Community of parasites inTriportheus curtusandTriportheus angulatus(Characidae) from a tributary of the Amazon River system (Brazil)

2016 ◽  
Vol 51 (1) ◽  
pp. 29-36 ◽  
Author(s):  
Marcos Sidney Brito Oliveira ◽  
Raissa Alves Gonçalves ◽  
Marcos Tavares-Dias
Keyword(s):  
Science ◽  
1986 ◽  
Vol 231 (4742) ◽  
pp. 1129-1131 ◽  
Author(s):  
J. I. HEDGES ◽  
J. R. ERTEL ◽  
P. D. QUAY ◽  
P. M. GROOTES ◽  
J. E. RICHEY ◽  
...  

1984 ◽  
Vol 89 (C2) ◽  
pp. 2061 ◽  
Author(s):  
Willard S. Moore ◽  
John M. Edmond
Keyword(s):  

2020 ◽  
Author(s):  
Werner Piller ◽  
Martin Gross

<p>Before the onset of the modern Amazon river system, north-western South America was shaped by an extensive wetland during the Miocene. This ‘Pebas mega-wetland’ kept a well renowned endemic mollusk and ostracod fauna, which initiated a persisting debate about marine ingressions reaching the center of Amazonia at that time. Due to high endemism, uniformitarian principles are hardly applicable to this biota but also other paleontological, sedimentological and geochemical information led to ambiguous paleoenvironmental interpretations. These results are based on ostracod and foraminiferal assemblages and the oxygen and carbon stable isotopy of their biogenic calcite from an outcrop at the cutbank of the Amazon river (NE-Peru, ~55 km S of Iquitos). While ostracods (e.g., <em>Cyprideis</em>) are able to calcify their carapaces along the entire salinity range, at least low saline conditions are a prerequisite for the biomineralization of calcareous foraminiferan tests. Hence, the finding of calcareous foraminifers (<em>Ammonia</em>, <em>Elphidium</em>), associated mainly with brackish water ostracods, indicates the presence of saline waters. In contrast, δ<sup>18</sup>O- and δ<sup>13</sup>C-analyses performed on co-occurring ostracod valves and foraminiferan tests yielded constantly very light ratios. Such values refer to a pure freshwater environment and are incompatible with the interference of isotopically heavier, marine waters or an evaporative stable isotope enrichment. Based on these opposing data, we hypothesize that the Pebas mega-wetland was episodically influenced by mineralized but isotopically light groundwater discharge. Possibly, the resulting specific hydrochemistry contributed not only to the evolution of the endemic Pebasian fauna but also facilitated the sporadic settlement of euryhaline foraminifers, which mimics short-lived marine incursions.</p>


2018 ◽  
Vol 55 (2) ◽  
pp. 157-165 ◽  
Author(s):  
M. S. B. Oliveira ◽  
L. Lima Corrêa ◽  
L. Prestes ◽  
L. R. Neves ◽  
A. R. P. Brasiliense ◽  
...  

Summary Hoplias malabaricus and Hoplerythrinus unitaeniatus are Erythrinidae family widely distributed in the Amazon River system of great value to both commercial and subsistence fishing for riverine populations. As such, the objective of the present study was to investigate the endoparasite communities of H. malabaricus and H. unitaeniatus of a tributary of the Amazon River in the north of Brazil. The endoparasite communities of H. unitaeniatus and H. malabaricus were taxonomically similar (85%) and consisted of Clinostomum marginatum, Contracaecum sp., Guyanema seriei seriei, Procamallanus (Spirocamallanus) inopinatus, Pseudoproleptus sp. and Gorytocephalus spectabilis, although the dominant endoparasite was C. marginatum, which was the most prevalent and abundant. All the specimens of both H. malabaricus and H. unitaeniatus were parasitized, with a total of 1237 helminths collected in the former host and 1151 helminths collected in the latter. Hoplerythrinus unitaeniatus possessed greater parasite species richness. Both hosts had an aggregate dispersion of parasites, and the abundance of C. marginatum, Contracaecum sp. and G. spectabilis correlated positively with the weight and length of the hosts. The condition factor was not affected by parasitism, but the abundance of C. marginatum and Contracaecum sp. increased when the condition factor of the hosts decreased. This is the first report of G. seriei seriei for H. malabaricus and Pseudoproleptus sp. for H. unitaeniatus.


2011 ◽  
Vol 58 (6) ◽  
pp. 525-528 ◽  
Author(s):  
CARLOS AZEVEDO ◽  
MARIANA RIBEIRO ◽  
SÉRGIO C. S. CLEMENTE ◽  
GRAÇA CASAL ◽  
LEILA LOPES ◽  
...  
Keyword(s):  

Author(s):  
Patrick T. Seyler ◽  
Gerald R. Boaventura

Measurements of trace metals in rivers are of substantial interest for researchers examining basic scientific questions related to geochemical weathering and transport and to scientists involved in pollution control evaluation. Trace metals in natural waters include essential elements such as cobalt, copper, zinc, manganese, iron, molybdenum, nickel, which may also be toxic at higher concentrations, and nonessential elements, which are toxic, such as cadmium, mercury and lead. Recent findings indicate that iron and, to a lesser extent, zinc and manganese play an important role in regulating the growth and ecology of phytoplankton (Martin et al. 1991), while in contrast, cadmium, arsenic, and mercury have long been recognized as poisonous to living organisms (see Pfeiffer et al. 1993, for a description of mercury problem in the Amazon basin). The release of potentially large quantities of these toxic metals, particularly in the river systems of industrialized countries, but also in tropical rivers, is an acute problem of great environmental concern. An understanding of the weathering and transport processes controlling the fate and flux of trace metals in pristine environments is important in evaluating the capacity of receiving waters to accommodate wastes without detrimental effects. The Amazon River system, which is relatively free of industrial and agricultural interference, represents an ideal case for the investigation of the origin and transport of trace metals. This understanding may also provide a scientific basis for the anticipated development of the Amazon basin. With regard to trace metals, Amazon River is still poorly documented. Martin and Meybeck (1979) and Martin and Gordeev (1986) presented a global tabulation of trace metal concentrations in particulate matter of major rivers including the Amazon, and Palmer and Edmond (1992) measured dissolved Fe, Al, and Sr concentrations in the Amazon mainstream and a number of its tributaries. Boyle et al. (1982) and Gordeev et al. (1990) published some data on Cu, Ni, Cd, and Ag dissolved concentrations at the mouth of the Amazon River and in its oceanic plume. Konhauser et al. (1994) reported the trace and rare earth elemental composition of sediments, soils and waters, mainly in the region of Manaus.


2010 ◽  
Vol 99 (3-4) ◽  
pp. 99-124 ◽  
Author(s):  
Edgardo M. Latrubesse ◽  
Mario Cozzuol ◽  
Silane A.F. da Silva-Caminha ◽  
Catherine A. Rigsby ◽  
Maria Lucia Absy ◽  
...  

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