Showing posts with label Rota Island. Show all posts
Showing posts with label Rota Island. Show all posts

Monday, 24 May 2021

Partula lutaensis: A new species of Partulid Tree Snail from Rota Island, in the the Mariana Archipelago.

Partulid Tree Snails are found across the islands of the tropical Pacific, reaching their maximum diversity towards the eastern end of their range, with the genus Partula reaching its highest diversity in the Society Islands, and the genus Samoana reaching maximum diversity in the Samoan Islands, although it is thought that these Snails originated further to the west. The Mariana Archipelago is a crescent-shaped chain of 15 volcanic islands extending roughly 2520 km from Farallon De Pajeros in the north to Guam in the south. These islands were long thought to be home to six species of Partulid Snails. Partula radiolata and Partula salifana were known only from Guam, Partula desolata, described from sub-fossil shells and probably extinct was known only from Rota, Partula langfordi was known only from Aguigan, and may also now be extinct, Samoana fragilis was known from both Guam and Rota, and Partula gibba known from seven islands, from Guam, in the south, to Pagan Island in the north.

In 2017 David Sischo of the US Department of Land and Natural Resources and the Pacific Biosciences Research Center at the University of Hawai‘i at Mānoa, and Michael Hadfield, also of the Pacific Biosciences Research Center at the University of Hawai‘i at Mānoa, published a paper in the Biological Journal of the Linnean Society, which described the results of a generic study of Partula gibba, which concluded that the population of this Snail on Rota Island is in fact genetically distinct, and represents a new, cryptic species which had not previously been identified.

 
Map of the Mariana Islands. Islands where partulids were sampled are indicated by stars. Sischo & Hadfield (2017).

In a second paper, published in the journal ZooKeys on 17 May 2021, David Sischo and Michael Hadfield formerly describe the new Tree Snail species as Partula lutaensis, which combines 'Luta', the indigenous Chamorro name for the island of Rota, and the suffix '-ensis' implies coming from.

The shell of Partula lutaensis is dextral, moderately thin, ovate-to-conic, and slightly perforate. The umbilicus is open, the whorls are moderately convex, and the suture is adpressed. The aperture is ovate-to-elongate, and slightly oblique. The outer lip is reflexed, thick, and glossy, the parietal lip glossy with light or dark colouration. The colour of embryonic the whorls and post-embryonic whorls is variable from shades of brown, buff, white and yellow with a prominent white subsutural band. The 48 specimens measured had an average height of 15.98 mm, and an average width of 10.64 mm.

 
(Left) Colour morphs of Partula lutaensis found within a 10 × 10-meter quadrat. (Right) Closeup of a Partula lutaensis with a dark shell. Sischo & Hadfield (2021).

All of the known specimens of Partula lutaensis were collected from two species of Plant, the Devil's Ivy, Epiprenmum aureum, and the Halberd Fern, Tectaria crenata. The species is currently present at fairly high densities on Rota Island, however other species of Partulid Snails in the Mariana Archipelago have gone from relative abundance to near-or-actual extinction in very short periods of time, largely due to the activities of introduced predators; a pattern that has been repeated on islands across the Pacific. Particularly troublesome for Partulid Snails are North American carnivorous Snail species in the genus Euglandina, and the New Guinea Flatworm, Platydemus manokwari. On Rota Island Platydemus manokwari has been observed predating Partula lutaensis, suggesting that this species is at risk. Partula gibba, the species to which these Snails were formerly assigned, is protected by a federal Endangered Species declaration, but this will not automatically transfer to the new species, for which reason Sischo and Hadfield consider it imperative that Partula lutaensis be listed as Endangered as soon as possible.

 
A Partula lutaensis freshly depredated by Platydemus manokwari observed on Rota. Sischo & Hadfield (2021).

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Monday, 21 October 2019

Magnitude 5.2 Earthquake to the southeast of Rota Island, Northern Mariana Islands.

The United States Geological Survey recorded a Magnitude 5.2 Earthquake at a depth of 94.1 km about 27 km off the southeast coast of the Rota Island, a US possession in the Northern Mariana Islands, slightly after 10.40 pm local time (slightly after 12.40 pm GMT) on Saturday 19 October 2019. There are no reports of any casualties this event, though it was felt across the Northern Marianas Islands and Guam.

The approximate location of the 19 September 2019 Rota Island Earthquake. USGS.

The volcanic Mariana Islands are located on the eastern margin of the Philippine Plate, close to its margin with the Pacific Plate. The Pacific Plate is being subducted beneath the Philippine Plate along the Mariana Trench. This is not a smooth process, an the plates constantly stick together then break apart again as the pressure builds up, resulting in Earthquakes.
 
 Simplified diagram of the subduction of the Pacific Plate beneath the Philippine plate, and how this fuels the volcanoes of the Mariana Islands. NOAA Ocean Explorer.
 
Witness accounts of quakes can help geologists to understand these events and the rock structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) you can report it to the USGS here.
 
See also...
 
https://sciencythoughts.blogspot.com/2019/06/magnitude-45-earthquake-to-north-of.htmlhttps://sciencythoughts.blogspot.com/2018/10/typhoon-yutu-kills-at-least-one-and.html
https://sciencythoughts.blogspot.com/2017/05/magnitude-54-earthquake-off-northeast.htmlhttps://sciencythoughts.blogspot.com/2017/02/persistent-organic-pollutants-in.html
http://sciencythoughts.blogspot.com/2014/04/japanese-volcanic-islands-merge.htmlhttp://sciencythoughts.blogspot.com/2013/11/volcano-creates-new-island-in-west.html
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Friday, 26 October 2018

Typhoon Yutu kills at least one and causes widespread devastation in the Northern Mariana Islands.

The Northern Mariana Islands, a Commonwealth of the United States in the Pacific Ocean, has suffered severe damage to infrastructure after Typhoon Yutu swept across the two main islands of Saipan and Tinian on Wednesday 24 October 2018. The island of Saipan has reportedly lost all electricity and mains water supplies, but remains in telephone contact with the outside world, with one person reported dead. The islands of Tinian and Rota have not been contacted since the storm passed, and the extent of the damage there is unclear.

The remains of a house on Saipan Island, Northern Marianas, destroyed during the passage of Typhoon Yutu this week. Glen Hunter/AP.

The storm was a Category 5 Typhoon when it hit the islands, bringing with it sustained wind speeds (wind speeds maintained for a minute or more) in excess of 290 kilometres per hour. The storm is reported to have caused widespread flooding, with a large storm surge hitting the islands, and to have triggered a number of landslides. Landslides are a common problem after severe weather events, as excess pore water pressure can overcome cohesion in soil and sediments, allowing them to flow like liquids. Approximately 90% of all landslides are caused by heavy rainfall. The storm is currently sweeping towards the Philippines and Taiwan, where it is expected to cause further problems.

The path and strength of Typhoon Yutu. Thick line indicates the past path of the storm (till 6.00 am GMT on Saturday 26 October 2018), while the thin line indicates the predicted future path of the storm, and the dotted circles the margin of error at 12, 24, 36, 72, 96, and 120 hours ahead. Colour indicated the severity of the storm. Tropical Storm Risk.

Tropical storms are caused by the warming effect of the Sun over tropical seas. As the air warms it expands, causing a drop in air pressure, and rises, causing air from outside the area to rush in to replace it. If this happens over a sufficiently wide area then the inrushing winds will be affected by centrifugal forces caused by the Earth's rotation (the Coriolis effect). This means that winds will be deflected clockwise in the northern hemisphere and anti-clockwise in the southern hemisphere, eventually creating a large, rotating Tropical Storm. They have different names in different parts of the world, with those in the north Pacific being referred to as typhoons.

Damage on the island of Tainan in the Northern Marianas before contact with the island was lost. Office of the Mayor of Tainan and Aguiguan/Reuters.

Despite the obvious danger of winds of this speed, which can physically blow people, and other large objects, away as well as damaging buildings and uprooting trees, the real danger from these storms comes from the flooding they bring. Each drop millibar drop in air-pressure leads to an approximate 1 cm rise in sea level, with big tropical storms capable of causing a storm surge of several meters. This is always accompanied by heavy rainfall, since warm air over the ocean leads to evaporation of sea water, which is then carried with the storm. These combined often lead to catastrophic flooding in areas hit by tropical storms.

See also...

https://sciencythoughts.blogspot.com/2017/05/magnitude-54-earthquake-off-northeast.htmlhttp://sciencythoughts.blogspot.co.uk/2012/07/eruption-on-pagan-island.html
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