Showing posts with label Greater Antilles. Show all posts
Showing posts with label Greater Antilles. Show all posts

Friday, 31 October 2025

At least 56 dead after Hurricane Melissa sweeps across Jamaica, Cuba, and Haiti.

At least 56 people have died in Jamaica and Haiti after Hurricane Melissa swept across the Greater Antilles between 25 and 29 October 2025. The storm first appeared as a tropical depression off the coast of West Africa around 16 October, moving across the Atlantic Ocean, then passing through the Windward Islands on 19 October, before continuing to move westwards across the Caribbean Sea. The weather system began to intensify on 21 October, provoking meteorologists to give it the name Tropical Storm Melissa. On 25 October it began to intensify further, becoming a Category 5 storm early on 27 October. At the same time it changed its direction of movement sweeping northward towards Jamaica, where it made landfall near New Hope about midday on 28 October.

The path and strength of Hurricane Melissa. Thick line indicates the past path of the storm (till 3.00 pm GMT on Friday 31 October 2025), while the thin line indicates the predicted future path of the storm, and the dotted circles the margin of error at 9, 21, 33, 45, 69, and 93 hours ahead. Colour indicated the severity of the storm. Tropical Storm Risk.

Hurricane Melissa reached Jamaica as the joint most intense Hurricane ever to make land, tying with the Labor Day Hurricane of 1935 in having a pressure of only 892 millibars, and a maximum recorded windspeed of 406 km per hour - the highest ever recorded for a storm on Earth. Flooding was reported in the town of Old Harbour ahead of the storm, with much of the parish of Saint Elizabeth under water when it hit. Several villages in the parish are described as being obliterated by the combination of flood waters and high winds, as was the town of Mandeville in neighbouring Manchester Parish. Flooding was also reported in Montego Bay and Kingston, buildings collapsed in Falmouth, and a landslide was reported in Gordon Town. At least 19 people died on the island, including eight in Saint Elizabeth Parish, two (including an infant) in Saint James Parish, nine in Westemoreland Parish, and a pregnant woman in Petersfield.

Storm damage around  St. John's Anglican Church in Black River, Saint Elizabeth Parish, Jamaica, following the passage of Hurricane Melissa. Ricardo Makyn/AFP/Getty Images.

From Jamaica, the storm moved northward to Cuba, where it caused widespread flooding and damage to buildings in Santiago de Cuba Province, although there are no reports of any fatalities there. However, high rainfall associated with the the storm caused several rivers to bust their banks in neighbouring Haiti, where at least 30 people have died and about 20 more are still missing. Four people are also reported to have died in the Dominican Republic, again due to flooding.

Vehicles buried in mud after a river burst its banks in  Petit-Goâve, Haiti, following rains associated with Hurricane Melissa. Clarens Siffroy/AFP/Getty Images.

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 northwest Atlantic and eastern Pacific being referred to as hurricanes.

The formation of a tropical cyclone. Natural Disaster Management.

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.

The formation and impact of a storm surge. eSchoolToday.

Hurricane Melissa was the thirteenth named storm in the tropical Atlantic in 2025, the fifth storm to be elevated to hurricane status, and the third Category 5 hurricane of the season. It was also the strongest tropical storm measured anywhere on Earth in 2025, the joint most powerful storm ever to have made land, and produced the highest windspeed ever recorded from a storm on Earth. The size and frequency of such storms is directly linked to the temperature of the sea and the air above it, with rising global temperatures subsequently fuelling more and larger storms, and other extreme weather events in the Caribbean and other tropical regions.

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Friday, 28 February 2025

Magnitude 5.9 Earthquake to the northeast of the Dominican Republic.

The United States Geological Survey recorded a Magnitude 5.9 Earthquake at a depth of 46 km roughly 109 km to the northeast of the Dominican Republic, slightly before 1.50 am local time (slightly before 5.50 am GMT) on Tuesday 25 February 2025. There are no reports of any damage or injuries associated with this event, and nor was a tsunami warning issued but people have reported feeling it across the eastern Dominican Republic as well as on Puerto Rico.

The approximate location of the 25 February 2025 Puerto Rico Earthquake. USGS.

The Dominican Republic forms the eastern part of the island of La Hispaniola, in the Greater Antilles.  The island has a complex geological structure, with parts of it lying on three different tectonic plates, and two plate margins running east-to-west across the island. The northernmost part of the island lies on the North American Plate. This is divided from the Gonâve Microplate by the Septentrional Fault Zone, which runs through Rio San Juan, along the north coast of the Dominican Republic and Haiti, then across the Windward Passage and along the south coast of Cuba. The Gonâve Microplate is moving east relative to the North American Plate, pushed by the Mid-Cayman Spreading centre to the west of Jamaica. To the south the Gonâve Microplate is separated from the Caribbean Plate by the Enriquilo-Plantain Garden Fault Zone, which runs across Southern Haiti and the Dominican Republic. To the west the fault runs through central Jamaica. The Caribbean Plate is rotating clockwise, effectively moving east relative to the Gonâve Microplate.

Plate movements and fault zones around the Gonâve Microplate. Mike Norton/Wikimedia Commons.

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Friday, 27 December 2024

Magnitude 6.1 earthquake off the south coast of Cuba.

The National Seismological Research Service of Cuba recorded a Magnitude 6.1 Earthquake at a depth of 9 km, about 35 km off the south coast of Cuba at about 1.00 am local time (about 6.00 am GMT) on Monday 23 December 2024. The event was felt across eastern Cuba, Jamaica, and the Cayman Islands, and while there are no reports of any injuries, minor damage to buildings has been reported from across eastern Cuba, and several roads were blocked by landslides triggered by the Earthquake.

The approximate location of the 23 January 2024 Cuba Earthquake. USGS.

Cuba lies on the southern portion of the North American Plate, to the north of the Septentrional Fault Zone, which forms the boundary with the Gonâve Microplate, a small tectonic plate underlying northern Jamaica and most of the island of Hispaniola. The Gonâve Microplate is moving east relative to the North American Plate, pushed by the Mid-Cayman Spreading centre to the west of Jamaica.

To the south the Gonâve Microplate is separated from the Caribbean Plate by the Enriquilo-Plantain Garden Fault Zone, which runs across Southern Haiti and the Dominican Republic. To the west the fault runs through central Jamaica. The Caribbean Plate is rotating clockwise, effectively moving east relative to the Gonâve Microplate.

Plate movements and fault zones around the Gonâve Microplate. Mike Norton/Wikimedia Commons.

None of these movements are smooth, with rock formations at the boundaries of the plates constantly sticking together then breaking apart as the pressure from the plate movement builds up, triggering Earthquakes in the process.

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Wednesday, 7 June 2023

Four dead following Magnitude 4.9 Earthquake in Haiti.

The United States Geological Survey recorded a Magnitude 4.9 Earthquake at a depth of 10.0 km roughly 9 km to the northeast of the commune of Les Abricots on the northern side of the Tiburon Peninsula, Haiti, slightly after 5.10 am local time (slightly after 9.10 am GMT) on Tuesday 6 June 2023. Four people are known to have died following this event, and injuring more than 25, including several children. Three of the deceased are reported to be members of the same family, killed when their house collapsed. 

The approximate location of the 6 June 2023 Haiti Earthquake. USGS.

Haiti forms the western part of the island of La Hispaniola, in the Greater Antilles. The island has a complex geological structure, with parts of it lying on three different tectonic plates, and two plate margins running east-to-west across the island. The northernmost part of the island lies on the North American Plate. This is divided from the Gonâve Microplate by the Septentrional Fault Zone, which runs through Rio San Juan, along the north coast of the Dominican Republic and the Tiburon Peninsula of Haiti, then across the Windward Passage and along the south coast of Cuba. The Gonâve Microplate is moving east relative to the North American Plate, pushed by the Mid-Cayman Spreading centre to the west of Jamaica. To the south the Gonâve Microplate is separated from the Caribbean Plate by the Enriquilo-Plantain Garden Fault Zone, which runs across Southern Haiti and the Dominican Republic. To the west the fault runs through central Jamaica. The Caribbean Plate is rotating clockwise, effectively moving east relative to the Gonâve Microplate.

Plate movements and fault zones around the Gonâve Microplate. Mike Norton/Wikimedia Commons.

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Thursday, 16 February 2023

Neoponera vejestoria: A Ponerine Ant from Miocene Dominican Amber, and its implications for the evolution of the ecological niches occupied by Ants in the Greater Antilles.

The makeup of modern ecological communities is determined by three factors, speciation, migration, and extinction. The first two of these can be largely understood through the examination of extant species, but our knowledge of past extinction events is entirely derived from the fossil record. Extinction events can create opportunities for surviving species to adapt into vacant niches, but can also lead to the vanishing of those niches, and of co-dependent niches and the organisms that occupy them. Island ecosystems are particularly vulnerable to extinction events, and their ecological communities are therefore particularly prone to being modified in this way. This makes the fossil history of island ecosystems, which are likely to have been shaped by numerous extinction events. of particular interest to evolutionary ecologists, although very few islands have fossil deposits that record past faunas in sufficient detail to be useful.

The island of Hispaniola in the Greater Antilles is home to 126 indigenous Ant species, drawn from a wide range of Neotropical groups which occupy different ecological roles. The island is also home to an excellent Fossil Lagerstätte, the Dominican Amber deposits, from which over 1100 species of Early Miocene Insects, including 86 species of Ants. The fauna recorded in this amber deposit is very similar to that of the modern Neotropics, with 84 of the described Ant species being placed in extant Neotropical genera. However, about a third of the genera found in the fossil fauna, while still present in the wider Neotropics, are absent from not just Hispaniola, but the wider Greater Antilles island group, implying that they have suffered local extinctions over the 16 million years since the amber was deposited. The ancient and modern faunas were studied by biologist Edward O. Wilson in the 1980s, who concluded that larger species and those with more specialize ecologies were more likely to have gone extinct. Since Wilson carried out his study, considerably more has been learned about both the fossil and living Hispaniolan Ant faunas, but Wilson's observations remain unchallenged.

In a paper published in the journal BMC Biology on 8 February 2023, Gianpiero Fiorentino of the Federated Department of Biological Sciences at the New Jersey Instituteof Technology, John Lattke of the Departamento de Zoologia at the Universidade Federal Do Paraná,  Adrian Troya of the Departamento de Biología at the Escuela Politécnica Nacional, Christine Sosiak, also of the Federated Department of Biological Sciences at the New Jersey Institute of Technology, Minsoo Dong of the Applied Biology Program at Kangwon National University, and Phillip Barden, again of the Federated Department of Biological Sciences at the New Jersey Institute of Technology, and of the Division of Invertebrate Zoology at the American Museum of Natural History, describe a new species of Ponerine Ant from Miocene Dominican Amber, and discuss its implications for the evolution of the ecological niches occupied by Ants in the Greater Antilles.

The new species is assigned to the Subfamily Ponerinae, one of the largest and most diverse Ant families, both in ecological and morphological terms, and to the genus Neoponera, which is one of the more diverse genera of Neotropical Ponerine Ants, with 58 extant species, divided among seven species groups. The majority of Neoponera species are arboreal in habit, which is unusual in Ponerine Ants, although the genus is quite ecologically variable, with individual species having lifestyle strategies which vary from generalist ground-dwelling hunters, to specialist Termite raiders, to mutuaslistic relationships with certain Trees, which they protect from herbivores in return for food and nesting spaces. Despite this ecological adaptability, the genus Neoponera does not appear to do well in island ecosystems, with a few species in the Lesser Antilles but none in the Greater Antilles or on other Neotropical islands.

The new species is named Neoponera vejestoria, where 'vejestoria' derives from the Spanish 'vejestorio' meaning an old person or thing. The new species is placed in the genus Neoponera on the basis of its eyers, which are convex eyes placed at about head mid-length (found in all members of the genus), its well developed aroliae (a lobe on the leg to which the pretarsus attaches, again well developed in all members of the genus), and its slit-shaped propodeal spiracle (breathing opening, found in most members of the genus). It resembles members of the foetida and aenescens species groups, being assigned to the former group on the basis of its well developed malar carinae (ridges on its 'cheeks') and the positioning of its eyes.

Photomicrographs of Neoponera vejestoria (Holotype, MNHNSD FOS 18.01). (A) Head in frontal view. (B) Body in dorsal view. (C) Body in lateral view. Scale bars: (A) 1 mm; (B), (C) 2 mm. Fiorentino et al. (2023).

Based upon its morphology, Neoponera vejestoria is thought to have been a ground-dwelling generalist predator. It is the first known fossil species within the genus Neoponera, as well as the first known fossil member of the Pachycondyla genus group of Ponerine Ants from the Neotropics. It is also the largest predatory Ant known from the island of Hispaniola, either in the Miocene Amber deposits or today, although it would only be considered a medium-sized compared to a wider sampling of Ants; most modern Ants on Hispaniola are quite small, and while the size-range present in the Miocene Ants is larger, none of them are exceptionally large.

Neoponera vejestoria (Holotype BALDR0443): (A) Lateral view of mesosoma; (B) Dorsal view of posterior mesosoma and propodeum; (C) Lateral view of gaster; (D) Ventral view of mesosoma; (E) Metatarsi 1-5; (F) Arolium and metatarsal claws; (G) Metapleural gland. Scale bars: (A) 2 mm, (B) 1 mm, (C) 2 mm, (D) 2 mm, (E) 0.25 mm, (F) 0.125 mm, (G) 0.25 mm. Fiorentino et al. (2023).

Living Ponerine Ants are less morphologically variable and, on average, smaller than fossil species. This is less true if only Ants from Hispaniola are considered, where the largest Ponerine Ants other than Neoponera vejestoria, livening or fossil, all belong to the genus Odontomachus, which is the only Ant genus on the island today containing medium-sized species. However, it is likely that the Dominican Amber deposits do not represent the full range of Miocene Ants on the island, and that other larger Ants may have existed on the island at that time.

Computerized tomographic reconstruction of Neoponera vejestoria to illustrate difficult to view characters. (A) Head in front view; (B) Profile view of mesosoma and gaster; Dorsal view of head, posterior mesosoma, and propodeum as a computerized tomographic reconstruction (C) and as a photograph of the fossil (D). Fiorentino et al. (2023).

Fiorentino et al.'s study suggests that the fauna of Hispaniola has been shaped not just by the extinction of lineages of Ants, but also the loss of the ecological niches which they once occupied. Predatory Ants on the island have always tended to be on the small side, but the range of sizes was clearly greater in the Early Miocene than it is today. Furthermore, Ants with more specialized feeding strategies, such as the Blind Army Ants of the genus Neivamyrmex, the Trap-jaw Ants, Acanthognathus spp., and the subterranean predatory Ants, Acanthostichus spp., have also died out on the island. The discovery that the island was once occupied by the Ponerine Ant Neoponera vejestoria provides further evidence of the modification of the island's ecological community through the extinction of certain ecological traits. Neoponera vejestoria is at least a third larger than any living predatory Ant on the island, which is a conspicuous difference in size, and likely to have been a ground-nesting generalist predator, which is not in itself unusual.

Artistic reconstruction of Neoponera vejestoria. Minsoo Dong in Fiorentino et al. (2023).

The Ant fauna of the Miocene of the island of Hispaniola is likely to be severely under-represented in Dominican Amber. The amber was formed from a resin extruded by a Leguminous Tree, and therefore best preserves the Insects which lived on, or at least visited the canopy of these trees, as well as, to a lesser extent, species which lived on the ground beneath. Insects which lived elsewhere on the island are highly unlikely to have been preserved at all. This could well imply that the Miocene size-range of Ants on the island was wider than has been preserved in the fossil record. Other lineages of larger Ants besides Neoponera appear to have been lost on Hispaniola, such as the large-bodied genus Paraponera, which is found in Dominican amber, but absent from the Caribbean region today.

Mammals, and other Vertebrates, often face selective pressures against larger sizes when groups become isolated on islands, but this is much harder to demonstrate in Insects, although it has previously been demonstrated in Carabid Beetles on European islands.

Excluding Neoponera vejestoria, the largest Ant species found on Hispaniola in both the Miocene and modern faunas belong to the genus Odontomachus. These Ants are ground dwelling generalist predators, something they share with Ants of the genus Neoponera. Today, these two Ant genera are seldom encountered on the same island, with Odontomachus being found on Hispaniola and the other islands of the Greater Antilles, as well as Cocos, Barbados, and Tobago, while Neoponera is only found on the island of Margarita. Fiorentino et al. therefore consider it possible that the two types of Ant compete for similar niches, which may have been a driver of the extinction of Neoponera on Hispaniola.

The discovery of Neoponera in Dominican Amber highlights the fact that these deposits still have much to tell us about the Miocene fauna of Hispaniola, and the way in which the island's ecology has changed over time, despite over five decades of study on the subject.

Neoponera vejestoria is clearly a distinct species, but nevertheless is morphologically very similar to extant species in the same genus, something which has been observed in other Ants from Miocene Dominican Amber. Most modern members of the genus Neoponera inhabit specialist niches, and the group is predominantly arboreal today, but some members are still ground-dwelling generalist predators, and it has previously been suggested that this is likely to be the ancestral state for the genus, a hypothesis supported by the discovery of Neoponera vejestoria, although the alternative hypothesis, that Neoponera vejestoria had secondarily adopted a ground-dwelling generalist lifestyle as an adaptation to island life, cannot be excluded.

The discovery of Neoponera vejestoria also sheds light on the history of the wider  Pachycondyla genus group (which includes Pachycondyla, Neoponera, and Dinoponera, among others), which are important members of Neotropical ecosystems, being the first fossil Ant confidently placed within the group, and the first fossil member of an extant genus in the group. Other fossils have previously been referred to this group, but none of them with confidence, and  Fiorentino et al. suggest that all of these specimens need re-examination, to shed better light on the history of the group. Molecular clock estimates of the age of the genus Neoponera have suggested that it first appeared between 26 and 12 million years ago, while the foetida species group has been thought to be no more than 12 million years old. A better understanding of the fossil record of the Pachycondyla genus group would clearly lead to better calibration of these molecular estimates.

The discovery of Neoponera vejestoria provides a rare example of island extinction in the fossil record. This is almost certainly linked to the body size of the species, which is likely to have placed it at greater risk of extinction in an island ecosystem. As the ecological niche occupied by Neoponera vejestoria is still in existence, this demonstrates that a large size in itself is a threat to Ant species on islands.

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