The Composition and Origin of the Foetal Fluids of the Pig

نویسندگان

  • T. DICKERSON
  • J. W. T. DICKERSON
چکیده

MANY of the unicellular organisms have a greater concentration of osmotically active material within their body fluids than there is in the medium surrounding them, and the higher animals have glands like the kidney and sweat glands which are able to elaborate fluids with much lower concentrations of sodium and chloride than the body-fluids from which they were derived. The concentrations of sodium and chloride in hypotonic urine and sweat are much lower than those in the serum, and consequently the total osmolar concentrations are also lower, but the urea is characteristically higher. There is no proof that the process is one involving the secretion of water; and, indeed, the kidney is now thought to produce a hypotonic urine by the active reabsorption of sodium from the distal tubule, the walls of which are impermeable to water unless there is posterior pituitary hormone in the circulation. The foetal fluids and membranes deserve more consideration in this connexion than they have hitherto received. Jacque (1903-4, 1905-6) pointed out that the allantoic fluid of the sheep was hypotonic and propounded the theory that this fluid was largely foetal urine which he also demonstrated to be hypotonic. This idea has been brought up to date by McDougall (1949) and by Alexander, Nixon, Widdas, & Wohlzogen (1955 a, b). Paton, Watson, & Kerr (1908-9) discussed the whole question of the origin of foetal fluids—human and otherwise—in the light of the knowledge which existed at that time. There is no doubt, as they pointed out, that these fluids are of foetal origin, but the progress of knowledge as to their nature and origin has always been obscured by (i) the great variability in their volume and composition even between littermates and certainly with the progress of gestation, (ii) obvious species differences, (iii) a tendency to compare their composition with foetal urine, rather than with foetal or maternal serum, (iv) a failure to appreciate the importance of their total osmolar concentration, and (v) neglecting to search for general principles and generalizations. Davies & Routh (1957) have recently made out a strong case for regarding the allantoic fluid of the rabbit as the product of the foetal mesonephros. Their essential findings have been confirmed (Dickerson & McCance, 1957) and the

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

PHY SICO-CHEMICAL CHARACTERISTICS OF MINERALIZING FLUIDS AT THE KAMARMEHDI MINE, TABAS REGION, IRAN

The data obtained from field and geothermometric studies and also the REE composition of fluorites associated with lead mineralization at the Kamar-Mehdi mine are compatible with a structurally controlled, fissure filling, epigenetic, hydrothermal origin. Homogenization and last ice melting temperatures for primary fluid inclusions trapped in fluorite crystals indicate that the mineralizati...

متن کامل

Tracing the Pig and Cattle Origin in Processed Food and Feed Products Targeting Mitochondrial 12S rRNA Gene

Background: Species identification in commercially processed food and feed products is one of the important issues. This study was conducted to develop a genetic method for the detection of pig and cattle species in processed food and feed products using newly designed species-specific primers targeting mitochondrial 12S rRNA gene fragments. Methods: Two sets of specific primers were designed ...

متن کامل

Investigation of genesis and fluid origin in Noghduz gold bearing quartz veins, East Azarbaijan Province, northwest of Iran

The Noghduz  prospecting area, as a part of the Arasbaran metallogenic zone is located about 20 km east of Ahar, East-Azarbaijan Province. The mineralization host rocks are andesite-trachy andesite with the age of  Late  Eocene. The hydrothermal alterations exposed in this area are silicic, argillic, and propylitic. Pyrite is the main hypogene sulfide mineral which is accompanied by lesser amou...

متن کامل

تورمالین‌زایی در توده گرانیتوئیدی رودگز، جنوب بجستان، خراسان رضوی

Roudgaz granitoid is located in south of Bajestan. In this granitoid body, tourmaline occurred in two forms, as luxullianite and as veins of quartz-tourmaline with a 30 cm width. Based on petrography and electron microprobe analyses data, these tourmalines are schorl-dravite- foitite in composition, with a tendency toward schorl end member, and belongs to alkali and vacancies groups. In compari...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2008