OpenLLM-France/wikimedia huggingface dataset:
# Central Bookstore

The Central Bookstore (traditional Chinese: 中央書局; simplified Chinese: 中央书局; pinyin: Zhōngyāng Shūjú) is a bookstore in Central District, Taichung, Taiwan.

## History
### Empire of Japan

The bookstore was originally opened on 3 January 1927 by Taiwanese Cultural Association as a meeting venue for pro-democracy and self-rule movement as a branch of the Central Club. The first and second floor housed selected Mainland Chinese, Japanese and Western books. It also served as the venue for the public to learn about writer Lu Xun and Ba Jin after the May Fourth Movement on 4 May 1919 in Peking. Later the shop caught attention of the government and it was then placed under heavy surveillance.

### Republic of China

After the handover of Taiwan from Japan to the Republic of China in 1945, the shop finally resumed to its normal operation. In the same year, it was later moved to its current building on Taiwan Boulevard which it was used to be used as the store dormitory and warehouse. In 1998, the store was closed due to financial difficulties. Since then, it had been used as wedding dress shop, convenience store and motorcycle helmet store. In 2016, the rights to use the building was obtained by Shang Shan Human Culture Foundation. Since then, the building was renovated and restored as a bookstore again with a cost of NT$20 million. The bookshop was reopened for trial in November 2019 and on 18 October 2020, it was officially reopened in a ceremony attended by Culture Minister Lee Yung-te

## Architecture

The bookstore is housed in a 3-story building with a circular shape.

## Transportation

The bookstore is accessible within walking distance northeast of Taichung Station of Taiwan Railways.
# Ananaspis

Ananaspis is a genus of trilobite in the order Phacopida, which existed in what is now the Czech Republic. It was described by Campbell in 1967, and the type species is Ananaspis fecundis, which was originally described as Phacops fecundus communis by Barrande in 1852.
# Andiceras

Andiceras is an enigmatic perisphinctacean ammonite belonging to the neocomitid subfamily Berriasellinae. Andiceras was named by Krantz in 1926 and is known from Tithonian sediments in Argentina and the Chinameca and La Caja Formations, Mexico.
# Angranoceras

Angranoceras is an extinct genus of cephalopod belonging to the Ammonite subclass.

## Distribution

None cataloged
# Anomphalidae

The Anomphalidae is an extinct family of fossil sea snails, marine gastropod mollusks. These are archaeogastropods which are included in the suborder Trochina. The Anomphalidae lived during the Paleozoic, from the Silurian to the Middle Permian. According to some authorities these snails belong instead to the Euomphalacea.

## Morphologic diagnosis

Shells of the Anomphalidae are rounded, almost discoidal, low-spired trochospiral inform, possibly with a globular body whorl. The aperture is oval, without exhalent slit or crease. The umbilicus is narrow, open or closed. The inner shell layer is seemingly nacreous. The shell surface is generally smooth, ornamentation consisting of fine transverse lyrae or growth lines parallel to the aperture lip.
The Anomphalidae differ from the Euomphalcea to which they have been reassigned in being more trochoidal, in lacking the angulation on the upper whorl surface characteristic of Euomphalacea, and in having the inner shell layer seemingly nacreous. (The inner shell layers of the Euomphalacea may be of laminar aragonite, but are never nacreous.) The Anomphalidea differ from the Pleurotomariacea in lacking the often deep slit or selenizone, which is characteristic of that taxon.

## Taxonomy

J Brooks Knight, et al, in the Treatise, 1960, assigned 10 genera to the Annomphalidae. They are
    Anomphalus Meek and Worthen 1866, the type genus
    Cycloscena Fletcher 1958
    Eiselia Dietz 1911
    Isonema Meek and Worthen 1866
    Pycnomphalus Lindström 1884
    Turbocheilus Perner 1907
    Sosiolytes Gemmellaro 1889
    Straparella Fischer 1885
    Turbinilopsis de Koninck 1881
    Tychonia de Koninck 1881
At present the Anompalideae has been expanded to include 17 genera in two subfamilies established by Peel, 1984.
Added to Anomphalus, Cycloscena, Eiselia, and Isonema in the Anomphalinae are:
Antirotiela Cossmann 1918, given in the Treatise as a synonym for Anomphalus
    Frydacosta Cook and Nützel 2005
    Delphinuella Heidelberger 2001
    Givediscus Heidelberger 2001
    Littorella Heidelberger 2001
    Nodinella Heidelberger 2001
Contained within the Pycnomphalinae in addition to Pycnomphalus, Turbocheilus, Sosiolites, Strapariella, and Tychonia:
    Pycnotrochus Perner 1903
    Turbinilopsis de Koninck 1881
Pycnotrochus, from the Upper Silurian of Europe, was removed from the Sinuopeidae (Pleurotomariacea); the lip has a sinus more characteristic of the original family. Turbinopsis, from the Lower Devonian of North America, was removed from the Palaeotrochidae (Palaeotrochacea); has a spiral chord not found on typical Anomphalidae and an aperture with a thicker, wider lip, also atypical.
Bouchet & Rocroi, 2005 simply included the Anomphalidae in "basal taxa that are certainly Gastropoda".
# Archaeocyon

Archaeocyon ("ancient dog") is an extinct genus of the Borophaginae subfamily of canids native to North America. It lived during the Oligocene epoch 32-24 Ma., existing for approximately 8 million years. Species of Archaeocyon are among the earliest known borophagines, although a species of Otarocyon has a slightly earlier first appearance. Fossils have been found across the northern Great Plains and along the west coast of North America.
Archaeocyon was a comparatively small and unspecialized dog. Its dentition (teeth) suggests a slightly more hypocarnivorous (omnivorous) diet than the otherwise similar Hesperocyon. The skeleton is also generalized, lacking specializations for running and retaining a plantigrade foot posture.
A few derived features of the dentition support a relationship to Borophaginae and Caninae (the subfamily that includes living canids), rather than to the basal canid subfamily Hesperocyoninae. The temporal position of Archaeocyon suggests an affinity to borophagines because the first members of Caninae appear substantially earlier.

## Species

Three species of Archaeocyon have been described. The two earlier species, A. pavidus and A. leptodus, differ primarily in size, with A. leptodus being larger. The third species, A. falkenbachi, is the size of A. leptodus and differs from other Archaeocyon species in having a shorter, broader skull.
# Arctohungarites

Arctohungarites is a genus of Triassic ammonoids now placed in the ceratitid family Danubitidae, but previously included in the Hungeritidae.
The shell of Arctohungerites is subdiscoidal, involute, with a rounded venter, weak sigmoidal folds on the body chamber and a distinct ventral keel on the distal end of the chambered portion. The suture is ceratitic.
Arctohungerites was found in Middle Triassic (Anisian) sediments in northern Siberia
# Arctosirenites

Arctosirenites is a genus of extinct ceratitid ammonoids from the Triassic of British Columbia and Nunavut, Canada, included in the Trachyceratidae.
# Arctoprionites

Arctoprionites is a genus of extinct ammonites (s.l.) from the Triassic, belonging to the ceratitid family Prionitidae. It has been found in Canada in British Columbia, in Japan, Kazakhstan, and in the U.S. in Nevada.
# Aristoptychites

Aristoptychites is an extinct genus of cephalopod from the Anisian stage of the Middle Triassic belonging to the ammonoid subclass.
Shell involute, whorls strongly embraced, venter acutely rounded. Suture curved, subammonitic; more closely resembles that of Flexoptychites or Discoptychites than of other ptychitids.
# Armatites

Armatites is an Upper Devonian goniatitid included in the tornoceratid family. The shell, or conch, is discoidal, with flattened flanks, a flattened venter with a double keel, and a deep ventral sinus, but without ventrolateral grooves. The lateral saddle of the suture is broad. Armatites is known from the Upper Devonian (Fammenian) of Canning Basin in Australia. The subfamily in which it is included, the Aulatornoceratinae is also known from France with the genus Aulatornoceras.
In terms of nomenclature Armatites started as Pseudoclymenia by Wedekind in 1918, became Tornoceras (Polonoceras) by Glenister in 1958, simply Polonoceras by Bogoslovskii, 1971, and finally Armatites by Becker in 1993.
# Asaphiscus

Asaphiscus is a genus of trilobite that lived in the Cambrian. Its remains have been found in Australia and North America, especially in Utah.

## Distribution

A. wheeleri occurs in the Middle Cambrian of the United States (Delamaran, Lower Wheeler Shale, Millard County, Utah, 40.0°N, 113.0°W; and Menevian, Wheeler Formation, House Range, Utah, 39.2° N, 113.3° W).

## Description

Asaphiscus are average size trilobites of (up to 8 centimetres or 3.1 inches) with a rather flat calcified dorsal exoskeleton of inverted egg-shaped outline, about 1+1⁄2× longer than wide, with the widest point near the back of the headshield (or cephalon). The cephalon is about 40% of the body length, is semi-circular in shape, has wide rounded genal angles, and a well defined border of about 1⁄8× the length of the cephalon. The central raised area of the cephalon (or glabella) is conical in outline with a wide rounded front and is separated from the border by a preglabellar field of about 1⁄8× the length of the cephalon, and has 3 sets of furrows that may be clear or inconspicuous. The articulated middle part of the body (or thorax) has 7-11 segments (9 in A. wheeleri), with rounded tips. The tailshield (or pygidium) is about 30% of the body length, is semi-circular in shape, with a wide flat border, and an entire margin.

## Reassigned species

Some species originally described as belonging to Asaphiscus have later been reassigned to other genera.
* A. capella = Glyphaspis capella
* A. granulatus = Genevievella granulata
* A. gregarius = Blainia gregarius
* A. minor = Cedaria minor
* A. unispinus = Weeksina unispina

## Sources

* A Pictorial Guide to Fossils by Gerard Ramon Case
# I Can See Clearly Now (Johnny Nash album)

Professional ratings :
| Review scores ||
| Source | Rating |
| Christgau's Record Guide | B |
| The Rolling Stone Album Guide | |
I Can See Clearly Now is an album by the American singer Johnny Nash, released in 1972. The album includes two of his biggest hit singles, the title track ("I Can See Clearly Now") and "Stir It Up." "I Can See Clearly Now" hit number one on the Billboard Hot 100 on November 4, 1972. Nash's backing band for the album was the Jamaican reggae group Fabulous Five Inc.

## Track listing

All tracks composed and arranged by Johnny Nash; except where indicated
* "Stir It Up" (Bob Marley)
* "That's the Way We Get By" (John "Rabbit" Bundrick)
* "Guava Jelly" (Bob Marley)
* "(It Was) So Nice While It Lasted"
* "Ooh Baby You've Been Good to Me"
* "You Poured Sugar on Me" (Bob Marley, Johnny Nash)
* "I Can See Clearly Now"
* "Comma Comma" (Bob Marley)
* "We're All Alike" (John "Rabbit" Bundrick)
* "How Good It Is"
* "The Fish and the Alley of Destruction" (on original pressings), later replaced by "Cream Puff" (Margaret Nash)
* "There Are More Questions Than Answers"

## Charts

| Chart (1972) | Peak position |
| Australia (Kent Music Report) | 29 |

## Personnel

* Bernie O'Gorman, Jack Clegg, John Middleton, Siddey - engineers
* Denis Waugh - cover photography
* Tim Fulford-Brown - back cover photography
* Marty Pekar - liner notes
# Austroraphidia

Austroraphidia is an extinct genus of snakefly in the family of Baissopteridae. Austroraphidia fossils were described by Willmann in 1994. The genus was later described by Michael S. Engel in 2002. It has five sister taxa; Baissoptera, Cretinocellia, Cretoraphidia, Cretoraphidiopsis and Lugala. Its fossils were found at the Crato MNHN collection in Brazil, often known as the Cretaceous of Brazil. It contains one species, the extinct Austroraphidia brasiliensis, which was described by Nel et al. in 1990. Its average body length is 12.3 centimetres (4.8 in), the forewing is 10.2 by 3.0 centimetres (4.0 in × 1.2 in) and the hindwing is 9.5 by 2.88 centimetres (3.74 in × 1.13 in).
# Vresselse Bossen

East of the village of Nijnsel and the hamlet of Vressel, both in Meierijstad, North Brabant, Netherlands, is the location of the Vresselse bossen or Vresselsche Bosch (Vressels Forest). The Vresselse Bossen is a forest area of 241 ha. It is owned and managed by the National Forest Service (Staatsbosbeheer). The forest is named after the nearby hamlet of Vressel.
It is a young forest that planted in a drift-sand ridge. At the beginning of the 20th century, there was scarcely a tree in the area. The area consisted mainly of dunes and heathland. At the edges of the area lived farmers who were severely affected by the shifting sands. To protect the fields was therefore decided to reforest the drift-sand. At that time, almost exclusively pine was used for the reforesting. In the 1920s, it had become a production forest consisting of Scots pine for the Limburgian mines.
Within the area, there are two main fen systems: The Hazenputten and the Oude Putten. Rare vegetation is found around the fens: among others White beak-sedge and bog asphodel can be found here.
The contemporary management by Staatsbosbeheer focuses on getting a more varied forest composition, including native oak, linden and beech. To prevent the Hazenputten from drying, competing for vegetation is removed around the pools. The area around the marshes has been grazed by Highland cattle and Exmoor horses in the past.
The area has a rich bird population. Breeding birds are: yellowhammer, kingfisher, black woodpecker, northern goshawk, little grebe, European green woodpecker, common buzzard, great egret, long-eared owl, coal tit, little owl, barn owl and crested tit.
Also many species of mammals can be encountered: These include: roe deer, European badger, Eurasian harvest mouse, European polecat, European water vole, European hedgehog, Eurasian red squirrel, common pipistrelle, European hare, brown long-eared bat, stoat, serotine bat, European mole, Natterer's bat, least weasel, red fox, Daubenton's bat, beech marten and several species of shrew, dormice, apodemus and arvicolinae.
The "Hazenputten" was nominated by Staatsbosbeheer for the title of "Most beautiful spot" in the Netherlands in 2013.
The Vresselse Bossen are part of Het Groene Woud, a vast nature area between Eindhoven, Den Bosch and Tilburg. West of the Vresselse Bossen lies the valley of the Dommel; in the northwest, the Vresselse Forest reaches the Moerkuilen. To the north, there is the reclaimed heathland of the Jekschot Heath and to the east lies the DAF test track and Mariahout Forest.

## Trivia

* A medium-distance hike can be done in the area while there are also some shorter circular walks possible.
* The area at the Hazenputten was affected by a small bush fire on 7 March 2014.
# Balatonites

Balatonites is a genus of extinct cephalopods belonging to the ceratitid family Balatonitidae. There are at least four known species: B. balatonicus, B. oyama, B. shoshonensis, and B. zitteli.
The shell of Balatonites is essentially evolute, coiled with earlier whorls showing, and is laterally compressed with flattish sides and a roof-like venter. The sides are covered with radial ribs that have tubercles generally arranged in umbilical, median and ventral rows.
Balatonites has been found in Hungary, the Alps, Balkans, Germany, Japan, and Nevada.
# Bavarilla

Bavarilla is an extinct genus of trilobites.
The species Bavarilla hofensis as bavarilla was found in the 19th century near Hof (Saale) and lived from 485 Ma to 478 Ma in the Paleozoic.
# Blancocamelus

Blancocamelus is an extinct genus of terrestrial herbivores the family Camelidae, endemic to North America during the Pliocene through Pleistocene—4.9 million years ago until 300,000 years ago, existing for about 4.6 million years.

## Taxonomy

Blancocamelus was named by Dalquest (1975). Its type species is Blancocamelus meadei. It was assigned to the Camelidae by Dalquest (1975) and Carroll (1988).
# Blanfordiceras

Blanfordiceras is a strongly ribbed, evolute ammonite included in the perisphinctacean family, Neocomitidae that lived during the latest Jurassic. The shell of Blanfordiceras is discoidal, with evolute coiling and all whorls visible so as to have a broad umbilicus. Exposed whorls are ornamented with strong ribbing that arises from the umbilicus, bifurcating on the outer flanks and extending onto the venter. In general form Blanfordiceras is similar to Berriasella, although with a more rounded whorl section.
# Bolbochasmops

Bolbochasmops is a genus of trilobite in the order Phacopida, which existed in what is now Estonia. It was described by McNamara in 1980, and the type species is Bolbochasmops emarginata, which was originally described as Chasmops bucculenta, and later as Phacops bucculenta by Schmidt in 1881.
# Brachycyon

Brachycyon is an extinct genus of terrestrial carnivores belonging to the suborder Caniformia, family Amphicyonidae ("bear dog"), which inhabited Eurasia and North America.
Brachycyon was named by Filhol (1872). It was assigned to Amphicyonidae by Carroll (1988).
# Old Tainan Magistrate Residence

The Old Tainan Magistrate Residence (traditional Chinese: 原臺南縣知事官邸; simplified Chinese: 原台南县知事官邸; pinyin: Yuán Táinán Xiàn Zhīshì Guāndǐ) or The Clock Building is a historical residence in East District, Tainan, Taiwan.

## History
### Empire of Japan

The magistrate residence building was originally constructed in 1900 as the residence for the Tainan Prefecture Governor Imai Konichi (Japanese: 今井艮一). In November 1901, the Cho administrative system was established, and the minister was moved to the nearby Tainan Minister's Residence. The magistrate residence building was then managed by Tainan Hall. Part of it was then lend to the army but was changed to serve as the Brigade Magistrate Residence. When Tainan Governor the Empire of Japan royal family came to visit Tainan, the magistrate residence building was named Tainan Governor's Residence. In 1920, prefectures changed to counties and Tainan Minister was assigned to be Tainan Prefecture Governor. The official residence of the governor was changed back to the magistrate residence building and was named Tainan Prefecture Magistrate Residence. In 1936, an underground air-raid shelter was built at the southeast side of the building due to the Second Sino-Japanese War. Fortunately the building survived the war.

### Republic of China

After the handover of Taiwan from Japan to the Republic of China in 1945, the building was partially rebuilt and was briefly used by the Taiwan Salt General Office and local Land Office. In the 1980s, it was used as the headquarter office for the Civil Defense and District Office. In 1998, it was declared as a historical building. After the declaration, the Cultural Affairs Bureau of Tainan City Government launched a restoration project that would last for about 10 years and outsourced its building management in 2010. On 8 October 2011, the building was reopened as Magistrate Residence Concert Hall when it was turned into a restaurant and café by Taiwan Artists Ensemble Culture Foundation. On 8 February 2015, the building was then renamed as Magistrate Residence when the Koche Development Co., Ltd. opened the 1900 Café, Knowledge Salon and Time of Old Tainan County Magistrate Residence. On 10 October 2020, the building was then placed under Antio Design Co., Ltd. in which they will reopened it as Magistrate Residence Living Center in which will house exhibitions, lectures, household items, afternoon tea, meals and beverages.

## Architecture

The residence is a two-story building with English colonial architectural style. It has arcade around the building which extends at the center and the two sides of the building which are covered with bricks.
# Bykivka

Bykivka (Ukrainian: Биківка) is a rural settlement in Zhytomyr Raion, Zhytomyr Oblast, Ukraine. Population: 1,650 (2022 estimate).

## History

Until 26 January 2024, Bykivka was designated urban-type settlement. On this day, a new law entered into force which abolished this status, and Bykivka became a rural settlement.
# Mobile infrared transmitter

A mobile infrared transmitter (MIRT) is an electronic traffic preemption device that city buses and emergency vehicles use to control the traffic control equipment for intersections they are approaching, in order to pass through the intersection as efficiently or safely as possible.

## Description

An MIRT device consists of a timer circuit connected to an infrared LED array. The timer causes the infrared LEDs to strobe at specific frequencies, such as 10Hz for low priority (buses) or 14 Hz for high priority (emergency vehicles). Low priority transmitters will control the intersection to perform a normal light change, while high priority transmitters will change an entire intersection immediately.

## Usage restrictions

Certain cities use specially encoded infrared pulses to prevent the use of home made transmitters.
People buying and selling the devices were stopped in August 2005 when President George W. Bush passed the Safe, Accountable, Flexible, Efficient Transportation Equity Act.
It established a minimum sentence of six months in prison for anyone who uses the device illegally. The act also said those selling the device illegally could serve a year in prison, according to the U.S. Department of Transportation web site.
# Kössen Formation

The Kössen Formation is a Late Triassic (Rhaetian-age) geological formation in the Northern Calcareous Alps of Austria and Germany, in the Tiroler-Lech Nature Park. During the Late Triassic, the area now occupied by the Northern Calcareous Alps was instead a long, passive coastline at the western tip of the Neotethys Ocean. The environment was initially dominated by a wide and shallow carbonate platform within a lagoon between the shore and a string of reefs. This carbonate platform is nowadays preserved as the Carnian to Norian-age Hauptdolomit and Dachstein Formation. The Kössen Formation represents a period of increased siliciclastic clay input into the lagoon, covering up the carbonate platform with marls and marly limestones instead of pure limestone or dolomite. The Eiberg Member of the Kössen Formation was deposited in the Eiberg basin, a narrow strip of deeper water which developed between the carbonate platform and the shoreline in the later part of the Rhaetian.
# Chinese frigate Dongguan

Dongguan (560) is a Type 053H1G (Jianghu-V) frigate of the People's Liberation Army Navy.
The frigate is based at Mischief Reef, 76 nautical miles from Half Moon Shoal, Spratly Islands in South China Sea. On 25 February 2011 she was involved in a confrontation in Jackson Atoll with three fishing boats from the Philippines. She ran aground on Half Moon Shoal on 11 July 2012.