IN-VIVO METABOLISM OF [1-C-14]LINOLENIC ACID (18 3(N-3)) AND [1-C-14]EICOSAPENTAENOIC ACID (20/5(N-3)) IN A MARINE FISH - TIME-COURSE OF THE DESATURATION/ELONGATION PATHWAY/
G. Mourente et Dr. Tocher, IN-VIVO METABOLISM OF [1-C-14]LINOLENIC ACID (18 3(N-3)) AND [1-C-14]EICOSAPENTAENOIC ACID (20/5(N-3)) IN A MARINE FISH - TIME-COURSE OF THE DESATURATION/ELONGATION PATHWAY/, Biochimica et biophysica acta, L. Lipids and lipid metabolism, 1212(1), 1994, pp. 109-118
The metabolism (via the desaturation/elongation pathways) of [1-C-14]1
8:3(n - 3) and [1-C-14]20:5(n - 3) in a marine fish, gilthead sea brea
m (Sparus aurata L.), were investigated over 8 days to determine the t
ime-courses for the production of Delta(6) and Delta(5)-desaturase pro
ducts and 22:6(n - 3). Fish were starved for 1 week prior to, and duri
ng, the period of the experiment. The recovery of radioactivity from [
1-C-14]20:5(n - 3) in tissue lipids exceeded that of [1-C-14]18:3(n -
3) at all time points. The recoveries of both fatty acids decreased by
85-89% between days 2 and 8, indicating that substantial loss of radi
oactivity due to P-oxidation occurred. Incorporation of 18:3(n - 3) an
d 20:5(n - 3) was predominantly into triacylglycerol but during the ti
me-course of the experiment there were decreased percentages of radioa
ctivity from both labelled fatty acids recovered in triacylglycerol wi
th concomitant increased percentages recovered in phospholipids indica
ting preferential oxidation of fatty acids in triacylglycerol and/or r
edistribution of incorporated fatty acids. Recovery of radioactivity i
n 22:6(n - 3) was 10-fold greater with [1-C-14]20:5(n - 3) than with [
1-C-14]18:3(n - 3). However, there were few consistently significant t
rends in the levels of components of the desaturation/elongation pathw
ays during the time-course of the experiment. In particular, the relat
ive recovery of radioactivity in 22:6(n - 3) did not increase during t
he experiment with either substrate. Substantial amounts of radioactiv
ity were found in 24:5(n - 3) and 24:6(n - 3), particularily after inj
ection with [1-C-14]20:5(n - 3), indicating that the conversion of 20:
5(n - 3) to 22:6(n - 3) in sea bream may occur by a pathway utilizing
Delta(6)-desaturase activity rather than by a Delta(4)-desaturation.