Sodium balance in the Australian crayfish Cherax destructor, Euastacus keirensis and E. spinifer (Decapoda : Parastacoidea)

1982 ◽  
Vol 33 (3) ◽  
pp. 507 ◽  
Author(s):  
P Greenaway ◽  
B Lawson
Keyword(s):  
Fresh Water ◽  
Northern Hemisphere ◽  
High Rate ◽  
Sodium Balance ◽  
Sodium Ions ◽  
Sodium Pumps ◽  
Ion Concentrations ◽  
Cherax Destructor

Sodium balance was examined in C. destructor. E. spinifer and E. keirensis to assess the degree of adaptation to fresh water and to permit comparisons with the better known astacoid crayfish of the Northern Hemisphere. The crayfishes had blood ion concentrations close to those reported in the Astacoidea and permeability to sodium ions was similarly low. The affinities of the sodium pumps for sodium ions were relatively low but this was compensated for by an unusually high rate of uptake of sodium following depletion, which enabled sodium balance to be maintained at low external concentrations. Adaptation to fresh water in the species examined is less advanced than in the astacoid species studied.

Sodium Balance in Eriocheir Sinensis (M. EDW.). The Adaptation of the Crustacea to Fresh Water

1961 ◽  
Vol 38 (1) ◽  
pp. 153-162
Author(s):  
J. SHAW
Keyword(s):  
Fresh Water ◽  
Body Surface ◽  
Eriocheir Sinensis ◽  
Vital Role ◽  
The Body ◽  
Sodium Balance ◽  
Progressive Reduction ◽  
Uptake Mechanism ◽  
Active Uptake ◽  
Main Factors

1. In Eriocheir sinensis active uptake of sodium plays a vital role in the maintenance of sodium balance. At external concentrations down to about 6 mM./l. the active uptake mechanism is fully saturated and the uptake rate just balances the rate of loss, which occurs primarily through the body surface. At lower external concentrations balance may be achieved, at least in part, by the activation of the uptake mechanism. 2. A hypothesis is put forward to account for the mechanism of adaptation of the Crustacea to fresh water. Two main factors are involved: (a) a progressive reduction in the permeability of the body surface to salts and, (b) the acquisition of an active uptake mechanism with a high affinity for the ions which it transports. 3. This hypothesis is discussed in relation to previous theories on the adaptation of the Crustacea to fresh water.

Salt and Water Balance in Salmon Smolts

1970 ◽  
Vol 52 (3) ◽  
pp. 553-564
Author(s):  
W. T. W. POTTS ◽  
MARGARET A. FOSTER ◽  
J. W. STATHER
Keyword(s):  
Water Balance ◽  
Fresh Water ◽  
Sodium Pump ◽  
Sea Water ◽  
High Rate ◽  
Exchange Diffusion ◽  
Rapid Changes ◽  
Alternative Hypotheses ◽  
Salt And Water Balance

1. Salmon smolts adapted to sea water maintain a high rate of turnover of both sodium and chloride, but when adapted to fresh water the rate of turnover is low. 2. Only a small part of the influx takes place through the gut. 3. On immediate transfer from sea water to dilute sea water or to fresh water the influxes decline rapidly, but on transfer from fresh water to sea water the restoration of the fluxes takes place slowly. 4. The alternative hypotheses that the rapid changes are due to exchange diffusion or to rapid adjustments of the sodium pump are discussed.

The effects of transecting the IXth and Xth cranial nerves on hydromineral balance in the eel Anguilla anguilla

1976 ◽  
Vol 64 (2) ◽  
pp. 461-475
Author(s):  
N. Mayer-Gostan ◽  
T. Hirano
Keyword(s):  
Fresh Water ◽  
Sea Water ◽  
Cranial Nerves ◽  
Anguilla Anguilla ◽  
Vagus Nerves ◽  
Rapid Reduction ◽  
Ion Concentrations ◽  
Excess Loss ◽  
Na Efflux ◽  
Hydromineral Balance

The IXth and the Xth cranial nerves in Anguilla anguilla were transected, and the effects upon ion and water balance were studied in fresh water and sea water, and during transfer from fresh water and vice versa. In fresh water there is a slow demineralization due to an excess loss of Na and Cl ions. During freshwater to seawater transfer the eel survives only for 4–5 days. The fish do not drink and Na efflux does not increase enough to extrude excess ions. In sea water the glossopharyngeal and vagus nerves are necessary for the maintenance of the hydromineral balance. Denervation is followed by an increase in plasma ion concentrations. Na fluxes are not modified and increased water loss is not compensated by drinking. The rapid reduction of Na efflux during transfer from sea water to fresh water is not modified by denervation.

Crocodilian diversity in space and time: the role of climate in paleoecology and its implication for understanding K/T extinctions

Paleobiology ◽  
1998 ◽  
Vol 24 (4) ◽  
pp. 470-497 ◽  
Author(s):  
Paul J. Markwick
Keyword(s):  
Northern Hemisphere ◽  
Middle Eocene ◽  
Temporal Trends ◽  
Late Eocene ◽  
High Rate ◽  
Mass Extinctions ◽  
Crown Group ◽  
Climatic Effects ◽  
General Decline

The taxonomic diversity of crocodilians (Crocodylia) through the last 100 million years shows a general decline in the number of genera and species to the present day. But this masks a more complex pattern. This is investigated here using a comprehensive database of fossil crocodilians that provides the opportunity to examine spatial and temporal trends, the influence of sampling, and the role of climate in regulating biodiversity.Crown-group crocodilians, comprising the extant families Alligatoridae, Crocodylidae, and Gavialidae, show the following trend: an initial exponential diversification through the Late Cretaceous and Paleocene that is restricted to the Northern Hemisphere until after the K/T boundary; relatively constant diversity from the Paleocene into the middle Eocene that may be an artifact of sampling, which might mask an actual decline in numbers; low diversity during the late Eocene and Oligocene; a second exponential diversification during the Miocene and leveling off in the late Miocene and Pliocene; and a precipitous drop in the Pleistocene and Recent. The coincidence of drops in diversity with global cooling is suggestive of a causal link—during the initial glaciation of Antarctica in the Eocene and Oligocene and the Northern Hemisphere glaciation at the end of the Pliocene. However, matters are complicated in the Northern Hemisphere by the climatic effects of regional uplift.Although the global trend of diversification is unperturbed at the K/T boundary, this is largely due to the exceptionally high rate of origination in the early Paleocene. Nonetheless, the survival of such a demonstrably climate-sensitive group strongly suggests that a climatic explanation for the K/T mass extinctions, especially the demise of the dinosaurs, must be reconsidered.

RENIN, CORTISOL AND PLASMA VOLUME IN MARINE TELEOST FISHES ADAPTED TO DILUTE MEDIA

1976 ◽  
Vol 70 (1) ◽  
pp. 47-59 ◽  
Author(s):  
HIROKO NISHIMURA ◽  
W. H. SAWYER ◽  
R. F. NIGRELLI
Keyword(s):  
Fresh Water ◽  
Plasma Volume ◽  
Renin Angiotensin System ◽  
Plasma Renin ◽  
Sodium Balance ◽  
Plasma Sodium ◽  
Teleost Fishes ◽  
Angiotensin System ◽  
Renin Angiotensin ◽  
American Eels

SUMMARY The renin–angiotensin system has been found in teleost fishes from both marine and freshwater environments. In an attempt to define whether activity of the renin–angiotensin system is related to sodium balance in fishes, we transferred two euryhaline teleosts from seawater to hypo-osmotic media. Plasma renin activity decreased in American eels, Anguilla rostrata, after they were transferred from seawater to fresh water, and it did not change in the aglomerular toadfish, Opsanus tau, after transfer from 50% seawater to 5% seawater. Plasma sodium concentrations decreased significantly in toadfish in 5% seawater and in one group of eels in fresh water. Plasma levels of cortisol, a major mineralocorticoid in teleosts, and plasma volume, measured in eels, remained relatively constant. There are no clear correlations between plasma renin levels and those of plasma sodium or plasma cortisol. These results provide no evidence that the need of these fishes to conserve sodium when in hypo-osmotic media stimulates the renin–angiotensin system.

scholarly journals Virological, epidemiological, clinic, and molecular genetic features of the influenza epidemic in 2015-2016: prevailing of the influenza A(H1N1)09 pdm virus in Russia and countries of the Northern hemisphere

2016 ◽  
Vol 61 (4) ◽  
pp. 159-166
Author(s):  
D. K. Lvov ◽  
E. I. Burtseva ◽  
L. V. Kolobukhina ◽  
I. T. Fedyakina ◽  
E. S. Kirillova ◽  
...  
Keyword(s):  
Northern Hemisphere ◽  
Russian Federation ◽  
Influenza A ◽  
Influenza Viruses ◽  
High Rate ◽  
Research Centre ◽  
Sequencing Data ◽  
Influenza A H1n1 ◽  
Antigenic Properties ◽  
The Russian Federation

This work describes the specific features of the influenza virus circulating in the period from October 2015 to March 2016 in 10 cities of Russia, the basic laboratories of CEEI at the D.I. Ivanovsky Institute of Virology “Federal Research Centre of Epidemilogy and Microbiology named after the honorary academician N.F. Gamaleya” of the Ministry of Health of the Russian Federation. The increase in the morbidity caused by influenza viruses was detected in January-February 2016. The duration of the morbidity peak was 4-5 weeks. The most vulnerable group included children at the age from 3 to 6; a high rate of hospitalization was also detected among people at the age of 15-64 (65%). In clinic symptoms there were middle and severe forms with high frequency of hospitalization as compared with the season of 2009-2010, but much higher in comparison with the season of 2014-2015. Some of the hospitalized patients had virus pneumonias, half of which were bilateral. Among these patients, 10% were children; 30%, adults. The mortality in the intensive care unit of the hospital was 46%. Almost all lethal cases were among unvaccinated patients in the case of late hospitalization and without early antiviral therapy. The predominance of the influenza A(H1N1)09pdm virus both in the Russian Federation and the major part of the countries in the Northern hemisphere was noted. The results of the study of the antigenic properties of influenza strains of A(H1N1)pdm09 virus did not reveal any differences with respect to the vaccine virus. The sequencing data showed the amino acid substitutions in hemagglutinin (receptor binding and Sa sites) and in genes encoding internal proteins (PA, NP, M1, NS1). Strains were sensitive to oseltamivir and zanamivir and maintained resistance to rimantadine. The participation of non-influenza ARI viruses was comparable to that in preliminary epidemic seasons.

Sodium Regulation and Adaptation to Fresh Water in the Isopod Genus Asellus

1974 ◽  
Vol 61 (3) ◽  
pp. 719-736
Author(s):  
D. W. SUTCLIFFE
Keyword(s):  
Fresh Water ◽  
Loss Rate ◽  
The Body ◽  
Sodium Balance ◽  
Short History ◽  
Sodium Influx ◽  
Km Value ◽  
Sodium Regulation ◽  
Natural Series ◽  
Total Concentrations

1. The principal features of the sodium regulatory mechanism are compared in Asellus communis Say, A. aquaticus (L.) and A. meridianus Rac. 2. Water content and total concentrations of sodium and chloride are similar in the three species, but they differ with respect to values for Kmax, Km, the loss rate, and the minimum sodium balance concentration. 3. It is suggested that A. meridianus, A. aquaticus and A. communis represent a natural series of increasing adaptation to fresh water. A. communis from North America is completely adapted to fresh water. It has the lowest loss rate, the lowest maximum saturation level (Kmax) for sodium influx, and the highest affinity (low Km value) for sodium ions in the transporting system at the body surface. In many respects A. meridianus resembles freshwater populations of Mesidotea entomon and Gammarus duebeni, and may therefore have had a relatively short history in fresh water.

Isotope geochemistry of stratified Lake "A," Ellesmere Island, N.W.T., Canada

1984 ◽  
Vol 21 (9) ◽  
pp. 1008-1017 ◽  
Author(s):  
M. O. Jeffries ◽  
H. R. Krouse ◽  
M. A. Shakur ◽  
S. A. Harris
Keyword(s):  
Stable Isotope ◽  
Fresh Water ◽  
Isotope Geochemistry ◽  
Ionic Composition ◽  
Ellesmere Island ◽  
Ocean Water ◽  
Cation Composition ◽  
Stratified Lake ◽  
Ion Concentrations ◽  
Different Depths

Ionic composition, salinity, temperature, pH, tritium, and stable isotope compositions of water and ions were determined for samples collected in 1969 and 1982 from different depths of stratified Lake "A" on Ellesmere Island. Tritium contents and ionic and stable isotope compositions were diagnostic of recent fresh water overlying older, deeper trapped seawater. A temperature maximum occurs at 15 m in the freshwater–seawater transition zone. Salinity, δ18O, and δD data suggest that the lake evaporated slightly and acquired about 12% fresh water prior to stratification. Individual ion concentrations reveal a slightly modified cation composition and marked depletions in sulphate and enrichments in dissolved carbonate compared with modern ocean water. The δ34S, δ18O, and δ13C data for [Formula: see text] and [Formula: see text] attest to extensive anaerobic [Formula: see text] reduction during the lake's history.

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