Showing posts with label Kagoshima Prefecture. Show all posts
Showing posts with label Kagoshima Prefecture. Show all posts

Saturday, 11 February 2023

Eruption on Mount Sakurajima in Kagoshima Prefecture, Japan.

Mount Sukurajima, a 1117 m high stratovolcano (cone-shaped volcano made up of layers of ash and lava) in Kagoshima Prefecture on Kyūshū Island, Japan, erupted on Wednesday 8 February 2023, according to the Kagoshima Meteorological Office. The volcano began erupting from the Showa Crater on the east side of the Minamidake Peak (the southernmost of the volcano's three summits), slightly after 10.50 am local time, and had by 11.10 am had produced an ash column over a kilometre high. The eruption was not unexpected, with volcanologists having detected swelling beneath the crater from 14 January 2023. A two kilometre exclusion zone was put in place around the crater as a precaution against pyroclastic flows.

An eruption on Mount Sakurajima, Japan, on 8 February 2023. Kyodo News Agency.

Japan has a complex tectonic situation, with parts of the country on four different tectonic plates. Kyūshū Island lies at the northeast end of the Ryukyu Island Arc, which sits on top of the boundary between the Eurasian and Philippine Plates. The Philippine Plate is being subducted beneath the Eurasian Plate, in the Ryukyo Trench, to the Southeast of the Islands. As it is drawn into the interior of the Earth, the tectonic plate is partially melted by the heat of the Earth's interior, and liquid magma rises up through the overlying Eurasian Plate to form the volcanoes of the Ryukyu Islands and Kyūshū.

The movement of the Pacific and Philippine Plates beneath eastern Honshu. Laurent Jolivet/Institut des Sciences de la Terre d'Orléans/Sciences de la Terre et de l'Environnement.

See also...

Follow Sciency Thoughts on Facebook.

Follow Sciency Thoughts on Twitter


Sunday, 7 June 2020

Enchiridium daidai: A giant Polycladid Flatworm from southwest Japan.

Polycladids are a diverse group of marine Flatworms (Bilateran Worms which lack a body cavity) found from litoral (tidal) environments to deep sea hydrothermal vents, though they are most numerous and diverse around Coral Reefs. They typically range from about 3-20 mm in length, with a flattened oval bodyshape, and often have paired tentacles at their front ends. Members of the Family Prosthiostomidae are characterised by (i) an elongated body with a ventral sucker after the female gonopore, (ii) a plicate tubular pharynx, and (iii) paired prostatic ducts, each of which extends from a spherical prostatic vesicle and enters the penis or the ejaculatory duct independently, instead of uniting to each other before the entrance. The Prosthiostomidae is composed of five genera: Enchiridium, Enterogonimus, Euprosthiostomum, Lurymare, and Prosthiostomum. The genus Enchiridium is distinguished from other Prosthiostomids by having a muscle sheath (or bulb) that encloses just the two prostatic vesicles among other male reproductive organs; i.e., the seminal vesicle and the male atrium are not enclosed by the muscle sheath.

In a paper published in the journal ZooKeys on 12 March 2020, Aoi Tsuyuki of the Graduate School of Science at Hokkaido University and Hiroshi Kajihara of the Faculty of Science at Hokkaido University, describe a new species of Enchiridium from Kagoshima and Okinawa.

Three Polyclad specimens were collected subtidally from under rocks on the coast of Bonomisaki in Kagoshima Prefecture and the coast of Nago on Okinawa Island, southwestern Japan. Worms were anaesthetised in seawater containing menthol before fixation. The relaxed worms were photographed with a Nikon D5600 digital camera with external strobe lighting provided by a pair of Morris Hikaru Komachi Di flash units. For DNA extraction, a posterior piece of the body was removed and stored in 99.5% ethanol. The rest of the body was fixed in Bouin’s solution for 24 hours and preserved in 70% ethanol for long-term storage.

Map showing distribution of Enchiridium daidai: point (A) off the coast of Bonomisaki, Kagoshima (type locality); point (B) Nago, Okinawa Island. Tsuyuki & Kajohara (2020).

The new species is named Enchiridium daidai, where 'daidai' means 'orange', in reference to a thin marginal orange line surrounding the entire dorsal fringe. The species is described from three specimens, all collected by Aoi Tsuyuki. One was collected at 13–14 m depth off the coast of Bonomisaki in Kagoshima Prefecture, and the other two were both collected at 5 m depth at Nago on Okinawa Island.

Enchiridium daidai, photograph taken in life and eyespots observed in fixed state after being cleared in xylene. Entire animal, dorsal view (left) and ventral view (right). Abbreviations: fg, female gonopore; mg, male gonopore; op, oral pore; ph, pharynx; su, sucker. Scale bar is 10 mm. Tsuyuki & Kajohara (2020).

The body of Enchiridium daidai is elongate, tapered posteriorly, 28–77 mm long (77 mm in the holotype) and 4.6–14 mm maximum width (14 mm in the holotype) in the living state; the anterior margin is rounded; the mid-point of the posterior margin is acute. Tentacles are absent. The dorsal surface is smooth, translucent, and fringed with a thin marginal orange line. The ventral surface is translucent, without colour pattern. A pair of cerebral-eyespot clusters is present, each consisting of 20–52 eyespots (left 20 and right 23 in holotype); each cluster is of an antero-posteriorly elongated spindle shape. Marginal-eyespot clusters form a single marginal band, extending to position of mouth (about anterior one-eighth of the body length) along margins on both sides; marginal eyespots are abundant along the anterior margin, diminishing posteriorly. Ventral eyespots are absent. The intestine is highly branched, spreading all over body. A plicated pharynx is tubular in shape, about one-fifth of the body length, and located in the anterior one-third of the body. The oral pore is situated at the anterior end of the pharynx, behind the brain. The Male gonopore and female gonopore are closely set, both situated behind the posterior end of pharynx. The male copulatory apparatus consists of a large seminal vesicle, a pair of prostatic vesicles, and an armed penis papilla. The antero-posterior length of  the seminal vesicle is more than twice as long as the diameter of each prostatic vesicle. Spermiducal vesicles form a single row on each side of the midline, separately entering into seminal vesicle. An ejaculatory duct with a thick muscular layer, enters the penis papilla. Prostatic ducts with muscular layer are connected to the ejaculatory duct separately at the proximal end of penis papilla. A pair of spherical prostatic vesicles is coated within thin non-nucleated muscular wall, arranged anterodorsally to the ejaculatory duct. A common muscular sheath encloses the two prostatic vesicles. The seminal vesicle is oval, coated with a thick muscular wall, narrowing anteriorly and forming the ejaculatory duct; the latter almost immediately penetrating the common muscular sheath. The penis papilla is armed with a pointed tubular stylet, enclosed in a penis pouch, and protrudes into the male atrium. The male atrium is elongated anteriorly, and lined with a ciliated, muscularised epithelium. The female reproductive system is immediately posterior to the male reproductive system. Cement glands are numerous, concentrated around the vagina and release their contents into a cement pouch. The vagina curves anteriorly, leading to two narrow lateral branches of uteri. Each branch of uteri turns laterally and then runs backwards. The Lang’s vesicle is absent. A sucker is set on the body centre.

The specimens from Kagoshima and Okinawa differed in body size. The holotype from Kagoshima was 77 mm long and 15 mm wide, whereas the paratype specimens from Okinawa were 28–37 mm long and 4.6–7.4 mm wide. In spite of the noticeable difference in body size, specimens from Kagoshima and Okinawa, all having reached sexual maturity, were identified as conspecific. They shared the following morphological characteristics: (i) a body dorsally fringed with a thin orange line, (ii) a marginal-eyespot band extending to the position of the mouth (about anterior one-eighth of the body), (iii) two prostatic vesicles covered by a common muscle sheath, and (iv) common muscle sheath penetrated by ejaculatory duct. In addition the proportion of nucleotide sites at which two sequences being compared were different was very low, indicative of being the same species.

Difference in mature body size among Enchiridium daidai. (A) ICHUM 5993 (holotype), from Kagoshima, (B) ICHUM 5995 (paratype), from Okinawa, (C) ICHUM 5994 (paratype), from Okinawa. Scale bar 10 mm. Tsuyuki & Kajohara (2020).

Reaching 77 mm in body length, Enchiridium daidai is the largest species in the genus, superseding Enchiridium punctatum (about 40 mm in body length). Indeed, Enchiridium daidai is the second largest species in the Prosthiostomidae after Prosthiostomum cyclops, which reaches 90 mm. Among about 80 species of Prosthiostomids, only Enchiridium daidai and Prosthiostomum cyclops are known to exceed 70 mm in body length, while most of the other species are less than 30 mm long. Therefore, Tsuyuki & Kajohira's new species is considered to be unusually big in body size for a Prosthiostomid.

See also...

https://sciencythoughts.blogspot.com/2020/03/temnocephala-ivandarioi-new-species-of.htmlhttps://sciencythoughts.blogspot.com/2019/01/difroehlichia-elenae-new-species-of.html
https://sciencythoughts.blogspot.com/2018/01/xenoturbella-japonica-new-species-of.htmlhttps://sciencythoughts.blogspot.com/2016/08/cratera-viridimaculata-new-species-of.html
https://sciencythoughts.blogspot.com/2015/03/a-trematode-flatworm-from-intestines-of.htmlhttps://sciencythoughts.blogspot.com/2014/07/a-new-species-of-liver-fluke-from.html
 
 
 
 
 
 
 
 
Follow Sciency Thoughts on Facebook.

Sunday, 3 November 2019

Eruption on Iōjima Island, Japan.

The Kikai Volcano on Iōjima Island in Japan's Kagoshima Prefecture erupted at about 5.35 pm on Saturday 2 November 2019, producing an ash column over a kilometre in height. Nobody is thought to have been injured by the event, as the island is only sparsely populated, but the Japan Meteorological Agency has raised the alert level around the volcano, warning people not to approach within a kilometre of the summit in case of flying rocks or pyroclastic flows.

 Eruption on Iōjima Volcano, Japan, on 2 November 2019. Sify News.

Iōjima is a 5 km long volcanic island that forms the exposed tip of the much larger, but mostly submerged, Kikai Volcano, with a maximum elevation of about 700 m above sea level. The island is thought to be a remnant of a much larger volcanic complex destroyed in a huge eruption about 6300 years ago, that caused devastation across much of southern Kyushu.

The approximate location of Iōjima Island. Google Maps.

Iōjima lies at the northeast end of the Ryukyu Island Arc, which sits on top of the boundary between the Eurasian and Philippine Plates. The Philippine Plate is being subducted beneath the Eurasian Plate, in the Ryukyo Trench, to the Southeast of the Islands. As it is drawn into the interior of the Earth, the tectonic plate is partially melted by the heat of the Earth's interior, and liquid magma rises up through the overlying Eurasian Plate to form the volcanoes of the Ryukyu Islands and Kyūshū.

 The movement of the Pacific and Philippine Plates beneath Japan. Laurent Jolivet/Institut des Sciences de la Terre d'Orléans/Sciences de la Terre et de l'Environnement.

See also...

https://sciencythoughts.blogspot.com/2019/01/eruption-on-mount-shindake-kuchinoerabu.htmlhttps://sciencythoughts.blogspot.com/2015/06/kuchinoerabu-island-evacuated-following.html
https://sciencythoughts.blogspot.com/2014/08/eruptionand-pyroclastic-flow-on-mount.htmlhttps://sciencythoughts.blogspot.com/2013/08/eruptions-on-sakurajima.html
https://sciencythoughts.blogspot.com/2013/07/eruption-on-suwanosejima.htmlhttps://sciencythoughts.blogspot.com/2012/02/mapping-subductioin-zone-beneath-taiwan.html
 
 
 
 
 
Follow Sciency Thoughts on Facebook.

Wednesday, 28 February 2018

Antipathozoanthus obscurus, Antipathozoanthus remengesaui, & Antipathozoanthus cavernus: Three new species of Parazoanthid Soft Coral from the Indo-Pacific region.

Parazoanthid Corals are colony forming Soft Corals noted for their tendency to grow on other benthic filter feeding animals, typically Sponges but sometimes Corals or other organisms, a form of facultative parasitism in which the Parazoanthid benefits from currents generated by the larger organism, while at the same time covering part of its surface, reducing the host’s ability to feed itself. Parazoanthids usually lack symbiotic Algae, and inhabit dark environments such as marine caves and deep sea cold seeps, where there are few predators, but also little food and limited natural currents, and thereby rely on their host’s ability to generate a current to survive.

In a paper published in the journal ZooKeys on 29 December 2017, Hiroki Kise of the Molecular Invertebrate Systematics and Ecology Laboratory at the University of the Ryukyus, and the Palau International Coral Reef Center, Takuma Fujii, also of the Molecular Invertebrate Systematics and Ecology Laboratory at the University of the Ryukyus, and of the Research Center for Island Studies Amami Station of Kagoshima University, Giovanni Diego Masucci and Piera Biondi, again of the Molecular Invertebrate Systematics and Ecology Laboratory at the University of the Ryukyus, and James Davis Reimer, once again of the Molecular Invertebrate Systematics and Ecology Laboratory at the University of the Ryukyus, and the Palau International Coral Reef Center, and of the Tropical Biosphere Research Center of the University of the Ryukyus, describe three new species of Parazoanthid Soft Coral from the Indo-Pacific region. All are placed in the genus Antipathozoanthus, which gets its name from its habit of overgrowing Antipatharian (Black) Corals.

The first new species described is given the name Antipathozoanthus obscurus, meaning ‘dark’ in reference to the dark environments in which it was found. The species was found in caves and crevices on reefs at depths of between 3 and 15 m, and, unusually, grew on a rocky, non-living substrate, where it was possibly able to survive due to strong currents generated by tidal action, which may have carried planktonic food into the caves. Polyps of this species reach 5-10 mm in height, with an oral disk that opens to a similar size in diameter, and have between 26 and 32 brown or orange tentacles. These polyps are connected by stolons which form a mesh-like network. The whole is covered by an encrustation of sand and other particles up to 8 mm in size. The species was found in the Okinawa Islands of Japan, and around Al Wajh Shaybarah on the Red Sea Coast of Saudi Arabia, which suggests a far wider distribution, probably encompassing the entire Indian Ocean and Western Pacific, and possibly further afield. 

Specimen of Antipathozoanthus obscurus. Collected from Cape Bise, Motobu, Okinawajima Island, Japan (26°42'34.4"N, 127°52'49.2"E) at a depth of 5 m by James Davis Reimer. Kise et al. (2017).

The second species described is named Antipathozoanthus remengesaui, in honour of Tommy Esang Remengesau, Jr., the current president of the Republic of Palau, for his support of marine research and conservation in Palau. This species was found growing on colonies of Corals of the genus Antipathes growing around the entrances to caves at depths of between 9 and 40 m, at Kagoshima (Japan) and Palau in the Pacific Ocean, in the Maldives in the Indian Ocean and around Al Wajh Shaybarah on the Red Sea Coast of Saudi Arabia. Polyps of this species are white in colour and reach 3-8 mm in height, with oral disks up to 8 mm in diameter, surrounded by 40-42 pinkish, translucent tentacles up to 4 mm in length. These polyps are solitary, or only weakly connected by a poorly developed coenenchyma. This species also tends to develop a coating of sand particles, though these tend to be smaller, at 1-3 mm.

Antipathozoanthus remengesaui, colony connected by poorly developed coenenchyma with white polyps on Antipathes sp., collected from Blue Hole, Palau (7°8'29.4"N, 134°13'23.3"E) at a depth of 23 m by James Davis Reimer. Kise et al. (2017).

The final species described is named Antipathozoanthus cavernus, in reference to its habit of living in caves. This species was found growing on colonies of the Coral Myripathes around cave entrances and on steep slopes at depths of between 19 and 39 m in Kagoshima and the Maldives. Polyps of this species reach 3-10 mm in height and have an orange oral disk 4-15 mm in diameter, surrounded by 32-40 translucent tentacles up to 5 mm in length. The polyps are connected by a highly developed coenenchyma, and again the colony is coated in sand and other particles 1-8 mm in size. 

Antipathozoanthus cavernus polyps connected by highly developed coenenchyme with orange ring around oral disk, collected from Siaes Tunnel, Palau (7°18'54.8"N, 134°13'13.3"E) at a depth of 39 m by James Davis Reimer. Kise et al. (2017).

See also...

http://sciencythoughts.blogspot.co.uk/2018/01/charting-long-term-coral-decline-in.htmlhttp://sciencythoughts.blogspot.co.uk/2018/01/porites-australiensis-exceptionally.html
http://sciencythoughts.blogspot.co.uk/2017/12/terpios-hoshinota-tracking-progress-of.htmlhttp://sciencythoughts.blogspot.co.uk/2017/09/looking-for-animals-in-wengan-biota.html
http://sciencythoughts.blogspot.co.uk/2017/04/flagelligorgia-gracilis-new-species-of.htmlhttp://sciencythoughts.blogspot.co.uk/2016/06/sclerangia-floridana-new-species-of.html
Follow Sciency Thoughts on Facebook.

Tuesday, 30 September 2014

A new species of parasitic Orchid from Takeshima Island, Japan.

Orchids of the genus Gastrodia are found across temperate and tropical Asia, Oceania and Madagascar. They are mycoheterotrophs; parasitic plants which obtain nutrients and sugars from Mycorrhizal Fungi (Fungi which normally form symbiotic relationships with plants).  They are a diverse group with over fifty species ranging in size from under five to over 100 cm.

In a paper published in the journal Phytotaxa on 5 August 2014, Kenji Suetsugu of the Graduate School of Human and Environmental Studies at Kyoto University describes a new species of Gastrodia from Takashima Island, off the coast of Kagoshima Prefecture on Kyushu Island, Japan.

The new species is named Gastrodia flexistyloides, though no explanation is given for this name. It is a 9-18 cm leafless Orchid, brown in colour with brown flowers with white spots and a tuberous rhizome (i.e. a tuberous root that can persist below ground outside the growing season and regrow into a new plant when conditions are favourable). The flowers do not open, the plant apparently reproducing entirely by self-fertilisation. Flowers are produced in mid-March to early April, seeds are contained within fruit produced from early April to early May. Gastrodia flexistyloides was found living in Bamboo forests.

Flowering plant of Gastrodia flexistyloides. Scale bar is 2 cm. Suetsugu (2014).

See also…

http://sciencythoughts.blogspot.co.uk/2014/06/the-freckled-cypripedium-classified-as.html The Freckled Cypripedium classified as Endangered.                                                 The International Union for the Conservation of Nature published its annual update of its Red List of Threatened Species on Thursday 12 June 2014, marking the 50th year of the list's existence, and revising the status of a number of Plant and Animal species from around the...
http://sciencythoughts.blogspot.co.uk/2013/10/a-new-species-of-thismia-from-northwest.html A new species of Thismia from northwest Yunnan Province, China.                         Thismias (Thismiaceae) are a small group of Parasitic Plants found throughout the tropics, with a few temperate species known from North America, Japan, New Zealand and Australia. They parasitize the...
http://sciencythoughts.blogspot.co.uk/2012/06/new-species-of-orchid-from-bahia-state.html A new species of Orchid from Bahia State, Brazil.  Orchids of the genus Encyclia are widespread in the American tropics, living as epiphytes (plants that live on other plants, typically on the branches of rainforest trees), terrestrial herbs and on exposed rocks. They are found from Florida to northern Argentina, and live in a wide variety of habitats... 

Follow Sciency Thoughts on Facebook.

Tuesday, 5 August 2014

Eruption and pyroclastic flow on Mount Furudake.

The Japan Meteorological Agency recorded an eruption on Mount Furudake on Kuchinoerabujima, an island about 130 km south of Kagoshima, at about 12.25 pm local time on Sunday 3 August 2014. The eruption consisted of a single powerful explosion followed by the generation of a 1.5 km high ash plume. This ash column lasted for about 10 minutes, then collapsed forming a pyroclastic flow (avalanche of hot gas and ash), but fortunately leading to no injuries or damage. The nearby town of Yakushima has been partially evacuated as a precaution. This is the first eruption on the volcano since 1980.

Pyroclastic flow on Kuchinoerabujima on 3 August 2014. Volcanic News Eruptions.


Japan has a complex tectonic environment with four plates underlying parts of the Islands; the Pacific in the east and the Othorsk in the North, there are the Philipine Plate to the south and the Eurasian Plate to the West. All of these plates are moving in different directions, and some subducting beneath the islands, leaning to a complex tectonic situation where earthquakes and volcanoes are common.

Kuchinoerabujima lies at the northeast end of the Ryukyu Island Arc, which sits on top of the boundary between the Eurasian and Philippine Plates. The Philippine Plate is being subducted beneath the Eurasian Plate, in the Ryukyo Trench, to the Southeast of the Islands. As it is drawn into the interior of the Earth, the tectonic plate is partially melted by the heat of the Earth's interior, and liquid magma rises up through the overlying Eurasian Plate to form the volcanos of the Ryukyu Islands and Kyūshū.

The location of Kuchinoerabujima Island. Google Maps.

See also


On 20 December 2013 the Japan Meteorological Agency detected an increase in seismic activity beneath Aso (or Asosan) a volcanic caldera on central Kyūshū Island, Japan. This grew steadily for the next week, prompting the agency to raise the alert level on the...



The Sakurajima Volcano, situated on an island in Kagoshima Bay, Kyushu, underwent a large explosive eruption on the morning of Friday 4 October 2013, producing a 4 km high ash column and...



On 9 August 2013 the Japan Meteorological Agency reported a 50 minute eruption on Sakurajima Volcano, which is one of Japan's most active and sits on an island in Kagoshima Bay, Kyushu Island, which produced a 3.5 km high ash column, as well as throwing...


Follow Sciency Thoughts on Facebook.

Saturday, 5 October 2013

Eruption and pyroclastic flow on Sakurajima, Kyushu.

The Sakurajima Volcano, situated on an island in Kagoshima Bay, Kyushu, underwent a large explosive eruption on the morning of Friday 4 October 2013, producing a 4 km high ash column and triggering a pyroclastic flow (avalanche of hot gas and ash) on the mountain's northwest flank. This was the third such eruption so far in October this year. The volcano is currently undergoing a particularly eruptive phase, and has undergone several hundred explosive eruptions so far this year (the exact figure is hard to derive as eruptions often occur close together and may run into one another).

Webcam image of Sakurajima on the morning of 4 October 2013, taken from the east. MBC.

Japan has a complex tectonic environment with four plates underlying parts of the Islands; in addition to the Pacific in the east and the Othorsk in the North, there are the Philipine Plate to the south and the Eurasian Plate to the West. Kyushu Island lies at the northeast end of the Ryukyu Island Arc, which sits on top of the boundary between the Eurasian and Philippine Plates. The Philippine Plate is being subducted beneath the Eurasian Plate, in the Ryukyo Trench, to the Southeast of the Islands. As it is drawn into the interior of the Earth, the tectonic plate is partially melted by the heat of the Earth's interior, and liquid magma rises up through the overlying Eurasian Plate to form the volcanos of the Ryukyu Islands and Kyushu.

The location of Mount Sakurajima on Kagoshima Island in Kagoshima Bay on the southern tip of Kyushu Island, Japan. Google Maps.


Follow Sciency Thoughts on Facebook.

Tuesday, 20 August 2013

Japanese city covered in ash by eruption on Sakurajima Volcano.

An eruption on Sakurajima Volcano, situated on an island in Kagoshima Bay, Kyushu, has coated the city of Kagoshima in a layer of ash. The eruption, which occurred in the afternoon of Monday 19 March 2013, from the Showa vent on the side of the volcano rather than the main caldera, and produced a 5 km high column of ash and smoke. This is the tallest ash column ever produced by the vent, but is not being taken as cause for alarm locally, as the volcano frequently undergoes larger events. The ashfall covering the city has been blamed on a lack of wind, which usually blows such ash away from the city, rather than exceptional volcanic activity on Sakurajima, which is one of Japan's most active volcanoes. Local press are describing this as the 500th event this year, though with such frequent eruptions this is hard to evaluate since eruptions often merge or overlap and it is difficult to say where one ends and the next starts.

Ash column from Sakurajima over the city of Kagoshima on Kyushu Island on Monday 19 August 2013. AP/Reuters.

Japan has a complex tectonic environment with four plates underlying parts of the Islands; in addition to the Pacific in the east and the Othorsk in the North, there are the Philipine Plate to the south and the Eurasian Plate to the West. Kyushu Island lies at the northeast end of the Ryukyu Island Arc, which sits on top of the boundary between the Eurasian and Philippine Plates. The Philippine Plate is being subducted beneath the Eurasian Plate, in the Ryukyo Trench, to the Southeast of the Islands. As it is drawn into the interior of the Earth, the tectonic plate is partially melted by the heat of the Earth's interior, and liquid magma rises up through the overlying Eurasian Plate to form the volcanos of the Ryukyu Islands and Kyushu.


Follow Sciency Thoughts on Facebook.