Showing posts with label Puerto Rico. Show all posts
Showing posts with label Puerto Rico. Show all posts

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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Sunday, 28 June 2020

Magnitude 4.8 Earthquake beneath southern Puerto Rico.

The United States Geological Survey recorded a Magnitude 4.8 Earthquake at a depth of 11.0 km roughly 5 km to the southwest of the town of Guánica in southern Puerto Rico, slightly after 2.40 am local time (slightly after 6.40 am GMT) on Sunday 28 June 2020 . There are no reports of any casualties or serious damage, though the quake was felt across the whole of Peurto Rico, as well as parts of the neighbouring  Dominican Republic.

The approximate location of the 28 June 2020 Puerto Rico Earthquake. USGS.

Puerto Rico is located at the northeastern fringe of the Caribbean Tectonic Plate. The Atlantic Plate (strictly speaking, an extension of the South American Plate which runs to the northeast of the Caribbean) is being subducted beneath this. The subduction of the Atlantic Plate beneath the Caribbean Plate is not a smooth process, with the two plates constantly sticking together then breaking apart as the tectonic pressure builds up, causing Earthquakes in the process, though since the boundary between the two plates is some way to the north and east of the islands, Earthquakes in this area tend to be both deep and offshore, which lessens their destructive potential.
 
The subduction of the Atlantic Plate beneath the Caribbean Plate fuels the volcanoes of the Lesser Antilles Volcanic Arc. George Pararas-Carayannis.
 
Witness accounts of quakes can help geologists to understand these events and the rock structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) you can report it to the USGS here.

See also...

https://sciencythoughts.blogspot.com/2019/12/magnitude-50-earthquake-off-south-coast.htmlhttps://sciencythoughts.blogspot.com/2019/09/magnitude-60-earthquake-to-northwest-of.html
https://sciencythoughts.blogspot.com/2018/02/magnitude-52-earthquake-to-north-of.htmlhttps://sciencythoughts.blogspot.com/2017/09/fifty-nine-confirmed-deaths-as.html
https://sciencythoughts.blogspot.com/2017/09/hurricane-irma-leaves-widespread.htmlhttps://sciencythoughts.blogspot.com/2017/08/magnitude-48-earthquake-to-north-of.html

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Saturday, 6 June 2020

Spirobranchus spp.: Christmas Tree Worms associated with new hosts found in Puerto Rico and the Netherlands Antilles.

Caribbean Christmas Tree Worms, Spirobranchus spp., are considered host generalists in their associations with Anthozoan (Scleractinia) and Hydrozoan (Millepora) Stony Corals. As planktonic larvae, they settle on Coral surfaces and start secreting a calcareous tube to be used as a dwelling. This tube usually becomes overgrown by the host Coral (except for its opening) and may get encapsulated deep inside the Coral skeleton. In this manner, the well-protected Worms grow and survive predation and other hazards, allowing them to live for over four decades. When the host Corals are overgrown by other organisms, such as Octocorals and Sponges, these may act as secondary hosts.

In a paper published in the journal Diversity on 21 March 2020, Bert Hoeksema of the Taxonomy and Systematics Group at the Naturalis Biodiversity Center, the Groningen Institute for Evolutionary Life Sciences at the University of Groningen, and the Institute of Biology Leiden at Leiden University, Jaaziel García-Hernández of the Marine Genomic Biodiversity Laboratory at the University of Puerto Rico - Mayagüez, Godfried van Moorsel of Ecosub and the ANEMOON Foundation, Gabriël Olthof also of the Taxonomy and Systematics Group at the Naturalis Biodiversity Center, and the Institute of Biology Leiden at Leiden University, and Harry ten Hove, again of the Taxonomy and Systematics Group at the Naturalis Biodiversity Center, report two new primary hosts (Scleractinians) and two new secondary hosts (a Zoantharian Soft Coral and an Ascidian colonial Sea Squirt), discovered during recent surveys (2015–2019) in the southern and eastern Caribbean, as well as in the Greater Antilles.

The Coral–Worm associations occurred in shallow subtidal water (less than 4 m depth), with the Knobby Brain Coral, Pseudodiploria clivosa, hosting Spirobranchus giganteus at St. Eustatius in the northern Leeward Islands, and the Golfball Coral, Favia fragum, hosting both Spirobranchus giganteus and Spirobranchus polycerus at Bonaire in the southern Leeward Islands. The secondary host observations, both for Spirobranchus giganteus, involved the Zoantharian Palythoa caribaeorum at Puerto Rico and the Ascidian Trididemnum solidum at Bonaire and Curaçao. Palythoa caribaeorum represents a first record as a secondary host for a species of the order Zoantharia. Until now, the only other Anthozoan secondary hosts were species in the order Alcyonacea (subclass Octorallia), whereas Trididemnum solidum represents an entirely new host phylum, the Chordata. The only other non-Anthozoan secondary hosts known to date are Sponges (Porifera).

A Coral of Pseudodiploria clivosa at 2 m depth, Scubaqua House Reef, St. Eustatius, Eastern Caribbean (2015) hosting Spirobranchus giganteus: (a) overall view and (b) close-up. Hoeksema et al. (2020).

The two new Scleractinian hosts are both typical for shallow subtidal water near the shoreline (less than 4 m depth), where a lack of previous surveys may explain why they have not previously been reported. The new records of secondary hosts are remarkable because these encrusting Animals are known to be aggressive in competition for space with Scleractinians by allelopathy (the production of harmful biochemicals) and can be abundant on shallow reef flats and slopes, where they usually outcompete and kill Scleractinian Corals by overgrowing them. In both cases, the Christmas Tree Worms survive by withstanding this overgrowth and maintain an open space near the tube opening.

Favia fragum hosting Spirobranchus spp. at 3–4 m depth, dive site 'Front Porch', Bonaire, Southern Caribbean (2019). (a)–(c) Spirobranchus giganteus: overall view (a), overgrown tube section indicated by red arrow (b); antler-shaped opercular spines showing dark pink colouration indicated by yellow arrow (c). (d) Spirobranchus polycerus: two individuals, one showing white spines on its operculum (blue arrow). Hoeksema et al. (2020).

Hoeksema et al.'s new host records confirm two Caribbean Christmas tree worms as generalist symbionts capable of infesting a large spectrum of host Corals. They are also strong survivors when their primary hosts become overgrown by more aggressive competitors for space. Previous host records mostly concern  Spirobranchus giganteus, but Hoeksema et al. also report a new host Coral for Spirobranchus polycerus. This worm species occurs in shallow water (less than 4 m depth), whereas Spirobranchus giganteus is commonly found down to 40 m depth. Both Spirobranchus species can easily be distinguished, as Spirobranchus giganteus shows long dark pink opercular spines, whereas those of Spirobranchus polycerus are short and white. Furthermore, Spirobranchus giganteus may be larger than Spirobranchus polycerus and usually shows six to seven (maximum eight) whorls in its branchial spires, whereas Spirobranchus polycerus has two to three (maximum five).

Palythoa caribaeorum acting as a secondary host for Spirobranchus giganteus at 5 m depth, Cayo Media Luna (La Parguera Natural Reserve), Puerto Rico, Greater Antilles (2017): (a) Worm extended and (b) retracted, showing the tube opening surrounded by dead Coral; damage to the Zoantharian host caused by the operculum of the extended Worm indicated by a black arrow. Hoeksema et al. (2020).

Hoeksema et al.'s observations suggest that future surveys may discover other hosts for both Spirobranchus species with the possibility of more host overlap. Whether such host sharing is related to their phylogenetic affinities or to ecological similarities (e.g., overlapping bathymetric distributions) is an open question that merits assessment.

Trididemnum solidum acting as a secondary host for Spirobranchus giganteus in the Southern Caribbean: (a), (b) dive site 'Thousand Steps', Bonaire (2019); (c) Marie Pampoen, Curaçao, 12 m depth (2017); (d), (e) Daaibooi Bay, Curaçao (2017). Extended Worms (a), (d) and the same individuals retracted, showing an open space in front of the Worm tube mouth (b), (e). Hoeksema et al. (2020).

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Sunday, 29 December 2019

Magnitude 5.0 Earthquake off the south coast of Puerto Rico.

The United States Geological Survey recorded a Magnitude 5.0 Earthquake at a depth of 6.0 km roughly 10 km off the south coast of Puerto Rico, slightly after 9.05 pm local time on Saturday 28 December 2019 (slightly after 1.05 am on Sunday 29 December GMT). There are no reports of any casualties or serious damage, though the quake was felt across Peurto Rico.
 
The approximate location of the 28 September 2019 Puerto Rico Earthquake. USGS.
 
Puerto Rico is located at the northeastern fringe of the Caribbean Tectonic Plate. The Atlantic Plate (strictly speaking, an extension of the South American Plate which runs to the northeast of the Caribbean) is being subducted beneath this. The subduction of the Atlantic Plate beneath the Caribbean Plate is not a smooth process, with the two plates constantly sticking together then breaking apart as the tectonic pressure builds up, causing Earthquakes in the process, though since the boundary between the two plates is some way to the north and east of the islands, Earthquakes in this area tend to be both deep and offshore, which lessens their destructive potential.
 
 The subduction of the Atlantic Plate beneath the Caribbean Plate fuels the volcanoes of the Lesser Antilles Volcanic Arc. George Pararas-Carayannis.
 
Witness accounts of quakes can help geologists to understand these events and the rock structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) you can report it to the USGS here.
 
See also...
 
https://sciencythoughts.blogspot.com/2019/09/magnitude-60-earthquake-to-northwest-of.htmlhttps://sciencythoughts.blogspot.com/2017/09/hurricane-irma-kills-forty-two-in.html
https://sciencythoughts.blogspot.com/2017/08/magnitude-48-earthquake-to-north-of.htmlhttps://sciencythoughts.blogspot.com/2015/08/tropical-storm-erika-kills-at-least-25.html
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