Calanoid copepods of the family Euchaetidae from the Gulf of Mexico and western Caribbean Sea

1975 ◽  
pp. 1-26 ◽  
Author(s):  
Taisoo Park
Keyword(s):  
Gulf Of Mexico ◽  
Caribbean Sea ◽  
Calanoid Copepods ◽  
The Family ◽  
Western Caribbean

New and rare micro-pagurid hermit crabs (Crustacea: Anomura: Paguridae) from the Caribbean Sea and Gulf of Mexico

Zootaxa ◽  
2020 ◽  
Vol 4722 (4) ◽  
pp. 301-325
Author(s):  
RAFAEL LEMAITRE
Keyword(s):  
New Species ◽  
Gulf Of Mexico ◽  
Florida Keys ◽  
Caribbean Sea ◽  
Hermit Crabs ◽  
Caribbean Region ◽  
Bocas Del Toro ◽  
The Family ◽  
Two New Species ◽  
The Caribbean

Six species of hermit crabs of the family Paguridae from the Caribbean Sea and Gulf of Mexico region, including two new species, Anisopagurus asteriscus sp. nov. and Pagurus alarius sp. nov., are documented. The two new species are described, and recognition characters summarized for the four previously known species. Reports of the latter, Nematopaguroides fagei Forest & de Saint Laurent, 1968, N. karukera Lemaitre, Felder & Poupin, 2017, Paguriscus robustus Lemaitre, Felder & Poupin, 2017, and Pylopaguridium markhami McLaughlin & Lemaitre, 2001, represent range extensions for all four species. Color photographs are included for four of the species, as well as remarks on their taxonomy and distributions. All six species included can be categorized as micro-pagurids (with shield length rarely exceeding 2.0 mm), and were collected from cryptic reef habitats in Bocas del Toro, Panama; the French Antillean island of Guadeloupe; and the Gulf of Mexico coasts of Louisiana, Yucatán, and Florida Keys. The discovery of these new or rare species supports the conclusion of recent studies that the diversity of pagurids from the Caribbean region has yet to be fully realized. 

Distribution and Abundance of Phyllosoma Larvae (Decapoda, Palinuridae) in the Southern Gulf of Mexico and the Western Caribbean Sea

Crustaceana ◽  
2004 ◽  
Vol 77 (1) ◽  
pp. 75-93 ◽  
Author(s):  
Rebeca Gasca ◽  
Heyden Manzanilla-Dominguez
Keyword(s):  
Gulf Of Mexico ◽  
Spiny Lobster ◽  
Caribbean Sea ◽  
Larval Stages ◽  
Retention System ◽  
Mexican Caribbean ◽  
Caribbean Area ◽  
Western Caribbean ◽  
Southern Gulf Of Mexico ◽  
Phyllosoma Larvae

AbstractFrom plankton samples collected during two oceanographic expeditions in the southern Gulf of Mexico (1991) and five in the Mexican Caribbean Sea, we studied the composition, abundance, and distribution of the phyllosoma larvae. A total of 118 phyllosomas belonging to five species of lobster were recorded. Panulirus argus was the most abundant and dominant, it represented 73.9% of the total number of phyllosomas collected, followed by Scyllarides aequinoctialis (18.0%). The phyllosomas were distributed mainly in the coastal areas, with decreasing densities oceanwards. Highest larval concentrations were recorded near the outer border of the Campeche Bank shelf in the southern Gulf of Mexico. In the Mexican Caribbean area, phyllosomas were most abundant around Banco Chinchorro, off Espiritu Santo Bay and Ascension Bay, and near Isla Mujeres; these are well-known spawning areas for the spiny lobster, P. argus and are indicated by the presence of the earliest larval stages. The oldest larvae were concentrated on the Campeche Bank; this was attributed to the effect of a local gyre that retains these larvae. The youngest phyllosomas tended to have an oceanic distribution thus allowing them to enter the oceanic system of mesoscale gyres of the Gulf. In the Mexican Caribbean the coastal shoreward currents seem to act as a retention system for lobster larvae. The distribution of the phyllosoma stages in the Caribbean area suggests a continuous presence of different stages year-round. Some of these larvae, in the northeastern sector, would likely be transported to the Campeche Bank.

scholarly journals Storm-wave trends in Mexican waters of the Gulf of Mexico and Caribbean Sea

2017 ◽  
Vol 17 (8) ◽  
pp. 1305-1317 ◽  
Author(s):  
Elena Ojeda ◽  
Christian M. Appendini ◽  
E. Tonatiuh Mendoza
Keyword(s):  
Time Series ◽  
Gulf Of Mexico ◽  
Tropical Cyclones ◽  
Wave Height ◽  
Energy Content ◽  
Caribbean Sea ◽  
Caribbean Region ◽  
Storm Events ◽  
Western Caribbean ◽  
Storm Wave

Abstract. Thirty-year time series of hindcast wave data were analysed for 10 coastal locations along the eastern Mexican coast to obtain information about storm events occurring in the region, with the goal of examining the possible presence of interannual trends in the number of storm-wave events and their main features (wave height, duration and energy content). The storms were defined according to their significant wave height and duration, and the events were classified as related to either tropical cyclones or Norte events. The occurrence and characteristics of both types of events were analysed independently. There is no statistically significant change in the number of storm-wave events related to Nortes or their characteristics during the study period. However, there is a subtle increase in the number of events related to tropical cyclones in the western Caribbean region and a more evident increase in wave height and energy content of these events.

Spatial Characteristics of Rain Fields Associated with Tropical Cyclones Landfalling over the Western Gulf of Mexico and Caribbean Sea

2018 ◽  
Vol 57 (8) ◽  
pp. 1711-1727 ◽  
Author(s):  
Yao Zhou ◽  
Corene J. Matyas
Keyword(s):  
Gulf Of Mexico ◽  
Tropical Cyclones ◽  
Gulf Coast ◽  
Hot Spot ◽  
Vertical Wind Shear ◽  
Precipitable Water ◽  
Caribbean Sea ◽  
Caribbean Coast ◽  
Near Surface ◽  
Western Caribbean

AbstractThe western Gulf Coast and Caribbean coast are regions that are highly vulnerable to precipitation associated with tropical cyclones (TCs). Defining the spatial dimensions of TC rain fields helps determine the timing and duration of rainfall for a given location. Therefore, this study measured the area, dispersion, and displacement of light and moderate rain fields associated with 35 TCs making landfalls in this region and explored conditions contributing to their spatial variability. The spatial patterns of satellite-estimated rain rates are determined through hot spot analysis. Rainfall coverage is largest as TCs approach the western Caribbean coast, and smaller as TCs move over the Gulf of Mexico (GM) after making landfall over the Yucatan Peninsula. The rain fields are displaced eastward and northward over the western and central Caribbean Sea and the central GM. Rainfall fields have more displacement toward the west and south, which is over land, when TCs move over the southern GM, possibly as a result of the influence of Central American gyres. The area and dispersion of rainfall are significantly correlated with storm intensity and total precipitable water. The displacement of rainfall is significantly correlated with vertical wind shear. Over the Bay of Campeche, TC precipitation extends westward, which may be related to the convergence of moisture above the boundary layer from the Pacific Ocean and near-surface convergence enhanced by land. Additionally, half of the storms produce rainfall over land about 48 h before landfall. TCs may produce light rainfall over land for more than 72 h in this region.

Dispersion of Rayleigh waves in the Gulf of Mexico and Caribbean Sea

1964 ◽  
Vol 54 (3) ◽  
pp. 909-925
Author(s):  
Basil C. Papazachos
Keyword(s):  
Gulf Of Mexico ◽  
Central America ◽  
Rayleigh Waves ◽  
Caribbean Sea ◽  
Eastern Coast ◽  
Phase Velocities ◽  
Central United States ◽  
Western Caribbean ◽  
Group And Phase Velocities ◽  
The Waves

Abstract Group and phase velocities of Rayleigh waves along 57 paths between Central America and the central United States were determined. The waves examined were of period between 15 and 60 seconds and crossed the Gulf of Mexico and Caribbean Sea in many directions. The following conclusions about the structure of the region are drawn: Along the paths crossing the western and central Gulf and the regions near the coast of Texas and the eastern coast of Mexico the velocities were found to be very low. This is attributed to the great thickness of the sediments in these regions. The velocities along paths crossing the eastern Gulf and westernmost Caribbean were found to be higher than the typical continental velocities. This is considered as an indication of a difference in structure between the eastern and western Gulf of Mexico. Along one path in the western Caribbean Sea between Colombia and Cuba the velocities were almost continental. High velocities found for part of the eastern Caribbean indicate an almost oceanic character for this region. For each earthquake examined the initial phases were determined with an error less than ± π/4. For a given earthquake in all cases except two the initial phases were found to be the same at all stations.

scholarly journals Storm-wave trends in Mexican waters of the Gulf of Mexico and Caribbean Sea

2017 ◽  
Author(s):  
Elena Ojeda ◽  
Christian Mario Appendini ◽  
Ernesto Tonatiuh Mendoza
Keyword(s):  
Time Series ◽  
Gulf Of Mexico ◽  
Tropical Cyclones ◽  
Wave Height ◽  
Energy Content ◽  
Caribbean Sea ◽  
Caribbean Region ◽  
Storm Events ◽  
Western Caribbean ◽  
Storm Wave

Abstract. Thirty-year time series of hindcast wave data were analysed for ten coastal locations along the eastern Mexican coast to obtain information about storm events occurring in the region, with the goal to examine the possible presence of interannual trends in the number of wave storm events and their main features (wave height, duration and energy content). The storms were defined according to their significant wave height and duration, and the events were classified as related to either tropical cyclones or Norte events. The occurrence and characteristics of both types of events were analysed independently. There is no statistically significant change in the number of wave storm events related to Nortes or their characteristics during the study period. However, there is a subtle increase in the number of events related to tropical cyclones in the western Caribbean region and a more evident increase in wave height and energy content of these events.

scholarly journals Nonlinear analysis of the occurrence of hurricanes in the Gulf of Mexico and the Caribbean Sea

2018 ◽  
Vol 25 (2) ◽  
pp. 291-300 ◽  
Author(s):  
Berenice Rojo-Garibaldi ◽  
David Alberto Salas-de-León ◽  
María Adela Monreal-Gómez ◽  
Norma Leticia Sánchez-Santillán ◽  
David Salas-Monreal
Keyword(s):  
Time Series ◽  
Gulf Of Mexico ◽  
Nonlinear Analysis ◽  
Chaotic Behavior ◽  
Caribbean Sea ◽  
Historical Record ◽  
Nonlinear Analyses ◽  
The North ◽  
The Caribbean ◽  
The Individual

Abstract. Hurricanes are complex systems that carry large amounts of energy. Their impact often produces natural disasters involving the loss of human lives and materials, such as infrastructure, valued at billions of US dollars. However, not everything about hurricanes is negative, as hurricanes are the main source of rainwater for the regions where they develop. This study shows a nonlinear analysis of the time series of the occurrence of hurricanes in the Gulf of Mexico and the Caribbean Sea obtained from 1749 to 2012. The construction of the hurricane time series was carried out based on the hurricane database of the North Atlantic basin hurricane database (HURDAT) and the published historical information. The hurricane time series provides a unique historical record on information about ocean–atmosphere interactions. The Lyapunov exponent indicated that the system presented chaotic dynamics, and the spectral analysis and nonlinear analyses of the time series of the hurricanes showed chaotic edge behavior. One possible explanation for this chaotic edge is the individual chaotic behavior of hurricanes, either by category or individually regardless of their category and their behavior on a regular basis.

Sign in / Sign up

Export Citation Format

Share Document