OpenLLM-France/wikimedia huggingface dataset:
# Dog in the Sand

Professional ratings :
| Aggregate scores ||
| Source | Rating |
| Metacritic | 73/100 |
| Review scores ||
| Source | Rating |
| AllMusic | |
| Alternative Press | 6/10 |
| The A.V. Club | B+ |
| Encyclopedia of Popular Music | |
| Magnet | |
| Mojo | |
| NME | 6/10 |
| Pitchfork | 7.8/10 |
| The Rolling Stone Album Guide | |
| Wall of Sound | 75/100 |
Dog in the Sand is Frank Black's third album with backing group the Catholics. It was released in 2001 by Cooking Vinyl in Europe and What Are Records? in the United States, and was produced by Nick Vincent. The album was generally met with favorable reviews. Though retaining the live-to-two-track method of recording of the previous two albums, this album found the band branching away from purely electric rock to incorporate acoustic guitar, pedal steel, and Rhodes Piano and Wurlitzer organ into the sonic template.
A notable change on the album is the induction of Black's former producer and keyboardist, Eric Drew Feldman, to the Catholics, a veteran of Captain Beefheart & His Magic Band and Pere Ubu. The album also features contributions from Moris Tepper (Captain Beefheart, Tom Waits) and Black's former Pixies bandmate Joey Santiago, as well as guitarist Dave Phillips, who would soon join the Catholics as a full-time member.
"When we got back to Los Angeles for a two week rehearsal (for the Dog in the Sand album), we added auxiliary guitarist Dave Philips, who was so good he ended up playing on every song," Black said.
The album was reissued by SpinART in 2003 including four bonus tracks.

## Track listing

All songs written by Frank Black.
* "Blast Off" – 7:13
* "I've Seen Your Picture" – 2:51
* "St. Francis Dam Disaster" – 5:02
* "Robert Onion" – 4:00
* "Stupid Me" – 2:31
* "Bullet" – 3:53
* "The Swimmer" – 2:48
* "Hermaphroditos" – 4:12
* "I'll Be Blue" – 3:34
* "Llano del Rio" – 4:14
* "If It Takes All Night" – 3:19
* "Dog in the Sand" – 3:48
2003 reissue bonus tracks
* "Robert Onion" (Acoustic)
* "Blast Off" (Acoustic)
* "Stupid Me" (Acoustic)
* "If It Takes All Night" (Acoustic)

## Personnel

Credits adapted from the album's liner notes.

### Frank Black and the Catholics

* Frank Black – vocals, acoustic guitar, guitar
* Scott Boutier – drums
* Eric Drew Feldman – electric piano, piano, clavioline, vocals
* Rich Gilbert – guitar, pedal steel guitar, dobro, vocals
* David McCaffery – bass, vocals

### Additional musicians

* Dave Phillips – acoustic guitar (tracks: 3, 5, 7, 9, 12), guitar (tracks: 1, 2, 4, 10, 11), pedal steel guitar (track 6), slide guitar (track 8), vocals (track 10)
* Joey Santiago – guitar (tracks 1, 4)
* Moris Tepper – banjo (track 3), bihuela (track 10), vocals (track 10)
* Nick Vincent – percussion (track 1)

### Technical

* Nick Vincent – producer
* Billy Joe Bowers – recording engineer
* Mike Terry – assistant engineer
* Eddy Schreyer – mastering engineer
* Andrew Swainson – cover design
* Steve Gullick – photography
# Millet butterflyfish

The millet butterflyfish (Chaetodon miliaris) is a species of butterflyfish in the family Chaetodontidae. Other common names include the lemon butterflyfish and the millet-seed butterflyfish. It is endemic to the Hawaiian Islands and the Johnston Atoll, where it is found at depths down to 250 m (820 ft). Although it has a limited range, it is common around Hawaii, and the International Union for Conservation of Nature has listed its conservation status as being of "least concern".

## Taxonomy

In its subgenus Exornator, it probably belongs to a group that also includes the African butterflyfish (C. dolosus), the crochet butterflyfish (C. guentheri) and the reef butterflyfish (C. sedentarius). The crochet butterflyfish might be the closest living relative of C. miliaris. If the genus Chaetodon is split up, Exornator might become a subgenus of Lepidochaetodon.

## Description

The millet butterflyfish grows to a maximum length of 13 cm (5 in). It is a deep-bodied, laterally flattened fish. The dorsal fin has 13 to 14 spines and 20 to 23 soft rays and the anal fin has 2 to 3 spines and 17 to 20 soft rays. The general body colour is whitish or yellow, with a number of vertical rows of dark spots on the flanks. A broad black stripe runs from above the eye to the base of the operculum, and there is a large black patch on the caudal peduncle.

## Distribution and habitat

This fish is endemic to the Hawaiian Islands and the Johnston Atoll, and is found down to depths of at least 250 m (820 ft). Its habitats include coastal fringing reefs, outer reefs and lagoons.

## Ecology

The millet butterflyfish is a schooling species found in mid-water that feeds on zooplankton. It also feeds opportunistically on polychaete worms and other small invertebrates on the seabed. Food is drawn into the mouth by rapid suction. It does not seem to be territorial but forms aggregations to feed at particular sites on the reef. Although its breeding habits are unknown, the gonads are large as compared with the body size, suggesting that it may have a promiscuous mating system. Breeding takes place between January and May, and newly settled juveniles are found in inner reef areas between April and June.
This butterflyfish is sometimes collected from the wild for the aquarium trade. Its feeding habits make it more suitable for keeping in a reef aquarium than more specialist butterflyfish species that feed on scleractinian corals. Although rare at Johnston Atoll, it is plentiful around the Hawaiian Islands. The International Union for Conservation of Nature believes that the population is stable and that collection has little impact, and they assess the conservation status of this fish as being of "least concern".
# Goła

Goła is a village in the administrative district of Gmina Gorzów Śląski, within Olesno County, Opole Voivodeship, in south-western Poland. It lies approximately 6 km (3.7 mi) north-west of Gorzów Śląski, 22 km (14 mi) north of Olesno, and 55 km (34 mi) north-east of the regional capital Opole.
# Keiji Shirahata

Keiji Shirahata (白幡 圭史, Shirahata Keiji, born 8 October 1973) is a retired Japanese speed skater.
With two silver and one bronze medals at the World All-Round Speed Skating Championships he has been the most successful Japanese long track speed skater in all-round competitions. He was ranked 4th on the Adelskalender in February 1997. Shirahata established 22 national records and was nine times national all-round champion.

## Records
### Personal records

Personal records :
| Men's speed skating |||||
| Event | Result | Date | Location | Notes |
| 500 m | 37.18 | 10 August 2001 | Calgary | |
| 1000 m | 1:22.86 | 18 February 1989 | Sapporo | |
| 1500 m | 1:47.78 | 9 February 2002 | Salt Lake City | |
| 3000 m | 3:47.00 | 1 December 2001 | Calgary | |
| 5000 m | 6:26.04 | 9 March 2001 | Salt Lake City | |
| 10000 m | 13:19.92 | 9 March 2001 | Salt Lake City | |
# Chinameca Formation

The Chinameca Formation is a geologic formation in Mexico. It preserves fossils dating back to the Jurassic period.
# Roberto Gándara

Roberto Gándara González (born 16 April 1990) is a Spanish professional footballer who plays for Santa Marta as a midfielder.

## Club career

Born in Salamanca, Gándara graduated from the youth academy of local UD Salamanca and made his debut for the reserves in 2009–10 season, in Tercera División. After a stint with Arenas Club de Getxo in the same tier (securing promotion to Segunda División B), he signed for CD Badajoz on a one-year contract on 18 July 2015.
On 16 July 2016, Gándara switched to CF Talavera de la Reina. At the end of the 2016–17 season, the club won promotion to Segunda División B. On 30 June 2018, he moved abroad for the first time in his career and joined Polish I liga club Podbeskidzie Bielsko-Biała.
# Beulieu Formation

The Beulieu Formation is a geologic formation in France. It preserves fossils dating back to the Devonian period.
# Bevahites

Bevahites is a Cretaceous ammonite with an evolute, ribbed, tuberculate, and keeled shell with a squarish to compressed whorl section.
Bevahites is a member of the collignoniceratid subfamily Texanitinae as well as of the Acanthoceratoidea and has been found in Upper Santonian to middle Campanian sediments in southern Africa and Madagascar.
Barrisioceras, Menabites, and Parabevahites are among related genera.
# Bright Green

Bright Green is a progressive UK politics blog primarily edited by members of the Green Party of England and Wales and the Scottish Greens.
Regular contributors include former MSP Mark Ballard, Maggie Chapman, Peter McColl, Adam Ramsay, Gary Dunion and Sarah Beattie-Smith.
In 2011 McColl was voted the UK's top Green blogger for his contributions to Bright Green.
The blog was listed in the top 100 political blogs by Total Politics in 2011.
Bright Green contributors are active in Scottish and UK politics beyond the website, hosting discussions and workshops at events and conferences, such as the 2012 Radical Independence Campaign national conference.
# Bigotites

Bigotites is strongly ribbed, round-whorled perisphinctid ammonitic cephalopod from the middle Jurassic with a smooth band along the outer edge of the shell.
# Blaa Mountain Formation

The Blaa Mountain Formation is a geologic formation in Nunavut. It preserves fossils dating back to the Triassic period.
# Black Creek Group

The Black Creek Group is a Late Cretaceous (early to middle Campanian)-aged geologic group in the southeastern United States, where it is known from the coastal plain of North Carolina and South Carolina. Deposited in brackish or nearshore marine conditions, it preserves fossils, including a diversity of dinosaurs and marine reptiles.
It consists of the following geologic formations:
* Tar Heel/Coachman Formation (oldest)
* Bladen Formation
* Donoho Creek Formation (youngest)

## Paleofauna

* cf. Deinosuchus rugosus
* cf. Coelosaurus antiquus
* cf. Dryptosaurus sp.
* cf. Lophorhoton atopus
* Hypsibema crassicauda - "Caudal vertebrae, fragmentary humerus, fragmentary tibia, metatarsal II."
* Leptoceratopsidae indet.
* Dromaeosauridae indet.
# Blacourt Formation

The Blacourt Formation is a geologic formation in France. It preserves fossils dating back to the Devonian period.

## Paleofauna
### Invertebrates

* Quasillites
* Rothpletzella
* Tentaculites

### Vertebrates

* Melanodus loonesi
* Pokorninella bricae
* cf. Synthetodus
# Bocatherium

Bocatherium is an extinct genus of tritylodont mammaliamorphs from the Pliensbachian (Early Jurassic) of Tamaulipas, Mexico. It is known only from a skull found at the Huizachal Canyon locality, "a Pliensbachian floodplain siltstone in the La Boca Formation".
# Hoover–Minthorn House

The Hoover–Minthorn House is a museum in Newberg, Oregon, United States, created from the residence of Herbert Hoover, thirty-first President of the United States. Hoover lived there from 1885 to 1891, with his uncle and aunt John and Laura Minthorn. The Minthorns were administrators of the Quaker school Friends Pacific Academy, now George Fox University, which Hoover and his brother Tad attended.
The house, an Italianate design built in 1881 by Jesse Edwards, a Quaker merchant, is the first residence Edwards built and the oldest house still standing in what is now Newberg, Oregon. Representing vernacular design in the Willamette Valley, it was restored and opened to the public in 1955. It is located on 115 South River Street. Owned and operated as a house museum by the Oregon chapter of The National Society of the Colonial Dames of America, it has been furnished with late 19th-century period furnishings, including the bedroom furniture used by Hoover as a boy.
The house was placed on the National Register of Historic Places (as the Dr. Henry J. Minthorn House aka Herbert Hoover House) in 2003.
# Bonanza Formation

The Bonanza Formation is a geologic formation in British Columbia. It preserves fossils dating back to the Jurassic period.
# Bonanza King Formation

The Bonanza King Formation is a geologic formation in Nevada. It preserves fossils dating back to the Cambrian period.
# Bon Homme Gravel

The Bon Homme Gravel is a geologic formation in South Dakota. It preserves fossils.
# Boulder Creek Formation

The Boulder Creek Formation is a geologic formation in northeastern British Columbia. It was named for a tributary to Commotion Creek in the Pine Pass area by E.M. Spieker in 1921. At one time considered to be a member of the Commotion Formation, it was elevated to formation status by D.F. Stott in 1982.
The formation was deposited in shallow marine to shoreline environments during the Albian stage of the Early Cretaceous period. It preserves ammonites, plant remains, and other fossils.

## Lithology and Environment of Deposition

The Boulder Creek Formation records the transition from marine conditions, represented by the shales of the underlying Hulcross Formation, to continental environments, with a return to marine conditions marked by the shales of the overlying Hasler Formation. Near shore and shoreface deposits consist of massive, fine grained, well sorted sandstones, and massive, silica-cemented conglomerates of quartz and chert pebbles in a matrix of coarse sand. Delta plain and floodplain deposits consist of interbedded argillaceous sandstones, carbonaceous shales and thin coal beds.

## Thickness and Distribution

Outcrops of the Boulder Creek Formation can be seen along the Peace River eastward from Hudson's Hope, and it is present in the subsurface in the Peace River plains to the east. It is well exposed in the foothills of the Canadian Rockies between the Peace and Wapiti Rivers, where it reaches thicknesses of up to 171 metres (560 ft). It can be traced southward through the foothills almost as far the Kakwa River near the British Columbia-Alberta boundary.

## Relationship to Other Units

The Boulder Creek Formation is part of the Fort St. John Group. Originally described as a member of the Commotion Formation, the Boulder Creek was elevated to formational status along with the other members of the Commotion by D.F. Stott in 1982, who proposed that the term 'Commotion Formation' be abandoned.
The Boulder Creek Formation conformably overlies the marine shales of the Hulcross Formation, and is conformably overlain by the marine shales of the Hasler Formation. It is equivalent to the Cadotte Member, and possibly the Paddy Member, of the Peace River Formation of the Peace River plains. It correlates with the middle part of the Buckinghorse Formation in the Muskwa River area, and with the Tussock Member of the Scatter Formation in the Liard River area. Equivalent beds may be present above the coal-bearing strata near Grande Cache.
# Brachycormus

Brachycormus is an extinct genus of salamandrid amphibian from the Oligocene–Miocene of Europe.
Neoteny is evident in some larval specimens by the retention of branchial arches and a high degree of ossification in the hyobranchial skeleton. The reason for this neoteny may be explained by a drop in global temperature during the Oligocene cooling event, which may have induced a delay in somatic development in relation to the gonadal development of these animals, thus allowing them to breed at the larval stage and shift the timing of their developmental change to cope with the changes in climate.
# Brachydegma

Brachydegma is an extinct genus of prehistoric freshwater ray-finned fish that lived during the Leonardian age (Cisuralian/lower Permian) in what is now Texas, United States. It is known from two fossils, which were recovered from the Clear Fork Formation. A potential record is also known from the concurrent Hennessey Formation of Oklahoma. It is one of the only fossil ray-finned fish from the Permian that preserves the skull bones in three dimensions.

## Classification

Brachydegma was first considered a "palaeoniscid". A later study rather suggested that Brachydegma could be one of the earliest crown neopterygians (Halecomorphi) known from the fossil record. However, this view relied on misinterpretations of cranial features. A more recent study yielded conflicting placements of Brachydegma on the actinopterygian tree of life, rendering its placement in an order or family difficult. It appears to be closely related or possibly a member of the crown group of Actinopterygii, though a closer relationship with either Neopterygii or Polypteriformes appears plausible.
# Bredyia

Bredyia is a genus of ammonites from the lower part of the Middle Jurassic, found in Europe and North America.
Bredyia is a member of the Hammatoceratidae, a family which comprises part of the Hildoceratoidea. Its shell is involute, strongly ribbed, with a small umbilicus. Whorls are strongly embracing; ribs thick, radially straight on the sides, curves forward on the venter but do not meet. The sides or flanks are outwardly bowed. The venter has a narrow keel and may be fastigate, like a gable roof.
# Breivik Formation

The Breivik Formation is a geologic formation in Norway. It preserves fossils dating back to the Cambrian period.
# Bretesuchus

Bretesuchus is an extinct genus of sebecosuchian mesoeucrocodylian within the family Sebecidae known from northwestern Argentina. It was a large apex predator (total length approximately 4 m).

## Discovery

Fossils of Bretesuchus have been found in the El Brete locality, from the Maíz Gordo Formation of northwestern Argentina and date back to the Thanetian stage of the late Palaeocene, about 58.7-55.8 million years ago. The highly bent premaxilla shows that it lies within the suborder Sebecosuchia, a group of mostly South American terrestrial carnivorous crocodylomorphs with distinctive laterally compressed snouts. Bretesuchus was originally assigned to its own family, the Bretesuchidae which was found to be the sister group of Sebecus. In 2007, a species of Sebecus, S. querejazus from the Early Paleocene Santa Lucia Formation in Bolivia, was reclassified as a bretesuchid. It was given its own genus, Zulmasuchus. However, recent phylogenetic analyses found Bretesuchidae to nest deeply within Sebecidae, and thus to be synonymous with it. Zulmasuchus was found to be closely related to Sebecus, as originally had been proposed.

## Etymology

Bretesuchus was named by Zulma Gasparini, Marta Fernandez and Jaime E. Powell in 1993 and the type species is Bretesuchus bonapartei. The generic name refers to the "El Brete" locality, where the fossil remains were found, and suchus, Latinized from the Greek souchos, an Egyptian crocodile god. The specific name honors Jose Bonaparte.
# Bronson Group

The Bronson Group is a geologic group in Missouri. It preserves fossils dating back to the Carboniferous period.
# Bucatunna Formation

The Bucatunna Formation is a geologic formation in Alabama. It preserves fossils dating back to the Paleogene period.
# Buckingham Formation

The Buckingham Formation is a geologic formation in Florida. It preserves fossils dating back to the Neogene period.
# Buffalo Canyon Formation

The Buffalo Canyon Formation is a geologic formation in Nevada. It preserves fossils dating back to the Neogene period.
# Bumpnose Formation

The Bumpnose Formation is a geologic formation in Florida. It preserves fossils dating back to the Paleogene period.
# Bush Bay Formation

The Bush Bay Formation is a geologic formation in Michigan. It preserves fossils dating back to the Silurian period.
* Earth sciences portal
* Michigan portal
* Paleontology portal
# Calcaire de Fontanil

The Calcaire de Fontanil is a geologic formation in France. It preserves fossils dating back to the Cretaceous period.
# Calcaires siliceux de Dole

The Calcaires siliceux de Dole is a geologic formation in France. It preserves fossils dating back to the Jurassic period.
# Caliente Formation

The Caliente Formation is a geologic formation in California. It preserves fossils dating back to the Neogene period.
# Calliphylloceras

Calliphylloceras is an ammonite belonging to the Phylloceratidae.

## Species

Species within this genus include:
* Calliphylloceras alontinum (Gemmellaro, 1884)
* Calliphylloceras bicicolae
* Calliphylloceras capitanii
* Calliphylloceras demidoffi (Rousseau, 1842)
* Calliphylloceras disputabile (type) Spath, 1927
* Calliphylloceras freibrocki Imlay, 1953
* Calliphylloceras kochi (Oppel, 1865)
* Calliphylloceras nilssoni
* Calliphylloceras nizinanum
* Calliphylloceras propinquum
* Calliphylloceras seroplicatum
* Calliphylloceras spadae
* Calliphylloceras supraliasicum
The holotype of C disputabile, the type species, named by Spath in 1927, which came from the Middle Jurassic of Hungary, is based on Phylloceras disputabile Zittil. Neocalliphylloceras Bresairie 1936, Captianioceras Kuvacs 1939 and Euphylloceras Draughtchitz 1953 are equivalent genera.

## Description

Calliphylloceras has a smooth, compressed involute shell with a rounded venter and periodic constrictions in the internal mold; surface covered with lirae as in Phylloceras. The first and 2nd lateral saddles are usually triphyllic, others diphyllic.

## Distribution

This species has been found in the Cretaceous of Bulgaria, Canada, France, Japan, United States and in the Jurassic of Argentina, Austria, Germany, Hungary, India, Iran, Italy, Japan, Madagascar, the Russian Federation, Spain, Turkey, United States
# Calymene niagarensis

Calymene niagarensis is a species of trilobite belonging to the genus Calymene. These nektobenthic carnivores lived in the Middle Silurian, from 436.0 to 426.2 Ma.

## Description

Calymene niagarensis is a small species, reaching a length of about 4 centimetres (1.6 in) and a width of about 2.7 centimetres (1.1 in). It has around 20 body segments and small, round eyes.

## Distribution

Fossils of this species have been found in the Silurian sediments of United States. Most specimens have been found in New York and Oklahoma.
# Camp Creek Formation

The Camp Creek Formation is a geologic formation in Texas. It preserves fossils dating back to the Permian period.
# Camp Springs Formation

The Camp Springs Formation is a geologic formation in the Dockum Group of Texas. It preserves fossils dating back to the Late Triassic. It has also been known as the Camp Springs Conglomerate or Camp Springs Member. The unit was originally named for an unknown locality in West Texas, and was later used in reference to sandstone and conglomerate deposits in Scurry County. It is likely equivalent to the basal beds (Tecolotito Member) of the Santa Rosa Formation, and some authors have suggested abandoning the usage of the term "Camp Springs Formation" and similar names.

## Paleobiota

Extinct taxa of the Camp Springs Conglomerate :
| Genus / Taxon | Species | Material | Notes | Images |
| Buettnererpeton | B. bakeri | | A metoposaurid temnospondyl amphibian known from the Elkins Place bone bed. Previously considered a species of Metoposaurus. | |
| Wannia | W. scurriensis | | A basal (non-mystriosuchine) phytosaur. Previously considered a species of Paleorhinus. | |
# Cancelloceras

Cancelloceras is an extinct genus of ammonites in the family Gastrioceratidae. Species are from the Carboniferous.
†Cancelloceras elegans Ruzhentsev and Bogoslovskaya 1978 is from the Carboniferous of the Russian Federation, Nevada (United States) and Uzbekistan.
# Canoe Formation

The Canoe Formation is a geologic formation in Texas. It preserves fossils dating back to the Paleogene period.
# Carbonera Formation, Mexico

The Carbonera Formation is a geologic formation in Mexico. It preserves fossils dating back to the Berriasian to Hauterivian stages of the Early Cretaceous period.

## Fossil content

The following fossils were reported from the formation:

### Ammonites

* Maderia casitensis
* Mexicanoceras laticostatum
* M. multicostatum
* ?Hemihoplites mexicanus
* cf. Phylloceras serum
* Distoloceras sp.

### Bivalves

* Exogyra reedi
* Plicatula pulchra
* Gryphaea sp.

### Gastropods

* Vermetus cornejoi
* Pleurotomaria sp.

### Brachiopods

* Ptilorhynchia (Proteorhynchia) durangensis

### Corals

* Paretallonia hispaniensis