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Current Knowledge Concerning Distribution of Freshwater Planktonic, Littoral and Benthic Rotifera and Microcrustacea (Cladocera, Copepoda and Ostracoda) in Central America and the Caribbean. Free access until march 22 usign the following link: https://authors.elsevier.com/c/1gWF~HHE-jEhc

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  • Asociación Guatemalteca de Limnología y Gestión de Lagos
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Abstract

Abstract Central America and the Caribbean, at the northern limit of the Neotropical region, is made up of a narrow strip of land and numerous islands, with a complex geological history, represents an important biogeographic connection between North and South America and contains diverse freshwater environments, including high mountain and lowlands lakes and wetlands. We examined literature reports and databases for freshwater planktonic, benthic and littoral Rotifera and microcrustacea distribution in the area in order to update, unify and summarize disparate information that has accumulated since Collado et al.’s initial contribution in 1984 that listed 369 specific and infraspecific taxa. We used the most common databases and keywords to locate papers on Rotifera, Cladocera, Ostracoda and Copepoda and found 457 new records from more than 200 study sites that list 92 genera and 782 species, as well as over 30 infraspecific taxa, for the region. These included 84%, 53%, 37% and 21% respectively, of known neotropical species of these groups. Analysis using the Sorensen-Dice Similarity Index showed high heterogeneity in species composition for the area and hierarchical clustering suggests three groups for the Caribbean islands. Lack of resources has hindered the formal publication of research. We conclude that a collaborative effort is needed to produce scientists capable of combining taxonomic information with ecological studies to enhance understanding of anthropogenic impacts on water resources.

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The free-living continental copepod fauna of the Yucatan Peninsula has been studied for decades; recent intensive surveys suggest that its biodiversity is higher than formerly realized. An updated, revised checklist of the Yucatan copepods is provided herein. This new list includes 59 species, more a than 30% increase from the most recent previous account. The Yucatan Peninsula has long been considered to have faunistic affinities with Central and Southern Mexico and with South America. A similarity analysis was performed using regional records of Copepoda and including two taxa, the orders Calanoida and Cyclopoida. Results from both groups suggest that the Yucatan copepod fauna diverges from that of Central Mexico. Central Mexico itself seems to be closest to the upper Central American fauna, an affinity explained by a longer geological connection. Overall, the Yucatan copepod fauna appears to have more biogeographic ties with Cuba and the insular Caribbean than with Central America or the rest of Mexico. The occurrence of nearctic diaptomids such as Arctodiaptomus and Leptodiaptomus in the Yucatan seems to be related to a general invasion of these calanoids that reached Central America and intermittently spread into the Yucatan Peninsula. With two endemic species in the Yucatan, Mastigodiaptomus appears to have become diversified in the peninsula, derived from other neotropical forms. The local high proportion of endemic forms of Copepoda and the particular geological history of the Yucatan make this karstic area a peculiar, separate entity within the neotropical region that should be studied in more detail.
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Cryptic species are organisms that look identical but represent distinct evolutionary lineages. They are an emerging trend in organismal biology across all groups, from flatworms, insects, amphibians, and primates, to vascular plants. This book critically evaluates the phenomenon of cryptic species and demonstrates how they can play a valuable role in improving our understanding of evolution, in particular of morphological stasis. It also explores how the recognition of cryptic species is intrinsically linked to the so-called species problem, the lack of a unifying species concept in biology, and suggests alternative approaches. Bringing together a range of perspectives from practising taxonomists, the book presents case studies of cryptic species across a range of animal and plant groups. It will be an invaluable text for all biologists interested in species and their delimitation, definition, and purpose, including undergraduate and graduate students and researchers.
Article
Elpidium ostracods are known by their very particular niche (water accumulated in tank-bromeliads), their relatively low dispersal ability and their dependency on amphibians for dispersal and colonization of new bromeliads. All these characteristics make the genus an interesting group for evolutionary, ecological and even taxonomic studies. However, the diversity of the group remains poorly studied. Here, we describe three new species of Elpidium, Elpidium littlei n. sp., Elpidium heberti n. sp. and Elpidium wolfi n. sp., and re-describe Elpidium laesslei, all from Jamaica. These species are characterized by a copulatory process with separated ejaculatory duct and distal glans, a feature so far unique within the genus. Each species can, in turn, be diagnosed by soft part and carapace morphology, most notably comparing hemipenis, valve ornamentation and degree of sexual dimorphism. The observed morphological diversity of Elpidium is discussed in relation to previous genetic estimates that suggested an even higher diversity in Jamaica. We point to intraspecific variation and lack of complete morphological descriptions as possible explanations. We also reaffirm the need of multidisciplinary studies in order to do more objective and secure taxonomic classifications in future studies.
Article
Previous studies of plankton from Guatemala lakes, by Meek (1908); Clark (1908); and Tilden (1908); have been purely qualitative in nature. Juday's (19,16) limnological study of Lake Amatitlan, however, included a single series of quantitative plankton collections at various depths. The present paper is a report on a series of quantitative collections taken from Lake AmatitIan over an eight-week period during the summer of 1951. General description of the lake.-Lake Amatitlan is of volcanic origin and is situated at 90030' west longitude and 14025' north latitude in the Republic of Guatemala. It is eight miles long, 21/2 miles wide and with a surface of 3870 feet above sea level. A crossing of the International Railways of Central America divides the lake into two basins. Mountains, 4670-5170 feet above sea level, surround the lake; those of the northwest are composed of granite; the others are principally of volcanic ash, pumice, and other loose materials which are easily eroded. The mountains to the north and northwest show evidence of erosion in the form of huge cuts which are visible for several miles. Entering the lake on the north side is the Villalobos (Lobos) River, which is the main affluent stream during the dry season. The single outlet is the Michatoya River which drains the northwest basin from the south. The greater part of the lake shore is steep, especially to the east and southeast. Half or more of the north and northeast shores consist of a broad, low plain which 'has been built up by the LoSos River and temporary streams which enter the lake from the north and northwest during the rainy season (MayNovember).
Article
For more than a century, the two largest bodies of water in Nicaragua, Lake Nicaragua and its smaller companion, Managua, have engaged naturalists from several disciplines. Perhaps their appeal has been as curiosities because of the occurrence of fish with marine affinities in the larger lake, especially a dangerous shark. The charm has been in Nicaragua or Cocibolca, rather than Managua, properly called Xolotlán. Even though the latter is saltier, it has no elasmobranchs or tarpons. The lakes, and specifically the larger, cover the greatest expanse of any body of water between Lake Titicaca, Bolivia-Peru, and the Laurentian Great Lakes 35° farther north. Despite this, very little limnologic work has been published concerning them.
Book
Their story began 500 million years ago, but we only started to get to know them in 1746, when Linné described the first ostracod species. Vividly portraying the freshwater ostracods, this comprehensive reference work gathers the knowledge gained during some 250 years, but which to date has remained scattered throughout the literature. It starts with an introduction to the class Ostracoda with a special focus on freshwater ostracods and highlights practical methods in their study. The systematic part includes an introduction to all families; identification keys for all subfamilies, genera and species; diagnoses for each subfamily and genus; and lists of synonyms and distribution of species. The text is richly illustrated with distribution maps, line drawings of key generic characteristics, and numerous SEM photographs. Serving as an excellent starting point for all further research on freshwater ostracods, it can be widely used not only by ostracodologists, but also by crustaceologists, evolutionists and ecologists. © Springer-Verlag Berlin Heidelberg 2012. All rights are reserved.
Article
CRUSTACEANS A N D ROTIFERS O F T H E "LAGUNA DEL TESORO" (CUBA) I n this paper a listof aquaticCrustacea and Rotatoria recorded during a visit to "Laguna del Tesoro" in Jannuary of 1983 is presented. The lagoon is situated in [he North-Easr of the "Cienaga de Zapata". The waters are fresh chloride-alkaline and cover on area of 700 Ha. The Rotifera and Crustacea's community is very rich in species; 13 Rotatoria, 20 Entomostraca and a Amphipoda have been identified. Thecommunity is divided into two very clear subcommunities: a planktonicand a heleoplanktonicone. The he!eoplanktonic community is found in the abundant macrophytic vegetation, and is particularly interesting due to its complexity and especies. The biology of some of these species as CycLertheria hislopi, Chydorus cilzatus and Microcyclops ceibaenrir, is not well known.
Article
Over the past decade, the availability of DNA sequence data from rotifers and the development of statistical and analytical tools linked to phylogenetic reconstructions allowed researchers to deepen our knowledge of patterns and processes in rotifer diversity. Here, I review the recent rotifer literature regarding: (i) the position of rotifers in the animal kingdom, with the wide consensus being within Spiralia, in a clade called Platyzoa together with Acanthocephalans, Gastrotricha, Gnathostomulida, Micrognathozoa, and Platyhelminthes; (ii) the still unresolved phylogenetic relationships within rotifers and the disputed position of Acanthocephala; (iii) the discovery of extensive hidden diversity through DNA taxonomy; (iv) phylogeography; and (v) the phylogenetic structure of rotifer communities. In order to facilitate the further discovery of hidden diversity in rotifers, I provide a simple tutorial on the currently available methods in DNA taxonomy from single locus data using a previously published rotifer dataset as an example. Moreover, I outline a brief perspective on the potentiality of the use of phylogenetic approaches in future rotifer studies.
Article
Gut contents of 1150 adults of Apocyclops panamensis were examined to obtain information on its feeding habits in extensive shrimp ponds during a 16-week period (10 June-5 Sept. 1999). Temporal changes in the relative abundance of ingested algae were studied and compared with the natural phytoplankton assemblage in the pond. The phytoplankton community was comprised of diatoms and blue-green and green algae; total abundance varied between 1.11 × 104 and 10.2 × 104 cells/ml, of which blue-green algae, such as Lyngbya limnetica, Spirulina nodosa, and Anabaenopsis sp., were the most abundant. During the study period, diatoms made up 89% of the algal cells consumed by A. panamensis. Among the diatoms, Nitzschia sp. was most important, while Navicula sp. and Amphora ovalis were also substantial. The green alga, Chlorella sp., accounted for 10.6%; blue-green algae were rarely consumed.
Article
Lakes Nicaragua and Managua are large, rather shallow, fresh-water bodies that lie in a late Tertiary and Quaternary graben in western Nicaragua. The bottom sediments comprise highly organic diatomaceous volcanic silts and clays in which quartz plagioclase feldspar, dioctahedral montmorillonite and volcanic glass are the principal constituents. Organic nitrogen content of the lake sediments ranges from 0.3-1.2 percent, about the same range as in eutrophic lakes of higher latitudes. Bitumen content is rather low, much like that of oligotrophic lakes. Hydrocarbon fractions of bitumens are similar in amount to an alkaline lake of western U. S. Non-hydrocarbon bitumens are high in proportion to hydrocarbons. Carbohydrates and amino acids sre similar in amount to those of eutrophic lake sediments. Chlorinoid pigments are similar to but flavinoid pigments are less than the typical pigments in eutrophic lake sediments. Studies of the pH, Eh, inorganic composition and organic chemical and fossil residues of the lake sediments indicate that they are moderately productive, early eutrophic or mesotrophic lakes. Despite the presence of elasmobranches and of several marine or brackish-water types of invertebrates, no definite evidence of former marine connection has been found in the sediments. It is suggested that the lakes have been fresh-water for all or nearly all of their history and may be a little more highly mineralized now than formerly.