Slave Raiders vs. Friars: Tierra Firme, 1513–1522

2017 ◽  
Vol 74 (2) ◽  
pp. 139-170
Author(s):  
Erin Stone

In early 1515, a small Spanish expedition set sail for the province of Cumaná, located along the coast of what was then called Tierra Firme (an area spanning much of present-day Central and South America). Nominally, the squadron, led by Spanish scribe Gomez de Ribera, was sent to punish a group of “Carib” Indians who had recently attacked and killed two Spaniards on the small island of San Vicente. Once caught, these “Caribs” would be enslaved and sold in the markets of Española, Puerto Rico, or Cuba. Caribs, though speakers of the Arawakan language, were inhabitants of the Lesser Antilles and were likely culturally and politically distinct from the Taíno of the Greater Antilles. Inhabitants of the Lesser Antilles first received the ethnic label of Carib during Christopher Columbus's second voyage in 1493. Over time, Europeans exacerbated the pre-Columbian divide between Caribs and Taínos, creating a colonial dichotomy that helped the Spanish to expand the indigenous slave trade. By the third decade of colonization, or the time of Ribera's expedition, the Spanish had begun labeling all rebellious Indians as Caribs or cannibals so as to legally enslave them.

Author(s):  

Abstract A new distribution map is provided for Nematospora coryli Peglion. Hosts: Cotton (Gossypium), Coffee (Coffea), Citrus, etc. Information is given on the geographical distribution in AFRICA, Central African Republic, Gambia, Kenya, Madagascar, Malawi, South Africa, Tanzania, Uganda, Zaire, Zambia, Zimbabwe, ASIA, Burma, China, Indonesia, Iran, Iraq, Japan, Philippines, Sri Lanka, Taiwan, EUROPE, Italy, NORTH AMERICA, Mexico, USA (California, Florida N. and South Carolina, Oklahoma, Va), CENTRAL AMERICA & WEST INDIES, Cuba, Jamaica, Lesser, Antilles, Puerto Rico, SOUTH AMERICA, Brazil (Sao Paulo).


2008 ◽  
Vol 19 (1) ◽  
pp. 47-63 ◽  
Author(s):  
Reniel Rodríguez Ramos ◽  
Elvis Babilonia ◽  
L. Antonio Curet ◽  
Jorge Ulloa

Pottery in contexts that predate the entrance of Arawak societies to the Antilles (500 B.C.) by at least one millennium demand a reassessment of the introduction of this technology to the islands. We summarize the available evidence of what we term the Pre-Arawak Pottery horizon and address the social implications of the introduction of such technology to the insular Caribbean, based on the role of pots as tools. We show that this early pottery is more widespread than originally thought, extending from Cuba to Hispanola and perhaps to Puerto Rico and the Lesser Antilles as well. We argue that the paucity of early ceramic contexts discovered thus far could have resulted from the consideration of pottery as intrusive in Pre-Arawak contexts and because of its technological and stylistic overlap with wares associated to the Ostionoid series (A.D. 600-1500) of the Greater Antilles. Based on this evidence, we conclude by suggesting that some of the post-Saladoid manifestations that have been identified in the islands could have resulted from a multifocal development of these pre-Arawak cultures rather than simply from the divergent evolution of Saladoid societies as has been argued thus far.


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>


2021 ◽  
Vol 217 ◽  
pp. 103617
Author(s):  
Jean-Jacques Cornée ◽  
Philippe Münch ◽  
Mélody Philippon ◽  
Marcelle BouDagher-Fadel ◽  
Frédéric Quillévéré ◽  
...  

2003 ◽  
Vol 14 (3) ◽  
pp. 323-338 ◽  
Author(s):  
Richard T. Callaghan

AbstractComputer simulations are used to shed light on the probable origins of the earliest Preceramic cultures of the Greater Antilles and to understand the navigation skills necessary for island colonization. These cultures, dating to between ca. 4000 B.C. and 2000 B.C., are found on Cuba, Hispaniola, and possibly Puerto Rico. Two areas, northern South America and northern Central America, have assemblages that bear resemblance to the assemblages of the Greater Antilles, but there are important differences. Chance discovery of the Greater Antilles is possible from three areas: northern South America, northern Central America, and southern Florida. Directed voyages have a high degree of success from all three areas. However, voyages from northern South America require the least navigational skill, making it the most likely source of colonization. From northern Central America, foreknowledge of the islands appears to be required, while directed voyages from southern Florida encounter considerable risk.


Crustaceana ◽  
2016 ◽  
Vol 89 (14) ◽  
pp. 1717-1728 ◽  
Author(s):  
Theodor S. Poettinger ◽  
Sebastian Klaus ◽  
Christoph D. Schubart

The primary freshwater crab family Pseudothelphusidae is distributed with almost 300 described species from northern Mexico to the southern tributaries of the Amazon, including most of the Greater and Lesser Antilles. Its systematic grouping is solely based on morphological characters. The most recent and commonly applied classification distinguishes two subfamilies, the Epilobocerinae on the Greater Antilles, and the Pseudothelphusinae on the mainland of Central and South America and the Lesser Antilles (Rodríguez, 1982). In addition, several tribes are recognized based on the morphology of the first pair of male pleopods, the so called gonopods: the Pseudothelphusini, the Potamocarcinini, the Hypolobocerini, the Kingsleyini, and the Strengerianini. Here, we present the first molecular phylogeny of the Pseudothelphusidae, including representatives of all the subfamilies and tribes. The generaAchlidon,Allacanthos, andPtychophallusform a strongly supported monophyletic unit, clustering independently of the tribi where they have been classified so far. We present preliminary suggestions for a possibly derived taxonomy of the family.


2011 ◽  
Vol 22 (4) ◽  
pp. 573-594 ◽  
Author(s):  
John G. Crock ◽  
Nanny Carder

AbstractThe investigation of social inequality in the Caribbean mainly has focused on the larger islands of the Greater Antilles where ethnohistoric records and monumental architecture form the basis for analysis of precolumbian complex societies. This paper presents evidence for status differentiation in the Lesser Antilles on the small island of Anguilla within a deposit at the Sandy Hill site and evaluates associated archaeofauna for evidence of rank-based differences in food consumption. When compared with three other sites, the higher density of status-related artifacts and higher densities of food remains at the Sandy Hill site are interpreted as the result of feasting. No evidence for inequality is observed in patterns of food consumption.


1976 ◽  
Vol 54 (21) ◽  
pp. 2465-2472 ◽  
Author(s):  
R. E. Hersey ◽  
S. P. Vander Kloet

Two species of Gaultheria have been reported from the Caribbean: G. domingensis is said to occur on the Greater Antillean island of Hispaniola and G. sphagnicola, for which the specific names of G. buxifolia and G. anastomosans (both species occurring in South America) have been listed in synonymy, is said to occur on the Lesser Antillean islands of Martinique and Guadeloupe. A close examination of living material from Martinique and of herbarium specimens from Martinique, South America. Hispaniola, and Mexico reveals the following: (1) the Martinique and Guadeloupe group is specifically distinct from the South American G. buxifolia and G. anastomosans groups; (2) the Lesser Antilles group and the Greater Antilles group should be placed in a single species with the name of G. domingensis; and (3) there is evidence for a possible Mexican origin for this one Caribbean species.


Author(s):  

Abstract A new distribution map is provided for Nematospora coryli Peglion. Hosts: Cotton (Gossypium), coffee (Coffea), Citrus, Corylus, Phaseolus and many others. Information is given on the geographical distribution in Africa, Central African Republic, Ethiopia, Gambia, Kenya, Madagascar, Malawi, Nigeria, South Africa, Tanzania, Uganda, Zaire, Zambia, Zimbabwe, Asia, China, Sichuan, India, Maharashtra, Assam, Indonesia, Java, Iran, Iraq, Japan, Myanmar, Philippines, Sri Lanka, Taiwan, Europe, Greece, Italy, Sicily, North America, Mexico, USA, Southern States, Central America & West Indies, Costa Rica, Cuba, Grenada, Jamaica, Lesser Antilles, Puerto Rico, South America, Brazil, Sao Paulo.


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>


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