Chyme entering the intestine from the stomach through the pyloric sphincter is typically neutralized quickly, despite at high feeding rates, acidic chyme might persist in the anterior intestine for part time (e.g., usher et al., 1990).
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From: Fish Physiology, 2019
Chris M. Wood, in Fish Physiology, 2019
Chyme entering the intestine from the stomach with the pyloric sphincter is normally neutralized quickly, despite at high feeding rates, acidic chyme might persist in the anterior intestine for part time (e.g., water level et al., 1990). Advertising food pellets space acidic as soon as hydrated (pH = 5.0–6.0), and also even in the agastric killifish, acidic chyme was existing in the anterior intestine in ~ 1–3 h postfeeding, yet was neutralized through 12–24 h (Wood et al., 2010). As for fasted animals, the potential role of the kidneys in this neutralization stays unknown, yet intestinal HCO3− secretion is certainly connected (Fig. 1).
The first-feeding related examination of intestinal HCO3− metabolism in seawater teleosts reported that rectal liquid samples contained around twofold higher HCO3−, measured together titratable base, in starved matches fed rainbow trout (Wilson et al., 1996), yet secretion and excretion prices were no measured. However a later study in the same species, making use of in vitro gut sac preparations, recorded a clean stimulation of intestinal HCO3− secretion complying with feeding, varying from four- to sevenfold in various sections of the intestine (Bucking et al., 2009). In the toadfish, Taylor and Grosell (2006b) tape-recorded an approximate copy of
The neuroendocrine, mechanical, and/or chemical signals for elevating minister HCO3− cheap after feeding have actually yet to it is in identified, though low pH in the chyme is believed to be an important stimulus (Holmgren and also Olsson, 2011); this is an essential area for future investigation. However, there space at the very least three obvious functional benefits. The an initial is to help neutralize the higher HCl cheap coming into the tract from the stomach, and also indirectly combination to this, the second is to aid clear the postprandial “alkaline tide” in the systemic blood currently (Bucking et al., 2009) brought about by this elevated gastric HCl secretion (Fig. 1; ar 3.3). The third is to promote intestinal water absorb at a time once the osmotic gradient the opposite this process will it is in greater due to the organic and also inorganic osmolytes originating from the food (Bucking et al., 2011; Taylor and also Grosell, 2006a,b).
The agastric seawater-acclimated killifish presents an interesting comparison (Wood et al., 2010). The HCO3− in the intestinal fluids to be markedly depressed at 1–3 h after feeding, and simply went back to the fasting level (which was quite low ~ 16 mmol L− 1; Fig. 2A) at 12–24 h. In gut sac preparations, the net rate of HCO3− secretion was also depressed after ~ feeding, even though Cl− and water absorption were elevated. The mystery was solved by the identification of an H+ pumping device (vH+ ATPase) that was active at this time, to run in parallel come Cl−/HCO3− exchange, as questioned in ar 2.1.3 (Fig. 1). Once this was inhibited through bafilomycin, the net prices of HCO3− secretion, Cl− absorption, and water absorption all increased.
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The killifish data administer evidence that the “CO2 recycling” system to enhance intestinal HCO3− cheap (Fig. 1; ar 2.1.3) might become much more important ~ feeding in naval teleosts. In killifish gut sacs, PCO2 key was biggest at 1–3 h postfeeding, and was lessened by bafilomycin and by fasting (Wood et al., 2010). Calculation PCO2 in intestinal chyme samples indigenous live killifish were roughly 78 torr in ~ 1–3 h and 22 torr at 12–24 h postfeeding, and an in similar way declined v fasting (Fig. 2B). As the stomach is absent, elevated chyme PCO2 obviously cannot originate from gastric HCl activity on ingested food. Calculated minister PCO2 was also elevated after feeding (22 torr in ~ 24 h matches 3 torr in fasting animals) in the gastric gulf toadfish (Taylor and Grosell, 2006b). Our recent straight PCO2 measurements in the anterior intestine that the gastric lemon sole show that PCO2 rises to over 50 torr after a meal, with similar values in other segments (E.H. Jung, J. Eom, and also C.M. Wood, unpublished). All these observations suggest an increased role for “CO2 recycling” after feeding. The algivorous Magadi tilapia (Alcolapia grahami) provides severe example. This varieties has a extremely acidic stomach (pH = 3.5) in order to digest the cell walls of cyanobacteria (Bergman et al., 2003). However, it stays in a bizarre, extremely alkaline but salty environment (pH = 10, titration alkalinity HCO3− > 250 mmol L− 1, osmolality ~ 60% seawater values) and also must drink the tool for osmoregulation (Wood et al., 2002). This species has progressed a distinctive anatomical shunting device so that drinking the the extremely alkaline water have the right to bypass the highly acidic stomach, staying clear of potentially fatal CO2 generation (Bergman et al., 2003). Nevertheless, HCO3− (measured through titration) in the chyme that the anterior intestine to be 157 mmol L− 1 in naturally feeding pets (Fig. 2A) and also calculated PCO2 was greater than 700 torr (Fig. 2B), the greatest values ever recorded because that a teleost fish.