Dendromonocotyle colorni sp n. (Monogenea : Monocotylidae) from the skin of Himantura uarnak (Dasyatididae) from Israel and a new host record for D-octodiscus from the Bahamas

Dendromonocotyle colorni sp. n. (Monogenea: Monocotylidae) is described from the dorsal skin surface of two specimens of Himantura uarnak (Forsskal) kept at the Eilat Underwater Observatory in Israel. Dendromonocotyle colorni is distinguished from the other eight species in the genus by the morphology of the terminal papillar sclerite on the haptor, the distal portion of the male copulatory organ and the morphology of the vagina. The development of the male copulatory organ is detailed for D. colorni and the adaptations of species of Dendromonocotyle to life on the dorsal skin surface of rays are discussed. Dendromonocotyle octodiscus Hargis, 1955 was identified from the dorsal skin surface of the southern stingray Dasyatis americana Hildebrand et Schroeder off Bimini, Bahamas and represents a new host record.

Towards radiocarbon calibration beyond 28ka using speleothems from the Bahamas

We present a new speleothem record of atmospheric Δ14C between 28 and 44 ka that offers considerable promise for resolving some of the uncertainty associated with existing radiocarbon calibration curves for this time period. The record is based on a comprehensive suite of AMS 14C ages, using new low-blank protocols, and U–Th ages using high precision MC-ICPMS procedures. Atmospheric Δ14C was calculated by correcting 14C ages with a constant dead carbon fraction (DCF) of 22.7 ± 5.9%, based on a comparison of stalagmite 14C ages with the IntCal04 (Reimer et al., 2004) calibration curve between 15 and 11 ka. The new Δ14C speleothem record shows similar structure and amplitude to that derived from Cariaco Basin foraminifera (Hughen et al., 2004, 2006), and the match is further improved if the latter is tied to the most recent Greenland ice core chronology (Svensson et al., 2008). These data are however in conflict with a previously published 14C data set for a stalagmite record from the Bahamas — GB-89-24-1 (Beck et al., 2001), which likely suffered from 14C analytical blank subtraction issues in the older part of the record. The new Bahamas speleothem ∆14C data do not show the extreme shifts between 44 and 40 ka reported in the previous study (Beck et al., 2001). Causes for the observed structure in derived atmospheric Δ14C variation based on the new speleothem data are investigated with a suite of simulations using an earth system model of intermediate complexity. Data-model comparison indicates that major fluctuations in atmospheric ∆14C during marine isotope stage 3 is primarily a function of changes in geomagnetic field intensity, although ocean–atmosphere system reorganisation also played a supporting role.

Bahamas y Barbados: evidencia empírica de la transmisión de las tasas de interés

Incluye Bibliografía

Bahamas and Barbados: empirical evidence of interest rate pass-through

Includes bibliography

National trade operations and procedure guide: Bahamas: preliminary draft

Includes bibliography

The organization of statistics in Bahamas, Barbados, Belize and Trinidad and Tobago

Includes bibliography

Hurricanes Frances and Jeanne in 2004: their impact in the Commonwealth of the Bahamas: preliminary version

Includes bibliography

The impact of immigration on Caribbean microstates: Bahamas, British Virgin Islands, Saint Maarten, United States Virgin Islands

Includes bibliography

Selected information on the Bahamas

Includes bibliography

Estudio económico de América Latina, 1979: Bahamas: versión preliminar = Economic survey of Latin America, 1979: Bahamas: preliminary version

Incluye Bibliografía

Informe BID: Bahamas

Incluye Bibliografía

Economic survey of Latin America, 1980: Bahamas: offprint = Estudio económico de América Latina 1980: Bahamas

Publicado anteriormente en español con el mismo símbolo

Economic survey of Latin America, 1981: Bahamas: preliminary version

Includes bibliography