Friday, 11 April 2025

Fireball meteor over Luxembourg.

Witnesses across Belgium, the Netherlands, Luxembourg, Switzerland, northern France, western Germany, southeast England, northern Italy, and parts of Austria, have reported observing a bright fireball meteor around 2.30 am local time (around 0.30 am GMT) on Sunday 6 April 2025. The fireball is described as having moved from southeast to northwest, appearing over the Grand Est region of northeastern France and disappearing overr Luxembourg. A fireball is defined as a meteor (shooting star) brighter than the planet Venus. These are typically caused by pieces of rock burning up in the atmosphere, but can be the result of man-made space-junk burning up on re-entry.

The 6 April 2025 meteor seen from the Saint-Luperce, France. Romain Kropp/Météo-Centre-Val de Loire/American Meteor Society.

Objects of this size probably enter the Earth's atmosphere several times a year, though unless they do so over populated areas they are unlikely to be noticed. They are officially described as fireballs if they produce a light brighter than the planet Venus. The brightness of a meteor is caused by friction with the Earth's atmosphere, which is typically far greater than that caused by simple falling, due to the initial trajectory of the object. Such objects typically eventually explode in an airburst called by the friction, causing them to vanish as a luminous object. However, this is not the end of the story as such explosions result in the production of a number of smaller objects, which fall to the ground under the influence of gravity (which does not cause the luminescence associated with friction-induced heating).

Heat map showing areas where sightings of the meteor were reported (warmer colours indicate more sightings), and the apparent path of the object (blue arrow). American Meteor Society.

These 'dark objects' do not continue along the path of the original bolide, but neither do they fall directly to the ground, but rather follow a course determined by the atmospheric currents (winds) through which the objects pass. Scientists are able to calculate potential trajectories for hypothetical dark objects derived from meteors using data from weather monitoring services.

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Thursday, 10 April 2025

Eruption on Mount Kanlaon.

Mount Kanlaon, a 2465 m stratovolcano (cone shaped volcano made up of layers of ash and lava) on northern Negros Island in the central Philippines, underwent an explosive eruption at 5.51 am local time on Tuesday 8 April 2025, producing an ash column 4 km high which drifted to the west and southwest, according to a bulletin issued by the Philippine Institute of Volcanology and Seismology. The sound of the eruption was heard about 20 km away, and pyroclastic flows were observed on the southern flanks of the volcano, and debris is reported to have set fire to vegetation close to the summit of the volcano. Ash falls were reported up to 50 km from the eruption.

An ash column over mount Kanlaon on 8 April 2025. Philippine Institute of Volcanology and Seismology.

No injuries have been associated with the eruption, but the Philippine Institute of Volcanology and Seismology has recommended that communities within 6 km of  the volcano evacuate the area, and has placed a ban on aircraft overflying the area.

The geology of the Philippines is complex, with the majority of the islands located on the east of the Sunda Plate. To the east of this lies the Philippine Sea plate, which is being subducted beneath the Sunda Plate (a breakaway part of the Eurasian Plate); further east, in the Mariana Islands, the Pacific Plate is being subducted beneath the Philippine Sea Plate. This is not a smooth process, and the rocks of the tectonic plates frequently stick together before eventually being broken apart by the rising pressure, leading to Earthquakes in the process. Material from the subducting Philippine Plate is heated by the temperature of the Earth's interior, causing lighter minerals to melt and the resultant magma to rise through the overlying Sunda Plate, fuelling the volcanoes of the Philippines.

Subduction beneath the Philippines. Yves Descatoire/Singapore Earth Observatory.

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Wednesday, 9 April 2025

Prunus luxurians: A new species of Cherry from southwestern Ecuador.

The genus Prunus has a worldwide distribution and contains several important food crops (including Cherries, Almonds, and Plums), ornametal species (Blossom Cherries), timber souces (e.g. Black Cherry) and medicinal Plants (e.g. African Cherry). There are thought to be about 450 valid species in the genus, but the situation is complicated with about 1230 species described within the genus, and over 2000 more in other genera that have since been synonymised with it (i.e. genera which have had all their putative members moved into Prunus

Historically, it has been thought that the majority of Prunus species are found in the northern temperate belt, with a smaller number of species found at high altitudes in tropical and subtropical zones. However, recent research has discovered that the genus is much more widespread in lowland tropical forests than previously realised, particularly in the Americas, raising the possibility that the genus is more diverse in these regions than in the temperate zone.

In a paper published in the journal PhytoKeys on 4 April 2025, Álvaro Pérez of the Herbario QCA at the Pontificia Universidad Católica del EcuadorJorge Andrés Pérez-Zabala of the Herbario Gabriel Gutiérrez Villegas at the Universidad Nacional de ColombiaKatya Romoleroux, also of the Herbario QCA at the Pontificia Universidad Católica del Ecuador, David Espinel-Ortiz, again of the Herbario QCA at the Pontificia Universidad Católica del Ecuador, and of the Bonn Institute of Organismic Biodiversity at the University of Bonn, and Chaquira Romoleroux and Natasha Albán-Vallejo, once again of the Herbario QCA at the Pontificia Universidad Católica del Ecuador, describe a new species of Prunus from southwestern Ecuador.

The new species is described from a small population of trees discovered in a cloud forest remnant in the Sambotambo Birón area of the Jocotoco Foundation-managed Reserve Buenaventura in El Oro Province, on the western flank of the Andes, between 1300 and 1400 m above sealevel. The new species is named Prunus luxurians, in reference to its 'profuse blooming and outstanding beauty', which makes it a conspicuous part of the lower and mid-strata of the forest.

Prunus luxurians: (A) Habit, (B branch with leaves and floriferous shoots, (C) flowers. Álvaro Pérez in Pérez et al. (2025).

Prunus luxurians forms trees up to 11 m high, with grooved dark brown bark with lighter lenticles (raised pores). Leaves are oblong-to-lance-shaped, waxy, and grow on alternating sides of leaf stems, they are 10–13.65 cm long and 3.5–4.65 cm wide. Flowers are white with light green centres, and born on floriferous shoots, which can have 14–27 individual flowers, clusetered together in groups of 3-4.

Only five living trees were found, in a fragment of montane evergreen forest, with high levels of bith diversity and endemism. The remaining forest fragments in this region are considered to be threatened by mining and farming activities, for which reason Pérez et al. recomend that Prunus luxurians be classified as Critically Endangered under the terms of the International Union for the Conservation of Nature's Red List of Threatened Species.

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Tuesday, 8 April 2025

Outbreak of Cholra in Angola.

Angola has been suffering a severe Cholera outbreak, with the first cases reported in January 2025, with 8543 reported cases and 329 fatalities, 112 occurred in the community, by 23 March, according to a press release issued by the World Health Organization. From the outset of the outbreak, the number of cases rose steadily until the first week of February, when over 1000  cases were reported in a single week. The number of cases then fell slightly, plateauing at slightly over 800 cases a week through most of February and March, before starting to rise again at the end of March.

Number of Cholera cases by epidemiological week of reporting, as of 23 March 2025. World Health Organization.

Younger people have been particularly badly hit by the outbreak, with 1976 reported cases (23.1% of the total) among 6-14-year-olds, 1850 cases (21.7% of the total) among 15-24-year-olds, and 1475 cases (17.3%) of cases among 25-34 year-olds. Males have been slightly more affected than females, making up 55.3% of the total (4725 cases). Cases have been reported in 16 of Angola's 21 provinces, with the worst affected provinces being Luanda, with 4143 cases (48.5% of the total) and Bengo, with 2485 cases (29.1% of the total).

Map of Cholera cases by province, as of 23 March 2025. World Health Organization.

Cholera is an acute enteric infection caused by ingesting the Bacterium Vibrio cholerae a Gram-negative, comma-shaped Gammaproteobacterium, related to other pathogenic Bacteria such as Yersinia pestis (Bubonic Plague), and Esherchia coli (food poisoning), which present in contaminated water or food. It is mainly linked to insufficient access to safe drinking water and inadequate sanitation. Cholera is an extremely virulent disease that can cause severe acute watery diarrhoea resulting in high morbidity and mortality, and can spread rapidly, depending on the frequency of exposure, the exposed population and the setting. Cholera affects both children and adults and can be fatal if untreated.

Scanning electron microscope image of Vibrio cholerae Bacteria. Kim et al. (2000).

The incubation period is between 12 hours and five days after ingestion of contaminated food or water. Most people infected with Vibrio cholerae do not develop any symptoms, although the bacteria are present in their faeces for 1-10 days after infection and are shed back into the environment, potentially infecting other people. The majority of people who develop symptoms have mild or moderate symptoms, while a minority develop acute watery diarrhoea and vomiting with severe dehydration. Cholera is an easily treatable disease. Most people can be treated successfully through prompt administration of oral rehydration solution.

The consequences of a Humanitarian crisis, such as disruption of water and sanitation systems, or the displacement of populations towards inadequate and overcrowded camps, can increase the risk of Cholera transmission, should the Bacteria be present or introduced. A multisectoral approach including a combination of surveillance, water, sanitation and hygiene, social mobilization, treatment, and oral Cholera vaccines is essential to control Cholera outbreaks and to reduce deaths.

Angola has suffered recurrent Cholera outbreaks since the 1970s, with a major outbreak in 1987 which infected around 16 000 people were infected and 1460 people died. Outbreaks were recorded every year from 1987 till 1996, after which the disease disappeared for a decade. Cholera returned in 2006, with another major outbreak in which around 67 000 people were infected and 2700 people died. Subsequent outbreaks were recorded in 2011-13 and 2016-18. Cholera infections generally peak in the rainy season (mid-October to mid-April), and outbreaks in Angola are often linked to outbreaks in the neighbouring Democratic Republic of Congo.

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Sunday, 6 April 2025

Million-and-a-half-year-old bone tools from Olduvai Gorge, Tanzania.

Hominins have been using stone tools to access meat from Animal carcases for at least 2.6 million years, and this use of stone tools is also presumed to have helped them switch to a significantly more carnivorous diet. Logically, a Hominin which can use stone tools to hunt large Animals should also be able to make tools from the bones of those Animals, but bone tools have a much more limited record than their stone counterparts.

A number of bone-objects from archaeological sites in Africa dated to between 2.5 and 0.8 million years ago have been interpreted as having been modified by use as tools, for such purposes as digging or Termite fishing, but do not appear to have been deliberately shaped prior to use. A few purpose modified tools have been repoted from Olduvai Gorge in Tanzania, but these were surface finds, lacking the context from which they could be dated. Bone tools are also known from the Konso site in Ethiopia, including a bone handaxe which has been dated to 1.4 million years ago. Bone tools start to appear across Eurasia around 500 000 years ago, and highly shaped bone tools, such as spear and arrow points, barbed points, awls and needles, appear in Africa about 90 000 years ago, spreading to Eurasia around 45 000 years ago.

In a paper published in the journal Nature on 5 March 2025, Ignacio de la Torre of the Instituto de Historia of the CSIC-Spanish National Research CouncilLuc Doyon of the Université de BordeauxAlfonso Benito-Calvo of the Centro Nacional de Investigación sobre la Evolución HumanaRafael Mora of the Facultat de Lletres at the Universitat Autonoma de Barcelona, Ipyana Mwakyoma, also of the Instituto de Historia of the CSIC-Spanish National Research Council, Jackson Njau of the Department of Earth and Atmospheric Sciences at Indiana University, and the Stone Age InstituteRenata Peters of the Institute of Archaeology at University College London, Angeliki Theodoropoulou, again of the Instituto de Historia of the CSIC-Spanish National Research Council, and Francesco d’Errico, also of the Université de Bordeaux, and of the SFF Center for Early Sapiens Behaviour at the University of Bergen, describe an assemblage of bone tools from a horizon at Olduvai Gorge Bed II, which has been dated to 1.5 million years ago.

The tools form part of an assemblage identified as the T69 complex, were derived from a layer between Middle and Upper Bed II, in the Frida Leakey Korongo West Gully at Olduvai Gorge, which has been  radiometrically dated to 1.5 million years ago. T69 complex materials have been derived from six tranches, the bulk of the material comprising early Acheulean stone tools. A total of 10 900 stone tools larger than 2 cm, and over 41 000 smaller artefacts have been recovered, mostly made from a local quartzite.

Geographic and stratigraphic context of the FLK T69 Complex site. (a) Location of Olduvai Gorge in Tanzania. (b) Main geographical features of the Olduvai Basin. The geographical image was adapted from the NASA /USGS ASTER Global Digital Elevation Model. (c) Position of the T69 Complex in the Main Gorge at Olduvai. (d) Stratigraphic position of the bone tool level shown on a composite section of the deepest part of trench T69 and the central area of the T69-T79 west section. (e) Position of the T69 Complex within the general chrono-stratigraphic sequence of Bed II in the Frida Leakey Korongo West Gully area. (f) Normal (left) and polarized (right) thin section photographs of the sandstone containing the bone tool horizon. De la Torre et al. (2025).

In addition to the tools, the assemblage contains abundant Vertebrate fossils, including 9419 identified bone fragments and 13 413 unidentified fragments. Many of the identifiable remains can be attributed to Fish, Crocodiles, and Hippopotamuses, suggesting that 1.5 million years ago, the site was close to water. The majority of the large Animals are Bovids and Hippopotamuses, with some relatively intact Hippopotamus carcasses present. Other large Animals present include Equids, Suids (Pigs), Rhinoceros, and Elephants. Hippopotamus bones are the most abundant, and many of these show signs of deliberate modification.

The faunal elements of the T69 assemblage, including bone tools, are excellently preserved, something not common at Middle Pleistocene sites, allowing for careful documentation and analysis of the material present. De la Torre et al. identify 27 artefacts as unequivocal stone tools, ruling out other forms of damage such as Carnivores gnawing, Crocodiles biting, trampling and fracturing to access marrow; in fact, Carnivore bones are very rare in the T69 assemblage, and the only signs of bone-modification by Carnivores are two possible tooth marks.

Tools are identified as bones with multiple fragments removed, which lack the striations associated with trampling. Experimental breaking of large Mammal bones to recover marrow failed to produce similar flaking. Patterns of breakage consistent with marrow-extraction are present on many bones present in the faunal assemblage, suggesting that this was something done by the Hominins here. This seldom results in more than two or three flakes being removed, whereas the 'tools' have an average of 12.9 flaking scars, typically arranged contiguously and preferentially on their lateral edges.

Twenty seven bone tools were recovered during excavations at Frida Leakey Korongo West Gully, eighteen of which are attributed to Mammals weighing more than two tonnes. Sixteen of these are identifiable, including eight tools made from Elephant bones, six tools are made from the bones of Hippopotamus, and two from the bones of large Bovids. Thus, in an assemblage dominated by Bovid bones, where 169 taxa are recorded and Elephant remains make up about 1.1% ot the total, more than half the tools are made from Elephant bones. One of the tools is made from the proximal portion of the radius of a large Bovid, all the others from long portion of limb bones, predominantly the femora, tibiae and humeri.

Tools made on long bone diaphysis of very large Mammals. (a) Indeterminable taxon larger than two tonnes (accession number T69L20-3009). (b) Elephant (accession number T79L10-2511). Scale bars are 5 cm. De la Torre et al.  (2025).

The Frida Leakey Korongo West Gully tools represent a set of technological and behavioural innovations previously unrecorded in Hominins of this antiquity. The tools are relatively 'fresh', which is to say they were apparently buried quite soon after being made, and do not show signs of having sat on the surface and subject to weathering. The Hippopotumus bone tools all appear to have been made from fresh bone (i.e. from Animals which had died shortly before the tools were made), but some of the Elephant bone tools appear to have been made from bones partially weathered before flaking occurred, suggesting that old Elephant bones were recognised as a valuable resource and collected separatley from scavenging carcases for food. Elephant bone tools range from 22 to 38 cm in length and from 8 to 15 cm in width, making them the largest in the assemblage. Hippopotamus bone tools are slightly smaller, 18 to 30 cm in length and 6 to 8 cm in width.

Elephant bone tools also show more working, showing on average 17.3 flake removal scars, compared to an average of 13.3 scars on Hippopotamus bone tools. Among the fifteen tools made from unidentified Animals, seven are comparable to Elephant or Hippopotamus bone tools in size, with similar numbers of scars, while eight are smaller, with an average of six flaking scars. The preferred method of tool making appears to have been to first remove large flakes to give the tools its shape, then remove smaller flakes to regularize the edge surfaces. Experimentally braking bones for marrow-extraction produced scars significantly shorter than the initial flaking used in tool production at Frida Leakey Korongo West Gully, indicating deliberate intent from the outset. The shape of the scars is compatible with the use of hand-held hammerstones, although these would have needed to be large and heavy.

Six of the large-Mammal bone tools show a recurrent shape, with one crescent-shaped end and one pointed end, combined with a large notch on the middle part of the tool. This was achieved using an average of 16.8 flake removals, the majority of which are associated with the creation of the notch. The pointed end of the tool corresponds to the robust part of the diaphysis (middle section) of the bone, which the rounded end appears to be derived from the metaphysis (wider, end-part) of the bone. 

Large bone tools made on diaphysis fragments. (a) Elephant humerus (accession number T79L10-9047). (b) Hippopotamus femur (accession number T79L10-18461). Scale bars are 5 cm. De la Torre et al. (2025).

The bone tools at Frida Leakey Korongo West Gully are larger, heavier, more elongated, and more worked than stone tools from the same site, suggesting that bone was deliberately chosen as the material of choice for such tools. The tool makers appear to have a good understanding of the properties bone as a material, and the anatomy of the Animals from which it was derived, preferentially choosing Elephant bone even when this was not fresh, and consistently making tools to the same plan, following a standard flaking pattern.

Recurrent distal fracture patterns on additional bone tools. (1) Tibia diaphysis of cf. Hippopotamus (accession number T69L20-1872; dimensions 222 × 80 × 54 mm). (2) Accession number T69L20-3633. (3) Accession number T77L64-823. (4) Elephant long bone diaphysis (accession number T78L84-75; dimensions 353 × 103 × 53 mm). Each scale bar segment is 1 cm. De la Torre et al. (2025).

The T69 technology from Frida Leakey Korongo West Gully represents evidence for bone tool production by Hominins 1.5 million years ago. Previously, our knowledge of bone tool use in the Early Stone Age consisted of bone fragments which had apparently been used as tools without modification, and isolated tools with possible evidence of working and/or dubious stratigraphy (dating), with the regular appearance of deliberately made bifacial bone tools not occurring till after 500 000 years ago. 

The Frida Leakey Korongo West Gully discovery shows that Hominins had a complex tool industry which included the production of large knapped bones a million years before bifaced bone tools become common. These tools date to a key period in technological innovation, during which the early Acheulean technology was replacing the late Oldowan technology, a change which probably reflects a general increase in behavioural complexity. This increased behavioural complexity appears to have included a greater ability to select materials, a better ability to imagine the shape of a finished tool and work towards it, and morse sophisticated knapping techniques to reach that end. At this point bifacial tools were starting to appear, forming a minor part of tool assemblages and not reaching the large sizes seen in later Acheulean assemblages. 

Hominins at this stage are known to have been scavenging the carcasses of large Mammals and actively developing butchery techniques, which would have made bone a readily available material. It is possible the large bone tools from the Frida Leakey Korongo West Gully fulfilled the same role as the large bifacial tools of later Acheulean assemblages, and that the development of these more advanced stone tools led to the abandonment of large bone tools. In this scenario, the bifacial bone tools of the Middle Pleistocene might represent a reversion to bone use among populations lacking access to good lithic material.

An alternative hypothesis is that bone technologies appeared and disappeared several times over the course of the Pleistocene, all being being slightly more common in the Early Stone Age than previously realised. Either way, Early Pleistocene use of bone tools is clearly an under-reported phenomenon, possibly due to collection bias (archaeologists finding stone tools, because that is what they are looking for). Further research may reveal earlier use of bone tools, as well as a more widespread use of bone as a tool making material in the Early and Middle Pleistocene.

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