Caribbean Landscapes and Their Biodiversity
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Economic Commission for Latin America and The
110 100 90 80 ° ° ° ° ECONOMIC COMMISSION FOR UNITED STATES OF AMERICA LATIN AMERICA AND THE CARIBBEAN 30° 30° Nassau Gulf of Mexico BAHAMAS La Habana Turks and ATLANTIC OCEAN CUBA Caicos Is. DOMINICAN co MEXICO i Is. REPUBLIC R gin to ir rgin I Cayman Is. r V Vi s. e S ish HAITI u it Mexico Kingston P U r P B 20 20° S ANTIGUA AND ° o a r JAMAICA t n BARBUDA BELIZE - SAINT KITTS a to Montserrat Belmopan u AND NEVIS D -P o Guadeloupe r m HONDURAS Caribbean Sea in in DOMINICA Martinique Guatemala ce go Tegucigalpa SAINT LUCIA GUATEMALA Netherlands BARBADOS NICARAGUA Aruba Antilles R r GRENADA SAINT VINCENT AND o Managua O d THE GRENADINES D a VA lv Port of Spain L a TRINIDAD AND SA n S San José EL Sa PANAMA Caracas TOBAGO COSTA RICA 10 Panamá town 10 ° rge ° VENEZUELA eo Medellín G G SURINAME Santa Fé U Paramaribo de Bogotá Y French Guiana A Cayenne N COLOMBIA A Equator Quito 0 ECUADOR 0 ° Galapagos Is. ° Guayaquil Manaus Belém PERU Recife BRAZIL 10° Lima 10° PACIFIC OCEAN La Paz Brasília BOLIVIA Sucre P 20 AR 20 ° A ° G U São Paulo A Rio de Janeiro Y Isla San Félix Asunción 100° 90° Isla San Ambrosio Members: Antigua and Barbuda Honduras Argentina Italy 30° Bahamas Jamaica Barbados Mexico Islas 30° Belize Netherlands Juan Fernãndez A Santiago N URUGUAY Bolivia Nicaragua ECLAC HQ I Brazil Panama T Buenos Aires Montevideo Canada Paraguay N Chile Peru E Colombia Portugal E G Costa Rica Saint Kitts and Nevis R L Cuba Saint Lucia 40° I A Dominica Saint Vincent and the Dominican Republic Grenadines H 40 Ecuador Spain ° C El Salvador Suriname 40 30 50 France Trinidad and Tobago ° ° ° Grenada United Kingdom l Capital city Guatemala United States of America The boundaries and names shown and the designations used Guyana Uruguay on this map do not imply official endorsement or acceptance Haiti Venezuela by the United Nations. -
Analysing the Influence of African Dust Storms on the Prevalence of Coral Disease in the Caribbean Sea Using Remote Sensing and Association Rule Data Mining
International Journal of Remote Sensing ISSN: 0143-1161 (Print) 1366-5901 (Online) Journal homepage: http://www.tandfonline.com/loi/tres20 Analysing the influence of African dust storms on the prevalence of coral disease in the Caribbean Sea using remote sensing and association rule data mining Heather Hunter & Guido Cervone To cite this article: Heather Hunter & Guido Cervone (2017) Analysing the influence of African dust storms on the prevalence of coral disease in the Caribbean Sea using remote sensing and association rule data mining, International Journal of Remote Sensing, 38:6, 1494-1521 To link to this article: http://dx.doi.org/10.1080/01431161.2016.1277279 Published online: 31 Jan 2017. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tres20 Download by: [Pennsylvania State University] Date: 31 January 2017, At: 12:46 INTERNATIONAL JOURNAL OF REMOTE SENSING, 2017 VOL. 38, NO. 6, 1494–1521 http://dx.doi.org/10.1080/01431161.2016.1277279 Analysing the influence of African dust storms on the prevalence of coral disease in the Caribbean Sea using remote sensing and association rule data mining Heather Hunter a and Guido Cervone b,c aDepartment of Applied Marine Physics, Rosenstiel School of Marine and Atmospheric Science, Miami, FL, USA; bDepartment of Geography and Institute for CyberScience, Pennsylvania State University, University Park, PA, USA; cLamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA ABSTRACT ARTICLE HISTORY The application of an association rule data mining algorithm is Received 29 July 2016 described to combine remote sensing and in-situ geophysical data Accepted 22 December 2016 to show a relationship between African dust storms, Caribbean climate, and Caribbean coral disease. -
Kinematic Reconstruction of the Caribbean Region Since the Early Jurassic
Earth-Science Reviews 138 (2014) 102–136 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Kinematic reconstruction of the Caribbean region since the Early Jurassic Lydian M. Boschman a,⁎, Douwe J.J. van Hinsbergen a, Trond H. Torsvik b,c,d, Wim Spakman a,b, James L. Pindell e,f a Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands b Center for Earth Evolution and Dynamics (CEED), University of Oslo, Sem Sælands vei 24, NO-0316 Oslo, Norway c Center for Geodynamics, Geological Survey of Norway (NGU), Leiv Eirikssons vei 39, 7491 Trondheim, Norway d School of Geosciences, University of the Witwatersrand, WITS 2050 Johannesburg, South Africa e Tectonic Analysis Ltd., Chestnut House, Duncton, West Sussex, GU28 OLH, England, UK f School of Earth and Ocean Sciences, Cardiff University, Park Place, Cardiff CF10 3YE, UK article info abstract Article history: The Caribbean oceanic crust was formed west of the North and South American continents, probably from Late Received 4 December 2013 Jurassic through Early Cretaceous time. Its subsequent evolution has resulted from a complex tectonic history Accepted 9 August 2014 governed by the interplay of the North American, South American and (Paleo-)Pacific plates. During its entire Available online 23 August 2014 tectonic evolution, the Caribbean plate was largely surrounded by subduction and transform boundaries, and the oceanic crust has been overlain by the Caribbean Large Igneous Province (CLIP) since ~90 Ma. The consequent Keywords: absence of passive margins and measurable marine magnetic anomalies hampers a quantitative integration into GPlates Apparent Polar Wander Path the global circuit of plate motions. -
North America Name North America
Not at same scale Hawaii (U.S.) Name North America Name North America Greenland North America ARCTIC Sea Bering Bering Strait OCEAN Canada is on the continent Helpful Sea of North America. Hint Greenland Alaska Beaufort (Denmark) One U.S. state, Sea Two countries, the United States and Mexico, (U.S.) Baffin share the continent with Canada. North Hawaii, is not Bay part of North Gulf of America also includes Greenland, the countries Alaska America. %Nuuk of Central America, and many islands. Labrador Use the map to answer these questions about North America. Sea Hudson Canada Bay 1. In which direction is Mexico from the United States? R 2. Name three countries O C Mississippi Ottawa% K River that share a border with Mexico. Y M O U N T ATLANTIC A I 3. What country shares a border N Washington, D.C.% S OCEAN on the south with Canada? United States PACIFIC Rio of America Grande Bermuda (U.K.) 4. What U.S. state is on the northwest OCEAN part of North America? Bahamas Gulf of Mexico Cuba Dominican North America Mexico Republic 5. What oceans border the east Haiti Puerto Rico (U.S.) % National capital Mexico City Jamaica and west coasts of North America? % Mountain Belize Border Honduras 6. What ocean is north of this continent? Caribbean Sea Guatemala Nicaragua El Salvador N N 7. What is the capital of Canada? NW NE Costa Rica Area of detail WE WE Panama SOUTH AMERICA 8. What river forms part of the border Miles SW SE 0 200 400 600 S S between the U.S. -
Surface Currents Near the Greater and Lesser Antilles
SURFACE CURRENTS NEAR THE GREATER AND LESSER ANTILLES by C.P. DUNCAN rl, S.G. SCHLADOW1'1 and W.G. WILLIAMS SUMMARY The surface flow around the Greater and Lesser Antilles is shown to differ considerably from the widely accepted current system composed of the Caribbean Current and Antilles Current. The most prominent features deduced from dynamic topography are a flow from the north into the Caribbean near Puerto Rico and a permanent eastward-flowing counter-current in the Caribbean itself between Puerto Rico and Venezuela. Noticeably absent is the Antilles Current. A satellite-tracked buoy substantiates the slow southward flow into the Caribbean and the absence of the Antilles Current. INTRODUCTION Pilot Charts for the North Atlantic and the Caribbean Sea (Defense Mapping Agency, 1968) show westerly surface currents to the North and South of Puerto Rico. The Caribbean Current is presented as an uninterrupted flow which passes through the Caribbean Sea, Yucatan Straits, Gulf of Mexico, and Florida Straits to become the Gulf Stream. It is joined off the east coast of Florida by the Antilles Current which is shown as flowing westwards along the north coast of Puerto Rico and then north-westerly along the northern edge of the Bahamas (BOISVERT, 1967). These surface currents are depicted as extensions of the North Equatorial Current and the Guyana Current, and as forming part of the subtropical gyre. As might be expected in the absence of a western boundary, the flow is slow-moving, shallow and broad. This interpretation of the surface currents is also presented by WUST (1964) who employs the same set of ship’s drift observations as are used in the Pilot Charts. -
By the Becreu^ 01 Uio Luterior NFS Form 10-900 USDI/NPS NRHP Registration Form (Rev
NATIONAL HISTORIC LANDMARK NOMINATION NFS Form 10-900 USDI/NPS NRHP Registration Form (Rev. 8-86) 0MB No. 1024-0018 FORT FREDERIK (U.S. VIRGIN ISLANDS) Page 1 United States Department of the Interior, National Park Service____________________________ National Register of Historic Places Registration Form l^NAMEOF PROPERTY Historic Name: FORT FREDERIK (U.S. VIRGIN ISLANDS) Other Name/Site Number: FREDERIKSFORT 2. LOCATION Street & Number: S. of jet. of Mahogany Rd. and Rt. 631, N end of Frederiksted Not for publication:N/A City/Town: Frederiksted Vicinity :N/A State: US Virgin Islands County: St. Croix Code: 010 Zip Code:QQ840 3. CLASSIFICATION Ownership of Property Category of Property Private: __ Building(s): X Public-local: __ District: __ Public-State: X Site: __ Public-Federal: Structure: __ Object: __ Number of Resources within Property Contributing Noncontributing 2 __ buildings 1 sites 1 __ structures _ objects 1 Total Number of Contributing Resources Previously Listed in the National Register :_2 Name of related multiple property listing: N/A tfed a by the becreu^ 01 uio luterior NFS Form 10-900 USDI/NPS NRHP Registration Form (Rev. 8-86) OMB No. 1024-0018 FORT FREDERIK (U.S. VIRGIN ISLANDS) Page 2 United States Department of the Interior, National Park Service _______________________________National Register of Historic Places Registration Form 4. STATE/FEDERAL AGENCY CERTIFICATION As the designated authority under the National Historic Preservation Act of 1966, as amended, I hereby certify that this __ nomination __ request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. -
2. Geophysics and the Structure of the Lesser Antilles Forearc1
2. GEOPHYSICS AND THE STRUCTURE OF THE LESSER ANTILLES FOREARC1 G. K. Westbrook, Department of Geological Sciences, University of Durham and A. Mascle and B. Biju-Duval, Institut Français du Pétrole2 ABSTRACT The Barbados Ridge complex lies east of the Lesser Antilles volcanic arc along the eastern margin of the Caribbean Plate. The complex dates in part from the Eocene, and elements of the arc system have been dated as Late Cretaceous and Late Jurassic, although most of the volcanic rocks date from the Tertiary, particularly the latter part. It is probable that the arc system was moved a considerable distance eastward with respect to North and South America during the Tertiary. The accretionary complex can be divided into zones running parallel to the arc, starting with a zone of initial accre- tion at the front of the complex where sediment is stripped from the ocean floor and the rate of deformation is greatest. This zone passes into one of stabilization where the deformation rate is generally lower, although there are localized zones of more active tectonics where the generally mildly deformed overlying blanket of sediment is significant dis- turbed. Supracomplex sedimentary basins that are locally very thick are developed in the southern part of the complex. The Barbados Ridge Uplift containing the island of Barbados lies at the western edge of the complex; between it and the volcanic arc lies a large forearc basin comprising the Tobago Trough and Lesser Antilles Trough. There are major longitudinal variations in the complex that are broadly related to the northward decrease in sedi- ment thickness away from terrigenous sources in South America and that are locally controlled by ridges in the oceanic igneous crust passing beneath the complex. -
The Evolution of Middle America and the Gulf of Mexico-Caribbean Sea Region During Mesozoic Time
The evolution of Middle America and the Gulf of Mexico-Caribbean Sea region during Mesozoic time THOMAS H. ANDERSON I Department of Geology and Planetary Science, University of Pittsburgh, Pittsburgh, Pennsylvania VICTOR A. SCHMIDT | 15260 ABSTRACT Geometric constraints suggest that of Central America, the Nicaraguan Rise, probably shear initially occurred along the and southeastern Cuba) was sutured A plate-tectonic model for the evolution Mexican volcanic zone near the end of the against the Maya East plate along the of Middle America and the Gulf of Mex- Middle Jurassic. Subsequently, probably present Motagua fault and Cayman ico-Caribbean Sea region is presented. about 160 m.y. ago, displacements that Trench. The model, which is based upon the exist- total ~800 km began along the Mojave- Our model is constrained by published ence of the Mojave-Sonora megashear, Sonora megashear. Contemporaneously, geologic data, the relative positions of incorporates into the Triassic Pangea re- Yucatan and fragments of pre-Cretaceous North and South America from Atlantic construction three microplates between rocks that compose parts of central and sea-floor magnetic anomalies, and the re- North and South America, thus avoiding western Cuba migrated northward toward quirement that the major transform faults the overlap of the Bullard fit. These plates their present positions. Rotation of Yuca- be compatible with the poles of rotation are the Yaqui, bounded on the north by tan was facilitated by considerable dis- for the appropriate relative motions be- the Mojave-Sonora megashear; the east placement along the proto-Motagua zone tween North and South America. Paleo- and west Maya plates, bounded on the and along a zone that is probably coinci- magnetic data from Middle America are north by the Mexican volcanic zone and dent with the modern Salina Cruz fault. -
Paleogeography of the Caribbean Region: Implications for Cenozoic Biogeography
PALEOGEOGRAPHY OF THE CARIBBEAN REGION: IMPLICATIONS FOR CENOZOIC BIOGEOGRAPHY MANUEL A. ITURRALDE-VINENT Research Associate, Department of Mammalogy American Museum of Natural History Curator, Geology and Paleontology Group Museo Nacional de Historia Natural Obispo #61, Plaza de Armas, CH-10100, Cuba R.D.E. MA~PHEE Chairman and Curator, Department of Mammalogy American Museum of Natural History BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY Number 238, 95 pages, 22 figures, 2 appendices Issued April 28, 1999 Price: $10.60 a copy Copyright O American Museum of Natural History 1999 ISSN 0003-0090 CONTENTS Abstract ....................................................................... 3 Resumen ....................................................................... 4 Resumo ........................................................................ 5 Introduction .................................................................... 6 Acknowledgments ............................................................ 8 Abbreviations ................................................................ 9 Statement of Problem and Methods ............................................... 9 Paleogeography of the Caribbean Region: Evidence and Analysis .................. 18 Early Middle Jurassic to Late Eocene Paleogeography .......................... 18 Latest Eocene to Middle Miocene Paleogeography .............................. 27 Eocene-Oligocene Transition (35±33 Ma) .................................... 27 Late Oligocene (27±25 Ma) ............................................... -
Thematic Report for the Insular Caribbean Sub-Region
CLME-TT/3 Prov Barbados, February 2007 Original: English THEMATIC REPORT FOR THE INSULAR CARIBBEAN SUB-REGION A discussion paper for the CLME Synthesis Workshop by Sherry Heileman, Ph.D. CLME Project Implementation Unit Centre for Resource Management and Environmental Studies (CERMES) University of the West Indies Cave Hill Campus, Barbados February 2007 Insular Caribbean - CLME Thematic report CONTENTS 1. INTRODUCTION ................................................................................................................................ 1 2. THE INSULAR CARIBBEAN .......................................................................................................... 1 Geography and oceanography ................................................................................................................... 1 Ecological features..................................................................................................................................... 3 Socio-economic background...................................................................................................................... 5 2.4 Environmental and socio-economic vulnerability of SIDS ................................................................. 6 3. PRIORITY TRANSBOUNDARY PROBLEMS.............................................................................. 7 3.1 Unsustainable exploitation of living marine resources ........................................................................ 8 3.1.1 Description of the problem and justification -
Caribbean Markets for US Wood Products
,~~~~United States Department of i_/ Agriculture Caribbean Markets Forest Service Southern Forest for U.S. Wood Experiment Station New Orleans, Products Louisiana Research Paper SO-225 July 1986 Harold W. Wisdom, James E. Granskog, and Keith A. Blatner Mexico I SUMMARY The West Indies and the continental countries bordering the Caribbean Sea constitute a significant market for U.S. wood products. In 1983, wood product exports to the region totaled almost $157 million. The Caribbean Basin primar- ily is a market for softwood products, with pine lumber being the most promi- nent item. The flow of exports to the region is dominated by (1) overseas shipments from southern ports to the West Indies and (2) overland shipments from the Southwestern United States to Mexico. CONTENTS INTRODUCTION ................................................. 1 THE CARIBBEAN BASIN .......................................... 1 Forests .......................................................... 1 Mexico ........................................................ 2 Central America ............................................... 2 South Rim ..................................................... 3 West Indies .................................................... 3 Wood Production and Trade ....................................... 3 U.S. WOOD EXPORTS ............................................. 4 Roundwood ...................................................... 5 Logs ........................................................... 5 Poles ......................................................... -
Active Structures in the Barbados Accretionary Wedge of the Lesser Antilles Subduction: Implications for Slip Partitioning
EGU2020-10732 https://doi.org/10.5194/egusphere-egu2020-10732 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Main active structures in the Barbados accretionary wedge of the Lesser Antilles Subduction: implications for slip partitioning Gaëlle Bénâtre1, Nathalie Feuillet1, Hélène Carton1, Eric Jacques1, and Thibaud Pichot2 1Université de Paris, Institut de Physique du Globe de Paris, CNRS UMR7154, Paris, F-75005, France ([email protected]) 2Beicip-Franlab, Rueil-Malmaison, France At the Lesser Antilles Subduction Zone (LASZ), the American plates subduct under the Caribbean plate at a slow rate of ~2 cm/yr. No major subduction megathrust earthquakes have occurred in the area since the 1839 and 1843 historical events, and the LASZ is typically considered weakly coupled. At the front of the LASZ, the Barbados accretionary wedge (BAW) is one of the largest accretionary wedges in the world. The width of the BAW decreases northward, owing to the increasing distance to the sediment source (Orinoco river) and the presence of several aseismic oceanic ridges, in particular the Tiburon ridge, that stops sediment progression. Marine geophysical studies conducted to date over the northern part of the BAW (Guadeloupe-Martinique sector) have mostly focused on resolving the geometry of the backstop. However, the structure of the wedge and the mechanical behavior of the subduction interface remain poorly known. Our study aims to describe the geometry of the BAW by a detailed morpho-tectonic analysis in order to place constraints on present and past dynamic interactions between the subducting and overriding plates.