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

Saturday, 28 December 2019

Human remains found inside Shark caught off Réunion Island identified.

A set of partial Human remains found inside a 3.4 m Tiger Shark, Galeocerdo cuvier, caught off the coast of La Réunion, an island in the western Indian Ocean which is a department of France, on Thursday 26 December 2019, have been identified. The remains comprised a pair of arms plus an item of jewelry, which has been identified as having belonged to an elderly kayaker who went missing off the island on 12 December. The shark was caught as part of a research program studying the feeding behaviour of the Sharks, following a number of attacks on Humans around La Réunion. This is the third Shark-related fatality recorded around the island this year.

A Tiger Shark, Galeocerdo cuvier, in the Western Indian Ocean. Thomas Peschak/Save Our Seas Foundation.

Despite their fearsome reputation, attacks by Sharks are relatively rare and most attacks on Humans by Sharks are thought to be mistakes. Tiger Sharks have a diverse diet, including invertebrates, Fish, Birds, Marine Reptiles and Marine Mammals, which we superficially resemble when we enter the water. Marine Mammals are attacked principally for their thick adipose (fat) layers, which are a nutritious high-energy food, but which we lack. Due to this, when Sharks do attack Humans these attacks are often broken off without the victim being consumed. Such attacks frequently result in severe injuries, but are seldom immediately fatal, and victims are likely to survive if they receive immediate medical attention.

See also...

https://sciencythoughts.blogspot.com/2019/11/two-english-tourists-injured-in-shark.htmlhttps://sciencythoughts.blogspot.com/2019/10/tourist-badly-imjured-in-shark-attack.html
https://sciencythoughts.blogspot.com/2019/08/sharks-and-rays-from-eocene-of.htmlhttps://sciencythoughts.blogspot.com/2019/06/mollisquama-mississippiensis-new.html
https://sciencythoughts.blogspot.com/2019/06/american-tourist-killed-in-shark-attack.htmlhttps://sciencythoughts.blogspot.com/2019/06/icelandic-fishermen-fired-for-cruelty.html
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Friday, 22 February 2019

Eruptions from new fissure on Piton de la Fournaise.

The Observatoire Volcanologique du Piton de la Fournaise reported sharp increase in seismic activity beneath Piton de la Fournaise, a shield volcano which forms much of the eastern part of Réunion Island, an island in the western Indian Ocean which forms a department of France, starting slightly after 3.20 pm on Saturday 16 February 2019, and persisting for slightly over an hour. This resumed slightly after 9.15 am on Monday 18 February, and was accompanied by rapid deformation on the eastern flank of the volcano, and eventually the opening of a fissure on that flank from which a lava fountain emerged, reaching heights of about 30 m, and resulting in a lava flow that reached about 1900 m down the flank of the volcano. This continued until about 10.00 pm. Further earthquakes and gas emissions were recorded on 19 February, and on the 20th an overflight by vulcanologists from the Observatoire Volcanologique du Piton de la Fournaise recorded another fissure on the eastern flank.

A lava flow on the eastern flank of Piton de la Fournaise on 20 February 2019. Le Chaundron de Vulcan.

Piton de la Fournaise is believed to have been active for about 530 000 years, though its geology is complicated to unravel as lava flows are interbedded with those from Piton des Neiges, a larger, older and now extinct volcano to the northwest, which is responsible for the formation of about two thirds of the island. The island sits on the Réunion Hotspot, a deep mantle plume which is thought to have been active for about 66 million years, originally forming under what is now northeastern India, where it was responsible for the Deccan Traps flood basalts, then moving southward across the Indian Ocean (or more precisely sitting still while the continental plate upon which India and the Indian Ocean sit moves to the north), over time forming the Laccadive Islands, the Maldives, the Seychelles, Rodrigues Island, Mauritius and Réunion.

See also...

https://sciencythoughts.blogspot.com/2018/04/eruption-on-piton-de-la-fournaise.htmlhttp://sciencythoughts.blogspot.co.uk/2018/04/volcanic-activity-on-reunion-island.html
http://sciencythoughts.blogspot.co.uk/2017/01/magnitude-55-earthquake-in-central.htmlhttp://sciencythoughts.blogspot.co.uk/2015/05/eruptions-on-piton-de-la-fournaise.html
http://sciencythoughts.blogspot.co.uk/2015/02/eruptions-on-piton-de-la-fournaise.htmlhttp://sciencythoughts.blogspot.co.uk/2014/01/fifteen-injured-as-cyclone-bejisa.html
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Saturday, 4 February 2017

Understanding the origins of the Giant Tortoises of the southwest Indian Ocean.

Giant Tortoises were once numerous on both continental and island landmasses, though most of the continental species became extinct in the Late Pleistocene and most of the island species in the Holocene, all of which extinctions have been linked to a single cause, the spread of Modern Humans around the globe. Today only two species of Giant Turtle remain, Chelonoidis nigra in the Galapagos and Aldabrachelys gigantean on Aldabra Island, a small coral atoll in the Indian Ocean, about 400 km north of Madagascar and about 600 km west of the east coast of Africa. The southwest Indian Ocean was formerly somewhat of a hotspot for Giant Tortoise diversity, with at least two species on Madagascar, plus two species on Mauritius, two species on Rodrigues and one on La Réunion.

An Aldabra Giant Tortoise, Aldabrachelys gigantean. Wikipedia.

How the Tortoises got to these islands is somewhat of a mystery; the ancestors of the Giant Tortoises of Madagascar presumably reached there while Madagascar was still attached to the Gondwanan supercontinent in the Cretaceous, or floating there from Africa in the Eocene or earlier, when prevalent currents in the southwest Indian Ocean ran from Africa towards Madagascar (Giant Tortoises seldom voluntarily swim, but float well and can survive long periods at sea, so Tortoises swept out to sea by, for example, flood events, have a reasonable chance of surviving till they reach a new landmass). However from the end of the Eocene onwards, prevalent currents in the southern Indian Ocean have all flowed east-to-west, making it highly unlikely that a Tortoise could drift from island to island in this direction without swimming hundreds of kilometres against the current. This makes the presence of Tortoises on smaller Indian Ocean islands hard to understand, as all of these islands have appeared since the end of the Eocene; Mauritius having first appeared about 8.9 million years ago, La Réunion about 2.2 million years ago and Rodrigues about 1.5 million years ago, while Aldabra, with a highest point only eight meters above sea level, has emerged from and been covered by the sea several times during the past million years, and is thought to have been continuously exposed only for the last 80 000 years.

In a paper published in the Journal of Biogeography on 11 March 2016, Lucienne Wilmé of the School of Agronomy at the University of Antananarivo, and the Missouri Botanical Garden's Madagascar Research & Conservation Program, Patrick Waeber of Forest Management and Development at the Swiss Federal Institute of Technology Zurich, and Joerg Ganzhorn of Animal Ecology and Conservation at Hamburg University, discuss the possibility that Giant Tortoises may have reached the islands of the southwest Indian Ocean not by drifting on ocean currents, but by active movement by Humans.

The earliest Humans arrived on Madagascar about 4000 years ago. These were fairly advanced, already having metal tools, and are thought to have come from Southeast Asia, with subsequent waves of arrivals from Arabia, Africa and eventually Europe. People from Southeast Asia began making ocean-crossing journeys about 45 000 years ago, hopping from island-to-island to reach remote parts of the Indian and Pacific Oceans, as well as the continent of Australia, and possibly South America.

During this process they introduced many animals and plants to the islands they visited, such as Pacific Rat, Rattus exulans, Chicken, Gallus gallus, Sweet Potato, Ipomea batatas, Taro, Colocasia sp., and Banana, Musa sp.. Giant Tortoises have been considered to be excellent eating by most cultures that have encountered them (most species being wiped out by encounters with hungry European sailors in the eighteenth and nineteenth centuries). It is not, therefore, an outlandish idea that early navigators might, having encountered Giant Tortoises on Madagascar, have moved small populations to other islands in the Indian Ocean as a potential food source, either for colonists living permanently on the islands or for other sailors visiting the islands (European sailors introduced Sheep and Goats to many small islands for similar reasons).

Giant land tortoises, geology, oceanography, archaeology of the south-western Indian Ocean, and distance between islands and ocean surface currents prevailing since the closure of the Tethys Ocean. (SdM = Saya de Malha; N = Nazareth; StB = St Brandon; LGM = Last Glacial Maximum). Wilmé et al. (2016).

Wilmé et al. note that no ancient archaeological sites have been found on the Mascarine Islands (Mauritius, Rodrigues and La Réunion), which would seem to present a problem to this theory. However they note that sealevels have varied considerably over the past few thousand years, which has a particularly strong effect on small islands, so that it is quite possible ancient coastal settlements around these islands may have been covered by rising seas.

More problematically, the Tortoises of the southwest Indian Ocean are considered to have belonged to eight different species, which seems unlikely if they were all transplanted from Madagascar (where only two species are known). Wilmé et al. do not dispute the current accepted taxonomy of these species, however they do observe that species isolated on small islands are known to evolve rapidly, and that Tortoises, which produce particularly large clutches of young, are potentially more prone to this effect than slower breeding groups such as Birds or Mammals.

See also...

http://sciencythoughts.blogspot.co.uk/2016/10/mendozachelys-wichmanni-new-species-of.htmlhttp://sciencythoughts.blogspot.co.uk/2016/10/paiutemys-tibert-new-species-of.html
http://sciencythoughts.blogspot.co.uk/2015/12/xiaochelys-ningchengensis-sinemydid.htmlhttp://sciencythoughts.blogspot.co.uk/2015/11/turtle-remains-from-late-miocene-to.html
http://sciencythoughts.blogspot.co.uk/2015/10/turtle-eggs-from-late-cretaceous-of.htmlhttp://sciencythoughts.blogspot.co.uk/2015/10/pappochelys-rosinae-proto-turtle-from.html
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Saturday, 12 September 2015

Partial Solar Eclipse to be visible from Southern Africa, Madagascar and Antarctica on 13 September 2015.

A partial Solar Eclipse will occur on Sunday 13 September 2015, visible from all of Namibia, Botswana, South Africa, Lesotho, Swaziland, Zimbabwe and Reunion Island and parts of Angola, Zambia, Mozambique, Madagascar and Antarctica. The eclipse will occur between 4.41 am and 9.06 am GMT.

The area over which the 13 September 2015 partial Solar Eclipse will be visible. Areas in darker grey will be able to observe the entire eclipse, in the lighter grey areas the eclipse will either begin before sunrise or end after sunset, so only part of the event will be visible. HMNautical Almanac Office.

Eclipses are a product of the way the Earth, Moon and Sun move about one-another. The Moon orbits the Earth every 28 days, while the Earth orbits the Sun every 365 days, and because the two Sun and Moon appear roughly the same size when seen from Earth, it is quite possible for the Moon to block out the light of the Sun. At first sight this would seem likely to happen every month at the New Moon, when the Moon is on the same side of the Earth as the Sun, and therefore invisible (the Moon produced no light of its own, when we see the Moon we are seeing reflected sunlight, but this can only happen when we can see parts of the Moon illuminated by the Sun). 

The relative positions of the Sun, Moon and Earth during a Solar eclipse. Starry Night.

However the Moon does not orbit in quite the same plane as the Earth orbits the Sun, so the Eclipses only occur when the two orbital planes cross one-another; this typically happens two or three times a year, and always at the New Moon. During Total Eclipses the Moon entirely blocks the light of the Sun, however most Eclipses are Partial, the Moon only partially blocks the light of the Sun.

How the differing inclinations of the Earth and Moon's orbits prevent us having an eclipse every 28 days. Starry Skies.

Although the light of the Sun is reduced during an Eclipse, it is still extremely dangerous to look directly at the Sun.

Animation showing the shadow of the Moon at five minute intervals on Friday 20 March 2015. Andrew Sinclair/HM Nautical Almanac.

See also...

The Earth will reach its aphelion, the furthest point in its orbit from the Sun, a distance of 152 093 481 km, at 7.41 pm GMT on Monday 6 July 2015. The Earth's orbit is slightly eccentric and slightly variable, leading to the distance between the Earth and the Sun varying...


The June (or Northern) Solstice falls on Sunday 21 June in 2015, the day on which the Sun rises highest in the sky and the longest day of the year in the Northern Hemisphere (where it is the Summer Solstice) and...


A total Lunar Eclipse will occur on a April 2015, starting at about 9.00 am GMT. It will be visible across much of the Pacific, as well as most of Alaska, the Russian Far East, eastern Japan and eastern Australia. Part of...

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