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Science and economics of the guano: Mona Island in Puerto Rico, nineteenth century

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Abstract

This paper presents a brief history of the island of Mona from the fields of geology and archeology to dimension space and the social actors involved, and the various activities that took effect in the second half of the XIX century to exploit its natural resources with the participation of government officials, scientists, entrepreneurs and workers with a clear purpose: to diversify production activities in response to the weakness of the economic model and the cyclical crises presented on the island before the sugar and coffee price shocks in the international market. Peru's successful experience with the exploitation and commercialization of guano in the European markets, generated many legends in Puerto Rico about the economic potential that could contain the islands of Mona and Monito, which in the best case would remain in the collective imagination as a utopia in the search and the implementation of economic development in Puerto Rico.

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Isla de Mona consists of a raised table-top Miocene-Pliocene reef platform bounded on three sides by vertical cliffs, up to 80 m high. Hundreds of caves ring the periphery of the island and are preferentially developed in, but not limited to, the Lirio Limestone/Isla de Mona Dolomite contact. These flank margin caves originally formed at sea level and are now exposed at various levels by tectonic uplift of the island (Franbk 1983; Mylroie et al. 1995b). Wall cusps, a characteristic feature of flank margin caves, are ubiquitois features. Comparisons among similar caves formed in the Bahamas and Isla de Mona reveal the same overall morphology throughout the entire range of sizes and complexities. The coincidence of the primary cave development zone with the Lirio Limestone/Isla de Mona Dolomite contact may result from syngenetic speleogenesis and dolomitization rather than preferential dissolution along a lithologic boundary. Tectonic uplift and glacioeustatic sea level fluctuations produced caves at a variety of elevations. Speleothem dissolution took place in many caves under phreatic conditions, evidence these caves were flooded after an initial period of subaerial exposure and speleothem growth. Several features around the perimeter of the island are interpreted to be caves whose roofs were removed by surficial denudation processes. Several large closed depressions and dense pit cave fields are further evidence of surficial karst features. The cliff retreat around the island perimeter since the speleogenesis of the major cave systems is small based upon the distribution of the remnant cave sections.
Article
Charcoal fragments were collected from a mixed charcoal and bon deposit from a chamber in Cueva Negra, Isla de Mona Puerto Rico. Radiocarbon dating yielded a conventional 14C age of 380 ± 60 Radiocarbon Years before present. Considering the standard deviation in the 14C data, the range in possible calendar dates is from 1480 to 1655 AD. This time period encompasses the first contact between Taino population and Europeans, and the subsequent removal of the last of the Taino from the island to Puerto Rico in 1578.
Article
Isla de Mona, Puerto Rico is ringed by hundreds of flank margin caves (Frank 1993; Mylroie et al. 1995). In the late 1800s and early 1990s ~150 000 metric tons of phosphorite, altered bat guano, were mined from the caves. A high phosphate content made the phosphorite a valuable fertilizer (Wadsworth 1973). Briggs (1974) indicates the guano deposits have been exhausted from seven of the eight largest known cave systems on the island. Many relics from the guano mining days are still present in the caves and surrounding areas today.
Article
Tesis Univ. Granada. Departamento de Prehistoria y Arqueología. Leída el 9 de abril de 2010
Article
Incluye bibliografía e índice
Article
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