Tuesday, 3 February 2015

Free-living Amoebae in the water system of a South African hospital.


Free-living Amoebae are unicellular protozoan’s common in aquatic ecosystems, which are also known to colonize Human created water systems such as water supply systems and swimming pools. Whilst in some ways these organisms can be helpful, consuming a range of Bacterial, Viral and Fungal pathogens, they have also been shown to cause a range of infections themselves, and can themselves be infected by a variety of pathogenic Bacteria, such as Legionella pneumophila, Mycobacteria, Pseudomonas aerugionosa and Acinetobacter baumannii. Whilst most Bacteria are consumed and digested by the Amoebae, these pathogenic species have been shown to be able to resist digestion, instead surviving within the Amoebae, where they receive protection from biocides and antibiotics, later emerging to cause infections in Humans.

In a paper published in the South African Journal of Science in January 2015, Petros Muchesa and Tobias Barnard of the Water and HealthResearch Centre at the Department of Biomedical Technology at the University of Johannesburg and Catheleen Bartie of Immunology and Microbiology at the National Institute for Occupational Health, describe the results of a series of tests in which water samples and swab samples from taps and showers were collected from a number of locations at a hospital in Johannesburg and cultured to determine the presence of free-living Amoebae.

Muchesa et al. were able to culture Amoebae belonging to three identified genera, Acanthamoeba, Hartmanella and Balamuthia, as well as a number of unidentified species, from 43.7% of the water samples and 45.1% of the swab samples.

Balamuthia cysts (indicated by arrows) in water and biofilm samples from ahospital water system. Muchesa et al. (2015).

There have been relatively few published studies on free-living Amoebae in hospital water supplies, but these results are higher than a study of water in a Swiss hospital in 2006 which found Amoebae in 5.7% of samples and a study from American hspitals in 2014, which found Amoebae in 14.8% of samples.

While there have not been any reported instances of Amoeba-related invfections at the hospital, Acanthamoeba and Balamuthia have previously been implicated in infections of the eyes, skin and nervous system, and the presence of these organisms in the water supply system is of concern, particularly as the hospital has a high proportion of immunocompromised patients.

See also…

http://sciencythoughts.blogspot.co.uk/2015/01/bacteria-from-biofilms-in-water-supply.htmlBacteria from biofilms in the water supply at Mafikeng, South Africa.                                           South Africa has an arid climate and a rapidly rising Human population, which can place a strain on the country’s attempts to provide clean water for its entire...

Scientists from the German Federal Institute for Geosciences and Natural Resources, working in northern Namibia have this month announced the discovery of a substantial new aquifer, named...
John Snow was a nineteenth century London doctor, who is widely credited with the discovery of the transmission mechanism of Cholera, a severe and often fatal infection of the small intestine caused by the bacterium Vibrio cholerae. In Snow's time our...
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Monday, 2 February 2015

First evidence of Human consumption by Katydids and Woodlice.

Modern forensic science typically involves the detailed examination of corpses where foul play is suspected, with the aim of identifying any marks on the body, and relating them to the cause of, and circumstances surrounding, the death of the person in question. Numerous Arthropods are known to feed on vertebrate carrion, including Human remains, and marks left by feeding Arthropods have in the past been mistaken for burns, evidence of intravenous drug use, bite marks, defensive wounds and a variety of other forms of evidence. As such forensic scientists in a number of areas have begun to experiment with Human remains left to decompose in the environment, in order to better understand how Arthropod feeding traces and other forms of environmental destruction affect a body after death.

In a paper published in the Journal of Medical Entomology in January 2015, a team of scientists led by Jennifer Pechal of the Department of Biology at the University of Dayton and the Department of Entomology at Michigan State University, discuss the results of an experiment in which a body was left exposed at the Forensic Anthropology Center at Texas State University, and subsequently targeted by a variety of Arthropods not previously associated with the consumption of Human remains.

Firstly the cadaver was targeted by a gravid female Katydid, Pediodectes haldemani, which began feeding on the lower right arm of the body, approximately 32 hours after it was placed in the field. Katydids, Tettigoniidae, are Orthopteran Insects related to Grasshoppers and Crickets, but unlike these plant-eating groups they are generally omnivorous in their dietary preferences, and the species Pediodectes haldemani is known to be almost totally carnivorous. While Katydid have previously been recorded consuming vertebrate carrion, this is the first recorded instance of the consumption of Human remains by a Katydid, and Pechal et al. suggest that this might be slightly atypical behaviour, fuelled by a need for extra protein in the gravid female.

A gravid, female Pediodectes haldemani (Orthoptera: Tettigoniidae) feeding on the right forearm of a set of human remains (top), and the resulting physical artifact (indicated by the black arrow) on the remains by the feeding Pediodectes haldemani (bottom). Pechal et al. (2015).

Secondly the remains were visited by a Common Woodlouse, Armadillidium cf. vulgare, this time feeding on the lower left arm. Woodlice are terrestrial Isopod Crustaceans, with a typicalldetritivorous diet; they are most commonly associated with plant remains, but are known to eat carrion, though once again this is the first time that a Woodlouse has been recorded eating Human remains.

Armadillidium cf. vulgare (Isopoda: Armadilidiidae) feeding on the left forearm of a human set of remains (top), and the resulting artifact (indicated by theblack arrow) on the remains from the isopod activity (bottom). Pechal et al. (2015).

Finally the body was visited by a colony of Red Fire Ants, Solenopsis invicta, an imported species in the US, but which has become common in grasslands; Ants, including Red Fire Ants, are common visitors to carrion. On this occasion it is unclear whether the Ants actually fed on the remains, rather they entered the body via the hole left by the Katydid’s feeding and appeared to build a shelter there, using soil and small pieces of woody debris, a structure which would have been difficult to interpret had its construction not been observed.

A structure consisting of soil, small organic woody debris, and other organic material by red imported Fire Ants, Solenopsis invicta (Hymenoptera: Formicidae), in the artifact resulting from Pediodectes haldemani feeding activity on the leftforearm of the descendent. The structure was re-constructed each time the remains were disturbed for sampling purposes. The small dots surrounding the debris pile are fly artifacts or speck. Pechal et al. (2015).

See also…

http://sciencythoughts.blogspot.co.uk/2015/01/two-new-species-of-katydids-from.htmlTwo new species of Katydids from Pakistan. Katydids (or Buschcrickets), Tettigonioidea, are Members of the Insect Order Orthoptera, which also includes Crickets and Grasshoppers. They are...


http://sciencythoughts.blogspot.co.uk/2014/11/the-impact-of-yellow-crazy-ant-on.htmlThe impact of the Yellow Crazy Ant on the VallĂ©e de Mai Palm Forest of Praslin Island. Ants are often highly adaptable animals, and many species have proven to be highly invasive pests, able to reach new homes by hitching a ride on cargo moved by Humans, and often proceeding modify the ...
http://sciencythoughts.blogspot.co.uk/2014/10/three-new-species-of-katydid-from-china.htmlThree new species of Katydid from China. Katydids of the genus Xizicusand its close relatives are found across eastern Asia, though the taxonomy of the group is currently somewhat confused, in part due to publications being published in different languages...

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Asteroid 2015 BE passes the Earth.

Asteroid 2015 BE passed by the Earth at a distance of 11 890 000 km (30.91 times the average distance between the Earth and the Moon, or 7.9 % of the average distance between the Earth and the Sun), at about 8.25 am GMT on Friday 30 January 2015. There was no danger of the asteroid hitting us, though had it done so it would have presented only a minor threat. 2015 BE has an estimated equivalent diameter of 21-65 m (i.e. it is estimated that a spherical object with the same volume would be 21-65 m in diameter), and an object of this size would be expected to break up in the atmosphere between 22 and 4 km above the ground, with only fragmentary material reaching the Earth's surface.

 The calculated orbit of 2015 BE JPL Small Body Database.

2015 BD511 was discovered on 16 January 2015 (fourteen days before its closest approach to the Earth) by the University of Hawaii's PANSTARRS telescope on Mount Haleakala on Maui. The designation 2015 BE implies that it was the 5th asteroid (asteroid E) discovered in the second half of January 2015 (period 2015 B).

 2015 BE has a 788 day year orbital period and an eccentric orbit tilted at an angle of 14.5° to the plane of the Solar System, which takes it from 0.92 AU from the Sun (i.e. 92% of the average distance at which the Earth orbits the Sun) to 2.42 AU from the Sun (i.e. 242% of the average distance at which the Earth orbits the Sun, considerably outside the orbit of Mars). It is therefore classed as an Apollo Group Asteroid (an asteroid that is on average further from the Sun than the Earth, but which does get closer). This means that close encounters between the asteroid and Earth are fairly  common, with another predicted for June this year.

See also...

http://sciencythoughts.blogspot.co.uk/2015/01/asteroid-2015-bd511-passes-earth.htmlAsteroid 2015 BD511 passes the Earth.   Asteroid 2015 BD511 passed by the Earth at a distance of 1 714 000 km (4.47 times the average distance between the Earth and the Moon, or 1.1 % of the average distance between the Earth and the Sun), slightly before 0.50 am GMT on Friday 30 January...

Comet C/2014 Q1 (Lovejoy) reached its perihelion (the closest point on its orbit to the Sun) on Friday 30 January 2015, when it will be 1.29 AU from the Sun....
 
Asteroid (162004) 1991 VE passed by the Earth at a distance of about 15 600 000 km (40.6 times the average distance between the Earth and the Moon, or 10.4% of the average distance between the Sun and the Earth), slightly after 3.30 am GMT on Saturday 17 January 2015. There was no danger of the asteroid hitting us, though were it to do so it would have presented a serious threat. (162004) 1991 VE has an...
 
 
 
 
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A new species of Ichneumon Wasp from Qinghai Province, China.


Ichneumon Wasps of the genus Campoplex are parasitiods of Beetles and Moths (i.e. their larvae live inside Beetles and Moths, eating their living host as they mature) found predominantly in Europe and Western Asia, with species also recorded from East and Southeast Asia, North America and Africa. Eleven species have previously been recorded from China.

In a paper published in the journal ZooKeys on 18 December 2014, Yu-Xiang Zhao of the The Key Laboratory for Silviculture and Conservation at Beijing Forestry University and the General Station of Forest Pest Management of the State Forestry Administration and Mao-Ling Sheng also of the General Station of Forest Pest Management of the State Forestry Administration, describe a new species of Campoplex from Qinghai Province in China.

The new species is named Campoplex bazariae, in reference to its host species the Moth Bazaria turensis. Females of the Wasp are 7.5-8.0 mm in length, males 8.0-8.2 mm. Both are predominantly black with some brown areas.

Female Campoplex bazariae inlateral view. Zhao & Sheng (2014).

The species was discovered while investigating an outbreak of Bazaria turensis (a form of Snout Moth) in a forest in Qinghai. The Wasps emerged from the cocoons of the Moths, both within clusters of leaves in the tree canopy and buried in soil on the forest floor.

See also…

http://sciencythoughts.blogspot.co.uk/2015/01/two-new-species-of-ichneumon-wasps-from.htmlTwo new species of Ichneumon Wasps from Fennoscandia and Hungary.                                    Ichneumon Wasps are parasitoids whose larvae develop on or in the bodies of other Arthropods, typically Insects or Spiders. Since Insect species are always described from adult specimens, species of parasitoid Wasps are generally named from specimens taken from the wild as adults, and the larval host of often unknown. However some scientists have developed an alternative method...
http://sciencythoughts.blogspot.co.uk/2014/12/two-new-species-of-ichneumon-wasps-from.htmlTwo new species of Ichneumon Wasps from Africa.                                                             Ichneumon Wasps are large parasitoid Wasps (the largest species can exceed 5 cm) closely related to Braconids. They are noted for their reproductive behaviour, in which the females sting another Insect or...
Ichneumon Wasps are a group of highly specialized...


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Five new species of Proetoid Trilobites from northeastern Oman.


Trilobites dominated the seas of the early Palaeozoic, but suffered a major loss of diversity in the Devonian extinction and became extinct at the end of the Permian. For a long time it was assumed that the group was in decline before this final extinction event, but a series of recent discoveries have shown the group underwent a significant expansion in the Permian Period, particularly in the eastern Tethyan Realm, which today outcrops from Sicily in the west across Arabia and South Asia to Timor in the east.

In a forthcoming paper in the journal Acta  Palaeontologica Polonica available online from 30 December 2014, Richard Fortey of the Department of Palaeontology at The Natural History Museum and Alan Heward of Malvern in Worcestershire, England, describe a new Trilobite fauna from the Early-to-Middle Permian Qarari Unit in northeastern Oman.

The fauna comprises five previously undescribed Proetoid Trilobites, with affinities to other southern Asian Permian Trilobite faunas, particularly those of the Artinskian limestones of Afghanistan. The Trilobites are preserved in thin-bedded fine-grained limestones interpreted as having come from bellow the storm wave base in a shallow marine environment, with well-oxygenated waters. The vast majority of the Trilobires are preserved in an encapsulated state, leading Fortey and Heward to speculate that they may have died as a result of some sudden environmental stress, which provoked a defensive response before death.

The first new species describedis placed in the genus Hentigia and given the specific name ornata, in reference to the elaborate sculpting on the cephalic (head) region. This Trilobite is 1-1.5 cm in diameter when encapsulated and has a glabella (face, front part of the cephalic region), which is enlarged and covered in tubercles.

Ditomopygine Trilobite Hentigia ornata from Kungurian–Roadian (Permian) of Wadi Khawr al Jaramah, Oman. (A) Enrolled completespecimen, in dorsal (A1), lateral  and(A2) views. Scale bars 2.5 mm. Fortey & Heward (2015).

The second new species described is placed in the genus Iranaspidion and given the specific name elephas, meaning ‘Elephant’ for its prominent cheek tubercles and the shape of its hypostome, which resembles an Elephant’s head with ears extended when viewed from the rear.

Ditomopygine Trilobite Iranaspidion elephasfrom Kungurian–Roadian (Permian) of Wadi Khawr al Jaramah, Oman. (A)Enrolled complete specimen; cephalon in dorsal (A1) and anterior (A2) views; pygidium and half thorax in dorsal view (A3). Scale bars 2.5 mm. Fortey & Heward (2015).

The third new species described is placed in a new genus, Simulopaladin, meaning ‘similar to Paladin’ another genus of Trilobites. The genus Paladin was originally used to describe deepwater Trilobites from the Carboniferous of North America, though a number of Permian shallow marine Asian species have subsequently been added to the genus. Fortey and Heward suspect that these Permian Trilobites are erroneously placed in the genus, and erect the genus Simulopaladin to describe this Omani species, pending a review of the group. It is given the specific name tridentifer, meaning ‘carrting three teeth’, in reference to three tubercles on the occipital ring (back part of the cephalic region).

Ditomopygine Trilobite Simulopaladin tridentifer from Kungurian–Roadian (Permian) of Wadi Khawr al Jaramah, Oman. (A) Holotype, enrolled complete specimen; cephalon in dorsal view (A1); pygidium and half thorax in dorsal (A2) view. Scale bars 2.5 mm. Fortey & Heward (2015).

The fourth new Trilobite described is placed in the genus Acanthophillipsia, and given the specific name felicitae, in honour of Felicity Heward who collected some of the specimens. This species is described from only two specimens, one of which is crushed. The cephalic region of this species is almost completely covered in tubercles.

Ditomopygine Trilobite Acanthophillipsia felicitae.(F) Enrolled complete specimen; pygidium and half thorax in dorsal view (F1); cephalon in dorsal (F2), lateral (F3), and anterior (F4) views. (G) Enrolled complete specimen; pygidium and half thorax inlateral (G1), dorsal (G3), and anterior (G4) views; cephalon in dorsal view (G2). Scale bars 2.5 mm. Fortey & Heward (2015).

The final new species described is placed in the genus Triproetus, and given the specific name bonbon, for its resemblance to a boiled sweet. This has a swollen, bulging glabella with a fine tuberculate surface.

Proetid Trilobite Triproetus bonbon (A) Enrolled complete specimen; cephalon in dorsal (A1) and lateral (A2) views. Scale bars 2.5 mm. Fortey & Heward (2015).

See also…

http://sciencythoughts.blogspot.co.uk/2012/03/preserved-trilobite-digestive-tracts.htmlPreserved Trilobite digestive tracts from the Middle Cambrian of Utah.                                 Trilobites were a group of Arthropods that flourished throughout the Palaeozoic, but died out at the end of the Permian. They are abundant and well studied fossils, but little is known of their internal anatomies.
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Follow up observations of Kepler candidate stars.


The Kepler Space Telescope observed a 115 square degree of space for four years (from May 2009 till May 2013), looking for potential planets around the 150 000 stars in the magnitude range 8-16 within the field. In this time it found a total of 4233 candidate planets, of which 965 have subsequently been confirmed. The conformation of such a planet requires follow up observations from ground-based telescopes in order to eliminate potential sources of false readings, such as previously undetected faint companion or background stars.

In a paper published on the arXiv database at Cornell University Library on 14 November 2014, and in the Astronomical Journal on 15 January 2015, a team of scientists led by Mark Everett of the National Optical Astronomy Observatory present the results of follow up observations on eighteen Kepler candidate stars, several of which are confirmed to host planets.

Follow up observations were made from the Differential SpeckleSurvey Instrument at Gemini North on 25−31 July 2013, although the observations were hampered by light leakage on 25 July and by Tropical Storm Flossie brushing the Hawaiian Islands on 29-30 July, so most of the useful observations were in fact made on 27 July 2013. Further follow up observations of several candidate stars were made with the Lick Observatory Shane 3.5 m, the PalomarObservatory Hale 5 m or the 10m Keck-II Telescopes.

The KOI 115 system (that is ‘Kepler Object of Interest’ 115, the designation given to star systems with unconfirmed planets in the Kepler field), has previously been confirmed to host two planets and redesignated as the Kepler 105 system (i.e. the 105th system in the Kepler Field confirmed to host one or more planets). These planets were reconfirmed by the Gemini North Survey. The star has an effective surface temperature of 6075 K (compared to 5778 K for our Sun) and a mass 1.027 times that of the Sun. The planets were previously found to have orbital periods of 5.4 and 7.1 days, the new data from Gemini North in addition suggests that these planets have radii of 2.54 and 1.44 times that of the Earth, respectively.

The KOI 265 system has a candidate planet with a radius of 1.71 times that of the Earth, with an orbital period of 3.6 days. Everett et al. validate this planet with a 94% certainty level, though this is not considered sufficient to confirm the existence of a planet.

KOI 268 is a dwarf star with an effective surface temperature of 6343 K, with a candidate planet orbiting every 110 days. Everett et al.’s data reveals the presence of two previously undiscovered nearby stars, identified as neighbours B and C. Of these neighbour B is a small star with an effective surface temperature of 4007 Kwhich lies close enough to KIO 268 that the candidate planet is impossible to validate. It could be a planet with a radius of 3.04 times that of the Earth orbiting KOI 268, but it could also be a planet with a radius of 9.33 times that of the Earth orbiting Neighbour B (a larger planet would be needed to reduce the total light produced by the two stars if the planet is occluding the dimmer star); if the latter were the case then it would have a low equilibrium temperature, about 217 K.

KOI 274 has previously been confirmed to host two planets with periods of 15 and 22.8 days, and redesignated as Kepler 128. Everett et al. were able to confirm theses planets, and that the star is a single system. They also estimate that the planets both have about 1.2 times the radius of the Earth.

KOI 284 has previously been confirmed to host three planets, and a possible fourth, and redesignated as Kepler 132. However a nearby star makes it hard to resolve the system further; it was impossible to determine whether this star is a companion (orbiting the main star) or a field star (behind the star and unrelated to it, close only because of the angle from which we are viewing the system), though a companion is thought to be the more likely scenario. If this is the case then all of the planets, including the unconfirmed candidate, will have a radius between 1-2 times that of the Earth.

KOI 369 is a dwarf star with an effective surface temperature of 6157 K has previously been confirmed to host two planets, and redesignated as Kepler 144. Everett et al. are able to reconfirm these planets and estimate that they have radii of 1.78 and 1.69 times that of the Earth, respectively.

KOI 1537 is a dwarf star with an effective surface temperature of 6260 K and a candidate planet with a period of 10 days. A previous study suggested that a second star was close to this star, either as a companion or a field star, however Everett et al. were able to find no evidence for this second star. They were able to validate the planet with an 86.7% certainty (not enough to confirm its existence) and estimate its radius to be 1.35 times that of the Earth.

KOI 1964 is a dwarf star with an effective surface temperature of 5574 K and a candidate planet with an orbital period of 2.2 days. It also has a neighbouring star about 4” (four arc seconds; the sky, imagined as a globe, is divided into 360 degrees, each of which is divided into 60 arcminutes, with each arc minute being further divided into 60 arcseconds) to its north, as seen from Earth. This makes it very hard to confirm the planet is orbiting KOI 1964, though Everett et al. were able to come up with three possible scenarios. Firstly the second star could be a bound companion to KOI 1964, and the planet could also orbit KOI 1964 and have a radius of 0.764 times that of the Earth. Secondly, the second star could be a field star somewhere in the background and the planet could orbit KOI 1964 and have a radius of 0.785 times that of the Earth. Thirdly the second star could be a field star, and the planet could orbit that star, in which case the star would have an effective surface temperature of 3892 K and the planet a radius of 2.03 times that of the Earth.
 
Example high resolution imagery of KOI 1964 and its surroundings in 4 filters. The upper two panels are reconstructed images from speckle observations at 692 nm (upper left) and 880 nm (upper right) taken at Gemini North. The lower two panels are adaptive optics images at J (lower left) and Ks (lower right) taken at the Palomar Hale Telescope. Each image is oriented with North at the top and East to the left. The speckle images are 1.8′′ ×1.8′′ and the adaptive optics images are approximately 15′′ ×15′′ as seen by the scales. A faint neighbour star is detected 0.4′′ to the north of the brighter KOI star. Everett et al. (2014).

KOI 2311 is a sunlike dwarf star with two candidate planets, orbiting with periods of 192 and 14 days. There is a faint second star at a separation of 1”, making it hard to establish the true nature of the planets. Everett et al. Calculate that if the inner planet orbits KOI 2311 then it has a radius of 0.932 that of the Earth and if it orbits the second star it has a radius of 4.16 times that of the Earth. The if the outer planet is orbiting KOI 2311 then it is calculated to be cool (337 K) and have a radius of 115 times that of the Earth, while if it orbits the second star then it is colder (117 K) and has a radius of 5.14 times that of the Earth (making it larger than Neptune).

KOI 2365 is a sunlike star with two candidate planets. This was found to be a solitary star, and the planets were validated with a confidence of 99.9%, considered enough to confirm their existence. The system is therefore redesignated as Kepler 430, and the planets as Kepler 430b (when naming objects in other star systems planets are given lower case letters and stars upper case letters), which has a 36 day orbital period, a radius of 3.25 times that of the Earth and a temperature of 667 K, and Kepler 430c, which has an 111 day orbital period, a radius of 175 times that of the Earth and a temperature of 458 K.

KOI 2593 is another isolated star, this time with a single candidate planet. Everett et al. were only able to validate the planet with a 90.6% confidence, though they did establish the star has a surface temperature of 6119 K and the potential planet has a mass of 1.10 times that of the Earth and a temperature of 974 K.

KOI 3097 is an isolated star with three candidate planets. Everett et al. were able to establish that the star has a surface temperature of 6004 K, and validate the planets with a confidence of 99.8%. The system is redesignatedKepler 431, and the planets become Kepler 431b, with a 6.8 day orbital period, a radius of 0.764 times that of the Earth and a temperature of 1032 K, Kepler 431c with an 8.7 day orbital period, a radius of 0.668 times that of the Earth and a temperature of 951 K, and Kepler 431d with an 11.9 day orbital period, a radius of 1.11 times that of the Earth and a temperature of 865 K.

KOI 3204 is a hot dwarf star with a surface temperature of 7338 K and a candidate planet which orbits it every 0.57 days. Everett et al. validated the planet with a confidence of 98.5% (not enough to confirm it), and calculate it has a radius of 1.01 times that of the Earth and a temperature of 3268 K.

KOI 3224 is an isolated dwarf star with a single candidate planet. Everett et al. calculate that the star has a surface temperature of 5382 K, and validate the planet with a 90.5% certainty. They calculate that this candidate planet has a radius of 0.667 times that of the Earth, and a temperature of 1129 K.

KOI 3255 is a faint, cool dwarf star with a surface temperature of 4427 K, a single candidate planet with a 66.7 day orbital period, and two close stars, the relatively bright neighbour B at a separation of 0.18”, and the fainter neighbour C at 3”. The closeness of neighbour B makes it impossible to validate the planet, though Everett et al. calculate that it could be orbiting KOI 3255, in which case it would have a radius of 2.11 times that of the Earth and a temperature of 294 K, or neighbour B, in which case it would have a radius of 2.42 times that of the Earth and a temperature of 276 K, either of which scenarios would make it a habitable zone candidate.

KOI 3284 is the smallest star included in this study. It has a surface temperature of 3688 K (smaller stars are cooler than larger stars) and a candidate planet with a 35 day orbital period. It also has two close stars, neighbour B which has a separation of 0.44” and neighbour C. Because of the closeness of neighbour B it was impossible to validate the planet, nor was it possible to determine if neighbour B was a companion or a field star, though neighbour C did appear to be a background star. Everett et al. calculate that if neighbour B is a background star and the planet orbots KOI 3284 then the planet will have a radius of 0.99 times that of the Earth and a temperature of 272 K, that if it orbits KOI 3284 and neighbour B is a bound companion it will have a radius of 1.00 times that of the Earth and a temperature of 272 K, or if it orbits neighbour B and neighbour B is a bound companion to KOI 3284, then the planet will have a radius of 1.46 times that of the Earth and a temperature of 184 K, scenarios that make it a small habitable zone candidate.

KOI 4407 is a dwarf star with a single candidate planet that has a 1.34 day orbital period, and two close by stars that might be gravitationally bound companion stars or background field stars. It was possible to calculate that the surface temperature of KOI 4407 is 6408 K, but the presence of the neighbour stars makes it difficult to characterise the planet. Everett et al. were able to validate this planet, but only with a confidence of 19.2%. They calculate that if the two neighbour stars are actually components of a triple star system, then the planet probably has a radius of 0.65 times that of the Earth and a temperature of 2121 K, though the radius could possibly be anywhere between 0.64 and 0.75 times the Earth’s.

See also…

http://sciencythoughts.blogspot.co.uk/2014/07/conformation-of-third-planet-in-kepler.htmlConformation of the third planet in the Kepler-51 System.                                               Kepler-51 is a G-type Yellow Dwarf star 2800 light years from Earth in the constellation of Cygnus. It has a...

Kepler 186f: an Earth-sized planet in the habitable zone of a Red Dwarf star.
One of the key objectives in the search for planets orbiting other stars has been to locate planets in the habitable zones of such stars, i.e. planets on which liquid water could potentially exist. A number of...



 The Kepler 210 planetary system.
Since it began its survey of the section of the sky dubbed the Kepler Deep Field in 2009, the Kepler Space Telescope has discovered 2321 probable planets around 1790 stars, and it is thought that the vast majority of these probable planets will turn out to be true...
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Saturday, 31 January 2015

Asteroid 2015 BD511 passes the Earth.

Asteroid 2015 BD511 passed by the Earth at a distance of 1 714 000 km (4.47 times the average distance between the Earth and the Moon, or 1.1 % of the average distance between the Earth and the Sun), slightly before 0.50 am GMT on Friday 30 January 2015. There was no danger of the asteroid hitting us, though had it done so it would have presented only a minor threat. 2015 BD511 has an estimated equivalent diameter of 7-25 m (i.e. it is estimated that a spherical object with the same volume would be 7-25 m in diameter), and an object of this size would be expected to break up in the atmosphere between 36 and 20 km above the ground, with only fragmentary material reaching the Earth's surface. 

The calculated orbit of 2015 BD511. JPL Small Body Database.

2015 BD511 was discovered on 26 January 2015 (four days before its closest approach to the Earth) by the University of Hawaii's PANSTARRS telescope on Mount Haleakala on Maui. The designation 2015 BD511 implies that it was the 12 779th asteroid (asteroid D511) discovered in the second half of January 2015 (period 2015 B).

2015 BD511 has a 640 day year orbital period and an eccentric orbit tilted at an angle of 12.1° to the plane of the Solar System, which takes it from 0.59 AU from the Sun (i.e. 59% of the average distance at which the Earth orbits the Sun, inside the orbit of Venus) to 2.31 AU from the Sun (i.e. 231% of the average distance at which the Earth orbits the Sun, considerably outside the orbit of Mars). It is therefore classed as an Apollo Group Asteroid (an asteroid that is on average further from the Sun than the Earth, but which does get closer). This means that close encounters between the asteroid and Earth are fairly  common, with the last having occured in August 2013. Close encounters between 2015 BD511 and Venus are also fairly common, with the last having occurred in December 1951.

See also...

Comet C/2014 Q1 (Lovejoy) reached its perihelion (the closest point on its orbit to the Sun) on Friday 30 January 2015, when it will be 1.29 AU from the Sun....

Asteroid (162004) 1991 VE passed by the Earth at a distance of about 15 600 000 km (40.6 times the average distance between the Earth and the Moon, or 10.4% of the average distance between the Sun and the Earth), slightly after 3.30 am GMT on Saturday 17 January 2015. There was no danger of the asteroid hitting us, though were it to do so it would have presented a serious threat. (162004) 1991 VE has an...

Asteroid (410088) 2007 EJ passed by the Earth at a distance of about 26 500 000 km (68.9 times the average distance between the Earth and the Moon, or 17.7% of the average distance between the Sun and...



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