The earthworm intestine has four physiologically distinct regions with varying ion transport properties, well-suited for conserving sodium in vivo.
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Caution against clinical translation from earthworm data; leaves open comparative studies on intestinal sodium transport segmentation.
Measurements of electrical potential difference (PD), short-circuit current (SCC) and unidirectional fluxes of sodium and chloride were made across portions of the intestine. Based on the results, the intestine can be divided into at least four physiologically distinct regions. 2. These four physiological regions, designated from anterior to posterior as R I-II, R III A, R III B and R IV, do not completely correspond to the four anatomically distinct regions of the intestine. 3. The PD (serosal side positive) in R I-II, R III A, R III B and R IV is 1.08, 12.4, 5.61 and 31.7 mV, respectively. 4. The SCC in these same regions is 9.9, 50.4, 49.7, and 16.4 micro A cm2, respectively. 5. When short-circuited, net sodium and net chloride fluxes in the above regions are -0.36 and -0.27, 1.46*** and -0.92*, 1.74*** and -0.06 and 1.01*** and 0.07 mumol cm-2 h-1, respectively. Positive fluxes indicate net mucosal to serosal movements and asterisks indicate significant net fluxes (* P less than 0.05, *** P less than 0.001). 6. There is good agreement between the SCC and net sodium transport in R III B. In the other regions of the intestine the ionic basis of the SCC has not been completely explained. 7. The properties of the intestine in vitro appear to make the intestine well suited for the task of conserving sodium, a function which the intestine performs in vivo.
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John Cornell (1982) studied this question.
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