola Gastropods are also numerous, including the genera Murchisonia, Euomphalus, Naticopsis. Nautiloid cephalopods are represented by tightly coiled nautilids, with straight-shelled and curved-shelled forms becoming increasingly rare. Goniatite ammonoids are common.

Trilobites are rarer than in previous periods, on a steady trend towards extinction, represented only by the proetid group. Ostracoda, a class of crustaceans, were abundant as representatives of the meiobenthos; genera included Amphissites, Bairdia, Beyrichiopsis, Cavellina, Coryellina, Cribroconcha, Hollinella, Kirkbya, Knoxiella, and Libumella.

Amongst the echinoderms, the crinoids were the most numerous. Dense submarine thickets of long-stemmed crinoids appear to have flourished in shallow seas, and their remains were consolidated into thick beds of rock. Prominent genera include Cyathocrinus, Woodocrinus, and Actinocrinus. Echinoids such as Archaeocidaris and Palaeechinus were also present. The blastoids, which included the Pentreinitidae and Codasteridae and superficially resembled crinoids in the possession of long stalks attached to the seabed, attain their maximum development at this time.

Freshwater and lagoonal invertebrates[link]

Freshwater Carboniferous invertebrates include various bivalve molluscs that lived in brackish or fresh water, such as Anthraconaia, Naiadites, and Carbonicola; diverse crustaceans such as Candona, Carbonita, Darwinula, Estheria, Acanthocaris, Dithyrocaris, and Anthrapalaemon.

The Eurypterids were also diverse, and are represented by such genera as Eurypterus, Glyptoscorpius, Anthraconectes, Megarachne (originally misinterpreted as a giant spider) and the specialised very large Hibbertopterus. Many of these were amphibious.

Frequently a temporary return of marine conditions resulted in marine or brackish water genera such as Lingula, Orbiculoidea, and Productus being found in the thin beds known as marine bands.

Terrestrial invertebrates[link]

The late Carboniferous giant dragonfly-like insect Meganeura grew to wingspans of 75 cm (30 in).

The gigantic Pulmonoscorpius from the early Carboniferous reached a length of up to 70 cm (28 in).

Fossil remains of air-breathing insects, myriapods and arachnids are known from the late Carboniferous, but so far not from the early Carboniferous. Their diversity when they do appear, however, shows that these arthropods were both well developed and numerous. Their large size can be attributed to the moistness of the environment (mostly swampy fern forests) and the fact that the oxygen concentration in the Earth's atmosphere in the Carboniferous was much higher than today ^[14] (35% then compared with 21% today). This required less effort for respiration and allowed arthropods to grow larger with the up to 2.6 metres long millipede-like Arthropleura being the largest known land invertebrate of all time. Among the insect groups are the huge predatory Protodonata (griffinflies), among which was Meganeura, a giant dragonfly-like insect and with a wingspan of ca. 75 cm (30 in) — the largest flying insect ever to roam the planet. Further groups are the Syntonopterodea (relatives of present-day mayflies), the abundant and often large sap-sucking Palaeodictyopteroidea, the diverse herbivorous Protorthoptera, and numerous basal Dictyoptera (ancestors of cockroaches). Many insects have been obtained from the coalfields of Saarbrücken and Commentry, and from the hollow trunks of fossil trees in Nova Scotia. Some British coalfields have yielded good specimens: Archaeoptitus, from the Derbyshire coalfield, had a spread of wing extending to more than 35 cm; some specimens (Brodia) still exhibit traces of brilliant wing colors. In the Nova Scotian tree trunks land snails (Archaeozonites, Dendropupa) have been found.

Fish[link]

Akmonistion zangerli of the shark order Symmoriida roamed the oceans of the early Carboniferous.

Many fish inhabited the Carboniferous seas; predominantly Elasmobranchs (sharks and their relatives). These included some, like Psammodus, with crushing pavement-like teeth adapted for grinding the shells of brachiopods, crustaceans, and other marine organisms. Other sharks had piercing teeth, such as the Symmoriida; some, the petalodonts, had peculiar cycloid cutting teeth. Most of the sharks were marine, but the Xenacanthida invaded fresh waters of the coal swamps. Among the bony fish, the Palaeonisciformes found in coastal waters also appear to have migrated to rivers. Sarcopterygian fish were also prominent, and one group, the Rhizodonts, reached very large size.

Most species of Carboniferous marine fish have been described largely from teeth, fin spines and dermal ossicles, with smaller freshwater fish preserved whole.

Freshwater fish were abundant, and include the genera Ctenodus, Uronemus, Acanthodes, Cheirodus, and Gyracanthus.

Sharks (especially the Stethacanthids) underwent a major evolutionary radiation during the Carboniferous.^[15] It is believed that this evolutionary radiation occurred because the decline of the placoderms at the end of the Devonian period caused many environmental niches to become unoccupied and allowed new organisms to evolve and fill these niches.^[15] As a result of the evolutionary radiation carboniferous sharks assumed a wide variety of bizarre shapes including Stethacanthus which possessed a flat brush-like dorsal fin with a patch of denticles on its top.^[15] Stethacanthus' unusual fin may have been used in mating rituals.^[15]

Tetrapods[link]

Carboniferous amphibians were diverse and common by the middle of the period, more so than they are today; some were as long as 6 meters, and those fully terrestrial as adults had scaly skin.^[16] They included a number of basal tetrapod groups classified in early books under the Labyrinthodontia. These had long bodies, a head covered with bony plates and generally weak or undeveloped limbs. The largest were over 2 meters long. They were accompanied by an assemblage of smaller amphibians included under the Lepospondyli, often only about 15 cm (6 in) long. Some Carboniferous amphibians were aquatic and lived in rivers (Loxomma, Eogyrinus, Proterogyrinus); others may have been semi-aquatic (Ophiderpeton, Amphibamus, Hyloplesion) or terrestrial (Dendrerpeton, Tuditanus, Anthracosaurus).

The Carboniferous Rainforest Collapse slowed the evolution of amphibians who could not survive as well in the cooler, drier conditions. Reptiles, however prospered due to specific key adaptations.^[8] One of the greatest evolutionary innovations of the Carboniferous was the amniote egg, which allowed for the further exploitation of the land by certain tetrapods. These included the earliest sauropsid reptiles (Hylonomus), and the earliest known synapsid (Archaeothyris). These small lizard-like animals quickly gave rise to many descendants. The amniote egg allowed these ancestors of all later birds, mammals, and reptiles to reproduce on land by preventing the desiccation, or drying-out, of the embryo inside.

Reptiles underwent a major evolutionary radiation, in response to the drier climate that proceeded the rainforest collapse.^[8][17] By the end of the Carboniferous period, amniotes had already diversified into a number of groups, including protorothyridids, captorhinids, aeroscelids, and several families of pelycosaurs.

Fungi[link]

Because plants and animals were growing in size and abundance in this time (for example, Lepidodendron), land fungi diversified further. Marine fungi still occupied the oceans. All modern classes of fungi were present in the Late Carboniferous (Pennsylvanian Epoch).^[18]

This section requires expansion.

Extinction events[link]

Romer's gap[link]

The first 15 million years of the Carboniferous has very limited terrestrial fossils. This gap in the fossil record, is called Romer's gap after the American palaentologist Alfred Romer. While it has long been debated whether the gap is a result of fossilisation or relates to an actual event, recent work indicates the gap period saw a drop in atmospheric oxygen levels, indicating some sort of ecological collapse.^[19] The gap saw the demise of the Devonian fish-like ichthyostegalian labyrinthodonts, and the rise of the more advanced temnospondyl and reptiliomorphan amphibians that so typify the Carboniferous terrestrial vertebrate fauna.

Middle Carboniferous rainforest collapse[link]

In the middle Carboniferous, an extinction event occurred. On land this event is referred to as the Carboniferous Rainforest Collapse (CRC).^[8] Vast tropical rainforests collapsed suddenly as the climate changed from hot and humid to cool and arid. This was likely caused by intense glaciation and a drop in sea levels.^[20]

The new climatic conditions were not favorable to the growth of rainforest and the animals within them. Rainforests shrank into isolated islands, surrounded by seasonally dry habitats. Towering lycopsid forests with a heterogenus mixture of vegetation were replaced by much less diverse tree-fern dominated flora.

Amphibians, the dominant vertebrates at the time, fared poorly through this event with large losses in biodiversity; reptiles continued to diversify due to key adaptations that let them survive in the drier habitat, specifically the hard-shelled egg and scales both of which retain water better than their amphibian counterparts.^[8]

See also[link]

• Carboniferous tetrapods
• Important Carboniferous Lagerstätten
  • East Kirkton Quarry; c. 350 mya; Bathgate, Scotland
  • Hamilton Quarry; 320 mya; Kansas, US
  • Mazon Creek; 300 mya; Illinois, US
• List of fossil sites (with link directory)

References[link]

Further reading[link]

 This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press. 

External links[link]

Wikimedia Commons has media related to: Carboniferous

• "Geologic Time Scale 2004". International Commission on Stratigraphy (ICS). http://www.stratigraphy.org/bak/geowhen/index.html. Retrieved November 8, 2009. 
• Examples of Carboniferous Fossils
• 60+ images of Carboniferous Foraminifera

Mike Patton
Background information
Birth name	Michael Allan Patton
Born	(1968-01-27) January 27, 1968 (age 44) Eureka, California, U.S.
Genres	Various
Occupations	Musician, songwriter, actor, producer
Instruments	Vocals, various electronic instrumentation/programming, sampler, drums, percussions, bass, guitar, keyboards
Years active	1985–present
Labels	Ipecac, Tzadik, Warner Bros. Records, Slash
Associated acts	Faith No More, Mr. Bungle, Fantômas, Tomahawk, Peeping Tom, Lovage, John Zorn, Kaada/Patton, Dillinger Escape Plan, Hemophiliac, Maldoror, General Patton vs. The X-Ecutioners, Rahzel, Zu,

Michael Allan "Mike" Patton (born January 27, 1968) is an American singer-songwriter, multi-instrumentalist, producer, and actor, best known as the lead singer of the experimental rock/alternative metal band Faith No More. He was also the founder and lead singer of Mr. Bungle, and has played with Tomahawk, Fantômas, Lovage, The Dillinger Escape Plan, and Peeping Tom.

Known for his eclectic influences and experimental projects, Patton has earned critical praise for his diverse vocalization. He has many producer or co-producer credits with artists such as John Zorn, Sepultura, Melvins, Melt-Banana, and Kool Keith. He co-founded Ipecac Recordings with Greg Werckman in 1999, and has run the label since.

Biography[link]

Early years[link]

Patton was born and raised in Eureka, California, where he formed Mr. Bungle, with Trey Spruance and Trevor Dunn, in 1984. During the late '80s Mr Bungle recorded the cassette-only recordings, The Raging Wrath of the Easter Bunny, Goddammit I Love America, Bowel of Chiley and OU818, featuring tracks that would later be included on their first Warner Brothers album.

Joining Faith No More[link]

Patton joined Faith No More in January 1989 replacing Chuck Mosley, who then played with Cement.

Faith No More's The Real Thing was released later that year. The album reached the top ten on the US charts, thanks largely to MTV's heavy rotation of the "Epic" music video, (which featured Patton in a Mr. Bungle T-shirt^[1]).

In the United States, Faith No More released three more studio albums; (Angel Dust, King for a Day... Fool for a Lifetime, and Album of the Year) Faith No More officially disbanded in 1998.^{[citation needed]}

When interviewed about his lyrical content with Faith No More, Patton responded, "I think that too many people think too much about my lyrics. I am more a person who works more with the sound of a word than with its meaning. Often I just choose the words because of the rhythm, not because of the meaning".^[2]

Mr. Bungle and beyond[link]

During his time in Faith No More, Patton continued to work with Mr. Bungle. His success in mainstream rock and metal ultimately helped secure Mr. Bungle a record deal with Warner Bros.^[3] The band released a self-titled album (produced by John Zorn) in 1991, and the experimental Disco Volante^[4] in 1995. Their final album, California, was released in 1999.

Patton's other projects included two solo albums on the Composer Series of John Zorn's Tzadik label, (Adult Themes for Voice in 1996 and Pranzo Oltranzista in 1997). He is a member of Hemophiliac, in which he performs vocal effects along with John Zorn on saxophone and Ikue Mori on laptop electronics. This group is billed as "improvisational music from the outer reaches of madness".^{[citation needed]} He has also guested on Painkiller and Naked City recordings. He has also on other Tzadik releases with Zorn and others.

In 1998, Patton formed the avant-garde metal supergroup Fantômas with Buzz Osbourne (of The Melvins), Trevor Dunn (of Mr. Bungle), and Dave Lombardo of Slayer. They have released four studio albums. The band is still together as of July 2011.

There have been several projects over the years featuring Patton that have not been officially released, although some live bootlegs do circulate. These projects include House of Discipline (with Bob Ostertag and Otomo Yoshihide), Moonraker (with Agata Ichirou of Melt-Banana, Buckethead and DJ Eddie Def), Christian Fennesz and Mike Patton, and Patton & Rahzel. Patton contributed vocals to the Team Sleep song Kool-Aid Party, but the song did not make it onto the final album.^{[citation needed]}

Patton performing with Fantômas at Quart Festival, Norway on July 9, 2005.

In 2004, Patton worked with Björk and the beat boxer Rahzel on her album, Medúlla.^[5]

In 2005, Patton signed on to compose the soundtrack for the independent movie Pinion, marking his debut scoring an American feature-length film. However, this had been held up in production and may be on the shelf permanently.^[6] His other film work includes portraying two major characters in the Steve Balderson film Firecracker. He has also expressed his desire to compose for film director David Lynch.

In February 2006, Mike Patton performed an operatic piece, composed by Eyvind Kang, at Teatro di Modena in Italy. Patton sang alongside vocalist Jessika Kinney, and was accompanied by the Modern Brass Ensemble, Bologna Chamber Choir, and Alberto Capelli and Walter Zanetti on electric and acoustic guitars. Patton remarked that it was extremely challenging to project the voice without a microphone.^[7]

Patton's Peeping Tom album was released on May 30, 2006 on his own Ipecac label. The set was pieced together by swapping song files through the mail with collaborators like Norah Jones, Kool Keith and Massive Attack, Odd Nosdam, Jel, Doseone, Bebel Gilberto, Kid Koala, and Dub Trio.^{[citation needed]}

"I don't listen to the radio, but if I did, this is what I'd want it to sound like", Patton said of the project. "This is my version of pop music. In a way, this is an exercise for me: taking all these things I've learned over the years and putting them into a pop format."

—Mike Patton

In May 2007 he performed with an orchestra a few concerts in Italy, by the name of Mondo Cane, singing Italian oldies from the 50s and the 60s.

Mike also provided the voices of the monsters in the 2007 film I Am Legend starring Will Smith.

He is regarded as very hard-working. Faith No More keyboardist Roddy Bottum remarked about Patton "caffeine is the only drug he does", in reference to the Faith No More song "Caffeine" from the album Angel Dust, which Patton wrote while in the middle of a sleep-deprivation experiment.^{[citation needed]} He also worked on the Derrick Scocchera short film "A Perfect Place" for the score/soundtrack, which is longer than the film itself.^{[citation needed]}

In December 2008 along with Melvins, Patton co-curated an edition of the All Tomorrow's Parties Nightmare Before Christmas festival.^[8] Patton chose half of the lineup and performed the album The Director's Cut in its entirety with Fantômas. Patton also appeared as Rikki Kixx in the Adult Swim show Metalocalypse in a special 2 part episode on August 24.^[9]

In 2009 Patton created the soundtrack to the movie Crank: High Voltage. He also performed vocals on the track "Lost Weekend" by The Qemists.

On May 4, 2010 Mondo Cane, where Patton worked live with a 30-piece orchestra, was released by Ipecac Recordings. The album was co-produced and arranged by Daniele Luppi.^[10]

"Recorded at a series of European performances including an outdoor concert in a Northern Italian piazza, the CD features traditional Italian pop songs as well as a rendition of Ennio Morricone's 'Deep Down'."^[11]

Video games[link]

Patton is known to be an avid video game player.^[12] In 2007, he provided the voice of the eponymous force in the video game The Darkness,^[13] working alongside Kirk Acevedo, Lauren Ambrose and Dwight Schultz. Patton reprised the role in The Darkness II in 2012.^[14]

He also had a minor role in Valve Corporation's 2007 release Portal as the voice of the Anger Sphere in the final confrontation with the insane supercomputer, GLaDOS. He has another role in the Valve title Left 4 Dead, voicing the majority of the infected zombies.^[15] He also voiced Nathan "Rad" Spencer, the main character in Capcom's 2009 video game Bionic Commando, a sequel of their classic NES title.

Faith No More reunion[link]

In February 2009, Faith No More announced that they were reforming for a tour and possibly new material, first as a footnote on a blurb for Patton's score for Crank: High Voltage and later as an official announcement on fnm.com.^[16] Their first gig on the road again was at the Brixton O2 Academy in London, where 1990's Live at the Brixton Academy was recorded, on June 10, 2009. They have played as one of three headliners at The Download Festival 2009, in Castle Donington, which was Faith No More's first time at the festival. At the festival they played "Chinese Arithmetic" while Patton humorously sang the lyrics to "Poker Face" using a beat-box effect embellishing Gaga's vocal style. Bassist Billy Gould has also stated that an American tour is "not out of the question". In June 2009 Faith No More announced that they will be headlining the NME stage at Reading & Leeds festival.^[17] On July 4, Faith No More performed a concert together at the Open'er festival in Kosakowo Airport near Gdynia, Poland.

Faith No More also played the large Roskilde Festival near the city of Roskilde, Denmark.^[18] Faith No More also performed in Portugal in Optimus Alive'10, where Mike Patton sang one song, "Evidence", completely in Portuguese. They had already played the same song completely in Italian on June 14, 2009, at the Rock in Idro Festival in Milan. 12 August 2009 was the date for FNM's first Turkish live appreance in Istanbul. On August 14, Faith no more played at the Spirit of Burgas Festival in Burgas, Bulgaria. Faith No More headlined the Australian Soundwave Festival in 2010. On the 27th of August 2009, Faith No More played in the Olympia Theatre in Dublin, Ireland and were supported by local band Adebisi Shank.

On September 1, 2009 Faith No More played at Israel Trade Fairs & Convention Center in Tel Aviv, Israel, supported by Monotonix and Dinosaur Jr. August 2009 Faith No More headlined the Radio 1/NME Stage at both Leeds & Reading Festival where they played the theme tune to popular UK Soap Eastenders as part of their setlist. On December 5, 2010, they played alongside Primus in Santiago de Chile,^[19] which was the day after their performance at the Teleton Chile.^[20] In 2011 they also performed at the Chilean Rock Concert Maquinaria^[21] on November 12 and 13, as well as at the SWU Festival on November 15.^[22]

Faith No More were to top the bill on Sunday July 8th 2012 of the Sonisphere Festival UK festival at the iconic Knebworth House venue, but On March 29, the festival was cancelled. ^[23]

Reaction to fame[link]

Patton (left) performing with Bill Laswell (bass) in a Jazz band.

Patton has garnered critical praise and has been made a heavy metal icon; however, Patton's reaction to this fame has been unconventional. He has acted irreverently towards the music industry, and expressed his distaste for the infamous lifestyles of rock stars. In a 1995 interview with the San Francisco Chronicle, he stated: "It's hard to see as much as you'd like to with our schedule on the road, but it's harder to do coke and fuck whores every night. Now that's a full time job."^[24] His attitude towards popular music is also evident in his songwriting, as Allmusic critic Cammila Albertson writes: "When Patton sings 'Roll it up and smoke it again/Bottoms up and drink it again/ Fix it up and shoot it again/ I can't believe I did it again,' (Mojo by Peeping Tom) he is keenly aware of the way it sounds for such an avant-garde composer as himself to recite perfect rock & roll cliches. His lyrics mock the self-important coolness of the music industry and self parody his own place in it."^[25] His contempt for the over-the-top antics of figures in popular music is often cited as the main reason that Patton has always been so guarded about his privacy and personal life.^[24] Mike Patton has stated that he enjoyed his time in Faith No More:

"They were good years. It was a decade of my life. It was lots of ups and lots of downs, but ultimately that's where I learned my chops and learned the craft and the business."

— Mike Patton, Artisan News Service

Personal life[link]

Patton married Italian artist Titi Zuccatosta in 1994. They separated in 2001. During an appearance on the radio show, Loveline (Listen), Patton said that it was a case of two people wanting different things and hinted that his excessive work habits may have been a factor. "It's very hard. It's a daily struggle", he commented in regards to the rigors of juggling a busy music career and a marriage. "It had to happen... Even though we knew each other really well when we got married, it doesn't get easier." He later added, "We're trying this. See what happens. There's still hope." Patton used to own a home in Bologna, Italy (which he sold around the time of the break-up), and speaks fluent Italian.^[26] He was interviewed by music journalist Lucas H. Gordon and the answers were given by Patton in Italian.^{[citation needed]}

Patton's right hand is permanently numb from an on-stage incident during his third concert with Faith No More, where he accidentally cut himself on a broken bottle and severed the tendons and nerves in his hand. He can use his hand, but he has no feeling in it (despite his doctor telling him the opposite would happen).^[27]

Style and influences[link]

Patton's vocals touch on crooning, falsetto, screaming, opera, death growls, rapping, mouth music, beatboxing, and scatting, among other techniques. Critic Greg Prato of Allmusic writes, "Patton could very well be one of the most versatile and talented singers in rock music";^[28] colleague Blake Butler called him "a complete and utter musical visionary and a mind-blowing and standard-warping genius."^[29]

Discography[link]

Selected filmography[link]

• 1990 - Live at the Brixton Academy, London: You Fat Bastards by Faith No More (VHS)
• 1993 - Video Macumba - Short film compiled by Mike Patton containing abstract and extreme footage
• 1998 - Who Cares a Lot: Greatest Videos by Faith No More (VHS)
• 2002 - A Bookshelf on Top of the Sky: 12 Stories About John Zorn
• 2005 - Firecracker - Frank/David
• 2007 - Kaada/Patton Live - Live performance DVD
• 2007 - I Am Legend - Creature Vocals (voice) (credited as Michael A. Patton)[2]
• 2008 - A Perfect Place - Short film soundtrack by Patton (Released with film as CD/DVD special edition)
• 2008 - Live From London 2006 - Live DVD release of a performance by the Fantomas Melvins Big Band in London on May 1, 2006
• 2008 - Metalocalypse - Patton voices the character of reformed rocker Rikki Kixx on episodes "Snakes N Barrels II" part one and part two. This special 2 part, half hour presentation aired on The Cartoon Network August 24, 2008.
• 2009 - Crank: High Voltage - Film Score
• 2010 - Bunraku - Narrator

Video games[link]

• 2007 - The Darkness - Voice of The Darkness (Starbreeze Studios)
• 2007 - Portal - Voice of the Anger Sphere (Valve Software)
• 2008 - Left 4 Dead - Infected voices (Valve Software)
• 2009 - Bionic Commando - Voice of Nathan Spencer - the Bionic Commando (Capcom)
• 2009 - Left 4 Dead 2 - Infected voices (Valve Software)
• 2012 - The Darkness 2 - Voice of The Darkness (Digital Extremes)

References[link]