scholarly journals Local Annual Survival and Seasonal Residency Rates of Semipalmated Sandpipers (Calidris Pusilla) in Puerto Rico

The Auk ◽  
2007 ◽  
Vol 124 (4) ◽  
pp. 1397-1406 ◽  
Author(s):  
Susan M. Rice ◽  
Jaime A. Collazo ◽  
Mathew W. Alldredge ◽  
Brian A. Harrington ◽  
Allen R. Lewis

Abstract We report seasonal residency and local annual survival rates of migratory Semipalmated Sandpipers (Calidris pusilla) at the Cabo Rojo salt flats, Puerto Rico. Residency rate (daily probability of remaining on the flats) was 0.991 ± 0.001 (x̄ ± SE), yielding a mean length of stay of 110 days. This finding supports the inclusion of the Caribbean as part of the species' winter range. Average estimated percentage of fat was low but increased throughout the season, which suggests that birds replenish some spent fat reserves and strive for energetic maintenance. Local annual survival rate was 0.62 ± 0.04, within the range of values reported for breeding populations at Manitoba and Alaska (0.53–0.76). The similarity was not unexpected because estimates were obtained annually but at opposite sites of their annual migratory movements. Birds captured at the salt flats appeared to be a mix of birds from various parts of the breeding range, judging from morphology (culmen's coefficient of variation = 9.1, n = 106). This suggested that origin (breeding area) of birds and their proportion in the data should be ascertained and accounted for in analyses to glean the full conservation implications of winter-based annual survival estimates. Those data are needed to unravel the possibility that individuals of distinct populations are affected by differential mortality factors across different migratory routes. Mean length of stay strongly suggested that habitat quality at the salt flats was high. Rainfall and tidal flow combine to increase food availability during fall. The salt flats dry up gradually toward late January, at the onset of the dry season. Semipalmated Sandpipers may move west to other Greater Antilles or south to sites such as coastal Surinam until the onset of spring migration. They are not an oversummering species at the salt flats. Conservation efforts in the Caribbean region require understanding the dynamics of this species throughout winter to protect essential habitat. Tasas de Supervivencia Anual Local y de Residencia Estacional de Calidris pusilla en Puerto Rico

The Auk ◽  
2007 ◽  
Vol 124 (4) ◽  
pp. 1397 ◽  
Author(s):  
Susan M. Rice ◽  
Jaime A. Collazo ◽  
Mathew W. Alldredge ◽  
Brian A. Harrington ◽  
Allen R. Lewis

2021 ◽  
Author(s):  
Leny Montheil ◽  
Douwe Van Hinsbergen ◽  
Philippe Münch ◽  
Pierre Camps ◽  
Mélody Philippon

<p>Since the Eocene, the northeastern corner of the Caribbean plate is shaped by the indentation of the buoyant Bahamas platform with the Greater Caribbean Arc, the suture of a portion of the Antillean subduction zone along Cuba and Hispaniola and the subsequent relocation of the plate boundary along the strike slip Cayman Trough. Puzzlingly enough, these major re-arrangements followed a plate motion reorganization (Boschmann et al., 2014). During this kinematic reorganization, the Lesser Antilles trench initiated (or subduction intensified) along the eastern boundary of the Caribbean plate and progressively bent, resulting in an increase of subduction obliquity from south to north (Philippon et al., 2020a). This curvature has been, and still may be, associated with deformation within the Caribbean plate. Interestingly, in the 10-15 Ma following the plate reorganization, a hypothetical, now submerged “landbridge” allowed the dispersion of terrestrial fauna from South America to the Greater Antilles: the GAARlandia landbridge (land of Greater Antilles and Aves Ridge). Although it has been recently shown that Puerto Rico and the Northern Lesser Antilles where connected once forming a land mass called GrANoLA around 33-35 Ma (Philippon et al., 2020b), these rapids and drastics geodynamical changes may have impacted the regional paleogeography, which remains to be constrained. The intraplate deformation in the north-est Caribbean region associated with the plate reorganization, the Bahamas indentation, and the plate boundary curvature likely hold the key to (part of) the evolution of this landbridge.<br>At present day, the N-Eastern border of the Caribbean plate shows parallel to the trench faults dissecting the plate in a sliver-like manner. This “sliver” is cross cutted by perpendicular to the trench faults in four crustal blocks: Gonave, Hispaniola, Puerto Rico and the Northern Lesser Antilles. Present-day and past kinematics of these blocks, and even their existence, are still debated.</p><p>In this study, in the course of the French GAARAnti project, we focus on paleomagnetically determined vertical axis rotations that affected Puerto Rico and the Northern Lesser Antilles blocks since the Eocene, and use these to inform kinematic reconstructions constrained by regional structural analysis and Ar<sup>40</sup>-Ar<sup>39</sup> geochronology. These reconstructions will be used to refine the paleogeographic evolution of the NEastern edge of the Caribbean plate since the Eocene in order test the GAARlandia hypothesis.</p><p>A new set of paleomagnetic data (180 Oligo-Miocene specimens of sediments sampled in 18 sites) indicates that the Puerto Rico block underwent an early to mid-Miocene 10° counterclockwise (CCW) rotation. This result clearly differs from those of Reid et al., 1991 who concluded a Late Miocene 25° CCW rotation and that is currently used by the community to interpret the tectonic history of the northeastern Caribbean plate. The use of a larger dataset, that geographically covers the entire island, and of a more recent reference frame explain the difference observed between the two results. This new result will lead to a re-interpretation of the tectonic evolution of the region that will be integrated in a regional kinematic reconstruction.</p>


2020 ◽  
Vol 3 (2) ◽  
Author(s):  
Adrián Fuentes-Luque ◽  
Pabsi Livmar González-Irizarry

Even though Audiovisual Translation (AVT) is growing and flourishing throughout the world, it is practically unheard-of in the Caribbean, where accessibility faces an even bleaker existence. The circumstances of the deaf and hard of hearing (also referred to as D/deaf) are no less alarming: social barriers and exclusion are widespread. This paper emphasizes the need to make subtitles accessible in the Spanish-speaking Caribbean, specifically on the islands of Puerto Rico, Cuba, and the Dominican Republic, and underscores the challenges faced by the D/deaf communities on each island. Our research focuses on issues like AVT laws and regulations, the habits of viewers of audiovisual (AV) products, and literacy and limitations on each island. This paper also examines the different types of D/deaf audiovisual consumers in the Spanish-speaking Caribbean and the difficulties each community faces when accessing media and entertainment. Our research reveals the current state of AVT accessibility in this region and provides a foundation for influencing legislators to begin enforcing AVT regulations and drafting SDH guidelines.


2020 ◽  
Vol 16 (4) ◽  
pp. 20190947 ◽  
Author(s):  
David C. Blackburn ◽  
Rachel M. Keeffe ◽  
María C. Vallejo-Pareja ◽  
Jorge Vélez-Juarbe

The nearly 200 species of direct-developing frogs in the genus Eleutherodactylus (the Caribbean landfrogs, which include the coquís) comprise an important lineage for understanding the evolution and historical biogeography of the Caribbean. Time-calibrated molecular phylogenies provide indirect evidence for the processes that shaped the modern anuran fauna, but there is little direct evidence from the fossil record of Caribbean frogs about their distributions in the past. We report a distal humerus of a frog from the Oligocene (approx. 29 Ma) of Puerto Rico that represents the earliest known fossil frog from any Caribbean island. Based on its prominent rounded distal humeral head, distally projecting entepicondyle, and reduced ectepicondyle, we refer it to the genus Eleutherodactylus . This fossil provides additional support for an early arrival of some groups of terrestrial vertebrates to the Greater Antilles and corroborates previous estimates based on molecular phylogenies suggesting that this diverse Caribbean lineage was present in the islands by the mid-Cenozoic.


2010 ◽  
Vol 132 (3) ◽  
Author(s):  
M. E. Angeles ◽  
J. E. González ◽  
D. J. Erickson ◽  
J. L. Hernández

Assessment of renewable energy resources such as surface solar radiation and wind current has great relevance in the development of local and regional energy policies. This paper examines the variability and availability of these resources as a function of possible climate changes for the Caribbean region. Global climate changes have been reported in the last decades, causing changes in the atmospheric dynamics, which affects the net solar radiation balance at the surface and the wind strength and direction. For this investigation, the future climate changes for the Caribbean are predicted using the parallel climate model (PCM) and it is coupled with the numerical model regional atmospheric modeling system (RAMS) to simulate the solar and wind energy spatial patterns changes for the specific case of the island of Puerto Rico. Numerical results from PCM indicate that the Caribbean basin from 2041 to 2055 will experience a slight decrease in the net surface solar radiation (with respect to the years 1996–2010), which is more pronounced in the western Caribbean sea. Results also indicate that the easterly winds have a tendency to increase in its magnitude, especially from the years 2070 to 2098. The regional model showed that important areas to collect solar energy are located in the eastern side of Puerto Rico, while the more intense wind speed is placed around the coast. A future climate change is expected in the Caribbean that will result in higher energy demands, but both renewable energy sources will have enough intensity to be used in the future as alternative energy resources to mitigate future climate changes.


2014 ◽  
Author(s):  
Lisa Nicole Jennings ◽  
Jamison Douglas ◽  
Emrys Treasure ◽  
Grizelle González

2021 ◽  
Author(s):  
Louise Cordrie ◽  
Audrey Gailler ◽  
Nathalie Feuillet

<p><span>The arc of the Lesser Antilles is one of the most quiet subduction zone in the world. In this region, the convergence of the Atlantic and the Caribbean plates is low (</span><span>few </span><span>mm/year) and most of the seismicity is a</span><span>n</span><span> intraplate and crustal seismicity. Among the Mw>7 earthquakes recorded in the historical catalog (1690 near Barbuda, 1843 near Guadeloupe, 1867 near the Virgin Islands, 1839 offshore Martinica, 1969 offshore Dominica, 1974 near Antigua), only the 1839 and 1843 events are suspected to be interplate earthquakes. The 1867 Virgin Island earthquake generated an important tsunami with waves of 10m that devastated the closest islands. A tsunami followed the 1843 earthquake but without much damage. These two events are the only known damaging tsunami in this region, but another older one might be added to the list. Indeed, an increasing number of tsunami deposits have been identified in the recent years on several islands of the arc, all of them being around 500 years old (~1450 AD). These deposits are all located in the northern segment of the arc, between Antigua and Puerto-Rico, in Anegada, St-Thomas (Virgin Islands), Anguilla </span><span>and</span><span> Scrub islands. There is </span><span>unfortunately</span><span> no record and no testimonies of an extreme event at that time.</span></p><p><span>The northern segment of the arc is particularly complex because located at the transition </span><span>between</span><span> the Greater Antilles </span><span>and the Lesser Antilles</span><span>. </span><span>It</span><span> is crossed by the Anegada Passage, a series of faults and basins cutting through the arc, which defines the limit between the Puerto-Rico micro-plate and the Caribbean plate. This passage and the numerous intra-arc fault systems present between the islands are active and likely compensate for the plates motion. The very low slip deficit detected with GPS measurements at the subduction contacts of Puerto-Rico and the Lesser Antilles indicates that the interface from Guadeloupe to Puerto-Rico can be considered as totally uncoupled or holding the characteristics of a very long seismic cycle. A tsunami generated by an extreme event 500 years ago in this region could be related to </span><span>intra-arc, outer-rise,</span><span> intraplate </span><span>or</span><span> interface fault rupture. The identification of the source </span><span>would</span><span> enable a better understanding of the seismic cycle and the dynamic of this part of the arc.</span></p><p><span>This study lists </span><span>and set models of</span><span> all the potential faults that could trigger an earthquake in the area encompassing the three islands : Anguilla, Anegada and StThomas. </span><span>We have created high-resolution bathymetric grids and</span><span> performed tsunami simulations </span><span>for each fault model</span><span>. </span><span>W</span><span>e uses run-up models to compare the simulated wave heights </span><span>and run-up distance</span><span> to all the deposits heights </span><span>and positions</span><span>. The magnitudes of our fault models range between 7 and </span><span>9,</span><span> but very few of them generate a strong enough tsunami t</span><span>o</span> <span>match</span><span> the observ</span><span>ed deposits</span><span>.</span></p>


Waterbirds ◽  
2016 ◽  
Vol 39 (3) ◽  
pp. 250-259
Author(s):  
Morgan A. Parks ◽  
Jaime A. Collazo ◽  
Katsí R. Ramos Álvarez

1970 ◽  
Vol 48 (5) ◽  
pp. 1093-1097 ◽  
Author(s):  
J. R. Tamsitt ◽  
Irving Fox

Twenty-eight species of ectoparasites, including one flea, one chigger, two ticks, six mites, and 18 streblids, are listed for 18 species of bats from Colombia, Guyana, Jamaica, and Puerto Rico. Most are new host or geographic records. Distributional observations are included when available.


Author(s):  
David Eduardo Barreto Sánchez ◽  
aura Gutiérrez Escobar ◽  
Catalina Toro Pérez ◽  
Line Algoed ◽  
Pambana Bassett ◽  
...  

Through an interdisciplinary conversation in the context of the project: Food Insecurity in Times of Climate Change: Sharing and Learning from Bottom-up Responses in the Caribbean Region, we expose the voices, history and knowledge of local communities and activists in Barbuda, Belize, Colombia (San Andres and Providencia), Jamaica and Puerto Rico to the food insecurity and ecological crisis in the Caribbean. The composite effect of climate injustice and the COVID-19 pandemic is outlined as anthropogenic crises that thrive on inequality and dependency in the Caribbean. The community experiences of the project countries reveal an emergence of knowledge and diverse ways of producing food and relating to the environment as alternatives to development. It is a criticism of the solutions imposed from above that ignore the knowledge, needs and practices of popular ecologies in the Caribbean.


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